Late Quaternary deglacial history across the Larsen B embayment, Antarctica
Autor: | Jae Il Lee, Ara Jeong, Hyun Hee Rhee, Byung Yong Yu, Eugene W. Domack, Ho Il Yoon, Yeong Bae Seong, Greg Balco, Kyu-Cheul Yoo |
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Rok vydání: | 2018 |
Předmět: |
Archeology
Global and Planetary Change geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences Climate change Geology Last Glacial Maximum 010502 geochemistry & geophysics 01 natural sciences Ice shelf Paleontology Facies Deglaciation Glacial period Quaternary Ecology Evolution Behavior and Systematics Holocene 0105 earth and related environmental sciences |
Zdroj: | Quaternary Science Reviews. 189:134-148 |
ISSN: | 0277-3791 |
Popis: | We measured meteoric 10 Be variation throughout a marine sediment core from the Larsen B embayment (LBE) of the Antarctic Peninsula, and collected in situ 10 Be and 14 C exposure ages on terrestrial glacial deposits from the northern and southern margins of the LBE. We use these data to reconstruct Last Glacial Maximum (LGM) to present deglaciation and ice shelf change in the LBE. Core sedimentary facies and meteoric 10 Be data show a monotonic progression from subglacial deposits to sub-ice-shelf deposits to open-marine conditions, indicating that its collapse in 2002 was unprecedented since the LGM. Exposure-age data from the southern LBE indicate 40 m of ice surface lowering between 14 and 6 ka, then little change between 6 ka and the 2002 collapse. Exposure-age data from the northern LBE show a bimodal distribution in which clusters of apparent exposure ages in the ranges 4.9–5.1 ka and 1.0–2.0 ka coexist near 50 m elevation. Based on these results, other published terrestrial and marine deglaciation ages, and a compilation of sea bed imagery, we suggest a north-to-south progression of deglaciation in the northeast Antarctic Peninsula in response to Holocene atmospheric and oceanic warming. We argue that local topography and ice configuration inherited from the LGM, in addition to climate change, are important in controlling the deglaciation history in this region. |
Databáze: | OpenAIRE |
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