Metabolic balance of the open sea

David M. Karl (), Edward A. Laws, Paul Morris, Peter J. leB. Williams and Steven Emerson
Additional contact information
David M. Karl: University of Hawaii
Edward A. Laws: University of Hawaii
Paul Morris: University of Hawaii
Peter J. leB. Williams: School of Ocean Sciences, University of Wales
Steven Emerson: School of Oceanography, University of Washington

Nature, 2003, vol. 426, issue 6962, 32-32

Abstract: Abstract The rise of oxygenic photosynthesis nearly three billion years ago led to the accumulation of free oxygen and to the subsequent diversification of life on Earth; today, nearly half of all oxygen production derives from the photosynthetic activities of marine phytoplankton1. The conclusion that the open sea –– and therefore much of our planet's surface –– is in a net heterotrophic metabolic state2,3,4 is enigmatic and is a first-order question in the global carbon cycle, as discussed by del Giorgio and Duarte5. Our findings suggest that autotrophy in the open sea is episodic and decoupled from the more constant heterotrophic processes. Consequently, the metabolic balance of the open sea depends on proper space and timescale integration to achieve an ecological understanding of life in the sea.

Date: 2003
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DOI: 10.1038/426032a

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