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Seasonal variability of primary production in the Cap-Ferret Canyon area (Bay of Biscay) during the ECOFER cruises
Institution:1. Institut de Physique du Globe de Paris, Sorbonne Paris Cité, University Paris Diderot, UMR 7154 CNRS, 1 rue Jussieu, 75238 Paris, France;2. Biogéosciences, Université de Bourgogne Franche-Comté, UMR6282 CNRS, 21000 Dijon, France;3. IUEM, Laboratoire Domaines Océaniques, Université de Bretagne Occidentale, UMR 6538, 29820 Plouzané, France;4. London Centre for Nanotechnology and Department of Earth Sciences, University College London, 17-19 Gordon Street, WC1H 0AH, United Kingdom;5. Department of Earth and Planetary Sciences/Geotop, McGill University, 3450 University Street, Montréal, QC H3A 0E8, Canada;1. Hainan Key Laboratory of Marine Geological Resources and Environment, Hainan Geological Survey, Haikou 570206, China;2. College of Earth Sciences and Engineering, Hohai University, Nanjing 211100, China;3. Yellow River Institute of Eco-Environment Research, YRBEEA, Zhengzhou 450003, China
Abstract:Primary production measurements were carried out during the five ECOFER cruises, in order to estimate the autochtonous contribution to particulate fluxes collected at two mooring sites, in the Cap-Ferret Canyon, from June 1989 to August 1991. Primary production rates are reported in relation to levels of chlorophyll and nitrogenous nutrients in the euphotic zone. Except in early spring, the water column remains stratified until the beginning of autumn surface-water cooling. During the stratified period, maximal chlorophyll concentrations were recorded at the bottom of the photic zone, near the 1% light depth, close to the nitracline; concentrations in some profiles were greater than those measured in surface waters during the early spring bloom. From June to October, a mean daily production of 0.4 g C m?2 may be used to estimate particulate fluxes, because the recorded variability was low. During April and May, mean daily production rates can be about 3–4 times higher. Extrapolation of our data gives an estimate of yearly production from 145 to 170 g C m?2 yr?1. The possibility of greater production rates, under stratified conditions, is discussed taking into account the occurrence of changes in the depth of the chlorophyll maximum during the day; such vertical movements could be caused by internal waves, particularly at the shelf break.
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