Articles | Volume 15, issue 1
Clim. Past, 15, 389–404, 2019
https://doi.org/10.5194/cp-15-389-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Clim. Past, 15, 389–404, 2019
https://doi.org/10.5194/cp-15-389-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Technical note 28 Feb 2019
Technical note | 28 Feb 2019
Technical note: Optimizing the utility of combined GPR, OSL, and Lidar (GOaL) to extract paleoenvironmental records and decipher shoreline evolution
Amy J. Dougherty et al.
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Chris S. M. Turney, Richard T. Jones, Nicholas P. McKay, Erik van Sebille, Zoë A. Thomas, Claus-Dieter Hillenbrand, and Christopher J. Fogwill
Earth Syst. Sci. Data, 12, 3341–3356, https://doi.org/10.5194/essd-12-3341-2020, https://doi.org/10.5194/essd-12-3341-2020, 2020
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The Last Interglacial (129–116 ka) experienced global temperatures and sea levels higher than today. The direct contribution of warmer conditions to global sea level (thermosteric) are uncertain. We report a global network of sea surface temperatures. We find mean global annual temperature anomalies of 0.2 ± 0.1˚C and an early maximum peak of 0.9 ± 0.1˚C. Our reconstruction suggests warmer waters contributed on average 0.08 ± 0.1 m and a peak contribution of 0.39 ± 0.1 m to global sea level.
Holly L. Taylor, Isaac J. Kell Duivestein, Juraj Farkas, Martin Dietzel, and Anthony Dosseto
Clim. Past, 15, 635–646, https://doi.org/10.5194/cp-15-635-2019, https://doi.org/10.5194/cp-15-635-2019, 2019
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Approximately 600 million years ago, major environmental changes set the course for the emergence of animal life. Lithium (Li) isotopes in calcium carbonates can be used as a proxy to understand changes in the palaeo-environment. We conducted experiments that allow us to use Li isotopes in dolostones to extend our understanding of palaeo-environmental changes deeper into the geological record, where other calcium carbonates archives are not present.
Chris S. M. Turney, Helen V. McGregor, Pierre Francus, Nerilie Abram, Michael N. Evans, Hugues Goosse, Lucien von Gunten, Darrell Kaufman, Hans Linderholm, Marie-France Loutre, and Raphael Neukom
Clim. Past, 15, 611–615, https://doi.org/10.5194/cp-15-611-2019, https://doi.org/10.5194/cp-15-611-2019, 2019
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This PAGES (Past Global Changes) 2k (climate of the past 2000 years working group) special issue of Climate of the Past brings together the latest understanding of regional change and impacts from PAGES 2k groups across a range of proxies and regions. The special issue has emerged from a need to determine the magnitude and rate of change of regional and global climate beyond the timescales accessible within the observational record.
Eleanor Rainsley, Chris S. M. Turney, Nicholas R. Golledge, Janet M. Wilmshurst, Matt S. McGlone, Alan G. Hogg, Bo Li, Zoë A. Thomas, Richard Roberts, Richard T. Jones, Jonathan G. Palmer, Verity Flett, Gregory de Wet, David K. Hutchinson, Mathew J. Lipson, Pavla Fenwick, Ben R. Hines, Umberto Binetti, and Christopher J. Fogwill
Clim. Past, 15, 423–448, https://doi.org/10.5194/cp-15-423-2019, https://doi.org/10.5194/cp-15-423-2019, 2019
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The New Zealand subantarctic islands, in the Pacific sector of the Southern Ocean, provide valuable records of past environmental change. We find that the Auckland Islands hosted a small ice cap around 384 000 years ago, but that there was little glaciation during the Last Glacial Maximum, around 21 000 years ago, in contrast to mainland New Zealand. This shows that the climate here is susceptible to changes in regional factors such as sea-ice expanse and the position of ocean fronts.
Florian Adolphi, Christopher Bronk Ramsey, Tobias Erhardt, R. Lawrence Edwards, Hai Cheng, Chris S. M. Turney, Alan Cooper, Anders Svensson, Sune O. Rasmussen, Hubertus Fischer, and Raimund Muscheler
Clim. Past, 14, 1755–1781, https://doi.org/10.5194/cp-14-1755-2018, https://doi.org/10.5194/cp-14-1755-2018, 2018
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The last glacial period was characterized by a number of rapid climate changes seen, for example, as abrupt warmings in Greenland and changes in monsoon rainfall intensity. However, due to chronological uncertainties it is challenging to know how tightly coupled these changes were. Here we exploit cosmogenic signals caused by changes in the Sun and Earth magnetic fields to link different climate archives and improve our understanding of the dynamics of abrupt climate change.
Zoë A. Thomas, Richard T. Jones, Chris J. Fogwill, Jackie Hatton, Alan N. Williams, Alan Hogg, Scott Mooney, Philip Jones, David Lister, Paul Mayewski, and Chris S. M. Turney
Clim. Past, 14, 1727–1738, https://doi.org/10.5194/cp-14-1727-2018, https://doi.org/10.5194/cp-14-1727-2018, 2018
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We report a high-resolution study of a 5000-year-long peat record from the Falkland Islands. This area sensitive to the dynamics of the Amundsen Sea Low, which plays a major role in modulating the Southern Ocean climate. We find wetter, colder conditions between 5.0 and 2.5 ka due to enhanced southerly airflow, with the establishment of drier and warmer conditions from 2.5 ka to present. This implies more westerly airflow and the increased projection of the ASL onto the South Atlantic.
Anthony Dosseto, Holly L. Taylor, Juraj Farkaš, Grant M. Cox, Andrew Kingston, Andrew Lorrey, Alexander J. Corrick, and Bing Shen
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-119, https://doi.org/10.5194/cp-2018-119, 2018
Revised manuscript not accepted
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Life experienced a big boost in complexity ~ 600 million years ago. This step forward in evolution happened not long after the largest glaciations experienced in Earth's history. This study shows that following the last major
Snowball Earth, the planet's surface rapidly recovered and the first animals emerged in an environment maybe not that different from our modern oceans.
Chris S.~M. Turney, Andrew Klekociuk, Christopher J. Fogwill, Violette Zunz, Hugues Goosse, Claire L. Parkinson, Gilbert Compo, Matthew Lazzara, Linda Keller, Rob Allan, Jonathan G. Palmer, Graeme Clark, and Ezequiel Marzinelli
The Cryosphere Discuss., https://doi.org/10.5194/tc-2017-51, https://doi.org/10.5194/tc-2017-51, 2017
Revised manuscript not accepted
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We demonstrate that a mid-twentieth century decrease in geopotential height in the southwest Pacific marks a Rossby wave response to equatorial Pacific warming, leading to enhanced easterly airflow off George V Land. Our results suggest that in contrast to ozone hole-driven changes in the Amundsen Sea, the 1979–2015 increase in sea ice extent off George V Land may be in response to reduced northward Ekman drift and enhanced (near-coast) production as a consequence of low latitude forcing.
Chris S. M. Turney, Christopher J. Fogwill, Jonathan G. Palmer, Erik van Sebille, Zoë Thomas, Matt McGlone, Sarah Richardson, Janet M. Wilmshurst, Pavla Fenwick, Violette Zunz, Hugues Goosse, Kerry-Jayne Wilson, Lionel Carter, Mathew Lipson, Richard T. Jones, Melanie Harsch, Graeme Clark, Ezequiel Marzinelli, Tracey Rogers, Eleanor Rainsley, Laura Ciasto, Stephanie Waterman, Elizabeth R. Thomas, and Martin Visbeck
Clim. Past, 13, 231–248, https://doi.org/10.5194/cp-13-231-2017, https://doi.org/10.5194/cp-13-231-2017, 2017
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The Southern Ocean plays a fundamental role in global climate but suffers from a dearth of observational data. As the Australasian Antarctic Expedition 2013–2014 we have developed the first annually resolved temperature record using trees from subantarctic southwest Pacific (52–54˚S) to extend the climate record back to 1870. With modelling we show today's high climate variability became established in the ~1940s and likely driven by a Rossby wave response originating from the tropical Pacific.
Christopher J. Fogwill, Erik van Sebille, Eva A. Cougnon, Chris S. M. Turney, Steve R. Rintoul, Benjamin K. Galton-Fenzi, Graeme F. Clark, E. M. Marzinelli, Eleanor B. Rainsley, and Lionel Carter
The Cryosphere, 10, 2603–2609, https://doi.org/10.5194/tc-10-2603-2016, https://doi.org/10.5194/tc-10-2603-2016, 2016
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Here we report new data from in situ oceanographic surveys and high-resolution ocean modelling experiments in the Commonwealth Bay region of East Antarctica, where in 2010 there was a major reconfiguration of the regional icescape due to the collision of the 97 km long iceberg B09B with the Mertz Glacier tongue. Here we compare post-calving observations with high-resolution ocean modelling which suggest that this reconfiguration has led to the development of a new polynya off Commonwealth Bay.
Steven J. Phipps, Christopher J. Fogwill, and Christian S. M. Turney
The Cryosphere, 10, 2317–2328, https://doi.org/10.5194/tc-10-2317-2016, https://doi.org/10.5194/tc-10-2317-2016, 2016
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We explore the effects of melting of the East Antarctic Ice Sheet on the Southern Ocean. Using a climate model, we find that melting changes the ocean circulation and causes warming of more than 1 °C at depth. We also discover the potential existence of a "domino effect", whereby the initial warming spreads westwards around the Antarctic continent. Melting of just one sector could therefore destabilise the wider Antarctic Ice Sheet, leading to substantial increases in global sea level.
C. S. M. Turney, R. T. Jones, C. Fogwill, J. Hatton, A. N. Williams, A. Hogg, Z. A. Thomas, J. Palmer, S. Mooney, and R. W. Reimer
Clim. Past, 12, 189–200, https://doi.org/10.5194/cp-12-189-2016, https://doi.org/10.5194/cp-12-189-2016, 2016
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Southern Hemisphere westerly airflow is considered a major driver of Southern Ocean and global climate. Observational records, however, are limited. Here we present a new Falkland Islands record that exploits "exotic" South America pollen and charcoal to reconstruct changing airflow. We find stronger winds 2000–1000 cal. yr BP, associated with increased burning, and a 250-year periodicity, suggesting solar forcing. Our results have important implications for understanding late Holocene climates.
C. S. M. Turney, C. J. Fogwill, A. R. Klekociuk, T. D. van Ommen, M. A. J. Curran, A. D. Moy, and J. G. Palmer
The Cryosphere, 9, 2405–2415, https://doi.org/10.5194/tc-9-2405-2015, https://doi.org/10.5194/tc-9-2405-2015, 2015
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Recent trends in ocean circulation, sea ice and climate over the Southern Ocean and Antarctica are highly complex. Here we report a new snow core from the South Pole alongside reanalysis of 20th century global atmospheric circulation. We demonstrate for the first time that atmospheric pressure anomalies in the mid-latitudes act as "gatekeepers" to meridional exchange over continental Antarctica, modulated by the tropical Pacific, with potentially significant impacts on surface mass balance.
Z. A. Thomas, F. Kwasniok, C. A. Boulton, P. M. Cox, R. T. Jones, T. M. Lenton, and C. S. M. Turney
Clim. Past, 11, 1621–1633, https://doi.org/10.5194/cp-11-1621-2015, https://doi.org/10.5194/cp-11-1621-2015, 2015
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Using a combination of speleothem records and model simulations of the East Asian Monsoon over the penultimate glacial cycle, we search for early warning signals of past tipping points. We detect a characteristic slower response to perturbations prior to an abrupt monsoon shift at the glacial termination; however, we do not detect these signals in the preceding shifts. Our results have important implications for detecting tipping points in palaeoclimate records outside glacial terminations.
A. Rouillard, G. Skrzypek, S. Dogramaci, C. Turney, and P. F. Grierson
Hydrol. Earth Syst. Sci., 19, 2057–2078, https://doi.org/10.5194/hess-19-2057-2015, https://doi.org/10.5194/hess-19-2057-2015, 2015
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We reconstructed a 100-year monthly history of flooding and drought of a large wetland in arid northwest Australia, using hydroclimatic data calibrated against 25 years of satellite images. Severe and intense regional rainfall, as well as the sequence of events, determined surface water expression on the floodplain. While inter-annual variability was high, changes to the flood regime over the last 20 years suggest the wetland may become more persistent in response to the observed rainfall trend.
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Holocene
Climate reconstructions based on GDGT and pollen surface datasets from Mongolia and Siberia: 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
Cold season warming in the North Atlantic during the last 2000 years: Evidence from Southwest Iceland
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
The 4.2 ka BP Event in the Mediterranean region: an overview
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
A Bayesian hierarchical model for reconstructing relative sea level: from raw data to rates of change
Inferring climate variability from nonlinear proxies: application to palaeo-ENSO studies
Technical Note: How accurate can stalagmite formation temperatures be determined using vapour bubble radius measurements in fluid inclusions?
High-resolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central Asia
Arctic Holocene proxy climate database – new approaches to assessing geochronological accuracy and encoding climate variables
Testing long-term summer temperature reconstruction based on maximum density chronologies obtained by reanalysis of tree-ring data sets from northernmost Sweden and Finland
Constraining Holocene hydrological changes in the Carpathian–Balkan region using speleothem δ18O and pollen-based temperature reconstructions
Sediment transport processes across the Tibetan Plateau inferred from robust grain-size end members in lake sediments
Similarity estimators for irregular and age-uncertain time series
Mid- and late Holocene dust deposition in western Europe: the Misten peat bog (Hautes Fagnes – Belgium)
A mid-Holocene climate reconstruction for eastern South America
North–south palaeohydrological contrasts in the central Mediterranean during the Holocene: tentative synthesis and working hypotheses
Late Neolithic Mondsee Culture in Austria: living on lakes and living with flood risk?
Tree-ring–based summer mean temperature variations in the Adamello–Presanella Group (Italian Central Alps), 1610–2008 AD
Long-term summer sunshine/moisture stress reconstruction from tree-ring widths from Bosnia and Herzegovina
Lucas Dugerdil, Sébastien Joannin, Odile Peyron, Isabelle Jouffroy-Bapicot, Boris Vannière, Boldgiv Bazartseren, Julia Unkelbach, Hermann Behling, and Guillemette Ménot
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-154, https://doi.org/10.5194/cp-2020-154, 2020
Revised manuscript accepted for CP
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Since the understanding of Holocene climate change appear 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 biomakers climate models. These calibrations appear to be more powerful than global calibrations, especially in Arid Central Asian context. These calibrations will improve the Monsoon Holocene oscillations understanding.
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
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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
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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.
Nora Richter, James M. Russell, Johanna Garfinkel, and Yongsong Huang
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-84, https://doi.org/10.5194/cp-2020-84, 2020
Revised manuscript accepted for CP
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We present a reconstruction of winter–spring temperatures from lake sediments in Iceland over the last 2000 years to improve our understanding of seasonal temperature changes in the North Atlantic region. We observe warming in winter–spring temperatures that is likely driven by increasing winter–spring insolation. On multi-decadal to centennial timescales, changes in cold season temperatures are associated with solar minima and volcanic eruptions but also internal climate variability.
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
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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
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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
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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
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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
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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
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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
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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
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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.
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
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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.
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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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
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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).
Niamh Cahill, Andrew C. Kemp, Benjamin P. Horton, and Andrew C. Parnell
Clim. Past, 12, 525–542, https://doi.org/10.5194/cp-12-525-2016, https://doi.org/10.5194/cp-12-525-2016, 2016
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We propose a Bayesian model for the reconstruction and analysis of former sea levels. The model provides a single, unifying framework for reconstructing and analyzing sea level through time with fully quantified uncertainty. We illustrate our approach using a case study of Common Era (last 2000 years) sea levels from New Jersey.
J. Emile-Geay and M. Tingley
Clim. Past, 12, 31–50, https://doi.org/10.5194/cp-12-31-2016, https://doi.org/10.5194/cp-12-31-2016, 2016
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Ignoring nonlinearity in palaeoclimate records (e.g. continental run-off proxies) runs the risk of severely overstating changes in climate variability. Even with the correct model and parameters, some information is irretrievably lost by such proxies. However, we find that a simple empirical transform can do much to improve the situation, and makes them amenable to classical analyses. Doing so on two palaeo-ENSO records markedly changes some of the quantitative inferences made from such records.
F. Spadin, D. Marti, R. Hidalgo-Staub, J. Rička, D. Fleitmann, and M. Frenz
Clim. Past, 11, 905–913, https://doi.org/10.5194/cp-11-905-2015, https://doi.org/10.5194/cp-11-905-2015, 2015
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Fluid inclusions inside stalagmites retain information on the cave temperature at the time they formed and thus can be used to reconstruct the continental climate of the past. A method for extracting this information based on a thermodynamic model and size measurements of femtosecond-laser-induced vapour bubbles is presented. Applying our method to stalagmites taken from the Milandre cave in the Swiss Jura Mountains demonstrate that palaeotemperatures can be determined with an accuracy of ±1°C.
B. Aichner, S. J. Feakins, J. E. Lee, U. Herzschuh, and X. Liu
Clim. Past, 11, 619–633, https://doi.org/10.5194/cp-11-619-2015, https://doi.org/10.5194/cp-11-619-2015, 2015
H. S. Sundqvist, D. S. Kaufman, N. P. McKay, N. L. Balascio, J. P. Briner, L. C. Cwynar, H. P. Sejrup, H. Seppä, D. A. Subetto, J. T. Andrews, Y. Axford, J. Bakke, H. J. B. Birks, S. J. Brooks, A. de Vernal, A. E. Jennings, F. C. Ljungqvist, K. M. Rühland, C. Saenger, J. P. Smol, and A. E. Viau
Clim. Past, 10, 1605–1631, https://doi.org/10.5194/cp-10-1605-2014, https://doi.org/10.5194/cp-10-1605-2014, 2014
V. V. Matskovsky and S. Helama
Clim. Past, 10, 1473–1487, https://doi.org/10.5194/cp-10-1473-2014, https://doi.org/10.5194/cp-10-1473-2014, 2014
V. Drăguşin, M. Staubwasser, D. L. Hoffmann, V. Ersek, B. P. Onac, and D. Veres
Clim. Past, 10, 1363–1380, https://doi.org/10.5194/cp-10-1363-2014, https://doi.org/10.5194/cp-10-1363-2014, 2014
E. Dietze, F. Maussion, M. Ahlborn, B. Diekmann, K. Hartmann, K. Henkel, T. Kasper, G. Lockot, S. Opitz, and T. Haberzettl
Clim. Past, 10, 91–106, https://doi.org/10.5194/cp-10-91-2014, https://doi.org/10.5194/cp-10-91-2014, 2014
K. Rehfeld and J. Kurths
Clim. Past, 10, 107–122, https://doi.org/10.5194/cp-10-107-2014, https://doi.org/10.5194/cp-10-107-2014, 2014
M. Allan, G. Le Roux, N. Piotrowska, J. Beghin, E. Javaux, M. Court-Picon, N. Mattielli, S. Verheyden, and N. Fagel
Clim. Past, 9, 2285–2298, https://doi.org/10.5194/cp-9-2285-2013, https://doi.org/10.5194/cp-9-2285-2013, 2013
L. F. Prado, I. Wainer, C. M. Chiessi, M.-P. Ledru, and B. Turcq
Clim. Past, 9, 2117–2133, https://doi.org/10.5194/cp-9-2117-2013, https://doi.org/10.5194/cp-9-2117-2013, 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
T. Swierczynski, S. Lauterbach, P. Dulski, and A. Brauer
Clim. Past, 9, 1601–1612, https://doi.org/10.5194/cp-9-1601-2013, https://doi.org/10.5194/cp-9-1601-2013, 2013
A. Coppola, G. Leonelli, M. C. Salvatore, M. Pelfini, and C. Baroni
Clim. Past, 9, 211–221, https://doi.org/10.5194/cp-9-211-2013, https://doi.org/10.5194/cp-9-211-2013, 2013
S. Poljanšek, A. Ceglar, and T. Levanič
Clim. Past, 9, 27–40, https://doi.org/10.5194/cp-9-27-2013, https://doi.org/10.5194/cp-9-27-2013, 2013
Cited articles
Bailey, R. M. and Arnold, L. J.: Statistical modelling of single grain quartz
De distributions and an assessment of procedures for estimating burial dose,
Quaternary Sci. Rev., 25, 2475–2502, 2006.
Barboza, E. G., Dillenburg, S. R., Rosa, M. L. C. C., Tomazelli, L. J., and
Hesp, P. A.: Ground-penetrating radar Profiles of Two Holocene Regressive
Barriers in Southern Brazil, J. Coastal Res., 1, 579–583, 2009.
Barboza, E., Rosa, M., Hesp, P., Dillenburg, S., Tomazelli, L., and
Ayup-Zouain, R.: Evolution of the Holocene Coastal Barrier of Pelotas Basin
(Southern Brazil) – a new approach with GPR data, J. Coastal Res., 64, 646–650,
2011.
Begg, J. G. and Mouslopoulou, V.: Analysis of late Holocene faulting within
an active rift using lidar, Taupo Rift, New Zealand, J. Volcanol. Geoth.
Res., 190, 152–167, 2010.
Bernard, H. A., LeBlanc, R. J., and Major, C. F.: Recent and Pleistocene
Geology of Southeast Texas: Field Excursion No. 3, 10 and 11 November 1962,
175–224, Houston Geological Society, Houston, Texas, USA, 1962.
Bristow, C. S. and Jol, H. M.: An introduction to ground penetrating radar
(GPR) in sediments, Geol. Soc. Spec. Publ., 211, 1–7, 2003.
Bristow, C. S. and Pucillo, K.: Quantifying rates of coastal progradation
from sediment volume using GPR and OSL: the Holocene fill of Guichen Bay,
south-east South Australia, Sedimentology, 53, 769–788, 2006.
Buynevich, I. V., FitzGerald, D. M., and van Heteren, S.: Sedimentary records
of intense storms in Holocene barrier sequences, Maine, USA, Mar. Geol., 210,
135–148, 2004.
Buynevich, I. V., FitzGerald, D. M., and Goble, R. J.: A 1500 a record of
North Atlantic storm activity based on optically dated relict beach scarps,
Geology, 35, 543–546, 2007.
Buynevich, I. V., Jol, H. M., and FitzGerald, D. M.: Coastal environments,
in: Ground penetrating radar: Theory and applications, edited by: Jol, H. M.,
299–322, 2009.
Caseldine, C. J. and Turney, C.: The bigger picture: Towards integrating
palaeoclimate and environmental data with a history of societal change, J.
Quaternary Sci., 25, 88–93, 2010.
Choi, K. H., Choi, J.-H., and Kim, J. W.: Reconstruction of Holocene coastal
progradation on the east coast of Korea based on OSL dating and GPR surveys
of beach-foredune ridges, Holocene, 24, 24–34, 2014.
Clemmensen, L. B., Bendixen, M., Hede, M. U., Kroon, A., Nielsen, L., and
Murray, A. S.: Morphological records of storm floods exemplified by the
impact of the 1872 Baltic storm on a sandy spit system in south-eastern
Denmark, Earth Surf. Proc. Land., 39, 499–508, 2014.
Coco, G., O'Hare, T. J., and Huntley, D. A.: Beach cusps: a comparison of
data and theories for their formation, J. Coastal Res., 15, 741–749, 1999.
Costas, S. and FitzGerald, D.: Sedimentary architecture of a spit-end
(Salisbury Beach, Massachusetts): The imprints of sea-level rise and inlet
dynamics, Mar. Geol., 284, 203–216, 2011.
Costas, S., Ferreira, Ó., Plomaritis, T. A., and Leorri, E.: Coastal
barrier stratigraphy for Holocene high-resolution sea-level reconstruction,
Sci. Rep., 6, 38726, https://doi.org/10.1038/srep38726, 2016.
Curray, J., Emmel, F., and Crampton, P.: Holocene history of a strand plain,
lagoonal coast, Nayarit, Mexico, in: Coastal Lagoons, a Symposium, edited by:
Ayala-Castañares, A. and Phleger, F. B., 63–100, University Nacional
Autonoma Mexico–UNESCO, Mexico, 1969.
Dougherty, A. and Dickson, M.: Sea level and storm control on the evolution
of a chenier plain, Firth of Thames, New Zealand, Mar. Geol., 307, 58–72,
2012.
Dougherty, A. and Nichol, S.: 3-D Stratigraphic Models of a Composite Barrier
System, Northern New Zealand, J. Coastal Res., 50, 922–926, 2007.
Dougherty, A. J.: Evolution of prograded coastal barriers in northern New
Zealand, ResearchSpace, Auckland, 2011.
Dougherty, A. J.: Extracting a record of Holocene storm erosion and
deposition preserved in the morphostratigraphy of a prograded coastal
barrier, Cont. Shelf Res., 86, 116–131, 2014.
Dougherty, A. J.: Punctuated transgression (?): Comment on Oliver, T. S. N.,
Donaldson, P., Sharples, C., Roach, M., and Woodroffe, C. D. “Punctuated
progradation of the Seven Mile Beach Holocene barrier system, southeastern
Tasmania”, Mar. Geol., 405, 120–130, https://doi.org/10.1016/j.margeo.2018.01.009,
2018a.
Dougherty, A. J.: Prograded coastal barriers provide paleoenvironmental
records of storms and sea level during late Quaternary highstands, J.
Quaternary Sci., 33, 501–517, https://doi.org/10.1002/jqs.3029, 2018b.
Dougherty, A. J.: Comment on Oliver, T. S. N., Tamura, T., Hudson, J. P., and
Woodroffe, C. D. “Integrating millennial and interdecadal
[intra-/inter-annual?] shoreline changes: Morpho-sedimentary investigation of
two prograded barriers in southeastern Australia” Geomorphology, accepted,
2018c.
Dougherty, A. J., FitzGerald, D. M., and Buynevich, I. V.: Evidence for
storm-dominated early progradation of Castle Neck barrier, Massachusetts,
USA, Mar. Geol., 210, 123–134, 2004.
Dougherty, A. J., Oliver, T. S., Cowell, P. J., and Woodroffe, C. D.:
Application of a model framework for assessing risk and adaptation to climate
change on the South Coast of New South Wales, New South Wales Coastal
Conference, Kiama, Australia, 21, 1–18, available at:
http://www.coastalconference.com/papers.php (last access:
31 January 2019), 2012.
Dougherty, A. J., Choi, J.-H., and Dosseto, A.: The potential of utilising
GPR with OSL to provide insight on theoretical and practical aspects of
coastal change, New South Wales Coastal Conference, Port Stephens, Australia,
24, 1–23, available at: http://www.coastalconference.com/papers.php
(last access: 31 January 2019), 2015.
Dougherty, A. J., Choi, J.-H., and Dosseto, A.: Prograded
Barriers + GPR + OSL = Insight on Coastal Change over
Intermediate Spatial and Temporal Scales, J. Coastal Res., 75, 368–372,
https://doi.org/10.2112/si75-074.1, 2016.
Fitzgerald, D. M., Baldwin, C. T., Ibrahim, N. A., and Humphries, S. M.:
Sedimentologic and morphologic evolution of a beach ridge barrier along an
indented coast: Buzzards Bay, Massachusetts, in: Quaternary Coasts of the
United States: Marine and Lacustrine Systems, edited by: Fletcher, C. H. and
Wehmiller, J. F., SEPM Special Publication, 48, 64–75, 1992.
Goslin, J. and Clemmensen, L. B.: Proxy records of Holocene storm events in
coastal barrier systems: Storm-wave induced markers, Quaternary Sci. Rev.,
174, 80–119, 2017.
Gutierrez, R., Gibeaut, J., Smyth, R., Hepner, T., Andrews, J., Weed, C.,
Gutelius, W., and Mastin, M.: Precise airborne lidar surveying for coastal
research and geo-hazards applications, Int. Arch. Photogramm., 34, 185–194,
2001.
Harley, M., Turner, I., Short, A., and Ranasinghe, R.: A reevaluation of
coastal embayment rotation: The dominance of cross-shore versus alongshore
sediment transport processes, Collaroy-Narrabeen Beach, southeast Australia,
J. Geophys. Res.-Earth, 116, F04033, https://doi.org/10.1029/2011JF001989, 2011.
Hein, C. J., FitzGerald, D. M., Cleary, W. J., Albernaz, M. B., De Menezes,
J. T., and Klein, A. H. d. F.: Evidence for a transgressive barrier within a
regressive strandplain system: Implications for complex coastal response to
environmental change, Sedimentology, 60, 469–502, 2013.
Hein, C. J., FitzGerald, D. M., de Souza, L. H. P., Georgiou, I. Y.,
Buynevich, I. V., Klein, A. H. d. F., de Menezes, J. T., Cleary, W. J., and
Scolaro, T. L.: Complex coastal change in response to autogenic basin
infilling: An example from a sub-tropical Holocene strandplain,
Sedimentology, 63, 1362–1395, 2016.
Hijma, M. P., Shen, Z., Törnqvist, T. E., and Mauz, B.: Late Holocene
evolution of a coupled, mud-dominated delta plain-chenier plain system,
coastal Louisiana, USA, Earth Surf. Dynam., 5, 689–710,
https://doi.org/10.5194/esurf-5-689-2017, 2017.
Huntley, D. J., Godfrey-Smith, D. I., and Thewalt, M. L. W.: Optical dating
of sediments, Nature, 313, 105–107, 1985.
IPCC: Climate change 2013: the physical science basis: Working Group I
contribution to the Fifth assessment report of the Intergovernmental Panel on
Climate Change, Cambridge, UK and New York, NY, USA, 110705799X, 2013.
Jacobs, Z.: Luminescence chronologies for coastal and marine sediments,
Boreas, 37, 508–535, 2008.
Jol, H. M., Smith, D. G., and Meyers, R. A.: Digital ground penetrating radar
(GPR): A new geophysical tool for coastal barrier research (examples from the
Atlantic, Gulf and Pacific coasts, U.S.A.), J. Coastal Res., 12, 960–968,
1996.
Klemas, V. V.: Coastal and environmental remote sensing from unmanned aerial
vehicles: An overview, J. Coastal Res., 31, 1260–1267, 2015.
Leatherman, S. P.: Coastal geomorphological applications of
ground-penetrating radar, J. Coastal Res., 3, 397–399, 1987.
Lindhorst, S., Betzler, C., and Hass, H. C.: The sedimentary architecture of
a Holocene barrier spit (Sylt, German Bight): Swash-bar accretion and storm
erosion, Sediment. Geol., 206, 1–16, 2008.
Little, S., Spencer, K. L., Schuttelaars, H. M., Millward, G. E., and
Elliott, M.: Unbounded boundaries and shifting baselines: Estuaries and
coastal seas in a rapidly changing world. Estuarine, Coast. Shelf Sci., 198,
311–319, 2017.
Long, A. J., Strzelecki, M. C., Lloyd, J. M., and Bryant, C. L.: Dating High
Arctic Holocene relative sea level changes using juvenile articulated marine
shells in raised beaches, Quaternary Sci. Rev., 48, 61–66, 2012.
Mallinson, D., Burdette, K., Mahan, S., and Brook, G.: Optically stimulated
luminescence age controls on late Pleistocene and Holocene coastal
lithosomes, North Carolina, USA, Quaternary Res., 69, 97–109, 2008.
Masselink, G., Hegge, B. J., and Pattiaratchi, C. B.: Beach cusp
morphodynamics, Earth Surf. Proc. Land., 22, 1139–1155, 1997.
Morton, R. A., Paine, J. G., and Blum, M. D.: Responses of stable bay-margin
and barrier-island systems to Holocene sea-level highstands, western Gulf of
Mexico, J. Sediment. Res., 70, 478–490, 2000.
Murray-Wallace, C. V., Banerjee, D., Bourman, R. P., Olley, J. M., and
Brooke, B. P.: Optically stimulated luminescence dating of Holocene relict
foredunes, Guichen Bay, South Australia, Quaternary Sci. Rev., 21,
1077–1086, 2002.
Muru, M., Rosentau, A., Preusser, F., Plado, J., Sibul, I., Jõeleht, A.,
Bjursäter, S., Aunap, R., and Kriiska, A.: Reconstructing Holocene shore
displacement and Stone Age palaeogeography from a foredune sequence on Ruhnu
Island, Gulf of Riga, Baltic Sea, Geomorphology, 303, 434–445, 2018.
Neal, A., Richards, J., and Pye, K.: Structure and development of shell
cheniers in Essex, southeast England, investigated using high-frequency
ground-penetrating radar, Mar. Geol., 185, 435–469, 2002.
Nichol, S. L., Regnauld, H., and Goff, J. R.: Sedimentary evidence for
tsunami on the northeast coast of New Zealand/Arguments sédimentaires
attestant un tsunami sur la côte nord-est de la Nouvelle-Zélande,
Geomorphologie, 10, 35–44, 2004.
Nielsen, L., Bendixen, M., Kroon, A., Hede, M. U., Clemmensen, L. B.,
Weßling, R., and Elberling, B.: Sea-level proxies in Holocene raised
beach ridge deposits (Greenland) revealed by ground-penetrating radar, Sci.
Rep., 7, 46460, https://doi.org/10.1038/srep46460, 2017.
Nooren, K., Hoek, W. Z., Winkels, T., Huizinga, A., Van der Plicht, H., Van
Dam, R. L., Van Heteren, S., Van Bergen, M. J., Prins, M. A., Reimann, T.,
Wallinga, J., Cohen, K. M., Minderhoud, P., and Middelkoop, H.: The
Usumacinta–Grijalva beach-ridge plain in southern Mexico: a high-resolution
archive of river discharge and precipitation, Earth Surf. Dynam., 5,
529–556, https://doi.org/10.5194/esurf-5-529-2017, 2017.
Nott, J. and Hayne, M.: High frequency of “super-cyclones” along the Great
Barrier Reef over the past 5,000 years, Nature, 413, 508–512, 2001.
Oliver, T., Dougherty, A., Gliganic, L., and Woodroffe, C.: A revised
chronology for the coastal plain at Moruya, NSW: Implications for modelling
and management, New South Wales Coastal Conference, Shoalhaven, Australia,
23, 1–17, available at: http://www.coastalconference.com/papers.php
(last access: 31 January 2019), 2014.
Oliver, T. S., Dougherty, A. J., Gliganic, L. A., and Woodroffe, C. D.:
Towards more robust chronologies of coastal progradation: Optically
stimulated luminescence ages for the coastal plain at Moruya, south-eastern
Australia, Holocene, 25, 536–546, 2015.
Oliver, T. S. N., Donaldson, P., Sharples, C., Roach, M., and Woodroffe, C.
D.: Punctuated progradation of the Seven Mile Beach Holocene barrier system,
southeastern Tasmania, Mar. Geol., 386, 76–87, 2017a.
Oliver, T. S. N., Tamura, T., Hudson, J. P., and Woodroffe, C. D.:
Integrating millennial and interdecadal shoreline changes: Morpho-sedimentary
investigation of two prograded barriers in southeastern Australia,
Geomorphology, 288, 129–147, 2017b.
Pullar, W. A. and Selby, M. J.: Coastal progradation of Rangitaiki Plains,
New Zealand, Soil Bureau, Department of Scientific and Industrial Research,
1971.
Rodriguez, A. B. and Meyer, C. T.: Sea-level variation during the Holocene
deduced from the morphologic and stratigraphic evolution of Morgan Peninsula,
Alabama, USA, J. Sediment. Res., 76, 257–269, 2006.
Roy, P. S. and Thom, B. G.: Late Quaternary marine deposition in New South
Wales and southern Queensland – an evolutionary model, J. Geol. Soc. Aust.,
28, 471–489, 1981.
Scheffers, A., Engel, M., Scheffers, S., Squire, P., and Kelletat, D.: Beach
ridge systems – archives for holocene coastal events?, Prog. Phys. Geogr.,
36, 5–37, 2012.
Schofield, J.: Coastal change at Omaha and Great Barrier Island, New Zealand
J. Geol. Geophys., 28, 313–322, 1985.
Short, A. D. and Trembanis, A. C.: Decadal scale patterns in beach
oscillation and rotation Narrabeen Beach, Australia – time series, PCA and
wavelet analysis, J. Coastal Res., 20, 523–532, 2004.
Tamura, T.: Beach ridges and prograded beach deposits as palaeoenvironment
records, Earth-Sci. Rev., 114, 279–297, 2012.
Thom, B. G., Polach, H. A., and Bowman, G. M.: Holocene Age Structure of
Coastal Sand Barriers in New South Wales, Australia: By BG Thom, HA Polach
(and) GM Bowman, Royal Military College, Duntroon, 1978.
Timmons, E. A., Rodriguez, A. B., Mattheus, C. R., and DeWitt, R.: Transition
of a regressive to a transgressive barrier island due to back-barrier
erosion, increased storminess, and low sediment supply: Bogue Banks, North
Carolina, USA, Marine Geology, 278, 100–114, 2010.
Tõnisson, H., Suursaar, Ü., Kont, A., Muru, M., Rivis, R., Rosentau,
A., Tamura, T., and Vilumaa, K.: Rhythmic Patterns of Coastal Formations as
Signs of Past Climate Fluctuations on Uplifting Coasts of Estonia, the Baltic
Sea, J. Coastal Res., 85, 611–615, 2018.
van Heteren, S., FitzGerald, D. M., Barber, D. C., Kelley, J. T., and
Belknap, D. F.: Volumetric Analysis of a New England Barrier System Using
Ground-Penetrating-Radar and Coring Techniques, J. Geol., 104, 471–483,
1996.
van Heteren, S., Fitzgerald, D. M., Mckinlay, P. A., and Buynevich, I. V.:
Radar facies of paraglacial barrier systems: coastal New England, USA,
Sedimentology, 45, 181–200, 1998.
Wilmshurst, J. M., Anderson, A. J., Higham, T. F., and Worthy, T. H.: Dating
the late prehistoric dispersal of Polynesians to New Zealand using the
commensal Pacific rat, P. Natl. Acad. Sci. USA, 105, 7676–7680, 2008.
