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  • 1
    Publication Date: 2001-09-29
    Description: Late Pleistocene changes in oceanic primary productivity along the equator in the Indian and Pacific oceans are revealed by quantitative changes in nanoplankton communities preserved in nine deep-sea cores. We show that variations in equatorial productivity are primarily caused by glacial-interglacial variability and by precession-controlled changes in the east-west thermocline slope of the Indo-Pacific. The precession-controlled variations in productivity are linked to processes similar to the Southern Oscillation phenomenon, and they precede changes in the oxygen isotopic ratio, which indicates that they are not the result of ice sheet fluctuations. The 30,000-year spectral peak in the tropical Indo-Pacific Ocean productivity records is also present in the Antarctica atmospheric CO2 record, suggesting an important role for equatorial biological productivity in modifying atmospheric CO2.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Beaufort, L -- de Garidel-Thoron, T -- Mix, A C -- Pisias, N G -- New York, N.Y. -- Science. 2001 Sep 28;293(5539):2440-4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉CNRS-CEREGE, BP 80, 13545 Aix-en-Provence Cedex 04, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11577233" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere ; Carbon Dioxide ; *Climate ; *Ecosystem ; *Eukaryota ; *Fossils ; Indian Ocean ; Light ; Marine Biology ; Oxygen Isotopes ; Pacific Ocean ; *Plankton ; Seawater ; Time
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2011-08-05
    Description: About one-third of the carbon dioxide (CO(2)) released into the atmosphere as a result of human activity has been absorbed by the oceans, where it partitions into the constituent ions of carbonic acid. This leads to ocean acidification, one of the major threats to marine ecosystems and particularly to calcifying organisms such as corals, foraminifera and coccolithophores. Coccolithophores are abundant phytoplankton that are responsible for a large part of modern oceanic carbonate production. Culture experiments investigating the physiological response of coccolithophore calcification to increased CO(2) have yielded contradictory results between and even within species. Here we quantified the calcite mass of dominant coccolithophores in the present ocean and over the past forty thousand years, and found a marked pattern of decreasing calcification with increasing partial pressure of CO(2) and concomitant decreasing concentrations of CO(3)(2-). Our analyses revealed that differentially calcified species and morphotypes are distributed in the ocean according to carbonate chemistry. A substantial impact on the marine carbon cycle might be expected upon extrapolation of this correlation to predicted ocean acidification in the future. However, our discovery of a heavily calcified Emiliania huxleyi morphotype in modern waters with low pH highlights the complexity of assemblage-level responses to environmental forcing factors.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Beaufort, L -- Probert, I -- de Garidel-Thoron, T -- Bendif, E M -- Ruiz-Pino, D -- Metzl, N -- Goyet, C -- Buchet, N -- Coupel, P -- Grelaud, M -- Rost, B -- Rickaby, R E M -- de Vargas, C -- 205150/European Research Council/International -- England -- Nature. 2011 Aug 3;476(7358):80-3. doi: 10.1038/nature10295.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉CEREGE, CNRS/Universite Aix-Marseille, Avenue L. Philibert BP80, 13545 Aix-en-Provence, Cedex 4, France. beaufort@cerege.fr〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21814280" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/chemistry/metabolism ; Atmosphere/chemistry ; Body Weight ; *Calcification, Physiologic ; Calcium/metabolism ; Calcium Carbonate/*analysis/chemistry/metabolism ; Carbon Cycle ; Carbon Dioxide/analysis/chemistry ; Carbonic Acid/*analysis/chemistry ; Fossils ; Geologic Sediments/chemistry ; Haptophyta/chemistry/*metabolism ; Hydrogen-Ion Concentration ; Molecular Sequence Data ; Oceans and Seas ; Pacific Ocean ; Partial Pressure ; Photosynthesis ; Phytoplankton/chemistry/*metabolism ; Seawater/*chemistry
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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