Articles | Volume 14, issue 11
https://doi.org/10.5194/cp-14-1755-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-1755-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Connecting the Greenland ice-core and U∕Th timescales via cosmogenic radionuclides: testing the synchroneity of Dansgaard–Oeschger events
Climate and Environmental Physics, Physics Institute & Oeschger
Centre for Climate Change Research, University of Bern, Sidlerstrasse 5,
3012 Bern, Switzerland
Quaternary Sciences, Department of Geology, Lund University,
Sölvegatan 12, 22362 Lund, Sweden
Christopher Bronk Ramsey
Research Laboratory for Archaeology and the History of Art, University
of Oxford, Dyson Perrins Building, South Parks Road, Oxford OX1 3QY, UK
Tobias Erhardt
Climate and Environmental Physics, Physics Institute & Oeschger
Centre for Climate Change Research, University of Bern, Sidlerstrasse 5,
3012 Bern, Switzerland
R. Lawrence Edwards
Insitute of Global Environmental Change, Xi'an Jiatong University,
Xi'an 710049, China
Hai Cheng
Insitute of Global Environmental Change, Xi'an Jiatong University,
Xi'an 710049, China
Department of Earth Sciences, University of Minnesota, Minneapolis,
Minnesota 55455, USA
Chris S. M. Turney
Palaeontology, Geobiology and Earth Archives Research Centre and ARC
Centre of Excellence in Australian Biodiversity and Heritage, School of
Biological, Earth and Environmental Sciences, University of New South Wales,
Sydney, NSW 2052, Australia
Alan Cooper
Australian Centre for Ancient DNA and ARC Centre of Excellence in
Australian Biodiversity and Heritage, School of Biological Sciences, The
University of Adelaide, Adelaide, SA 5005, Australia
Anders Svensson
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen, Denmark
Sune O. Rasmussen
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen, Denmark
Hubertus Fischer
Climate and Environmental Physics, Physics Institute & Oeschger
Centre for Climate Change Research, University of Bern, Sidlerstrasse 5,
3012 Bern, Switzerland
Raimund Muscheler
Quaternary Sciences, Department of Geology, Lund University,
Sölvegatan 12, 22362 Lund, Sweden
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- The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) P. Reimer et al. 10.1017/RDC.2020.41
- Precise date for the Laacher See eruption synchronizes the Younger Dryas F. Reinig et al. 10.1038/s41586-021-03608-x
- Decadal-scale progression of the onset of Dansgaard–Oeschger warming events T. Erhardt et al. 10.5194/cp-15-811-2019
- The timing and effect of the earliest human arrivals in North America L. Becerra-Valdivia & T. Higham 10.1038/s41586-020-2491-6
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Discussed (final revised paper)
Latest update: 16 Nov 2024
Short summary
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.
The last glacial period was characterized by a number of rapid climate changes seen, for...