Marine anoxia and sedimentary mercury enrichments during the Late Cambrian SPICE event in northern Scotland

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Decoupling biogeochemical records, extinction, and environmental change during the Cambrian SPICE event

Several positive carbon isotope excursions in Lower Paleozoic rocks, including the prominent Upper Cambrian Steptoean Positive Carbon Isotope Excursion (SPICE), are thought to reflect intermittent perturbations in the hydrosphere-biosphere system. Models explaining these secular changes are abundant, but the synchronicity and regional variation of the isotope signals are not well understood. Ex...

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ژورنال

عنوان ژورنال: Geology

سال: 2019

ISSN: 0091-7613

DOI: 10.1130/g45871.1