Planktonic carbon budget in the eastern subtropical North Atlantic

被引:27
作者
Maranon, Emilio [1 ]
Perez, Valesca
Fernandez, Emilio
Anadon, Ricardo
Bode, Antonio
Gonzalez, Natalia
Huskin, Inaki
Isla, Alejandro
Moran, Xose Anxelu G.
Mourino, Beatriz
Quevedo, Mario
Robinson, Carol
Serret, Pablo
Teira, Eva
Varela, Marta M.
Woodward, E. Malcolm S.
Zubkov, Mikhail V.
机构
[1] Univ Vigo, Dept Ecol & Biol Anim, Vigo 36210, Spain
[2] Univ Oviedo, Dept Biol Organismos & Sistemas, E-33071 Oviedo, Spain
[3] Ctr Oceanog A Coruna, Inst Espanol Oceanog, La Coruna 15001, Spain
[4] Univ Rey Juan Carlos, Escuela Super Ciencias Expt & Technol, Mostoles 28933, Spain
[5] Ctr Oceanog Xixon, Inst Ospanol Oceanog, Xixon, Spain
[6] Leibniz Inst Marine Sci, D-24105 Kiel, Germany
[7] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
[8] Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands
[9] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England
关键词
plankton; primary production; bacterial production; respiration; grazing; subtropical NE Atlantic; Atlantic meridional transect;
D O I
10.3354/ame048261
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We used data collected at > 60 stations over a 10 yr period to build the carbon budget of the plankton community in the euphotic layer of the Eastern North Atlantic Subtropical Gyre (NASE). Autotrophic biomass exceeded microbial heterotrophic biomass by a factor of 1.7. Mean ( SE), integrated chlorophyll a concentration and net particulate primary production (PP) were 17 +/- 1 Mg m(2) and 271 +/- 29 mg C m(-2) d(-1), respectively. Protist grazing on phytoplankton represented > 90% of PP. Bacterial production (BP) was 17 +/- 3 mg C m(-2) d(-1). In vitro O-2-evolution experiments indicated that net community production was -65 +/- 16 mmolO(2) m(-2) d(-1), while community respiration (CR) averaged 124 +/- 13 mmolO(2) m(-2) d-1, equivalent to 1324 +/- 142 mg C m(-2) d(-1). However, the sum of the respiration rates by each microbial group, estimated from their biomass and metabolic rates, ranged from 402 to 848 Mg C m(-2) d-1. Therefore, CR could not be reconciled with the respiratory fluxes sustained by each microbial group. Comparison between estimated gross photosynthesis by phytoplankton (481 to 616 mg C m(-2) d-1) and the sum of respiration by each group suggests that the microbial community in the NASE province is close to metabolic balance, which would agree with the observed O-2 supersaturation in the euphotic layer. Taking into account the mean open-ocean values for PP, BP, CR and bacterial growth efficiency, we show that bacteria account for approximately 20% of CR. Our results suggest that the view that bacteria dominate carbon cycling in the unproductive ocean must be reconsidered, or else that in vitro incubations misrepresent the real metabolic rates of one or several microbial groups.
引用
收藏
页码:261 / 275
页数:15
相关论文
共 70 条
  • [1] Food-web structure and elemental (C, N and P) fluxes in the eastern tropical North Atlantic
    Agusti, S
    Duarte, CM
    Vaqué, D
    Hein, M
    Gasol, JM
    Vidal, M
    [J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (10) : 2295 - 2321
  • [2] Large-scale variability in surface bacterial carbon demand and growth efficiency in the subtropical northeast Atlantic Ocean
    Alonso-Saez, Laura
    Gasol, Josep M.
    Aristegui, Javier
    Vilas, Juan C.
    Vaque, Dolors
    Duarte, Carlos M.
    Agusti, Susana
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 2007, 52 (02) : 533 - 546
  • [3] Microbial loop carbon cycling in ocean environments studied using a simple steady-state model
    Anderson, TR
    Ducklow, HW
    [J]. AQUATIC MICROBIAL ECOLOGY, 2001, 26 (01) : 37 - 49
  • [4] Dominance of bacterial metabolism in oligotrophic relative to eutrophic waters
    Biddanda, B
    Ogdahl, M
    Cotner, J
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 2001, 46 (03) : 730 - 739
  • [5] Pelagic bacteria and phytoplankton in oceanic waters near the Canary Islands in summer
    Bode, A
    Barquero, S
    Varela, M
    Braun, JG
    de Armas, D
    [J]. MARINE ECOLOGY PROGRESS SERIES, 2001, 209 : 1 - 17
  • [6] The use of oxygen microprobes to measure bacterial respiration for determining bacterioplankton growth efficiency
    Briand, E
    Pringault, O
    Jacquet, S
    Torréton, JP
    [J]. LIMNOLOGY AND OCEANOGRAPHY-METHODS, 2004, 2 : 406 - 416
  • [7] Buck KR, 1996, AQUAT MICROB ECOL, V10, P283
  • [8] THE CONTRIBUTION OF MICROORGANISMS TO PARTICULATE CARBON AND NITROGEN IN SURFACE WATERS OF THE SARGASSO SEA NEAR BERMUDA
    CARON, DA
    DAM, HG
    KREMER, P
    LESSARD, EJ
    MADIN, LP
    MALONE, TC
    NAPP, JM
    PEELE, ER
    ROMAN, MR
    YOUNGBLUTH, MJ
    [J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1995, 42 (06) : 943 - 972
  • [9] BIOGEOCHEMICAL SIGNIFICANCE OF BACTERIAL BIOMASS IN THE OCEANS EUPHOTIC ZONE
    CHO, BC
    AZAM, F
    [J]. MARINE ECOLOGY PROGRESS SERIES, 1990, 63 (2-3) : 253 - 259
  • [10] Light dependence of [3H]leucine incorporation in the oligotrophic North Pacific ocean
    Church, MJ
    Ducklow, HW
    Karl, DA
    [J]. APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2004, 70 (07) : 4079 - 4087