Neoproterozoic to early Phanerozoic rise in island arc redox state due to deep ocean oxygenation and increased marine sulfate levels

Stolper, Daniel A.; Bucholz, Claire E.

doi:10.1073/pnas.1821847116

Title: Neoproterozoic to early Phanerozoic rise in island arc redox state due to deep ocean oxygenation and increased marine sulfate levels

Journal Article · Thu Apr 11 00:00:00 EDT 2019 · Proceedings of the National Academy of Sciences of the United States of America

DOI:https://doi.org/10.1073/pnas.1821847116· OSTI ID:1561912

^[1]; Bucholz, Claire E. ^[2]

Univ. of California, Berkeley, CA (United States). Department of Earth and Planetary Science; Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Earth and Environmental Services Area
California Inst. of Technology (CalTech), Pasadena, CA (United States). Division of Geological and Planetary Sciences

A rise in atmospheric O₂levels between 800 and 400 Ma is thought to have oxygenated the deep oceans, ushered in modern biogeochemical cycles, and led to the diversification of animals. Over the same time interval, marine sulfate concentrations are also thought to have increased to near-modern levels. We present compiled data that indicate Phanerozoic island arc igneous rocks are more oxidized (Fe³⁺/ΣFe ratios are elevated by 0.12) vs. Precambrian equivalents. We propose this elevation is due to increases in deep-ocean O₂and marine sulfate concentrations between 800 and 400 Ma, which oxidized oceanic crust on the seafloor. Once subducted, this material oxidized the subarc mantle, increasing the redox state of island arc parental melts, and thus igneous island arc rocks. We test this using independently compiled V/Sc ratios, which are also an igneous oxybarometer. Average V/Sc ratios of Phanerozoic island arc rocks are elevated (by +1.1) compared with Precambrian equivalents, consistent with our proposal for an increase in the redox state of the subarc mantle between 800 and 400 Ma based on Fe³⁺/ΣFe ratios. This work provides evidence that the more oxidized nature of island arc vs. midocean-ridge basalts is related to the subduction of material oxidized at the Earth’s surface to the subarc mantle. It also indicates that the rise of atmospheric O₂and marine sulfate to near-modern levels by the late Paleozoic influenced not only surface biogeochemical cycles and animal diversification but also influenced the redox state of island arc rocks, which are building blocks of continental crust.

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Research Organization:: Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: AC02-05CH11231

OSTI ID:: 1561912

Journal Information:: Proceedings of the National Academy of Sciences of the United States of America, Vol. 116, Issue 18; ISSN 0027-8424

Publisher:: National Academy of Sciences, Washington, DC (United States)Copyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 35 works

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Oxygen fugacity at the base of the Talkeetna arc, Alaska Bucholz, Claire E.; Kelemen, Peter B. Contributions to Mineralogy and Petrology, Vol. 174, Issue 10 https://doi.org/10.1007/s00410-019-1609-z	journal	September 2019
Phanerozoic radiation of ammonia oxidizing bacteria Ward, L. M.; Johnston, D. T.; Shih, P. M. Scientific Reports, Vol. 11, Issue 1 https://doi.org/10.1038/s41598-021-81718-2	journal	January 2021
Effect of redox on Fe–Mg–Mn exchange between olivine and melt and an oxybarometer for basalts Blundy, Jon; Melekhova, Elena; Ziberna, Luca Contributions to Mineralogy and Petrology, Vol. 175, Issue 11 https://doi.org/10.1007/s00410-020-01736-7	journal	October 2020

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