Model experiment on heterotrophic denitrification vs. autotrophic anammox - quantifying collateral effects on the oceanic carbon cycle ...

The conversion of fixed nitrogen to N2 in suboxic waters is estimated to contribute roughly a third to total oceanic losses of fixed nitrogen and is hence understood to be of major importance to global oceanic production and, therefore, to the role of the ocean as a sink of atmospheric CO2. At prese...

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Bibliographic Details
Main Authors: Koeve, Wolfgang, Kähler, Paul
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.843015
https://doi.pangaea.de/10.1594/PANGAEA.843015
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Summary:The conversion of fixed nitrogen to N2 in suboxic waters is estimated to contribute roughly a third to total oceanic losses of fixed nitrogen and is hence understood to be of major importance to global oceanic production and, therefore, to the role of the ocean as a sink of atmospheric CO2. At present heterotrophic denitrification and autotrophic anammox are considered the dominant sinks of fixed nitrogen. Recently, it has been suggested that the trophic nature of pelagic N2-production may have additional, "collateral" effects on the carbon cycle, where heterotrophic denitrification provides a shallow source of CO2 and autotrophic anammox a shallow sink. Here, we analyse the stoichiometries of nitrogen and associated carbon conversions in marine oxygen minimum zones (OMZ) focusing on heterotrophic denitrification, autotrophic anammox, and dissimilatory nitrate reduction to nitrite and ammonium in order to test this hypothesis quantitatively. For open ocean OMZs the combined effects of these processes turn ... : Please note that this data set does not show data from observations or experimentation but instead output from a theoretical work generated by a numerical model! Read the publication for essential details necessary to understand what the numbers in this data set mean!The data are organized according to the figures in the publication. ...