EAR-PF: Testing if the SPICE is right - disentangling diagenesis, seawater chemistry, and ecological change across Cambrian trilobite extinctions using Ca and Mg isotope ratios

EAR-PF：测试 SPICE 是否正确 - 使用 Ca 和 Mg 同位素比率解开寒武纪三叶虫灭绝过程中的成岩作用、海水化学和生态变化

• 批准号: 2204376
• 负责人: Preston Kemeny
• 金额: $ 18万
• 依托单位: Kemeny, Preston Cosslett
• 依托单位国家: 美国
• 项目类别: Fellowship Award
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-09-01 至 2024-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2204376&HistoricalAwards=false
• 关键词: EAR; PF; Testing; SPICE; right

Dr. Preston Cosslett Kemeny has been awarded an NSF Earth Sciences Postdoctoral Fellowship to carry out research, professional development, and outreach activities at the University of Chicago under the mentorship of Dr. Clara Blättler. In this project, Dr. Kemeny will investigate the relationship between trilobite extinction and seawater chemistry during the Cambrian Period (approximately 540 to 485 million years ago). This work has broad implications for establishing robust environmental and ecological policy in the coming decades because understanding the interwoven nature of ancient life and climate provides fundamental context for predicting and responding to anthropogenic climate change. Previously, many interpretations of chemical variability in rocks implicated causal linkages between the global carbon cycle and ecological turnover. However, recent developments in the study of sedimentary processes have suggested that extinction and diversification may only weakly relate to environmental perturbations. The Cambrian Period offers unique opportunities for testing connections between ecology and seawater chemistry because it contains multiple trilobite extinction and diversification intervals associated with chemical anomalies. In this work, Dr. Kemeny will perform geochemical measurements on Cambrian rocks and fossils, and synthesize those observations within a numerical model, to better understand the relationship between extinction and the global carbon cycle. In addition, Dr. Kemeny will continue efforts to create an inclusive community through research, teaching, mentorship, and service activities that increase diversity, equity, inclusivity, and accessibility in the geosciences. These activities will include mentoring undergraduate and graduate students, training in effective and inclusive pedagogy, and working with local teachers to develop publicly available lesson plans on the global carbon cycle and paleontology.This project will study the coevolution of life with climate by quantifying connections between the global carbon cycle and trilobite extinction during the Cambrian Period. Dr. Kemeny will (1) measure calcium and magnesium isotope ratios in drill core samples from the Missouri basin to determine whether the Cambrian Steptoean Positive Carbon Isotope Excursion (SPICE) reflects a shift in the marine 13C/12C ratio or a shift in either the style of post-depositional alteration or mineralogy, (2) test existing hypotheses of marine anoxia during the SPICE event using sulfur and uranium isotope ratios, (3) evaluate trilobite fossils as a novel proxy for diagenetic modification and seawater chemistry, and (4) reproduce the isotopic observations within a box model of the ocean-atmosphere system and numerically constrain the temporal and spatial scales over which diagenesis can produce carbon isotope excursions. By disentangling biodiversity change from environmental change during the SPICE event, this project will take concrete steps towards understanding the coevolution of life with climate. Furthermore, by exploring a trilobite-based proxy for diagenetic alteration, the proposed work may provide a new tool to the geochemical community for reconstructing marine chemistry and for studying connections between the global carbon cycle and ecological turnover throughout the Paleozoic.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.

Preston Cosslett Kemeny 博士获得了 NSF 地球科学博士后奖学金，将在 Clara Blättler 博士的指导下在芝加哥大学开展研究、专业发展和外展活动。在该项目中，Kemeny 博士将调查这种关系。这项工作对于寒武纪时期（大约 540 至 4.85 亿年前）三叶虫灭绝和海水化学之间的关系具有广泛的意义。未来几十年，因为了解古代生命和气候的相互交织的性质为预测和应对人为气候变化提供了基础背景。此前，对岩石化学变化的许多解释都暗示了全球碳循环和生态周转之间的因果关系。沉积过程的研究表明，灭绝和多样化可能与环境扰动只有微弱的关系，寒武纪时期为测试生态学和海水化学之间的联系提供了独特的机会，因为它包含与化学相关的多个三叶虫灭绝和多样化区间。在这项工作中，Kemeny 博士将对寒武纪岩石和化石进行地球化学测量，并将这些观测结果综合到数值模型中，以更好地了解灭绝与全球碳循环之间的关系。此外，Kemeny 博士将继续努力。通过研究、教学、指导和服务活动创建一个包容性社区，以提高地球科学的多样性、公平性、包容性和可及性。这些活动将包括指导本科生和研究生、有效和包容性教学法培训以及工作。与当地教师一起制定有关全球碳循环和古生物学的公开课程计划。该项目将通过量化寒武纪期间全球碳循环与三叶虫灭绝之间的联系来研究生命与气候的共同进化。 (1)测量密苏里盆地钻芯样本中的钙和镁同位素比率，以确定寒武纪阶梯正碳同位素偏移 (SPICE) 是否反映了海洋 13C/12C 比率的变化或沉积后蚀变或矿物学类型的转变，(2) 使用硫和铀同位素比测试 SPICE 事件期间海洋缺氧的现有假设，(3) 评估三叶虫化石作为成岩作用和海水化学的新代理，（4）再现海洋-大气系统盒模型内的同位素观测结果，并在数值上限制成岩作用产生碳的时间和空间尺度通过在 SPICE 事件期间将生物多样性变化与环境变化分开，该项目将采取具体步骤来了解生命与气候的共同进化。此外，通过探索基于三叶虫的成岩改变代理，拟议的工作可能会提供一种新的方法。地球化学界重建海洋化学和研究全球碳循环与整个古生代生态周转之间联系的工具。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。