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

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 c...

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Published in:Biogeosciences
Main Authors: M. Rembauville, I. Salter, N. Leblond, A. Gueneugues, S. Blain
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://doi.org/10.5194/bg-12-3153-2015
https://doaj.org/article/4fef684294e949e3bdb7c8bad580ab37
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spelling ftdoajarticles:oai:doaj.org/article:4fef684294e949e3bdb7c8bad580ab37 2023-05-15T18:25:10+02:00 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 M. Rembauville I. Salter N. Leblond A. Gueneugues S. Blain 2015-06-01T00:00:00Z https://doi.org/10.5194/bg-12-3153-2015 https://doaj.org/article/4fef684294e949e3bdb7c8bad580ab37 EN eng Copernicus Publications https://www.biogeosciences.net/12/3153/2015/bg-12-3153-2015.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-12-3153-2015 1726-4170 1726-4189 https://doaj.org/article/4fef684294e949e3bdb7c8bad580ab37 Biogeosciences, Vol 12, Pp 3153-3170 (2015) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2015 ftdoajarticles https://doi.org/10.5194/bg-12-3153-2015 2022-12-31T15:36:33Z 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 (< 0.5 mmol m −2 d −1 ), although two episodic export events (< 14 days) of 1.5 mmol m −2 d −1 were recorded. These increases in flux occurred with a 1-month time lag from peaks in surface chlorophyll and together accounted for approximately 40% of the annual flux budget. The annual POC flux of 98.2 ± 4.4 mmol m −2 yr −1 was low considering the shallow deployment depth but comparable to independent estimates made at similar depths (~ 300 m) over the plateau, and to deep-ocean (> 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. Article in Journal/Newspaper Southern Ocean Directory of Open Access Journals: DOAJ Articles Kerguelen Southern Ocean Biogeosciences 12 11 3153 3170
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
M. Rembauville
I. Salter
N. Leblond
A. Gueneugues
S. Blain
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
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
description 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 (< 0.5 mmol m −2 d −1 ), although two episodic export events (< 14 days) of 1.5 mmol m −2 d −1 were recorded. These increases in flux occurred with a 1-month time lag from peaks in surface chlorophyll and together accounted for approximately 40% of the annual flux budget. The annual POC flux of 98.2 ± 4.4 mmol m −2 yr −1 was low considering the shallow deployment depth but comparable to independent estimates made at similar depths (~ 300 m) over the plateau, and to deep-ocean (> 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.
format Article in Journal/Newspaper
author M. Rembauville
I. Salter
N. Leblond
A. Gueneugues
S. Blain
author_facet M. Rembauville
I. Salter
N. Leblond
A. Gueneugues
S. Blain
author_sort M. Rembauville
title 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
title_short 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
title_full 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
title_fullStr 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
title_full_unstemmed 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
title_sort 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
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/bg-12-3153-2015
https://doaj.org/article/4fef684294e949e3bdb7c8bad580ab37
geographic Kerguelen
Southern Ocean
geographic_facet Kerguelen
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source Biogeosciences, Vol 12, Pp 3153-3170 (2015)
op_relation https://www.biogeosciences.net/12/3153/2015/bg-12-3153-2015.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
doi:10.5194/bg-12-3153-2015
1726-4170
1726-4189
https://doaj.org/article/4fef684294e949e3bdb7c8bad580ab37
op_doi https://doi.org/10.5194/bg-12-3153-2015
container_title Biogeosciences
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