School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom; School of Geography, Earth and Environmental Sciences, Plymouth University, Drake Circus, Plymouth, Devon, PL4 8AA, United Kingdom; School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, Southampton, SO14 3ZH, United Kingdom; Department of Earth Sciences, University of California, Riverside, CA 92521, United States; MARUM - Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, Bremen, 28359, Germany; NERC Isotope Geosciences Facilities, British Geological Survey, Nottingham, NG12 5GG, United Kingdom; Organic Geochemistry Unit, Cabot Institute, School of Chemistry, University of Bristol, Bristol, BS8 1TS, United Kingdom; Departamento de Ciencias de la Tierra, Instituto Universitario de Ciencias Ambientales, Universidad de Zaragoza, Zaragoza, 50009, Spain; Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool, L69 3GP, United Kingdom; Centre for Environmental Geochemistry, University of Nottingham, Nottingham, NG7 2RD, United Kingdom
Recommended Citation:
Dunkley Jones T.,Manners H.R.,Hoggett M.,et al. Dynamics of sediment flux to a bathyal continental margin section through the Paleocene-Eocene Thermal Maximum[J]. Climate of the Past,2018-01-01,14(7)