Collaborative Research: Do arc-continent collisions in the tropics set the Earth's climate state?

合作研究：热带地区的弧大陆碰撞是否决定了地球的气候状态？

• 批准号: 1925863
• 负责人: Oliver Jagoutz
• 金额: $ 44.32万
• 依托单位: Massachusetts Institute of Technology
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-08-01 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1925863&HistoricalAwards=false
• 关键词: Collaborative; Research; Do; arc; continent

Over its history, Earth has experienced warm ice-free and cold glacial climates, but it is unknown if transitions between these background climate states were the result of changes in CO2 sources or sinks. On these multi-million year geological timescales, CO2 enters the ocean and atmosphere primarily by volcanic outgassing and is removed primarily though the chemical erosion of rocks, which delivers calcium and magnesium via rivers to the ocean where they react with CO2 to form carbonate. It is hypothesized that the tectonic closure of ocean basins and formation of mountains at equatorial latitudes could drive cooling by creating topography and eroding highly soluble oceanic rocks in the warm, wet tropics. This process increases global weatherability, thereby increasing Earth's potential to sequester CO2 in carbonates through chemical erosion. The investigators aim to test the hypothesis that changes in global weatherability have controlled the Earth's background climate state with coupled geological, geochemical, and modelling studies. This broader impact of this work will benefit society by generating and disseminating knowledge about geological climate change at both the K-12 and college level. The researchers have developed a global database of arc-continent collisions through the Phanerozoic, which mark the closure of former ocean basins, and reconstructed their position with state-of-the-art paleogeographic models. The results from this analysis revealed a temporal coincidence between the maximum global extent of arc-continent collision in the tropics and the occurrence of every major glacial period in the Phanerozoic. The investigators will refine geological constraints and tectonic reconstructions in five critical belts. Through these case studies, the researchers will generate thermochronological data and refine the exhumation history of New Guinea and construct a new paleogeographic model for suturing in the Alpine-Himalaya belt. The investigators will also acquire new stratigraphic, geochronological, geological, petrographic, geochemical, and paleomagnetic data along Permo-Carboniferous sutures from Mexico to South America, Ordovician sutures in the northern Appalachian, and Neoproterozoic sutures in the Arabian-Nubian Shield. These field and laboratory data will be integrated with paleogeographic, weathering, and climate models to develop estimates for the change in pCO2 resulting from arc-continent collisions in the tropics utilizing the GEOCLIM model framework. This framework integrates climate models run at varying pCO2 with global weathering models such that the variable climatology can be used to estimate the effect of changes in global weatherability model on long-term steady-state pCO2 levels. In this framework, the investigators will perform sensitivity tests to isolate the effects of specific parameters such as lithology or topography. The researchers will further calibrate these models with source-to-sink cation studies in modern and paleo ophiolite watersheds. Finally, they will develop statistical methods to evaluate the strength of correlation and test hypothesized causal mechanisms for environmental change. Through this research the investigators will directly train a postdoctoral researcher, 5 PhD students and numerous undergraduate research assistants. To disseminate this basic research, the team will hold public seminars and workshops with K-12 teachers, and construct classes on Tectonics and Climate with online course materials, both at the high-school and undergraduate level.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

在其历史上，地球经历过温暖的无冰气候和寒冷的冰川气候，但尚不清楚这些背景气候状态之间的转变是否是二氧化碳源或汇变化的结果。在这数百万年的地质时间尺度上，二氧化碳主要通过火山喷发进入海洋和大气，主要通过岩石的化学侵蚀被清除，这些化学侵蚀通过河流将钙和镁输送到海洋中，在那里它们与二氧化碳反应形成碳酸盐。据推测，赤道纬度海洋盆地的构造闭合和山脉的形成可以通过在温暖潮湿的热带地区创造地形和侵蚀高可溶性海洋岩石来驱动冷却。这一过程增加了全球的耐候性，从而增加了地球通过化学侵蚀将二氧化碳封存在碳酸盐中的潜力。研究人员的目标是通过地质、地球化学和模拟研究来验证全球气候能力的变化控制了地球背景气候状态的假设。这项工作的广泛影响将通过在K-12和大学水平上产生和传播有关地质气候变化的知识来造福社会。研究人员已经建立了一个横跨显生宙的弧-大陆碰撞的全球数据库，这标志着前海洋盆地的关闭，并用最先进的古地理模型重建了它们的位置。这一分析的结果揭示了热带弧形大陆碰撞的全球最大范围与显生宙每个主要冰期的发生在时间上的一致性。研究人员将细化五个关键带的地质约束和构造重建。通过这些案例研究，研究人员将生成热年代学数据，完善新几内亚的发掘历史，并构建一个新的古地理模型，用于缝合阿尔卑斯-喜马拉雅带。研究人员还将获得新的地层学、地质年代学、地质、岩石学、地球化学和古地磁数据，这些数据沿着墨西哥至南美洲的二叠纪-石炭纪缝合线、阿巴拉契亚北部的奥陶纪缝合线和阿拉伯-努比亚地盾的新元古代缝合线。这些野外和实验室数据将与古地理、风化和气候模型相结合，利用GEOCLIM模型框架对热带地区弧-陆碰撞导致的二氧化碳分压变化进行估计。该框架将运行在不同二氧化碳分压下的气候模式与全球风化模式相结合，使得可变气候学可以用来估计全球气候能力模式的变化对长期稳态二氧化碳分压水平的影响。在此框架下，研究人员将进行灵敏度测试，以隔离特定参数（如岩性或地形）的影响。研究人员将在现代和古蛇绿岩流域进行源-汇阳离子研究，进一步校准这些模型。最后，他们将开发统计方法来评估相关性的强度，并测试环境变化的假设因果机制。通过这项研究，研究者将直接培养1名博士后，5名博士生和众多本科生研究助理。为了传播这一基础研究，该团队将与K-12教师一起举办公开研讨会和讲习班，并在高中和本科阶段使用在线课程材料构建构造和气候课程。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。