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ABSTRACT The regulation of oceanic primary production of biomass is important in the global carbon cycle because it constitutes 40% of total primary production on Earth1. Here we present
results from short-term experiments in the nutrient-poor central Atlantic Ocean. We find a small but significant stimulation of primary production (15-19%) in response to elevated CO2
concentrations that simulate the CO2 rise in surface waters that will occur over the next 100-200 years. Access through your institution Buy or subscribe This is a preview of subscription
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ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support REFERENCES * Falkowski, P. G. _Photosynth. Res_. 39, 235–258 (1994). Google
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references AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * Freshwater Biological Laboratory, University of Copenhagen, Helsingrsgade 51, DK-3400, Hillerd, Denmark Mette Hein & Kaj
Sand-Jensen Authors * Mette Hein View author publications You can also search for this author inPubMed Google Scholar * Kaj Sand-Jensen View author publications You can also search for this
author inPubMed Google Scholar RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Hein, M., Sand-Jensen, K. CO2 increases oceanic primary production.
_Nature_ 388, 526–527 (1997). https://doi.org/10.1038/41457 Download citation * Issue Date: 07 August 1997 * DOI: https://doi.org/10.1038/41457 SHARE THIS ARTICLE Anyone you share the
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