Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 11, issue 2
Biogeosciences, 11, 507-523, 2014
https://doi.org/10.5194/bg-11-507-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 11, 507-523, 2014
https://doi.org/10.5194/bg-11-507-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 31 Jan 2014

Research article | 31 Jan 2014

Microbial activity and carbonate isotope signatures as a tool for identification of spatial differences in methane advection: a case study at the Pacific Costa Rican margin

S. Krause1, P. Steeb1, C. Hensen1, V. Liebetrau1, A. W. Dale1, M. Nuzzo2, and T. Treude1 S. Krause et al.
  • 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1–3, 24148 Kiel, Germany
  • 2IDL, University of Lisbon, Lisbon, Portugal & Portuguese Institute for the Sea and Atmosphere (IPMA), Lisbon, Portugal

Abstract. The forearc of the convergent margin offshore Costa Rica is a region characterized by strong advection of methane-charged fluids causing the formation of ubiquitous cold seeps (mounds). Presented here are the first measurements of microbial anaerobic oxidation of methane (AOM) and sulfate reduction (SR) rates in sediments from two mounds (11 and 12), applying radiotracer techniques in combination with numerical modelling. In addition, analysis of microbial, methane-dependent carbonate δ18O, δ13C, and 87Sr / 86Sr signatures constrained the origin of the carbonate-precipitating fluid. Average rates of microbial activities differed by a factor of ~5 to 6 between Mound 11 (AOM 140.71 (±40.84 SD) mmol m−2 d−1, SR 117.25 (±82.06 SD) mmol m−2 d−1) and Mound 12 (AOM 22.37 (±0.85 SD) mmol m−2 d−1, SR 23.99 (±5.79 SD) mmol m−2 d−1). Modelling results yielded upward fluid advection velocities of 200 cm yr−1 at Mound 11 and 15 cm yr−1 at Mound 12. Analysis of oxygen and carbon isotope variations of authigenic carbonates from the two locations revealed more enriched values for Mound 11 (δ18O : 3.18 to 6.15‰; δ13C: −14.14 to −29.56‰) compared to Mound 12 (δ18O : 3.09 to 4.48‰; δ13C : −39.53 to −48.98‰). The variation of carbonate 87Sr / 86Sr indicated considerable admixture of deep-source fluid at Mound 11, while seawater 87Sr / 86Sr characteristics prevailed at Mound 12 during precipitation. The present study is in accordance with previous work supporting considerable differences of methane flux between the two mounds. It also strengthens the hypothesis of a dominant deep fluid source with thermogenic methane at Mound 11 versus a shallow source of biogenic methane at Mound 12. The results demonstrate that measurements of methane-driven microbial activity in combination with numerical modelling are a valid tool for constraining recent methane fluxes in the study area. In addition, the analysis of methane-derived authigenic carbonates provides an independent line of evidence for long-term fluid contribution to the porewater chemistry of shallow sediments in the study area.

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