The Atlantic Meridional Overturning Circulation as productivity regulator of the North Atlantic Subtropical Gyre

Nave, Sílvia; Lebreiro, Susana; Michel, Elisabeth; Kissel, Catherine; Figueiredo, Maria Ondina; Guihou, Abel; Ferreira, Antonio; Labeyrie, Laurent; Alberto, Ana. 2019 The Atlantic Meridional Overturning Circulation as productivity regulator of the North Atlantic Subtropical Gyre. Quaternary Research, 91 (1). 399-413. https://doi.org/10.1017/qua.2018.88

Before downloading, please read NORA policies.

Preview

Text 2018_Nave_etal_accepted.pdf - Accepted Version Download (5MB) | Preview

Abstract/Summary

Spatially extensive and intense phytoplankton blooms observed off Iberia, in satellite pictures, are driven by significant nutrient supply by upper-ocean vertical mesoscale activity rather than by horizontal advection by coastal upwelling. Productivity of oligotrophic regions is still poorly depicted by discrete instrumental and model data sets. The paleoproductivity reconstructions of these areas represent the mean productivity over long periods, bringing new insights into the total biomass fluxes. Here, we present paleoproductivity records from the oceanic Tore Seamount region, covering the period from 140 to 60 ka. They show higher nutrient supplies during Termination II, Marine Oxygen Isotope Stage (MIS) 4, MIS 6, and warming transitions of the MIS 5 sub-stages. The highest nutrient content (higher productivity) in phase with tracers of bottom-water ventilation (benthic δ13C,231Pa/230Th) establishes a strong linkage with variability of Southern Ocean-sourced waters. Low productivity and ventilation over warm sub-stages of MIS 5 respond instead to North Atlantic Deep Water. Assuming that the Tore Seamount is representative of oligotrophic regions, the glacial-interglacial relationship observed between paleoproductivity and Atlantic Meridional Overturning Circulation strength opens new insights into the importance of estimating the total biomass in these regions. The subtropical gyres might play a considerable role in the carbon cycle over (sub-)glacial-interglacial time scales than previously thought.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1017/qua.2018.88
ISSN:	0033-5894
Date made live:	16 Nov 2018 12:31 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/521599

Actions (login required)

View Item

Document Downloads

More statistics for this item...