Clumped Isotope Reordering Kinetics in Carbonate Minerals: The key to accurate ocean paleotemperatures and basin thermal histories

碳酸盐矿物中的团簇同位素重排动力学：准确海洋古温度和盆地热历史的关键

• 批准号: 1915647
• 负责人: Ethan Grossman
• 金额: $ 34.06万
• 依托单位: Texas A&M University
• 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 2023-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1915647&HistoricalAwards=false
• 关键词: Clumped; Isotope; Reordering; Kinetics; Carbonate

One of the most exciting new ideas in geochemistry is to measure two rare isotopes in calcium carbonate instead of just one and "clump" them together. This provides a new and powerful tool to study the temperature of ancient oceans and sediments and will help scientists looking at climate change, plate tectonics, and petroleum exploration. This study will help identify the calcium carbonate minerals most likely to preserve ancient temperatures. It will also provide the chemical information needed to use two minerals at the same time to better estimate the temperature history of the rocks. This project will develop this new tool by connecting atom-level processes with observed chemical reactions. The study will improve temperature estimates of ancient oceans and the temperature history of rocks related to petroleum reservoirs. The project will train graduate and undergraduate students and will add a new section of a capstone undergraduate course that will introduce seniors to the field. The project will also engage chemistry graduate and undergraduate students from underrepresented minority groupsOne of the most exciting developments in geochemistry in the 21st century is the ability to measure the relative abundance of molecules with two rare isotopes ("clumped isotopes") in calcium carbonate minerals (e.g., calcite) and apply this technique to reveal the temperatures of ancient oceans or the burial temperatures of sediments now exposed at the surface. A major complication in clumped isotope paleothermometry however is reequilibration (reordering) of the signatures at elevated temperatures (100oC) on million-year timescales. While complicating paleoclimate studies, this reordering provides great potential for measuring rates of burial, uplift, and exhumation of geologic formations, but only if the rates (kinetics) of reordering are well understood. Currently, only the reordering kinetics of the mineral calcite (CaCO3) has been studied in detail. To address this knowledge gap, experiments will be conducted in which different minerals are heated and the rate at which they reorder is measured. The mechanisms of clumped isotope reordering will be examined at an atomistic level using a range of sophisticated chemical techniques such as programmable heated-stage synchrotron X-ray diffraction, total scattering, Raman spectroscopy, and scanning transmission X-ray microscopy, in conjunction with advanced models for atomic bonding. Correlating atomic characteristics with kinetic parameters and mineralogical characterization will allow determination of detailed equations governing the rates of reordering in a variety of carbonate minerals. The project will train graduate and undergraduate students and will add a new section of a capstone undergraduate course that will introduce seniors to the field. The project will also engage chemistry graduate and undergraduate students from underrepresented minority groupsThis 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.

地球化学中最令人兴奋的新想法之一是测量碳酸钙中的两种稀有同位素，而不是仅一种，并将它们“聚集”在一起。 这为研究古代海洋和沉积物的温度提供了一个新的强大工具，并将帮助科学家研究气候变化、板块构造和石油勘探。这项研究将有助于确定最有可能保持古代温度的碳酸钙矿物。 它还将提供同时使用两种矿物所需的化学信息，以更好地估计岩石的温度历史。该项目将通过将原子级过程与观察到的化学反应联系起来来开发这种新工具。这项研究将改善对古代海洋的温度估计以及与石油储层相关的岩石的温度历史。 该项目将培训研究生和本科生，并将增加本科生课程的一个新部分，向高年级学生介绍该领域。该项目还将吸引来自代表性不足的少数群体的化学研究生和本科生。21世纪地球化学最令人兴奋的发展之一是能够测量碳酸钙矿物（例如方解石）中两种稀有同位素（“团块同位素”）分子的相对丰度，并应用该技术来揭示古代海洋的温度或沉积物的埋藏温度 现在暴露在表面。 然而，团簇同位素古温度测量的一个主要并发症是在百万年时间尺度的高温（100℃）下特征的重新平衡（重新排序）。虽然使古气候研究变得复杂，但这种重新排序为测量地质构造的埋藏、隆起和折返速率提供了巨大的潜力，但前提是重新排序的速率（动力学）得到充分理解。目前，仅详细研究了矿物方解石（CaCO3）的重排序动力学。为了解决这一知识差距，我们将进行实验，加热不同的矿物并测量它们重新排序的速率。将使用一系列复杂的化学技术，例如可编程加热级同步加速器 X 射线衍射、全散射、拉曼光谱和扫描透射 X 射线显微镜，并结合先进的原子键合模型，在原子水平上研究簇同位素重排序的机制。将原子特征与动力学参数和矿物学特征相关联将有助于确定控制各种碳酸盐矿物重排序速率的详细方程。 该项目将培训研究生和本科生，并将增加本科生课程的一个新部分，向高年级学生介绍该领域。该项目还将吸引来自代表性不足的少数群体的化学研究生和本科生。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。