Letter. Diatom carbon export enhanced by silicate upwelling in the northeast Atlantic

Allen, John T., Brown, Louise, Sanders, Richard, Moore, C. Mark, Mustard, Alexander, Fielding, Sophie, Lucas, Mike, Rixen, Michel, Savage, Graham, Henson, Stephanie and Mayor, Dan (2005) Letter. Diatom carbon export enhanced by silicate upwelling in the northeast Atlantic. Nature, 437, (7059), 728-732. (doi:10.1038/nature03948)

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Official URL: http://dx.doi.org/10.1038/nature03948

Description/Abstract

Diatoms are unicellular or chain-forming phytoplankton that use silicon (Si) in cell wall construction. Their survival during periods of apparent nutrient exhaustion enhances carbon sequestration in frontal regions of the northern North Atlantic. These regions may therefore have a more important role in the 'biological pump' than they have previously been attributed1, but how this is achieved is unknown. Diatom growth depends on silicate availability, in addition to nitrate and phosphate2, 3, but northern Atlantic waters are richer in nitrate than silicate4. Following the spring stratification, diatoms are the first phytoplankton to bloom2, 5. Once silicate is exhausted, diatom blooms subside in a major export event6, 7. Here we show that, with nitrate still available for new production, the diatom bloom is prolonged where there is a periodic supply of new silicate: specifically, diatoms thrive by 'mining' deep-water silicate brought to the surface by an unstable ocean front. The mechanism we present here is not limited to silicate fertilization; similar mechanisms could support nitrate-, phosphate- or iron-limited frontal regions in oceans elsewhere.

Item Type:Article
ISSN:0028-0836 (print)
Related URLs:http://dx.doi.org/10.1038/nature03948
Subjects:Q Science > QH Natural history > QH301 Biology
G Geography. Anthropology. Recreation > GC Oceanography
Divisions:University Structure - Pre August 2011 > National Oceanography Centre (NERC)
ePrint ID:21057
URI:http://eprints.soton.ac.uk/id/eprint/21057
Deposited On:09 Mar 2006
Last Modified:02 Mar 2012 12:45

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