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Evidence for the long-term sedimentary environment in an Antarctic subglacial lake

机译:南极沉积湖中长期沉积环境的证据

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摘要

Lakes beneath the Antarctic Ice Sheet are of fundamental scientific interest for their ability to contain unique records of ice sheet history and microbial life in their sediments. However, no records of subglacial lake sedimentation have yet been acquired from beneath the interior of the ice sheet, and understanding of sediment pathways, processes and structure in subglacial lake environments remains uncertain. Here we present an analysis of seismic data from Subglacial Lake Ellsworth, showing that the lake bed comprises very fine-grained sediments deposited in a low energy environment, with low water- and sediment-fluxes. Minimum sediment thickness is 6 m, the result of prolonged low sedimentation rates. Based on the few available analogues, we speculate this sediment age range is a minimum of 150 ka, and possibly 1 Ma. Sediment mass movements have occurred, but they are rare and have been buried by subsequent sedimentation. We present a new conceptual model of subglacial lake sedimentation, allowing a framework for evaluating processes in subglacial lake environments, and for determining future lake access locations and interpreting subglacial lake samples. (C) 2018 The Authors. Published by Elsevier B.V.
机译:南极冰盖下面的湖泊对其沉积物中含有独特记录的冰盖历史和微生物生活的能力至关重要。然而,没有从冰盖内部的下面获得沉淀的沉淀的记录,并且沉积物途径的理解,底层湖环境中的沉积物途径,过程和结构仍然不确定。在这里,我们展示了Sublacial Lake Ellsworth的地震数据分析,表明湖床包括沉积在低能量环境中的非常细粒度的沉积物,具有低水和沉积物。最小沉积物厚度为6米,延长沉降率延长的结果。基于少数可用类似物,我们推测这种沉积物年龄范围至少为150 ka,可能& 1 ma。已经发生沉积物质量运动,但它们是罕见的,并且已经被随后的沉降掩埋。我们展示了一个新的底杉湖沉降概念模型,允许框架评估子杉木湖环境中的过程,以及确定未来的湖泊接入位置和解释子涂布湖样本。 (c)2018年作者。由elsevier b.v出版。

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