期刊论文详细信息
Aquatic Microbial Ecology
Planktonic carbon budget in the eastern subtropical North Atlantic
Valesca Pérez1  Marta M. Varela1  Beatriz Mouriño1  Emilio Fernández1  Mikhail V. Zubkov1  E. Malcolm S. Woodward1  Natalia González1  Antonio Bode1  Iñaki Huskin1  Ricardo Anadón1  Eva Teira1  Pablo Serret1  Mario Quevedo1  Alejandro Isla1  Carol Robinson1  Xosé Anxelu G. Morán1  Emilio Marañón1 
关键词: Plankton;    Primary production;    Bacterial production;    Respiration;    Grazing;    Subtropical NE Atlantic;    Atlantic Meridional Transect;   
DOI  :  10.3354/ame048261
学科分类:生物科学(综合)
来源: Inter-Research
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【 摘 要 】

ABSTRACT: 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 mgC m–2 d–1, respectively. Protist grazing on phytoplankton represented >90% of PP. Bacterial production (BP) was 17 ± 3 mgC m–2 d–1. In vitro O2-evolution experiments indicated that net community production was –65 ± 16 mmolO2 m–2 d–1, while community respiration (CR) averaged 124 ± 13 mmolO2 m–2 d–1, equivalent to 1324 ± 142 mgC 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 mgC 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 mgC 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 O2 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.

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