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Abrupt mid-Holocene ice loss in the western Weddell Sea Embayment of Antarctica

机译:南威尔科西部韦德尔海扶矿中的中全新世冰损失

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摘要

The glacial history of the westernmost Weddell Sea sector of Antarctica since the Last Glacial Maximum is virtually unknown, and yet it has been identified as critical for improving reliability of glacio-isostatic adjustment models that are required to correct satellite-derived estimates of ice sheet mass balance. Better knowledge of the glacial history of this region is also important for validating ice sheet models that are used to predict future contribution of the Antarctic ice sheet to sea level rise. Here we present a new Holocene deglacial chronology from a site on the Lassiter Coast of the Antarctic Peninsula, which is situated in the western Weddell Sea sector. Samples from 12 erratic cobbles and 18 bedrock surfaces from a series of presently-exposed ridges were analysed for cosmogenic Be-10 exposure dating, and a smaller suite of 7 bedrock samples for in situ C-14 dating. The resulting Be-10 ages are predominantly in the range 80-690 ka, whereas bedrock yielded much younger in situ C-14 ages, in the range 6.0-7.5 ka for samples collected from 138-385 m above the modern ice surface. From these we infer that the ice sheet experienced a period of abrupt thinning over a short time interval (no more than 2700 years) in the mid-Holocene, resulting in lowering of its surface by at least 250 m. Any late Holocene change in ice sheet thickness - such as re-advance, postulated by several modelling studies - must lie below the present ice sheet surface. The substantial difference in exposure ages derived from Be-10 and C-14 dating for the same samples additionally implies ubiquitous Be-10 inheritance acquired during ice-free periods prior to the last deglaciation, an interpretation that is consistent with our glacial-geomorphological field observations for former cold-based ice cover. The results of this study provide evidence for an episode of abrupt ice sheet surface lowering in the mid-Holocene, similar in rate, timing and magnitude to at least two other locations
机译:自最近冰川最大值以来,南极洲最西部德国海洋海洋部门的冰川历史几乎不为人知,但它已被确定为提高粗略卫星级估计冰片质量估算所需的Glacio-iSoStatic调整模型的可靠性至关重要平衡。更好地了解该地区的冰川历史对于验证用于预测南极冰板对海平面上升的未来贡献的冰板模型也很重要。在这里,我们展示了来自南极半岛的Lassiter海岸的网站的新全新世纪年代学,位于韦德尔海洋部门。分析来自12个不稳定的鹅卵石和18个基岩表面的来自一系列目前暴露的脊,用于美容为-10曝光约会,以及较小的7个基岩样品套件,用于原位C-14约会。由此产生的BE-10年龄主要在80-690 ka的范围内,而Bebrock在原位C-14岁的情况下产生了更小的,其范围为6.0-7.5ka,用于从现代冰表面上方138-385米收集的样品。从这些我们推断冰盖在中全新世中经历了一段时间内的突然稀疏(不超过2700年),导致其表面降低至少250米。冰盖厚度的任何晚期全新世 - 如重新进展,由几项建模研究发起 - 必须位于本发明的冰盖表面下方。来自BE-10和C-14的暴露年龄的差异差异另外暗示在最后一个谴责之前在无冰期间获得的无处不在的BE-10遗传,这是与我们的冰川地貌领域一致的解释前冷冰盖的观察。本研究的结果为中全新世中降低的突然冰盖表面的一集,与至少两个其他位置类似的速度,时序和幅度相似

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