Collaborative Research: An Ultra-High Resolution Holocene Climate Record from a Varved Sediment Sequence from the Adelie Coast, Antarctica (IODP Exp 318)

分析东南极冰盖（EAIS）长期和短期行为的一个关键区域是威尔克斯陆缘的东段，位于东南极洲最大的冰下盆地威尔克斯冰下盆地的向海终端。威尔克斯冰下盆地实际上可能以类似于南极西部冰盖的方式对气候变化作出反应。此外，所有南极底层水的很大一部分可能来自南极海岸的这一部分，使该地区成为海洋环流模式的关键参与者。前往威尔克斯地的综合大洋钻探计划第318远征队最近获得了近3,000米的沉积岩芯。钻井现场U1357，获得了一个独特的超高积累率沉积序列从阿德利盆地，从最新的冰期一直延伸到全新世。这些季节性层状沉积物构成了世界上最大的全新世环境变化档案之一。沉积物包含一个近年度的分辨率记录，何时以及如何从货架冰盖边缘退缩~12,000 kyr B. P.他们还包含过去的水温，水体水库年龄，分层，生产力，海冰范围，并可能在整个全新世底层水生产的变化记录。在这份合作提案中，P.I.的请求资金用于从沉积柱中回收的有孔虫的形态测量、稳定同位素和地球化学分析。这些将用于制作第一个高分辨率（近十年至十年）南极边缘有孔虫同位素和化学气候时间序列：知识价值--该项目的结果将首次提供近十年至十年分辨率的必要数据，以解决与全新世期间南极洲及其周围发生的海洋学和气候变化有关的若干问题，包括：1）与南极边缘的其他部分相比，东南极边缘沿着冰川消退的方式和时间如何？2)东南极边缘冰川系统对冰消作用以及全球和区域全新世气候波动的响应是什么？3)海洋环流和底层水生产在全新世是如何变化的？作为我们探险后教育外展的一部分，我们将在本研究过程中针对科学博物馆和中学组织另外两场互动网络广播。在斯坦福大学，我们将继续通过美国宇航局资助的一个项目向中学传播这项工作的成果，在这个项目中，他定期与来自旧金山湾区的科学教师会面。此外，我们还邀请了皇后学院和斯坦福大学的8名本科生作为实习生参与该项目，并将指导他们完成设想过程

A key region for analysis of long- and short-term behavior of the East Antarctic Ice Sheet (EAIS) is the eastern sector of the Wilkes Land margin, located at the seaward termination of the largest subglacial basin in East Antarctica, the Wilkes subglacial basin. The Wilkes subglacial basin may in fact respond to climate variability in a fashion similar to the West Antarctic Ice Sheet. Additionally, a significant portion of all Antarctic Bottom Water may originate from this part of the Antarctic coast, making this region a key player in oceanic circulation patterns. The Integrated Ocean Drilling Program Expedition 318 to Wilkes Land recently obtained nearly 3,000 meters of sedimentary cores. Drill site U1357, obtained a unique ultra-high accumulation rate sedimentary sequence from the Adelie Basin that extends from the latest glacial interval through the Holocene. These seasonally laminated deposits constitute one of the world's most expanded archives of environmental change during the Holocene. The sediments contain a near annual-resolution record of when and how the ice sheet margin retreated from the shelf ~12,000 kyr B.P. They also contain a record of past changes in water temperature, water mass reservoir age, stratification, productivity, sea ice extent, and possibly bottom water production throughout the Holocene. In this collaborative proposal, the P.I.'s request funding for morphometric, stable isotopic, and geochemical analyses of foraminifera recovered from the sediment column. These will be used to produce the first high-resolution (sub-decadal to decadal) foraminiferal isotopic and chemical climate time series from the Antarctic margin.Intellectual Merit - The results from this project will provide, for the first time, the requisite data at subdecadal to decadal resolution to address a number of questions related to oceanographic and climatic changes that occurred on and around Antarctica during the Holocene, including: 1) How does the style and timing of deglaciation along the East Antarctic Margin compare with other parts of the Antarctic Margin? 2) What were the responses of the East Antarctic Margin glacial system to deglaciation as well as global and regional Holocene climate fluctuations? 3) How did oceanic circulation and bottom water production vary during the Holocene? As part of our post-expedition educational outreach, we will organize two additional interactive webcasts targeting science museums and secondary schools during the course of this research. At Stanford, we will continue to disseminate the results of this work to secondary schools via a funded NASA project wherein he is meeting regularly with science teachers from around the SF Bay Area. Additionally, we are engaging up to 8 undergraduate students at Queens College and Stanford University in the project as interns and will guide them through the process of envisioning