Particle flux in the northeast Atlantic Ocean during the POMME experiment (2001): Results from mass, carbon, nitrogen, and lipid biomarkers from the drifting sediment traps

Madeleine Goutx, Catherine Guigue, Nathalie Leblond, Anne Desnues, Aurélie Dufour, Diego Aritio, Cecile Guieu

Research output: Contribution to journalArticle

Abstract

During 48 hour stations during the three Programme Océan Multidisciplinaire M-aceso Echelle (POMME) cruises in 2001 (late winter, spring, and late summer) at different locations within the region studied (38°-45°N, 15°-21°W), drifting sediment traps were deployed at 200 m and 400 m. Fluxes increased from late winter (POMME 1) to spring (POMME 2), with highest values in the North Atlantic gyre (109.1, 20.1, and 3.5 mg m2 d-1 for mass, C, and N, respectively) and decreased during POMME 3 to reach threshold values (19.1 ± 6.0, 4.4 ± 1.1, and 0.7 ± 0.2 mg m-2 d-1, respectively). Lipid class tracers and their fatty acid composition analyzed by gaseous chromatography were used to assess the quality and quantity of organic matter fluxes. Wide seasonal variability was observed in biogenic lipid fluxes (0.42 ± 0.19 and 0.39 ± 0.13 mg m-2 d-1, 1.78 ± 1.08, and 0.69 ± 0.56 mg m-2 d-1, and 0.71 ± 0.14 and 0.45 mg m-2 d-1 on average at 200 m and 400 m during late winter, spring, and late summer, respectively) in relation with the development of the spring phytoplankton bloom. In a northern persistent anticyclonic eddy a major export of algal matter occurred through zooplankton activity. In contrast with this pattern, the southernmost anticyclonic eddy exhibited the lowest particle fluxes in relation to the low productivity and the high bacterial carbon demand prevailing in the surface waters. In the main cyclonic structure (C4) and the saddle zone (during POMME 2) the pattern of lipid biotracers reflected the permanence of a zooplankton community and likely advective transfer of matter between 43.5°N and 42°N through sidbsurface water circulation.

Original languageEnglish (US)
Pages (from-to)1-15
Number of pages15
JournalJournal of Geophysical Research C: Oceans
Volume110
Issue number7
DOIs
StatePublished - Jul 8 2005

Fingerprint

Sediment traps
Atlantic Ocean
biomarkers
Biomarkers
sediment trap
flux (rate)
lipids
biomarker
sediments
Nitrogen
Carbon
lipid
traps
Fluxes
Lipids
nitrogen
zooplankton
carbon
winter
ocean

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Particle flux in the northeast Atlantic Ocean during the POMME experiment (2001) : Results from mass, carbon, nitrogen, and lipid biomarkers from the drifting sediment traps. / Goutx, Madeleine; Guigue, Catherine; Leblond, Nathalie; Desnues, Anne; Dufour, Aurélie; Aritio, Diego; Guieu, Cecile.

In: Journal of Geophysical Research C: Oceans, Vol. 110, No. 7, 08.07.2005, p. 1-15.

Research output: Contribution to journalArticle

@article{712776d9e68f4b4c8647e4125c003292,
title = "Particle flux in the northeast Atlantic Ocean during the POMME experiment (2001): Results from mass, carbon, nitrogen, and lipid biomarkers from the drifting sediment traps",
abstract = "During 48 hour stations during the three Programme Oc{\'e}an Multidisciplinaire M-aceso Echelle (POMME) cruises in 2001 (late winter, spring, and late summer) at different locations within the region studied (38°-45°N, 15°-21°W), drifting sediment traps were deployed at 200 m and 400 m. Fluxes increased from late winter (POMME 1) to spring (POMME 2), with highest values in the North Atlantic gyre (109.1, 20.1, and 3.5 mg m2 d-1 for mass, C, and N, respectively) and decreased during POMME 3 to reach threshold values (19.1 ± 6.0, 4.4 ± 1.1, and 0.7 ± 0.2 mg m-2 d-1, respectively). Lipid class tracers and their fatty acid composition analyzed by gaseous chromatography were used to assess the quality and quantity of organic matter fluxes. Wide seasonal variability was observed in biogenic lipid fluxes (0.42 ± 0.19 and 0.39 ± 0.13 mg m-2 d-1, 1.78 ± 1.08, and 0.69 ± 0.56 mg m-2 d-1, and 0.71 ± 0.14 and 0.45 mg m-2 d-1 on average at 200 m and 400 m during late winter, spring, and late summer, respectively) in relation with the development of the spring phytoplankton bloom. In a northern persistent anticyclonic eddy a major export of algal matter occurred through zooplankton activity. In contrast with this pattern, the southernmost anticyclonic eddy exhibited the lowest particle fluxes in relation to the low productivity and the high bacterial carbon demand prevailing in the surface waters. In the main cyclonic structure (C4) and the saddle zone (during POMME 2) the pattern of lipid biotracers reflected the permanence of a zooplankton community and likely advective transfer of matter between 43.5°N and 42°N through sidbsurface water circulation.",
author = "Madeleine Goutx and Catherine Guigue and Nathalie Leblond and Anne Desnues and Aur{\'e}lie Dufour and Diego Aritio and Cecile Guieu",
year = "2005",
month = "7",
day = "8",
doi = "10.1029/2004JC002749",
language = "English (US)",
volume = "110",
pages = "1--15",
journal = "Journal of Geophysical Research: Space Physics",
issn = "0148-0227",
publisher = "Wiley-Blackwell",
number = "7",

}

TY - JOUR

T1 - Particle flux in the northeast Atlantic Ocean during the POMME experiment (2001)

T2 - Results from mass, carbon, nitrogen, and lipid biomarkers from the drifting sediment traps

AU - Goutx, Madeleine

AU - Guigue, Catherine

AU - Leblond, Nathalie

AU - Desnues, Anne

AU - Dufour, Aurélie

AU - Aritio, Diego

AU - Guieu, Cecile

PY - 2005/7/8

Y1 - 2005/7/8

N2 - During 48 hour stations during the three Programme Océan Multidisciplinaire M-aceso Echelle (POMME) cruises in 2001 (late winter, spring, and late summer) at different locations within the region studied (38°-45°N, 15°-21°W), drifting sediment traps were deployed at 200 m and 400 m. Fluxes increased from late winter (POMME 1) to spring (POMME 2), with highest values in the North Atlantic gyre (109.1, 20.1, and 3.5 mg m2 d-1 for mass, C, and N, respectively) and decreased during POMME 3 to reach threshold values (19.1 ± 6.0, 4.4 ± 1.1, and 0.7 ± 0.2 mg m-2 d-1, respectively). Lipid class tracers and their fatty acid composition analyzed by gaseous chromatography were used to assess the quality and quantity of organic matter fluxes. Wide seasonal variability was observed in biogenic lipid fluxes (0.42 ± 0.19 and 0.39 ± 0.13 mg m-2 d-1, 1.78 ± 1.08, and 0.69 ± 0.56 mg m-2 d-1, and 0.71 ± 0.14 and 0.45 mg m-2 d-1 on average at 200 m and 400 m during late winter, spring, and late summer, respectively) in relation with the development of the spring phytoplankton bloom. In a northern persistent anticyclonic eddy a major export of algal matter occurred through zooplankton activity. In contrast with this pattern, the southernmost anticyclonic eddy exhibited the lowest particle fluxes in relation to the low productivity and the high bacterial carbon demand prevailing in the surface waters. In the main cyclonic structure (C4) and the saddle zone (during POMME 2) the pattern of lipid biotracers reflected the permanence of a zooplankton community and likely advective transfer of matter between 43.5°N and 42°N through sidbsurface water circulation.

AB - During 48 hour stations during the three Programme Océan Multidisciplinaire M-aceso Echelle (POMME) cruises in 2001 (late winter, spring, and late summer) at different locations within the region studied (38°-45°N, 15°-21°W), drifting sediment traps were deployed at 200 m and 400 m. Fluxes increased from late winter (POMME 1) to spring (POMME 2), with highest values in the North Atlantic gyre (109.1, 20.1, and 3.5 mg m2 d-1 for mass, C, and N, respectively) and decreased during POMME 3 to reach threshold values (19.1 ± 6.0, 4.4 ± 1.1, and 0.7 ± 0.2 mg m-2 d-1, respectively). Lipid class tracers and their fatty acid composition analyzed by gaseous chromatography were used to assess the quality and quantity of organic matter fluxes. Wide seasonal variability was observed in biogenic lipid fluxes (0.42 ± 0.19 and 0.39 ± 0.13 mg m-2 d-1, 1.78 ± 1.08, and 0.69 ± 0.56 mg m-2 d-1, and 0.71 ± 0.14 and 0.45 mg m-2 d-1 on average at 200 m and 400 m during late winter, spring, and late summer, respectively) in relation with the development of the spring phytoplankton bloom. In a northern persistent anticyclonic eddy a major export of algal matter occurred through zooplankton activity. In contrast with this pattern, the southernmost anticyclonic eddy exhibited the lowest particle fluxes in relation to the low productivity and the high bacterial carbon demand prevailing in the surface waters. In the main cyclonic structure (C4) and the saddle zone (during POMME 2) the pattern of lipid biotracers reflected the permanence of a zooplankton community and likely advective transfer of matter between 43.5°N and 42°N through sidbsurface water circulation.

UR - http://www.scopus.com/inward/record.url?scp=24944515273&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=24944515273&partnerID=8YFLogxK

U2 - 10.1029/2004JC002749

DO - 10.1029/2004JC002749

M3 - Article

AN - SCOPUS:24944515273

VL - 110

SP - 1

EP - 15

JO - Journal of Geophysical Research: Space Physics

JF - Journal of Geophysical Research: Space Physics

SN - 0148-0227

IS - 7

ER -