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ABSTRACT Reorganizations of the Atlantic meridional overturning circulation were associated with large and abrupt climatic changes in the North Atlantic region during the last glacial
period1,2,3,4. Projections with climate models suggest that similar reorganizations may also occur in response to anthropogenic global warming5,6,7. Here I use ensemble simulations with a
coupled climate–ecosytem model of intermediate complexity to investigate the possible consequences of such disturbances to the marine ecosystem. In the simulations, a disruption of the
Atlantic meridional overturning circulation leads to a collapse of the North Atlantic plankton stocks to less than half of their initial biomass, owing to rapid shoaling of winter mixed
layers and their associated separation from the deep ocean nutrient reservoir. Globally integrated export production declines by more than 20 per cent owing to reduced upwelling of
nutrient-rich deep water and gradual depletion of upper ocean nutrient concentrations. These model results are consistent with the available high-resolution palaeorecord, and suggest that
global ocean productivity is sensitive to changes in the Atlantic meridional overturning circulation. Access through your institution Buy or subscribe This is a preview of subscription
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Learn more Buy this article * Purchase on SpringerLink * Instant access to full article PDF Buy now Prices may be subject to local taxes which are calculated during checkout ADDITIONAL
ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS WEAKENING OF THE ATLANTIC MERIDIONAL
OVERTURNING CIRCULATION DRIVEN BY SUBARCTIC FRESHENING SINCE THE MID-TWENTIETH CENTURY Article 18 November 2024 HUMAN-INDUCED CHANGES IN THE GLOBAL MERIDIONAL OVERTURNING CIRCULATION ARE
EMERGING FROM THE SOUTHERN OCEAN Article Open access 13 March 2023 CONTINUED ATLANTIC OVERTURNING CIRCULATION EVEN UNDER CLIMATE EXTREMES Article Open access 26 February 2025 REFERENCES *
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Productivity data sets were provided by D. Antoine and W. Gregg. Discussions with A. Oschlies, M. Sarnthein, M. Weinelt and H. Kinkel were appreciated. This research was supported as part of
the research unit (Forschergruppe 451) on ocean gateways by the Deutsche Forschungsgemeinschaft (DFG). AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * College of Oceanic and Atmospheric
Sciences, Oregon State University, 104 COAS Admin. Bldg, Corvallis, Oregon, 97331, USA Andreas Schmittner Authors * Andreas Schmittner View author publications You can also search for this
author inPubMed Google Scholar CORRESPONDING AUTHOR Correspondence to Andreas Schmittner. ETHICS DECLARATIONS COMPETING INTERESTS The authors declare that they have no competing financial
interests. RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Schmittner, A. Decline of the marine ecosystem caused by a reduction in the Atlantic
overturning circulation. _Nature_ 434, 628–633 (2005). https://doi.org/10.1038/nature03476 Download citation * Received: 06 August 2004 * Accepted: 07 February 2005 * Issue Date: 31 March
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