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首页> 外文期刊>The holocene >New insights into paleoenvironmental changes in Laguna Potrok Aike, southern Patagonia, since the Late Pleistocene: The PASADO multiproxy record
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New insights into paleoenvironmental changes in Laguna Potrok Aike, southern Patagonia, since the Late Pleistocene: The PASADO multiproxy record

机译:自晚更新世以来,巴塔哥尼亚南部Laguna Potrok Aike的古环境变化的新见解:PASADO多代理记录

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摘要

A series of long sediment cores was retrieved from Laguna Potrok Aike, Southern Patagonia, within the framework of PASADO (Potrok Aike Maar Lake Sediment Archive Drilling Project), an ICDP (International Continental Scientific Drilling Program) lake drilling project. This maar lake, located at 52°S, 70°W in the Province of Santa Cruz (Argentina), in the southernmost continental area of the world, is one of the few permanent lakes in the region, providing a unique continuous paleoclimatic and paleoecological lacustrine record for the last glacial cycle. Previous multiproxy studies of this site have characterized the environmental history of these dry lands in the Patagonian Steppe for the last 16 cal. ka BP. This new series of sediment cores provides a much longer record of climate variability in Southern Patagonia since 51.3 cal. ka BP. Using a multiproxy strategy, a set of samples (mostly from core catcher material) was analyzed for physical properties, rock magnetism, geochemistry, CNS elemental analysis, stable isotopes, pollen and diatoms. This preliminary multiproxy limnogeological interpretation sheds new light on the regional Pleistocene and Holocene environmental history, revealing lake-level variations through time and identifying time windows of interest where higher resolution analyses will be carried out.
机译:在ICDP(国际大陆科学钻探计划)湖钻探项目PASADO(波特罗克·艾克·马尔湖沉积物档案钻探项目)的框架内,从巴塔哥尼亚南部的拉古纳·波特罗克·艾克检索了一系列长的沉积物岩心。位于世界最南端的圣克鲁斯省(阿根廷),南纬52°,南纬70°的马尔湖是该地区为数不多的永久湖泊之一,提供独特的连续古气候和古生态环境上一个冰川周期的湖相记录。对该地点的先前多代理研究已表征了巴塔哥尼亚草原最近16年来这些旱地的环境历史。 ka BP。自51.3 cal以来,这个新系列的沉积物核芯为巴塔哥尼亚南部的气候变化提供了更长的记录。 ka BP。使用多代理策略,分析了一组样品(主要来自岩心捕手的材料)的物理性质,岩石磁性,地球化学,CNS元素分析,稳定同位素,花粉和硅藻。这种初步的多代理森林地质学解释为区域更新世和全新世环境历史提供了新的亮点,揭示了随着时间的推移湖面变化,并确定了将进行更高分辨率分析的感兴趣的时间窗。

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