BG5.2

Methane is one of the most important greenhouse gasses with ever-rising atmospheric concentrations. While anthropogenic sources are comparably well understood, it is still a major scientific challenge to understand and quantify the contribution of natural sources. One reason for this knowledge gap is that (bio)geochemical and geological controls on methane dynamics in aquatic and terrestrial systems as well as the spatial distribution of methane in marine and aquatic sediments, soils and permafrost areas is not well constrained.
The topics of the session will include:
- methane formation (biological and geological processes)
- subsurface fluid flow and methane/hydrocarbon transport mechanisms
- ‘marine’ methane-rich systems: e.g. gas hydrates, shallow gas, cold seep-related systems
- ‘terrestrial’ methane-rich systems: e.g. wet lands (natural & artificial), lakes (from puddles to inland seas), permafrost areas and rivers
- methane-associated (bio)geochemical reactions, microbial communities and food web structures
- methane-derived carbonates and microbe-mineral interactions
- monitoring of methane emission
- methane in paleo environments
- methane and as a new alternative energy sourcse

We aim at gathering scientists from the fields of geology, (bio/geo)chemistry, (geo)physics, modeling, (micro)biology and ecology, to evaluate our current knowledge of aquatic and terrestrial methane dynamics, interactions between element cycles and ecosystems, environmental controls and mechanisms.

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Convener: Helge Niemann | Co-convener: Alina Stadnitskaia
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| Thu, 07 May, 08:30–12:30 (CEST)

Methane is one of the most important greenhouse gasses with ever-rising atmospheric concentrations. While anthropogenic sources are comparably well understood, it is still a major scientific challenge to understand and quantify the contribution of natural sources. One reason for this knowledge gap is that (bio)geochemical and geological controls on methane dynamics in aquatic and terrestrial systems as well as the spatial distribution of methane in marine and aquatic sediments, soils and permafrost areas is not well constrained.
The topics of the session will include:
- methane formation (biological and geological processes)
- subsurface fluid flow and methane/hydrocarbon transport mechanisms
- ‘marine’ methane-rich systems: e.g. gas hydrates, shallow gas, cold seep-related systems
- ‘terrestrial’ methane-rich systems: e.g. wet lands (natural & artificial), lakes (from puddles to inland seas), permafrost areas and rivers
- methane-associated (bio)geochemical reactions, microbial communities and food web structures
- methane-derived carbonates and microbe-mineral interactions
- monitoring of methane emission
- methane in paleo environments
- methane and as a new alternative energy sourcse

We aim at gathering scientists from the fields of geology, (bio/geo)chemistry, (geo)physics, modeling, (micro)biology and ecology, to evaluate our current knowledge of aquatic and terrestrial methane dynamics, interactions between element cycles and ecosystems, environmental controls and mechanisms.

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