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DOI10.1038/s41467-021-23304-8
The kaolinite shuttle links the Great Oxidation and Lomagundi events
Hao W.; Mänd K.; Li Y.; Alessi D.S.; Somelar P.; Moussavou M.; Romashkin A.E.; Lepland A.; Kirsimäe K.; Planavsky N.J.; Konhauser K.O.
发表日期2021
ISSN2041-1723
卷号12期号:1
英文摘要The ~2.22–2.06 Ga Lomagundi Event was the longest positive carbon isotope excursion in Earth’s history and is commonly interpreted to reflect perturbations in continental weathering and the phosphorous cycle. Previous models have focused on mechanisms of increasing phosphorous solubilization during weathering without focusing on transport to the oceans and its dispersion in seawater. Building from new experimental results, here we report kaolinite readily absorbs phosphorous under acidic freshwater conditions, but quantitatively releases phosphorous under seawater conditions where it becomes bioavailable to phytoplankton. The strong likelihood of high weathering intensities and associated high kaolinite content in post-Great-Oxidation-Event paleosols suggests there would have been enhanced phosphorus shuttling from the continents into marine environments. A kaolinite phosphorous shuttle introduces the potential for nonlinearity in the fluxes of phosphorous to the oceans with increases in chemical weathering intensity. © 2021, The Author(s).
语种英语
scopus关键词aluminum hydroxide; aluminum oxide; aluminum silicate; ferric hydroxide; ferric oxide; fresh water; kaolin; phosphorus; sea water; acidity; carbon isotope; chemical weathering; kaolin; marine environment; oxidation; paleosol; phosphorite; phosphorus cycle; solubilization; adsorption; Article; bacterial growth; dispersion; nonhuman; nonlinear system; oxidation; phytoplankton; river; sea; solubilization; Synechococcus; weathering; X ray diffraction
来源期刊Nature Communications
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/251443
作者单位Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada; Department of Geology, University of Tartu, Tartu, Estonia; Department of Geology, University of Science and Technology of Masuku, Franceville, Gabon; Institute of Geology, Karelian Science Centre, Petrozavodsk, Russian Federation; CAGE—Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway; Geological Survey of Norway (NGU), Trondheim, Norway; The Department of Earth and Planetary Sciences, Yale University, New Haven, CT, United States
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Hao W.,Mänd K.,Li Y.,et al. The kaolinite shuttle links the Great Oxidation and Lomagundi events[J],2021,12(1).
APA Hao W..,Mänd K..,Li Y..,Alessi D.S..,Somelar P..,...&Konhauser K.O..(2021).The kaolinite shuttle links the Great Oxidation and Lomagundi events.Nature Communications,12(1).
MLA Hao W.,et al."The kaolinite shuttle links the Great Oxidation and Lomagundi events".Nature Communications 12.1(2021).
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