Large environmental disturbances caused by magmatic activity during the Late Devonian Hangenberg Crisis
Abstract
A wide range of various proxies (e.g., mineralogy, organic carbon, inorganic geochemistry, C and Mo isotopes, and framboidal pyrite) were applied for interpretation of changing oceanic redox conditions, bioproductivity, and the regional history of magmatic activity. This resulted in internally consistent interpretation of the late Famennian Hangenberg Crisis in subtropical deepest water sites of the epeiric Rhenohercynian and Saxo–Thuringian...
Paper Details
Title
Large environmental disturbances caused by magmatic activity during the Late Devonian Hangenberg Crisis
Published Date
Jul 1, 2020
Journal
Volume
190
Pages
103155 - 103155
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