Geomicrobiology of the Deep Biosphere
Geomicrobiology of the Deep Biosphere
Session ID#: 121259
Session Description:
Earth’s subsurface is home to distinctive microbial ecosystems – often called the “deep biosphere.” Microbial activity in the terrestrial and marine deep biosphere drives global geochemical cycles, yet processes are poorly constrained. In addition, some microbial communities can persist over geological time periods despite energy-starvation, and they can revive after prolonged periods of dormancy. Unlocking the secrets of this biosphere is thus important for understanding how life survives “buried alive” and harnesses available energy sources, which has implications for the search for life elsewhere in the universe. The deep biosphere is also vulnerable and relevant to human activities such as mining, fracking, waste disposal, and carbon capture and sequestration industries. In this session, we invite presentations of the form, function, and geomicrobiology of Earth’s subsurface environments, of how the deep biosphere responds to perturbations, and of the astrobiological translation to the habitability of other planetary bodies.
Index Terms:
0414 Biogeochemical cycles, processes, and modeling [BIOGEOSCIENCES]
0448 Geomicrobiology [BIOGEOSCIENCES]
0456 Life in extreme environments [BIOGEOSCIENCES]
4840 Microbiology and microbial ecology [OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL]
Primary Convener: Beth Orcutt, Bigelow Laboratory for Ocean Sciences, East Boothbay, ME, United States
Conveners: Magdalena R Osburn, Northwestern University, Earth and Planetary Sciences, Evanston, IL, United States, James Andrew Bradley, Queen Mary, University of London, London, United Kingdom and Julie A Huber, Woods Hole Oceanographic Institution, Woods Hole, MA, United States
Primary Liaison: Beth Orcutt, Bigelow Laboratory for Ocean Sciences, East Boothbay, ME, United States
See more of: Biogeosciences