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Ecological stability of late Maastrichtian benthic foraminifera amidst Deccan volcanism - Ocean Acidification
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Ecological stability of late Maastrichtian benthic foraminifera amidst Deccan volcanism - Ocean Acidification
Highlights Abstract The late Maastrichtian witnessed profound disruptions in biogeochemical cycles, leading to the fifth mass extinction at the Cretaceous–Paleogene (K/Pg) boundary. At Bidart section (France), the final ∼60 kyr of the Maastrichtian coincide with mercury (Hg) peaks, low magnetic susceptibility, evidence of biological stress and taphonomic alteration in planktic foraminifera, indicative of an ocean […] The post Ecological stabilit…
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