“…Conversely, Posidonia (particularly Harderode) and Alum shale samples would contain an active hydrocarbon-degrading methane-producing community. The actual current in situ transformation of residual hydrocarbons to methane and CO 2 , however, will eventually rely on other factors such as current temperature, availability of water, salinity, N, P and other micronutrients, listed by Schlegel et al (2013). On the other hand, the presence of toxic substances could inhibit microbial growth, whereas at sulphate concentrations high enough (Siegert et al, 2011) methanogens would probably be out-competed by sulphate reducers.…”