Limited variability in the phytoplankton Emiliania huxleyi since the pre-industrial era in the Subantarctic Southern Ocean
Author:
Funder
H2020 Marie Skłodowska-Curie Actions
Publisher
Elsevier BV
Subject
Earth and Planetary Sciences (miscellaneous),Ecology,Global and Planetary Change
Reference87 articles.
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4. Discoloration of the sea due to Coccolithus huxley I “bloom”;Berge;Sarsia,1962
5. Impact of the ocean carbonate chemistry on living foraminiferal shell weight: Comment on “Carbonate ion concentration in glacial-age deep waters of the Caribbean Sea” by W. S;Bijma;Broecker and E. Clark. Geochemistry, Geophysics, Geosystems,2002
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1. Technical note: A comparison of methods for estimating coccolith mass;Biogeosciences;2024-03-28
2. Reduction in size of the calcifying phytoplankton Calcidiscus leptoporus to environmental changes between the Holocene and modern Subantarctic Southern Ocean;Frontiers in Marine Science;2023-06-22
3. Fossil coccolith morphological attributes as a new proxy for deep ocean carbonate chemistry;Biogeosciences;2023-05-09
4. Coccolithophore paleoproductivity since the Last Glacial Maximum in the Atlantic Ocean: Relationship with calcification and preservation variability;Quaternary International;2023-01
5. Coccolith dissolution versus productivity changes during the Plio-Pleistocene (3.14–1.80 MA) in the South Atlantic (ODP site 1090);Palaeogeography, Palaeoclimatology, Palaeoecology;2022-10
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