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Quantifying the volcanic emissions which triggered Oceanic Anoxic Event 1a and their effect on ocean acidification
Author(s) -
Bauer Kohen W.,
Zeebe Richard E.,
Wortmann Ulrich G.
Publication year - 2017
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/sed.12335
Subject(s) - geology , anoxic waters , carbonate , carbonate compensation depth , carbon cycle , ocean acidification , volcano , isotopes of carbon , saturation (graph theory) , oceanography , geochemistry , total organic carbon , seawater , environmental chemistry , chemistry , calcite , ecology , mathematics , organic chemistry , combinatorics , ecosystem , biology
The Cretaceous Oceanic Anoxic Event 1a (Early Aptian) is thought to be causally related to the eruption of the Ontong Java Plateau large igneous province. This study uses osmium isotope records to quantify the magnitude of the respective CO 2 emissions up to the onset of Oceanic Anoxic Event 1a, and model the associated changes in carbonate saturation state (Ω), atmospheric pCO 2 , carbon isotope ratios and the carbonate compensation depth with a carbon cycle model. These model results suggest that volcanism associated with the rapid negative 187/188 osmium ratios observed during the onset of Oceanic Anoxic Event 1a (Selli Event) increased the planetary CO 2 degassing flux at least six‐fold, causing a negative δ 13 C excursion of ca 1·5‰ in the dissolved surface ocean inorganic carbon pool. This is consistent with previously published δ 13 C data. Volcanic degassing of this magnitude would also suppress the aragonite saturation state of surface water to near under‐saturated values (Ω ca 1·1 to 0·9), shoal the carbonate compensation depth by 1500 m and increase the atmospheric pCO 2 by 3000 p.p.m., before increased weathering and anoxia would counter the pCO 2 increase.