DOI: 10.1016/j.quascirev.2017.11.028
Scopus记录号: 2-s2.0-85036472202
论文题名: Response of a land-terminating sector of the western Greenland Ice Sheet to early Holocene climate change: Evidence from 10Be dating in the Søndre Isortoq region
作者: Lesnek A.J. ; Briner J.P.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 180 起始页码: 145
结束页码: 156
语种: 英语
英文关键词: 10Be exposure dating
; Greenland Ice Sheet
; Holocene
; Moraines
Scopus关键词: Climate change
; Deposition
; Glaciers
; Water
; Climatic variability
; Greenland Ice Sheet
; Holocenes
; Laurentide ice sheets
; Moraines
; North Atlantic Ocean
; Tidewater glaciers
; ^10Be exposure dating
; Ice
; beryllium isotope
; climate forcing
; climate variation
; glacier retreat
; Holocene
; ice sheet
; moraine
; Arctic
; Atlantic Ocean
; Atlantic Ocean (North)
; Greenland
; Greenland Ice Sheet
英文摘要: The prevalence of land-terminating Greenland Ice Sheet margins is expected to increase as tidewater glaciers retreat onto land, yet few studies have characterized the sensitivity of these slow-moving margins to climatic variability. The response of land-terminating ice sheet sectors to climate forcing can be assessed by examining records of paleo-ice margin positions preserved in ice sheet moraine systems. In western Greenland, the extensive Fjord Stade moraine system was deposited by minor readvances or stillstands of the Greenland Ice Sheet margin during early Holocene net recession. Here, we combine new moraine mapping and cosmogenic 10Be exposure dating to constrain the timing of Fjord Stade moraine deposition in the Søndre Isortoq region. We find that the Fjord Stade moraines are composed of a western stage and an eastern stage, which we constrain to 9.7 ± 0.7 ka (n = 7; 1 SD) and 9.0 ± 0.3 ka (n = 7; 1 SD), respectively. Synchronous deposition of the Fjord Stade moraine complex across at least 350 km of western Greenland implies a widespread response of the western Greenland Ice Sheet to the 9.3 ka event. Furthermore, these new moraine ages may correlate with Laurentide Ice Sheet-sourced freshwater pulses into the North Atlantic Ocean. We also show that the response of the western Greenland Ice Sheet to early Holocene freshwater forcing was not restricted to fast-flowing, marine-terminating outlet glaciers; the land-terminating margin in the Søndre Isortoq region halted or reversed its pattern of retreat in response to climatic change. © 2017 Elsevier Ltd Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112331
Appears in Collections: 气候减缓与适应
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作者单位: Department of Geology, University at Buffalo, Buffalo, NY 14260, United States
Recommended Citation:
Lesnek A.J.,Briner J.P.. Response of a land-terminating sector of the western Greenland Ice Sheet to early Holocene climate change: Evidence from 10Be dating in the Søndre Isortoq region[J]. Quaternary Science Reviews,2018-01-01,180