Earth SciencesCommunications Earth & Environment
Calcium isotope ratios of malformed foraminifera reveal biocalcification stress preceded Oceanic Anoxic Event 2
G. D. Kitch, A. D. Jacobson, et al.
This groundbreaking study reveals how ocean acidification triggered biocalcification stress in planktic foraminifera during the Cretaceous Ocean Anoxic Event 2. Researchers from Northwestern University and the University of Urbino explore critical calcium isotope shifts and their implications for understanding past climate events and developing ocean alkalinity enhancement strategies.
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