The spatial extent of N fixation in the Atlantic Ocean is examined by determining the isotopic composition of N in suspended particulate organic nitrogen (?N PON). The samples were collected from zonal and meridional transects of the Atlantic Ocean during a 3-year period. There is a consistent depleted ?N PON signal extending over the center of the northern subtropical gyre, which partly coincides with a region where the tracer N* increases westward following the gyre circulation. This nonconservative behavior of N* implies that N fixation is responsible for the depleted ? N PON . A mixing model suggests that N fixation over parts of the northern gyre provides up to 74% of the N utilized by phytoplankton. However, since the PON represents only a small fraction of the total N pool, N fixation probably only plays a minor role in supplying new N to the euphotic zone in the surface waters of the northern subtropical gyre. Copyright 2007 by the American Geophysical Union.

How widespread and important is N2 fixation in the North Atlantic Ocean?

Landolfi A;
2007

Abstract

The spatial extent of N fixation in the Atlantic Ocean is examined by determining the isotopic composition of N in suspended particulate organic nitrogen (?N PON). The samples were collected from zonal and meridional transects of the Atlantic Ocean during a 3-year period. There is a consistent depleted ?N PON signal extending over the center of the northern subtropical gyre, which partly coincides with a region where the tracer N* increases westward following the gyre circulation. This nonconservative behavior of N* implies that N fixation is responsible for the depleted ? N PON . A mixing model suggests that N fixation over parts of the northern gyre provides up to 74% of the N utilized by phytoplankton. However, since the PON represents only a small fraction of the total N pool, N fixation probably only plays a minor role in supplying new N to the euphotic zone in the surface waters of the northern subtropical gyre. Copyright 2007 by the American Geophysical Union.
2007
Istituto di Scienze Marine - ISMAR
marine biogeochemistry
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/410628
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