Articles | Volume 14, issue 4
https://doi.org/10.5194/essd-14-1447-2022
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the Creative Commons Attribution 4.0 License.
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https://doi.org/10.5194/essd-14-1447-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Last interglacial sea-level proxies in the glaciated Northern Hemisphere
Department of Physical Geography and Geoecology, Charles University,
Prague, Czech Republic
Department of Earth and Environmental Sciences, Kumamoto University,
Kumamoto, Japan
Alfred Wegener Institute, Helmholtz Center for Polar and Marine
Research, Bremerhaven, Germany
MARUM, University of Bremen, Bremen, Germany
Jan Mangerud
Department of Earth Science, University of Bergen and Bjerknes Centre
for Climate Research, Bergen, Norway
Per Möller
Department of Geology, Quaternary Sciences, Lund University, Lund,
Sweden
Juha P. Lunkka
Geology Research Group, Oulu Mining School, University of Oulu, P.O.
Box 9000, Oulu 90014, Finland
Valery Astakhov
Institute of Earth Sciences, St. Petersburg University,
Universitetskaya 7/9, 199034, St. Petersburg, Russia
A. P. Karpinsky Russian Geological Research Institute (VSEGEI), Sredny
pr. 74, 199178, St. Petersburg, Russia
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During the last interglacial (130 to 115 ka), global sea level was higher than present. The World Atlas of Last Interglacial Shorelines (WALIS) has been created to document this. In this paper, we have compiled data for southeastern South America. There are landforms that indicate that sea level was 5 to 25 m higher than present during this time period. However, the quality of these data is hampered by limitations on elevation measurements, chronology, and geological descriptions.
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Short summary
The last interglacial (LIG; 130 to 115 ka) is a useful analogue for improving predictions of future changes to sea level. Here, we describe the location and characteristics of 82 LIG marine sites from the glaciated Northern Hemisphere (Russia, northern Europe, Greenland and North America). Sites are located in a variety of settings, including boreholes, riverbank exposures and along coastal cliffs.
The last interglacial (LIG; 130 to 115 ka) is a useful analogue for improving predictions of...
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