N-cycling and balancing of the N-deficit generated in the oxygen minimum zone over the Namibian shelf-An isotope-based approach.
Nagel, Birgit, Emeis, Kay-Christian, Flohr, Anita, Rixen, Tim, Schlarbaum, Tim, Mohrholz, Volker and van der Plas, Anja (2013) N-cycling and balancing of the N-deficit generated in the oxygen minimum zone over the Namibian shelf-An isotope-based approach. Journal of Geophysical Research: Biogeosciences, 118 (1). pp. 361-371. DOI https://doi.org/10.1002/jgrg.20040.
Full text not available from this repository.Abstract
[1] The northern Benguela upwelling system is a nutrient‐replete region with high plankton biomass production and a seasonally changing oxygen minimum zone. Nitrate:phosphate ratios in fresh upwelling water are low due to denitrification in the near‐seafloor oxygen minimum zone and phosphate efflux from sediments. This makes the region a candidate for substantial dinitrogen fixation, for which evidence is scarce. Nutrient and oxygen data, N isotope data of nitrate, nitrogen isotope ratios of particulate matter, particulate organic carbon content, and suspended matter concentrations on a transect across the shelf and upper slope at 23°S illustrate N‐cycling processes and are the basis for estimating the contribution of N‐sources and N‐sinks to the reactive nitrogen pool. It appears that N‐removal due to denitrification exceeds N gain by N2 fixation and physical mixing processes by a factor of >6, although inorganic N:P ratios again increase as surface water is advected offshore. Nitrate and ammonium regeneration, nutrient assimilation with N:P < 16, shelf break mixing, atmospheric input, and N2 fixation all contribute to the restoration of inorganic N:P ratios back to Redfield conditions, but in seasonally changing proportions. The Benguela upwelling system thus is a nutrient source for the oceanic‐mixed layer where N‐sources and N‐sinks are not in balance and Redfield conditions can only re‐adjust by advection and mixing processes integrated over time.
Document Type: | Article |
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Programme Area: | UNSPECIFIED |
Research affiliation: | Biogeochemistry and Geology > Carbon and Nutrient Cycling |
Refereed: | Yes |
Open Access Journal?: | No |
DOI: | https://doi.org/10.1002/jgrg.20040 |
ISSN: | 21698953 |
Date Deposited: | 16 Aug 2019 15:16 |
Last Modified: | 01 Oct 2020 12:59 |
URI: | http://cris.leibniz-zmt.de/id/eprint/2669 |
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