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The natural iron fertilization experiment KEOPS (KErguelen Ocean and Plateau compared Study): An overview

Citation

Blain, S and Queguiner, B and Trull, T, The natural iron fertilization experiment KEOPS (KErguelen Ocean and Plateau compared Study): An overview, Deep Sea Research Part II: Topical Studies in Oceanography, 55, (5-7) pp. 559-565. ISSN 0967-0645 (2008) [Non Refereed Article]


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DOI: doi:10.1016/j.dsr2.2008.01.002

Abstract

When the first scientific voyages went to the Southern Ocean, high levels of living biomass were observed in the vicinity of islands. Hart (1942) was the first to mention that the abundant biomass might be due to the release of oligoelements like iron from the island. This hypothesis, however, remained unverified for more than half a century because of the experimental difficulties in properly manipulating water with subnanomolar iron concentrations. When John Martin formulated the iron hypothesis (Martin, 1990) and provided the first supporting evidence of it, he also suggested using the chlorophyll plume observed westward of the Galapagos Island in the Equatorial Pacific as a natural iron fertilization experiment

Item Details

Item Type:Non Refereed Article
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical Oceanography
Objective Division:Environment
Objective Group:Physical and Chemical Conditions of Water
Objective Field:Physical and Chemical Conditions of Water in Marine Environments
Author:Trull, T (Professor Thomas Trull)
ID Code:54183
Year Published:2008
Web of Science® Times Cited:27
Deposited By:IASOS
Deposited On:2009-02-12
Last Modified:2009-06-10
Downloads:0

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