Experimental validation of the planktic foraminifera fragmentation index as proxy for the end-Cretaceous Ocean Acidification
Author:
Funder
DST, India) INSPIRE Faculty Award
Publisher
Elsevier BV
Subject
Paleontology,Oceanography
Reference59 articles.
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2. Characterization of late campanian and maastrichtian planktonic foraminiferal depth habitats and vital activities based on stable isotopes;Abramovich;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2003
3. Global climate change and planktic foraminiferal response in the Maastrichtian;Abramovich;Paleoceanography,2010
4. Glacial–interglacial stability of ocean pH inferred from foraminifer dissolution rates;Anderson;Nature,2002
5. Biogeochemical constraints on the Triassic-Jurassic boundary carbon cycle event;Beerling;Glob. Biogeochem. Cycles,2002
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1. Untangling the biotic stress in the late Maastrichtian Deccan-benchmark interval of Bidart (France);Journal of Palaeogeography;2024-04
2. Foraminifera dissolution phases in the upper cretaceous succession of Jebel Duwi, Egypt;Journal of Umm Al-Qura University for Applied Sciences;2023-03-01
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