Sandel, Vera, Kiko, Rainer , Brandt, Peter , Dengler, Marcus , Stemmann, Lars, Vandromme, Pieter, Sommer, Ulrich and Hauss, Helena (2015) Nitrogen Fuelling of the Pelagic Food Web of the Tropical Atlantic. PLoS ONE, 10 (6). e0131258. DOI 10.1371/journal.pone.0131258.

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	Text (Eddy diffusivity (Kρ) section along 23°W (Panel A) and grouped by region (Panel B; colored crosses denote individual profiles, corresponding colored horizontal lines maximum NOx gradient and black line region mean). Mixed layer data are omitted from plot) S1_Fig.docx - Supplemental Material Available under License Creative Commons: Attribution 3.0. Download (417kB)
	Text (Species and number of individuals sampled at each station (three replicates each). doi:10.1371/journal.pone.0131258.s002) journal.pone.0131258.s002.docx - Supplemental Material Available under License Creative Commons: Attribution 3.0. Download (19kB)
	Text (Species and number of individuals sampled at each station (three replicates each). doi:10.1371/journal.pone.0131258.s002) journal.pone.0131258.s003.docx - Supplemental Material Available under License Creative Commons: Attribution 3.0. Download (14kB)

Abstract

We estimated the relative contribution of atmosphere (ic Nitrogen (N) input (wet and dry deposition and N fixation) to the epipelagic food web by measuring N isotopes of different functional groups of epipelagic zooplankton along 23°W (17°N-4°S) and 18°N (20-24°W) in the Eastern Tropical Atlantic. Results were related to water column observations of nutrient distribution and vertical diffusive flux as well as colony abundance of Trichodesmium obtained with an Underwater Vision Profiler (UVP5). The thickness and depth of the nitracline and phosphocline proved to be significant predictors of zooplankton stable N isotope values. Atmospheric N input was highest (61% of total N) in the strongly stratified and oligotrophic region between 3 and 7°N, which featured very high depth-integrated Trichodesmium abundance (up to 9.4×104 colonies m-2), strong thermohaline stratification and low zooplankton δ15N (~2‰). Relative atmospheric N input was lowest south of the equatorial upwelling between 3 and 5°S (27%). Values in the Guinea Dome region and north of Cape Verde ranged between 45 and 50%, respectively. The microstructure-derived estimate of the vertical diffusive N flux in the equatorial region was about one order of magnitude higher than in any other area (approximately 8 mmol m-2 d 1). At the same time, this region received considerable atmospheric N input (35% of total). In general, zooplankton δ15N and Trichodesmium abundance were closely correlated, indicating that N fixation is the major source of atmospheric N input. Although Trichodesmium is not the only N fixing organism, its abundance can be used with high confidence to estimate the relative atmospheric N input in the tropical Atlantic (r2 = 0.95). Estimates of absolute N fixation rates are two- to tenfold higher than incubation-derived rates reported for the same regions. Our approach integrates over large spatial and temporal scales and also quantifies fixed N released as dissolved inorganic and organic N. In a global analysis, it may thus help to close the gap in oceanic N budgets.

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