Deglaciation of the Scandinavian Ice Sheet and a Younger Dryas ice cap in the outer Hardangerfjorden area, southwestern Norway

IF 2.4 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Boreas Pub Date : 2021-11-15 DOI:10.1111/bor.12568
Carl Regnéll, Jason P. Briner, Haflidi Haflidason, Jan Mangerud, John Inge Svendsen
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引用次数: 1

Abstract

Understanding past responses of ice sheets to climate change provides an important long-term context for observations of present day, and projected future, ice-sheet change. In this work, we reconstruct the deglaciation of the marine-terminating western margin of the Scandinavian Ice Sheet in the outer Hardangerfjorden area of southwestern Norway, following the Last Glacial Maximum (LGM) until the start of the Holocene. We base our interpretations on a combination of geomorphological mapping using high-resolution (LiDAR) terrain models, 68 new cosmogenic nuclide 10Be exposure ages and radiocarbon-dated lake sediment cores, supported by the stratigraphic position of the 12.1 ka Vedde Ash. We show that even the highest mountain summits in the area (~1200–1400 m a.s.l.) were ice-covered during the LGM, thus settling debates concerning the Scandinavian Ice Sheet thickness in this region. These summits emerged as nunataqs through the ice sheet about 22–18 ka, potentially owing to upstream ice thinning caused by the break-up and retreat of the Norwegian Channel Ice Stream. Following the break-up of the Norwegian Channel Ice Stream, the ice margin seemingly stabilized at the outermost coast for 3500–5500 years before the mouth of Hardangerfjorden became ice free at c. 14.5 ka. Subsequently, during the Bølling and Allerød periods, the ice sheet retreated rapidly into the inner parts of Hardangerfjorden before a major ice sheet re-advance during the Younger Dryas. We identify and reconstruct a sizeable, independent ice cap on the Ulvanosa mountain massif during the Younger Dryas (YD), a massif that earlier was mapped as covered by the Scandinavian Ice Sheet during the YD. We also document ice-free areas that are more extensive than previously thought between Hardangerfjorden and Matersfjorden during the YD.

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挪威西南部外哈当厄峡湾地区的斯堪的纳维亚冰盖和新仙女木时期冰帽的消冰作用
了解过去冰盖对气候变化的响应,为观测当前和预估未来冰盖变化提供了重要的长期背景。在这项工作中,我们重建了挪威西南部外哈当厄峡湾地区斯堪的纳维亚冰盖的海洋终止西边缘,从末次盛冰期(LGM)到全新世开始的冰川消融。我们的解释基于使用高分辨率(LiDAR)地形模型的地貌测绘,68个新的宇宙成因核素10Be暴露年龄和放射性碳定年的湖泊沉积物岩心,并得到12.1 ka Vedde Ash的地层位置的支持。我们发现,在LGM期间,即使是该地区最高的山峰(约1200-1400米a.s.l.)也被冰覆盖,从而解决了关于该地区斯堪的纳维亚冰盖厚度的争论。大约22-18年前,这些峰顶以冰凌的形式出现,可能是由于挪威海峡冰流的破裂和退缩导致上游冰层变薄。随着挪威海峡冰流的破裂,冰缘似乎在最外海岸稳定了3500-5500年,直到哈当厄峡湾口在约14.5 ka时无冰。随后,在Bølling和Allerød时期,冰盖迅速退缩到哈当厄峡湾的内部,然后在新仙女木时期,一个主要的冰盖重新前进。我们在新仙女木期(YD)确定并重建了Ulvanosa山地块上一个相当大的独立冰盖,该地块早先被绘制为在YD期间被斯堪的纳维亚冰盖覆盖。我们还记录了在YD期间,Hardangerfjorden和matersjorden之间的无冰区比以前认为的更广泛。
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来源期刊
Boreas
Boreas 地学-地球科学综合
CiteScore
5.90
自引率
4.50%
发文量
36
审稿时长
>12 weeks
期刊介绍: Boreas has been published since 1972. Articles of wide international interest from all branches of Quaternary research are published. Biological as well as non-biological aspects of the Quaternary environment, in both glaciated and non-glaciated areas, are dealt with: Climate, shore displacement, glacial features, landforms, sediments, organisms and their habitat, and stratigraphical and chronological relationships. Anticipated international interest, at least within a continent or a considerable part of it, is a main criterion for the acceptance of papers. Besides articles, short items like discussion contributions and book reviews are published.
期刊最新文献
Issue Information Boreas Reviewers, volume 53 Late Middle Pleistocene (MIS 11-6) in Europe – introduction Late Middle Pleistocene Wolstonian Stage (MIS 6) glaciation in lowland Britain and its North Sea regional equivalents – a review Issue Information
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