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Bacterioplankton responses to riverine and atmospheric inputs in a coastal upwelling system (Ria de Vigo, NW Spain)

Teira, E. (författare)
Univ Vigo, Spain
Hernandez-Ruiz, M. (författare)
Univ Vigo, Spain
Barber-Lluch, E. (författare)
Univ Vigo, Spain
visa fler...
Sobrino, C. (författare)
Univ Vigo, Spain
Teixeira, I. G. (författare)
Univ Vigo, Spain;CSIC, Inst Invest Marinas, Spain
Alvarez-Salgado, X. A. (författare)
CSIC, Inst Invest Marinas, Spain
Nieto-Cid, M. (författare)
CSIC, Inst Invest Marinas, Spain
Martínez-García, Sandra (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM),Univ Vigo, Spain
Figueiras, F. G. (författare)
CSIC, Inst Invest Marinas, Spain
Fernandez, E. (författare)
Univ Vigo, Spain
visa färre...
 (creator_code:org_t)
Inter-Research Science Center, 2016
2016
Engelska.
Ingår i: Marine Ecology Progress Series. - : Inter-Research Science Center. - 0171-8630 .- 1616-1599. ; 542, s. 39-50
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Anthropogenic pressures are changing the magnitude and nature of matter inputs into the ocean. The Ria de Vigo (NW Spain) is a highly productive and dynamic coastal system that is likely affected by such alterations. Previous nutrient-addition microcosm experiments conducted during contrasting hydrographic conditions suggested that heterotrophic bacteria are limited by organic carbon (C) and occasionally co-limited by inorganic nutrients in this coastal area. In order to assess short-term responses in biomass, production, and respiration of heterotrophic bacteria from the Ria de Vigo to increasing amounts of natural inputs of matter, we conducted 6 microcosm experiments, wherein surface seawater collected in spring, summer, and autumn was mixed with increasing amounts of dissolved natural matter concentrates from riverine and atmospheric origin. Simultaneous experiments with controlled inorganic and/or organic additions indicated that bacteria were co-limited by inorganic nutrients and C in spring and summer and primarily limited by C in autumn. Production responded more than biomass to increasing inputs of matter, whereas respiration did not change. The bacterial production response to increasing dissolved organic C load associated with riverine and atmospheric inputs was strongly related to the relative phosphorus (P) content of the dissolved matter concentrates. Our data suggest that bacterial production might decrease with the increase of P-deficient allochthonous matter inputs, which would have important biogeochemical consequences for C cycling in coastal areas.

Ämnesord

NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)

Nyckelord

Bacterioplankton
Production
Biomass
Riverine water
Atmospheric deposition
Spain
Galicia
Ria de Vigo
Akvatisk ekologi
Aquatic Ecology

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