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McNichol, Jesse C.; Stryhanyuk, Hryhoriy; Sylva, Sean P.; Thomas, François; Musat, Niculina; Seewald, Jeffrey S.; Sievert, Stefan M. (National Academy of Sciences, 2018-06-11)The existence of a chemosynthetic subseafloor biosphere was immediately recognized when deep-sea hot springs were discovered in 1977. However, quantifying how much new carbon is fixed in this environment has remained ...
Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma) Ostrander, Chadlin; Owens, Jeremy D.; Nielsen, Sune G. (American Association for the Advancement of Science, 2017-08-09)The rates of marine deoxygenation leading to Cretaceous Oceanic Anoxic Events are poorly recognized and constrained. If increases in primary productivity are the primary driver of these episodes, progressive oxygen loss ...
Holmquist, James R.; Windham-Myers, Lisamarie; Bernal, Blanca; Byrd, Kristin B.; Crooks, Stephen; Gonneea, Meagan E.; Herold, Nate; Knox, Sara H.; Kroeger, Kevin D.; McCombs, John; Megonigal, J. Patrick; Lu, Meng; Morris, James T.; Sutton-Grier, Ariana E.; Troxler, Tiffany G. (IOP Science, 2018-11-12)Coastal wetlands store carbon dioxide (CO2) and emit CO2 and methane (CH4) making them an important part of greenhouse gas (GHG) inventorying. In the contiguous United States (CONUS), a coastal wetland inventory was recently ...