Ground-truthing lithium paleo-proxies: Experimental study on the Li incorporation and isotope fractionation during inorganic calcite and aragonite precipitation

真实的锂古代理：无机方解石和霰石沉淀过程中锂的掺入和同位素分馏的实验研究

• 批准号: 2001927
• 负责人: Joji Uchikawa
• 金额: $ 39.24万
• 依托单位: University of Hawaii
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2020
• 资助国家: 美国
• 起止时间: 2020-08-01 至 2023-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2001927&HistoricalAwards=false
• 关键词: Ground; truthing; lithium; paleo; proxies

Chemical break down of continental silicate rocks (referred to as “weathering”) consumes atmospheric CO2. During this process, lithium (Li) contained in silicate rocks is released and eventually delivered into the ocean by rivers. Intensity of weathering is known to influence the amount and isotopic composition (δ7Li) of Li delivered into the ocean. Thus, changes in the concentration of Li in seawater and its δ7Li can provide valuable information on the history and evolution of silicate weathering and its roles in regulating global carbon cycle and the Earth’s climate. Calcium carbonate (CaCO3) minerals produced by certain groups of marine organisms are known to incorporate trace amounts of Li from seawater, and thus they can be used as a recorder for those changes. However, our current understanding on how Li is incorporated into CaCO3 and what controls the process is extremely limited. In this study, researchers from the University of Hawaii (UH) will perform a series of laboratory experiments to better understand the mechanism of Li incorporation into CaCO3. This work will pave the road for further development in the use of marine CaCO3 minerals as the tracer for past changes in seawater Li and hence continental silicate weathering. The project will enhance education and career development in the geosciences for graduate and undergraduate students at the University of Hawaii. This team will also talk about their findings in the annual open house events such as “Mad About Science” and “Science Alive” at the Bishop MuseumWeathering of continental silicate rocks while releasing and eventually delivering Li into the ocean by rivers. Changes in seawater Li concentration and δ7Li can provide valuable information on the history and evolution of silicate weathering and its roles in regulating global carbon cycle and the Earth’s climate. CaCO3 minerals that incorporate Li can be used as a recorder for those changes. This study will be based on well-established inorganic CaCO3 precipitation experiments, where an array of solution physicochemical parameters will be systematically varied from the same control condition for straightforward comparisons of their impacts on δ7Li and Li concentrations in CaCO3. Furthermore, with the use of seeds, both calcite and aragonite samples will be synthesized under identical experimental conditions to examine the polymorphic controls on Li incorporation. This project is expected to provide by far the most complete experimental datasets, which will be combined with the use of surface kinetic modelling to establish a firm inorganic (kinetic and equilibrium) baseline for the elemental and isotopic partitioning of Li between solution and CaCO3 minerals. The project enhances education and career development in the geosciences for graduate and undergraduate students at the University of Hawaii, where the student population has diverse and often underrepresented ethnic background. This team will also talk about their findings in the annual open house events such as “Mad About Science” and “Science Alive” at the Bishop MuseumThis 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.

大陆硅酸盐岩石的化学分解（称为“风化”）消耗大气中的二氧化碳。在这个过程中，硅酸盐岩石中含有的锂（Li）被释放出来，最终通过河流进入海洋。已知风化强度会影响进入海洋的锂的数量和同位素组成（δ7Li）。因此，海水中Li含量及其δ7Li的变化可以为硅酸盐风化的历史和演化及其在全球碳循环和地球气候中的调节作用提供有价值的信息。已知某些海洋生物产生的碳酸钙（CaCO3）矿物含有海水中的微量Li，因此它们可以用作这些变化的记录器。然而，我们目前对Li如何被纳入CaCO3以及控制该过程的因素的了解非常有限。在这项研究中，来自夏威夷大学（UH）的研究人员将进行一系列实验室实验，以更好地了解Li掺入CaCO 3的机制。这项工作将铺平道路，进一步开发利用海洋碳酸钙矿物作为示踪剂过去的变化，海水锂，因此大陆硅酸盐风化。该项目将加强夏威夷大学研究生和本科生在地球科学方面的教育和职业发展。 该团队还将在每年的开放日活动中讨论他们的发现，如主教博物馆的“为科学而疯狂”和“科学活着”，以及大陆硅酸盐岩石的风化，同时释放并最终通过河流将Li输送到海洋中。海水Li浓度和δ7Li的变化可以为硅酸盐风化的历史和演化及其在全球碳循环和气候调节中的作用提供有价值的信息。含有Li的CaCO3矿物可以用作这些变化的记录器。本研究将基于成熟的无机CaCO3沉淀实验，其中溶液物理化学参数阵列将系统地从相同的控制条件变化，以直接比较它们对CaCO3中δ7Li和Li浓度的影响。此外，使用种子，方解石和文石样品将在相同的实验条件下合成，以检查对Li掺入的多晶型控制。该项目预计将提供迄今为止最完整的实验数据集，将结合使用表面动力学建模，为锂在溶液和CaCO3矿物之间的元素和同位素分配建立一个坚实的无机（动力学和平衡）基线。该项目加强了夏威夷大学研究生和本科生在地球科学方面的教育和职业发展，该大学的学生群体具有多样性，而且往往代表性不足。 该团队还将在年度开放日活动中讨论他们的发现，如主教博物馆的“疯狂科学”和“科学活着”。该奖项反映了NSF的法定使命，并被认为值得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来支持。