Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-351-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-351-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Vegetation history and paleoclimate at Lake Dojran (FYROM/Greece) during the Late Glacial and Holocene
Department of Environmental Biology, Sapienza University, Rome, Italy
Alexander Francke
Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany
Wollongong Isotope Geochronology Laboratory, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, Australia
Caterina Pepe
Department of Environmental Biology, Sapienza University, Rome, Italy
Matthias Thienemann
Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany
Bernd Wagner
Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany
Laura Sadori
Department of Environmental Biology, Sapienza University, Rome, Italy
Related authors
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.
Monica Bini, Giovanni Zanchetta, Aurel Perşoiu, Rosine Cartier, Albert Català, Isabel Cacho, Jonathan R. Dean, Federico Di Rita, Russell N. Drysdale, Martin Finnè, Ilaria Isola, Bassem Jalali, Fabrizio Lirer, Donatella Magri, Alessia Masi, Leszek Marks, Anna Maria Mercuri, Odile Peyron, Laura Sadori, Marie-Alexandrine Sicre, Fabian Welc, Christoph Zielhofer, and Elodie Brisset
Clim. Past, 15, 555–577, https://doi.org/10.5194/cp-15-555-2019, https://doi.org/10.5194/cp-15-555-2019, 2019
Short summary
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.
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.
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.
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.
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.
Alice R. Paine, Isabel M. Fendley, Joost Frieling, Tamsin A. Mather, Jack H. Lacey, Bernd Wagner, Stuart A. Robinson, David M. Pyle, Alexander Francke, Theodore R. Them II, and Konstantinos Panagiotopoulos
Biogeosciences, 21, 531–556, https://doi.org/10.5194/bg-21-531-2024, https://doi.org/10.5194/bg-21-531-2024, 2024
Short summary
Short summary
Many important processes within the global mercury (Hg) cycle operate over thousands of years. Here, we explore the timing, magnitude, and expression of Hg signals retained in sediments of lakes Prespa and Ohrid over the past ∼90 000 years. Divergent signals suggest that local differences in sediment composition, lake structure, and water balance influence the local Hg cycle and determine the extent to which sedimentary Hg signals reflect local- or global-scale environmental changes.
Stephanie Scheidt, Matthias Lenz, Ramon Egli, Dominik Brill, Martin Klug, Karl Fabian, Marlene M. Lenz, Raphael Gromig, Janet Rethemeyer, Bernd Wagner, Grigory Federov, and Martin Melles
Geochronology, 4, 87–107, https://doi.org/10.5194/gchron-4-87-2022, https://doi.org/10.5194/gchron-4-87-2022, 2022
Short summary
Short summary
Levinson-Lessing Lake in northern central Siberia provides an exceptional opportunity to study the evolution of the Earth's magnetic field in the Arctic. This is the first study carried out at the lake that focus on the palaeomagnetic record. It presents the relative palaeointensity and palaeosecular variation of the upper 38 m of sediment core Co1401, spanning ~62 kyr. A comparable high-resolution record of this time does not exist in the Eurasian Arctic.
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.
Monica Bini, Giovanni Zanchetta, Aurel Perşoiu, Rosine Cartier, Albert Català, Isabel Cacho, Jonathan R. Dean, Federico Di Rita, Russell N. Drysdale, Martin Finnè, Ilaria Isola, Bassem Jalali, Fabrizio Lirer, Donatella Magri, Alessia Masi, Leszek Marks, Anna Maria Mercuri, Odile Peyron, Laura Sadori, Marie-Alexandrine Sicre, Fabian Welc, Christoph Zielhofer, and Elodie Brisset
Clim. Past, 15, 555–577, https://doi.org/10.5194/cp-15-555-2019, https://doi.org/10.5194/cp-15-555-2019, 2019
Short summary
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.
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.
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.
Aleksandra Cvetkoska, Elena Jovanovska, Alexander Francke, Slavica Tofilovska, Hendrik Vogel, Zlatko Levkov, Timme H. Donders, Bernd Wagner, and Friederike Wagner-Cremer
Biogeosciences, 13, 3147–3162, https://doi.org/10.5194/bg-13-3147-2016, https://doi.org/10.5194/bg-13-3147-2016, 2016
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
Janna Just, Norbert R. Nowaczyk, Leonardo Sagnotti, Alexander Francke, Hendrik Vogel, Jack H. Lacey, and Bernd Wagner
Biogeosciences, 13, 2093–2109, https://doi.org/10.5194/bg-13-2093-2016, https://doi.org/10.5194/bg-13-2093-2016, 2016
Short summary
Short summary
The magnetic record from Lake Ohrid reflects a strong change in geochemical conditions in the lake. Before 320 ka glacial sediments contain iron sulfides, while later glacials are dominated by siderite. Superimposed on this large-scale pattern are climatic induced changes in the magnetic mineralogy. Glacial and stadial sediments are characterized by relative increases of high- vs. low-coercivity minerals which relate to enhanced erosion in the catchment, possibly due to a sparse vegetation.
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.
X. S. Zhang, J. M. Reed, J. H. Lacey, A. Francke, M. J. Leng, Z. Levkov, and B. Wagner
Biogeosciences, 13, 1351–1365, https://doi.org/10.5194/bg-13-1351-2016, https://doi.org/10.5194/bg-13-1351-2016, 2016
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.
Elena Jovanovska, Aleksandra Cvetkoska, Torsten Hauffe, Zlatko Levkov, Bernd Wagner, Roberto Sulpizio, Alexander Francke, Christian Albrecht, and Thomas Wilke
Biogeosciences, 13, 1149–1161, https://doi.org/10.5194/bg-13-1149-2016, https://doi.org/10.5194/bg-13-1149-2016, 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.
H. A. Dugan, P. T. Doran, B. Wagner, F. Kenig, C. H. Fritsen, S. A. Arcone, E. Kuhn, N. E. Ostrom, J. P. Warnock, and A. E. Murray
The Cryosphere, 9, 439–450, https://doi.org/10.5194/tc-9-439-2015, https://doi.org/10.5194/tc-9-439-2015, 2015
Short summary
Short summary
Lake Vida is one of the largest lakes in the McMurdo dry valleys, Antarctica, and has the thickest known ice cover of any lake on Earth. For the first time, Lake Vida was drilled to a depth of 27m. With depth the ice cover changes from freshwater ice to salty ice interspersed with thick sediment layers. It is hypothesized that the repetition of sediment layers in the ice will reveal climatic and hydrologic variability in the region over the last 1000--3000 years.
V. Wennrich, P. S. Minyuk, V. Borkhodoev, A. Francke, B. Ritter, N. R. Nowaczyk, M. A. Sauerbrey, J. Brigham-Grette, and M. Melles
Clim. Past, 10, 1381–1399, https://doi.org/10.5194/cp-10-1381-2014, https://doi.org/10.5194/cp-10-1381-2014, 2014
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
K. Panagiotopoulos, A. Böhm, M. J. Leng, B. Wagner, and F. Schäbitz
Clim. Past, 10, 643–660, https://doi.org/10.5194/cp-10-643-2014, https://doi.org/10.5194/cp-10-643-2014, 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
A. Francke, V. Wennrich, M. Sauerbrey, O. Juschus, M. Melles, and J. Brigham-Grette
Clim. Past, 9, 2459–2470, https://doi.org/10.5194/cp-9-2459-2013, https://doi.org/10.5194/cp-9-2459-2013, 2013
N. R. Nowaczyk, E. M. Haltia, D. Ulbricht, V. Wennrich, M. A. Sauerbrey, P. Rosén, H. Vogel, A. Francke, C. Meyer-Jacob, A. A. Andreev, and A. V. Lozhkin
Clim. Past, 9, 2413–2432, https://doi.org/10.5194/cp-9-2413-2013, https://doi.org/10.5194/cp-9-2413-2013, 2013
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
A. C. Gebhardt, A. Francke, J. Kück, M. Sauerbrey, F. Niessen, V. Wennrich, and M. Melles
Clim. Past, 9, 1933–1947, https://doi.org/10.5194/cp-9-1933-2013, https://doi.org/10.5194/cp-9-1933-2013, 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
A. Francke, B. Wagner, M. J. Leng, and J. Rethemeyer
Clim. Past, 9, 481–498, https://doi.org/10.5194/cp-9-481-2013, https://doi.org/10.5194/cp-9-481-2013, 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
V. Wennrich, A. Francke, A. Dehnert, O. Juschus, T. Leipe, C. Vogt, J. Brigham-Grette, P. S. Minyuk, M. Melles, and El'gygytgyn Science Party
Clim. Past, 9, 135–148, https://doi.org/10.5194/cp-9-135-2013, https://doi.org/10.5194/cp-9-135-2013, 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
Related subject area
Subject: Vegetation Dynamics | Archive: Terrestrial Archives | Timescale: Holocene
Refining data–data and data–model vegetation comparisons using the Earth mover's distance (EMD)
Palynological evidence reveals an arid early Holocene for the northeast Tibetan Plateau
Holocene wildfire regimes in western Siberia: interaction between peatland moisture conditions and the composition of plant functional types
2400 years of climate and human-induced environmental change recorded in sediments of Lake Młynek in northern Poland
Climate impacts on vegetation and fire dynamics since the last deglaciation at Moossee (Switzerland)
The 4.2 ka event in the vegetation record of the central Mediterranean
Vegetation and geochemical responses to Holocene rapid climate change in the Sierra Nevada (southeastern Iberia): the Laguna Hondera record
Response of Pinus sylvestris var. mongolica to water change and drought history reconstruction in the past 260 years, northeast China
Holocene climate aridification trend and human impact interrupted by millennial- and centennial-scale climate fluctuations from a new sedimentary record from Padul (Sierra Nevada, southern Iberian Peninsula)
Dendrochronologically dated pine stumps document phase-wise bog expansion at a northwest German site between ca. 6700 and ca. 3400 BC
Autumn–winter minimum temperature changes in the southern Sikhote-Alin mountain range of northeastern Asia since 1529 AD
Postglacial fire history and interactions with vegetation and climate in southwestern Yunnan Province of China
Precipitation changes in the Mediterranean basin during the Holocene from terrestrial and marine pollen records: a model–data comparison
Environmental changes, climate and anthropogenic impact in south-east Tunisia during the last 8 kyr
Climate variability and human impact in South America during the last 2000 years: synthesis and perspectives from pollen records
Holocene Asian monsoon evolution revealed by a pollen record from an alpine lake on the southeastern margin of the Qinghai–Tibetan Plateau, China
7300 years of vegetation history and climate for NW Malta: a Holocene perspective
Climate-driven expansion of blanket bogs in Britain during the Holocene
Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)
Effects of past climate variability on fire and vegetation in the cerrãdo savanna of the Huanchaca Mesetta, NE Bolivia
Environmental and climatic changes in central Chilean Patagonia since the Late Glacial (Mallín El Embudo, 44° S)
Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum – extending the concept of pollen source area to pollen-based climate reconstructions from large lakes
The last 7 millennia of vegetation and climate changes at Lago di Pergusa (central Sicily, Italy)
Contrasting patterns of climatic changes during the Holocene across the Italian Peninsula reconstructed from pollen data
Climate and vegetation changes during the Lateglacial and early–middle Holocene at Lake Ledro (southern Alps, Italy)
The Medieval Climate Anomaly and the Little Ice Age in the eastern Ecuadorian Andes
Palynological evidence for gradual vegetation and climate changes during the African Humid Period termination at 13°N from a Mega-Lake Chad sedimentary sequence
Climate, people, fire and vegetation: new insights into vegetation dynamics in the Eastern Mediterranean since the 1st century AD
Pollen-based reconstruction of Holocene vegetation and climate in southern Italy: the case of Lago Trifoglietti
Vegetation history of central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater
A seesaw in Mediterranean precipitation during the Roman Period linked to millennial-scale changes in the North Atlantic
Hydroclimate variability in the low-elevation Atacama Desert over the last 2500 yr
Pollen, vegetation change and climate at Lake Barombi Mbo (Cameroon) during the last ca. 33 000 cal yr BP: a numerical approach
Late Holocene plant and climate evolution at Lake Yoa, northern Chad: pollen data and climate simulations
Holocene vegetation and biomass changes on the Tibetan Plateau – a model-pollen data comparison
Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
Putting the rise of the Inca Empire within a climatic and land management context
Manuel Chevalier, Anne Dallmeyer, Nils Weitzel, Chenzhi Li, Jean-Philippe Baudouin, Ulrike Herzschuh, Xianyong Cao, and Andreas Hense
Clim. Past, 19, 1043–1060, https://doi.org/10.5194/cp-19-1043-2023, https://doi.org/10.5194/cp-19-1043-2023, 2023
Short summary
Short summary
Data–data and data–model vegetation comparisons are commonly based on comparing single vegetation estimates. While this approach generates good results on average, reducing pollen assemblages to single single plant functional type (PFT) or biome estimates can oversimplify the vegetation signal. We propose using a multivariate metric, the Earth mover's distance (EMD), to include more details about the vegetation structure when performing such comparisons.
Nannan Wang, Lina Liu, Xiaohuan Hou, Yanrong Zhang, Haicheng Wei, and Xianyong Cao
Clim. Past, 18, 2381–2399, https://doi.org/10.5194/cp-18-2381-2022, https://doi.org/10.5194/cp-18-2381-2022, 2022
Short summary
Short summary
We reconstructed the vegetation and climate change since the last 14.2 ka BP from a fossil pollen record together with multiple proxies (grain size, contents of total organic carbon and total nitrogen) on the northeast Tibetan Plateau. The results reveal that an arid climate occurs in the early Holocene and the vegetation could be disturbed by human activities to some extent after ca. 0.24 ka BP (1710 CE).
Angelica Feurdean, Andrei-Cosmin Diaconu, Mirjam Pfeiffer, Mariusz Gałka, Simon M. Hutchinson, Geanina Butiseaca, Natalia Gorina, Spassimir Tonkov, Aidin Niamir, Ioan Tantau, Hui Zhang, and Sergey Kirpotin
Clim. Past, 18, 1255–1274, https://doi.org/10.5194/cp-18-1255-2022, https://doi.org/10.5194/cp-18-1255-2022, 2022
Short summary
Short summary
We used palaeoecological records from peatlands in southern Siberia. We showed that warmer climate conditions have lowered the water level and increased the fuel amount and flammability, consequently also increasing the frequency and severity of fires as well as the composition of tree types.
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.
Fabian Rey, Erika Gobet, Christoph Schwörer, Albert Hafner, Sönke Szidat, and Willy Tinner
Clim. Past, 16, 1347–1367, https://doi.org/10.5194/cp-16-1347-2020, https://doi.org/10.5194/cp-16-1347-2020, 2020
Short summary
Short summary
We present a novel post Last Glacial Maximum sediment record from Moossee (Swiss Plateau, southern central Europe). For the first time, five major reorganizations of vegetation could be definitely linked to paramount postglacial temperature and/or moisture changes. Present-day beech-dominated forests have been resilient to long-term climate change and human land use. They may prevail in future if climate warming does not exceed the amplitude of Mid Holocene temperature and moisture variability.
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
Jose M. Mesa-Fernández, Gonzalo Jiménez-Moreno, Marta Rodrigo-Gámiz, Antonio García-Alix, Francisco J. Jiménez-Espejo, Francisca Martínez-Ruiz, R. Scott Anderson, Jon Camuera, and María J. Ramos-Román
Clim. Past, 14, 1687–1706, https://doi.org/10.5194/cp-14-1687-2018, https://doi.org/10.5194/cp-14-1687-2018, 2018
Liangjun Zhu, Qichao Yao, David J. Cooper, Shijie Han, and Xiaochun Wang
Clim. Past, 14, 1213–1228, https://doi.org/10.5194/cp-14-1213-2018, https://doi.org/10.5194/cp-14-1213-2018, 2018
Short summary
Short summary
This paper presents a 260-year tree-ring-based PDSI reconstruction for the central Daxing'an Mountains, northeast China. A warm–wet pattern was identified for the Daxing'an Mountains in recent decades, while a warm–dry pattern was found for the Mongolian Plateau. Overall, the dry/wet variability of the Daxing'an Mountains and its relationship with the surrounding areas might be driven by Pacific and Atlantic Ocean oscillations.
María J. Ramos-Román, Gonzalo Jiménez-Moreno, Jon Camuera, Antonio García-Alix, R. Scott Anderson, Francisco J. Jiménez-Espejo, and José S. Carrión
Clim. Past, 14, 117–137, https://doi.org/10.5194/cp-14-117-2018, https://doi.org/10.5194/cp-14-117-2018, 2018
Short summary
Short summary
In this study we carried out a multiproxy high-resolution analysis on a sediment record from the Padul Basin in the Sierra Nevada (southern Iberian Peninsula). Padul is a classical and very unique site from the Mediterranean area as it contains a very long and continuous Quaternary sedimentary record. However, the uppermost part of the record was never recovered. In this study we focus on the last 4700 cal yr BP of Holocene climate variability and human activity in the Mediterranean area.
Inke Elisabeth Maike Achterberg, Jan Eckstein, Bernhard Birkholz, Andreas Bauerochse, and Hanns Hubert Leuschner
Clim. Past, 14, 85–100, https://doi.org/10.5194/cp-14-85-2018, https://doi.org/10.5194/cp-14-85-2018, 2018
Short summary
Short summary
At a bog site at Totes Moor in northwest Germany a layer of pine tree stumps at the fen–bog transition was exposed by peat mining. The lateral expansion of ombrotrophic bog between 6703 BC and 3403 BC was reconstructed using the locations and dendrochronological dates of the tree stumps. The spatial pattern relates to the elevation a.s.l. of the mineral base beneath the peat. The temporal distribution of bog expansion pulses relates to climatic variation.
Olga N. Ukhvatkina, Alexander M. Omelko, Alexander A. Zhmerenetsky, and Tatyana Y. Petrenko
Clim. Past, 14, 57–71, https://doi.org/10.5194/cp-14-57-2018, https://doi.org/10.5194/cp-14-57-2018, 2018
Short summary
Short summary
We reconstructed the minimum temperature for 505 years and found cold and warm periods, which correlate with reconstructed data for the Northern Hemisphere and neighboring territories. Our reconstructions are reflected in the fluctuations in ENSO, the short-term solar cycle, PDO, and the de Vries 200-year solar activity cycle. This is the first temperature reconstruction for this region and it is important for studying the climatic processes in the study region and in all of northeastern Asia.
Xiayun Xiao, Simon G. Haberle, Ji Shen, Bin Xue, Mark Burrows, and Sumin Wang
Clim. Past, 13, 613–627, https://doi.org/10.5194/cp-13-613-2017, https://doi.org/10.5194/cp-13-613-2017, 2017
Short summary
Short summary
Knowledge of the past fire activity is a key for making sustainable management policies for forest ecosystems. A high-resolution macroscopic charcoal record from southwestern China reveals the postglacial fire history. Combined with the regional climate records and vegetation histories, it is concluded that fire was mainly controlled by climate before 4.3 ka and by combined action of climate and humans after 4.3 ka, and the relationship between fire activity and vegetation were also examined.
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.
Sahbi Jaouadi, Vincent Lebreton, Viviane Bout-Roumazeilles, Giuseppe Siani, Rached Lakhdar, Ridha Boussoffara, Laurent Dezileau, Nejib Kallel, Beya Mannai-Tayech, and Nathalie Combourieu-Nebout
Clim. Past, 12, 1339–1359, https://doi.org/10.5194/cp-12-1339-2016, https://doi.org/10.5194/cp-12-1339-2016, 2016
S. G. A. Flantua, H. Hooghiemstra, M. Vuille, H. Behling, J. F. Carson, W. D. Gosling, I. Hoyos, M. P. Ledru, E. Montoya, F. Mayle, A. Maldonado, V. Rull, M. S. Tonello, B. S. Whitney, and C. González-Arango
Clim. Past, 12, 483–523, https://doi.org/10.5194/cp-12-483-2016, https://doi.org/10.5194/cp-12-483-2016, 2016
Short summary
Short summary
This paper serves as a guide to high-quality pollen records in South America that capture environmental variability during the last 2 millennia. We identify the pollen records suitable for climate modelling and discuss their sensitivity to the spatial signature of climate modes. Furthermore, evidence for human land use in pollen records is useful for archaeological hypothesis testing and important in distinguishing natural from anthropogenically driven vegetation change.
Enlou Zhang, Yongbo Wang, Weiwei Sun, and Ji Shen
Clim. Past, 12, 415–427, https://doi.org/10.5194/cp-12-415-2016, https://doi.org/10.5194/cp-12-415-2016, 2016
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.
A. V. Gallego-Sala, D. J. Charman, S. P. Harrison, G. Li, and I. C. Prentice
Clim. Past, 12, 129–136, https://doi.org/10.5194/cp-12-129-2016, https://doi.org/10.5194/cp-12-129-2016, 2016
Short summary
Short summary
It has become a well-established paradigm that blanket bog landscapes in the British Isles are a result of forest clearance by early human populations. We provide a novel test of this hypothesis using results from bioclimatic modelling driven by cimate reconstructions compared with a database of peat initiation dates. Both results show similar patterns of peat initiation over time and space. This suggests that climate was the main driver of blanket bog inception and not human disturbance.
J. Azuara, N. Combourieu-Nebout, V. Lebreton, F. Mazier, S. D. Müller, and L. Dezileau
Clim. Past, 11, 1769–1784, https://doi.org/10.5194/cp-11-1769-2015, https://doi.org/10.5194/cp-11-1769-2015, 2015
Short summary
Short summary
High-resolution pollen analyses undertaken on two cores from southern France allow us to separate anthropogenic effects from climatic impacts on environments over the last 4500 years. A long-term aridification trend is highlighted during the late Holocene, and three superimposed arid events are recorded around 4400, 2600 and 1200cal BP coinciding in time with Bond events. Human influence on vegetation is attested since the Bronze Age and became dominant at the beginning of the High Middle Ages.
S. Y. Maezumi, M. J. Power, F. E. Mayle, K. K. McLauchlan, and J. Iriarte
Clim. Past, 11, 835–853, https://doi.org/10.5194/cp-11-835-2015, https://doi.org/10.5194/cp-11-835-2015, 2015
Short summary
Short summary
A 14,500-year, high-resolution, sedimentary record from Huanchaca Mesetta, a palm swamp located in the cerrãdo savanna in northeastern Bolivia, was analyzed for phytoliths, stable isotopes and charcoal. A non-analogue, cold-adapted vegetation community dominated the Late Glacial-Early Holocene period (14.5-9ka), which included trees and C3 Pooideae and C4 Panicoideae grasses. The Late Glacial vegetation was fire sensitive and fire activity during this period was low, likely responding to fuel av
M. E. de Porras, A. Maldonado, F. A. Quintana, A. Martel-Cea, O. Reyes, and C. Méndez
Clim. Past, 10, 1063–1078, https://doi.org/10.5194/cp-10-1063-2014, https://doi.org/10.5194/cp-10-1063-2014, 2014
Y. Wang, U. Herzschuh, L. S. Shumilovskikh, S. Mischke, H. J. B. Birks, J. Wischnewski, J. Böhner, F. Schlütz, F. Lehmkuhl, B. Diekmann, B. Wünnemann, and C. Zhang
Clim. Past, 10, 21–39, https://doi.org/10.5194/cp-10-21-2014, https://doi.org/10.5194/cp-10-21-2014, 2014
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
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. Joannin, B. Vannière, D. Galop, O. Peyron, J. N. Haas, A. Gilli, E. Chapron, S. B. Wirth, F. Anselmetti, M. Desmet, and M. Magny
Clim. Past, 9, 913–933, https://doi.org/10.5194/cp-9-913-2013, https://doi.org/10.5194/cp-9-913-2013, 2013
M.-P. Ledru, V. Jomelli, P. Samaniego, M. Vuille, S. Hidalgo, M. Herrera, and C. Ceron
Clim. Past, 9, 307–321, https://doi.org/10.5194/cp-9-307-2013, https://doi.org/10.5194/cp-9-307-2013, 2013
P. G. C. Amaral, A. Vincens, J. Guiot, G. Buchet, P. Deschamps, J.-C. Doumnang, and F. Sylvestre
Clim. Past, 9, 223–241, https://doi.org/10.5194/cp-9-223-2013, https://doi.org/10.5194/cp-9-223-2013, 2013
J. Bakker, E. Paulissen, D. Kaniewski, J. Poblome, V. De Laet, G. Verstraeten, and M. Waelkens
Clim. Past, 9, 57–87, https://doi.org/10.5194/cp-9-57-2013, https://doi.org/10.5194/cp-9-57-2013, 2013
S. Joannin, E. Brugiapaglia, J.-L. de Beaulieu, L. Bernardo, M. Magny, O. Peyron, S. Goring, and B. Vannière
Clim. Past, 8, 1973–1996, https://doi.org/10.5194/cp-8-1973-2012, https://doi.org/10.5194/cp-8-1973-2012, 2012
A. A. Andreev, E. Morozova, G. Fedorov, L. Schirrmeister, A. A. Bobrov, F. Kienast, and G. Schwamborn
Clim. Past, 8, 1287–1300, https://doi.org/10.5194/cp-8-1287-2012, https://doi.org/10.5194/cp-8-1287-2012, 2012
B. J. Dermody, H. J. de Boer, M. F. P. Bierkens, S. L. Weber, M. J. Wassen, and S. C. Dekker
Clim. Past, 8, 637–651, https://doi.org/10.5194/cp-8-637-2012, https://doi.org/10.5194/cp-8-637-2012, 2012
E. M. Gayo, C. Latorre, C. M. Santoro, A. Maldonado, and R. De Pol-Holz
Clim. Past, 8, 287–306, https://doi.org/10.5194/cp-8-287-2012, https://doi.org/10.5194/cp-8-287-2012, 2012
J. Lebamba, A. Vincens, and J. Maley
Clim. Past, 8, 59–78, https://doi.org/10.5194/cp-8-59-2012, https://doi.org/10.5194/cp-8-59-2012, 2012
A.-M. Lézine, W. Zheng, P. Braconnot, and G. Krinner
Clim. Past, 7, 1351–1362, https://doi.org/10.5194/cp-7-1351-2011, https://doi.org/10.5194/cp-7-1351-2011, 2011
A. Dallmeyer, M. Claussen, U. Herzschuh, and N. Fischer
Clim. Past, 7, 881–901, https://doi.org/10.5194/cp-7-881-2011, https://doi.org/10.5194/cp-7-881-2011, 2011
A. Vincens, G. Buchet, M. Servant, and ECOFIT Mbalang collaborators
Clim. Past, 6, 281–294, https://doi.org/10.5194/cp-6-281-2010, https://doi.org/10.5194/cp-6-281-2010, 2010
A. J. Chepstow-Lusty, M. R. Frogley, B. S. Bauer, M. J. Leng, K. P. Boessenkool, C. Carcaillet, A. A. Ali, and A. Gioda
Clim. Past, 5, 375–388, https://doi.org/10.5194/cp-5-375-2009, https://doi.org/10.5194/cp-5-375-2009, 2009
Cited articles
Allen, J. R. M. and Huntley, B.: Last Interglacial palaeovegetation,
palaeoenvironments and chronology: a new record from Lago Grande di
Monticchio, southern Italy, Quaternary Sci. Rev., 28, 1521–1538, 2009. a
Andersen, S. T.: Identification of wild grasses and cereal pollen, in:
Danmarks Geologiske Undersøgelse, Årbog, Copenhagen, Denmark, 69–92,
1979. a
Azzella, M. M. and Scarfó, F.: Atlante della vegetazione ripariale e
sommersa della Riserva Naturale Lago di Vico, Collana Atlanti Locali,
edizioni ARP, Roma, 2010. a
Behre, K.-E.: Some reflections on anthropogenic indicators and the record of
prehistoric occupation phases in pollen diagrams from the Near East, in:
Man's Role in the Shaping of the Eastern Mediterranean Landscape, edited by:
Bottema, S., Entjes-Nieborg, G., and van Zeist, W., Balkema, Rotterdam,
219–230, 1990. a
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P.,
Priore, P., Cullen, H., Hajdas, I., and Bonani, G.: A Pervasive
Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates,
Science, 278, 1257–1266, 1997. a
Büntgen, U., Tegel W., and Nicolussi, K.: 2500 years of European climate
variability and human susceptibility, Science, 331, 578–582, 2011. a
Čarni, A., Kostadinovski, M., and Matevski, V.: Species composition and
syntaxonomic consideration of two communities of the
Drabo-Cardaminion hirsutae in the southern part of the Republic of
Macedonia, Acta Bot. Croat., 62, 47–56, 2003. a
Caroli, I. and Caldara, M.: Vegetation history of Lago Battaglia (Eastern
Gargano coast, Apulia Italy) during the middle-late Holocene, Veg. Hist.
Archaeobot., 16, 317–327, 2007. a
Combourieu-Nebout, N., Peyron, O., Bout-Roumazeilles, V., Goring, S., Dormoy,
I., Joannin, S., Sadori, L., Siani, G., and Magny, M.: Holocene vegetation
and climate changes in the central Mediterranean inferred from a
high-resolution marine pollen record (Adriatic Sea), Clim. Past, 9,
2023–2042, https://doi.org/10.5194/cp-9-2023-2013, 2013. a
de Beaulieu, J.-L., Brugiapaglia, E., Joannin, S., Guiter, F., Zanchetta, G.,
Wulf, S., Peyron, O., Bernardo, L., Didier, J., Stock, A., Rius, D., and
Magny, M.: Late Glacial-Holocene abrupt vegetation changes at Lago
Trifoglietti in Calabria, southern Italy: the setting of ecosystems in a
refugial zone, Quaternary Sci. Rev., 158, 44–57, 2017. a
Denéfle, M., Lézine, A.-M., Fouache, E., and Dufaure, J.-J.: A
12,000-Year Pollen Record from Lake Maliq, Albania, Quaternary Res., 54,
423–432, 2000. a
Di Rita, F. and Magri, D.: Holocene drought, deforestation and evergreen
vegetation development in the central Mediterranean: a 5500 year record from
Lago Alimini Piccolo, Apulia, southeast Italy, Holocene, 19, 295–306, 2009. a
Eastwood, J. E.: East Mediterranean vegetation and climate change, in: Balkan
Biodiversity Pattern and Process in the European Hotspot, edited by:
Griffiths, H. I., Kryštufek, B., and Reed, J. M., Springer, 25–48, 2004. a
Francke, A., Wagner, B., Leng, M. J., and Rethemeyer, J.: Biogeochemical,
sedimentological and isotopic sediment record of Lake Dojran, PANGAEA,
https://doi.org/10.1594/PANGAEA,860791, 2013b. a
Giesecke, T., Hickler, T., Kunkel, T., Sykes, M. T., and Bradshaw, R. H. W.:
Towards an understanding of the Holocene distribution of Fagus sylvatica L.,
J. Biogeogr., 34, 118–131, 2007. a
Gimbutas, M.: Anza, ca. 6500–5000 B.C.: A Cultural Yardstick for the Study
of Neolithic Southeast Europe, J. Field Archaeol., 1, 27–66, 1974. a
Giraudi, C., Magny, M., Zanchetta, G., and Drysdale, R. N.: The Holocene
climatic evolution of Mediterranean Italy: A review of the continental
geological data, Holocene, 21, 105–115, 2011. a
Gogou, A., Triantaphyllou, M., Xoplaki, E., Izdebski, A., Parinos, C.,
Dimiza, M., Bouloubassi, I., Luterbacher, J., Kouli, K., Martrat, B., Toreti,
A., Fleitmann, D., Rousakis, G., Kaberi, H., Athanasiou, M., and Lykousis,
V.: Climate variability and socio-environmental changes in the northern
Aegean (NE Mediterranean) during the last 1500 years, Quaternary Sci. Rev.,
136, 209–228, 2016. a
Göktürk, O. M., Fleitmann, D., Badertscher, S., Cheng, H., Edwards, R.
L., Leuenberger, M., Fankhauser, A., Tüysüz, O., and Kramers, J.: Climate
on the southern Black Sea coast during the Holocene: implications from the
Sofular Cave record, Quaternary Sci. Rev., 30, 2433–2445, 2011. a
Harris, W. V.: Defining and detecting Mediterranean deforestation, 800 BCE
to 700 CE. The Ancient Mediterranean environment between science and
history, Brill, 173–194, 2013. a
Izdebski, A., Koloch, G., and Sloczynski, T.: Exploring Byzantine and Ottoman
Economic History with the Use of Palynological Data: A Quantitative Approach,
Jahrbuch der Osterreichischen Byzantinistik, 65, 67–109, 2015. a
Jahns, S. and van den Bogaard, C.: New palynological and
tephrostratigraphical investigations of two salt lagoons on the island of
Mljet, south Dalmatia, Croatia, Veg. Hist. Archaeobot., 7, 219–234, 1998. a
Johnsen, S. J., Dahl-Jensen, D., Gundestrup, N., Steffensen, J. P., Clausen,
H. B., Miller, H., Masson-Delmotte, V., Sveinbjörnsdottir, A. E., and
White, J.: Oxygen isotope and palaeotemperature records from six Greenland
ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP,
J. Quaternary Sci., 16, 299–307, 2001. a
Kaiser, T. and Voytek, B.: Sedentism and Economic Change in the Balkan
Neolithic, J. Anthropol. Archaeol., 2, 323–353, 1983. a
Keukelaar, F., de Goffau, A., Pradhan, T., Sutmuller, G., Misurovic, A.,
Ivanovic, S., Uskokovic, B., Hetoja, A., Haxhimihali, E., rifti, A.,
Kapidani, E., Kashta, L., and Gulan, A.: Lake Shkoder Transboundary
Diagnostics Analysis, Albania & Montenegro, World Bank (IBRD), 178 pp.,
available at: http://www.gov.me/files/1248091671.pdf (last access:
March 2018), 2006. a
Kokkinidou, D. and Trantalidou, K.: Neolithic and Bronze Age Settlement in
Western Macedonia, Annu. Brit. Sch. Athens, 86, 93–106, 1991. a
Kotthoff, U., Müller, U. C., Pross, J., Schmiedl, G., Lawson, I. T., van de
Schootbrugge, B., and Schulz, H.: Late Glacial and Holocene vegetation
dynamics in the Aegean region: an integrated view based on pollen data from
marine and terrestrial archives, Holocene, 18, 1019–1032, 2008. a
Kouli, K. and Dermitzakis, M. D.: Lake Orestiás (Kastoria, Northern
Greece), Grana, 49, 154–156, 2010. a
Lézine, A. M., Von Grafenstein, U., Andersen, N., Belmecheri, S., Bordon,
A., Caron, B., Cazet, J. P., Erlenkeuser, H., Fouache, E., Grenier, C.,
Huntsman-Mapila, P., Hureau-Mazaudier, D., Manelli, D., Mazaud, A., Robert,
C. Sulpizio, R., Tiercelin, J. J., Zanchetta, G., and Zeqollari, Z.: Lake
Ohrid, Albania, provides an exceptional multi-proxy record of environmental
changes during the last glacial–interglacial cycle, Palaeogeogr. Palaeocl.,
287, 116–127, 2010. a
Litt, T., Ohlwein, C., Neumann, F. H., Hense, A., and Stein, M.: Holocene
climate variability in the Levant from the Dead Sea pollen record, Quaternary
Sci. Rev., 49, 95–105, 2012. a
Marignani, M., Chiarucci, A., Sadori, L., and Mercuri, A. M.: Natural and
human impact in Mediterranean landscapes: An intriguing puzzle or only a
question of time?, Plant Biosyst., 151, 900–905, 2017. a
Masi, A., Francke, A., Pepe, C., Thienemann, M., Wagner, B., and Sadori, L.:
Pollen and biomarker record of Lake Dojran, PANGAEA,
https://doi.org/10.1594/PANGAEA.885797, 2017. a, b
Mazzini, I., Gliozzi, E., Galaty, M., Bejko, L., Sadori, L., Soulie-Marsche,
I., Koçi, R., Van Welden, A., and Bushati, S.: Holocene evolution of Lake
Shkodra: Multidisciplinary evidence for diachronic landscape change in
northern Albania, Quaternary Sci. Rev., 136, 85–95, 2016. a
Melovski, L., Velevski, M., Matevski, V., Avukatov, V., and Sarov, A.: Using
important plant areas and important bird areas to identify Key Biodiversity
Areas in the Republic of Macedonia, J. Threat. Taxa, 4, 2766–2778, 2012. a
Mercuri, A. M., Bandini Mazzanti, M., Torri, P., Vigliotti, L., Bosi, G.,
Florenzano, A., Olmi, L., and Massamba N'siala, I.: 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. Archaeobot., 21, 353–372, 2012. a
Mercuri, A. M., Mazzanti, M. B., Florenzano, A., Montecchi, M. C.,
Rattighieri, E., and Torri, P.: Anthropogenic Pollen Indicators (API) from
archaeological sites as local evidence of human-induced environments in the
Italian peninsula, Annali di Botanica, 3, 143–153, 2013b. a
Miebach, A., Niestrath, P., Roeser, P., and Litt, T.: Impacts of climate and
humans on the vegetation in northwestern Turkey: palynological insights from
Lake Iznik since the Last Glacial, Clim. Past, 12, 575–593,
https://doi.org/10.5194/cp-12-575-2016, 2016. a, b
Milner, A. M., Collier, R. E. L., Roucoux, K. H., Muller, U. C., Pross, J.,
Kalaitzidis, S., Christanis, K., and Tzedakis, P. C.: Enhanced seasonality of
precipitation in the Mediterranean during the early part of the Last
Interglacial, Geology, 40, 919–922, 2012. a
Morellon, M., Anselmetti, F. S., Ariztegui, D., Brushulli, B., Sinopoli, G.,
Wagner, B., Sadori, L., Gilli, A., and Pambuku, A.: Human-climate
interactions in the central Mediterranean region during the last millennia:
The laminated record of Lake Butrint (Albania), Quaternary Sci. Rev., 136,
134–152, 2016. a
Müller, U. C., Pross, J., Tzedakis, P. C., Gamble, C., Kotthoff, U.,
Schmiedl, G., Wulf, S., and Christanis, K.: The role of climate in the spread
of modern humans into Europe, Quaternary Sci. Rev., 30, 273–279, 2011. a
Panagiotopoulos, K., Böhm, A., Leng, M. J., Wagner, B., and Schäbitz,
F.: Climate variability over the last 92 ka in SW Balkans from analysis of
sediments from Lake Prespa, Clim. Past, 10, 643–660,
https://doi.org/10.5194/cp-10-643-2014, 2014. a
Petkovski, S., Matevski, V., Melovski, L., Andonov, S., and Spirkovski, Z.:
Capacity self-assessment within the thematic area of biodiversity, UNDP,
Skopje, 2004. a
Popovska, C., Bonacci, O., and Geshovska, V.: Climatic or Anthropogenic
Impacts – Case Study Dojran Lake, International Journal of Environmental
Engineering and Natural Resources, 1, 140–149, 2014. a
Pollegioni, P., Woeste, K., Chiocchini, F., Del Lungo, S., Ciolfi, M.,
Olimpieri, I., Tortolano, V., Clark, J., Hemery, G. E., Mapelli, S., and
Malvolti, M. E.: Rethinking the history of common walnut (Juglans regia L.) in Europe: Its origins and human interactions, PLoS ONE, 12,
e0172541, https://doi.org/10.1371/journal.pone.0172541, 2017. a
Pross, J., Koutsodendris, A., Christanis, K., Fischer, T., Fletcher, W. J.,
Hardiman, M., Kalaitzidis, S., Knipping, M., Kotthoff, U., Milner, A. M.,
Müller, U. C., Schmiedl, G., Siavalas, G., Tzedakis, P. C., and Wulf, S.:
The 1.35-Ma-long terrestrial climate archive of Tenaghi Philippon,
northeastern Greece: Evolution, exploration, and perspectives for future
research, Newsl. Stratigr., 48, 253–276, 2015. a
Reille, M.: Pollen et spores d'Europe et d'Afrique du Nord, Laboratoire de
Botanique Historique et Palynologie, Université d'Aix Marseille III,
Marseille, 1992. a
Reille, M.: Pollen et spores d'Europe et d'Afrique du Nord – Suppément 1,
Laboratoire de Botanique Historique et Palynologie, Université d'Aix
Marseille III, Marseille, 1995. a
Reille, M.: Pollen et spores d'Europe et d'Afrique du Nord – Supplément 2,
Laboratoire de Botanique Historique et Palynologie, Université d'Aix
Marseille III, Marseille, 1998. a
Roucoux, K. H., Tzedakis, P. C., Lawson, I. T., and Margari, V.: Vegetation
history of the penultimate glacial period (Marine Isotope Stage 6) at
Ioannina, north-west Greece, J. Quaternary Sci., 26, 616–626, 2011. a
Sadori, L., Giraudi, C., Petitti, P., and Ramrath, A.: Human impact at Lago
di Mezzano (central Italy) during the Bronze Age: A multidisciplinary
approach, Quatern. Int., 113, 5–17, 2004. a
Sadori, L., Zanchetta, G., and Giardini, M.: Last Glacial to Holocene
palaeoenvironmental evolution at Lago di Pergusa (Sicily, Southern Italy) as
inferred by pollen, microcharcoal, and stable isotopes, Quatern. Int., 181,
4–14, 2008. a
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. a
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,
2015a. a
Sadori, L., Giraudi, C., Masi, A., Magny, M., Ortu, E., Zanchetta, G., and
Izdebski, A.: Climate, environment and society in southern Italy during the
last 2000 years. A review of the environmental, historical and archaeological
evidence, Quaternary Sci. Rev., 136, 173–188, 2016a. a
Sadori, L., Koutsodendris, A., Panagiotopoulos, K., Masi, A., Bertini, A.,
Combourieu-Nebout, N., Francke, A., Kouli, K., Joannin, S., Mercuri, A. M.,
Peyron, O., Torri, P., Wagner, B., Zanchetta, G., Sinopoli, G., and Donders,
T. H.: Pollen-based paleoenvironmental and paleoclimatic change at Lake Ohrid
(south-eastern Europe) during the past 500 ka, Biogeosciences, 13,
1423–1437, https://doi.org/10.5194/bg-13-1423-2016, 2016b. a, b
Smit, A.: A scanning electron microscopical study of the pollen morphology in
the genus Quercus, Acta Bot. Neerl., 22, 655–665, 1973. a
Staubwasser, M. and Weiss, H.: Holocene climate and cultural evolution in
late prehistoric–early historic West Asia, Quaternary Res., 66, 372–387,
2006. a
Stockmarr, J.: Tables with spores used in absolute pollen analysis, Pollen
and Spores, 13, 614–621, 1971. a
Thienemann, M., Masi, A., Kusch, S., Sadori, L., John, S., Francke, A.,
Wagner, B., and Rethemeyer, J.: Reconstructing environmental and human
settlement history on the southern Balkan Peninsula using lipid biomarker,
pollen, and microcharcoal data from Lake Dojran sediments, Holocene, 27,
1103–1114, 2017. a, b, c, d, e, f, g, h
Tinner, W., van Leeuwen, J. F. N., Colombaroli, D., Vescovi, E., van der
Knaap, W. O., Henne, P. D., Pasta, S., D'Angelo, S., and La Mantia, T.:
Holocene environmental and climatic changes at Gorgo Basso, a coastal lake in
southern Sicily, Italy, Quaternary Sci. Rev., 28, 1498–1510, 2009. a
Tonkov, S., Panovska, H., Possnert, G., and Bozilova, E.: The Holocene
vegetation history of Northern Pirin Mountain, southwestern Bulgaria: pollen
analysis and radiocarbon dating of a core from Lake Ribno Ban derishko,
Holocene, 12, 201–210, 2002. a
Tonkov, S., Possnert, G., Bozilova, E., Marinova, E., and Pavlova, D.: On the
Holocene vegetation history of the Central Rila Mountains, Bulgaria: The
palaeoecological record of peat bog Vodniza (2113 m), Rev. Palaeobot.
Palyno., 250, 16–26, 2018. a
Tzedakis, P. C.: Seven ambiguities in the Mediterranean palaeoenvironmental
narrative, Quaternary Sci. Rev., 26, 2042–2066, 2007. a
Tzedakis, P. C., Hooghiemstra, H., and Pälike, H.: The last 1.35 million
years at Tenaghi Philippon: revised chronostratigraphy and long-term
vegetation trends, Quaternary Sci. Rev., 25, 3416–3430, 2006. a
Valsecchi, V., Finsinger, W., Tinner, V., and Ammann, B.: Testing the
influence of climate, human impact and fire on the Holocene population
expansion of Fagus sylvatica in the southern Prealps (Italy), Holocene, 18,
603–614, 2008. a
Vanniére, B., Power, M. J., Roberts, N., Tinner, W., Carrión, J., Magny,
M., Bartlein, P., Colombaroli, D., Daniau, A. L., Finsinger, W., Gil-Romera,
G., Kaltenrieder, P., Pini, R., Sadori, L., Turner, R., Valsecchi, V., and
Vescovi, E.: Circum-Mediterranean fire activity and climate changes during
the mid-Holocene environmental transition (8500–2500 cal. BP), Holocene, 21,
53–73, 2011. a
van Zeist, W., Woldring, H., and Stapert, D.: Late Quaternary vegetation and
climate of southwestern Turkey, Palaeohistoria, 17, 55–143, 1975. a
Wagner, B., Lotter, A. F., Nowaczyk, N., Reed, J. M., Schwalb, A., Sulpizio,
R., Valsecchi, V., Wessels, M., and Zanchetta, G.: A 40,000-year record of
environmental change from ancient Lake Ohrid (Albania and Macedonia), J.
Paleolimnol., 41, 407–430, 2009. 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
Whitlock, C., Higuera, P. E., McWethy, D. B., and Briles, C. E.:
Paleoecological Perspectives on Fire Ecology: Revisiting the Fire-Regime
Concept, Open Ecol. J., 3, 6–23, 2010. a
Xoplaki, E., Fleitmann, D., Luterbacher, J., Wagner, S., Haldon, J. F.,
Zorita, E., Telelis, I., Toreti, A., and Izdebski, A.: The Medieval Climate
Anomaly and Byzantium: A review of the evidence on climatic fluctuations,
economic performance and societal change, Quaternary Sci. Rev., 136,
229–252, 2016. a
Zanchetta, G., Van Welden, A., Baneschi, I., Drysdale, R., Sadori, L.,
Roberts, N., Giardini, M., Beck, C., Pascucci, V., and Sulpizio, R.:
Multiproxy record for the last 4500 years from Lake Shkodra
(Albania/Montenegro), J. Quaternary Sci., 27, 780–789, 2012. a
Zanchetta, G., Regattieri, E., Isola, I., Drysdale, R. N., Bini, M.,
Baneschi, I., and Hellstrom, J. C.: The so-called “4.2 event” in the
central mediterranean and its climatic teleconnections, Alpine and
Mediterranean Quaternary, 29, 5–17, 2016. a
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.
The first high-resolution Lake Dojran pollen record for the last 12 500 years is presented. The...