Articles | Volume 9, issue 3
https://doi.org/10.5194/cp-9-1001-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-9-1001-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Excursions to C4 vegetation recorded in the Upper Pleistocene loess of Surduk (Northern Serbia): an organic isotope geochemistry study
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), UMR8212, CEA-CNRS-UVSQ, 91198 Gif-sur-Yvette, France
C. Gauthier
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), UMR8212, CEA-CNRS-UVSQ, 91198 Gif-sur-Yvette, France
D.-D. Rousseau
Laboratoire de Météorologie Dynamique, UMR8539, CNRS-ENS, 75231 Paris, France
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
P. Antoine
Laboratoire de Géographie Physique, CNRS-Univ. Paris 1, 92195 Meudon, France
M. Fuchs
Department of Geography, Justus-Liebig-University Giessen, 35390 Giessen, Germany
F. Lagroix
Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Univ Paris Diderot, UMR7154, CNRS, 75005 Paris, France
S. B. Marković
Chair of Physical Geography, University of Novi Sad, Novi Sad, Serbia
O. Moine
Laboratoire de Géographie Physique, CNRS-Univ. Paris 1, 92195 Meudon, France
A. Sima
Laboratoire de Météorologie Dynamique, UMR8539, CNRS-ENS, 75231 Paris, France
Related authors
Solène Quéro, Christine Hatté, Sophie Cornu, Adrien Duvivier, Nithavong Cam, Floriane Jamoteau, Daniel Borschneck, and Isabelle Basile-Doelsch
SOIL, 8, 517–539, https://doi.org/10.5194/soil-8-517-2022, https://doi.org/10.5194/soil-8-517-2022, 2022
Short summary
Short summary
Although present in food security key areas, Arenosols carbon stocks are barely studied. A 150-year-old land use change in a Mediterranean Arenosol showed a loss from 50 Gt C ha-1 to 3 Gt C ha-1 after grape cultivation. 14C showed that deep ploughing in a vineyard plot redistributed the remaining microbial carbon both vertically and horizontally. Despite the drastic degradation of the organic matter pool, Arenosols would have a high carbon storage potential, targeting the 4 per 1000 initiative.
Papa Mamadou Sitor Ndour, Christine Hatté, Wafa Achouak, Thierry Heulin, and Laurent Cournac
SOIL, 8, 49–57, https://doi.org/10.5194/soil-8-49-2022, https://doi.org/10.5194/soil-8-49-2022, 2022
Short summary
Short summary
Unravelling relationships between plant rhizosheath, root exudation and soil C dynamic may bring interesting perspectives in breeding for sustainable agriculture. Using four pearl millet lines with contrasting rhizosheaths, we found that δ13C and F14C of root-adhering soil differed from those of bulk and control soil, indicating C exudation in the rhizosphere. This C exudation varied according to the genotype, and conceptual modelling performed with data showed a genotypic effect on the RPE.
Denis-Didier Rousseau, Pierre Antoine, Niklas Boers, France Lagroix, Michael Ghil, Johanna Lomax, Markus Fuchs, Maxime Debret, Christine Hatté, Olivier Moine, Caroline Gauthier, Diana Jordanova, and Neli Jordanova
Clim. Past, 16, 713–727, https://doi.org/10.5194/cp-16-713-2020, https://doi.org/10.5194/cp-16-713-2020, 2020
Short summary
Short summary
New investigations of European loess records from MIS 6 reveal the occurrence of paleosols and horizon showing slight pedogenesis similar to those from the last climatic cycle. These units are correlated with interstadials described in various marine, continental, and ice Northern Hemisphere records. Therefore, these MIS 6 interstadials can confidently be interpreted as DO-like events of the penultimate climate cycle.
Corey R. Lawrence, Jeffrey Beem-Miller, Alison M. Hoyt, Grey Monroe, Carlos A. Sierra, Shane Stoner, Katherine Heckman, Joseph C. Blankinship, Susan E. Crow, Gavin McNicol, Susan Trumbore, Paul A. Levine, Olga Vindušková, Katherine Todd-Brown, Craig Rasmussen, Caitlin E. Hicks Pries, Christina Schädel, Karis McFarlane, Sebastian Doetterl, Christine Hatté, Yujie He, Claire Treat, Jennifer W. Harden, Margaret S. Torn, Cristian Estop-Aragonés, Asmeret Asefaw Berhe, Marco Keiluweit, Ágatha Della Rosa Kuhnen, Erika Marin-Spiotta, Alain F. Plante, Aaron Thompson, Zheng Shi, Joshua P. Schimel, Lydia J. S. Vaughn, Sophie F. von Fromm, and Rota Wagai
Earth Syst. Sci. Data, 12, 61–76, https://doi.org/10.5194/essd-12-61-2020, https://doi.org/10.5194/essd-12-61-2020, 2020
Short summary
Short summary
The International Soil Radiocarbon Database (ISRaD) is an an open-source archive of soil data focused on datasets including radiocarbon measurements. ISRaD includes data from bulk or
whole soils, distinct soil carbon pools isolated in the laboratory by a variety of soil fractionation methods, samples of soil gas or water collected interstitially from within an intact soil profile, CO2 gas isolated from laboratory soil incubations, and fluxes collected in situ from a soil surface.
Marwa Tifafi, Marta Camino-Serrano, Christine Hatté, Hector Morras, Lucas Moretti, Sebastián Barbaro, Sophie Cornu, and Bertrand Guenet
Geosci. Model Dev., 11, 4711–4726, https://doi.org/10.5194/gmd-11-4711-2018, https://doi.org/10.5194/gmd-11-4711-2018, 2018
Short summary
Short summary
The role of soil carbon in climate dynamics becomes one of the major uncertainties in land surface models. This work is a presentation of a new version of the land surface model called ORCHIDEE incorporating the radiocarbon (14C) used as integrator of the soil carbon dynamics. It has been possible to highlight an underestimation of the age of carbon in the soil and that model improvements should focus more on a depth-dependent parameterization mainly for the diffusion.
Alexia Paul, Christine Hatté, Lucie Pastor, Yves Thiry, Françoise Siclet, and Jérôme Balesdent
Biogeosciences, 13, 6587–6598, https://doi.org/10.5194/bg-13-6587-2016, https://doi.org/10.5194/bg-13-6587-2016, 2016
Short summary
Short summary
The terrestrial environment has been affected by tritium contamination. There is a need to assess the dynamics of organic hydrogen in soils in order to predict the fate of tritium. In the present study we traced carbon and hydrogen from plant-derived molecules and hydrogen from water in different soil types. The main findings of the work are that water is the main donor of organic hydrogen and the long-term fate of hydrogen (and tritium) will depend on the status of soil carbon dynamics.
É. Boucher, J. Guiot, C. Hatté, V. Daux, P.-A. Danis, and P. Dussouillez
Biogeosciences, 11, 3245–3258, https://doi.org/10.5194/bg-11-3245-2014, https://doi.org/10.5194/bg-11-3245-2014, 2014
D.-D. Rousseau, M. Ghil, G. Kukla, A. Sima, P. Antoine, M. Fuchs, C. Hatté, F. Lagroix, M. Debret, and O. Moine
Clim. Past, 9, 2213–2230, https://doi.org/10.5194/cp-9-2213-2013, https://doi.org/10.5194/cp-9-2213-2013, 2013
A. Sima, M. Kageyama, D.-D. Rousseau, G. Ramstein, Y. Balkanski, P. Antoine, and C. Hatté
Clim. Past, 9, 1385–1402, https://doi.org/10.5194/cp-9-1385-2013, https://doi.org/10.5194/cp-9-1385-2013, 2013
Susana Barbosa, Maria Eduarda Silva, and Denis-Didier Rousseau
Nonlin. Processes Geophys., 31, 433–447, https://doi.org/10.5194/npg-31-433-2024, https://doi.org/10.5194/npg-31-433-2024, 2024
Short summary
Short summary
The characterisation of abrupt transitions in palaeoclimate records allows understanding of millennial climate variability and potential tipping points in the context of current climate change. In our study an algorithmic method, the matrix profile, is employed to characterise abrupt warmings designated as Dansgaard–Oeschger (DO) events and to identify the most similar transitions in the palaeoclimate time series.
Mathias Vinnepand, Peter Fischer, Ulrich Hambach, Olaf Jöris, Carol-Ann Craig, Christian Zeeden, Barry Thornton, Thomas Tütken, Charlotte Prud'homme, Philipp Schulte, Olivier Moine, Kathryn E. Fitzsimmons, Christian Laag, Frank Lehmkuhl, Wolfgang Schirmer, and Andreas Vött
E&G Quaternary Sci. J., 72, 163–184, https://doi.org/10.5194/egqsj-72-163-2023, https://doi.org/10.5194/egqsj-72-163-2023, 2023
Short summary
Short summary
Loess–palaeosol sequences (LPSs) represent continental and non-aquatic archives providing detailed information on Quaternary environmental and climate changes. We present an integrative approach combining sedimentological, rock magnetic, and bulk geochemical data, as well as information on Sr and Nd isotope composition. The approach adds to a comprehensive understanding of LPS formation including changes in dust composition and associated circulation patterns during Quaternary climate changes.
Solène Quéro, Christine Hatté, Sophie Cornu, Adrien Duvivier, Nithavong Cam, Floriane Jamoteau, Daniel Borschneck, and Isabelle Basile-Doelsch
SOIL, 8, 517–539, https://doi.org/10.5194/soil-8-517-2022, https://doi.org/10.5194/soil-8-517-2022, 2022
Short summary
Short summary
Although present in food security key areas, Arenosols carbon stocks are barely studied. A 150-year-old land use change in a Mediterranean Arenosol showed a loss from 50 Gt C ha-1 to 3 Gt C ha-1 after grape cultivation. 14C showed that deep ploughing in a vineyard plot redistributed the remaining microbial carbon both vertically and horizontally. Despite the drastic degradation of the organic matter pool, Arenosols would have a high carbon storage potential, targeting the 4 per 1000 initiative.
Ludwig Zöller, Manfred Fischer, Zdzisław Jary, Pierre Antoine, and Marcin Krawczyk
E&G Quaternary Sci. J., 71, 59–81, https://doi.org/10.5194/egqsj-71-59-2022, https://doi.org/10.5194/egqsj-71-59-2022, 2022
Short summary
Short summary
Comparing quartz optically stimulated luminescence (OSL) and fine-grain post-infrared infrared stimulated luminescence (pIRIR) ages, agreement was largely found, e.g. the bracketing of the L1SS1 pedocomplex to ca. 30–40 ka. Nevertheless some age differences between the Bayreuth (OSL) and the Gliwice (pIRIR) data invite further discussion. Exact dating using various protocols and grain sizes remains challenging, in particular for a periglacial environment with strong heterogeneity of material.
Denis-Didier Rousseau, Witold Bagniewski, and Michael Ghil
Clim. Past, 18, 249–271, https://doi.org/10.5194/cp-18-249-2022, https://doi.org/10.5194/cp-18-249-2022, 2022
Short summary
Short summary
The study of abrupt climate changes is a relatively new field of research that addresses paleoclimate variations that occur in intervals of tens to hundreds of years. Such timescales are much shorter than the tens to hundreds of thousands of years that the astronomical theory of climate addresses. We revisit several high-resolution proxy records of the past 3.2 Myr and show that the abrupt climate changes are nevertheless affected by the orbitally induced insolation changes.
Papa Mamadou Sitor Ndour, Christine Hatté, Wafa Achouak, Thierry Heulin, and Laurent Cournac
SOIL, 8, 49–57, https://doi.org/10.5194/soil-8-49-2022, https://doi.org/10.5194/soil-8-49-2022, 2022
Short summary
Short summary
Unravelling relationships between plant rhizosheath, root exudation and soil C dynamic may bring interesting perspectives in breeding for sustainable agriculture. Using four pearl millet lines with contrasting rhizosheaths, we found that δ13C and F14C of root-adhering soil differed from those of bulk and control soil, indicating C exudation in the rhizosphere. This C exudation varied according to the genotype, and conceptual modelling performed with data showed a genotypic effect on the RPE.
Thomas Kolb, Konrad Tudyka, Annette Kadereit, Johanna Lomax, Grzegorz Poręba, Anja Zander, Lars Zipf, and Markus Fuchs
Geochronology, 4, 1–31, https://doi.org/10.5194/gchron-4-1-2022, https://doi.org/10.5194/gchron-4-1-2022, 2022
Short summary
Short summary
The µDose system is an innovative analytical instrument developed for the cost- and time-efficient determination of environmental radionuclide concentrations required for the calculation of sedimentation ages in palaeo-environmental and geo-archaeological research. The results of our study suggest that accuracy and precision of µDose measurements are comparable to those of well-established methods and that the new approach shows the potential to become a standard tool in environmental dosimetry.
Dominik Faust and Markus Fuchs
E&G Quaternary Sci. J., 70, 243–246, https://doi.org/10.5194/egqsj-70-243-2021, https://doi.org/10.5194/egqsj-70-243-2021, 2021
Denis-Didier Rousseau
E&G Quaternary Sci. J., 70, 229–233, https://doi.org/10.5194/egqsj-70-229-2021, https://doi.org/10.5194/egqsj-70-229-2021, 2021
Short summary
Short summary
A year after his doctoral thesis, Ložek chose to share with the international community not only his vision but also the one that the Czechoslovakian researchers working on loess deposits had at that time, through a paper published in the well-established E&G journal. It represented a detailed and complete state of the art of loess and mollusc studies at that time, an extraordinarily synthetic review that still yields a modern flavor as many of the points made remain relevant today.
Frank Preusser, Markus Fuchs, and Christine Thiel
E&G Quaternary Sci. J., 70, 201–203, https://doi.org/10.5194/egqsj-70-201-2021, https://doi.org/10.5194/egqsj-70-201-2021, 2021
Frank Preusser, Markus Fuchs, and Christine Thiel
DEUQUA Spec. Pub., 3, 1–3, https://doi.org/10.5194/deuquasp-3-1-2021, https://doi.org/10.5194/deuquasp-3-1-2021, 2021
Kim H. Stadelmaier, Patrick Ludwig, Pascal Bertran, Pierre Antoine, Xiaoxu Shi, Gerrit Lohmann, and Joaquim G. Pinto
Clim. Past, 17, 2559–2576, https://doi.org/10.5194/cp-17-2559-2021, https://doi.org/10.5194/cp-17-2559-2021, 2021
Short summary
Short summary
We use regional climate simulations for the Last Glacial Maximum to reconstruct permafrost and to identify areas of thermal contraction cracking of the ground in western Europe. We find ground cracking, a precondition for the development of permafrost proxies, south of the probable permafrost border, implying that permafrost was not the limiting factor for proxy development. A good agreement with permafrost and climate proxy data is achieved when easterly winds are modelled more frequently.
Sascha Scherer, Benjamin Höpfer, Katleen Deckers, Elske Fischer, Markus Fuchs, Ellen Kandeler, Jutta Lechterbeck, Eva Lehndorff, Johanna Lomax, Sven Marhan, Elena Marinova, Julia Meister, Christian Poll, Humay Rahimova, Manfred Rösch, Kristen Wroth, Julia Zastrow, Thomas Knopf, Thomas Scholten, and Peter Kühn
SOIL, 7, 269–304, https://doi.org/10.5194/soil-7-269-2021, https://doi.org/10.5194/soil-7-269-2021, 2021
Short summary
Short summary
This paper aims to reconstruct Middle Bronze Age (MBA) land use practices in the northwestern Alpine foreland (SW Germany, Hegau). We used a multi-proxy approach including biogeochemical proxies from colluvial deposits in the surroundings of a MBA settlement, on-site archaeobotanical and zooarchaeological data and off-site pollen data. From our data we infer land use practices such as plowing, cereal growth, forest farming and use of fire that marked the beginning of major colluvial deposition.
Denis-Didier Rousseau, Pierre Antoine, Niklas Boers, France Lagroix, Michael Ghil, Johanna Lomax, Markus Fuchs, Maxime Debret, Christine Hatté, Olivier Moine, Caroline Gauthier, Diana Jordanova, and Neli Jordanova
Clim. Past, 16, 713–727, https://doi.org/10.5194/cp-16-713-2020, https://doi.org/10.5194/cp-16-713-2020, 2020
Short summary
Short summary
New investigations of European loess records from MIS 6 reveal the occurrence of paleosols and horizon showing slight pedogenesis similar to those from the last climatic cycle. These units are correlated with interstadials described in various marine, continental, and ice Northern Hemisphere records. Therefore, these MIS 6 interstadials can confidently be interpreted as DO-like events of the penultimate climate cycle.
Zhongshi Zhang, Qing Yan, Ran Zhang, Florence Colleoni, Gilles Ramstein, Gaowen Dai, Martin Jakobsson, Matt O'Regan, Stefan Liess, Denis-Didier Rousseau, Naiqing Wu, Elizabeth J. Farmer, Camille Contoux, Chuncheng Guo, Ning Tan, and Zhengtang Guo
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-38, https://doi.org/10.5194/cp-2020-38, 2020
Manuscript not accepted for further review
Short summary
Short summary
Whether an ice sheet once grew over Northeast Siberia-Beringia has been debated for decades. By comparing climate modelling with paleoclimate and glacial records from around the North Pacific, this study shows that the Laurentide-Eurasia-only ice sheet configuration fails in explaining these records, while a scenario involving the ice sheet over Northeast Siberia-Beringia succeeds. It highlights the complexity in glacial climates and urges new investigations across Northeast Siberia-Beringia.
Christopher Lüthgens, Daniela Sauer, Michael Zech, Becky Briant, Eleanor Brown, Elisabeth Dietze, Markus Fuchs, Nicole Klasen, Sven Lukas, Jan-Hendrik May, Julia Meister, Tony Reimann, Gilles Rixhon, Zsófia Ruszkiczay-Rüdiger, Bernhard Salcher, Tobias Sprafke, Ingmar Unkel, Hans von Suchodoletz, and Christian Zeeden
E&G Quaternary Sci. J., 68, 243–244, https://doi.org/10.5194/egqsj-68-243-2020, https://doi.org/10.5194/egqsj-68-243-2020, 2020
Johanna Lomax, Thomas Kolb, and Markus Fuchs
E&G Quaternary Sci. J., 68, 241–242, https://doi.org/10.5194/egqsj-68-241-2020, https://doi.org/10.5194/egqsj-68-241-2020, 2020
Corey R. Lawrence, Jeffrey Beem-Miller, Alison M. Hoyt, Grey Monroe, Carlos A. Sierra, Shane Stoner, Katherine Heckman, Joseph C. Blankinship, Susan E. Crow, Gavin McNicol, Susan Trumbore, Paul A. Levine, Olga Vindušková, Katherine Todd-Brown, Craig Rasmussen, Caitlin E. Hicks Pries, Christina Schädel, Karis McFarlane, Sebastian Doetterl, Christine Hatté, Yujie He, Claire Treat, Jennifer W. Harden, Margaret S. Torn, Cristian Estop-Aragonés, Asmeret Asefaw Berhe, Marco Keiluweit, Ágatha Della Rosa Kuhnen, Erika Marin-Spiotta, Alain F. Plante, Aaron Thompson, Zheng Shi, Joshua P. Schimel, Lydia J. S. Vaughn, Sophie F. von Fromm, and Rota Wagai
Earth Syst. Sci. Data, 12, 61–76, https://doi.org/10.5194/essd-12-61-2020, https://doi.org/10.5194/essd-12-61-2020, 2020
Short summary
Short summary
The International Soil Radiocarbon Database (ISRaD) is an an open-source archive of soil data focused on datasets including radiocarbon measurements. ISRaD includes data from bulk or
whole soils, distinct soil carbon pools isolated in the laboratory by a variety of soil fractionation methods, samples of soil gas or water collected interstitially from within an intact soil profile, CO2 gas isolated from laboratory soil incubations, and fluxes collected in situ from a soil surface.
Jan Johannes Miera, Jessica Henkner, Karsten Schmidt, Markus Fuchs, Thomas Scholten, Peter Kühn, and Thomas Knopf
E&G Quaternary Sci. J., 68, 75–93, https://doi.org/10.5194/egqsj-68-75-2019, https://doi.org/10.5194/egqsj-68-75-2019, 2019
Short summary
Short summary
This study investigates Neolithic settlement dynamics by combining archaeological source criticism and archaeopedological data from colluvial deposits. It is shown that the distribution of Neolithic sites in the Baar region is distorted by superimposition due to erosion. Furthermore, the preservation conditions for pottery are limited by weathering effects. By complementing archaeological data with phases of colluviation we are able to point out settlement dynamics throughout the Neolithic.
Marwa Tifafi, Marta Camino-Serrano, Christine Hatté, Hector Morras, Lucas Moretti, Sebastián Barbaro, Sophie Cornu, and Bertrand Guenet
Geosci. Model Dev., 11, 4711–4726, https://doi.org/10.5194/gmd-11-4711-2018, https://doi.org/10.5194/gmd-11-4711-2018, 2018
Short summary
Short summary
The role of soil carbon in climate dynamics becomes one of the major uncertainties in land surface models. This work is a presentation of a new version of the land surface model called ORCHIDEE incorporating the radiocarbon (14C) used as integrator of the soil carbon dynamics. It has been possible to highlight an underestimation of the age of carbon in the soil and that model improvements should focus more on a depth-dependent parameterization mainly for the diffusion.
Markus Fuchs
DEUQUA Spec. Pub., 1, 1–2, https://doi.org/10.5194/deuquasp-1-1-2018, https://doi.org/10.5194/deuquasp-1-1-2018, 2018
Johanna Lomax, Raphael Steup, Lyudmila Shumilovskikh, Christian Hoselmann, Daniela Sauer, Veit van Diedenhoven, and Markus Fuchs
DEUQUA Spec. Pub., 1, 15–28, https://doi.org/10.5194/deuquasp-1-15-2018, https://doi.org/10.5194/deuquasp-1-15-2018, 2018
Niklas Boers, Mickael D. Chekroun, Honghu Liu, Dmitri Kondrashov, Denis-Didier Rousseau, Anders Svensson, Matthias Bigler, and Michael Ghil
Earth Syst. Dynam., 8, 1171–1190, https://doi.org/10.5194/esd-8-1171-2017, https://doi.org/10.5194/esd-8-1171-2017, 2017
Short summary
Short summary
We use a Bayesian approach for inferring inverse, stochastic–dynamic models from northern Greenland (NGRIP) oxygen and dust records of subdecadal resolution for the interval 59 to 22 ka b2k. Our model reproduces the statistical and dynamical characteristics of the records, including the Dansgaard–Oeschger variability, with no need for external forcing. The crucial ingredients are cubic drift terms, nonlinear coupling terms between the oxygen and dust time series, and non-Markovian contributions.
Denis-Didier Rousseau, Anders Svensson, Matthias Bigler, Adriana Sima, Jorgen Peder Steffensen, and Niklas Boers
Clim. Past, 13, 1181–1197, https://doi.org/10.5194/cp-13-1181-2017, https://doi.org/10.5194/cp-13-1181-2017, 2017
Short summary
Short summary
We show that the analysis of δ18O and dust in the Greenland ice cores, and a critical study of their source variations, reconciles these records with those observed on the Eurasian continent. We demonstrate the link between European and Chinese loess sequences, dust records in Greenland, and variations in the North Atlantic sea ice extent. The sources of the emitted and transported dust material are variable and relate to different environments.
Alexia Paul, Christine Hatté, Lucie Pastor, Yves Thiry, Françoise Siclet, and Jérôme Balesdent
Biogeosciences, 13, 6587–6598, https://doi.org/10.5194/bg-13-6587-2016, https://doi.org/10.5194/bg-13-6587-2016, 2016
Short summary
Short summary
The terrestrial environment has been affected by tritium contamination. There is a need to assess the dynamics of organic hydrogen in soils in order to predict the fate of tritium. In the present study we traced carbon and hydrogen from plant-derived molecules and hydrogen from water in different soil types. The main findings of the work are that water is the main donor of organic hydrogen and the long-term fate of hydrogen (and tritium) will depend on the status of soil carbon dynamics.
É. Boucher, J. Guiot, C. Hatté, V. Daux, P.-A. Danis, and P. Dussouillez
Biogeosciences, 11, 3245–3258, https://doi.org/10.5194/bg-11-3245-2014, https://doi.org/10.5194/bg-11-3245-2014, 2014
D.-D. Rousseau, M. Ghil, G. Kukla, A. Sima, P. Antoine, M. Fuchs, C. Hatté, F. Lagroix, M. Debret, and O. Moine
Clim. Past, 9, 2213–2230, https://doi.org/10.5194/cp-9-2213-2013, https://doi.org/10.5194/cp-9-2213-2013, 2013
A. Sima, M. Kageyama, D.-D. Rousseau, G. Ramstein, Y. Balkanski, P. Antoine, and C. Hatté
Clim. Past, 9, 1385–1402, https://doi.org/10.5194/cp-9-1385-2013, https://doi.org/10.5194/cp-9-1385-2013, 2013
J. Dabkowski, J. Andrews, P. Antoine, and A. Marca-Bell
Clim. Past Discuss., https://doi.org/10.5194/cpd-9-1657-2013, https://doi.org/10.5194/cpd-9-1657-2013, 2013
Revised manuscript not accepted
Related subject area
Subject: Continental Surface Processes | Archive: Terrestrial Archives | Timescale: Millenial/D-O
Reconstructing Younger Dryas ground temperature and snow thickness from cave deposits
Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ18O and δ2H values
Eurasian contribution to the last glacial dust cycle: how are loess sequences built?
Paul Töchterle, Anna Baldo, Julian B. Murton, Frederik Schenk, R. Lawrence Edwards, Gabriella Koltai, and Gina E. Moseley
Clim. Past, 20, 1521–1535, https://doi.org/10.5194/cp-20-1521-2024, https://doi.org/10.5194/cp-20-1521-2024, 2024
Short summary
Short summary
We present a reconstruction of permafrost and snow cover on the British Isles for the Younger Dryas period, a time of extremely cold winters that happened approximately 12 000 years ago. Our results indicate that seasonal sea ice in the North Atlantic was most likely a crucial factor to explain the observed climate shifts during this time.
Sophie F. Warken, Therese Weißbach, Tobias Kluge, Hubert Vonhof, Denis Scholz, Rolf Vieten, Martina Schmidt, Amos Winter, and Norbert Frank
Clim. Past, 18, 167–181, https://doi.org/10.5194/cp-18-167-2022, https://doi.org/10.5194/cp-18-167-2022, 2022
Short summary
Short summary
The analysis of fluid inclusions from a Puerto Rican speleothem provides quantitative information about past rainfall conditions and temperatures during the Last Glacial Period, when the climate was extremely variable. Our data show that the region experienced a climate that was generally colder and drier. However, we also reconstruct intervals when temperatures reached nearly modern values, and convective activity was comparable to or only slightly weaker than the present day.
Denis-Didier Rousseau, Anders Svensson, Matthias Bigler, Adriana Sima, Jorgen Peder Steffensen, and Niklas Boers
Clim. Past, 13, 1181–1197, https://doi.org/10.5194/cp-13-1181-2017, https://doi.org/10.5194/cp-13-1181-2017, 2017
Short summary
Short summary
We show that the analysis of δ18O and dust in the Greenland ice cores, and a critical study of their source variations, reconciles these records with those observed on the Eurasian continent. We demonstrate the link between European and Chinese loess sequences, dust records in Greenland, and variations in the North Atlantic sea ice extent. The sources of the emitted and transported dust material are variable and relate to different environments.
Cited articles
Antoine, P., Rousseau, D.-D., Fuchs, M., Hatté, C., Gauthier, C., Marković, S. B., Jovanović, M., Gaudenyi, T., Moine, O., and Rossignol, J.: High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia), Quaternary Int., 198, 19–36, https://doi.org/10.1016/j.quaint.2008.12.008, 2009a.
Antoine, P., Rousseau, D.-D., Moine, O., Kunesch, S., Hatté, C., Lang, A., and Zöller, L.: Rapid and cyclic aeolian deposition during the Last Glacial in European loess : a high-resolution records from Nussloch, Germany, Quaternary Sci. Rev., 28, 2955–2973, 2009b.
Austin, M. P.: Continuum concept, ordination methods, and niche theory, Annu. Rev. Ecol. Syst., 16, 39–61, 1985.
Bartov, Y., Goldstein, S. L., Stein, M., and Enzel, Y.: Catastrophic arid episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich events, Geology, 31, 439–442, 2003.
Buggle, B., Glaser, B., Zöller, L., Hambach, U., Markovic, S. B., Glaser, I., and Gerasimenko, N.: Geochemical characterization and origin of Southeastern and Eastern European loesses (Serbia, Romania, Ukraine), Quaternary Sci. Rev., 27, 1058–1075, 2008.
Cowling, S. A. and Sykes, M. T.: Physiological significance of low atmospheric CO2 for plant-climate interactions, Quaternary Res., 52, 237–242, 1999.
Deines, P.: The isotopic composition of reduced organic carbon, in: Hand book of environmental isotope geochemistry, edited by: Fritz, P. and Fontes, J.-C., Elsevier, Amsterdam, 329–406, 1980.
Derbyshire, E. and Mellors, T. W.: Geological and geotechnical characteristics of some loess and loessic soils from China and Britain: a comparison, Eng. Geol., 25, 135–175, 1988.
Farquhar, G. D.: Carbon dioxide and vegetation, Science, 278, 1411–1411, 1997.
Farquhar, G. D., O'Leary, M. H., and Berry, J. A.: On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves, Aust. J. Plant Physiol., 9, 121–137, 1982.
Farquhar, G. D., Ehleringer, J. R. R., and Hubick, K. T.: Carbon isotope discrimination and photosynthesis, Annu. Rev. Plant Phys., 40, 503–537, 1989.
Finke, P. A.: Modeling the genesis of luvisols as a function of topographic position in loess parent material, Quaternary Int., 265, 3–17, 2012.
Finke, P. A. and Hutson, J. L.: Modelling soil genesis in calcareous loess, Geoderma, 145, 462–479, 2008.
Florineth, D. and Schlüchter, C.: Alpine evidence for atmospheric circulation patterns in Europe during the Last Glacial Maximum, Quaternary Res., 54, 295–308, 2000.
Frank, C.: Plio-pleistozäne and holozäne Mollusken Österreichs, Verlad der Österreichschen Akademie der Wissenschaften, Wien, 2006.
Fuchs, M., Rousseau, D.-D., Antoine, P., Hatté, C., Gauthier, C., Marković, S. B., and Zöller, L.: Chronology of the Last Climatic Cycle (Upper Pleistocene) of the Surduk loess sequence, Vojvodina, Serbia, Boreas, 37, 66–73, https://doi.org/10.1111/j.1502-3885.2007.00012.x, 2008.
Fuchs, M., Kreutzer, S., Rousseau, D.-D., Antoine, P., Hatté, C., Lagroix, F., Moine, O., Gauthier, C., Svoboda, J., and Lisa, L.: The loess sequence of Dolni Vestonice, Czech Republic: A new OSL based chronology of the Last Climatic Cycle, Boreas, online first, https://doi.org/10.1111/j.1502-3885.2012.00299.x, 2012.
Galović, L., Frechen, M., Halamić, J., Durn, G., and Romić, M.: Loess chronostratigraphy in Eastern Croatia – A luminescence dating approach, Quaternary Int., 198, 85–97, 2009.
Gauthier, C. and Hatté, C.: Effects of handling, storage, and chemical treatments on delta C-13 values of terrestrial fossil organic matter, Geophy. Geochem. Geosys., 9, Q08011, https://doi.org/10.1029/2008gc001967, 2008.
Gocke, M., Kuzyakov, Y., and Wiesenberg, G. L. B.: Rhizoliths in loess – evidence for post-sedimentary incorporation of root-derived organic matter in terrestrial sediments as assessed from molecular proxies, Org. Geochem., 41, 1198–1206, 2010.
Guo, Z. T., Ruddiman, W. F., Hao, Q. Z., Wu, H. B., Qiao, Y. S., Zhu, R. X., Peng, S. Z., Wei, J. J., Yuan, B. Y., and Liu, T. S.: Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China, Nature, 416, 159–163, 2002.
Hatté, C.: Les isotopes du Carbone (14C et 13C) dans la matière organique des loess de l'Europe du Nord-Ouest: applications paléoclimatiques, Ph-D, Geology department, Paris XI, Orsay, 2000.
Hatté, C. and Guiot, J.: Palaeoprecipitation reconstruction by inverse modelling using the isotopic signal of loess organic matter: application to the Nussloch loess sequence (Rhine Valley, Germany), Clim. Dynam., 25, 315–327, 2005.
Hatté, C., Fontugne, M. R., Rousseau, D.-D., Antoine, P., and Tisnérat-Laborde, N.: δ13C variations of loess organic matter as a record of the vegetation response to climatic changes during the Weichselian, Geology, 26, 583–586, 1998.
Hatté, C., Antoine, P., Fontugne, M. R., Lang, A., Rousseau, D.-D., and Zöller, L.: δ13C variation of loess organic matter as a potential proxy for paleoprecipitation, Quaternary Res., 55, 33–38, 2001a.
Hatté, C., Morvan, J., Noury, C., and Paterne, M.: Is classical Acid-Alkali-Acid treatment responsible for contamination? An alternative proposition, Radiocarbon, 43, 177–182, 2001b.
Hatté, C., Pessenda, L. C. R., Lang, A., and Paterne, M.: Development of an accurate and reliable 14C chronology for loess sequences. Application to the loess sequence of Nu{ß}loch (Rhine valley, Germany), Radiocarbon, 43, 611–618, 2001c.
Hatté, C., Rousseau, D.-D., and Guiot, J.: Climate reconstruction from pollen and δ13C records using inverse vegetation modeling – Implication for past and future climates, Clim. Past, 5, 147–156, https://doi.org/10.5194/cp-5-147-2009, 2009.
Josey, S. A., Somot, S., and Tsimplis, M.: Impacts of atmospheric modes of variability on Mediterranean Sea surface heat exchange, J. Geophys. Res., 116, C02032, https://doi.org/10.1029/2010JC006685, 2011.
Jost, A., Lunt, D., Kageyama, M., Abe-Ouchi, A., Peyron, O., Valdes, P. J., and Ramstein, G.: High-resolution simulations of the last glacial maximum climate over Europe: a solution to discrepancies with continental palaeclimatic reconstructions?, Clim. Dynam., 24, 577–590, https://doi.org/10.1007/s00382-005-0009-4, 2005.
Jovanović, M.: Paleoenvironmental record of loess-paleosol sequences in surrounding of Požarevac city, NE Serbia, Master, Faculty of Sciences, Novi Sad University, Novi Sad, Serbia, 2005 (in Serbian with English summary).
Jovanović, M., Marković, S., Gaudenyi, T., Oches, E. A., Hambach, U., Zöller, L., and Machalett, B.: "Warm" glacial climate during loess deposition recorded at exposures of the Požarevac brickyard, NE Serbia, Geophys. Res. Abstr., EGU06-A-10599, EGU General Assembly 2006, Vienna, Austria, 2006.
Klein Tank, A. M. G., Wijngaard, J. B., Können, G. P., Böhm, R., Demarée, G., Gocheva, A., Mileta, M., Pashiardis, S., Hejkrlik, L., Kern-Hansen, C., Heino, R., Bessemoulin, P., Müller-Westermeier, G., Tzanakou, M., Szalai, S., Palsdottir, T., Fitzgerald, D., Rubin, S., Capaldo, M., Maugeri, M., Leitass, A., Bukantis, A., Aberfeld, R., van Engelen, A. F. V., Forland, E., Mietus, M., Coelho, F., Mares, C., Razuvaev, V., Nieplova, E., Cegnar, T., Anonio Lopez, J., Dahlström, B., Moberg, A., Kirchhofer, W., Ceylan, A., Pachaliuk, O., Alexander, L. V., and Petrovic, P.: Daily dataset of 20th century surface air temperature and precipitation series for European Climate Assessment, Int. J. Climatol., 22, 1441–1453, 2002.
Krichak, S. O. and Alpert, P.: Signatures of the NAO in the atmospheric circulation during wet winter months over the Mediterranean region, Theor. Appl. Clim., 82, 27–39, 2005.
Kühlemann, J., Rohling, E. J., Krumrei, I., Kubik, P., Ivy-Ochs, S., and Kucera, M.: Regional synthesis of Mediterranean atmospheric circulation during the Last Glacial Maximum, Science, 321, 1338–1340, 2008.
Kühlemann, J., Milivojevic, M., Krumrei, I., and Kubik, P. W.: Last glaciation of the Sara Range (Balkan Peninsula): Increasing dryness from the LGM to the Holocene, Aust. J. Earth Sci., 102, 146–158, 2009.
Kukla, G. J.: Pleistocene land-sea correlations: 1. Europe, Earth-Sci. Rev., 13, 307–374, 1977.
Lautridou, J.-P.: Le Cycle Périglaciaire Pléistocène en Europe du Nord-Ouest et plus particulièrement en Normandie, Centre de Géomorphologie, Caen, Caen, 908 pp., 1985.
Leng, M. J., Wagner, B., Boehm, A., Panagiotopoulos, K., Vane, C. H., Snelling, A., Haidon, C., Woodley, E., Vogel, H., Zanchetta, G., and Baneschi, I.: Understanding past climatic and hydrological variability in the Mediterranean from Lake Prespa sediment isotope and geochemical record over the Last Glacial cycle, Quaternary Sci. Rev., 66, 123–136, https://doi.org/10.1016/j.quascirev.2012.07.015, 2012.
Lézine, A.-M., von Grafenstein, U., Andersen, N., Belmecheri, S., Bordon, A., Caron, B., Cazet, J.-P., Erlernkeuser, 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.
Lloyd, J. and Farquhar, G. D.: 13C discrimination during CO2 assimilation by the terrestrial biosphere, Oecologia, 99, 201–215, 1994.
Ložek, V.: Quatärmollusken des Tschechoslowakei, Rozpravy \'{U}středního ústavu geologického, Rozpravy \'{U}středního ústavu geologického, Nakladatelství ČSAV Praha sv. 31, 374 pp., 1964.
Marković, S. B., Oches, E. A., Jovanović, M., Gaudenyi, T., Hambach, U., Zöller, L., and Sümegi, P.: Paleoclimate record in the Late Pleistocene loess-paleosol sequence at Mišeluk (Vojvodina, Serbia), Quaternaire, 15, 361–368, 2004.
Marković, S. B., McCoy, W. D., Oches, E. A., Savic, S., Gaudenyi, T., Jovanović, M., Stevens, T., Walther, R., Ivanisevic, P., and Galic, Z.: Paleoclimate record in the Upper Pleistocene loess-paleosol sequence at Petrovaradin brickyard (Vojvodina, Serbia), Geol. Carpath., 56, 545–552, 2005.
Marković, S. B., Oches, E. A., Sümegi, P., Jovanović, M., and Gaudenyi, T.: An introduction to the Middle and Upper Pleistocene loess-paleosol sequence at Ruma brickyard, Vojvodina, Serbia, Quaternary Int., 149, 80–86, 2006.
Marković, S. B., Oches, E. A., McCoy, W. D., Frechen, M., and Gaudenyi, T.: Malacological and sedimentological evidence for "warm" glacial climate from the Irig loess sequence, Vojvodina, Serbia, Geochem. Geophy. Geosys., 8, Q09008, https://doi.org/10.1029/2006GC001565, 2007.
Marković, S. B., Bokhorst, M. P., Vandenberghe, J., McCoy, W. D., Oches, E. A., Hambach, U., Gaudenyi, T., Jovanović, M., Zöller, L., Stevens, T., and Machalett, B.: Late Pleistocene loess-paleosol sequences in the Vijvodina Region, north Serbia, J. Quaternary Sci., 23, 73–84, 2008.
Mitrović, B.: Pleistocene malacofauna of Požarevac Danube Area (NE Serbia), Geološki Anali Balkanskoga Poluostrva, 68, 81–89, 2007.
Moine, O., Rousseau, D.-D., and Antoine, P.: Terrestrial molluscan records of Weichselian Lower to Middle Pleniglacial climatic changes from the Nussloch loess series (Rhine Valley, Germany): the impact of local factors, Boreas, 34, 363–380, 2005.
Moine, O., Rousseau, D.-D., and Antoine, P.: The impact of Dansgaard-Oeschger cycles on the loessic environment and malacofauna of Nussloch (Germany) during the Upper Weichselian, Quaternary Res., 70, 91–104, 2008.
Moine, O., Antoine, P., Deschodt, L., and Sellier-Segard, N.: High resolution molluscan records in Upper Weichselian loess and tundra gleys: first examples from Northern France, Quaternaire, 22, 307–325, 2011.
O'Leary, M. H.: Carbon isotope fractionation in plants, Phytochemistry, 20, 553–567, 1981.
Paruelo, J. M. and Lauenroth, W. K.: Relative abundance of plant functional types in grasslands and shrublands of North America, Ecol. Appl., 6, 1212–1224, 1996.
Peyron, O., Guiot, J., Cheddadi, R., Tarasov, P., Reille, M., de Beaulieu, J.-L., Bottema, S., and Andrieu, V.: Climatic reconstruction in Europe for 18,000 yr B.P. from pollen data, Quaternary Res., 49, 183–196, 1998.
Polley, W. H., Johnson, H. B., Marino, B. D., and Mayeux, H. S.: Increase in C3-plant water-use efficiency and biomass over glacial to present CO2 concentrations, Nature, 361, 61–64, 1993.
Pustovoytov, K. and Terhorst, B.: An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany, Revista Mexicana de Ciencias Geologicas, 21, 88–93, 2004.
Pyankov, V. I., Ziegler, H., Akhani, H., Deigele, C., and Lüttge, U.: European plants with C4 photosynthesis: geographical and taxonomic distribution and relations to climate parameters, Botanica Journal of Linnean Society, 163, 283–304, 2010.
Reimer, P. J., Baillie, M. G. L., Bard, E., Bayliss, A., Beck, W. J., Blackwell, P. G., Bronk Ramsey, C., Buck, C. E., Burr, G. S., Edwards, R. L., Friedrich, M., Grootes, P. M., Guilderson, T. P., Hajdas, I., Heaton, T. J., Hogg, A. G., Hughen, K. A., Kaiser, K. F., Kromer, B., McCormac, F. G., Manning, S. W., Reimer, R. W., Richards, D. A., Southon, J. R., Talamo, S., Turney, C. S. M., Van der Pflicht, J., and Weyhenmeyer, C. E.: Intcal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP, Radiocarbon, 51, 1111–1150, 2009.
Rousseau, D.-D., Puisségur, J.-J., and Lautridou, J.-P.: Biogeography of the Pleistocene pleniglacial malacofaunas in Europe. Stratigraphic and climatic implications, Palaeogeogr. Palaeocl., 80, 7–23, 1990.
Rousseau, D.-D., Sima, A., Antoine, P., Hatté, C., Lang, A., and Zöller, L.: Link between European and North Atlantic abrupt climate changes over the last glaciation, Geophys. Res. Lett., 34, L22713, https://doi.org/10.1029/2007gl031716, 2007.
Rousseau, D.-D., Antoine, P., Gerasimenko, N., Sima, A., Fuchs, M., Hatté, C., Moine, O., and Zoeller, L.: North Atlantic abrupt climatic events of the last glacial period recorded in Ukrainian loess deposits, Clim. Past, 7, 221–234, https://doi.org/10.5194/cp-7-221-2011, 2011.
Schmidt, E. D., Machalett, B., Marković, S. B., Tsukamoto, S., and Frechen, M.: Luminescence chronology of the upper part of the Stari Slankamen loess sequence (Vojvodina, Serbia), Quaternary Geochronol., 5, 137–142, 2010.
Schwan, J.: The origin of horizontal alternating bedding in Weichselian aeolian sands in northwestern Europe, Sediment. Geol., 49, 73–108, 1986.
Sebe, K., Csillag, G., Ruskiczay-Rüdiger, Z., Fodor, L., Thamo-Bozso, E., Müller, P., and Braucher, R.: Wind erosion under cold climate: a Pleistocene periglacial mega-yardang system in Central Europe (Western Pannonian Basin, Hungary), Geomorphology, 134, 470–482, 2011.
Sierro, F. J., Hodell, D. A., Curtis, J. H., Flores, J. A., Reguera, I., Colmenero-Hidalgo, E., Barcena, M. A., Grimalt, J. O., Cacho, I., Frigola, J., and Canals, M.: Impact of iceberg melting on Mediterranean thermohaline circulation during Heinrich events, Paleoceanography, 20, PA2019, https://doi.org/10.1029/2004PA001051, 2005.
Sima, A., Rousseau, D.-D., Kageyama, M., Ramstein, G., Schulz, M., Balkanski, Y., Antoine, P., Dulac, F., and Hatté, C.: Imprint of North-Atlantic abrupt climatic changes on Western European loess deposits as viewed in a dust emission model, Quaternary Sci. Rev., 28, 2851–2866, 2009.
Sima, A., Kageyama, M., Rousseau, D.-D., Ramstein, G., Balkanski, Y., Antoine, P., and Hatté, C.: Modeling dust emission response to MIS 3 millennial climate variations from the perspective of East European loess deposits, Clim. Past Discuss., 9, 143–185, https://doi.org/10.5194/cpd-9-143-2013, 2013.
Stevens, T., Marković, S. B., Zech, M., Hambach, U., and Sümegi, P.: Dust deposition and climate in the Carpathian Basin over an independently dated last glacial-interglacial cycle, Quaternary Sci. Rev., 30, 662–681, 2011.
Sümegi, P.: Loess ad Upper Paleolithic environment in Hungary, Aurea, Nagykovácsi, 312 pp., 2005.
Willis, K. J. and van Andel, T. H.: Trees or no trees? the environments of central and eastern Europe during the Last Glaciation, Quaternary Sci. Rev., 23, 2369–2387, 2004.
Willis, K. J., Rudner, E., and Sümegi, P.: The full-glacial forest of Central and Southeastern Europe, Quaternary Res., 53, 203–213, 2000.
Wynn, J. G. and Bird, M. I.: C4-derived soil organic carbon decomposes faster than its C3 counterpart in mixed C3/C4 soils, Glob. Change Biol., 13, 2206–2217, https://doi.org/10.1111/j.1365-2486.2007.01435.x, 2007.
Yu, Y. Y., Finke, P. A., Wu, H. B., and Guo, Z. T.: Sensitivity analysis and calibration of a soil carbon model (SoilGen2) in two contrasting loess forest soils, Geosci. Model Dev., 6, 29–44, https://doi.org/10.5194/gmd-6-29-2013, 2013.
Zech, M., Buggle, B., Leiber, K., Marković, S. B., Glaser, B., Hambach, U., Huwe, B., Stevens, T., Sümegi, P., Wiesenberg, G. L. B., and Zöller, L.: Reconstructing Quaternary vegetation history in the Carpathian Basin, SE Europe, using n-alkane biomarkers as molecular fossils, Quaternary Sci. J., 58, 148–155, 2009.