19Anaerobic oxidation of methane (AOM) coupled to sulfate reduction is mediated by, 20 respectively, anaerobic methanotrophic archaea (ANME) and sulfate reducing bacteria (SRB). 21 When a microbial community from coastal marine Lake Grevelingen sediment, containing 22 ANME-3 as the most abundant type of ANME, was incubated under a pressure gradient (0.1-40 23 MPa) for 77 days, ANME-3 was more pressure sensitive than the SRB. ANME-3 activity was 24 higher at lower (0.1, 0.45 MPa) over higher (10, 20 and 40 MPa) CH 4 total pressures. Moreover, 25 the sulfur metabolism was shifted upon changing the incubation pressure: only at 0.1 MPa 26 elemental sulfur was detected in a considerable amount and SRB of the Desulfobacterales order 27 were more enriched at elevated pressures than the Desulfubulbaceae. This study provides 28 evidence that ANME-3 can be constrained at shallow environments, despite the scarce 29 bioavailable energy, because of its pressure sensitivity. Besides, the association between ANME-30 3 and SRB can be steered by changing solely the incubation pressure.
31
Importance
32Anaerobic oxidation of methane (AOM) coupled to sulfate reduction is a biological process 33 largely occurring in marine sediments, which contributes to the removal of almost 90% of 34 sedimentary methane, thereby controlling methane emission to the atmosphere. AOM is 35 mediated by slow growing archaea, anaerobic methanotrophs (ANME) and sulfate reducing 36 bacteria. The enrichment of these microorganisms has been challenging, especially considering 37 the low solubility of methane at ambient temperature and pressure. Previous studies showed 38 strong positive correlations between the growth of ANME and the methane pressure, since the 39 higher the pressure the more methane is dissolved. In this research, a shallow marine sediment 40 3 was incubated under methane pressure gradients. The investigated effect of pressure on the 41 AOM-SR activity, the formation sulfur intermediates and the microbial community structure is 42 important to understand the pressure influence on the processes and the activity of the 43 microorganisms involved to further understand their metabolism and physiology.
48The thermodynamics of this reaction depend on the concentration of dissolved CH 4 . CH 4 is 49 poorly soluble: 1.3 mM is its concentration in sea water at ambient pressure and at 15°C (2).
50Theoretically, an elevated CH 4 pressure favors the AOM coupled to SR (AOM-SR) 51 bioconversion since i) the Gibbs free energy becomes more negative at higher CH 4 partial 52 pressures and ii) the dissolved CH 4 concentration increases and is thus more bioavailable (Table 53 1). Thus, the activity and the growth of the microorganisms mediating the process, namely 54 anaerobic methanotrophs (ANME) and sulfate reducing bacteria (SRB), is expected to be higher 55 at elevated pressures. 56 ANME are grouped into three distinct clades, i.e. ANME-1, ANME-2 and ANME-3 based on the 57 phylogenetic analysis of their 16S rRNA genes (3-5). In vitro incubations of A...