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

晚白垩纪（83-66 Ma）经历了一个重要的气候转变，从晚白垩纪早期的极端温暖到早古新世的较冷条件。来自多个海洋盆地的证据表明，这种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是争论的主题。一些解释认为是南方成分水（SCW）在全球海洋中的扩张，可能通过寒冷的深水低纬度上涌导致大范围的降温。另一些人则认为，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，导致了盆内热输送和气候的变化。这项由来自密苏里-哥伦比亚大学、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。在他们早期发现的基础上，研究人员将产生新的地球化学代理数据，这些数据将与现有数据相结合，限制可能的中深海来源和循环模式。他们还将通过气候模式模拟来评估古海洋学解释的合理性，测试关于通道和温室气体浓度对环流模式和深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认识，并以这种方式有助于预测未来的气候变化。此外，研究人员会进行一些具体的活动，以促进通识教育和传播科学知识，以及培训和指导青年科学家，其中包括：(i)制作短片，向公众宣传古海洋学研究的激动人心和新奇之处，并在自然历史博物馆展出。（ii）培训每个参与机构的研究生，（iii）通过出版物、专业会议上的演讲，以及将研究成果整合到研究生和本科生的讲座材料、讨论和课堂练习中来传播结果。

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.