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From:Climate of the Past (Vol. 16, Issue 3) Peer-ReviewedMorphological changes in coccoliths, tiny calcite platelets covering the outer surface of coccolithophores, can be induced by physiological responses to environmental changes. Coccoliths recovered from sedimentary...
From:Ocean Science (Vol. 15, Issue 4) Peer-Reviewed
Diatoms account for up to 50 % of marine primary production and are considered to be key players in the biological carbon pump. Ocean acidification (OA) is expected to affect diatoms primarily by changing the...
From:Marine Biology (Vol. 159, Issue 8) Peer-ReviewedThe flux of organic particles below the mixed layer is one major pathway of carbon from the surface into the deep ocean. The magnitude of this export flux depends on two major processes--remineralization rates and...
From:Limnology and Oceanography (Vol. 56, Issue 6) Peer-ReviewedAbstract Only
From:Biogeosciences (Vol. 13, Issue 10) Peer-ReviewedStudies investigating the effect of increasing CO.sub.2 levels on the phosphorus cycle in natural waters are lacking although phosphorus often controls phytoplankton development in many aquatic systems. The aim of our...
From:Biogeosciences (Vol. 17, Issue 19) Peer-ReviewedEastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The production of organic material is fueled by upwelling of nutrient-rich deep waters and high incident light at the...
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