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Cold-seep habitat mapping: High-resolution spatial characterization of the Blake Ridge Diapir seep field
Institution:1. Department of Earth Sciences, Sapienza University of Rome, P.le A. Moro 5, 00185 Rome, Italy;2. CNR-IGAG (Istituto di Geologia Ambientale e Geoingegneria), UOS Roma, P.le A. Moro, 5, 00185, Rome, Italy;3. Institut de Ciències del Mar, Consejo Superior de Investigaciones Cientificas, Pg. Marítim de la Barceloneta 37–49, 08003 Barcelona, Spain;1. Benthic Habitat Research Group, Institute of Marine Research, PO Box 1870 Nordnes, N-5817 Bergen, Norway;2. Geological Survey of Norway, PO Box 6315 Sluppen, N-7491 Trondheim, Norway;1. Laboratoire de Planétologie et Géodynamique Bio-Indicateur Actuels et Fossiles, LPG-BIAF, CNRS - UMR 6112, Université d''Angers UFR Sciences, CNRS, 2 Boulevard Lavoisier, 49000 Angers, France;2. Laboratoire Littoral Environnement Télédétection Géomatique, LETG, CNRS – UMR 6554, Université de Nantes, Campus Tertre, BP 81227 44312 Nantes Cedex 3, France;3. LUSAC, EA 4253, Normandie Univ, Unicaen, 50100 Cherbourg, France;4. Cnam/Intechmer, 50100 Cherbourg, France;5. Laboratoire de recherche en Hydrodynamique, Énergétique et Environnement Atmosphérique, LHEEA, CNRS – UMR 6598, École Centrale de Nantes - SEM-REV, 1 Rue de la Noë, BP 92101 44321 Nantes Cedex 3, France
Abstract:Relationships among seep community biomass, diversity, and physiographic controls such as underlying geology are not well understood. Previous efforts to constrain these relationships at the Blake Ridge Diapir were limited to observations from piloted deep-submergence vehicles. In August 2012, the autonomous underwater vehicle (AUV) Sentry collected geophysical and photographic data over a 0.131 km2 area at the Blake Ridge Diapir seeps. A nested survey approach was used that began with a regional or reconnaissance-style survey using sub-bottom mapping systems to locate and identify seeps and underlying conduits. This survey was followed by AUV-mounted sidescan sonar and multibeam echosounder systems mapping on a mesoscale to characterize the seabed physiography. At the most detailed survey level, digital photographic imaging was used to resolve sub-meter characteristics of the biology. Four pockmarks (25–70 m diameter) were documented, each supporting chemosynthetic communities. Concentric zonation of mussels and clams suggests the influence of chemical gradients on megafaunal distribution. Data collection and analytical techniques used here yield high-resolution habitat maps that can serve as baselines to constrain temporal evolution of seafloor seeps, and to inform ecological niche modeling and resource management.
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