Do sedimentary sulfur phases link the biogeochemical cycle of calcium to atmospheric carbon dioxide concentrations?

沉积硫相是否将钙的生物地球化学循环与大气二氧化碳浓度联系起来？

• 批准号: RGPIN-2018-05873
• 负责人: Wortmann, Ulrich
• 金额: $ 1.82万
• 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: 2020
• 资助国家: 加拿大
• 起止时间: 2020-01-01 至 2021-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=713926
• 关键词: Do; sedimentary; sulfur; phases; link

The weathering and burial of carbon and sulfur compounds controls the long term balance of atmospheric oxygen, carbon-dioxide, as well nutrient availability and uptake in the ocean. These so called biogeochemical cycles are controlled by physical processes like weathering, and microbial redox reactions in the sub-seafloor. While the carbon cycle is well understood, much less is known about the sulfur cycle. Since the amount of oxidized sulfur (sulfate) in the ocean is large, and the input and output fluxes are thought to be small, it is generally assumed that measurable changes to the sulfur cycle only occur over very long timescales (tenth of millions of years). Recent research shows however that sulfur fluxes can undergo large and fast fluctuations. Preliminary analysis shows that these flux changes are large enough to be able to affect ocean oxygenation and atmospheric carbon dioxide concentrations. Here I propose to explore these effects in detail to gain a better understanding how they e.g., affected glacial/interglacial carbon dioxide levels.

碳和硫化合物的风化和埋葬控制了大气氧，二氧化碳，养分的可用性和海洋吸收的长期平衡。这些所谓的生物地球化学循环由诸如风化之类的物理过程和亚层发里的微生物氧化还原反应控制。虽然碳循环众所周知，但对硫循环的了解少得多。由于海洋中的氧化硫（硫酸盐）量很大，并且输入和输出通量被认为很小，因此通常认为硫循环的可测量变化仅发生在很长的时间表中（十亿年的十分之一）。然而，最近的研究表明，硫通量会发生大而快速的波动。初步分析表明，这些通量变化足够大，可以影响海洋氧合和大气二氧化碳浓度。在这里，我建议详细探讨这些效果，以更好地了解它们如何影响冰川/冰川间二氧化碳水平。