Stable isotope systematics in complex carbonates: Decoding geochemical processes and environmental conditions on Earth and other planets

复杂碳酸盐中的稳定同位素系统学：解码地球和其他行星上的地球化学过程和环境条件

• 批准号: RGPIN-2020-05810
• 负责人: Kim, SangTae
• 金额: $ 2.62万
• 依托单位: McMaster University
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2021
• 资助国家: 加拿大
• 起止时间: 2021-01-01 至 2022-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=740844
• 关键词: Stable; isotope; systematics; complex; carbonates

Carbonates, such as corals and cave deposits, have been one of the most abundant minerals on Earth's surface throughout its geological history. Carbonates of varying chemical compositions were also found in some Martian meteorites. Therefore, carbonates have been extensively studied by earth scientists as a natural archive from which Earth and other planet's environmental history can be reconstructed. My research program has focused on studying stable isotope systematics of carbonate minerals to accurately decode geochemical and environmental signals hidden in the carbonate minerals. The main objective of my Discovery research proposal is to gain a detailed understanding of stable isotope systematics of structurally complex carbonate minerals, such as dolomite (CaMg(CO3)2) with two distinct cation layers and ikaite (CaCO3·6H2O) containing water in its crystal structure. Although they are less abundant than the well-known carbonate, or calcite, under Earth's surface condition, these structurally complex carbonates are still of geological importance and have high potential as geochemical proxies for probing geochemical processes and climatic/environmental conditions from terrestrial and extraterrestrial environments, including Antarctica and Mars. My research team will synthesize two complex carbonates, dolomite and ikaite, under various laboratory conditions by refining my laboratory's well-established synthesis methods and specialized facilities. These carbonates will then be examined carefully for their mineralogical and stable isotope characteristics with respective to their formation mechanisms and conditions to better interpret geochemical or environmental information from the carbonates. Cost-effective or time-efficient analytical techniques, without sacrificing the existing analytical precision, will also be explored for accurate stable isotopic analyses of the two target carbonates not only for my proposed research, but also for the benefit of a broader scientific community. I will also examine natural samples, obtained through national/international collaborations (e.g., ikaite from Antarctica), to validate our experimental findings and interpret geochemical data from natural carbonates to accurately uncover Earth and other planet's climate/environmental history. The outcome of my proposed research will open a new opportunity to use terrestrial or extraterrestrial carbonates that have been neglected or unexplored by the scientific community due to lack of scientific understanding and analytical challenges to uncover Earth and other planet's climate/environmental history. This is important to predict Earth's future climate variability, providing our government and public to prepare for relevant guidelines and regulations. My proposed research will also provide highly qualified personnel (HQP) with cutting-edge research experience and help them to develop essential analytical and research skills required for their future careers.

碳酸盐，如珊瑚和洞穴沉积物，在其地质历史上一直是地球表面最丰富的矿物之一。在一些火星陨石中也发现了不同化学成分的碳酸盐。因此，碳酸盐作为一种自然档案被地球科学家广泛研究，从中可以重建地球和其他行星的环境历史。我的研究方向是研究碳酸盐矿物的稳定同位素系统，准确解码隐藏在碳酸盐矿物中的地球化学和环境信号。我的Discovery研究计划的主要目的是详细了解结构复杂的碳酸盐矿物的稳定同位素系统，例如具有两个不同阳离子层的白云岩（CaMg(CO3)2）和晶体结构中含有水的岩（CaCO3·6H2O）。尽管在地球表面条件下，这些结构复杂的碳酸盐不如众所周知的碳酸盐或方解石丰富，但它们仍然具有重要的地质意义，并且具有很高的潜力，可以作为探测地球化学过程和地球外环境（包括南极洲和火星）气候/环境条件的地球化学代用物。我的研究小组将在不同的实验室条件下，通过完善我实验室完善的合成方法和专门的设备，合成白云石和艾克石两种复杂的碳酸盐。然后仔细检查这些碳酸盐的矿物学和稳定同位素特征，以及它们的形成机制和条件，以更好地解释来自碳酸盐的地球化学或环境信息。在不牺牲现有分析精度的情况下，还将探索具有成本效益或时间效率的分析技术，以便对两种目标碳酸盐进行准确的稳定同位素分析，这不仅是为了我提出的研究，也是为了更广泛的科学界的利益。我还将检查通过国家/国际合作获得的自然样本（例如，来自南极洲的岩），以验证我们的实验结果，并解释来自天然碳酸盐的地球化学数据，以准确揭示地球和其他行星的气候/环境历史。我提出的研究结果将打开一个新的机会，利用由于缺乏科学理解和分析挑战而被科学界忽视或未探索的陆地或外星碳酸盐来揭示地球和其他行星的气候/环境历史。这对于预测地球未来的气候变化非常重要，为我们的政府和公众准备相关的指导方针和法规。我提出的研究也将为高素质人才（HQP）提供尖端的研究经验，并帮助他们发展未来职业所需的基本分析和研究技能。