Benthic Foraminifers identify the source of displaced sediment from a sediment density flow at ~1840 m near the Seafloor Instrument Node of the Monterey Coordinated Canyon Experiment
Mary McGann1, Katherine L Maier2, Jenny A. Gales3, Charles K Paull4, Roberto Gwiazda5, James Barry6, Cristian Carvajal4, Michael Andrew Clare3, Matthieu Cartigny7, Mark R Chaffey4, Daniel R Parsons8, Thomas C O'Reilly4, Kurt J Rosenberger9, Monica Wolfson-Schwehr4, Steve Simmons10, Esther Sumner7, Peter Talling11, Jingping Xu12 and the Monterey Coordinated Canyon Experiment Team, (1)USGS Pacific Coastal and Marine Science Center Menlo Park, Menlo Park, CA, United States, (2)National Institute of Water and Atmospheric Research, Wellington, New Zealand, (3)National Oceanography Centre, Southampton, United Kingdom, (4)Monterey Bay Aquarium Research Institute, Moss Landing, CA, United States, (5)Monterey Bay Aquarium Research Institute, Moss Landing, United States, (6)Monterey Bay Aquarium Research Institute, Research, Moss Landing, CA, United States, (7)University of Southampton, National Oceanography Centre, Southampton, United Kingdom, (8)University of Hull, Energy & Environment Institute, Hull, United Kingdom, (9)U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, United States, (10)University of Hull, Hull, United Kingdom, (11)University of Durham, Earth Sciences and Geography, Durham, United Kingdom, (12)Ocean University of China, Qingdao, China
