Collaborative Research: Pleistocene-Holocene Climate Variability of the Southern Appalachian Region, Southeastern U.S.

中全新世温暖期（MHWP）最近受到越来越多的关注，作为一个模拟的近期气候条件，预计在全球变暖的反应。美国东南部内陆地区缺乏高分辨率的古气候代用记录，迫使气候建模者根据北美更知名的地区进行区域解释。然而，墨西哥湾的早期和快速变暖可能强烈影响了美国东南部的气候，导致了显著的区域气候差异。本研究旨在加深对该地区更新世-全新世古水文和古气候变化的理解，特别关注MHWP的开始时间，持续时间，幅度和季节特征以及其他气候事件的陆地足迹。本研究的目的是利用多个，高质量的陆地气候代用指标，这些代用指标保存的记录在时间分辨率和对它们特别敏感的年度季节方面各不相同。研究人员将分析来自七个地点的三个陆地档案，每个档案都保存了不同但互补的时间分辨率的气候记录：洞穴沉积物;湖泊沉积物;湖泊和洪泛平原沉积物。每种类型的记录的地方已经确定，初步研究表明，这种方法的可行性，这项研究的结果将限制在美国东南部的内部，特别是水文敏感，人口稠密的田纳西河流域的气候系统的区域特征。这项研究将深入了解气候变化对水文的影响，包括融水脉冲对洪泛区的发展和演变。美国东南部也是研究长期人类-气候相互作用的关键地区。东南部的考古遗址揭示了文化转型和创新的多个时期，包括MHWP期间早期栽培植物的证据。研究结果将提供背景和过去的环境条件与美洲原住民职业和文化转型之间的联系。古气候/环境研究项目在调查人员的实验室已经共享，通过课堂活动和独立的研究项目，与K-12学生和教师通过几个外展计划，包括NSF GK-12赠款，以改善地球科学教育在田纳西州的农村中学。调查人员将让学校教师参与这项研究的实地和实验室工作，并将继续根据这里提出的研究的各个方面开发实践项目。

The mid-Holocene warm period (MHWP) has recently received increased attention as an analog for near-future climate conditions expected in response to global warming. The lack of high-resolution paleoclimate proxy records for the interior southeastern US region has forced climate modelers to make regional interpretations based on better-known areas of North America. However, early and rapid warming of the Gulf of Mexico may have strongly influenced climate in the Southeastern US, resulting in significant regional climate differences. The present study seeks improved understanding of the Pleistocene-Holocene paleohydrological and paleoclimatic variability of the region, with special focus on the onset time, duration, amplitude, and seasonality characteristics of the MHWP and the terrestrial footprints of other climate events.The objective of this research is to extract a semi-quantitative to quantitative, high resolution, full-season paleoclimate history using multiple, high-quality terrestrial climate proxies that preserve records differing in temporal resolution and in the annual seasons to which they are particularly sensitive. The researchers will analyze three terrestrial archives from seven locations, each preserving a record of climate with different, but complementary, temporal resolution: speleothems; lake sediments; and lacustrine and floodplain deposits. Localities for each type of record have been identified and preliminary studies demonstrate the feasibility of this approach.The results of this study will constrain regional characteristics of the climate system in the interior SE US, especially the hydrologically-sensitive, populated Tennessee River Valley. The research will yield insights into the hydrological impact of climate changes, including meltwater pulses on floodplain development and evolution. The Southeastern US is also a critical area for investigating human-climate interaction over long time scales. Archaeological sites in the Southeast reveal multiple periods of cultural transition and innovation, including evidence for early cultivated plants during the MHWP. Research results will provide an essential linkage between context and association of past environmental conditions with Native American occupation and cultural transformation. Paleo-climate/-environmental research projects in the investigators' laboratories have been shared, through class activities and independent research projects, with K-12 students and teachers through several outreach programs, including an NSF GK-12 grant to improve Earth science education in rural middle schools in Tennessee. The investigators will involve school teachers in field and lab work for this research, and will continue to develop hands-on projects based on various aspects of the research proposed here.