The influence of dissolved organic matter on the marine production of carbonyl sulfide (OCS) and carbon disulfide (CS2) in the Eastern Tropical South Pacific

Lennartz, Sinikka T.; Booge, Dennis; Koch, Boris P.; Gonçalves-Araujo, Rafael; Quack, Birgit; Fischer, Tim; Bittig, Henry; Röttgers, Rüdiger; Marandino, Christa A.; Ksionzek, Kerstin B.; von Hobe, Marc; Bracher, Astrid

doi:10.5194/os-2019-1

Journal Article

FZJ-2019-02381

The influence of dissolved organic matter on the marine production of carbonyl sulfide (OCS) and carbon disulfide (CS<sub>2</sub>) in the Eastern Tropical South Pacific

Lennartz, S. T. (Corresponding author) ; von Hobe, M.FZJ* ; Booge, D. ; Bittig, H. ; Fischer, T. ; Gonçalves-Araujo, R. ; Ksionzek, K. B. ; Koch, B. P. ; Bracher, A. ; Röttgers, R. ; Quack, B. ; Marandino, C. A.

2019
EGU Katlenburg-Lindau

Ocean science discussions ( ), 1 - 32 (2019) [10.5194/os-2019-1]

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Please use a persistent id in citations: http://hdl.handle.net/2128/22016 doi:10.5194/os-2019-1

Abstract: Oceanic emissions of the climate relevant trace gases carbonyl sulfide (OCS) and carbon disulfide (CS2) are a major source to their atmospheric budget. Their current and future emission estimates are still uncertain due to incomplete process understanding and, therefore, inexact quantification across different biogeochemical regimes. Here we present the first concurrent measurements of both gases together with related fractions of the dissolved organic matter (DOM) pool, i.e. solid-phase extractable dissolved organic sulfur (DOSSPE), chromophoric (CDOM) and fluorescent dissolved organic matter (FDOM) from the Eastern Tropical South Pacific (ETSP). These observations are used to estimate in-situ production rates and identify their drivers. We find different limiting factors of marine photoproduction: while OCS production is limited by the humic-like DOM fraction that can act as a photosensitizer, high CS2 production coincides with high DOSSPE concentration. The lack of correlation between OCS production and DOSSPE may be explained by the active cycling of sulfur between OCS and dissolved inorganic sulfide via OCS photoproduction and hydrolysis. In addition, the only existing parameterization for OCS dark production is validated and updated with new rates from the ETSP and the Indian Ocean. Our results will help to predict oceanic concentrations and emissions of both gases on regional and, potentially, global scales.

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