Constant Flux Proxies and Pleistocene Sediment Accumulation Rates on the Juan de Fuca Ridge in the Northeast Pacific
Jennifer L Middleton1,2, Sujoy Mukhopadhyay3, Charles H Langmuir1, Kassandra Costa4, Jerry F McManus5, Marcelle d'Almeida6, Peter J Huybers7 and Gisela Winckler8, (1)Harvard University, Earth and Planetary Sciences, Cambridge, United States, (2)University of California Davis, Earth and Planetary Sciences, Davis, CA, United States, (3)Arizona State University, School of Earth and Space Exploration, Tempe, AZ, United States, (4)Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, United States, (5)Columbia University, Earth and Environmental Sciences, New York, United States, (6)University of California Davis, Department of Earth and Planetary Sciences, Davis, CA, United States, (7)Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA, United States, (8)Lamont-Doherty Earth Observatory of Columbia University, Palisades, United States
