The configuration of Northern Hemisphere ice sheets through the Quaternary

被引:373
作者
Batchelor, Christine L. [1 ,2 ]
Margold, Martin [3 ]
Krapp, Mario [4 ]
Murton, Della K. [4 ]
Dalton, April S. [5 ]
Gibbard, Philip L. [1 ]
Stokes, Chris R. [5 ]
Murton, Julian B. [6 ]
Manica, Andrea [4 ]
机构
[1] Univ Cambridge, Scott Polar Res Inst, Dept Geog, Cambridge CB2 1ER, England
[2] Norwegian Univ Sci & Technol NTNU, Dept Geosci & Petr, NO-7491 Trondheim, Norway
[3] Charles Univ Prague, Dept Phys Geog & Geoecol, Prague 12843, Czech Republic
[4] Univ Cambridge, Dept Zool, Cambridge CB2 3EJ, England
[5] Univ Durham, Dept Geog, Durham DH1 3LE, England
[6] Univ Sussex, Dept Geog, Brighton BN1 9RH, E Sussex, England
基金
瑞典研究理事会;
关键词
LAST GLACIAL MAXIMUM; SEA-LEVEL; PLEISTOCENE GLACIATIONS; HISTORY; CLIMATE; RECONSTRUCTION; TOPOGRAPHY; MODEL; CYCLE; STRATIGRAPHY;
D O I
10.1038/s41467-019-11601-2
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-level change is currently limited by a lack of knowledge of the configuration of ice sheets prior to the Last Glacial Maximum (LGM). Here, we compile a synthesis of empirical data and numerical modelling results related to pre-LGM ice sheets to produce new hypotheses regarding their extent in the Northern Hemisphere (NH) at 17 time-slices that span the Quaternary. Our reconstructions illustrate pronounced ice-sheet asymmetry within the last glacial cycle and significant variations in ice-marginal positions between older glacial cycles. We find support for a significant reduction in the extent of the Laurentide Ice Sheet (LIS) during MIS 3, implying that global sea levels may have been 30-40 m higher than most previous estimates. Our ice-sheet reconstructions illustrate the current state-of-the-art knowledge of pre-LGM ice sheets and provide a conceptual framework to interpret NH landscape evolution.
引用
收藏
页数:10
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