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Ocean-bottom sediments tell a story about ancient Greenland summers

 E-Mail IMAGE: Ocean-bottom sediments, shown after materials such as leaf wax chemicals have been extracted. These sediments collected in 1985 by the Ocean Drilling Program were processed recently at UB. view more  Credit: Douglas Levere / University at Buffalo BUFFALO, N.Y. Over hundreds of thousands of years, sediments from southern Greenland have been making their way into the ocean, where they re carried by underwater currents to a location in the Labrador Sea called the Eirik Drift. Here, they settle on the ocean floor, where they form a record of history, accumulating in layers that document the environmental past of the lands from which they came.

Multiple carbon incorporation strategies support microbial survival in cold subseafloor crustal fluids

19). Decreasing cell concentrations after drilling has also been observed in other CORKs [Juan de Fuca ridge flank; ( 21)] and groundwater well systems ( 5)], low cell counts likely indicate that the North Pond system had recovered from drilling and that the 2017 fluids (and resulting data) are the best representation of microbial activity in the cold, oxic crustal subseafloor aquifer to date. Table 1 North Pond CORK fluids and bottom water values for cell enumeration, dissolved inorganic carbon (DIC), and dissolved organic carbon (DOC) from 2017 samples collected for this study. Additional geochemistry (oxygen, nitrate, and pH) reproduced from ( 5) also collected in 2017. Ammonium concentrations were all below detection (

New Geology articles published online ahead of print in April

reconstructed from sub-ice shelf and offshore sediments J.A. Smith; C.-D. Hillenbrand; C. Subt; B.E. Rosenheim; T. Frederichs . Abstract: Because ice shelves respond to climatic forcing over a range of time scales, from years to millennia, an understanding of their long-term history is critically needed for predicting their future evolution. We present the first detailed reconstruction of the Larsen C Ice Shelf (LCIS), eastern Antarctic Peninsula (AP), based on data from sediment cores recovered from below and in front of the ice shelf. Sedimentologic and chronologic information reveals that the grounding line (GL) of an expanded AP ice sheet had started its retreat from the midshelf prior to 17.7 ± 0.53

Modeling the probability of methane hydrate deposits on the seafloor

 E-Mail IMAGE: Using Sandia National Laboratories longstanding expertise in probabi­listic modeling and machine learning algorithms from the U.S. Naval Research Laboratory, the researchers determined the probabil­ity of finding methane hydrate off the. view more  Credit: Image courtesy of William Eymold/Sandia National Laboratories RALEIGH, N.C. Methane hydrate, an ice-like material made of compressed natural gas, burns when lit and can be found in some regions of the seafloor and in Arctic permafrost. Thought to be the world s largest source of natural gas, methane hydrate is a potential fuel source, and if it melts and methane gas is released into the atmosphere, it is a potent greenhouse gas. For these reasons, knowing where methane hydrate might be located, and how much is likely there, is important.

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