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Using Radiochemical Data from Collapsed Ice Shelf Sediments to Understand the Nature and Timing of the Benthic Response to High-Latitude Climate Change

利用崩塌冰架沉积物的放射化学数据了解底栖生物对高纬度气候变化响应的性质和时间

基本信息

批准号：
1341669
负责人：
David DeMaster
金额：
$ 44.96万
依托单位：
North Carolina State University
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2013
资助国家：
美国
起止时间：
2013-10-01 至 2017-09-30
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1341669&HistoricalAwards=false
关键词：
Using Radiochemical Data Collapsed Ice

项目摘要

Intellectual Merit: The PI requests support to analyze sediments from multi-cores and mega-cores previously collected from beneath the former Larsen B and Larsen A ice shelves. These unique cores will allow the PI to develop a time-integrated understanding of the benthic response to ice shelf collapse off the East Antarctic Peninsula over time periods as short as 5 years following ice shelf collapse up to 170 years after collapse. High latitudes are responding to climate change more rapidly than the rest of the planet and the disappearance of ice shelves are a key manifestation of climate warming. The PI will investigate the newly created benthic environments and associated ecosystems that have resulted from the re-initiation of fresh planktonic material to the sediment-water interface. This proposal will use a new geochemical technique, based on naturally occurring 14C that can be used to assess the distribution and inventory of recently produced organic carbon accumulating in the sediments beneath the former Larsen A and B ice shelves. The PI will couple 14C measurements with 210Pb analyses to assess turnover times for sedimentary labile organic matter. By comparing the distributions and inventories of labile organic matter as well as the bioturbation intensities among different locations as a function of time following ice shelf collapse/retreat, the nature and timing of the benthic response to ice shelf collapse can be assessed. Broader impacts: This study will provide important information characterizing changes occurring on the seafloor after the collapse of ice shelves. This research will support the research project of a graduate student. This project brings together researchers from both the European community and the LARISSA Project.

智力优势：PI请求支持分析先前从前Larsen B和Larsen A冰架下收集的多岩心和巨型岩心的沉积物。这些独特的岩心将使PI能够对东南极半岛冰架崩塌后5年至崩塌后170年的时间内底栖生物对冰架崩塌的反应进行时间综合了解。高纬度地区对气候变化的反应比地球其他地区更快，冰架的消失是气候变暖的一个主要表现。主要研究者将调查新形成的底栖环境和相关生态系统，这些环境和生态系统是由于新鲜的浮游物质重新进入沉积物-水界面而产生的。这项提议将使用一种新的地球化学技术，以天然存在的14 C为基础，可用于评估在前拉森A和B冰架下沉积物中积累的最近产生的有机碳的分布和存量。PI将把14 C测量与210 Pb分析结合起来，以评估沉积不稳定有机物的周转时间。通过比较不稳定有机物的分布和库存以及不同地点之间的生物扰动强度作为冰架崩溃/退缩后的时间函数，可以评估底栖生物对冰架崩溃的反应的性质和时间。更广泛的影响：这项研究将提供重要的信息，说明冰架崩塌后海底发生的变化。这项研究将支持一个研究生的研究项目。该项目汇集了来自欧洲共同体和LARISSA项目的研究人员。