Quaternary Glacial History and Paleoenvironments of the East Antarctic Margin

9909793曼利该奖项由极地项目办公室的南极地质和地球物理项目提供，支持对普里兹湾和麦克罗伯逊陆架进行的多机构、国际（美国-澳大利亚）海洋地质和地球物理调查，该调查将在 RVIB N.B. 约 60 天的巡航期间完成。帕尔默.主要目标是利用通过 kasten 和巨型活塞取芯收集的沉积岩芯来记录第四纪期间的气候和海洋变化。 将根据地震剖面（Seabeam 2112 和 Bathy2000）选择核心地点。对南极冰盖对全球海洋和大气系统的核心作用的认识主要基于沿南极西部边缘收集的数据，而来自更广泛的南极东部边缘的类似广泛和高分辨率数据集却很少。该项目的目标包括 (1) 建立一个世纪至千年尺度的全新世古环境记录，(2) 检验有关陆架上先前冰川和间冰期事件沉积记录的假设，并评估沿南极东部边缘 500 公里延伸的最大冰川作用的时间和范围。高分辨率地震测绘和内陆架凹陷沉积物的取芯将用于重建全新世古环境。 在南极半岛和罗斯海的类似沉积环境中，沉积记录表明全新世期间初级生产和海冰范围存在千年和世纪尺度的变化，这与放射性碳分布的时间周期性有关，表明太阳变化在驱动全新世气候的某些变化中可能发挥作用。来自东南极洲边缘的类似高分辨率全新世记录将用于开发一套环南极数据，这些数据涉及南部冰川和海洋系统对晚第四纪气候变化的响应。 此外，这些数据将帮助我们评估南极东部边缘对全球变暖的反应。 对普里兹海峡 - 阿默里洼地地区的初步调查揭示了先前更新世间冰期沉积的序列。 上部全新世和下部（未标明日期）硅质单元可以在普里兹海峡 15,000 平方公里范围内追踪到，但需要更多的地下地震反射剖面结合该区域的密集取心来确定这些单元的空间分布和范围。 按时间顺序排列的工作将确定更新世晚期南极东部边缘冰川海洋沉积的时间和持续时间。分析将侧重于详细的沉积学、地球化学、微古生物学和古地磁技术。 这种多参数方法是在这些冰川海洋沉积物中提取有价值的古环境信号的最有效方法。 这些结果预计将导致对近代地质时期南极冰盖和海洋系统行为的理解取得重大进展。研究人员都具有多年在高纬度海洋环境中工作的经验，他们的结合将提供一个有效的团队来完成该项目。 大学和学院教师（该项目的主要研究者）将监督参与该项目各个阶段的本科生和研究生，以便实现教育目标与该项目的研究目标。

9909793ManleyThis award, provided by the Antarctic Geology and Geophysics Program of the Office of Polar Programs, supports a multi-institutional, international (US - Australia) marine geologic and geophysical investigation of Prydz Bay and the MacRobertson Shelf, to be completed during an approximately 60-day cruise aboard the RVIB N.B. Palmer. The primary objective is to develop a record of climate and oceanographic change during the Quaternary, using sediment cores collected via kasten and jumbo piston coring. Core sites will be selected based on seismic profiling (Seabeam 2112 and Bathy2000). Recognition of the central role of the Antarctic Ice Sheet to global oceanic and atmospheric systems is based primarily on data collected along the West Antarctic margin, while similar extensive and high resolution data sets from the much more extensive East Antarctic margin are sparse. Goals of this project include (1) development of a century- to millennial-scale record of Holocene paleoenvironments, and (2) testing of hypotheses concerning the sedimentary record of previous glacial and interglacial events on the shelf, and evaluation of the timing and extent of maximum glaciation along this 500 km stretch of the East Antarctic margin. High-resolution seismic mapping and coring of sediments deposited in inner shelf depressions will be used to reconstruct Holocene paleoenvironments. In similar depositional settings in the Antarctic Peninsula and Ross Sea, sedimentary records demonstrate millennial- and century- scale variability in primary production and sea-ice extent during the Holocene, which have been linked to chronological periodicities in radiocarbon distribution, suggesting the possible role of solar variability in driving some changes in Holocene climate. Similar high-resolution Holocene records from the East Antarctic margin will be used to develop a circum-Antarctic suite of data regarding the response of southern glacial and oceanographic systems to late Quaternary climate change. In addition, these data will help us to evaluate the response of the East Antarctic margin to global warming. Initial surveys of the Prydz Channel - Amery Depression region reveal sequences deposited during previous Pleistocene interglacials. The upper Holocene and lower (undated) siliceous units can be traced over 15,000 km2 of the Prydz Channel, but more sub-bottom seismic reflection profiling in conjunction with dense coring over this region is needed to define the spatial distribution and extent of the units. Chronological work will determine the timing and duration of previous periods of glacial marine sedimentation on the East Antarctic margin during the late Pleistocene. Analyses will focus on detailed sedimentologic, geochemical, micropaleontological, and paleomagnetic techniques. This multi-parameter approach is the most effective way to extract a valuable paleoenvironmental signal in these glacial marine sediments. These results are expected to lead to a significant advance in understanding of the behavior of the Antarctic ice-sheet and ocean system in the recent geologic past.The combination of investigators, all with many years of experience working in high latitude marine settings, will provide an effective team to complete the project. University and College faculty (Principal Investigators on this project) will supervise a combination of undergraduate and post-graduate students involved in all stages of the project so that educational objectives will be met in tandem with the research goals of the project.