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DOI	10.1016/j.earscirev.2020.103267
	The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics
	Canfield D.E.; Bjerrum C.J.; Zhang S.; Wang H.; Wang X.
发表日期	2020
ISSN	0012-8633
卷号	208
英文摘要	The cycles of phosphorus, carbon and oxygen are intimately linked. Indeed, in many models, phosphorus is considered the driver of the carbon and oxygen cycles, and low concentrations of atmospheric oxygen during the Mesoproterozoic Era have been linked to extreme phosphorus limitation in the Mesoproterozoic oceans. To evaluate the Mesoproterozoic Era phosphorus cycle, we analyze the concentrations of phosphorus, organic carbon, and selected trace metals in several geological formations of Mesoproterozoic age. We combine these analyses with literature data to explore the relationship between phosphorus and organic carbon removal into Mesoproterozoic Era sediments through a variety of water depths and water-column chemistries. We find that the ratio of organic carbon to reactive phosphorus (Corg/Preact) is largely invariant between different paleo-settings with average Corg/Preact that is either equal to or less than the Redfield ratio of 106/1 through all environments we explored. We put these results in the context of the modern phosphorus cycle which is reviewed here. Compared to modern phosphorus dynamics, we see no evidence for an anoxic-euxinic feedback between phosphorus burial, carbon burial and oxygen production during Mesoproterozoic times. However, we do identify an additional potential phosphorus feedback related to the relationship between anoxia and deep-sea phosphorus dynamics that could have importance in oxygen regulation through time. We find that the average value of Corg/Preact during the Mesoproterozoic Era was greater than the average for modern sediments. This result suggests that equal or more organic carbon was buried per unit of phosphorus during Mesoproterozoic times compared to today, a conclusion broadly consistent with the carbon isotope record. These results offer the possibility of a strong oxygen source to the atmosphere during the Mesoproterozoic Era, raising the conundrum as to why atmospheric oxygen levels were lower then when compared to now. We suggest that a variety of factors may explain these differences in oxygen concentration including elevated rates of mantle degassing, reduced rates of phosphorus weathering and the lack of a terrestrial biosphere. © 2020 Elsevier B.V.
语种	英语
scopus关键词	anoxic conditions; chemostratigraphy; concentration (composition); euxinic environment; feedback mechanism; formation mechanism; organic carbon; paleoatmosphere; paleoceanography; paleoproductivity; phosphorus cycle; Proterozoic; terrestrial ecosystem
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209562
作者单位	Institute of Biology and Nordcee, University of Southern Denmark, Campusvej 55, Odense M, 5230, Denmark; Key Laboratory of Petroleum Geochemistry, China National Petroleum Corporation, Beijing, 100083, China; Department of Geosciences and Natural Resource Management, Section of Geology and Nordcee, ØsterVoldgade 10, København K, 1350, China
推荐引用方式 GB/T 7714	Canfield D.E.,Bjerrum C.J.,Zhang S.,et al. The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics[J],2020,208.
APA	Canfield D.E.,Bjerrum C.J.,Zhang S.,Wang H.,&Wang X..(2020).The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics.EARTH-SCIENCE REVIEWS,208.
MLA	Canfield D.E.,et al."The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics".EARTH-SCIENCE REVIEWS 208(2020).