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Plate Tectonics Fuels a Vast Underground Ecosystem

The subsurface is among Earth’s largest biomes, but the extent to which microbial communities vary across tectonic plate boundaries or interact with subduction-scale geological processes remains unknown. In a recently published study, scientists compare bacterial community composition with deep-subsurface geochemistry from 21 hot springs across the Costa Rican convergent margin.

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Where Iron and Water Mix

A new study by researchers from University of Washington (UW), Woods Hole Oceanographic Institution (WHOI), and the University of Southern California, demonstrates that chemical-laden plumes erupted from vents at one section of Mid Ocean Ridge in the SE Pacific can be traced all the way across the Pacific for more than 4000 kilometers.  Further, the study shows how the iron transported by this process is ultimately brought to the surface oceans of Antarctica where it is serves as a key life-sustaining micro-nutrient supporting up to 30 percent of all the organic carbon uptake in that ocean. 

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Researchers from WHOI and MBL Receive $1.2 Million Grant for Collaborative Salt-Marsh Study

Researchers from WHOI and MBL Receive $1.2 Million Grant for Collaborative Salt-Marsh Study

Scientists from the Marine Biological Laboratory (MBL) and the Woods Hole Oceanographic Institution (WHOI) were recently awarded a $1.2 million collaborative grant from the National Science Foundation (NSF) for studies on the role of sulfur-oxidizing bacteria in salt marsh nitrogen and carbon cycling. The fieldwork will be conducted at the Plum Island Ecosystem Long-Term Ecological Research (LTER) site on the North Shore of Boston.

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