Cenozoic/Mesozoic variability of seawater sulfate concentrations

海水硫酸盐浓度的新生代/中生代变化

• 批准号: 261234-2013
• 负责人: Wortmann, UlrichGeorg
• 金额: $ 2.91万
• 依托单位: University of Toronto
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2014
• 资助国家: 加拿大
• 起止时间: 2014-01-01 至 2015-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=547693
• 关键词: Cenozoic; Mesozoic; variability; seawater; sulfate

Microbial sulfate reduction (MSR) is the fundamental process linking the biogeochemical cycles of carbon (C), oxygen (O), sulfur (S) and phosphorous (P). MSR respires approximately 85% of all sedimentary organic matter in marine sediments, and is thus a major control on atmospheric oxygen levels. MSR is also a key element for anaerobic methane oxidation, which critically controls the flux of methane (a major greenhouse gas) across the sediment water interface. MSR depends on sulfate as an electron acceptor, and variable sulfate concentrations affect this process in a non-linear way (Wortmann & Chernyavsky, Nature, 2007). While it is generally assumed that marine sulfate concentrations have been fairly stable through time (about 28mmol/l), I recently published the hypothesis that seawater sulfate concentrations fluctuated between 1 to 30 mmol/l throughout the last 130 Ma (Wortmann & Paytan, Science, 2012). Sulfate concentration changes of this magnitude will alter organic matter remineralization rates by a factor of three (Wortmann & Chernyavsky, 2007), affect microbial nitrogen fixation, and considerably modify the size of the marine phosphate reservoir, a major control on ocean fertility. Furthermore, it is likely that variable sulfate concentrations will influence the concentration of sulfate aerosols thus altering the radiative properties of the atmosphere (Wortmann & Paytan, 2012). Given the far reaching consequences of variable seawater sulfate concentrations, it is important to understand the robustness of this hypothesis. Here I propose to use a combination of modeling and fieldwork to evaluate whether alternative explanations are consistent with the geologic record and our understanding of ocean chemistry. These research questions are at the leading edge of the field and will result in high impact publications, furthering the international reputation of Canada's research competence. This proposal provides opportunities to train three Ph.D. and six M.Sc. students in data analysis, wet chemical laboratory methods, stable isotope analysis, computer programming, and international collaboration. These skills build the foundations for Canada's next generation of academic and business leaders.

微生物硫酸盐还原（MSR）是连接碳（C）、氧（O）、硫（S）和磷（P）生物地球化学循环的基本过程。 MSR 呼吸了海洋沉积物中约 85% 的沉积有机物，因此是大气中氧气水平的主要控制因素。 MSR 也是厌氧甲烷氧化的关键要素，它严格控制甲烷（一种主要温室气体）穿过沉积物水界面的通量。 MSR 依赖于硫酸盐作为电子受体，并且不同的硫酸盐浓度以非线性方式影响该过程（Wortmann & Chernyavsky，Nature，2007）。虽然人们普遍认为海洋硫酸盐浓度随着时间的推移相当稳定（约 28 毫摩尔/升），但我最近发表了这样的假设：在过去 130 Ma 中，海水硫酸盐浓度在 1 至 30 毫摩尔/升之间波动（Wortmann & Paytan，《科学》） ，2012）。 这种程度的硫酸盐浓度变化将使有机物再矿化率改变三倍（Wortmann & Chernyavsky，2007），影响微生物固氮，并显着改变海洋磷酸盐库的规模，而海洋磷酸盐库是海洋肥力的主要控制因素。此外，硫酸盐浓度的变化可能会影响硫酸盐气溶胶的浓度，从而改变大气的辐射特性（Wortmann & Paytan，2012）。考虑到海水硫酸盐浓度变化的深远影响，了解这一假设的稳健性非常重要。在这里，我建议结合使用建模和实地考察来评估替代解释是否与地质记录和我们对海洋化学的理解一致。这些研究问题处于该领域的前沿，并将产生具有高影响力的出版物，进一步提高加拿大研究能力的国际声誉。 该提案提供了培养三名博士的机会。和六个硕士学位学生学习数据分析、湿化学实验室方法、稳定同位素分析、计算机编程和国际合作。这些技能为加拿大下一代学术和商业领袖奠定了基础。