Articles | Volume 9, issue 12
Biogeosciences, 9, 4969–4977, 2012
Biogeosciences, 9, 4969–4977, 2012

Research article 05 Dec 2012

Research article | 05 Dec 2012

Aerobic methanotrophy within the pelagic redox-zone of the Gotland Deep (central Baltic Sea)

O. Schmale1, M. Blumenberg2, K. Kießlich1, G. Jakobs1, C. Berndmeyer2, M. Labrenz1, V. Thiel2, and G. Rehder1 O. Schmale et al.
  • 1Leibniz Institute for Baltic Sea Research Warnemünde (IOW), Rostock, Germany
  • 2Geobiology Group, Geoscience Centre, Georg-August-University Göttingen, Göttingen, Germany

Abstract. Water column samples taken in summer 2008 from the stratified Gotland Deep (central Baltic Sea) showed a strong gradient in dissolved methane concentrations from high values in the saline deep water (max. 504 nM) to low concentrations in the less dense, brackish surface water (about 4 nM). The steep methane-gradient (between 115 and 135 m water depth) within the redox-zone, which separates the anoxic deep part from the oxygenated surface water (oxygen concentration 0–0.8 mL L−1), implies a methane consumption rate of 0.28 nM d−1. The process of microbial methane oxidation within this zone was evident by a shift of the stable carbon isotope ratio of methane between the bottom water (δ13C CH4 = −82.4‰ and the redox-zone (δ13C CH4 = −38.7‰. Water column samples between 80 and 119 m were studied to identify the microorganisms responsible for the methane turnover in that depth interval. Notably, methane monooxygenase gene expression analyses for water depths covering the whole redox-zone demonstrated that accordant methanotrophic activity was probably due to only one phylotype of the aerobic type I methanotrophic bacteria. An imprint of these organisms on the particular organic matter was revealed by distinctive lipid biomarkers showing bacteriohopanepolyols and lipid fatty acids characteristic for aerobic type I methanotrophs (e.g., 35-aminobacteriohopane-30,31,32,33,34-pentol), corroborating their role in aerobic methane oxidation in the redox-zone of the central Baltic Sea.

Final-revised paper