The Experts below are selected from a list of 285 Experts worldwide ranked by ideXlab platform
Mathieu Rembauville - One of the best experts on this subject based on the ideXlab platform.
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export fluxes in a naturally iron fertilized area of the southern ocean part 1 seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
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Export fluxes in a naturally iron-fertilized area of the Southern Ocean – Part 1: Seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
Stephane Blain - One of the best experts on this subject based on the ideXlab platform.
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export fluxes in a naturally iron fertilized area of the southern ocean part 1 seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
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Export fluxes in a naturally iron-fertilized area of the Southern Ocean – Part 1: Seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
Ian Salter - One of the best experts on this subject based on the ideXlab platform.
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export fluxes in a naturally iron fertilized area of the southern ocean part 1 seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
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Export fluxes in a naturally iron-fertilized area of the Southern Ocean – Part 1: Seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
Nathalie Leblond - One of the best experts on this subject based on the ideXlab platform.
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export fluxes in a naturally iron fertilized area of the southern ocean part 1 seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
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Export fluxes in a naturally iron-fertilized area of the Southern Ocean – Part 1: Seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
A Gueneugues - One of the best experts on this subject based on the ideXlab platform.
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export fluxes in a naturally iron fertilized area of the southern ocean part 1 seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.
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Export fluxes in a naturally iron-fertilized area of the Southern Ocean – Part 1: Seasonal dynamics of Particulate Organic Carbon export from a moored sediment trap
Biogeosciences, 2015Co-Authors: Mathieu Rembauville, Ian Salter, Nathalie Leblond, A Gueneugues, Stephane BlainAbstract:Abstract. A sediment trap moored in the naturally iron-fertilized Kerguelen Plateau in the Southern Ocean provided an annual record of Particulate Organic Carbon and nitrogen fluxes at 289 m. At the trap deployment depth, current speeds were typically low (~ 10 cm s−1) and primarily tidal-driven (M2 tidal component). Although advection was weak, the sediment trap may have been subject to hydrodynamical and biological (swimmer feeding on trap funnel) biases. Particulate Organic Carbon (POC) flux was generally low ( 2 km) fluxes measured from similarly productive iron-fertilized blooms. Although undertrapping cannot be excluded in shallow moored sediment trap deployment, we hypothesize that grazing pressure, including mesozooplankton and mesopelagic fishes, may be responsible for the low POC flux beneath the base of the winter mixed layer. The importance of plankton community structure in controlling the temporal variability of export fluxes is addressed in a companion paper.