Methanogenesis sustained by sulfide weathering during the Great Oxidation Event View Full Text


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Article Info

DATE

2019-04

AUTHORS

Shui-Jiong Wang, Roberta L. Rudnick, Richard M. Gaschnig, Hao Wang, Laura E. Wasylenki

ABSTRACT

The Great Oxidation Event following the end of the Archaean eon (~2.4 Ga) was a profound turning point in the history of Earth and life, but the relative importance of various contributing factors remains an intriguing puzzle. Controls on methane flux to the atmosphere were of particular consequence; too much methane would have inhibited a persistent rise of O2, but too little may have plunged Earth into severe and prolonged ice ages. Here, we document a shift in the weathering reactions controlling the ocean-bound flux of nickel—an essential micronutrient for the organisms that produced methane in Precambrian oceans—by applying Ni stable isotope analysis to Mesoarchaean and Palaeoproterozoic glacial sediments. Although Ni flux to the ocean dropped dramatically as Ni content of the continental crust decreased, the onset of sulfide weathering delivered a small, but vital, flux of Ni to the oceans, sustaining sufficient methane production to prevent a permanent icehouse, while allowing O2 to rise. Oxidative weathering supplied a crucial flux of nutrients to the late Archaean oceans that sustained methanogenesis and kept the Archaean atmosphere in a methane sweet-spot, according to analyses of nickel isotopes from glacial deposits. More... »

PAGES

296-300

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41561-019-0320-z

DOI

http://dx.doi.org/10.1038/s41561-019-0320-z

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https://app.dimensions.ai/details/publication/pub.1112505502


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53 schema:description The Great Oxidation Event following the end of the Archaean eon (~2.4 Ga) was a profound turning point in the history of Earth and life, but the relative importance of various contributing factors remains an intriguing puzzle. Controls on methane flux to the atmosphere were of particular consequence; too much methane would have inhibited a persistent rise of O2, but too little may have plunged Earth into severe and prolonged ice ages. Here, we document a shift in the weathering reactions controlling the ocean-bound flux of nickel—an essential micronutrient for the organisms that produced methane in Precambrian oceans—by applying Ni stable isotope analysis to Mesoarchaean and Palaeoproterozoic glacial sediments. Although Ni flux to the ocean dropped dramatically as Ni content of the continental crust decreased, the onset of sulfide weathering delivered a small, but vital, flux of Ni to the oceans, sustaining sufficient methane production to prevent a permanent icehouse, while allowing O2 to rise. Oxidative weathering supplied a crucial flux of nutrients to the late Archaean oceans that sustained methanogenesis and kept the Archaean atmosphere in a methane sweet-spot, according to analyses of nickel isotopes from glacial deposits.
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