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• W2020129317 abstract "MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 256:13-27 (2003) - doi:10.3354/meps256013 Phytoplankton production in the North Water Polynya: size-fractions and carbon fluxes, April to July 1998 Zhi-Ping Mei1,6,*, Louis Legendre1,2, Yves Gratton3, Jean-Éric Tremblay4, Bernard LeBlanc1, Bert Klein1, Michel Gosselin5 1GIROQ, Department of Biology, Laval University, Sainte-Foy, Québec G1K 7P4, Canada 2Laboratoire d¹Océanographie de Villefranche (LOV), BP 28, 06234 Villefranche-sur-Mer Cedex, France 3INRS-Eau, 2800 rue Einstein, Sainte-Foy, Québec G1K 4C7, Canada 4McGill University, Department of Biology, 1205 Dr. Penfield, Montreal, Québec H3A 1B1, Canada 5Institut des sciences de la mer (ISMER), Université du Québec à Rimouski, 310 Allée des Ursulines, Rimouski, Québec G5L 3A1, Canada 6Present address: Institut des sciences de la mer (ISMER), Université du Québec à Rimouski, 310 Allée des Ursulines, Rimouski, Québec G5L 3A1, Canada *Email: zhi-ping.mei@uqar.qc.ca ABSTRACT: In order to understand the mechanisms responsible for the high productivity and biogeochemical cycling of carbon in the North Water Polynya (NOW), we determined physical properties and nutrient concentrations of the upper water column, and phytoplankton production, during spring/summer (April to July) 1998. Phytoplankton production of total organic carbon (PTOC) was partitioned into production of dissolved and particulate organic carbon (PDOC and PPOC, respectively), the latter being further partitioned into production of large and small phytoplankton (PL and PS, respectively) using 5 µm as threshold. The highest PTOC was 6 gC m-2 d-1 at peak bloom. The fraction of PDOC in PTOC was lower in periods of high PTOC than those of low PTOC. Averaged over the whole polynya for the sampling period, PDOC and PPOC accounted for 34 and 66% of the fixed carbon, respectively, and 81 and 19% of PPOC were in the PL and PS fractions, respectively. Variations in the integrated assimilation numbers of large and small phytoplankton were mostly explained by nutrients and irradiance. Even though PPOC was dominated by large phytoplankton, the sinking rates of the phytoplankton cells were relatively low (0 to 0.7 m d-1), hence low export of PPOC to depth (17%), and relatively high potential transfer to large pelagic organisms through the herbivorous food web. This explains why the NOW is a major feeding and spawning area for fish, mammals and birds. KEY WORDS: Primary production · Phytoplankton biomass · Dissolved organic carbon · Particulate organic carbon · PBopt · Export · Biogeochemical cycling · North Water (NOW) Polynya Full text in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 256. Online publication date: July 17, 2003 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2003 Inter-Research." @default.
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• W2020129317 date "2003-01-01" @default.
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• W2020129317 title "Phytoplankton production in the North Water Polynya: size-fractions and carbon fluxes, April to July 1998" @default.
• W2020129317 cites W1488584644 @default.
• W2020129317 cites W1539227095 @default.
• W2020129317 cites W1754304843 @default.
• W2020129317 cites W1965624816 @default.
• W2020129317 cites W1965645800 @default.
• W2020129317 cites W1965801259 @default.
• W2020129317 cites W1966636533 @default.
• W2020129317 cites W1967781798 @default.
• W2020129317 cites W1972015729 @default.
• W2020129317 cites W1973644811 @default.
• W2020129317 cites W1974403017 @default.
• W2020129317 cites W1974409700 @default.
• W2020129317 cites W1976181659 @default.
• W2020129317 cites W1979222613 @default.
• W2020129317 cites W1982236333 @default.
• W2020129317 cites W1982658513 @default.
• W2020129317 cites W1982925205 @default.
• W2020129317 cites W1983026648 @default.
• W2020129317 cites W1985849949 @default.
• W2020129317 cites W1986963144 @default.
• W2020129317 cites W1988392661 @default.
• W2020129317 cites W1992014556 @default.
• W2020129317 cites W1994178044 @default.
• W2020129317 cites W1997929646 @default.
• W2020129317 cites W1998293680 @default.
• W2020129317 cites W2005006578 @default.
• W2020129317 cites W2007465231 @default.
• W2020129317 cites W2017901741 @default.
• W2020129317 cites W2019697937 @default.
• W2020129317 cites W2022996522 @default.
• W2020129317 cites W2023727639 @default.
• W2020129317 cites W2027418741 @default.
• W2020129317 cites W2036166609 @default.
• W2020129317 cites W2037509287 @default.
• W2020129317 cites W2039781035 @default.
• W2020129317 cites W2043925622 @default.
• W2020129317 cites W2048732593 @default.
• W2020129317 cites W2055300166 @default.
• W2020129317 cites W2061327448 @default.
• W2020129317 cites W2065141406 @default.
• W2020129317 cites W2066376163 @default.
• W2020129317 cites W2070539490 @default.
• W2020129317 cites W2073165315 @default.
• W2020129317 cites W2073470504 @default.
• W2020129317 cites W2074260957 @default.
• W2020129317 cites W2076607489 @default.
• W2020129317 cites W2081297498 @default.
• W2020129317 cites W2090617924 @default.
• W2020129317 cites W2094672189 @default.
• W2020129317 cites W2094836065 @default.
• W2020129317 cites W2095024266 @default.
• W2020129317 cites W2095283170 @default.
• W2020129317 cites W2105288518 @default.
• W2020129317 cites W2105796581 @default.
• W2020129317 cites W2110516330 @default.
• W2020129317 cites W2119301253 @default.
• W2020129317 cites W2121041595 @default.
• W2020129317 cites W2126692524 @default.
• W2020129317 cites W2126722179 @default.
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• W2020129317 cites W2130689769 @default.
• W2020129317 cites W2135743399 @default.
• W2020129317 cites W2139782989 @default.
• W2020129317 cites W2155390904 @default.
• W2020129317 cites W2165503280 @default.
• W2020129317 cites W2171280987 @default.
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