Occurrence of benthic microbial nitrogen fixation coupled to sulfate reduction in the seasonally hypoxic Eckernforde Bay, Baltic Sea.

Bertics, V. J., Loscher, C. R., Salonen, I., Dale, A. W., Gier, J., Schmitz-Streit, Ruth and Treude, T. (2013) Occurrence of benthic microbial nitrogen fixation coupled to sulfate reduction in the seasonally hypoxic Eckernforde Bay, Baltic Sea. Biogeosciences, 10 (3). pp. 1243-1258.

Full text not available from this repository.

Abstract

Despite the worldwide occurrence of marine hypoxic regions, benthic nitrogen (N) cycling within these areas is poorly understood and it is generally assumed that these areas represent zones of intense fixed N loss from the marine system. Sulfate reduction can be an important process for organic matter degradation in sediments beneath hypoxic waters and many sulfate-reducing bacteria (SRB) have the genetic potential to fix molecular N (N-2). Therefore, SRB may supply fixed N to these systems, countering some of the N lost via microbial processes, such as denitrification and anaerobic ammonium oxidation. The objective of this study was to evaluate if N-2 fixation, possibly by SRB, plays a role in N cycling within the seasonally hypoxic sediments from the Eckernforde Bay, Baltic Sea. Monthly samplings were performed over the course of one year to measure nitrogenase activity (NA) and sulfate reduction rates, to determine the seasonal variations in bioturbation (bioirrigation) activity and important benthic geochemical profiles, such as sulfur and N compounds, and to monitor changes in water column temperature and oxygen concentrations. Additionally, at several time points, the active N-fixing community was examined via molecular tools. Integrated rates of N-2 fixation (approximated from NA) and sulfate reduction showed a similar seasonality pattern, with highest rates occurring in August (approx. 22 and 880 nmol cm(-3) d(-1) of N and SO42-, respectively) and October (approx. 22 and 1300 nmol cm(-3) d(-1) of N and SO42-, respectively), and lowest rates occurring in February (approx. 8 and 32 nmol cm(-3) d(-1) of N and SO42-, respectively). These rate changes were positively correlated with bottom water temperatures and previous reported plankton bloom activities, and negatively correlated with bottom water oxygen concentrations. Other variables that also appeared to play a role in rate determination were bioturbation, bubble irrigation and winter storm events. Molecular analysis demonstrated the presence of nifH sequences related to two known N-2 fixing SRB, namely Desulfovibrio vulgaris and Desulfonema limicola, supporting the hypothesis that some of the nitrogenase activity detected may be attributed to SRB. Overall, our data show that Eckernforde Bay represents a complex ecosystem where numerous environmental variables combine to influence benthic microbial activities involving N and sulfur cycling.

Document Type: Article
Additional Information: Times Cited: 23 Bertics, V. J. Loescher, C. R. Salonen, I. Dale, A. W. Gier, J. Schmitz, R. A. Treude, T.
Research affiliation: Kiel University
Kiel University > Kiel Marine Science
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
ISSN: 1726-4170
Projects: Future Ocean
Date Deposited: 30 Jan 2017 10:29
Last Modified: 30 Jan 2017 10:29
URI: http://oceanrep.geomar.de/id/eprint/35534

Actions (login required)

View Item View Item