Marine sediments are the world's largest known reservoir of methane. In many coastal
regions, methane is trapped in sediments buried at depths ranging from centimeters to …

Anaerobic oxidation of methane (AOM) is a microbial process that consumes dissolved
methane (CH 4) in anoxic sediments and soils and mitigates CH 4 release to the …

Microbial production of methane is an important terminal metabolic process during organic
matter degradation in marine sediments. It is generally acknowledged that hydrogenotrophic …

Key features: Captures the historic context and recent developments in science and policy
arenas that address the potential for coastal wetlands to be considered as significant …

Inland waters are increasingly recognized as critical sites of methane emissions to the
atmosphere, but the biogeochemical reactions driving such fluxes are less well understood …

Methane concentrations in the water column and emissions to the atmosphere were
determined for three tropical coastal lagoons surrounded by mangrove forests on the …

Knowledge regarding the diversity of methanogenic archaeal communities in hypersaline
environments is limited because of the lack of efficient cultivation efforts as well as their low …

Vegetated coastal ecosystems (VCEs; ie, mangroves, saltmarshes, and seagrasses)
represent important sources of natural methane emission. Despite recent advances in the …

Mangroves are known to sequester carbon at rates exceeding even those of other tropical
forests; however, to understand carbon cycling in these systems, soil-atmosphere fluxes and …

The biogeochemistry of sulfur and carbon during early-diagenetic processes within organic-
rich marine mangrove sediments was studied in the “Manche à Eau” lagoon, Guadeloupe …