Annual benthic metabolism and organic carbon fluxes in a semi-enclosed Mediterranean bay dominated by the macroalgae Caulerpa prolifera

被引:8
作者
Ruiz-Halpern, Sergio [1 ,2 ]
Vaquer-Sunyer, Raquel [2 ,3 ]
Duarte, Carlos M. [2 ,4 ]
机构
[1] Southern Cross Univ, Sch Environm Sci & Engn, Ctr Coastal Biogeochem, 1 Mil Rd, Lismore, NSW 2480, Australia
[2] Univ Illes Balears, CSIC, Inst Mediterrani Estudis Avancats, Dept Global Change, Esporles, Spain
[3] Univ Balearic Isl, Dept Biol, Interdisciplinary Ecol Grp, Palma De Mallorca, Spain
[4] Univ Western Australia, UWA Oceans Inst, Sch Plant Biol, Crawley, WA, Australia
关键词
dissolved organic carbon (DOC); exchangeable dissolved organic carbon (EDOC); volatile organic carbon (VOC); macroalgae; carbon cycling; metabolism; fluxes; production; SEAGRASS POSIDONIA-OCEANICA; TEMPERATURE; EXCHANGE; MACROFAUNA; DEPOSITION; EXCRETION; DYNAMICS; CLIMATE; MEADOW; FATE;
D O I
10.3389/fmars.2014.00067
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Coastal areas play an important role on carbon cycling. Elucidating the dynamics on the production, transport, and fate of organic carbon (OC) is relevant to gain a better understanding on the role coastal areas play in the global carbon budget. Here, we assess the metabolic status and associated OC fluxes of a semi-enclosed Mediterranean bay supporting a meadow of Caulerpa prolifera. We test whether the EDOC pool is a significant component of the OC pool and associated fluxes in this ecosystem. The Bay of Portocolom was in net metabolic balance on a yearly basis, but heterotrophic during the summer months. Community respiration (CR) was positively correlated to C. prolifera biomass, while net community production (NCP) had a negative correlation. The benthic compartment represented, on average, 72.6 +/- 5.2% of CR and 86.8 +/- 4.5% of gross primary production (GPP). Dissolved organic carbon (DOC) production peaked in summer and was always positive, with the incubations performed in the dark almost doubling the flux of those performed in the light. Exchangeable dissolved organic carbon (EDOC), however, oscillated between production and uptake, being completely recycled within the system and representing around 14% of the DOC flux. The pools of bottom and surface DOC were high for an oligotrophic environment, and were positively correlated to the pool of EDOC. Thus, despite being in metabolic balance, this ecosystem acted as a conduit for OC, as it is able to export OC to adjacent areas derived from allochtonous inputs during heterotrophic conditions. These inputs likely come from groundwater discharge, human activity in the watershed, delivered to the sediments through the high capacity of C. prolifera to remove particles from the water column, and from the air-water exchange of EDOC, demonstrating that these communities are a major contributor to the cycling of OC in coastal embayments.
引用
收藏
页数:10
相关论文
共 34 条
  • [1] From biota to chemistry and climate: towards a comprehensive description of trace gas exchange between the biosphere and atmosphere
    Arneth, A.
    Sitch, S.
    Bondeau, A.
    Butterbach-Bahl, K.
    Foster, P.
    Gedney, N.
    de Noblet-Ducoudre, N.
    Prentice, I. C.
    Sanderson, M.
    Thonicke, K.
    Wania, R.
    Zaehle, S.
    [J]. BIOGEOSCIENCES, 2010, 7 (01) : 121 - 149
  • [2] Dissolved organic carbon fluxes by seagrass meadows and macroalgal beds
    Barron, Cristina
    Apostolaki, Eugenia T.
    Duarte, Carlos M.
    [J]. FRONTIERS IN MARINE SCIENCE, 2014, 1
  • [3] Dissolved organic matter release in a Posidonia oceanica meadow
    Barron, Cristina
    Duarte, Carlos M.
    [J]. MARINE ECOLOGY PROGRESS SERIES, 2009, 374 : 75 - 84
  • [4] Submarine Groundwater Discharge to the Coastal Environment of a Mediterranean Island (Majorca, Spain): Ecosystem and Biogeochemical Significance
    Basterretxea, Gotzon
    Tovar-Sanchez, Antonio
    Beck, Aaron J.
    Masque, Pere
    Bokuniewicz, Henry J.
    Coffey, Ruth
    Duarte, Carlos M.
    Garcia-Orellana, Jordi
    Garcia-Solsona, Esther
    Martinez-Ribes, Lorena
    Vaquer-Sunyer, Raquel
    [J]. ECOSYSTEMS, 2010, 13 (05) : 629 - 643
  • [5] Bravo-Linares CM, 2010, J CHIL CHEM SOC, V55, P227, DOI 10.4067/S0717-97072010000200018
  • [6] NEW MEASUREMENTS OF OXYGEN SOLUBILITY IN PURE AND NATURAL WATER
    CARPENTER, JH
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 1966, 11 (02) : 264 - +
  • [7] High atmosphere-ocean exchange of organic carbon in the NE subtropical Atlantic -: art. no. L21807
    Dachs, J
    Calleja, ML
    Duarte, CM
    del Vento, S
    Turpin, B
    Polidori, A
    Herndl, GJ
    Agustí, S
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (21) : 1 - 4
  • [8] Duarte CM, 2013, NAT CLIM CHANGE, V3, P961, DOI [10.1038/nclimate1970, 10.1038/NCLIMATE1970]
  • [9] The fate of marine autotrophic production
    Duarte, CM
    Cebrian, J
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 1996, 41 (08) : 1758 - 1766
  • [10] Major role of marine vegetation on the oceanic carbon cycle
    Duarte, CM
    Middelburg, JJ
    Caraco, N
    [J]. BIOGEOSCIENCES, 2005, 2 (01) : 1 - 8