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Dimethylsulfide production variations over the past 200 k.y. in the Equatorial Atlantic: a first estimate
Geologisch-Paläontologisches Institut, University of Kiel.
Biogeochemistry Centre, Earth Sciences, University of Bristol.
Biogeochemistry Centre, Earth Sciences, University of Bristol.
2000 (English)In: Geology, ISSN 0091-7613, E-ISSN 1943-2682, Vol. 28, no 6, p. 499-502Article in journal (Refereed) Published
Abstract [en]

Dimethylsulfide (DMS) released from phytoplankton produces cloud condensation nuclei in the marine troposphere, thereby providing a climate-regulating mechanism by increasing cloud albedo. A 200-k.y.-long sedimentary record from the equatorial Atlantic of DMS-producing phytoplankton suggests that DMS production increased during the glacial stages, thus potentially working to further cool the glacial world. Important factors limiting the operation of this possible feedback mechanism for planetary cooling may be the strength of trade winds and the availability of fine, iron-rich dust needed to fertilize growth of DMS producers.

Place, publisher, year, edition, pages
2000. Vol. 28, no 6, p. 499-502
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URN: urn:nbn:se:ltu:diva-5586DOI: 10.1130/0091-7613(2000)0282.3.CO;2Local ID: 3b8552a0-7d6e-11dc-b50c-000ea68e967bOAI: oai:DiVA.org:ltu-5586DiVA, id: diva2:978460
Note
Upprättat; 2000; 20071018 (ysko)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2017-11-24Bibliographically approved

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