N2 fixation in eddies of the eastern tropical South Pacific Ocean.

Löscher, Carolin, Bourbonnais, A., Dekaezemacker, J., Charoenpong, C. N., Altabet, M. A., Bange, Hermann W. , Czeschel, Rena , Hoffmann, C. and Schmitz, Ruth (2016) N2 fixation in eddies of the eastern tropical South Pacific Ocean. Open Access Biogeosciences (BG), 13 . pp. 2889-2899. DOI 10.5194/bg-13-2889-2016.

[thumbnail of bg-13-2889-2016.pdf]
Preview
Text
bg-13-2889-2016.pdf - Published Version
Available under License Creative Commons: Attribution 3.0.

Download (2MB) | Preview
[thumbnail of bg-13-2889-2016-supplement.pdf]
Preview
Text
bg-13-2889-2016-supplement.pdf - Supplemental Material
Available under License Creative Commons: Attribution 3.0.

Download (510kB) | Preview

Supplementary data:

Abstract

Mesoscale eddies play a major role in controlling ocean biogeochemistry. By impacting nutrient availability and water column ventilation, they are of critical importance for oceanic primary production. In the eastern tropical South Pacific Ocean off Peru, where a large and persistent oxygen deficient zone is present, mesoscale processes have been reported to occur frequently. However, investigations on their biological activity are mostly based on model simulations, and direct measurements of carbon and dinitrogen (N2) fixation are scarce.

We examined an open ocean cyclonic eddy and two anticyclonic mode water eddies: a coastal one and an open ocean one in the waters off Peru along a section at 16° S in austral summer 2012. Molecular data and bioassay incubations point towards a difference between the active diazotrophic communities present in the cyclonic eddy and the anticyclonic mode water eddies.

In the cyclonic eddy, highest rates of N2 fixation were measured in surface waters but no N2 fixation signal was detected at intermediate water depths. In contrast, both anticyclonic mode water eddies showed pronounced maxima in N2 fixation below the euphotic zone as evidenced by rate measurements and geochemical data. N2 fixation and carbon (C) fixation were higher in the young coastal mode water eddy compared to the older offshore mode water eddy. A co-occurrence between N2 fixation and biogenic N2, an indicator for N loss, indicated a link between N loss and N2 fixation in the mode water eddies, which was not observed for the cyclonic eddy. The comparison of two consecutive surveys of the coastal mode water eddy in November and December 2012 revealed also a reduction of N2 and C fixation at intermediate depths along with a reduction in chlorophyll by half, mirroring an aging effect in this eddy. Our data indicate an important role for anticyclonic mode water eddies in stimulating N2 fixation and thus supplying N offshore.

Document Type: Article
Research affiliation: OceanRep > SFB 754 > B4
OceanRep > SFB 754
OceanRep > SFB 754 > A5
Kiel University
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-CH Chemical Oceanography
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-PO Physical Oceanography
Refereed: Yes
Open Access Journal?: Yes
Publisher: Copernicus Publications (EGU)
Projects: SOPRAN, SFB754
Expeditions/Models/Experiments:
Date Deposited: 14 Dec 2015 12:31
Last Modified: 23 Sep 2019 22:47
URI: https://oceanrep.geomar.de/id/eprint/30534

Actions (login required)

View Item View Item