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- W3118274399 abstract "Multiple lines of evidence suggest that volcanic and thermogenic gas emanations from the voluminous eruptions of the Central Atlantic Magmatic Province (CAMP) triggered the end-Triassic mass extinction. However, a comparison of the timing and duration of the biotic and environmental crises with the timing and duration of the magmatic activity is difficult with existing data, especially when comparing the sedimentary archives below radioisotopically dated CAMP lavas. Here, we report multiple iridium anomalies interpreted to be the remnants of weathered basaltic ashes or aerosols of CAMP eruptions from three basins across a 15° swath of paleolatitude. Milankovitch-controlled climate cycles pace the lacustrine strata of these basins, and in conjunction with paleomagnetic reversal stratigraphy and abundant palynological data, allow us to constrain the timing of magmatic events to be coincident with the extinctions. Thus, platinum group element concentrations provide geochemical traces of CAMP eruptions and can serve as potential proxies for CAMP eruptive pulses in both marine and nonmarine Triassic-Jurassic boundary successions, permitting evaluation of correlations worldwide." @default.
- W3118274399 created "2021-01-18" @default.
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- W3118274399 creator A5052777304 @default.
- W3118274399 creator A5078368575 @default.
- W3118274399 date "2021-01-08" @default.
- W3118274399 modified "2023-10-17" @default.
- W3118274399 title "Platinum Group Element Traces of CAMP Volcanism Associated With Low‐Latitude Environmental and Biological Disruptions" @default.
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