The production and fate of volatile organosulfur compounds in sulfidic and ferruginous sediment

Wilkening, Jean V., Turchyn, Alexandra V., Redeker, Kelly R., Mills, Jennifer V., Antler, Gilad, Carrión, Ornella and Todd, Jonathan D. (2019) The production and fate of volatile organosulfur compounds in sulfidic and ferruginous sediment. Journal of Geophysical Research: Biogeosciences, 124 (11). pp. 3390-3402. ISSN 2169-8953

[thumbnail of Wilkening_et_al-2019-Journal_of_Geophysical_Research__Biogeosciences]
Preview
PDF (Wilkening_et_al-2019-Journal_of_Geophysical_Research__Biogeosciences) - Published Version
Available under License Creative Commons Attribution.

Download (6MB) | Preview

Abstract

Volatile organic sulfur compounds (VOSCs) link the atmospheric, marine, and terrestrial sulfur cycles in marine and marginal marine environments. Despite the important role VOSCs play in global biogeochemical sulfur cycling, less is known about how the local geochemical conditions influence production and consumption of VOSCs. We present a study of dimethyl sulfide (DMS), methanethiol (MeSH), and dimethylsulfoniopropionate (DMSP) in sulfide-rich (sulfidic) and iron-rich (ferruginous) salt marsh sediment from north Norfolk, UK. Initial results illustrate the importance of minimizing time between sampling in remote field locations and laboratory analysis, due to rapid degradation of VOSCs. With rapid analysis of sediment from different depths, we observe high concentrations of DMS, MeSH, and DMSP, with concentrations in surface sediment an order of magnitude higher than those in previous studies of surface water. We measure systematic differences in the concentration and depth distribution of MeSH and DMS between sediment environments; DMS concentrations are higher in ferruginous sediment, and MeSH concentrations are higher in sulfidic sediment. With repeated measurements over a short time period, we show that the degradation patterns for DMS and MeSH are different in the ferruginous versus sulfidic sediment. We discuss potential biogeochemical interactions that could be driving the observed differences in VOSC dynamics in ferruginous and sulfidic sediment.

Item Type: Article
Uncontrolled Keywords: dimethyl sulfide,dimethylsulfoniopropionate,methanethiol,salt marsh,volatile organosulfur compounds,geophysics,forestry,oceanography,aquatic science,ecology,water science and technology,soil science,geochemistry and petrology,earth-surface processes,atmospheric science,earth and planetary sciences (miscellaneous),space and planetary science,palaeontology,sdg 14 - life below water ,/dk/atira/pure/subjectarea/asjc/1900/1908
Faculty \ School: Faculty of Science > School of Biological Sciences
UEA Research Groups: Faculty of Science > Research Groups > Molecular Microbiology
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 30 Nov 2019 02:05
Last Modified: 04 Mar 2024 17:51
URI: https://ueaeprints.uea.ac.uk/id/eprint/73225
DOI: 10.1029/2019JG005248

Downloads

Downloads per month over past year

Actions (login required)

View Item View Item