Collaborative Research: Investigation of paired uranium and chromium isotope behavior during authigenic metal uptake into continental margin sediments

合作研究：研究大陆边缘沉积物吸收自生金属过程中的成对铀和铬同位素行为

• 批准号: 1657832
• 负责人: James McManus
• 金额: $ 22.34万
• 依托单位: Bigelow Laboratory for Ocean Sciences
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2017
• 资助国家: 美国
• 起止时间: 2017-04-01 至 2022-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1657832&HistoricalAwards=false
• 关键词: Collaborative; Research; Investigation; paired; uranium

Chemical measurements in ocean sediment cores can be used to reconstruct past variations in the composition of seawater, environmental conditions, and climate. In order to do so we must understand exactly how the chemical composition of sediments is set and how it relates to environmental conditions. The concentrations of trace metals such as uranium (U) and, to a lesser extent, chromium (Cr) in sediments have been used to reconstruct past variations in ocean biological production, bottom water oxygen concentrations, or both. Potentially even more valuable than absolute concentrations of these elements are variations in the ratios of their different isotopes. In order to fully understand and use this tool for interpreting the past, this study will involve a detailed investigation of uranium and chromium isotope chemistry in modern ocean sediments. One graduate student, one postdoctoral researcher, and several undergraduate students will be funded through this project. Outreach activities will be coordinated with the Rutgers Marine Sciences outreach program. Severmann and her lab members will lead the annual Climate Change Teen Summit and will introduce the students and teachers to themes related directly to the research. This program is aimed at stimulating the interest of about 200 NY-NJ high school students in science, technology, engineering and math (STEM). The program will introduce young people to scientific concepts through hands-on activities and talks, and support students in planning and implementing science-related service projects in their local communities. The primary goal of this project is to advance the calibration and development of U and Cr isotopes as paleo-redox proxies. Authigenic metal isotope proxies offer a distinct advantage over simple metal abundances as they can provide additional information regarding the mechanism 
of metal uptake, and they do not require correction for variable mass accumulation rates.
 Current measurements of U and Cr isotope compositions in marine sediments, combined with experimental results, provide a first-order understanding of the dominant isotope effects associated with 
different sedimentary sinks and their uptake mechanism. However, since authigenic uptake for 
both metals takes place predominantly within the sediment package, a detailed investigation
 of the isotope effects during early diagenetic transformation is essential for fully exploiting 
these isotope systems as paleoproxies. The investigators will measure U and Cr isotope compositions in a suite of sites that are representative 
of typical continental margins. For both metals, these types of sediments represent a dominant
 oceanic sink; results from this study will thus fill a major gap in efforts to constrain the global isotope mass balance. By pairing sediment with porewater measurements the investigators will quantify the specific isotope fractionations associated with metal sequestration into 
reducing sediments. They will pair isotope measurements with detailed investigation
 of the elements' fundamental biogeochemical behavior in these settings, which currently is lacking, especially for Cr. The cumulative isotope effect at depth will be compared
 to depositional boundary conditions such as organic carbon burial rates and bottom water oxygenation, which will facilitate parameterization of sedimentary sinks globally. The central thesis is that these two elements will exhibit predictable behavior that is directly tied to organic
matter cycling (U) and metal oxide cycling (Cr) and that their paired isotope systems will 
prove to be a powerful combination for tracing net oxygenation in the ocean.

海洋沉积物岩心的化学测量可用于重建过去海水成分、环境条件和气候的变化。为此，我们必须准确了解沉积物的化学成分是如何形成的以及它与环境条件的关系。沉积物中微量金属（例如铀（U）和较小程度的铬（Cr））的浓度已被用来重建海洋生物生产、底层水氧浓度或两者的过去变化。比这些元素的绝对浓度更有价值的是它们不同同位素比率的变化。为了充分理解和使用这个工具来解释过去，这项研究将详细调查现代海洋沉积物中的铀和铬同位素化学。该项目将资助一名研究生、一名博士后研究员和多名本科生。外展活动将与罗格斯大学海洋科学外展计划协调。塞弗曼和她的实验室成员将主持年度气候变化青少年峰会，并向学生和教师介绍与研究直接相关的主题。该计划旨在激发约 200 名纽约州-新泽西州高中生对科学、技术、工程和数学 (STEM) 的兴趣。该计划将通过实践活动和讲座向年轻人介绍科学概念，并支持学生在当地社区规划和实施与科学相关的服务项目。该项目的主要目标是推进 U 和 Cr 同位素作为古氧化还原代理的校准和开发。自生金属同位素代理与简单金属丰度相比具有明显的优势，因为它们可以提供有关金属吸收机制的附加信息，并且不需要对可变质量积累率进行校正。目前对海洋沉积物中 U 和 Cr 同位素组成的测量，结合实验结果，提供了对与不同沉积汇及其吸收机制相关的主要同位素效应的一级了解。然而，由于“两种金属的自生吸收主要发生在沉积物包内，因此需要进行详细的调查”。早期成岩转化过程中同位素效应的研究对于充分利用这些同位素系统作为古代理至关重要。研究人员将在一系列代表典型大陆边缘的地点测量铀和铬同位素组成。对于这两种金属来说，这些类型的沉积物代表了主要的沉积物。海洋汇；因此，这项研究的结果将填补限制全球同位素质量平衡努力中的一个重大空白。通过将沉积物与孔隙水测量配对，研究人员将量化与金属封存到“还原沉积物”中相关的特定同位素分馏。他们会将同位素测量与详细调查结合起来——这些环境中元素基本生物地球化学行为的研究目前还缺乏，尤其是 Cr。将比较深度的累积同位素效应——有机碳埋藏率和底层水氧化等沉积边界条件，这将有助于全球沉积汇的参数化。中心论点是，这两种元素将表现出与有机物循环（U）和金属氧化物循环（Cr）直接相关的可预测行为，并且它们的配对同位素系统将被证明是追踪海洋净氧合的强大组合。

项目成果

Towards balancing the oceanic Ni budget

• DOI: 10.1016/j.epsl.2020.116461
• 发表时间: 2020-10
• 期刊: Earth and Planetary Science Letters
• 影响因子: 5.3
• 作者: S. Little;C. Archer;James McManus;J. Najorka;A. Wegorzewski;Derek Vance

Isotopically Light Cd in Sediments Underlying Oxygen Deficient Zones

• DOI: 10.3389/feart.2021.623720
• 发表时间: 2021-03
• 作者: Le-Tian Chen;S. Little;K. Kreissig;S. Severmann;J. McManus