Respiration in the dark ocean -: art. no. 1041

被引:42
作者
Arístegui, J
Agustí, S
Duarte, CM
机构
[1] Univ de las Palmas de Gran Canaria, Fac Ciencias Mar, Las Palmas Gran Canaria 35017, Islas Canarias, Spain
[2] Inst Mediterraneo Estudios Avanzados, UIB, CSIC, IMEDEA, Esporles 07190, Islas Baleares, Spain
关键词
D O I
10.1029/2002GL016227
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
[1] The dark ocean, the waters below 200 m depth, comprises about 95% of the volume of the ocean, but its contribution to the metabolism of the ocean is poorly quantified. Here we show that the respiration rate of microplankton declines exponentially at a rate of 0.53 km(-1) in the dark ocean, and is enhanced at the interface between the mesopelagic and the abyssal layers (1,000-2,000 m). The respiratory CO2 production in the dark ocean, estimated at 20 to 33.3 Gt C yr(-1), renders it a major component of the carbon flux in the biosphere.
引用
收藏
页码:13 / 1
页数:4
相关论文
共 27 条
[1]   Water-column remineralization in the Indian sector of the Southern Ocean during early spring [J].
Arístegui, J ;
Denis, M ;
Almunia, J ;
Montero, MF .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2002, 49 (9-10) :1707-1720
[2]   Major contribution from mesopelagic plankton to heterotrophic metabolism in the upper ocean [J].
Biddanda, B ;
Benner, R .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1997, 44 (12) :2069-2085
[3]   ANNUAL FLUX OF DISSOLVED ORGANIC-CARBON FROM THE EUPHOTIC ZONE IN THE NORTHWESTERN SARGASSO SEA [J].
CARLSON, CA ;
DUCKLOW, HW ;
MICHAELS, AF .
NATURE, 1994, 371 (6496) :405-408
[4]   CARBON OXIDATION IN THE DEEP MEDITERRANEAN SEA: EVIDENCE FOR DISSOLVED ORGANIC CARBON SOURCE [J].
Christensen, J. ;
Packard, T. ;
Dortch, F. ;
Minas, H. ;
Gascard, J. ;
Richez, C. ;
Garfield, P. .
GLOBAL BIOGEOCHEMICAL CYCLES, 1989, 3 (04) :315-335
[5]   RESPIRATION AND PHYSIOLOGICAL-STATE IN MARINE-BACTERIA [J].
CHRISTENSEN, JP ;
OWENS, TG ;
DEVOL, AH ;
PACKARD, TT .
MARINE BIOLOGY, 1980, 55 (04) :267-276
[6]   The CO2 balance of unproductive aquatic ecosystems [J].
Duarte, CM ;
Agustí, S .
SCIENCE, 1998, 281 (5374) :234-236
[7]   Evidence for a heterotrophic subtropical northeast Atlantic [J].
Duarte, MC ;
Agustí, S ;
Arístegui, J ;
González, N ;
Anadón, R .
LIMNOLOGY AND OCEANOGRAPHY, 2001, 46 (02) :425-428
[9]   Biogeochemical controls and feedbacks on ocean primary production [J].
Falkowski, PG ;
Barber, RT ;
Smetacek, V .
SCIENCE, 1998, 281 (5374) :200-206
[10]   Primary production of the biosphere: Integrating terrestrial and oceanic components [J].
Field, CB ;
Behrenfeld, MJ ;
Randerson, JT ;
Falkowski, P .
SCIENCE, 1998, 281 (5374) :237-240