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DOI | 10.1073/pnas.1516908113 |
Widespread collapse of the Ross Ice Shelf during the late Holocene | |
Yokoyama Y.; Anderson J.B.; Yamane M.; Simkins L.M.; Miyairi Y.; Yamazaki T.; Koizumi M.; Suga H.; Kusahara K.; Prothro L.; Hasumi H.; Southon J.R.; Ohkouchi N. | |
发表日期 | 2016 |
ISSN | 0027-8424 |
起始页码 | 2354 |
结束页码 | 2359 |
卷号 | 113期号:9 |
英文摘要 | The stability of modern ice shelves is threatened by atmospheric and oceanic warming. The geologic record of formerly glaciated continental shelves provides a window into the past of how ice shelves responded to a warming climate. Fields of deep (-560 m), linear iceberg furrows on the outer, western Ross Sea continental shelf record an early post-Last Glacial Maximum episode of ice-shelf collapse that was followed by continuous retreat of the grounding line for ∼200 km. Runaway grounding line conditions culminated once the ice became pinned on shallow banks in the western Ross Sea. This early episode of ice-shelf collapse is not observed in the eastern Ross Sea, where more episodic grounding line retreat took place. More widespread (∼280,000 km2) retreat of the ancestral Ross Ice Shelf occurred during the late Holocene. This event is recorded in sediment cores by a shift from terrigenous glacimarine mud to diatomaceous open-marine sediment as well as an increase in radiogenic beryllium (10Be) concentrations. The timing of ice-shelf breakup is constrained by compound specific radiocarbon ages, the first application of this technique systematically applied to Antarctic marine sediments. Breakup initiated around 5 ka, with the ice shelf reaching its current configuration ∼1.5 ka. In the eastern Ross Sea, the ice shelf retreated up to 100 km in about a thousand years. Three-dimensional thermodynamic ice-shelf/ocean modeling results and comparison with ice-core records indicate that ice-shelf breakup resulted from combined atmospheric warming and warm ocean currents impinging onto the continental shelf. © 2016, National Academy of Sciences. All rights reserved. |
英文关键词 | Antarctica; Ice sheet; Ice shelf; Radiocarbon; Ross Sea |
语种 | 英语 |
scopus关键词 | beryllium; carbon 14; Article; atmosphere; climate; collapse; concentration (parameters); continental shelf; ice shelf; last glacial maximum; Late Holocene; marine environment; priority journal; sediment; warming |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/159080 |
作者单位 | Yokoyama, Y., Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwa-no-ha, Kashiwa, 275-8564, Japan, Department of Earth and Planetary Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan, Department of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka, 237-0061, Japan; Anderson, J.B., Department of Earth Science, Rice University, Houston, TX 77005, United States; Yamane, M., Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwa-no-ha, Kashiwa, 275-8564, Japan, Department of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka, 237-0061, Japan; Simkins, L.M., Department of Earth Science, Rice University, Houston, TX 77005, United States; Miyairi, Y., Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwa-no-ha, Kashiwa, 275-8564, Japan; Yamazaki, T., Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 K... |
推荐引用方式 GB/T 7714 | Yokoyama Y.,Anderson J.B.,Yamane M.,et al. Widespread collapse of the Ross Ice Shelf during the late Holocene[J],2016,113(9). |
APA | Yokoyama Y..,Anderson J.B..,Yamane M..,Simkins L.M..,Miyairi Y..,...&Ohkouchi N..(2016).Widespread collapse of the Ross Ice Shelf during the late Holocene.Proceedings of the National Academy of Sciences of the United States of America,113(9). |
MLA | Yokoyama Y.,et al."Widespread collapse of the Ross Ice Shelf during the late Holocene".Proceedings of the National Academy of Sciences of the United States of America 113.9(2016). |
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