Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-555-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-15-555-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| Highlight paper
| 
27 Mar 2019
Review article | Highlight paper |
| 27 Mar 2019
| 27 Mar 2019
The 4.2 ka BP Event in the Mediterranean region: an overview
Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy
Giovanni Zanchetta
Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy
Aurel Perşoiu
Emil Racoviţă Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania
Rosine Cartier
Quaternary Sciences, Department of Geology, Lund University, Lund, Sweden
Albert Català
GRC Geociències Marines, Departament de Dinàmica de la Terra i de l'Oceà,
Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain
Isabel Cacho
GRC Geociències Marines, Departament de Dinàmica de la Terra i de l'Oceà,
Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain
Jonathan R. Dean
School of Environmental Sciences, University of Hull, Hull, UK
Federico Di Rita
Dipartimento di Biologia Ambientale, University of Rome “La Sapienza”, Rome, Italy
Russell N. Drysdale
School of Geography, University of Melbourne, Melbourne, Australia
Martin Finnè
Department of Archaeology and Ancient History, Uppsala University, Uppsala,
Sweden
Department of Physical Geography, Stockholm University, Stockholm, Sweden
Ilaria Isola
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Pisa, Italy
Bassem Jalali
LOCEAN Laboratory, Sorbonne Universités (UPMC, Universitè de Paris 06)-CNRS-IRD-MNHN, Paris, France
Fabrizio Lirer
Istituto di Scienze Marine (ISMAR)-CNR Napoli, Naples, Italy
Donatella Magri
Dipartimento di Biologia Ambientale, University of Rome “La Sapienza”, Rome, Italy
Alessia Masi
Dipartimento di Biologia Ambientale, University of Rome “La Sapienza”, Rome, Italy
Leszek Marks
Faculty of Geology, University of Warsaw, Warsaw, Poland
Anna Maria Mercuri
Dipartimento di Scienze della Vita, Università di Reggio Emilia e Modena, Modena, Italy
Odile Peyron
Institut des Sciences de l'Evolution (ISEM), Université de Montpellier, Montpellier, France
Laura Sadori
Dipartimento di Biologia Ambientale, University of Rome “La Sapienza”, Rome, Italy
Marie-Alexandrine Sicre
LOCEAN Laboratory, Sorbonne Universités (UPMC, Universitè de Paris 06)-CNRS-IRD-MNHN, Paris, France
Fabian Welc
Institute of Archaeology, Cardinal Stefan Wyszynski University, Warsaw, Poland
Christoph Zielhofer
Chair of Physical Geography, Leipzig University, Leipzig, Germany
Elodie Brisset
IPHES, Institut Català de Paleoecologia Humana i Evolució Social, Tarragona,
Spain
Àrea de Prehistòria, Universitat Rovira i Virgili, Tarragona, Spain
Related authors
Fabrizio Marra, Alberto Frepoli, Dario Gioia, Marcello Schiattarella, Andrea Tertulliani, Monica Bini, Gaetano De Luca, and Marco Luppichini
Nat. Hazards Earth Syst. Sci., 22, 2445–2457, https://doi.org/10.5194/nhess-22-2445-2022, https://doi.org/10.5194/nhess-22-2445-2022, 2022
Short summary
Short summary
Through the analysis of the morphostructural setting in which the seismicity of Rome is framed, we explain why the city should not expect to suffer damage from a big earthquake.
Ilaria Isola, Giovanni Zanchetta, Russell N. Drysdale, Eleonora Regattieri, Monica Bini, Petra Bajo, John C. Hellstrom, Ilaria Baneschi, Piero Lionello, Jon Woodhead, and Alan Greig
Clim. Past, 15, 135–151, https://doi.org/10.5194/cp-15-135-2019, https://doi.org/10.5194/cp-15-135-2019, 2019
Short summary
Short summary
To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
Christoph Zielhofer, Marie Kaniecki, Anne Köhler, Vera Seeburg, Arnela Rollo, Laura Bergmann, Stefanie Berg, Barbara Stammel, Rita Gudermann, William J. Fletcher, Ulrike Werban, Anja Linstädter, and Natascha Mehler
E&G Quaternary Sci. J., 74, 105–124, https://doi.org/10.5194/egqsj-74-105-2025, https://doi.org/10.5194/egqsj-74-105-2025, 2025
Short summary
Short summary
This study presents a quantitative reconstruction over a 235-year time frame of the development of the natural Donaumoos fen and Danube River into an anthroposphere. The selected proxies are the Donaumoos drainage ditch length and the Danube surface water area traced through the multi-temporal analysis of old maps. A comparison of quantitative proxies with the state of research from written sources leads to the discovery of potential great transitions in floodplain and peatland transformation.
Himadri Saini, David K. Hutchinson, Josephine R. Brown, Russell N. Drysdale, Yanxuan Du, and Laurie Menviel
EGUsphere, https://doi.org/10.5194/egusphere-2025-1990, https://doi.org/10.5194/egusphere-2025-1990, 2025
This preprint is open for discussion and under review for Climate of the Past (CP).
Short summary
Short summary
This study examines how large ice sheets during the last Ice Age influenced global weather patterns. We found that the presence of these ice sheets affected rainfall patterns in regions like Eurasia and Australia. By altering wind and weather systems, they shifted the position of the tropical rainbelt and impacted the circulation of air in both the Northern and Southern Hemispheres. Our research helps us understand past climate changes and their potential effects on future climate patterns.
Calla N. Gould-Whaley, Russell N. Drysdale, Pauline C. Treble, Jan-Hendrik May, Stacey C. Priestley, John C. Hellstrom, Christopher R. Vardanega, and Clare C. Buswell
Clim. Past, 21, 857–876, https://doi.org/10.5194/cp-21-857-2025, https://doi.org/10.5194/cp-21-857-2025, 2025
Short summary
Short summary
Climate change is causing enhanced aridity across many regions of the globe, leading to increased reliance on groundwater resources. We need to understand how groundwater recharge behaves in arid regions over long timescales; unfortunately, arid landscapes tend to preserve very little evidence of their climatic past. We present evidence to suggest that carbonate formations that grow in groundwater can be used as archives of past groundwater recharge in Australia's arid zone.
Léa d'Oliveira, Sébastien Joannin, Guillemette Ménot, Nathalie Combourieu-Nebout, Lucas Dugerdil, Marion Blache, Mary Robles, Assunta Florenzano, Alessia Masi, Anna Maria Mercuri, Laura Sadori, Marie Balasse, and Odile Peyron
EGUsphere, https://doi.org/10.5194/egusphere-2025-1106, https://doi.org/10.5194/egusphere-2025-1106, 2025
This preprint is open for discussion and under review for Climate of the Past (CP).
Short summary
Short summary
We studied climate change in the central Mediterranean during the Holocene by analysing 38 pollen records. Several methods were used to obtain reliable results on seasonal temperatures and precipitation. Our results show that, during the Holocene, summer temperatures were colder in the south and warmer in the north, with wetter winters and drier summers, especially in the south. Unlike winter conditions, summers ones did not follow variations in insolation, suggesting other factors.
Amy Cromartie, Cindy De Jonge, Guillemette Ménot, Mary Robles, Lucas Dugerdil, Odile Peyron, Marta Rodrigo-Gámiz, Jon Camuera, Maria Jose Ramos-Roman, Gonzalo Jiménez-Moreno, Claude Colombié, Lilit Sahakyan, and Sébastien Joannin
EGUsphere, https://doi.org/10.5194/egusphere-2025-526, https://doi.org/10.5194/egusphere-2025-526, 2025
Short summary
Short summary
BrGDGT are a molecular biomarker utilized for paleotemperature reconstructions. One issue, however, with utilizing brGDGTs is that the distribution differs in relation to sediment environments (i.e., peat, lake, soil) which change overtime. We utilize the probability estimate outputs from five machine learning algorithms, and a new modern brGDGTs database to track change and apply these models’ to two downcore records utilizing pollen and non-pollen polymorphs to confirm the model’s accuracy.
Dael Sassoon, Nathalie Combourieu-Nebout, Odile Peyron, Adele Bertini, Francesco Toti, Vincent Lebreton, and Marie-Hélène Moncel
Clim. Past, 21, 489–515, https://doi.org/10.5194/cp-21-489-2025, https://doi.org/10.5194/cp-21-489-2025, 2025
Short summary
Short summary
Climatic reconstructions of Marine Isotope Stages (MISs) 19, 11, and 5 and the current interglacial (MIS 1) based on pollen data from a marine core (Alboran Sea) show that, compared with MIS 1, MIS 19 was colder and highly variable, MIS 11 was longer and more stable, and MIS 5 was warmer. There is no real equivalent to the current interglacial, but past interglacials give insights into the sensitivity of the southwestern Mediterranean to global climatic changes in conditions similar to MIS 1.
Mary Robles, Valérie Andrieu, Pierre Rochette, Séverine Fauquette, Odile Peyron, François Demory, Oktay Parlak, Eliane Charrat, Belinda Gambin, and Mehmet Cihat Alçiçek
EGUsphere, https://doi.org/10.5194/egusphere-2025-174, https://doi.org/10.5194/egusphere-2025-174, 2025
Short summary
Short summary
This study aims to characterize the vegetation and lake dynamics based on pollen and Non-Pollen Palynomorph (NPP) proxies, to quantitatively reconstruct climate changes using a multimethod approach and to morphologically characterize the large pollen grains of Poaceae (Cerealia-type).
Judit Torner, Isabel Cacho, Heather Stoll, Ana Moreno, Joan O. Grimalt, Francisco J. Sierro, Joan J. Fornós, Hai Cheng, and R. Lawrence Edwards
Clim. Past, 21, 465–487, https://doi.org/10.5194/cp-21-465-2025, https://doi.org/10.5194/cp-21-465-2025, 2025
Short summary
Short summary
We offer a clearer view of the timing of three relevant past glacial terminations. By analyzing the climatic signal recorded in stalagmite and linking it with marine records, we revealed differences in the intensity and duration of the ice melting associated with these three key deglaciations. This study shows that some deglaciations began earlier than previously thought; this improves our understanding of natural climate processes, helping us to contextualize current climate change.
Bassem Jalali, Marie-Alexandrine Sicre, Jian Ren, Zhongqiao Li, Youcheng Bai, Liang Su, Vincent Klein, and Jianfang Chen
EGUsphere, https://doi.org/10.5194/egusphere-2025-325, https://doi.org/10.5194/egusphere-2025-325, 2025
Short summary
Short summary
This work investigates the spatiotemporal variations of terrestrial material from surface and core sediments from the Chukchi Sea using bulk parameters and biomarkers. We found a growing imprint of terrestrial material at higher latitudes resulting from the transport of eroded matter or remobilized from shelf sediments by sea ice. The 300 year TERR-alkanes and ACL27-31 composites from 5 cores evidence increasing export of terrestrial carbon since the early 20th century accelerating after 1980.
Biagio Giaccio, Bernd Wagner, Giovanni Zanchetta, Adele Bertini, Gian Paolo Cavinato, Roberto de Franco, Fabio Florindo, David A. Hodell, Thomas A. Neubauer, Sebastien Nomade, Alison Pereira, Laura Sadori, Sara Satolli, Polychronis C. Tzedakis, Paul Albert, Paolo Boncio, Cindy De Jonge, Alexander Francke, Christine Heim, Alessia Masi, Marta Marchegiano, Helen M. Roberts, Anders Noren, and the MEME team
Sci. Dril., 33, 249–266, https://doi.org/10.5194/sd-33-249-2024, https://doi.org/10.5194/sd-33-249-2024, 2024
Short summary
Short summary
A total of 42 Earth scientists from 14 countries met in Gioia dei Marsi, central Italy, on 23 to 27 October 2023 to explore the potential for deep drilling of the thick lake sediment sequence of the Fucino Basin. The aim was to reconstruct the history of climate, ecosystem, and biodiversity changes and of the explosive volcanism and tectonics in central Italy over the last 3.5 million years, constrained by a detailed radiometric chronology.
Frédéric Parrenin, Marie Bouchet, Christo Buizert, Emilie Capron, Ellen Corrick, Russell Drysdale, Kenji Kawamura, Amaëlle Landais, Robert Mulvaney, Ikumi Oyabu, and Sune Olander Rasmussen
Geosci. Model Dev., 17, 8735–8750, https://doi.org/10.5194/gmd-17-8735-2024, https://doi.org/10.5194/gmd-17-8735-2024, 2024
Short summary
Short summary
The Paleochrono-1.1 probabilistic dating model allows users to derive a common and optimized chronology for several paleoclimatic sites from various archives (ice cores, speleothems, marine cores, lake cores, etc.). It combines prior sedimentation scenarios with chronological information such as dated horizons, dated intervals, stratigraphic links and (for ice cores) Δdepth observations. Paleochrono-1.1 is available under an open-source license.
Juan Luis Bernal-Wormull, Ana Moreno, Yuri Dublyansky, Christoph Spötl, Reyes Giménez, Carlos Pérez-Mejías, Miguel Bartolomé, Martin Arriolabengoa, Eneko Iriarte, Isabel Cacho, Richard Lawrence Edwards, and Hai Cheng
EGUsphere, https://doi.org/10.5194/egusphere-2024-3612, https://doi.org/10.5194/egusphere-2024-3612, 2024
Short summary
Short summary
We present in this manuscript a record of temperature changes during the last deglaciation and the Holocene using isotopes of fluid inclusions in stalagmites from the northeastern region of the Iberian Peninsula. This innovative climate proxy for this study region provides a quantitative understanding of the abrupt temperature changes in southern Europe of the last 16500 years before present.
Timothy J. Pollard, Jon D. Woodhead, Russell N. Drysdale, R. Lawrence Edwards, Xianglei Li, Ashlea N. Wainwright, Mathieu Pythoud, Hai Cheng, John C. Hellstrom, Ilaria Isola, Eleonora Regattieri, Giovanni Zanchetta, and Dylan S. Parmenter
EGUsphere, https://doi.org/10.5194/egusphere-2024-3594, https://doi.org/10.5194/egusphere-2024-3594, 2024
Short summary
Short summary
The uranium-thorium and uranium-lead radiometric dating methods are both capable of dating carbonate samples ranging in age from about 400,000 to 650,000 years. Here we test agreement between the two methods by 'double dating' speleothems (i.e. secondary cave mineral deposits) that grew within this age range. We demonstrate excellent agreement between the two dating methods and discuss their relative strengths and weaknesses.
Marco M. Lehmann, Josie Geris, Ilja van Meerveld, Daniele Penna, Youri Rothfuss, Matteo Verdone, Pertti Ala-Aho, Matyas Arvai, Alise Babre, Philippe Balandier, Fabian Bernhard, Lukrecija Butorac, Simon Damien Carrière, Natalie C. Ceperley, Zuosinan Chen, Alicia Correa, Haoyu Diao, David Dubbert, Maren Dubbert, Fabio Ercoli, Marius G. Floriancic, Teresa E. Gimeno, Damien Gounelle, Frank Hagedorn, Christophe Hissler, Frédéric Huneau, Alberto Iraheta, Tamara Jakovljević, Nerantzis Kazakis, Zoltan Kern, Karl Knaebel, Johannes Kobler, Jiří Kocum, Charlotte Koeber, Gerbrand Koren, Angelika Kübert, Dawid Kupka, Samuel Le Gall, Aleksi Lehtonen, Thomas Leydier, Philippe Malagoli, Francesca Sofia Manca di Villahermosa, Chiara Marchina, Núria Martínez-Carreras, Nicolas Martin-StPaul, Hannu Marttila, Aline Meyer Oliveira, Gaël Monvoisin, Natalie Orlowski, Kadi Palmik-Das, Aurel Persoiu, Andrei Popa, Egor Prikaziuk, Cécile Quantin, Katja T. Rinne-Garmston, Clara Rohde, Martin Sanda, Matthias Saurer, Daniel Schulz, Michael Paul Stockinger, Christine Stumpp, Jean-Stéphane Venisse, Lukas Vlcek, Stylianos Voudouris, Björn Weeser, Mark E. Wilkinson, Giulia Zuecco, and Katrin Meusburger
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-409, https://doi.org/10.5194/essd-2024-409, 2024
Preprint under review for ESSD
Short summary
Short summary
This study describes a unique large-scale isotope dataset to study water dynamics in European forests. Researchers collected data from 40 beech and spruce forest sites in spring and summer 2023, using a standardized method to ensure consistency. The results show that water sources for trees change between seasons and vary by tree species. This large dataset offers valuable information for understanding plant water use, improving ecohydrological models, and mapping water cycles across Europe.
Mauro Antonio Di Vito, Ilaria Rucco, Sandro de Vita, Domenico Maria Doronzo, Marina Bisson, Mattia de' Michieli Vitturi, Mauro Rosi, Laura Sandri, Giovanni Zanchetta, Elena Zanella, and Antonio Costa
Solid Earth, 15, 405–436, https://doi.org/10.5194/se-15-405-2024, https://doi.org/10.5194/se-15-405-2024, 2024
Short summary
Short summary
We study the distribution of two historical pyroclastic fall–flow and lahar deposits from the sub-Plinian Vesuvius eruptions of 472 CE Pollena and 1631. The motivation comes directly from the widely distributed impact that both the eruptions and lahar phenomena had on the Campanian territory, not only around the volcano but also down the nearby Apennine valleys. Data on about 500 stratigraphic sections and modeling allowed us to evaluate the physical and dynamical impact of these phenomena.
Miguel Bartolomé, Ana Moreno, Carlos Sancho, Isabel Cacho, Heather Stoll, Negar Haghipour, Ánchel Belmonte, Christoph Spötl, John Hellstrom, R. Lawrence Edwards, and Hai Cheng
Clim. Past, 20, 467–494, https://doi.org/10.5194/cp-20-467-2024, https://doi.org/10.5194/cp-20-467-2024, 2024
Short summary
Short summary
Reconstructing past temperatures at regional scales during the Common Era is necessary to place the current warming in the context of natural climate variability. We present a climate reconstruction based on eight stalagmites from four caves in the Pyrenees, NE Spain. These stalagmites were dated precisely and analysed for their oxygen isotopes, which appear dominated by temperature changes. Solar variability and major volcanic eruptions are the two main drivers of observed climate variability.
Philip Meister, Anne Alexandre, Hannah Bailey, Philip Barker, Boris K. Biskaborn, Ellie Broadman, Rosine Cartier, Bernhard Chapligin, Martine Couapel, Jonathan R. Dean, Bernhard Diekmann, Poppy Harding, Andrew C. G. Henderson, Armand Hernandez, Ulrike Herzschuh, Svetlana S. Kostrova, Jack Lacey, Melanie J. Leng, Andreas Lücke, Anson W. Mackay, Eniko Katalin Magyari, Biljana Narancic, Cécile Porchier, Gunhild Rosqvist, Aldo Shemesh, Corinne Sonzogni, George E. A. Swann, Florence Sylvestre, and Hanno Meyer
Clim. Past, 20, 363–392, https://doi.org/10.5194/cp-20-363-2024, https://doi.org/10.5194/cp-20-363-2024, 2024
Short summary
Short summary
This paper presents the first comprehensive compilation of diatom oxygen isotope records in lake sediments (δ18OBSi), supported by lake basin parameters. We infer the spatial and temporal coverage of δ18OBSi records and discuss common hemispheric trends on centennial and millennial timescales. Key results are common patterns for hydrologically open lakes in Northern Hemisphere extratropical regions during the Holocene corresponding to known climatic epochs, i.e. the Holocene Thermal Maximum.
Youcheng Bai, Marie-Alexandrine Sicre, Jian Ren, Vincent Klein, Haiyan Jin, and Jianfang Chen
Biogeosciences, 21, 689–709, https://doi.org/10.5194/bg-21-689-2024, https://doi.org/10.5194/bg-21-689-2024, 2024
Short summary
Short summary
Algal biomarkers were used to assess sea ice and pelagic algal production across the western Arctic Ocean with changing sea-ice conditions. They show three distinct areas along with a marked latitudinal gradient of sea ice over pelagic algal production in surface sediments that are reflected by the H-Print index. Our data also show that efficient grazing consumption accounted for the dramatic decrease of diatom-derived biomarkers in sediments compared to that of particulate matter.
Léa d'Oliveira, Lucas Dugerdil, Guillemette Ménot, Allowen Evin, Serge D. Muller, Salomé Ansanay-Alex, Julien Azuara, Colline Bonnet, Laurent Bremond, Mehmet Shah, and Odile Peyron
Clim. Past, 19, 2127–2156, https://doi.org/10.5194/cp-19-2127-2023, https://doi.org/10.5194/cp-19-2127-2023, 2023
Short summary
Short summary
In southern Europe, Holocene climate variability is characterized by a strong heterogeneity whose patterns are still poorly understood. Here, a multi-proxy approach (pollen and biomarkers) is applied to the Canroute sequence to reconstruct the climatic variation over the last 15 000 years in southern Massif Central, France. Results reveal that reconstructions of regional climate trends notably differ depending on proxies and sites, notably concerning the presence of a Holocene thermal maximum.
Frida S. Hoem, Adrián López-Quirós, Suzanna van de Lagemaat, Johan Etourneau, Marie-Alexandrine Sicre, Carlota Escutia, Henk Brinkhuis, Francien Peterse, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 19, 1931–1949, https://doi.org/10.5194/cp-19-1931-2023, https://doi.org/10.5194/cp-19-1931-2023, 2023
Short summary
Short summary
We present two new sea surface temperature (SST) records in comparison with available SST records to reconstruct South Atlantic paleoceanographic evolution. Our results show a low SST gradient in the Eocene–early Oligocene due to the persistent gyral circulation. A higher SST gradient in the Middle–Late Miocene infers a stronger circumpolar current. The southern South Atlantic was the coldest region in the Southern Ocean and likely the main deep-water formation location in the Middle Miocene.
Ulrike Herzschuh, Thomas Böhmer, Manuel Chevalier, Raphaël Hébert, Anne Dallmeyer, Chenzhi Li, Xianyong Cao, Odile Peyron, Larisa Nazarova, Elena Y. Novenko, Jungjae Park, Natalia A. Rudaya, Frank Schlütz, Lyudmila S. Shumilovskikh, Pavel E. Tarasov, Yongbo Wang, Ruilin Wen, Qinghai Xu, and Zhuo Zheng
Clim. Past, 19, 1481–1506, https://doi.org/10.5194/cp-19-1481-2023, https://doi.org/10.5194/cp-19-1481-2023, 2023
Short summary
Short summary
A mismatch between model- and proxy-based Holocene climate change may partially originate from the poor spatial coverage of climate reconstructions. Here we investigate quantitative reconstructions of mean annual temperature and annual precipitation from 1908 pollen records in the Northern Hemisphere. Trends show strong latitudinal patterns and differ between (sub-)continents. Our work contributes to a better understanding of the global mean.
Liang Su, Jian Ren, Marie-Alexandrine Sicre, Youcheng Bai, Ruoshi Zhao, Xibing Han, Zhongqiao Li, Haiyan Jin, Anatolii S. Astakhov, Xuefa Shi, and Jianfang Chen
Clim. Past, 19, 1305–1320, https://doi.org/10.5194/cp-19-1305-2023, https://doi.org/10.5194/cp-19-1305-2023, 2023
Short summary
Short summary
We reconstructed sea ice and organic carbon composition variabilities based on biomarkers and carbon stable isotopes in the northern Chukchi Sea, western Arctic Ocean, over the past 200 years. Under permanent ice cover, organic carbon was dominated by land sources transported by sea ice and ocean currents, while local primary productivity was suppressed by light limitation. Since ice retreated in 20th century, organic carbon from primary production gradually overtook the terrestrial component.
Ulrike Herzschuh, Thomas Böhmer, Chenzhi Li, Manuel Chevalier, Raphaël Hébert, Anne Dallmeyer, Xianyong Cao, Nancy H. Bigelow, Larisa Nazarova, Elena Y. Novenko, Jungjae Park, Odile Peyron, Natalia A. Rudaya, Frank Schlütz, Lyudmila S. Shumilovskikh, Pavel E. Tarasov, Yongbo Wang, Ruilin Wen, Qinghai Xu, and Zhuo Zheng
Earth Syst. Sci. Data, 15, 2235–2258, https://doi.org/10.5194/essd-15-2235-2023, https://doi.org/10.5194/essd-15-2235-2023, 2023
Short summary
Short summary
Climate reconstruction from proxy data can help evaluate climate models. We present pollen-based reconstructions of mean July temperature, mean annual temperature, and annual precipitation from 2594 pollen records from the Northern Hemisphere, using three reconstruction methods (WA-PLS, WA-PLS_tailored, and MAT). Since no global or hemispheric synthesis of quantitative precipitation changes are available for the Holocene so far, this dataset will be of great value to the geoscientific community.
Timothy Pollard, Jon Woodhead, John Hellstrom, John Engel, Roger Powell, and Russell Drysdale
Geochronology, 5, 181–196, https://doi.org/10.5194/gchron-5-181-2023, https://doi.org/10.5194/gchron-5-181-2023, 2023
Short summary
Short summary
When using the uranium–lead (U–Pb) radiometric dating method on very young materials (e.g. Quaternary age zircon and carbonate minerals), it is important to accurately account for the production and decay of intermediate
daughterisotopes in the uranium-series decay chain. DQPB is open-source software that allows users to easily perform such calculations for a variety of sample types and produce publication-ready graphical outputs of the resulting age information.
Thibauld M. Béjard, Andrés S. Rigual-Hernández, José A. Flores, Javier P. Tarruella, Xavier Durrieu de Madron, Isabel Cacho, Neghar Haghipour, Aidan Hunter, and Francisco J. Sierro
Biogeosciences, 20, 1505–1528, https://doi.org/10.5194/bg-20-1505-2023, https://doi.org/10.5194/bg-20-1505-2023, 2023
Short summary
Short summary
The Mediterranean Sea is undergoing a rapid and unprecedented environmental change. Planktic foraminifera calcification is affected on different timescales. On seasonal and interannual scales, calcification trends differ according to the species and are linked mainly to sea surface temperatures and carbonate system parameters, while comparison with pre/post-industrial assemblages shows that all three species have reduced their calcification between 10 % to 35 % according to the species.
Mary Robles, Odile Peyron, Guillemette Ménot, Elisabetta Brugiapaglia, Sabine Wulf, Oona Appelt, Marion Blache, Boris Vannière, Lucas Dugerdil, Bruno Paura, Salomé Ansanay-Alex, Amy Cromartie, Laurent Charlet, Stephane Guédron, Jacques-Louis de Beaulieu, and Sébastien Joannin
Clim. Past, 19, 493–515, https://doi.org/10.5194/cp-19-493-2023, https://doi.org/10.5194/cp-19-493-2023, 2023
Short summary
Short summary
Quantitative climate reconstructions based on pollen and brGDGTs reveal, for the Late Glacial, a warm Bølling–Allerød and a marked cold Younger Dryas in Italy, showing no latitudinal differences in terms of temperatures across Italy. In terms of precipitation, no latitudinal differences are recorded during the Bølling–Allerød, whereas 40–42° N appears as a key junction point between wetter conditions in southern Italy and drier conditions in northern Italy during the Younger Dryas.
Hege Kilhavn, Isabelle Couchoud, Russell N. Drysdale, Carlos Rossi, John Hellstrom, Fabien Arnaud, and Henri Wong
Clim. Past, 18, 2321–2344, https://doi.org/10.5194/cp-18-2321-2022, https://doi.org/10.5194/cp-18-2321-2022, 2022
Short summary
Short summary
The analysis of stable carbon and oxygen isotopic ratios, trace element ratios, and growth rate from a Spanish speleothem provides quantitative information on past hydrological conditions during the early Holocene in south-western Europe. Our data show that the cave site experienced increased effective recharge during the 8.2 ka event. Additionally, the oxygen isotopes indicate a change in the isotopic composition of the moisture source, associated with the meltwater flux to the North Atlantic.
Zuorui Liu, Amy Prendergast, Russell Drysdale, and Jan-Hendrik May
E&G Quaternary Sci. J., 71, 227–241, https://doi.org/10.5194/egqsj-71-227-2022, https://doi.org/10.5194/egqsj-71-227-2022, 2022
Short summary
Short summary
Past studies used two sampling strategies, the "bulk" and "sequential" drilling methods, for stable isotopic analysis of mammoth tooth enamel and paleoenvironmental reconstruction. This study applied both methods to the same enamel ridges of multiple mammoth teeth and compared their respective δ18O values. Offsets were detected between the bulk and average sequential δ18O values. The potential reasons for the offsets and their impacts on cross-method data comparison were discussed.
Fabrizio Marra, Alberto Frepoli, Dario Gioia, Marcello Schiattarella, Andrea Tertulliani, Monica Bini, Gaetano De Luca, and Marco Luppichini
Nat. Hazards Earth Syst. Sci., 22, 2445–2457, https://doi.org/10.5194/nhess-22-2445-2022, https://doi.org/10.5194/nhess-22-2445-2022, 2022
Short summary
Short summary
Through the analysis of the morphostructural setting in which the seismicity of Rome is framed, we explain why the city should not expect to suffer damage from a big earthquake.
Nick Thompson, Ulrich Salzmann, Adrián López-Quirós, Peter K. Bijl, Frida S. Hoem, Johan Etourneau, Marie-Alexandrine Sicre, Sabine Roignant, Emma Hocking, Michael Amoo, and Carlota Escutia
Clim. Past, 18, 209–232, https://doi.org/10.5194/cp-18-209-2022, https://doi.org/10.5194/cp-18-209-2022, 2022
Short summary
Short summary
New pollen and spore data from the Antarctic Peninsula region reveal temperate rainforests that changed and adapted in response to Eocene climatic cooling, roughly 35.5 Myr ago, and glacially related disturbance in the early Oligocene, approximately 33.5 Myr ago. The timing of these events indicates that the opening of ocean gateways alone did not trigger Antarctic glaciation, although ocean gateways may have played a role in climate cooling.
Aleix Cortina-Guerra, Juan José Gomez-Navarro, Belen Martrat, Juan Pedro Montávez, Alessandro Incarbona, Joan O. Grimalt, Marie-Alexandrine Sicre, and P. Graham Mortyn
Clim. Past, 17, 1523–1532, https://doi.org/10.5194/cp-17-1523-2021, https://doi.org/10.5194/cp-17-1523-2021, 2021
Short summary
Short summary
During late 20th century a singular Mediterranean circulation episode called the Eastern Mediterranean Transient (EMT) event occurred. It involved changes on the seawater physical and biogeochemical properties, which can impact areas broadly. Here, using paleosimulations for the last 1000 years we found that the East Atlantic/Western Russian atmospheric mode was the main driver of the EMT-type events in the past, and enhancement of this mode was coetaneous with low solar insolation.
Ana Moreno, Miguel Iglesias, Cesar Azorin-Molina, Carlos Pérez-Mejías, Miguel Bartolomé, Carlos Sancho, Heather Stoll, Isabel Cacho, Jaime Frigola, Cinta Osácar, Arsenio Muñoz, Antonio Delgado-Huertas, Ileana Bladé, and Françoise Vimeux
Atmos. Chem. Phys., 21, 10159–10177, https://doi.org/10.5194/acp-21-10159-2021, https://doi.org/10.5194/acp-21-10159-2021, 2021
Short summary
Short summary
We present a large and unique dataset of the rainfall isotopic composition at seven sites from northern Iberia to characterize their variability at daily and monthly timescales and to assess the role of climate and geographic factors in the modulation of δ18O values. We found that the origin, moisture uptake along the trajectory and type of precipitation play a key role. These results will help to improve the interpretation of δ18O paleorecords from lacustrine carbonates or speleothems.
Lucas Dugerdil, Sébastien Joannin, Odile Peyron, Isabelle Jouffroy-Bapicot, Boris Vannière, Bazartseren Boldgiv, Julia Unkelbach, Hermann Behling, and Guillemette Ménot
Clim. Past, 17, 1199–1226, https://doi.org/10.5194/cp-17-1199-2021, https://doi.org/10.5194/cp-17-1199-2021, 2021
Short summary
Short summary
Since the understanding of Holocene climate change appears to be a relevant issue for future climate change, the paleoclimate calibrations have to be improved. Here, surface samples from Mongolia and Siberia were analyzed to provide new calibrations for pollen and biomarker climate models. These calibrations appear to be more powerful than global calibrations, especially in an arid central Asian context. These calibrations will improve the understanding of monsoon Holocene oscillations.
Fabian Welc, Jerzy Nitychoruk, Leszek Marks, Krzysztof Bińka, Anna Rogóż-Matyszczak, Milena Obremska, and Abdelfattah Zalat
Clim. Past, 17, 1181–1198, https://doi.org/10.5194/cp-17-1181-2021, https://doi.org/10.5194/cp-17-1181-2021, 2021
Short summary
Short summary
Młynek Lake, located near the village of Janiki Wielkie (in the Warmia and Masuria region of north-east Poland) has been selected for multi-faceted palaeoenvironmental research based on a precise radiocarbon scale. Bottom sediments of this reservoir also contain unique information about anthropogenic activity and climate changes during last 2400 years.
Aurel Perşoiu, Nenad Buzjak, Alexandru Onaca, Christos Pennos, Yorgos Sotiriadis, Monica Ionita, Stavros Zachariadis, Michael Styllas, Jure Kosutnik, Alexandru Hegyi, and Valerija Butorac
The Cryosphere, 15, 2383–2399, https://doi.org/10.5194/tc-15-2383-2021, https://doi.org/10.5194/tc-15-2383-2021, 2021
Short summary
Short summary
Extreme precipitation events in summer 2019 led to catastrophic loss of cave and surface ice in SE Europe at levels unprecedented during the last century. The projected continuous warming and increase in precipitation extremes could pose an additional threat to glaciers in southern Europe, resulting in a potentially ice-free SE Europe by the middle of the next decade (2035 CE).
Matej Lipar, Andrea Martín-Pérez, Jure Tičar, Miha Pavšek, Matej Gabrovec, Mauro Hrvatin, Blaž Komac, Matija Zorn, Nadja Zupan Hajna, Jian-Xin Zhao, Russell N. Drysdale, and Mateja Ferk
The Cryosphere, 15, 17–30, https://doi.org/10.5194/tc-15-17-2021, https://doi.org/10.5194/tc-15-17-2021, 2021
Short summary
Short summary
The U–Th ages of subglacial carbonate deposits from a recently exposed surface previously occupied by the disappearing glacier in the SE European Alps suggest the glacier’s presence throughout the entire Holocene. These thin deposits, formed by regelation, would have been easily eroded if exposed during previous Holocene climatic optima. The age data indicate the glacier’s present unprecedented level of retreat and the potential of subglacial carbonates to act as palaeoclimate proxies.
Carmen-Andreea Bădăluţă, Aurel Perșoiu, Monica Ionita, and Natalia Piotrowska
Clim. Past, 16, 2445–2458, https://doi.org/10.5194/cp-16-2445-2020, https://doi.org/10.5194/cp-16-2445-2020, 2020
Short summary
Short summary
We present a reconstruction of summer temperature for the last millennium in east-central Europe that shows little summer temperature differences between the Medieval Warm Period and the Little Ice Age on centennial scales as well as the fact that well-expressed minima and maxima occurred synchronously with periods of low and high solar activity, respectively. Furthermore, summer temperatures fluctuated with a periodicity similar to that of the Atlantic Multidecadal Oscillation.
Basil A. S. Davis, Manuel Chevalier, Philipp Sommer, Vachel A. Carter, Walter Finsinger, Achille Mauri, Leanne N. Phelps, Marco Zanon, Roman Abegglen, Christine M. Åkesson, Francisca Alba-Sánchez, R. Scott Anderson, Tatiana G. Antipina, Juliana R. Atanassova, Ruth Beer, Nina I. Belyanina, Tatiana A. Blyakharchuk, Olga K. Borisova, Elissaveta Bozilova, Galina Bukreeva, M. Jane Bunting, Eleonora Clò, Daniele Colombaroli, Nathalie Combourieu-Nebout, Stéphanie Desprat, Federico Di Rita, Morteza Djamali, Kevin J. Edwards, Patricia L. Fall, Angelica Feurdean, William Fletcher, Assunta Florenzano, Giulia Furlanetto, Emna Gaceur, Arsenii T. Galimov, Mariusz Gałka, Iria García-Moreiras, Thomas Giesecke, Roxana Grindean, Maria A. Guido, Irina G. Gvozdeva, Ulrike Herzschuh, Kari L. Hjelle, Sergey Ivanov, Susanne Jahns, Vlasta Jankovska, Gonzalo Jiménez-Moreno, Monika Karpińska-Kołaczek, Ikuko Kitaba, Piotr Kołaczek, Elena G. Lapteva, Małgorzata Latałowa, Vincent Lebreton, Suzanne Leroy, Michelle Leydet, Darya A. Lopatina, José Antonio López-Sáez, André F. Lotter, Donatella Magri, Elena Marinova, Isabelle Matthias, Anastasia Mavridou, Anna Maria Mercuri, Jose Manuel Mesa-Fernández, Yuri A. Mikishin, Krystyna Milecka, Carlo Montanari, César Morales-Molino, Almut Mrotzek, Castor Muñoz Sobrino, Olga D. Naidina, Takeshi Nakagawa, Anne Birgitte Nielsen, Elena Y. Novenko, Sampson Panajiotidis, Nata K. Panova, Maria Papadopoulou, Heather S. Pardoe, Anna Pędziszewska, Tatiana I. Petrenko, María J. Ramos-Román, Cesare Ravazzi, Manfred Rösch, Natalia Ryabogina, Silvia Sabariego Ruiz, J. Sakari Salonen, Tatyana V. Sapelko, James E. Schofield, Heikki Seppä, Lyudmila Shumilovskikh, Normunds Stivrins, Philipp Stojakowits, Helena Svobodova Svitavska, Joanna Święta-Musznicka, Ioan Tantau, Willy Tinner, Kazimierz Tobolski, Spassimir Tonkov, Margarita Tsakiridou, Verushka Valsecchi, Oksana G. Zanina, and Marcelina Zimny
Earth Syst. Sci. Data, 12, 2423–2445, https://doi.org/10.5194/essd-12-2423-2020, https://doi.org/10.5194/essd-12-2423-2020, 2020
Short summary
Short summary
The Eurasian Modern Pollen Database (EMPD) contains pollen counts and associated metadata for 8134 modern pollen samples from across the Eurasian region. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives. The purpose of the EMPD is to provide calibration datasets and other data to support palaeoecological research on past climates and vegetation cover over the Quaternary period.
Ferréol Salomon, Darío Bernal-Casasola, José J. Díaz, Macarena Lara, Salvador Domínguez-Bella, Damien Ertlen, Patrick Wassmer, Pierre Adam, Philippe Schaeffer, Laurent Hardion, Cécile Vittori, Stoil Chapkanski, Hugo Delile, Laurent Schmitt, Frank Preusser, Martine Trautmann, Alessia Masi, Cristiano Vignola, Laura Sadori, Jacob Morales, Paloma Vidal Matutano, Vincent Robin, Benjamin Keller, Ángel Sanchez Bellón, Javier Martínez López, and Gilles Rixhon
Sci. Dril., 27, 35–47, https://doi.org/10.5194/sd-27-35-2020, https://doi.org/10.5194/sd-27-35-2020, 2020
Short summary
Short summary
PalaeoCADIX-Z is an interdisciplinary project that studied three cores drilled in a marine palaeochannel that ran through the ancient city of Cádiz (Spain). These cores reveal a ≥ 50 m thick Holocene sedimentary sequence. Importantly, most of the deposits date from the 1st millennium BCE to the 1st millennium CE. Geoarchaeologists, geomorphologists, archaeologists, sedimentologists, palaeoenvironmentalists, geochemists, and geochronologists collaborated within this project.
Lucas Dugerdil, Sébastien Joannin, Odile Peyron, Isabelle Jouffroy-Bapicot, Boris Vannière, Bazartseren Boldgiv, and Guillemette Ménot
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-475, https://doi.org/10.5194/bg-2019-475, 2020
Preprint withdrawn
Hans von Suchodoletz, Stefanie Berg, Eileen Eckmeier, Lukas Werther, and Christoph Zielhofer
E&G Quaternary Sci. J., 68, 237–240, https://doi.org/10.5194/egqsj-68-237-2020, https://doi.org/10.5194/egqsj-68-237-2020, 2020
Short summary
Short summary
In this editorial, we give a short state of the art of geoarchaeology, including recent advancements and challenges, and shortly present the seven contributions to our special issue.
Laurie Menviel, Emilie Capron, Aline Govin, Andrea Dutton, Lev Tarasov, Ayako Abe-Ouchi, Russell N. Drysdale, Philip L. Gibbard, Lauren Gregoire, Feng He, Ruza F. Ivanovic, Masa Kageyama, Kenji Kawamura, Amaelle Landais, Bette L. Otto-Bliesner, Ikumi Oyabu, Polychronis C. Tzedakis, Eric Wolff, and Xu Zhang
Geosci. Model Dev., 12, 3649–3685, https://doi.org/10.5194/gmd-12-3649-2019, https://doi.org/10.5194/gmd-12-3649-2019, 2019
Short summary
Short summary
As part of the Past Global Changes (PAGES) working group on Quaternary Interglacials, we propose a protocol to perform transient simulations of the penultimate deglaciation for the Paleoclimate Modelling Intercomparison Project (PMIP4). This design includes time-varying changes in orbital forcing, greenhouse gas concentrations, continental ice sheets as well as freshwater input from the disintegration of continental ice sheets. Key paleo-records for model-data comparison are also included.
Albert Català, Isabel Cacho, Jaime Frigola, Leopoldo D. Pena, and Fabrizio Lirer
Clim. Past, 15, 927–942, https://doi.org/10.5194/cp-15-927-2019, https://doi.org/10.5194/cp-15-927-2019, 2019
Short summary
Short summary
We present a new high-resolution sea surface temperature (SST) reconstruction for the Holocene (last 11 700 years) in the westernmost Mediterranean Sea. We identify three sub-periods: the Early Holocene with warmest SST; the Middle Holocene with a cooling trend ending at 4200 years, which is identified as a double peak cooling event that marks the transition between the Middle and Late Holocene; and the Late Holocene with very different behaviour in both long- and short-term SST variability.
Aurel Perşoiu, Monica Ionita, and Harvey Weiss
Clim. Past, 15, 781–793, https://doi.org/10.5194/cp-15-781-2019, https://doi.org/10.5194/cp-15-781-2019, 2019
Short summary
Short summary
We present a reconstruction of winter climate around 4.2 ka cal BP in Europe, west Asia, and northern Africa that shows generally low temperatures and heterogeneously distributed precipitation. We hypothesize that in the extratropical Northern Hemisphere the 4.2 ka BP event was caused by the strengthening and expansion of the Siberian High, which effectively blocked the moisture-carrying westerlies from reaching west Asia and also resulted in outbreaks of northerly cold and dry winds.
Bassem Jalali, Marie-Alexandrine Sicre, Julien Azuara, Violaine Pellichero, and Nathalie Combourieu-Nebout
Clim. Past, 15, 701–711, https://doi.org/10.5194/cp-15-701-2019, https://doi.org/10.5194/cp-15-701-2019, 2019
Christoph Zielhofer, Anne Köhler, Steffen Mischke, Abdelfattah Benkaddour, Abdeslam Mikdad, and William J. Fletcher
Clim. Past, 15, 463–475, https://doi.org/10.5194/cp-15-463-2019, https://doi.org/10.5194/cp-15-463-2019, 2019
Short summary
Short summary
Based on a Holocene oxygen stable isotope record from Lake Sidi Ali (Morocco) we correlate Western Mediterranean precipitation anomalies with North Atlantic ice-rafted debris (Bond) events to identify a probable teleconnection between Western Mediterranean winter rains and subpolar North Atlantic cooling phases. Our data show a noticeable similarity between Western Mediterranean winter rain minima and Bond events during the Early Holocene and an opposite pattern during the Late Holocene.
Rosine Cartier, Florence Sylvestre, Christine Paillès, Corinne Sonzogni, Martine Couapel, Anne Alexandre, Jean-Charles Mazur, Elodie Brisset, Cécile Miramont, and Frédéric Guiter
Clim. Past, 15, 253–263, https://doi.org/10.5194/cp-15-253-2019, https://doi.org/10.5194/cp-15-253-2019, 2019
Short summary
Short summary
A major environmental change, 4200 years ago, was recorded in the lacustrine sediments of Lake Petit (Mediterranean Alps). The regime shift was described by a modification in erosion processes in the watershed and aquatic species in the lake. This study, based on the analysis of the lake water balance by using oxygen isotopes in diatoms, revealed that these environmental responses were due to a rapid change in precipitation regime, lasting ca. 500 years.
Federico Di Rita and Donatella Magri
Clim. Past, 15, 237–251, https://doi.org/10.5194/cp-15-237-2019, https://doi.org/10.5194/cp-15-237-2019, 2019
Ilaria Isola, Giovanni Zanchetta, Russell N. Drysdale, Eleonora Regattieri, Monica Bini, Petra Bajo, John C. Hellstrom, Ilaria Baneschi, Piero Lionello, Jon Woodhead, and Alan Greig
Clim. Past, 15, 135–151, https://doi.org/10.5194/cp-15-135-2019, https://doi.org/10.5194/cp-15-135-2019, 2019
Short summary
Short summary
To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
Gaia Sinopoli, Odile Peyron, Alessia Masi, Jens Holtvoeth, Alexander Francke, Bernd Wagner, and Laura Sadori
Clim. Past, 15, 53–71, https://doi.org/10.5194/cp-15-53-2019, https://doi.org/10.5194/cp-15-53-2019, 2019
Short summary
Short summary
Climate changes occur today as they occurred in the past. This study deals with climate changes reconstructed at Lake Ohrid (Albania and FYROM) between 160 000 and 70 000 years ago. Climate reconstruction, based on a high-resolution pollen study, provides quantitative estimates of past temperature and precipitation. Our data show an alternation of cold/dry and warm/wet periods. The last interglacial appears to be characterized by temperatures higher than nowadays.
Laurie Menviel, Emilie Capron, Aline Govin, Andrea Dutton, Lev Tarasov, Ayako Abe-Ouchi, Russell Drysdale, Philip Gibbard, Lauren Gregoire, Feng He, Ruza Ivanovic, Masa Kageyama, Kenji Kawamura, Amaelle Landais, Bette L. Otto-Bliesner, Ikumi Oyabu, Polychronis Tzedakis, Eric Wolff, and Xu Zhang
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-106, https://doi.org/10.5194/cp-2018-106, 2018
Preprint withdrawn
Short summary
Short summary
The penultimate deglaciation (~ 138–128 ka), which represents the transition into the Last Interglacial period, provides a framework to investigate the climate and environmental response to large changes in boundary conditions. Here, as part of the PAGES-PMIP working group on Quaternary Interglacials, we propose a protocol to perform transient simulations of the penultimate deglaciation as well as a selection of paleo records for upcoming model-data comparisons.
Alessia Masi, Alexander Francke, Caterina Pepe, Matthias Thienemann, Bernd Wagner, and Laura Sadori
Clim. Past, 14, 351–367, https://doi.org/10.5194/cp-14-351-2018, https://doi.org/10.5194/cp-14-351-2018, 2018
Short summary
Short summary
The first high-resolution Lake Dojran pollen record for the last 12 500 years is presented. The ecological succession shows Late Glacial steppe vegetation gradually replaced, since 11 500 yr BP, by Holocene mesophilous forests. The first human traces are recorded around 5000 yr BP and increased considerably since the Bronze Age. Pollen data and sedimentological, biomarker and diatom data available from the same core contribute to an understanding of the environmental history of the Balkans.
Carmen-Andreea Bădăluță, Aurel Perșoiu, Monica Ionita, Viorica Nagavciuc, and Petruț-Ionel Bistricean
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-6, https://doi.org/10.5194/hess-2018-6, 2018
Manuscript not accepted for further review
Ulrich Kotthoff, Jeroen Groeneveld, Jeanine L. Ash, Anne-Sophie Fanget, Nadine Quintana Krupinski, Odile Peyron, Anna Stepanova, Jonathan Warnock, Niels A. G. M. Van Helmond, Benjamin H. Passey, Ole Rønø Clausen, Ole Bennike, Elinor Andrén, Wojciech Granoszewski, Thomas Andrén, Helena L. Filipsson, Marit-Solveig Seidenkrantz, Caroline P. Slomp, and Thorsten Bauersachs
Biogeosciences, 14, 5607–5632, https://doi.org/10.5194/bg-14-5607-2017, https://doi.org/10.5194/bg-14-5607-2017, 2017
Short summary
Short summary
We present reconstructions of paleotemperature, paleosalinity, and paleoecology from the Little Belt (Site M0059) over the past ~ 8000 years and evaluate the applicability of numerous proxies. Conditions were lacustrine until ~ 7400 cal yr BP. A transition to brackish–marine conditions then occurred within ~ 200 years. Salinity proxies rarely allowed quantitative estimates but revealed congruent results, while quantitative temperature reconstructions differed depending on the proxies used.
Virgil Drăguşin, Sorin Balan, Dominique Blamart, Ferenc Lázár Forray, Constantin Marin, Ionuţ Mirea, Viorica Nagavciuc, Iancu Orăşeanu, Aurel Perşoiu, Laura Tîrlă, Alin Tudorache, and Marius Vlaicu
Hydrol. Earth Syst. Sci., 21, 5357–5373, https://doi.org/10.5194/hess-21-5357-2017, https://doi.org/10.5194/hess-21-5357-2017, 2017
Bronwyn C. Dixon, Jonathan J. Tyler, Andrew M. Lorrey, Ian D. Goodwin, Joëlle Gergis, and Russell N. Drysdale
Clim. Past, 13, 1403–1433, https://doi.org/10.5194/cp-13-1403-2017, https://doi.org/10.5194/cp-13-1403-2017, 2017
Short summary
Short summary
Existing sedimentary palaeoclimate records in Australasia were assessed for suitability for examining the last 2 millennia. A small number of high-quality records were identified, and new Bayesian age models were constructed for each record. Findings suggest that Australasian record chronologies and confidence in proxy–climate relationships are the main factors limiting appropriate data for examining Common Era climate variability. Recommendations for improving data accessibility are provided.
María Fernanda Sánchez Goñi, Stéphanie Desprat, Anne-Laure Daniau, Frank C. Bassinot, Josué M. Polanco-Martínez, Sandy P. Harrison, Judy R. M. Allen, R. Scott Anderson, Hermann Behling, Raymonde Bonnefille, Francesc Burjachs, José S. Carrión, Rachid Cheddadi, James S. Clark, Nathalie Combourieu-Nebout, Colin. J. Courtney Mustaphi, Georg H. Debusk, Lydie M. Dupont, Jemma M. Finch, William J. Fletcher, Marco Giardini, Catalina González, William D. Gosling, Laurie D. Grigg, Eric C. Grimm, Ryoma Hayashi, Karin Helmens, Linda E. Heusser, Trevor Hill, Geoffrey Hope, Brian Huntley, Yaeko Igarashi, Tomohisa Irino, Bonnie Jacobs, Gonzalo Jiménez-Moreno, Sayuri Kawai, A. Peter Kershaw, Fujio Kumon, Ian T. Lawson, Marie-Pierre Ledru, Anne-Marie Lézine, Ping Mei Liew, Donatella Magri, Robert Marchant, Vasiliki Margari, Francis E. Mayle, G. Merna McKenzie, Patrick Moss, Stefanie Müller, Ulrich C. Müller, Filipa Naughton, Rewi M. Newnham, Tadamichi Oba, Ramón Pérez-Obiol, Roberta Pini, Cesare Ravazzi, Katy H. Roucoux, Stephen M. Rucina, Louis Scott, Hikaru Takahara, Polichronis C. Tzedakis, Dunia H. Urrego, Bas van Geel, B. Guido Valencia, Marcus J. Vandergoes, Annie Vincens, Cathy L. Whitlock, Debra A. Willard, and Masanobu Yamamoto
Earth Syst. Sci. Data, 9, 679–695, https://doi.org/10.5194/essd-9-679-2017, https://doi.org/10.5194/essd-9-679-2017, 2017
Short summary
Short summary
The ACER (Abrupt Climate Changes and Environmental Responses) global database includes 93 pollen records from the last glacial period (73–15 ka) plotted against a common chronology; 32 also provide charcoal records. The database allows for the reconstruction of the regional expression, vegetation and fire of past abrupt climate changes that are comparable to those expected in the 21st century. This work is a major contribution to understanding the processes behind rapid climate change.
Pauline C. Treble, Andy Baker, Linda K. Ayliffe, Timothy J. Cohen, John C. Hellstrom, Michael K. Gagan, Silvia Frisia, Russell N. Drysdale, Alan D. Griffiths, and Andrea Borsato
Clim. Past, 13, 667–687, https://doi.org/10.5194/cp-13-667-2017, https://doi.org/10.5194/cp-13-667-2017, 2017
Short summary
Short summary
Little is known about the climate of southern Australia during the Last Glacial Maximum and deglaciation owing to sparse records for this region. We present the first high-resolution data, derived from speleothems that grew 23–5 ka. It appears that recharge to the Flinders Ranges was higher than today, particularly during 18.9–15.8 ka, argued to be due to the enhanced availability of tropical moisture. An abrupt shift to aridity is recorded at 15.8 ka, associated with restored westerly airflow.
Bernd Wagner, Thomas Wilke, Alexander Francke, Christian Albrecht, Henrike Baumgarten, Adele Bertini, Nathalie Combourieu-Nebout, Aleksandra Cvetkoska, Michele D'Addabbo, Timme H. Donders, Kirstin Föller, Biagio Giaccio, Andon Grazhdani, Torsten Hauffe, Jens Holtvoeth, Sebastien Joannin, Elena Jovanovska, Janna Just, Katerina Kouli, Andreas Koutsodendris, Sebastian Krastel, Jack H. Lacey, Niklas Leicher, Melanie J. Leng, Zlatko Levkov, Katja Lindhorst, Alessia Masi, Anna M. Mercuri, Sebastien Nomade, Norbert Nowaczyk, Konstantinos Panagiotopoulos, Odile Peyron, Jane M. Reed, Eleonora Regattieri, Laura Sadori, Leonardo Sagnotti, Björn Stelbrink, Roberto Sulpizio, Slavica Tofilovska, Paola Torri, Hendrik Vogel, Thomas Wagner, Friederike Wagner-Cremer, George A. Wolff, Thomas Wonik, Giovanni Zanchetta, and Xiaosen S. Zhang
Biogeosciences, 14, 2033–2054, https://doi.org/10.5194/bg-14-2033-2017, https://doi.org/10.5194/bg-14-2033-2017, 2017
Short summary
Short summary
Lake Ohrid is considered to be the oldest existing lake in Europe. Moreover, it has a very high degree of endemic biodiversity. During a drilling campaign at Lake Ohrid in 2013, a 569 m long sediment sequence was recovered from Lake Ohrid. The ongoing studies of this record provide first important information on the environmental and evolutionary history of the lake and the reasons for its high endimic biodiversity.
Odile Peyron, Nathalie Combourieu-Nebout, David Brayshaw, Simon Goring, Valérie Andrieu-Ponel, Stéphanie Desprat, Will Fletcher, Belinda Gambin, Chryssanthi Ioakim, Sébastien Joannin, Ulrich Kotthoff, Katerina Kouli, Vincent Montade, Jörg Pross, Laura Sadori, and Michel Magny
Clim. Past, 13, 249–265, https://doi.org/10.5194/cp-13-249-2017, https://doi.org/10.5194/cp-13-249-2017, 2017
Short summary
Short summary
This study aims to reconstruct the climate evolution of the Mediterranean region during the Holocene from pollen data and model outputs. The model- and pollen-inferred precipitation estimates show overall agreement: the eastern Medit. experienced wetter-than-present summer conditions during the early–late Holocene. This regional climate model highlights how the patchy nature of climate signals and data in the Medit. may lead to stronger local signals than the large-scale pattern suggests.
Maria-Angela Bassetti, Serge Berné, Marie-Alexandrine Sicre, Bernard Dennielou, Yoann Alonso, Roselyne Buscail, Bassem Jalali, Bertil Hebert, and Christophe Menniti
Clim. Past, 12, 1539–1553, https://doi.org/10.5194/cp-12-1539-2016, https://doi.org/10.5194/cp-12-1539-2016, 2016
Short summary
Short summary
This work represents the first attempt to decipher the linkages between rapid climate changes and continental Holocene paleohydrology in the NW Mediterranean shallow marine setting. Between 11 and 4 ka cal BP, terrigenous input increased and reached a maximum at 7 ka cal BP, probably as a result of a humid phase. From ca. 4 ka cal BP to the present, enhanced variability in the land-derived material is possibly due to large-scale atmospheric circulation and rainfall patterns in western Europe.
Giovanni Zanchetta, Eleonora Regattieri, Biagio Giaccio, Bernd Wagner, Roberto Sulpizio, Alex Francke, Hendrik Vogel, Laura Sadori, Alessia Masi, Gaia Sinopoli, Jack H. Lacey, Melanie J. Leng, and Niklas Leicher
Biogeosciences, 13, 2757–2768, https://doi.org/10.5194/bg-13-2757-2016, https://doi.org/10.5194/bg-13-2757-2016, 2016
Short summary
Short summary
Chronology is fundamental in paleoclimatology for understanding timing of events and their origin. In this paper we try to obtain a more detailed chronology for the interval comprised between ca. 140 and 70 ka for the DEEP core in Lake Ohrid using regional independently-dated archives (i.e. speleothems and/or lacustrine succession with well-dated volcanic layers). This allows to insert the DEEP chronology within a common chronological frame between different continental and marine proxy records.
Niklas Leicher, Giovanni Zanchetta, Roberto Sulpizio, Biagio Giaccio, Bernd Wagner, Sebastien Nomade, Alexander Francke, and Paola Del Carlo
Biogeosciences, 13, 2151–2178, https://doi.org/10.5194/bg-13-2151-2016, https://doi.org/10.5194/bg-13-2151-2016, 2016
Mercè Cisneros, Isabel Cacho, Jaime Frigola, Miquel Canals, Pere Masqué, Belen Martrat, Marta Casado, Joan O. Grimalt, Leopoldo D. Pena, Giulia Margaritelli, and Fabrizio Lirer
Clim. Past, 12, 849–869, https://doi.org/10.5194/cp-12-849-2016, https://doi.org/10.5194/cp-12-849-2016, 2016
Short summary
Short summary
We present a high-resolution multi-proxy study about the evolution of sea surface conditions along the last 2700 yr in the north-western Mediterranean Sea based on five sediment records from two different sites north of Minorca. The novelty of the results and the followed approach, constructing stack records from the studied proxies to preserve the most robust patterns, provides a special value to the study. This complex period appears to have significant regional changes in the climatic signal.
Jack H. Lacey, Melanie J. Leng, Alexander Francke, Hilary J. Sloane, Antoni Milodowski, Hendrik Vogel, Henrike Baumgarten, Giovanni Zanchetta, and Bernd Wagner
Biogeosciences, 13, 1801–1820, https://doi.org/10.5194/bg-13-1801-2016, https://doi.org/10.5194/bg-13-1801-2016, 2016
Short summary
Short summary
We use stable isotope data from carbonates to provide a palaeoenvironmental reconstruction covering the last 637 kyr at Lake Ohrid (FYROM/Albania). Our results indicate a relatively stable climate until 450 ka, wetter climate conditions at 400–250 ka, and a transition to a drier climate after 250 ka. This work emphasises the importance of Lake Ohrid as a valuable archive of climate change in the northern Mediterranean region.
Laura Sadori, Andreas Koutsodendris, Konstantinos Panagiotopoulos, Alessia Masi, Adele Bertini, Nathalie Combourieu-Nebout, Alexander Francke, Katerina Kouli, Sébastien Joannin, Anna Maria Mercuri, Odile Peyron, Paola Torri, Bernd Wagner, Giovanni Zanchetta, Gaia Sinopoli, and Timme H. Donders
Biogeosciences, 13, 1423–1437, https://doi.org/10.5194/bg-13-1423-2016, https://doi.org/10.5194/bg-13-1423-2016, 2016
Short summary
Short summary
Lake Ohrid (FYROM/Albania) is the deepest, largest and oldest lake in Europe. To understand the climatic and environmental evolution of its area, a palynological study was undertaken for the last 500 ka. We found a correspondence between forested/non-forested periods and glacial-interglacial cycles of marine isotope stratigraphy. Our record shows a progressive change from cooler and wetter to warmer and dryer interglacial conditions. This shift is also visible in glacial vegetation.
Alexander Francke, Bernd Wagner, Janna Just, Niklas Leicher, Raphael Gromig, Henrike Baumgarten, Hendrik Vogel, Jack H. Lacey, Laura Sadori, Thomas Wonik, Melanie J. Leng, Giovanni Zanchetta, Roberto Sulpizio, and Biagio Giaccio
Biogeosciences, 13, 1179–1196, https://doi.org/10.5194/bg-13-1179-2016, https://doi.org/10.5194/bg-13-1179-2016, 2016
Short summary
Short summary
Lake Ohrid (Macedonia, Albania) is thought to be more than 1.2 million years old. To recover a long paleoclimate record for the Mediterranean region, a deep drilling was carried out in 2013 within the scope of the Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project. Here, we present lithological, sedimentological, and (bio-)geochemical data from the upper 247.8 m composite depth of the overall 569 m long DEEP site record.
B. Gambin, V. Andrieu-Ponel, F. Médail, N. Marriner, O. Peyron, V. Montade, T. Gambin, C. Morhange, D. Belkacem, and M. Djamali
Clim. Past, 12, 273–297, https://doi.org/10.5194/cp-12-273-2016, https://doi.org/10.5194/cp-12-273-2016, 2016
Short summary
Short summary
Based on the study of ancient microfossils, such as pollen and spores, this paper explores climate change in a Mediterranean island context. Using a multi-disciplinary approach this original research corroborates existing archaeological and historical data. It also uses comparative data from elsewhere in the central Mediterranean to ensure that the current research is placed within the appropriate geographic context.
B. Jalali, M.-A. Sicre, M.-A. Bassetti, and N. Kallel
Clim. Past, 12, 91–101, https://doi.org/10.5194/cp-12-91-2016, https://doi.org/10.5194/cp-12-91-2016, 2016
B. A. A. Hoogakker, R. S. Smith, J. S. Singarayer, R. Marchant, I. C. Prentice, J. R. M. Allen, R. S. Anderson, S. A. Bhagwat, H. Behling, O. Borisova, M. Bush, A. Correa-Metrio, A. de Vernal, J. M. Finch, B. Fréchette, S. Lozano-Garcia, W. D. Gosling, W. Granoszewski, E. C. Grimm, E. Grüger, J. Hanselman, S. P. Harrison, T. R. Hill, B. Huntley, G. Jiménez-Moreno, P. Kershaw, M.-P. Ledru, D. Magri, M. McKenzie, U. Müller, T. Nakagawa, E. Novenko, D. Penny, L. Sadori, L. Scott, J. Stevenson, P. J. Valdes, M. Vandergoes, A. Velichko, C. Whitlock, and C. Tzedakis
Clim. Past, 12, 51–73, https://doi.org/10.5194/cp-12-51-2016, https://doi.org/10.5194/cp-12-51-2016, 2016
Short summary
Short summary
In this paper we use two climate models to test how Earth’s vegetation responded to changes in climate over the last 120 000 years, looking at warm interglacial climates like today, cold ice-age glacial climates, and intermediate climates. The models agree well with observations from pollen, showing smaller forested areas and larger desert areas during cold periods. Forests store most terrestrial carbon; the terrestrial carbon lost during cold climates was most likely relocated to the oceans.
H. Baumgarten, T. Wonik, D. C. Tanner, A. Francke, B. Wagner, G. Zanchetta, R. Sulpizio, B. Giaccio, and S. Nomade
Biogeosciences, 12, 7453–7465, https://doi.org/10.5194/bg-12-7453-2015, https://doi.org/10.5194/bg-12-7453-2015, 2015
Short summary
Short summary
Gamma ray (GR) fluctuations and K values from downhole logging data obtained in the sediments of Lake Ohrid correlate with the global climate reference record (LR04 stack from δ18O) (Lisiecki and Raymo, 2005). GR and K values are considered a reliable proxy to depict glacial-interglacial cycles and document warm, humid and cold, drier periods. A robust age model for the downhole logging data over the past 630kyr was established and will play a crucial role for other working groups.
B. Giaccio, E. Regattieri, G. Zanchetta, B. Wagner, P. Galli, G. Mannella, E. Niespolo, E. Peronace, P. R. Renne, S. Nomade, G. P. Cavinato, P. Messina, A. Sposato, C. Boschi, F. Florindo, F. Marra, and L. Sadori
Sci. Dril., 20, 13–19, https://doi.org/10.5194/sd-20-13-2015, https://doi.org/10.5194/sd-20-13-2015, 2015
Short summary
Short summary
As a pilot study for a possible depth-drilling project, an 82m long sedimentary succession was retrieved from the Fucino Basin, central Apennines, which hosts ca. 900m of lacustrine sediments. The acquired paleoclimatic record, from the retrieved core, spans the last 180ka and reveals noticeable variations related to the last two glacial-interglacial cycles. In light of these results, the Fucino sediments are likely to provide one of the longest continuous record for the last 2Ma.
M. D'Addabbo, R. Sulpizio, M. Guidi, G. Capitani, P. Mantecca, and G. Zanchetta
Biogeosciences, 12, 7087–7106, https://doi.org/10.5194/bg-12-7087-2015, https://doi.org/10.5194/bg-12-7087-2015, 2015
Short summary
Short summary
Leaching experiments were carried out on fresh ash samples from the 2012 Popocatépetl, and 2011/12 Etna eruptions, in order to investigate the release of compounds in water. Results were discussed in the light of changing pH and release of compounds for the different leachates. They were used for toxicity experiments on living biota (Xenopus laevis). They are mildly toxic, and no significant differences exist between the toxic profiles of the two leachates.
I. Hernández-Almeida, F.-J. Sierro, I. Cacho, and J.-A. Flores
Clim. Past, 11, 687–696, https://doi.org/10.5194/cp-11-687-2015, https://doi.org/10.5194/cp-11-687-2015, 2015
Short summary
Short summary
This manuscript presents new Mg/Ca and previously published δ18O measurements of Neogloboquadrina pachyderma sinistral for MIS 31-19, from a sediment core from the subpolar North Atlantic. The mechanism proposed here involves northward subsurface transport of warm and salty subtropical waters during periods of weaker AMOC, leading to ice-sheet instability and IRD discharge. This is the first time that these rapid climate oscillations are described for the early Pleistocene.
O. Margalef, I. Cacho, S. Pla-Rabes, N. Cañellas-Boltà, J. J. Pueyo, A. Sáez, L. D. Pena, B. L. Valero-Garcés, V. Rull, and S. Giralt
Clim. Past Discuss., https://doi.org/10.5194/cpd-11-1407-2015, https://doi.org/10.5194/cpd-11-1407-2015, 2015
Manuscript not accepted for further review
Short summary
Short summary
The Rano Aroi peat record (Easter Island, 27ºS) is characterized by six major events of enhanced precipitation between 38 and 65 kyr BP coinciding with Heinrich and Dansgaard-Oeschger (DO) Stadials. These events draw a coherent regional picture involving atmospheric and oceanic reorganization. The singular location of Easter Island, filling a gap in an area where marine records are not available, contributes to understand the mechanisms behind these global rapid climatic excursions.
B. Wagner, T. Wilke, S. Krastel, G. Zanchetta, R. Sulpizio, K. Reicherter, M. J. Leng, A. Grazhdani, S. Trajanovski, A. Francke, K. Lindhorst, Z. Levkov, A. Cvetkoska, J. M. Reed, X. Zhang, J. H. Lacey, T. Wonik, H. Baumgarten, and H. Vogel
Sci. Dril., 17, 19–29, https://doi.org/10.5194/sd-17-19-2014, https://doi.org/10.5194/sd-17-19-2014, 2014
B. Wagner, M. J. Leng, T. Wilke, A. Böhm, K. Panagiotopoulos, H. Vogel, J. H. Lacey, G. Zanchetta, and R. Sulpizio
Clim. Past, 10, 261–267, https://doi.org/10.5194/cp-10-261-2014, https://doi.org/10.5194/cp-10-261-2014, 2014
M. Magny, N. Combourieu-Nebout, J. L. de Beaulieu, V. Bout-Roumazeilles, D. Colombaroli, S. Desprat, A. Francke, S. Joannin, E. Ortu, O. Peyron, M. Revel, L. Sadori, G. Siani, M. A. Sicre, S. Samartin, A. Simonneau, W. Tinner, B. Vannière, B. Wagner, G. Zanchetta, F. Anselmetti, E. Brugiapaglia, E. Chapron, M. Debret, M. Desmet, J. Didier, L. Essallami, D. Galop, A. Gilli, J. N. Haas, N. Kallel, L. Millet, A. Stock, J. L. Turon, and S. Wirth
Clim. Past, 9, 2043–2071, https://doi.org/10.5194/cp-9-2043-2013, https://doi.org/10.5194/cp-9-2043-2013, 2013
N. Combourieu-Nebout, O. Peyron, V. Bout-Roumazeilles, S. Goring, I. Dormoy, S. Joannin, L. Sadori, G. Siani, and M. Magny
Clim. Past, 9, 2023–2042, https://doi.org/10.5194/cp-9-2023-2013, https://doi.org/10.5194/cp-9-2023-2013, 2013
L. Sadori, E. Ortu, O. Peyron, G. Zanchetta, B. Vannière, M. Desmet, and M. Magny
Clim. Past, 9, 1969–1984, https://doi.org/10.5194/cp-9-1969-2013, https://doi.org/10.5194/cp-9-1969-2013, 2013
M.-A. Sicre, G. Siani, D. Genty, N. Kallel, and L. Essallami
Clim. Past, 9, 1375–1383, https://doi.org/10.5194/cp-9-1375-2013, https://doi.org/10.5194/cp-9-1375-2013, 2013
O. Peyron, M. Magny, S. Goring, S. Joannin, J.-L. de Beaulieu, E. Brugiapaglia, L. Sadori, G. Garfi, K. Kouli, C. Ioakim, and N. Combourieu-Nebout
Clim. Past, 9, 1233–1252, https://doi.org/10.5194/cp-9-1233-2013, https://doi.org/10.5194/cp-9-1233-2013, 2013
S. Desprat, N. Combourieu-Nebout, L. Essallami, M. A. Sicre, I. Dormoy, O. Peyron, G. Siani, V. Bout Roumazeilles, and J. L. Turon
Clim. Past, 9, 767–787, https://doi.org/10.5194/cp-9-767-2013, https://doi.org/10.5194/cp-9-767-2013, 2013
M. Damaschke, R. Sulpizio, G. Zanchetta, B. Wagner, A. Böhm, N. Nowaczyk, J. Rethemeyer, and A. Hilgers
Clim. Past, 9, 267–287, https://doi.org/10.5194/cp-9-267-2013, https://doi.org/10.5194/cp-9-267-2013, 2013
B. Wagner, A. Francke, R. Sulpizio, G. Zanchetta, K. Lindhorst, S. Krastel, H. Vogel, J. Rethemeyer, G. Daut, A. Grazhdani, B. Lushaj, and S. Trajanovski
Clim. Past, 8, 2069–2078, https://doi.org/10.5194/cp-8-2069-2012, https://doi.org/10.5194/cp-8-2069-2012, 2012
S. Frisia, A. Borsato, R. N. Drysdale, B. Paul, A. Greig, and M. Cotte
Clim. Past, 8, 2039–2051, https://doi.org/10.5194/cp-8-2039-2012, https://doi.org/10.5194/cp-8-2039-2012, 2012
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Holocene
High-resolution Holocene record based on detailed tephrochronology from Torfdalsvatn, north Iceland, reveals natural and anthropogenic impacts on terrestrial and aquatic environments
Multi-century mean summer temperature variations in the Southern Rhaetian Alps reconstructed from Larix decidua blue intensity data
A continental reconstruction of hydroclimatic variability in South America during the past 2000 years
A Holocene history of climate, fire, landscape evolution, and human activity in northeastern Iceland
A global compilation of diatom silica oxygen isotope records from lake sediment – trends and implications for climate reconstruction
BrGDGT-based seasonal paleotemperature reconstruction for the last 15 000 years from a shallow lake on the eastern Tibetan Plateau
Reconstructing 15 000 years of southern France temperatures from coupled pollen and molecular (branched glycerol dialkyl glycerol tetraether) markers (Canroute, Massif Central)
Pollen-based reconstructions of Holocene climate trends in the eastern Mediterranean region
Spatiotemporal Intertropical Convergence Zone dynamics during the last 3 millennia in northeastern Brazil and related impacts in modern human history
Holocene climates of the Iberian Peninsula: pollen-based reconstructions of changes in the west–east gradient of temperature and moisture
Holocene climate and oceanography of the coastal Western United States and California Current System
Reconstructing Holocene temperatures in time and space using paleoclimate data assimilation
Long-term trends in diatom diversity and palaeoproductivity: a 16 000-year multidecadal record from Lake Baikal, southern Siberia
A 406-year non-growing-season precipitation reconstruction in the southeastern Tibetan Plateau
Climatic variations during the Holocene inferred from radiocarbon and stable carbon isotopes in speleothems from a high-alpine cave
Winter–spring warming in the North Atlantic during the last 2000 years: evidence from southwest Iceland
Climate reconstructions based on GDGT and pollen surface datasets from Mongolia and Baikal area: calibrations and applicability to extremely cold–dry environments over the Late Holocene
Sampling density and date along with species selection influence spatial representation of tree-ring reconstructions
Changes in high-intensity precipitation on the northern Apennines (Italy) as revealed by multidisciplinary data over the last 9000 years
Neoglacial trends in diatom dynamics from a small alpine lake in the Qinling mountains of central China
Centennial- to millennial-scale monsoon changes since the last deglaciation linked to solar activities and North Atlantic cooling
Algal lipids reveal unprecedented warming rates in alpine areas of SW Europe during the industrial period
Reconstructing seasonality through stable-isotope and trace-element analyses of the Proserpine stalagmite, Han-sur-Lesse cave, Belgium: indications for climate-driven changes during the last 400 years
Two millennia of Main region (southern Germany) hydroclimate variability
Combining a pollen and macrofossil synthesis with climate simulations for spatial reconstructions of European climate using Bayesian filtering
Lignin oxidation products as a potential proxy for vegetation and environmental changes in speleothems and cave drip water – a first record from the Herbstlabyrinth, central Germany
How dry was the Younger Dryas? Evidence from a coupled δ2H–δ18O biomarker paleohygrometer applied to the Gemündener Maar sediments, Western Eifel, Germany
Siberian tree-ring and stable isotope proxies as indicators of temperature and moisture changes after major stratospheric volcanic eruptions
Technical note: Optimizing the utility of combined GPR, OSL, and Lidar (GOaL) to extract paleoenvironmental records and decipher shoreline evolution
The onset of neoglaciation in Iceland and the 4.2 ka event
Hydroclimatic variations in southeastern China during the 4.2 ka event reflected by stalagmite records
Fire, vegetation, and Holocene climate in a southeastern Tibetan lake: a multi-biomarker reconstruction from Paru Co
Climate impact on the development of Pre-Classic Maya civilisation
Synchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minima
Technical note: Open-paleo-data implementation pilot – the PAGES 2k special issue
A chironomid-based record of temperature variability during the past 4000 years in northern China and its possible societal implications
Insights into Atlantic multidecadal variability using the Last Millennium Reanalysis framework
Three distinct Holocene intervals of stalagmite deposition and nondeposition revealed in NW Madagascar, and their paleoclimate implications
Examining bias in pollen-based quantitative climate reconstructions induced by human impact on vegetation in China
A dual-biomarker approach for quantification of changes in relative humidity from sedimentary lipid D∕H ratios
Pseudo-proxy tests of the analogue method to reconstruct spatially resolved global temperature during the Common Era
Development and evaluation of a system of proxy data assimilation for paleoclimate reconstruction
A chironomid-based mean July temperature inference model from the south-east margin of the Tibetan Plateau, China
Assessing performance and seasonal bias of pollen-based climate reconstructions in a perfect model world
Quantitative reconstruction of summer precipitation using a mid-Holocene δ13C common millet record from Guanzhong Basin, northern China
North Atlantic Oscillation controls on oxygen and hydrogen isotope gradients in winter precipitation across Europe; implications for palaeoclimate studies
A 368-year maximum temperature reconstruction based on tree-ring data in the northwestern Sichuan Plateau (NWSP), China
Inferring late-Holocene climate in the Ecuadorian Andes using a chironomid-based temperature inference model
A high-altitude peatland record of environmental changes in the NW Argentine Andes (24 ° S) over the last 2100 years
Technical note: The Linked Paleo Data framework – a common tongue for paleoclimatology
David J. Harning, Christopher R. Florian, Áslaug Geirsdóttir, Thor Thordarson, Gifford H. Miller, Yarrow Axford, and Sædís Ólafsdóttir
Clim. Past, 21, 795–815, https://doi.org/10.5194/cp-21-795-2025, https://doi.org/10.5194/cp-21-795-2025, 2025
Short summary
Short summary
Questions remain about the past climate in Iceland, including the relative impacts of natural and human factors on vegetation change and soil erosion. We present a sub-centennial-scale record of landscape and algal productivity from a lake in north Iceland. Along with a high-resolution tephra age constraint that covers the last ∼ 12 000 years, our record provides an environmental template for the region and novel insight into the sensitivity of the Icelandic ecosystem to natural and human impacts.
Riccardo Cerrato, Maria Cristina Salvatore, Michele Brunetti, Andrea Somma, and Carlo Baroni
Clim. Past, 21, 609–626, https://doi.org/10.5194/cp-21-609-2025, https://doi.org/10.5194/cp-21-609-2025, 2025
Short summary
Short summary
Understanding past climates requires data extending beyond modern instrumental records. This study shows that blue intensity (BI) measurements from European larch trees in the Southern Rhaetian Alps provide a stronger proxy for reconstructing past summer temperatures than traditional tree-ring-width data. BI processing enables regional-scale reconstructions and helps extend these reconstructions to the Mediterranean Basin and northern Europe, with excellent correlations to existing data.
Mathurin A. Choblet, Janica C. Bühler, Valdir F. Novello, Nathan J. Steiger, and Kira Rehfeld
Clim. Past, 20, 2117–2141, https://doi.org/10.5194/cp-20-2117-2024, https://doi.org/10.5194/cp-20-2117-2024, 2024
Short summary
Short summary
Past climate reconstructions are essential for understanding climate mechanisms and drivers. Our focus is on the South American continent over the past 2000 years. We offer a new reconstruction that particularly utilizes data from speleothems, previously absent from continent-wide reconstructions. We use paleoclimate data assimilation, a reconstruction method that combines information from climate archives and climate simulations.
Nicolò Ardenghi, David J. Harning, Jonathan H. Raberg, Brooke R. Holman, Thorvaldur Thordarson, Áslaug Geirsdóttir, Gifford H. Miller, and Julio Sepúlveda
Clim. Past, 20, 1087–1123, https://doi.org/10.5194/cp-20-1087-2024, https://doi.org/10.5194/cp-20-1087-2024, 2024
Short summary
Short summary
Analysing a sediment record from Stóra Viðarvatn (NE Iceland), we reveal how natural factors and human activities influenced environmental changes (erosion, wildfires) over the last 11 000 years. We found increased fire activity around 3000 and 1500 years ago, predating human settlement, likely driven by natural factors like precipitation shifts. Declining summer temperatures increased erosion vulnerability, exacerbated by farming and animal husbandry, which in turn may have reduced wildfires.
Philip Meister, Anne Alexandre, Hannah Bailey, Philip Barker, Boris K. Biskaborn, Ellie Broadman, Rosine Cartier, Bernhard Chapligin, Martine Couapel, Jonathan R. Dean, Bernhard Diekmann, Poppy Harding, Andrew C. G. Henderson, Armand Hernandez, Ulrike Herzschuh, Svetlana S. Kostrova, Jack Lacey, Melanie J. Leng, Andreas Lücke, Anson W. Mackay, Eniko Katalin Magyari, Biljana Narancic, Cécile Porchier, Gunhild Rosqvist, Aldo Shemesh, Corinne Sonzogni, George E. A. Swann, Florence Sylvestre, and Hanno Meyer
Clim. Past, 20, 363–392, https://doi.org/10.5194/cp-20-363-2024, https://doi.org/10.5194/cp-20-363-2024, 2024
Short summary
Short summary
This paper presents the first comprehensive compilation of diatom oxygen isotope records in lake sediments (δ18OBSi), supported by lake basin parameters. We infer the spatial and temporal coverage of δ18OBSi records and discuss common hemispheric trends on centennial and millennial timescales. Key results are common patterns for hydrologically open lakes in Northern Hemisphere extratropical regions during the Holocene corresponding to known climatic epochs, i.e. the Holocene Thermal Maximum.
Xiaohuan Hou, Nannan Wang, Zhe Sun, Kan Yuan, Xianyong Cao, and Juzhi Hou
Clim. Past, 20, 335–348, https://doi.org/10.5194/cp-20-335-2024, https://doi.org/10.5194/cp-20-335-2024, 2024
Short summary
Short summary
We present an ice-free season temperature based on brGDGTs over last 15 kyr on the eastern Tibetan Plateau (TP). The result shows that Holocene Thermal Maximum occurred during 8–3.5 ka, which lags behind pollen-based temperature recorded in same core, indicating a significant seasonal bias between different proxies. We also investigated previously published brGDGT-based temperatures on the TP to determine the pattern of Holocene temperature changes and possible reasons for the diverse records.
Léa d'Oliveira, Lucas Dugerdil, Guillemette Ménot, Allowen Evin, Serge D. Muller, Salomé Ansanay-Alex, Julien Azuara, Colline Bonnet, Laurent Bremond, Mehmet Shah, and Odile Peyron
Clim. Past, 19, 2127–2156, https://doi.org/10.5194/cp-19-2127-2023, https://doi.org/10.5194/cp-19-2127-2023, 2023
Short summary
Short summary
In southern Europe, Holocene climate variability is characterized by a strong heterogeneity whose patterns are still poorly understood. Here, a multi-proxy approach (pollen and biomarkers) is applied to the Canroute sequence to reconstruct the climatic variation over the last 15 000 years in southern Massif Central, France. Results reveal that reconstructions of regional climate trends notably differ depending on proxies and sites, notably concerning the presence of a Holocene thermal maximum.
Esmeralda Cruz-Silva, Sandy P. Harrison, I. Colin Prentice, Elena Marinova, Patrick J. Bartlein, Hans Renssen, and Yurui Zhang
Clim. Past, 19, 2093–2108, https://doi.org/10.5194/cp-19-2093-2023, https://doi.org/10.5194/cp-19-2093-2023, 2023
Short summary
Short summary
We examined 71 pollen records (12.3 ka to present) in the eastern Mediterranean, reconstructing climate changes. Over 9000 years, winters gradually warmed due to orbital factors. Summer temperatures peaked at 4.5–5 ka, likely declining because of ice sheets. Moisture increased post-11 kyr, remaining high from 10–6 kyr before a slow decrease. Climate models face challenges in replicating moisture transport.
Giselle Utida, Francisco W. Cruz, Mathias Vuille, Angela Ampuero, Valdir F. Novello, Jelena Maksic, Gilvan Sampaio, Hai Cheng, Haiwei Zhang, Fabio Ramos Dias de Andrade, and R. Lawrence Edwards
Clim. Past, 19, 1975–1992, https://doi.org/10.5194/cp-19-1975-2023, https://doi.org/10.5194/cp-19-1975-2023, 2023
Short summary
Short summary
We reconstruct the Intertropical Convergence Zone (ITCZ) behavior during the past 3000 years over northeastern Brazil based on oxygen stable isotopes of stalagmites. Paleoclimate changes were mainly forced by the tropical South Atlantic and tropical Pacific sea surface temperature variability. We describe an ITCZ zonal behavior active around 1100 CE and the period from 1500 to 1750 CE. The dataset also records historical droughts that affected modern human population in this area of Brazil.
Mengmeng Liu, Yicheng Shen, Penelope González-Sampériz, Graciela Gil-Romera, Cajo J. F. ter Braak, Iain Colin Prentice, and Sandy P. Harrison
Clim. Past, 19, 803–834, https://doi.org/10.5194/cp-19-803-2023, https://doi.org/10.5194/cp-19-803-2023, 2023
Short summary
Short summary
We reconstructed the Holocene climates in the Iberian Peninsula using a large pollen data set and found that the west–east moisture gradient was much flatter than today. We also found that the winter was much colder, which can be expected from the low winter insolation during the Holocene. However, summer temperature did not follow the trend of summer insolation, instead, it was strongly correlated with moisture.
Hannah M. Palmer, Veronica Padilla Vriesman, Caitlin M. Livsey, Carina R. Fish, and Tessa M. Hill
Clim. Past, 19, 199–232, https://doi.org/10.5194/cp-19-199-2023, https://doi.org/10.5194/cp-19-199-2023, 2023
Short summary
Short summary
To better understand and contextualize modern climate change, this systematic review synthesizes climate and oceanographic patterns in the Western United States and California Current System through the most recent 11.75 kyr. Through a literature review and coded analysis of past studies, we identify distinct environmental phases through time and linkages between marine and terrestrial systems. We explore climate change impacts on ecosystems and human–environment interactions.
Michael P. Erb, Nicholas P. McKay, Nathan Steiger, Sylvia Dee, Chris Hancock, Ruza F. Ivanovic, Lauren J. Gregoire, and Paul Valdes
Clim. Past, 18, 2599–2629, https://doi.org/10.5194/cp-18-2599-2022, https://doi.org/10.5194/cp-18-2599-2022, 2022
Short summary
Short summary
To look at climate over the past 12 000 years, we reconstruct spatial temperature using natural climate archives and information from model simulations. Our results show mild global mean warmth around 6000 years ago, which differs somewhat from past reconstructions. Undiagnosed seasonal biases in the data could explain some of the observed temperature change, but this still would not explain the large difference between many reconstructions and climate models over this period.
Anson W. Mackay, Vivian A. Felde, David W. Morley, Natalia Piotrowska, Patrick Rioual, Alistair W. R. Seddon, and George E. A. Swann
Clim. Past, 18, 363–380, https://doi.org/10.5194/cp-18-363-2022, https://doi.org/10.5194/cp-18-363-2022, 2022
Short summary
Short summary
We investigated the diversity of algae called diatoms in Lake Baikal, the oldest and deepest lake in the world, because algae sit at the base of aquatic foodwebs and provide energy (in the form of primary production) for other organisms to use. Diatom diversity and primary production have been influenced by both long-term and abrupt climate change over the past 16 000 years. The shape of these responses appears to be time-period specific.
Maierdang Keyimu, Zongshan Li, Bojie Fu, Guohua Liu, Fanjiang Zeng, Weiliang Chen, Zexin Fan, Keyan Fang, Xiuchen Wu, and Xiaochun Wang
Clim. Past, 17, 2381–2392, https://doi.org/10.5194/cp-17-2381-2021, https://doi.org/10.5194/cp-17-2381-2021, 2021
Short summary
Short summary
We created a residual tree-ring width chronology and reconstructed non-growth-season precipitation (NGSP) over the period spanning 1600–2005 in the southeastern Tibetan Plateau (SETP), China. Reconstruction model verification as well as similar variations of NGSP reconstruction and Palmer Drought Severity Index reconstructions from the surrounding region indicate the reliability of the present reconstruction. Our reconstruction is representative of NGSP variability of a large region in the SETP.
Caroline Welte, Jens Fohlmeister, Melina Wertnik, Lukas Wacker, Bodo Hattendorf, Timothy I. Eglinton, and Christoph Spötl
Clim. Past, 17, 2165–2177, https://doi.org/10.5194/cp-17-2165-2021, https://doi.org/10.5194/cp-17-2165-2021, 2021
Short summary
Short summary
Stalagmites are valuable climate archives, but unlike other proxies the use of stable carbon isotopes (δ13C) is still difficult. A stalagmite from the Austrian Alps was analyzed using a new laser ablation method for fast radiocarbon (14C) analysis. This allowed 14C and δ13C to be combined, showing that besides soil and bedrock a third source is contributing during periods of warm, wet climate: old organic matter.
Nora Richter, James M. Russell, Johanna Garfinkel, and Yongsong Huang
Clim. Past, 17, 1363–1383, https://doi.org/10.5194/cp-17-1363-2021, https://doi.org/10.5194/cp-17-1363-2021, 2021
Short summary
Short summary
We present a reconstruction of winter–spring temperatures developed using organic proxies preserved in well-dated lake sediments from southwest Iceland to assess seasonal temperature changes in the North Atlantic region over the last 2000 years. The gradual warming trend observed in our record is likely influenced by sea surface temperatures, which are sensitive to changes in ocean circulation and seasonal insolation, during the winter and spring season.
Lucas Dugerdil, Sébastien Joannin, Odile Peyron, Isabelle Jouffroy-Bapicot, Boris Vannière, Bazartseren Boldgiv, Julia Unkelbach, Hermann Behling, and Guillemette Ménot
Clim. Past, 17, 1199–1226, https://doi.org/10.5194/cp-17-1199-2021, https://doi.org/10.5194/cp-17-1199-2021, 2021
Short summary
Short summary
Since the understanding of Holocene climate change appears to be a relevant issue for future climate change, the paleoclimate calibrations have to be improved. Here, surface samples from Mongolia and Siberia were analyzed to provide new calibrations for pollen and biomarker climate models. These calibrations appear to be more powerful than global calibrations, especially in an arid central Asian context. These calibrations will improve the understanding of monsoon Holocene oscillations.
Justin T. Maxwell, Grant L. Harley, Trevis J. Matheus, Brandon M. Strange, Kayla Van Aken, Tsun Fung Au, and Joshua C. Bregy
Clim. Past, 16, 1901–1916, https://doi.org/10.5194/cp-16-1901-2020, https://doi.org/10.5194/cp-16-1901-2020, 2020
Short summary
Short summary
We found that increasing the density of chronologies in the tree-ring network resulted in estimated soil moisture conditions that better matched the spatial variability of the values that were instrumentally recorded for droughts and, to a lesser extent, pluvials. By sampling trees in 2010 compared to 1980, the sensitivity of tree rings to soil moisture decreased in the southern portion of our region, where severe drought conditions have been absent over recent decades.
Stefano Segadelli, Federico Grazzini, Veronica Rossi, Margherita Aguzzi, Silvia Marvelli, Marco Marchesini, Alessandro Chelli, Roberto Francese, Maria Teresa De Nardo, and Sandro Nanni
Clim. Past, 16, 1547–1564, https://doi.org/10.5194/cp-16-1547-2020, https://doi.org/10.5194/cp-16-1547-2020, 2020
Short summary
Short summary
In an attempt to consolidate trends in the hydrological cycle induced by recent warming, we conducted a multidisciplinary study combining meteorological data, climate proxies from the literature, and original coring and pollen data acquired in an area that has been hit by record-breaking precipitation events. A detailed study of recent flash-flood deposits compared with fossil peat bog and lake sediments supports the expected increase in precipitation intensity during warm climatic phases.
Bo Cheng, Jennifer Adams, Jianhui Chen, Aifeng Zhou, Qing Zhang, and Anson W. Mackay
Clim. Past, 16, 543–554, https://doi.org/10.5194/cp-16-543-2020, https://doi.org/10.5194/cp-16-543-2020, 2020
Short summary
Short summary
The Qinling mountains in China are biodiversity rich. We studied one of the high-latitude lakes on Mount Taibai with a view to looking at how aquatic diversity responded to long-term changes in climate over the past 3500 years. We specifically looked at a group of single-celled algae called diatoms, as they are very sensitive to the environment. We found that these algae changed gradually over time, but they showed abrupt change during the period known as the Little Ice Age, about 400 years ago.
Xingxing Liu, Youbin Sun, Jef Vandenberghe, Peng Cheng, Xu Zhang, Evan J. Gowan, Gerrit Lohmann, and Zhisheng An
Clim. Past, 16, 315–324, https://doi.org/10.5194/cp-16-315-2020, https://doi.org/10.5194/cp-16-315-2020, 2020
Short summary
Short summary
The East Asian summer monsoon and winter monsoon are anticorrelated on a centennial timescale during 16–1 ka. The centennial monsoon variability is connected to changes of both solar activity and North Atlantic cooling events during the Early Holocene. Then, North Atlantic cooling became the major forcing of events during the Late Holocene. This work presents the great challenge and potential to understand the response of the monsoon system to global climate changes in the past and the future.
Antonio García-Alix, Jaime L. Toney, Gonzalo Jiménez-Moreno, Carmen Pérez-Martínez, Laura Jiménez, Marta Rodrigo-Gámiz, R. Scott Anderson, Jon Camuera, Francisco J. Jiménez-Espejo, Dhais Peña-Angulo, and María J. Ramos-Román
Clim. Past, 16, 245–263, https://doi.org/10.5194/cp-16-245-2020, https://doi.org/10.5194/cp-16-245-2020, 2020
Short summary
Short summary
In this paper we identify warming thresholds, rates, and forcing mechanisms from a novel alpine temperature record of the southern Iberian Peninsula during the Common Era in order to contextualize the modern warming and its potential impact on these vulnerable alpine ecosystems. To do so, we have developed and applied the first lacustrine temperature calibration in alpine lakes for algal compounds, called long-chain alkyl diols, which is a significant advance in biomarker paleothermometry.
Stef Vansteenberge, Niels J. de Winter, Matthias Sinnesael, Sophie Verheyden, Steven Goderis, Stijn J. M. Van Malderen, Frank Vanhaecke, and Philippe Claeys
Clim. Past, 16, 141–160, https://doi.org/10.5194/cp-16-141-2020, https://doi.org/10.5194/cp-16-141-2020, 2020
Short summary
Short summary
We measured the chemical composition (trace-element concentrations and stable-isotope ratios) of a Belgian speleothem that deposited annual layers. Our sub-annual resolution dataset allows us to investigate how the chemistry of this speleothem recorded changes in the environment and climate in northwestern Europe. We then use this information to reconstruct climate change during the 16th and 17th century on the seasonal scale and demonstrate that environmental change drives speleothem chemistry.
Alexander Land, Sabine Remmele, Jutta Hofmann, Daniel Reichle, Margaret Eppli, Christian Zang, Allan Buras, Sebastian Hein, and Reiner Zimmermann
Clim. Past, 15, 1677–1690, https://doi.org/10.5194/cp-15-1677-2019, https://doi.org/10.5194/cp-15-1677-2019, 2019
Short summary
Short summary
With the use of precipitation sensitive oak ring-width series from the Main River region (southern Germany) a 2000-year long hydroclimate reconstruction has been developed. The ring series are sensitive to the sum of rainfall from 26 February to 6 July. This region suffered from severe, long-lasting droughts in the past two millennia (e.g., AD 500/510s, 940s, 1170s, 1390s and 1160s). In the AD 550s, 1050s, 1310s and 1480s, multi-year periods with high rainfall hit the region.
Nils Weitzel, Andreas Hense, and Christian Ohlwein
Clim. Past, 15, 1275–1301, https://doi.org/10.5194/cp-15-1275-2019, https://doi.org/10.5194/cp-15-1275-2019, 2019
Short summary
Short summary
A new method for probabilistic spatial reconstructions of past climate states is presented, which combines pollen data with a multi-model ensemble of climate simulations in a Bayesian framework. The approach is applied to reconstruct summer and winter temperature in Europe during the mid-Holocene. Our reconstructions account for multiple sources of uncertainty and are well suited for quantitative statistical analyses of the climate under different forcing conditions.
Inken Heidke, Denis Scholz, and Thorsten Hoffmann
Clim. Past, 15, 1025–1037, https://doi.org/10.5194/cp-15-1025-2019, https://doi.org/10.5194/cp-15-1025-2019, 2019
Short summary
Short summary
This is the first quantitative study of lignin biomarkers in stalagmites and cave drip water. Lignin is only produced by higher plants; therefore, its analysis can be used to reconstruct the vegetation of the past. We compared our lignin results with stable isotope and trace element records from the same samples and found correlations or similarities with P, Ba, U and Mg concentrations as well as δ13C values. These results can help to better interpret other vegetation proxies.
Johannes Hepp, Lorenz Wüthrich, Tobias Bromm, Marcel Bliedtner, Imke Kathrin Schäfer, Bruno Glaser, Kazimierz Rozanski, Frank Sirocko, Roland Zech, and Michael Zech
Clim. Past, 15, 713–733, https://doi.org/10.5194/cp-15-713-2019, https://doi.org/10.5194/cp-15-713-2019, 2019
Olga V. Churakova (Sidorova), Marina V. Fonti, Matthias Saurer, Sébastien Guillet, Christophe Corona, Patrick Fonti, Vladimir S. Myglan, Alexander V. Kirdyanov, Oksana V. Naumova, Dmitriy V. Ovchinnikov, Alexander V. Shashkin, Irina P. Panyushkina, Ulf Büntgen, Malcolm K. Hughes, Eugene A. Vaganov, Rolf T. W. Siegwolf, and Markus Stoffel
Clim. Past, 15, 685–700, https://doi.org/10.5194/cp-15-685-2019, https://doi.org/10.5194/cp-15-685-2019, 2019
Short summary
Short summary
We present a unique dataset of multiple tree-ring and stable isotope parameters, representing temperature-sensitive Siberian ecotones, to assess climatic impacts after six large stratospheric volcanic eruptions at 535, 540, 1257, 1640, 1815, and 1991 CE. Besides the well-documented effects of temperature derived from tree-ring width and latewood density, stable carbon and oxygen isotopes in tree-ring cellulose provide information about moisture and sunshine duration changes after the events.
Amy J. Dougherty, Jeong-Heon Choi, Chris S. M. Turney, and Anthony Dosseto
Clim. Past, 15, 389–404, https://doi.org/10.5194/cp-15-389-2019, https://doi.org/10.5194/cp-15-389-2019, 2019
Áslaug Geirsdóttir, Gifford H. Miller, John T. Andrews, David J. Harning, Leif S. Anderson, Christopher Florian, Darren J. Larsen, and Thor Thordarson
Clim. Past, 15, 25–40, https://doi.org/10.5194/cp-15-25-2019, https://doi.org/10.5194/cp-15-25-2019, 2019
Short summary
Short summary
Compositing climate proxies in sediment from seven Iceland lakes documents abrupt summer cooling between 4.5 and 4.0 ka, statistically indistinguishable from 4.2 ka. Although the decline in summer insolation was an important factor, a combination of superposed changes in ocean circulation and explosive Icelandic volcanism were likely responsible for the abrupt perturbation recorded by our proxies. Lake and catchment proxies recovered to a colder equilibrium state following the perturbation.
Haiwei Zhang, Hai Cheng, Yanjun Cai, Christoph Spötl, Gayatri Kathayat, Ashish Sinha, R. Lawrence Edwards, and Liangcheng Tan
Clim. Past, 14, 1805–1817, https://doi.org/10.5194/cp-14-1805-2018, https://doi.org/10.5194/cp-14-1805-2018, 2018
Short summary
Short summary
The collapses of several Neolithic cultures in China are considered to have been associated with abrupt climate change during the 4.2 ka BP event; however, the hydroclimate of this event in China is still poorly known. Based on stalagmite records from monsoonal China, we found that north China was dry but south China was wet during this event. We propose that the rain belt remained longer at its southern position, giving rise to a pronounced humidity gradient between north and south China.
Alice Callegaro, Dario Battistel, Natalie M. Kehrwald, Felipe Matsubara Pereira, Torben Kirchgeorg, Maria del Carmen Villoslada Hidalgo, Broxton W. Bird, and Carlo Barbante
Clim. Past, 14, 1543–1563, https://doi.org/10.5194/cp-14-1543-2018, https://doi.org/10.5194/cp-14-1543-2018, 2018
Short summary
Short summary
Holocene fires and vegetation are reconstructed using different molecular markers with a single analytical method, applied for the first time to lake sediments from Tibet. The early Holocene shows oscillations between grasses and conifers, with smouldering fires represented by levoglucosan peaks, and high-temperature fires represented by PAHs. The lack of human FeSts excludes local human influence on fire and vegetation changes. Late Holocene displays an increase in local to regional combustion.
Kees Nooren, Wim Z. Hoek, Brian J. Dermody, Didier Galop, Sarah Metcalfe, Gerald Islebe, and Hans Middelkoop
Clim. Past, 14, 1253–1273, https://doi.org/10.5194/cp-14-1253-2018, https://doi.org/10.5194/cp-14-1253-2018, 2018
Short summary
Short summary
We present two new palaeoclimatic records for the central Maya lowlands, adding valuable new insights to the impact of climate change on the development of Maya civilisation. Lake Tuspan's diatom record is indicative of precipitation changes at a local scale, while a beach ridge elevation record from the world's largest late Holocene beach ridge plain provides a regional picture.
Markus Czymzik, Raimund Muscheler, Florian Adolphi, Florian Mekhaldi, Nadine Dräger, Florian Ott, Michał Słowinski, Mirosław Błaszkiewicz, Ala Aldahan, Göran Possnert, and Achim Brauer
Clim. Past, 14, 687–696, https://doi.org/10.5194/cp-14-687-2018, https://doi.org/10.5194/cp-14-687-2018, 2018
Short summary
Short summary
Our results provide a proof of concept for facilitating 10Be in varved lake sediments as a novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. They also point to some limitations of 10Be in these archives mainly connected to in-lake sediment resuspension processes.
Darrell S. Kaufman and PAGES 2k special-issue editorial team
Clim. Past, 14, 593–600, https://doi.org/10.5194/cp-14-593-2018, https://doi.org/10.5194/cp-14-593-2018, 2018
Short summary
Short summary
We explain the procedure used to attain a high and consistent level of data stewardship across a special issue of the journal Climate of the Past. We discuss the challenges related to (1) determining which data are essential for public archival, (2) using data generated by others, and (3) understanding data citations. We anticipate that open-data sharing in paleo sciences will accelerate as the advantages become more evident and as practices that reduce data loss become the accepted convention.
Haipeng Wang, Jianhui Chen, Shengda Zhang, David D. Zhang, Zongli Wang, Qinghai Xu, Shengqian Chen, Shijin Wang, Shichang Kang, and Fahu Chen
Clim. Past, 14, 383–396, https://doi.org/10.5194/cp-14-383-2018, https://doi.org/10.5194/cp-14-383-2018, 2018
Short summary
Short summary
The chironomid-inferred temperature record from Gonghai Lake exhibits a stepwise decreasing trend since 4 ka. A cold event in the Era of Disunity, the Sui-Tang Warm Period, the Medieval Warm Period and the Little Ice Age can all be recognized in our record, as well as in many other temperature reconstructions in China. Local wars in Shanxi Province, documented in the historical literature during the past 2700 years, are statistically significantly correlated with changes in temperature.
Hansi K. A. Singh, Gregory J. Hakim, Robert Tardif, Julien Emile-Geay, and David C. Noone
Clim. Past, 14, 157–174, https://doi.org/10.5194/cp-14-157-2018, https://doi.org/10.5194/cp-14-157-2018, 2018
Short summary
Short summary
The Atlantic Multidecadal Oscillation (AMO) is prominent in the climate system. We study the AMO over the last 2000 years using a novel proxy framework, the Last Millennium Reanalysis. We find that the AMO is linked to continental warming, Arctic sea ice retreat, and an Atlantic precipitation shift. Low clouds decrease globally. We find no distinct multidecadal spectral peak in the AMO over the last 2 millennia, suggesting that human activities may have enhanced the AMO in the modern era.
Ny Riavo Gilbertinie Voarintsoa, Loren Bruce Railsback, George Albert Brook, Lixin Wang, Gayatri Kathayat, Hai Cheng, Xianglei Li, Richard Lawrence Edwards, Amos Fety Michel Rakotondrazafy, and Marie Olga Madison Razanatseheno
Clim. Past, 13, 1771–1790, https://doi.org/10.5194/cp-13-1771-2017, https://doi.org/10.5194/cp-13-1771-2017, 2017
Short summary
Short summary
This research has been an investigation of two stalagmites from two caves in NW Madagascar to reconstruct the region's paleoenvironmental changes, and to understand the linkage of such changes to the dynamics of the ITCZ. Stable isotopes, mineralogy, and petrography suggest wetter climate conditions than today during the early and late Holocene, when the mean ITCZ was south, and drier during the mid-Holocene when the ITCZ was north.
Wei Ding, Qinghai Xu, and Pavel E. Tarasov
Clim. Past, 13, 1285–1300, https://doi.org/10.5194/cp-13-1285-2017, https://doi.org/10.5194/cp-13-1285-2017, 2017
Short summary
Short summary
Pollen-based past climate reconstruction for regions with long-term human occupation is always controversial. We examined the bias induced by the human impact on vegetation in a climate reconstruction for temperate eastern China by comparing the deviations in the reconstructed results for a fossil record based on two pollen–climate calibration sets. Climatic signals in pollen assemblages are indeed obscured by human impact; however, the extent of the bias could be assessed.
Oliver Rach, Ansgar Kahmen, Achim Brauer, and Dirk Sachse
Clim. Past, 13, 741–757, https://doi.org/10.5194/cp-13-741-2017, https://doi.org/10.5194/cp-13-741-2017, 2017
Short summary
Short summary
Currently, reconstructions of past changes in the hydrological cycle are usually qualitative, which is a major drawback for testing the accuracy of models in predicting future responses. Here we present a proof of concept of a novel approach to deriving quantitative paleohydrological data, i.e. changes in relative humidity, from lacustrine sediment archives, employing a combination of organic geochemical methods and plant physiological modeling.
Juan José Gómez-Navarro, Eduardo Zorita, Christoph C. Raible, and Raphael Neukom
Clim. Past, 13, 629–648, https://doi.org/10.5194/cp-13-629-2017, https://doi.org/10.5194/cp-13-629-2017, 2017
Short summary
Short summary
This contribution aims at assessing to what extent the analogue method, a classic technique used in other branches of meteorology and climatology, can be used to perform gridded reconstructions of annual temperature based on the limited information from available but un-calibrated proxies spread across different locations of the world. We conclude that it is indeed possible, albeit with certain limitations that render the method comparable to more classic techniques.
Atsushi Okazaki and Kei Yoshimura
Clim. Past, 13, 379–393, https://doi.org/10.5194/cp-13-379-2017, https://doi.org/10.5194/cp-13-379-2017, 2017
Short summary
Short summary
Data assimilation has been successfully applied in the field of paleoclimatology to reconstruct past climate. However, data reconstructed from proxies have been assimilated, as opposed to the actual proxy values, which prevented full utilization of the information recorded in the proxies. This study propose a new data assimilation system in which actual proxy data are directly assimilated.
Enlou Zhang, Jie Chang, Yanmin Cao, Hongqu Tang, Pete Langdon, James Shulmeister, Rong Wang, Xiangdong Yang, and Ji Shen
Clim. Past, 13, 185–199, https://doi.org/10.5194/cp-13-185-2017, https://doi.org/10.5194/cp-13-185-2017, 2017
Short summary
Short summary
This paper reports the first development of sub-fossil chironomid-based mean July temperature transfer functions from China. The transfer functions yield reliable reconstructions that are comparable to the instrumental record. The application of this new tool will provide long-term quantitative palaeoclimate estimates from south-western China which is a critical region for understanding the dynamic and evolution of the Indian Ocean south-west Monsoon system.
Kira Rehfeld, Mathias Trachsel, Richard J. Telford, and Thomas Laepple
Clim. Past, 12, 2255–2270, https://doi.org/10.5194/cp-12-2255-2016, https://doi.org/10.5194/cp-12-2255-2016, 2016
Short summary
Short summary
Indirect evidence on past climate comes from the former composition of ecological communities such as plants, preserved as pollen grains in sediments of lakes. Transfer functions convert relative counts of species to a climatologically meaningful scale (e.g. annual mean temperature in degrees C). We show that the fundamental assumptions in the algorithms impact the reconstruction results in he idealized model world, in particular if the reconstructed variables were not ecologically relevant.
Qing Yang, Xiaoqiang Li, Xinying Zhou, Keliang Zhao, and Nan Sun
Clim. Past, 12, 2229–2240, https://doi.org/10.5194/cp-12-2229-2016, https://doi.org/10.5194/cp-12-2229-2016, 2016
Short summary
Short summary
The fossilized seeds of common millet are suited to the production of quantitative Holocene precipitation reconstructions. Our reconstructed results showed that summer precipitation from 7.7–3.4 ka BP was ~ 50 mm, or 17 % higher than present levels. Maximal mean summer precipitation peaked at 414 mm during 6.1–5.5 ka BP, ~ 109 mm, or 36 % higher than today, indicating the EASM peaked at this time. This work can provide a new proxy for further research into continuous paleoprecipitation sequences.
Michael Deininger, Martin Werner, and Frank McDermott
Clim. Past, 12, 2127–2143, https://doi.org/10.5194/cp-12-2127-2016, https://doi.org/10.5194/cp-12-2127-2016, 2016
Short summary
Short summary
This study investigates the NAO (Northern Atlantic Oscillation)-related mechanisms that control winter precipitation stable oxygen and hydrogen isotope gradients across Europe. The results show that past longitudinal stable oxygen and hydrogen isotope gradients in European rainfall stored in palaeoclimate archives (e.g. speleothems) can be used to infer the past winter NAO modes from its variations.
Liangjun Zhu, Yuandong Zhang, Zongshan Li, Binde Guo, and Xiaochun Wang
Clim. Past, 12, 1485–1498, https://doi.org/10.5194/cp-12-1485-2016, https://doi.org/10.5194/cp-12-1485-2016, 2016
Short summary
Short summary
We present a 368-year late summer maximum temperature reconstruction based on spruce tree rings. It touches on the critical topic of climate reconstruction in the eastern edge of Tibetan Plateau and represents an extension and enhancement of climate records for this area. The Little Ice Age was well represented and 20th century warming was not obvious in this reconstruction. This temperature variation may be affected by global land–sea atmospheric circulation as well as solar and volcanic forcing.
Frazer Matthews-Bird, Stephen J. Brooks, Philip B. Holden, Encarni Montoya, and William D. Gosling
Clim. Past, 12, 1263–1280, https://doi.org/10.5194/cp-12-1263-2016, https://doi.org/10.5194/cp-12-1263-2016, 2016
Short summary
Short summary
Chironomidae are a family of two-winged aquatic fly of the order Diptera. The family is species rich (> 5000 described species) and extremely sensitive to environmental change, particualy temperature. Across the Northern Hemisphere, chironomids have been widely used as paleotemperature proxies as the chitinous remains of the insect are readily preserved in lake sediments. This is the first study using chironomids as paleotemperature proxies in tropical South America.
Karsten Schittek, Sebastian T. Kock, Andreas Lücke, Jonathan Hense, Christian Ohlendorf, Julio J. Kulemeyer, Liliana C. Lupo, and Frank Schäbitz
Clim. Past, 12, 1165–1180, https://doi.org/10.5194/cp-12-1165-2016, https://doi.org/10.5194/cp-12-1165-2016, 2016
Short summary
Short summary
Cushion peatlands are versatile climate archives for the study of past environmental changes. We present the environmental history for the last 2100 years of Cerro Tuzgle peatland, which is located in the NW Argentine Puna. The results reflect prominent late Holocene climate anomalies and provide evidence that Northern Hemisphere climate oscillations were extensive. Volcanic forcing at the beginning of the 19th century seems to have had an impact on climatic settings in the Central Andes
Nicholas P. McKay and Julien Emile-Geay
Clim. Past, 12, 1093–1100, https://doi.org/10.5194/cp-12-1093-2016, https://doi.org/10.5194/cp-12-1093-2016, 2016
Short summary
Short summary
The lack of accepted data formats and data standards in paleoclimatology is a growing problem that slows progress in the field. Here, we propose a preliminary data standard for paleoclimate data, general enough to accommodate all the proxy and measurement types encountered in a large international collaboration (PAGES 2k). We also introduce a data format for such structured data (Linked Paleo Data, or LiPD), leveraging recent advances in knowledge representation (Linked Open Data).
Cited articles
Almogi-Labin, A., Bar-Matthews, M., Shriki, D., Kolosovsky, E., Paterne, M.,
Schilman, B., Ayalon, A., Aizenshtat, Z., and Matthews, A.: Climatic
variability during the last 90 ka of the southern and northern Levantine
Basin as evident from marine records and speleothems, Quaternary Sci. Rev.,
28, 2882–2896, 2009.
Alpert, P., Baldi, M., Ilani, R., Krichak, S., Price, C., Rodo, X., Saaroni,
H., Ziv, B., Kishcha, P., Barkan, J., Mariotti, A., and Xoplaki, E.: Relations
between climate variability in the Mediterranean region and the tropics:
ENSO, South Asian and African monsoons, hurricanes and Saharan dust, in:
Developments in Earth and Environmental Sciences, Elsevier, 4, 149–177, 2006 a
Bajo, P., Hellstrom, J., Frisia, S., Drysdale, R., Black, J., Woodhead, J.,
Borsato, A., Wallace, M. W., Regattieri, E., and Haese, R.: “Cryptic”
diagenesis and its implications for speleothem geochronologies, Quaternary
Sci. Rev., 148, 17–28, 2016. a
Baldini, L. M., McDermott, F., Foley, A. M., and Baldini, J. U.: Spatial
variability in the European winter precipitation
δ18O–NAO relationship: Implications for
reconstructing NAO-mode climate variability in the Holocene, Geophys.
Res. Lett., 35, L04709, https://doi.org/10.1029/2007GL032027, 2008. a
Bard, E., Delaygue, G., Rostek, F., Antonioli, F., Silenzi, S., and Schrag,
D.: Hydrological conditions in the western Mediterranean basin during the
deposition of Sapropel 6 (ca. 175 kyr), Earth Planet. Sc. Lett., 202,
481–494, 2002. a
Bar-Matthews, M. and Ayalon, A.: Mid-Holocene climate variations revealed by
high-resolution speleothems records from Soreq Cave, Israel and their
correlation with cultural changes, Holocene, 21, 163–171, 2011.
Baroni, C., Zanchetta, G., Fallick, A. E., and Longinelli, A.: Molluscs
stable isotope record of a core from Lake Frassino (northern Italy):
hydrological and climatic changes during the last 14 ka, Holocene, 16,
827–837, 2006. a
Belli, R., Frisia, S., Borsato, A., Drysdale R., Hellstrom, J., Zhao J.-X.,
and Spötl, C.: Regional climate variability and ecosystem responses to
the last deglaciation in the northern hemisphere from stable isotope data and
calcite fabrics in two northern Adriatic stalagmites, Quaternary Sci. Rev.,
72, 146–158, 2013. a
Berger, A. and Loutre, M. F.: Insolation values for the climate of the last
10 million years, Quaternary Sci. Rev., 10, 297–317, 1991. a
Birks, J., Battarbee, R., Mackay, A., and Oldfield, F.: Global Change in the
Holocene, Routledge, 544 pp., 2005. a
Birks, H. J. B., Heiri, O., Seppa, H., and Bjune, A.: Strengths and
weaknesses of quantitative climate reconstructions based on late-Quaternary
biological proxies, Open Ecol. J., 3, 68–110, 2010. a
Blanco-Gonzalez, A., Lillios, K. T., López-Sáez, J. A., and Drake, B.
L.: Cultural, demographic and environmental dynamics of the Copper and Early
Bronze Age in Iberia (3300–1500 BC): towards an interregional multiproxy
comparison at the time of the 4.2 ky BP event, J. World Prehist., 31,
1–79, 2018. a, b
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., de Menocal, P.,
Priore, P., Cullen, H., Hajdas, I., and Bonani, G.: A pervasive
millennial-scale cycle in the North Atlantic Holocene and glacial climates,
Science, 294, 2130–2136, 1997. a
Booth, R. K., Jackson, S. T., Forman, S. L., Kutzbach, J. E., Bettis III, E.
A., Kreig, J., and Wright, D. K.: A severe centennial-scale drought in
midcontinental North America 4200 years ago and apparent global linkages,
Holocene, 15, 321–328, 2005. a
Braconnot, P., Otto-Bliesner, B., Harrison, S., Joussaume, S., Peterchmitt,
J.-Y., Abe-Ouchi, A., Crucifix, M., Driesschaert, E., Fichefet, Th., Hewitt,
C. D., Kageyama, M., Kitoh, A., Laîné, A., Loutre, M.-F., Marti, O.,
Merkel, U., Ramstein, G., Valdes, P., Weber, S. L., Yu, Y., and Zhao, Y.:
Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial
Maximum – Part 1: experiments and large-scale features, Clim. Past, 3,
261–277, https://doi.org/10.5194/cp-3-261-2007, 2007. a
Brayshaw, D. J., Hoskins, B., and Black, E.: Some physical drivers of changes
in the winter storm tracks over the North Atlantic and Mediterranean during
the Holocene, Philos. Tr. R. Soc. S.-A, 368, 5185–5223, 2010. a
Brewer, S., Guiot J., and Barboni, D.: Pollen methods and studies, Use of
Pollen as Climate Proxies, Encyclopedia of Quaternary Science, 805–815,
https://doi.org/10.1016/B978-0-444-53643-3.00180-1, 2013. a
Brisset, E., Miramont, C., Guiter, F., Anthony, E.J., Tachikawa, K.,
Poulenard, J., Arnaud, F., Delhon, C., Meunier, J.-D., Bard, E., and
Suméra, F.: Non-reversible geosystem destabilisation at 4200 cal. BP:
Sedimentological, geochemical and botanical markers of soil erosion recorded
in a Mediterranean alpine lake, Holocene 23, 1863–1874, 2013. a, b
Cacho, I., Grimalt, J. O., Canals, M., Sbaffi, L., Shackleton, N.,
Schönfeld, J., and Zahn, R.: Variability of the western Mediterranean Sea
surface temperature during the last 25 000 years and its connection with the
Northern Hemisphere climatic changes, Paleoceanography, 16, 40–52, 2001.
Carter, V. A., Shinker, J. J., and Preece, J.: Drought and vegetation change
in the central Rocky Mountains and western Great Plains: potential climatic
mechanisms associated with megadrought conditions at 4200 cal yr BP, Clim.
Past, 14, 1195–1212, https://doi.org/10.5194/cp-14-1195-2018, 2018. a
Cartier, R., Brisset, E., Guiter, F., Sylvestre, F., Tachikawa, K., Anthony,
E. J., Paillès, C., Bruneton, H., Bard, E., and Miramont, C.: Multiproxy
analyses of Lake Allos reveal synchronicity and divergence in geosystem
dynamics during the Lateglacial/Holocene in the Alps, Quaternary Sci. Rev.,
186, 60–77, 2018.
Cartier, R., Sylvestre, F., Paillès, C., Sonzogni, C., Couapel, M.,
Alexandre, A., Mazur, J.-C., Brisset, E., Miramont, C., and Guiter, F.:
Diatom-oxygen isotope record from high-altitude Lake Petit (2200 m a.s.l.)
in the Mediterranean Alps: shedding light on a climatic pulse at 4.2 ka,
Clim. Past, 15, 253–263, https://doi.org/10.5194/cp-15-253-2019, 2019. a, b
Cartier, R., Brisset, E., Paillès, C., Guiter, F., Sylvestre, F.,
Ruaudel, F., Anthony, E. J., and Miramont, C.: 5000 yr of lacustrine
ecosystem changes from Lake Petit (Southern Alps, 2200 m a.s.l.): Regime
shift and resilience of algal communities, Holocene, 25, 1231–1245, 2015. a
Castaneda, I. S., Schefuß, E., Pätzold, J., Sinninghe Damsté, J.
S., Weldeab, S., and Schouten, S.: Millennial-scale sea surface temperature
changes in the eastern Mediterranean (Nile River Delta region) over the last
27 000 years, Paleoceanography, 25, PA1208, https://doi.org/10.1029/2009PA001740, 2010. a
Català, A., Cacho, I., Frigola, J., Pena, L. D., and Lirer, F.: Holocene
hydrography evolution in the Alboran Sea: a multi-record and multiproxy
comparison, Clim. Past Discuss., https://doi.org/10.5194/cp-2018-163, in
review, 2018. a
Cisneros, M., Cacho, I., Frigola, J., Canals, M., Masqué, P., Martrat,
B., Casado, M., Grimalt, J. O., Pena, L. D., Margaritelli, G., and Lirer, F.:
Sea surface temperature variability in the central-western Mediterranean Sea
during the last 2700 years: a multi-proxy and multi-record approach, Clim.
Past, 12, 849–869, https://doi.org/10.5194/cp-12-849-2016, 2016. a, b
Constantin, S., Bojar, A.-V., Lauritzen, S.-E., and Lundberg, J.: Holocene
and Late Pleistocene climate in the sub-Mediterranean continental
environment: A speleothem record from Poleva Cave (Southern Carpathians,
Romania), Palaeogeogr. Palaeocl., 243, 322–338, 2007.
Conte, M., Giuffrida, S., and Tedesco, S.: The Mediterranean Oscillation:
Impact on Precipitation and Hydrology in Italy, Conference on Climate and
Water Academy of Finland, 121–137, 1989. a
Craig, H. and Gordon, L. I.: Deuterium and oxygen 18 variations in the ocean
and marine atmosphere, in: Proc. Stable Isotopes in Oceanographic Studies and
Paleotemperatures, edited by: Tongiogi, E., V. Lischi & F. Pisa, 9–130,
1965. a
Cullen, H. M., deMenocal, P., Hemming, S., Hemming, G., Brown, F. H.,
Guilderson, T., and Sirocko, F.: Climate change and the collapse of the
Akkadian empire: Evidence from the deep sea, Geology, 28, 379–382, 2000. a
Dansgaard, W., Johnsen S. J., Clausen, H. B., Dahl-Jensen, D., Gunderstrup,
N. S., Hammer, C. U., Hvidberg, C. S., Steffensen, J. P.,
Sveinbjörnsdottir, A. E., Jouzel, J., and Bond G.: Evidence for general
instability of past climate from a 250-kyr ice-core record, Nature, 364,
218–222, 1993. a
Dean, J. R., Jones, M. D., Leng, M. J., Noble, S. R., Metcalfe, S. E.,
Sloane, H. J., Sahy, D., Warren, J., Eastwood, W. J., and Roberts, N.:
Eastern Mediterranean hydroclimate over the late glacial and Holocene,
reconstructed from the sediments of Nar lake, central Turkey, using
stable isotopes and carbonate mineralogy, Quaternary Sci. Rev., 124,
162–174, 2015.
Denton, G. H. and Karlén, W.: Holocene climatic variations – Their
pattern and possible cause, Quaternary Res., 3, 155–205, 1973. a
Dermody, B. J., de Boer, H. J., Bierkens, M. F. P., Weber, S. L., Wassen, M.
J., and Dekker, S. C.: A seesaw in Mediterranean precipitation during the
Roman Period linked to millennial-scale changes in the North Atlantic, Clim.
Past, 8, 637–651, https://doi.org/10.5194/cp-8-637-2012, 2012. a, b, c
Di Rita, F., Lirer, F., Bonomo, S., Cascella, A., Ferraro, L., Florindo, F.,
Insinga, D. D., Lurcock, P. C., Margaritelli, G., Petrosino, P., Rettori, R.,
Vallefuoco, M., and Magri, D.: Late Holocene forest dynamics in the Gulf of
Gaeta (central Mediterranean) in relation to NAO variability and human
impact, Quaternary Sci. Rev., 179, 137–152, 2018a. a, b
Di Rita, F., Fletcher, W. J., Aranbarri, J., Margaritelli, G., Lirer, F., and
Magri, D.: Holocene forest dynamics in central and western Mediterranean:
periodicity, spatio-temporal patterns and climate influence, Sci. Rep., 8,
8929, https://doi.org/10.1038/s41598-018-27056-2, 2018b. a, b, c
Dominguez-Villar, D., Wang, X., Krklec, K., Cheng, H., and Edwards, R. L.:
The control of the tropical North Atlantic on Holocene millennial climate
oscillations, Geology, 45, 303–306, 2017. a
Dormoy, I., Peyron, O., Combourieu Nebout, N., Goring, S., Kotthoff, U.,
Magny, M., and Pross, J.: Terrestrial climate variability and seasonality
changes in the Mediterranean region between 15 000 and 4000 years BP deduced
from marine pollen records, Clim. Past, 5, 615–632,
https://doi.org/10.5194/cp-5-615-2009, 2009.
D'Ortenzio, F. and Ribera d'Alcalà, M.: On the trophic regimes of the
Mediterranean Sea: a satellite analysis, Biogeosciences, 6, 139–148,
https://doi.org/10.5194/bg-6-139-2009, 2009. a, b
Drǎguşin, V., Staubwasser, M., Hoffmann, D. L., Ersek, V., Onac, B.
P., and Veres, D.: Constraining Holocene hydrological changes in the
Carpathian–Balkan region using speleothem δ18O and pollen-based
temperature reconstructions, Clim. Past, 10, 1363–1380,
https://doi.org/10.5194/cp-10-1363-2014, 2014. a
Drescher-Schneider, R., De Beaulieu, J. L., Magny, M., Walter-Simonnet, A.
V., Bossuet, G., Millet, L., and Drescher, A.: Vegetation history, climate
and human impact over the last 15,000 years at Lago dell'Accesa (Tuscany,
Central Italy), Veget. Hist. Archaeob., 16, 279–299, 2007. a
Duplessy, J. C., Bard, E., Arnold, M., Shackleton, N. J., Duprat, J., and
Labeyrie, L. D.: How fast did the ocean-atmosphere system run during the last
deglaciation?, Earth Planet. Sc. Lett., 103, 41–54, 1991.
Eastwood, W. J., Leng, M. J., Roberts, N., and Davis, B.: Holocene climate
change in the eastern Mediterranean region: a comparison of stable isotope
and pollen data from Lake Gölhisar, Southwest Turkey, J. Quat. Sci., 22,
327–341, 2007.
Emeis, K.-C., Struck, U., Schulz, H.-M., Bernasconi, S., Sakamoto, T., and
Martinez-Ruiz, F.: Temperature and salinity of Mediterranean Sea surface
waters over the last 16 000 years: constraints on the physical environment of
S1 sapropel formation based on stable oxygen isotopes and alkenone
unsaturation ratios, Palaeogeogr. Palaecol., 158, 259–280, 2000.
Emile-Geay, J., McKay, N. P., Kaufman, D. S., Von Gunten, L., Wang, J.,
Anchukaitis, K. J., and Henley, B. J.: A global multiproxy database for
temperature reconstructions of the Common Era, Sci. Data, 4, 170088,
https://doi.org/10.1038/sdata.2017.88, 2017. a
England, A., Eastwood, C. N., Roberts, C. N., Tuner, R., and Haldon, J. F.:
Historical landscape change in Cappadocia (central Turkey): a
palaeoecological investigation of annually laminated sediments from Nar lake,
Holocene, 18, 1229–1245, 2008 a
Eshel, G.: Mediterranean climates, Israel J. Earth Sci., 51, 157–168, 2002. a
Fairchild, I. J. and Treble, P.: Trace elements in speleothems as recorders
of environmental change, Quaternary Sci. Rev., 28, 449–468, 2009.
Field, R. D.: Observed and modeled controls on precipitation
δ18O over Europe: From local temperature to the Northern
Annular Mode, J. Geophys. Res, 115, D12101, https://doi.org/10.1029/2009JD013370, 2010. a
Finné, M., Holmgren, K., Sundqvist, H. S., Weiberg, E., and Lindblom, M.:
Climate in the eastern Mediterranean, and adjacent regions, during the past
6000 years – a review, J. Archaeol. Sci., 38, 3153–3173, 2011. a
Fleitmann, D., Burns, S. J., Mudelsee, M., Neff, U., Kramers, J., Mangini,
A., and Matter A.: Holocene Forcing of the Indian Monsoon Recorded in a
Stalagmite from Southern Oman, Science, 300, 1737–1739, 2003. a
Fohlmeister, J., Schröder-Ritzrau, A., Scholz, D., Spötl, C.,
Riechelmann, D. F. C., Mudelsee, M., Wackerbarth, A., Gerdes, A.,
Riechelmann, S., Immenhauser, A., Richter, D. K., and Mangini, A.: Bunker
Cave stalagmites: an archive for central European Holocene climate
variability, Clim. Past, 8, 1751–1764,
https://doi.org/10.5194/cp-8-1751-2012, 2012.
Francke, A., Wagner, B., Leng, M. J., and Rethemeyer, J.: A Late Glacial to
Holocene record of environmental change from Lake Dojran (Macedonia, Greece),
Clim. Past, 9, 481–498, https://doi.org/10.5194/cp-9-481-2013, 2013.
Frigola, J., Moreno, A., Cacho, I., Sierro, F. J., Flores, J. A., Grimalt, J.
O., Hodell, D. A., and Curtis, J. H.: Holocene climate variability in the
western Mediterranean region from a deepwater sediment record,
Paleoceanography, 22, PA2209, https://doi.org/10.1029/2006PA001307, 2007.
Frisia, S., Borsato, A., Spötl, C., Villa, I. M., and Cucchi, F.: Climate
variability in the SE Alps of Italy over the past 17000 years reconstructed
from a stalagmite record, Boreas, 34, 445–455, 2005. a
Frisia, S., Borsato, A., Mangini, A., Spötl, C., and Madonna, G.:
Holocene climate varibility from a discontinuous stalagmite record and the
Mesolithic to Neolithic transition, Quaternary Res., 66, 388–400, 2006. a
Frogley, M. R., Griffiths, H. I., and Heaton, T. H. E.: Historical
biogeography and Late Quaternary environmental change of Lake Pamvotis,
Ioannina (north-western Greece): evidence from ostracods, J. Biogeogr., 28,
745–756, 2001.
Gaetani, M., Pohl, B., Douville, H., and Fontaine, B.: West African Monsoon
influence on the summer Euro-Atlantic circulation, Geophys. Res. Lett., 38,
L09705, https://doi.org/10.1029/2011GL047150, 2011. a
Gambin, B., Andrieu-Ponel, V., Médail, F., Marriner, N., Peyron, O.,
Montade, V., Gambin, T., Morhange, C., Belkacem, D., and Djamali, M.: 7300
years of vegetation history and climate for NW Malta: a Holocene perspective,
Clim. Past, 12, 273–297, https://doi.org/10.5194/cp-12-273-2016, 2016.
Genty, D., Blamart, D., Ghaleb, B., Plagnes, V., Caussed, Ch., Bakalowicz,
M., Zouarif, K., Chkir, N., Hellstrom, J. C., K. Wainer, K., and Bourgesh,
F.: 2006 Timing and dynamics of the last deglaciation from European and North
African δ13C stalagmite profiles comparison with Chinese and South
Hemisphere stalagmites, Quaternary Sci. Rev., 25, 2118–2142, 2006. a, b
Giunta, S., Emeis, K. C., and Negri, A.: Sea-surface temperature
reconstruction of the last 16 000 years in the Eastern Mediterranean Sea,
Riv. It. Paleont. Stratigr., 107, 463–476, 2001. a
Guiot, J.: Methodology of the last climatic cycle reconstruction in France
from pollen data, Palaeogeogr. Palaeocl., 80, 49–69, 1990. a
Hellstrom, J. C.: U-Th dating of speleothems with high initial 230Th using
stratigraphical constraint, Quat. Geochronol., 1, 289–295, 2006. a
Holmes, J., Arrowsmith, C., Austin, W., Boyle, J., Fisher, E., Holme, R.,
Marshall, J., Oldfield, F., and van der Post, K.: Climate and atmospheric
circulation changes over the past 1000 years reconstructed from oxygen
isotopes in lake-sediment carbonate from Ireland, The Holocene, 20,
1105–1111, 2010. a
Isola, I., Zanchetta, G., Drysdale, R. N., Regattieri, E., Bini, M., Bajo,
P., Hellstrom, J. C., Baneschi, I., Lionello, P., Woodhead, J., and Greig,
A.: The 4.2 ka event in the central Mediterranean: new data from a Corchia
speleothem (Apuan Alps, central Italy), Clim. Past, 15, 135–151,
https://doi.org/10.5194/cp-15-135-2019, 2019. a
Jalali, B., Sicre, M.-A., Bassetti, M.-A., and Kallel, N.: Holocene climate
variability in the North-Western Mediterranean Sea (Gulf of Lions), Clim.
Past, 12, 91–101, https://doi.org/10.5194/cp-12-91-2016, 2016. a, b, c
Jalali, B., Sicre, M. A., Kallel, N., Azuara, J., Combourieu-Nebout, N.,
Bassetti, M. A., and Klein, V.: High-resolution Holocene climate and
hydrological variability from two major Mediterranean deltas (Nile and
Rhone), Holocene, 27, 1158–1168, 2017. a
Jalali, B., Sicre, M. A., Klein, V., Schmidt, S., Maselli, V., Lirer, F., and
Petrosino, P.: Deltaic and coastal sediments as recorders of Mediterranean
regional climate and human impact over the past three millennia,
Paleoceanogr. Paleocl., 33, 579–593, https://doi.org/10.1029/2017PA003298, 2018. a
Jones, M. D., Leng, M. J., Eastwood, W. J., Keen, D. H., and Turney, C. S.
M.: Interpreting stable isotope records from freshwater snail shell
carbonate: a Holocene case study from Lake Gölhisar, Turkey, Holocene,
12, 629–634, 2002.
Kaniewski, D., Van Campo, E., Morhange, C., Guiot, J., Zviely, D., Shaked,
I., Otto, T., and Artzy, M.: Early urban impact on Mediterranean coastal
environments, Sci. Rep., 3, 3540, https://doi.org/10.1038/srep03540, 2013. a, b
Kaniewski, D., Marriner, N., Morhange, C., Faivre, S., Otto, T., and Van
Campo, E.: Solar pacing of storm surges, coastal flooding and agricultural
losses in the Central Mediterranean, Sci. Rep., 6, 25197,
https://doi.org/10.1038/srep25197, 2016. a
Lacey, J. H., Leng, M. J., Francke, A., Sloane, H. J., Milodowski, A., Vogel,
H., Baumgarten, H., Zanchetta, G., and Wagner, B.: Northern Mediterranean
climate since the Middle Pleistocene: a 637 ka stable isotope record from
Lake Ohrid (Albania/Macedonia), Biogeosciences, 13, 1801–1820,
https://doi.org/10.5194/bg-13-1801-2016, 2016. a
Lachniet, M. S.: Climatic and environmental controls on speleothem
oxygen-isotope values, Quaternary Sci. Rev., 28, 412–432, 2009. a
Leng, M. J. and Marshall, J. D.: Palaeoclimate interpretation of
stable isotope data from lake sediment archives, Quaternary Sci. Rev., 23,
811–831, 2004. a
Leng, M. J., Baneschi, I., Zanchetta, G., Jex, C. N., Wagner, B., and Vogel,
H.: Late Quaternary palaeoenvironmental reconstruction from Lakes Ohrid and
Prespa (Macedonia/Albania border) using stable isotopes, Biogeosciences, 7,
3109–3122, https://doi.org/10.5194/bg-7-3109-2010, 2010a. a, b, c, d, e, f
Leng, M. J., Wagner, B., Boehm, A., Panagiotopoulos, K., Vane, C. H.,
Snelling, A., Haidon, C., Woodley, E., Vogel, H., Zanchetta, G., and
Baneschi, I.: Understanding past climatic and hydrological variability in the
Mediterranean from Lake Prespa sediment isotope and geochemical record over
the Last Glacial cycle, Quaternary Sci. Rev., 66, 123–136, 2013. a, b, c
Le Roy, M., Deline, P., Carcaillet, J., Schimmelpfenning, I., Ermini, M., and
ASTER Team: 10Be exposure dating of the timing of Neoglacial glacier
advances in the Ecrins-Pelvoux massif, southern French Alps, Quaternary Sci.
Rev., 178, 118–138, 2017. a
Lillios, K. T., Blanco González, A., Drake, B. L., and
López-Sáez, J.A.: Mid-Late Holocene climate, demography, and cultural
dynamics in Iberia: a multi-proxy approach, Quaternary Sci. Rev., 135,
138–153, 2016. a
Longman, J., Veres, D., Ersek, V., Salzmann, U., Hubay, K., Bormann, M.,
Wennrich, V., and Schäbitz, F.: Periodic input of dust over the Eastern
Carpathians during the Holocene linked with Saharan desertification and human
impact, Clim. Past, 13, 897–917, https://doi.org/10.5194/cp-13-897-2017,
2017. a, b
López-Moreno, J. I., Vicente-Serrano, S. M., Morán- Tejeda, E.,
Lorenzo-Lacruz, J., Kenawy, A., and Beniston M.: Effects of the North
Atlantic Oscillation (NAO) on combined temperature and precipitation winter
modes in the Mediterranean mountains: Observed relationships and projections
for the 21st century, Global Planet. Change, 77, 62–76, 2011. a
Lowe, J. J., Blockley, S., Trincardi, F., Asioli, A., Cattaneo, A., Matthews,
I. P., Pollard, M., and Wulf, S.: Age modelling of late Quaternary marine
sequences in the Adriatic: towards improved precision and accuracy using
volcanic event stratigraphy, Cont. Shelf Res., 27, 560–582, 2007. a
Magny, M., de Beaulieu, J. L., Drescher-Schneider, R., Vannière, B.,
Walter-Simonnet, A. V., Miras, Y., Millet, L., Bossuet, G., Peyron, O.,
Brugiapaglia, E., and Leroux, A.: Holocene climate changes in the central
Mediterranean as recorded by lake-level fluctuations at Lake Accesa (Tuscany,
Italy), Quaternary Sci. Rev., 26, 1736–1758, 2007. a, b
Magny, M., Vanniére, B., Calo, C., Millet, L., Leroux, A., Peyron, O.,
Zanchetta, G., La Mantia, T., and Tinner, W.: Holocene hydrological changes
in south-western Mediterranean as recorded by lake-level fluctuations at Lago
Preola, a coastal lake in southern Sicily, Italy, Quaternary Sci. Rev., 30,
2459–2475, 2011. a
Marcott, S. A., Shakun, J. D., Clark, P. U., and Mix, A.: A Reconstruction of
Regional and Global Temperature for the Past 11,300 Years, Science, 339,
1198–2001, 2013. a
Margaritelli, G., Vallefuoco, M., Di Rita, F., Capotondi, L., Bellucci, L.
G., Insinga, D. D., Petrosino, P., Bonomo, S., Cacho, I., Cascella, A.,
Ferraro, L., Florindo, F., Lubritto, C., Lubritto C., Lurcock, P. C., Magri,
D., Pelosi, N., Rettori, R., and Lirer, F.: Marine response to climate
changes during the last five millennia in the central Mediterranean Sea,
Global Planet. Change 142, 53–72, 2016. a, b
Marks, L., Salem, A., Welc, F., Nitychoruk, J., Chen, Z., Blaauw, M., Zalat,
A., Majecka, A., Szymanek, M., Chodyka, M., Tołoczko-Pasek, A., Sun, Q.,
Zhao, X., and Jiang, J.: Holocene lake sediments from the Faiyum Oasis in
Egypt: a record of environmental and climate change, Boreas, 47, 62–79,
2018. a, b
Marriner, N., Flaux, C., Kaniewski, D., Morhange, C., Leduc, G., Moron, V.,
Chen, Z., Empereur, J.-Y., and Stanley, J.-D.: ITCZ and ENSO-like pacing of
Nile delta hydro-geomorphology during the Holocene, Quaternary Sci. Rev., 45,
73–84, 2012. a
Marriner, N., Kaniewski, D., Morhange, C., Flaux, F., Giaime, M., Vacchi, M.,
and Goff, J.: Tsunamis in the geological record: making waves with a
cautionary tale from the Mediterranean, Sci. Adv., 3, e1700485,
https://doi.org/10.1126/sciadv.1700485 , 2017. a
Marsicek, J., Shuman, B. N., Bartlein, P. J., Shafer, S., and Brewer, S.:
Reconciling divergent trends and millennialvariations in Holocene
temperatures, Nature, 554, 92–96, 2018.
Martrat, B., Jimenez-Amat, P., Zahn, R., and Grimalt, J.-O.: Similarities and
dissimilarities between the last two deglaciations and interglaciations in
the North Atlantic region, Quaternary Sci. Rev., 99, 122–134, 2014.
Mauri, A., Davis, B. A. S., Collins, P. M., and Kaplan, J. O.: The influence
of atmospheric circulation on the mid-Holocene climate of Europe: a
data–model comparison, Clim. Past, 10, 1925–1938,
https://doi.org/10.5194/cp-10-1925-2014, 2014. a
Mauri, A., Davis, B., Collins, P. M., and Kaplan, J.: The climate of Europe
during the Holocene: A gridded pollen-based reconstruction and its
multi-proxy evaluation, Quaternary Sci. Rev., 112, 109–127, 2015. a
Mayewski, P. A., Rohling, E. E., Stager, J. C., Karlen, W., Maasch, K. A.,
Meeker, L. D., Meyerson, E. A., Gasse, F., van Kreveld, S., Holmgren, K.,
Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneider, R. R., and
Steig, E. J.: Holocene climate variability, Quaternary Res., 62, 243–255, 2004. a
McDermott, F., Frisia, S., Huang, Y., Longinelli, A., Spiro, B., Heaton, T.
H. E., Hawkesworth, C. J., Borsato, A, Keppens, E., Fairchild, I. J., van der
Borg, K., Verheyden, S., and Selmo, E. M.: Holocene climate variability in
Europe: evidence from δ18O, textural and extension-rate
variations in three speleothems, Quaternary Sci. Rev., 18, 1021–1038, 1999. a
McDermott, F., Atkinson, T. C., Fairchild, I. J., Baldini, L. M., and Mattey,
D. P.: A first evaluation of the spatial gradients in δ18O
recorded by European Holocene speleothems, Global Planet. Change, 79,
275–287, 2011. a
Mercuri, A.M., Accorsi, C.A., and Mazzanti, M.B.: The long history of
Cannabis and its cultivation by the Romans in central Italy, shown by pollen
records from Lago Albano and Lago di Nemi, Veget. Hist. Archaeob., 11,
263-276, 2002. a
Mercuri, A. M., Mazzanti, M. B., Torri, P., Vigliotti, L., Bosi, G.,
Florenzano, A., and N'siala, I.M.: A marine/terrestrial integration for
mid-late Holocene vegetation history and the development of the cultural
landscape in the Po valley as a result of human impact and climate change.
Veg. Hist. Archaeob., 21(4-5), 353-372, 2012. a
Moreno, A., Pérez, A., Frigola, J., Nieto-Moreno, V., Rodrigo-Gámiz,
M., Martrat, B., and Belmonte, Á: The Medieval Climate Anomaly in the
Iberian Peninsula reconstructed from marine and lake records, Quaternary Sci.
Rev., 43, 16–32, 2012. a
Moreno, A., Svensson, A., Brooks, S., Engels, S., Fletcher, W., Genty, D.,
Heiri, I., Labuhn, O., Persoiu, A., Sadori, L., Valero-Garcés, B., Wulf,
S., Zanchetta, G., and data contributors: A compilation of Western European
terrestrial records 60–8 ka BP: towards an understanding of latitudinal
climatic gradients, Quaternary Sci. Rev., 106, 167–185, 2014. a
Moreno, A., Pérez-Mejías, C., Bartolomé, C., Cacho, I., Stoll,
H., Delgado-Huertas, A., Hellstrom, J., Edwards, R. L., and Cheng, H.: New
speleothem data from Molinos and Ejulve caves reveal Holocene hydrological
variability in northeast Iberia, Quaternary Res., 88, 223–233, 2017.
Mühlinghaus, C., Scholz, D., and Mangini, A.: Modelling fractionation of
stable isotopes in stalagmites, Geochim. Cosmochim. Ac., 73, 7275–7289,
2009. a
Muñoz, A., Bartolomé, M., Muñoz, A., Sancho, C., Moreno, A.,
Hellstrom, J. C., Osàcar, M. C., and Chaco, I.: Solar influence and
hydrological variability during the Holocene from a speleothem annual record
(Molinos Cave, NE Spain), Terra Nova, 27, 300–311, 2015.
Nagashima, K., Tada, R., Tani, A., Sun, Y., Isozaki, Y., Toyoda, S., and
Hasegawa, H.: Millennial-scale oscillations of the westerly jet path during
the last glacial period, J. Asian Earth Sci., 40, 1214–1220, 2011. a
Nieto-Moreno, V., Martínez-Ruiz, F., Willmott, V., García-Orellana,
J., Masqué, P., and Damsté, J. S.: Climate conditions in the
westernmost Mediterranean over the last two millennia: An integrated
biomarker approach, Org. Geochem., 55, 1–10, 2013. a
Perşoiu, A., Onac, B. P., Wynn, J. G., Blaauw, M., Ionita, M., and
Hansson, M.: Holocene winter climate variability in Central and Eastern
Europe, Sci. Rep., 7, 1196, https://doi.org/10.1038/s41598-017-01397-w, 2017. a, b
Persoiu, A., Ionita, M., and Weiss, H.: Blocking induced by the strengthened
Siberian High led to drying in west Asia during the 4.2 ka BP event – a
hypothesis, Clim. Past Discuss., https://doi.org/10.5194/cp-2018-161, in
review, 2018. a, b
Peyron, O., Goring, S., Dormoy, I., Kotthoff, U., Pross, J., de Bealieu, J.
L., Drescher-Schneider, R., and Magny, M.: Holocene seasonality changes in
the central Mediterranean region reconstructed from the pollen sequences of
Lake Accesa (Italy) and Tenaghi Philippon (Greece), Holocene, 21, 131–146,
2011. a
Peyron, O., Magny, M., Goring, S., Joannin, S., de Beaulieu, J.-L.,
Brugiapaglia, E., Sadori, L., Garfi, G., Kouli, K., Ioakim, C., and
Combourieu-Nebout, N.: Contrasting patterns of climatic changes during the
Holocene across the Italian Peninsula reconstructed from pollen data, Clim.
Past, 9, 1233–1252, https://doi.org/10.5194/cp-9-1233-2013, 2013.
Peyron, O., Combourieu-Nebout, N., Brayshaw, D., Goring, S., Andrieu-Ponel,
V., Desprat, S., Fletcher, W., Gambin, B., Ioakim, C., Joannin, S., Kotthoff,
U., Kouli, K., Montade, V., Pross, J., Sadori, L., and Magny, M.:
Precipitation changes in the Mediterranean basin during the Holocene from
terrestrial and marine pollen records: a model–data comparison, Clim. Past,
13, 249–265, https://doi.org/10.5194/cp-13-249-2017, 2017. a, b, c
Piccini, L., Zanchetta, G., Drysdale, R. N., Hellstrom, J., Isola, I.,
Fallick, A. E., Leone, G., Doveri, M., Mussi, M., Mantelli, F., Molli, G.,
Lotti, L., Roncioni, A., Regattieri, E., Meccheri, M., and Vaselli, L.: The
environmental features of the Monte Corchia cave system (Apuan Alps, central
Italy) and their effects on speleothems growths, Int. J. Speleol., 37,
153–173, 2008.
Railsback, L. B., Liang, F., Brook, G. A., Riavo, N., Voarintsoa, G.,
Sletten, H. R., Marais, E., Hardt, B., Cheng, H., and Edwards, R. L.: The
timing, two-pulsed nature, and variable climatic expression of the 4.2 ka
event: A review and new high-resolution stalagmite data from Namibia,
Quaternary Sci. Rev., 186, 78–90, 2018. a, b, c
Richards, D. A. and Dorale, J. A.: Uranium-series chronology and
environmental applications of speleothems, Rev. Mineral. Geochem., 52,
407–460, 2003. a
Roberts, N., Reed, J., Leng, M. J., Kuzucuoǧlu, C., Fontugne, M.,
Bertaux, J., Woldring, H., Bottema, S., Black, S., Hunt, E., and
Karabiyikoǧlu, M.: The tempo of Holocene climatic change in the eastern
Mediterranean region: new high-resolution crater-lake sediment data from
central Turkey, Holocene, 11, 721–736, 2001.
Roberts, N., Stevenson, A. C., Davis, B., Cheddadi, R., Brewer, S., Rosen, A.
M., Battarbee, R. W., Gasse, F., and Stickey, C. E.: Holocene climate,
environment and cultural change in the circum-Mediterranean region, in: Past
climate variability through Europe and Africa, Battarbee, edited by:
Battarbee, R. W., Gasse, F., and Stickley, C. E., Kluwer, Dordrecht,
343–362, 2004. a, b
Roberts, N., Jones, M. D., Benkaddur, A., Eastwood, W. J., Filippi, M. L.,
Frogley, M. R., Lamb, H. F., Leng, M. J., Reed, J. M., Stein, M., Stevens,
L., Valero- Garcè, B., and Zanchetta G.: Stable isotope records of Late
Quaternary climate and hydrology from Mediterranean lakes: the ISOMED
synthesis, Quaternary Sci. Rev., 27, 2426–2441, 2008. a, b, c, d, e, f
Roberts, N., Moreno, A., Valero-Garcés, B. L., Corella, J. P., Jones, M.,
Allcock, S., Woodbridge, J., Morellón, M., Luterbacher, J., Xoplaki, E.,
and Türkeş, M.: Palaeolimnological evidence for an east–west climate
see-saw in the Mediterranean since AD 900, Global Planet. Change, 84–85,
23–34, 2012. a
Roland, T. P., Caseldine, C. J., Charman, D. J., Turney, C. S. M., and
Amesbury, M. J.: Was there a “4.2 ka event” in Great Britain and Ireland?
Evidence from the peatland record, Quaternary Sci. Rev., 83, 11–27, 2014. a
Ruan, J., Kherbouche, F., Genty, D., Blamart, D., Cheng, H., Dewilde, F.,
Hachi, S., Edwards, R. L., Régnier, E., and Michelot, J.-L.: Evidence of
a prolonged drought ca. 4200 yr BP correlated with prehistoric settlement
abandonment from the Gueldaman GLD1 Cave, Northern Algeria, Clim. Past, 12,
1–14, https://doi.org/10.5194/cp-12-1-2016, 2016.
Sadori, L., Ortu, E., Peyron, O., Zanchetta, G., Vannière, B., Desmet,
M., and Magny, M.: The last 7 millennia of vegetation and climate changes at
Lago di Pergusa (central Sicily, Italy), Clim. Past, 9, 1969–1984,
https://doi.org/10.5194/cp-9-1969-2013, 2013.
Sadori, L., Giardini, M., Gliozzi, E., Mazzini, I., Sulpizio, R., van Welden,
A., and Zanchetta, G.: Vegetation, climate and environmental history of the
last 4500 years at lake Shkodra (Albania/Montenegro), Holocene, 25, 435–444,
2015.
Sadori, L.: The Lateglacial and Holocene vegetation and climate history of
Lago di Mezzano (central Italy), Quaternary Sci. Rev., 202, 30–44,
https://doi.org/10.1016/j.quascirev.2018.09.004, 2018. a
Scholz, D., Frisia, S., Borsato, A., Spötl, C., Fohlmeister, J.,
Mudelsee, M., Miorandi, R., and Mangini, A.: Holocene climate variability in
north-eastern Italy: potential influence of the NAO and solar activity
recorded by speleothem data, Clim. Past, 8, 1367–1383,
https://doi.org/10.5194/cp-8-1367-2012, 2012. a
Seppä, H., Bjune, A. E., Telford, R. J., Birks, H. J. B., and Veski, S.:
Last nine-thousand years of temperature variability in Northern Europe, Clim.
Past, 5, 523–535, https://doi.org/10.5194/cp-5-523-2009, 2009. a
Sharifi, A., Pourmand, A., Canuel, E. A., Ferer-Tyler, E., Peterson, L. C.,
Aichner, B., Feakins, S. J., Daryaee, T., Djamali, M., Beni, A. N., Lahijani,
H. A. K., and Swart, P. K.: Abrupt climate variability since the last
deglaciation based on a high resolution, multi-proxy peat record from NW
Iran: the hand that rocked the Cradle of Civilization?, Quaternary Sci. Rev.,
123, 215–230, 2015. a
Siani, G., Paterne, M., Michel, E., Sulpizio, R., Sbrana, A., Arnold, M., and
Haddas, G.: Mediterranean Sea surface radiocarbon reservoir age changes since
the Last Glacial Maximum, Science, 294, 1917–1920, 2001. a
Siani, G., Magny, M., Paterne, M., Debret, M., and Fontugne, M.:
Paleohydrology reconstruction and Holocene climate variability in the South
Adriatic Sea, Clim. Past, 9, 499–515, https://doi.org/10.5194/cp-9-499-2013,
2013.
Sicre, M. A., Jalali, B., Martrat, B., Schmidt, S., Bassetti, M. A., and
Kallel, N.: Sea surface temperature variability in the North Western
Mediterranean Sea (Gulf of Lion) during the Common Era, Earth Planet. Sc.
Lett., 456, 124–133, 2016. a
Smith, A. C., Wynn, P. M., Barker, P. A., Leng, M. J., Stephen, R., Noble, S.
R., and Tych, W.: North Atlantic forcing of moisture delivery to Europe
throughout the Holocene, Sci. Rep., 6, 24745, https://doi.org/10.1038/srep24745, 2016. a, b
Stevens, L. R., Wright Jr., H. E., and Ito, E.: Proposed changes in
seasonality of climate during the late-glacial and Holocene at Lake Zeribar,
Iran, Holocene, 11, 747–756, 2001.
Stevens, L. R., Ito, E., Schwalb, A., and Wright Jr., H. E.: Timing of
atmospheric precipitation in the Zagros Mountains inferred from a multi-proxy
record from Lake Mirabad, Iran, Quaternary Res., 66, 494–500, 2006.
Stiller, M. and Hutchinson, G. E.: The Waters of Merom: a study of Lake Huleh
VI, Stable isotope composition of carbonates of a 54 m core: paleoclimatic
and paleotrophic implications, Arc. Hydrobiol., 89, 275–302, 1980.
Stoll, H. M., Moreno, A., Mendez-Vicente, A., Gonzalez-Lemos, S.,
Jimenez-Sanchez, M., Dominguez-Cuesta, M. J., Edwards, R. L., Cheng, H., and
Wang, X.: Paleoclimate and growth rates of speleothems in the northwestern
Iberian Peninsula over the last two glacial cycles, Quat, Res., 80, 284–290,
2013. a
Tǎmaş, T., Onac, B. P., and Bojar, A. V.: Lateglacial-Middle Holocene
stable isotope records in two coeval stalagmites from the Bihor Mountains, NW
Romania, Geol. Q., 49, 185–194, 2005.
Telford, R. J. and Birks, H. J. B.: The secret assumption of transfer
functions: problems with spatial autocorrelation in evaluating model
performance, Quaternary Sci. Rev., 24, 2173–2179, 2005. a
Ternois, Y., Sicre, M. A., Boireau, A., and Conte, M. H.: Evaluation of
long-chain alkenones as paleo-temperature indicators in the Mediterranean
Sea, Deep-Sea Res. Pt. I, 44, 271–286, 1997. a
Totti, C., Civitarese, G., Acri, F., Barletta, D., Candelari, G., Paschini,
E., and Solazzi, A.: Seasonal variability of phytoplankton populations in the
middle Adriatic sub-basin, J. Plankton Res., 22, 1735–1756, 2000. a
van der Schriek, T. and Giannakopoulos, C.: Determining the causes for the
dramatic recent fall of Lake Prespa (southwest Balkans), Hydrol. Sci. J., 62,
1131–1148, 2017. a
Wagner, B., Wilke, T., Francke, A., Albrecht, C., Baumgarten, H., Bertini,
A., Combourieu-Nebout, N., Cvetkoska, A., D'Addabbo, M., Donders, T. H.,
Föller, K., Giaccio, B., Grazhdani, A., Hauffe, T., Holtvoeth, J.,
Joannin, S., Jovanovska, E., Just, J., Kouli, K., Koutsodendris, A., Krastel,
S., Lacey, J. H., Leicher, N., Leng, M. J., Levkov, Z., Lindhorst, K., Masi,
A., Mercuri, A. M., Nomade, S., Nowaczyk, N., Panagiotopoulos, K., Peyron,
O., Reed, J. M., Regattieri, E., Sadori, L., Sagnotti, L., Stelbrink, B.,
Sulpizio, R., Tofilovska, S., Torri, P., Vogel, H., Wagner, T.,
Wagner-Cremer, F., Wolff, G. A., Wonik, T., Zanchetta, G., and Zhang, X. S.:
The environmental and evolutionary history of Lake Ohrid (FYROM/Albania):
interim results from the SCOPSCO deep drilling project, Biogeosciences, 14,
2033–2054, https://doi.org/10.5194/bg-14-2033-2017, 2017. a
Wanner, H., Solomina, O., Grosjean, M., Ritz, S. P., and Jetel, M.: Structure
and origin of Holocene cold events, Quaternary Sci. Rev. 30, 3109–3123,
2011. a
Wassenburg, J. A., Dietrich, S., Fietzke, J., Fohlmeister, J., Jochum, K. P.,
Scholz, D., Richter, D. K., Sabaoui, A., Spötl, C., Lohmann, G., Meinrat,
O., Andreae, M. O., and Immenhauser, A.: Reorganization of the North Atlantic
Oscillation during early Holocene deglaciation, Nat. Geosci., 9, 602–605,
2016. a, b, c, d
Weiss, H., Courty, M. A., Wetterstrom, W., Guichard, F., Senior, L., Meadow,
R., and Curnow, A.: The genesis and collapse of third millennium North
Mesopotamian civilization, Science, 261, 995–1004, 1993. a
Wick, L., Lemcke, G., and Sturm, M.: Evidence of Late glacial and Holocene
climatic change and human impact in eastern Anatolia: high-resolution pollen,
charcoal, isotopic and geochemical records from the laminated sediments of
Lake Van, Turkey, Holocene 13, 665–675, 2003.
Wright, H. E., Kutzbach, J. E., Webb III, T., Ruddiman, W. F.,
Street-Perrott, F. A., and Bartlein, P. J. (Eds.): Global Climate since the
Last Glacial Maximum, University of Minesota Press, Minneapolis, London,
569 pp., 1993. a
Xoplaki, E., González-Rouco, F., Luterbacher, J., and Wanner, H.: Wet
season Mediterranean precipitation variability: influence of large-scale
dynamics and trends, Clim. Dynam., 23, 63–78, 2004. a
Zanchetta, G., Di Vito, A., Fallick, A. E., and Sulpizio, R.: Stable isotopes
of pedogenic carbonate from Somma-Vesuvius area, Southern Italy, over the
last 18 ka: palaeoclimatic implications, J. Quat. Sci., 15, 813–824, 2000. a
Zanchetta, G., Drysdale, R. N., Hellstrom, J. C., Fallick, A. E., Isola, I.,
Gagan, M. K., and Pareschi, M. T.: Enhanced rainfall in the Western
Mediterranean during deposition of sapropel S1: stalagmite evidence from
Corchia cave (Central Italy), Quaternary Sci. Rev., 26, 279–286, 2007a.
Zanchetta, G., Sulpizio, R., Roberts, N., Cioni, R., Eastwood, W. J., Siani,
G., Caron, B., Paterne, M., and Santacroce, R.: Tephrostratigraphy,
chronology and climatic events of the Mediterranean basin during the
Holocene: An overview, Holocene, 21, 33–52, 2011. a
Zanchetta, G., Bini, M., Cremaschi, M., Magny, M., and Sadori, L.: The
transition from natural to anthropogenic-dominated environmental change in
Italy and the surrounding regions since the Neolithic: an introduction,
Quatern. Int., 303, 1–9, 2013. a
Zanchetta, G., Bar-Matthews, M., Drysdale, R. N., Lionello, P., Ayalon, A.,
Hellstrom, J. C., Isola, I., and Regattieri, E.: Coeval dry events in the
central and eastern Mediterranean basin at 5.2 and 5.6 ka recorded in
Corchia (Italy) and Soreq Cave (Israel) speleothems, Global. Planet. Chane,
122, 130–139, 2014. a, b
Zanchetta, G., Bini, M., Giaccio, B., Manganelli, G., Benocci, A.,
Regattieri, E., Colonese, A. C., Boschi, C., and Biagioni, C.: Middle
Pleistocene (MIS 14) environmental conditions in the central Mediterranean
derived from terrestrial molluscs and carbonate stable isotopes from Sulmona
Basin (Italy), Palaeogeogr. Palaeocl., 485, 236–246, 2017. a
Zanchetta, G., Bini, M., Di Vito, M. A., Sulpizio, R., and Sadori, L.:
Tephrostratigraphy of paleoclimatic archives in central Mediterranean during
the Bronze Age, Quatern. Int., 499, 186–194,
https://doi.org/10.1016/j.quaint.2018.06.012, 2018. a, b, c
Zielhofer, C., Fletcher, W. J., Mischke, S., De Batist, M., Campbell, J. F.
E., Joannin, S., Tjallingii, R., El Hamouti, N., Junginger, A., Stele, A.,
Bussmann, J., Schneider, B., Lauer, T., Spitzer, K., Strupler, M., Brachert,
T., and Mikdad, A.: Atlantic forcing of Western Mediterranean winter rain
minima during the last 12,000 years, Quaternary Sci. Rev., 157, 29–51,
2017a. a
Zielhofer, C., von Suchodoletz, H., Fletcher, W. J., Schneider, B., Dietze,
E., Schlegel, M., Schepanski, K., Weninger, B., Mischke, S., and Mikdad, A.:
Millennial-scale fluctuations in Saharan dust supply across the decline of
the African Humid Period, Quaternary Sci. Rev., 171, 119–135, 2017b. a, b, c
Zielhofer, C., Köhler, A., Mischke, S., Benkaddour, A., Mikdad, A., and
Fletcher, W. J.: Western Mediterranean hydro-climatic consequences of
Holocene iceberg advances (Bond events), Clim. Past Discuss.,
https://doi.org/10.5194/cp-2018-97, in review, 2018. a, b
Ziveri, P., Rutten, A., De Lange, G. J., Thomson, J., and Corselli, C.:
Present-day coccolith fluxes recorded in central eastern Mediterranean
sediment traps and surface sediments. Palaeogeogr. Palaeocl., 158, 175–195,
2000. a
Download
The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.
- Article
(8959 KB) - Full-text XML
Short summary
The Mediterranean region has returned some of the clearest evidence of a climatically dry period occurring approximately 4200 years ago. We reviewed selected proxies to infer regional climate patterns between 4.3 and 3.8 ka. Temperature data suggest a cooling anomaly, even if this is not uniform, whereas winter was drier, along with dry summers. However, some exceptions to this prevail, where wetter condition seems to have persisted, suggesting regional heterogeneity.
The Mediterranean region has returned some of the clearest evidence of a climatically dry period...
Special issue