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Science 10 July 1998: Vol. 281. no. 5374, pp. 237 - 240 DOI: 10.1126/science.281.5374.237
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Reports
Primary Production of the Biosphere: Integrating Terrestrial and Oceanic Components
Christopher B. Field,
*
Michael J. Behrenfeld,
James T. Randerson,
Paul Falkowski
Integrating conceptually similar models of the growth of marine and
terrestrial primary producers yielded an estimated global net primary
production (NPP) of 104.9 petagrams of carbon per year, with roughly
equal contributions from land and oceans. Approaches based on satellite
indices of absorbed solar radiation indicate marked heterogeneity in
NPP for both land and oceans, reflecting the influence of physical and
ecological processes. The spatial and temporal distributions of ocean
NPP are consistent with primary limitation by light, nutrients, and
temperature. On land, water limitation imposes additional constraints.
On land and ocean, progressive changes in NPP can result in altered
carbon storage, although contrasts in mechanisms of carbon storage and
rates of organic matter turnover result in a range of relations between carbon storage and changes in NPP.
C. B. Field, Department of Plant Biology, Carnegie
Institution of Washington, Stanford, CA 94305, USA. M. J. Behrenfeld and P. Falkowski, Institute of Marine and Coastal Sciences,
Rutgers University, New Brunswick, NJ 08901-8521, USA. J. T. Randerson, Department of Plant Biology, Carnegie Institution of
Washington, Stanford, CA 94305, USA, and Department of Biological
Sciences, Stanford University, Stanford, CA 94305, USA.
*
To whom correspondence should be addressed.
Read the Full Text
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