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Laboratory-determined Phosphorus Flux from Lake Sediments as a Measure of Internal Phosphorus Loading
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La reducción de la fijación de nitrógeno en el océano glacial se deduce de los cambios en los inventarios marinos de

Raja S Ganeshram1, Thomas F Pedersen, Stephen Calvert

  • 1Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK. Raja.Ganeshram@glg.ed.ac.uk

Nature
|January 24, 2002
PubMed
Resumen

Durante los períodos glaciales, el nitrógeno y el fósforo marinos aumentaron, pero las mayores proporciones de N / P probablemente suprimieron la fijación de nitrógeno, cuestionando la hipótesis de la fertilización del hierro para aumentar la productividad marina y la absorción de dióxido de carbono.

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