Collaborative Research: Sources and circulation of intermediate and deep waters and their role in Campanian-Maastrichtian global cooling

合作研究：中层水和深层水的来源和循环及其在坎帕尼亚-马斯特里赫特全球变冷中的作用

• 批准号: 1261562
• 负责人: Ellen Martin
• 金额: $ 19.87万
• 依托单位: University of Florida
• 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: 2013-07-01 至 2018-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1261562&HistoricalAwards=false
• 关键词: Collaborative; Research; Sources; circulation; intermediate

The late Cretaceous period (83-66 Ma) saw an important climatic transition from the extreme warmth of the early Late Cretaceous to the cooler conditions of the Early Paleocene. Evidence from multiple ocean basins indicates that this transition was accompanied by major changes in ocean circulation. However, the nature of these oceanographic changes and their role in global cooling are the subject of debate. Some interpretations call for expansion of southern component water (SCW) through the global ocean, possibly causing widespread cooling through low-latitude upwelling of cold deep waters. Others suggest shifts in the dominance of regional sources of deep-water formation, including initiation of North Atlantic sources, leading to changes in intra-basinal heat transport and climate. This collaborative research, involving scientists from the University of Missouri-Columbia, the University of Florida, and the University of Michigan, seeks to resolve these controversies. Building on their earlier findings, the researchers will generate new geochemical proxy data from locations that will, in combination with existing data, constrain possible intermediate- and deep ocean sources and circulation modes. They will also evaluate the plausibility of paleoceanographic interpretations through climate model simulations, testing hypotheses regarding the effect of gateways and greenhouse gas concentrations on circulation patterns and deep convection and their links with global climate change. The results of this work will add to our knowledge about the relationship between ocean circulation and global climate change and, in this way, contribute to efforts to predict future climate change. In addition, the researchers will conduct specific activities that contribute to general education and the dissemination of scientific understanding, and the training and mentoring of young scientists including the following: (i) developing short videos to communicate the excitement and novelty of paleoceanographic research to the public, to be featured in displays at natural history museums at the researchers? home institutions, and posted on popular websites, (ii) training graduate students at each of the participating institutions, and (iii) disseminating results through publications, presentations at professional meetings, and by integrating research into lecture material, discussions, and classroom exercises for graduate and undergraduate students.

白垩纪晚期（83-66Ma）经历了一个重要的气候转变，从晚白垩世早期的极端温暖到古新世早期的凉爽条件。来自多个洋盆的证据表明，这一转变伴随着海洋环流的重大变化。然而，这些海洋变化的性质及其在全球变冷中的作用仍然是争论的主题。一些解释认为，南方成分水（SCW）在全球海洋中扩张，可能会通过低纬度寒冷深水的上升流导致大范围变冷。其他人认为深水形成的区域来源的主导地位发生了变化，包括北大西洋来源的开始，导致盆地内热传输和气候的变化。这项由密苏里大学哥伦比亚分校、佛罗里达大学和密歇根大学的科学家参与的合作研究旨在解决这些争议。基于他们早期的发现，研究人员将从地点生成新的地球化学代理数据，这些数据将与现有数据相结合，限制可能的中海和深海来源和环流模式。他们还将通过气候模型模拟来评估古海洋学解释的合理性，测试有关网关和温室气体浓度对环流模式和深层对流的影响及其与全球气候变化的联系的假设。这项工作的结果将增加我们对海洋环流与全球气候变化之间关系的了解，从而有助于预测未来气候变化的努力。此外，研究人员还将开展有助于普通教育和科学理解传播以及年轻科学家培训和指导的具体活动，包括：（i）制作短视频，向公众传达古海洋学研究的兴奋和新颖性。公众，在研究人员的自然历史博物馆展出？母机构，并发布在热门网站上，(ii) 在每个参与机构培训研究生，以及 (iii) 通过出版物、专业会议上的演讲以及将研究成果融入到讲座材料、讨论和课堂练习中来传播结果研究生和本科生。