Full-depth profile (0–2000 m) of bacteria, heterotrophic nanoflagellates and ciliates in the NW Mediterranean Sea: Vertical partitioning of microbial trophic structures
By Tsuneo Tanaka, F. Rassoulzadegan. 2002
141 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/761d686c535fdfa7e3916ac1b4993c35eec1ded1
How researchers see this paper
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In Ecology
In Oceanography
- C. Robinson
- Carlos M. Duarte
- E. Rochelle-Newall
- F. Wambeke
- P. Rinaldi
- R. Lémée
- J. Arístegui
- J. Gasol
Citations in the corpus
- Emerging concepts on microbial processes in the bathypelagic ocean-ecology, biogeochemistry, and genomics (2010, background): “The abundance ratio of HNF to prokaryote tends to decrease from a typical value of 10-3 in surface oceans to around 1 – 2 10-4 in bathypelagic layers (Tanaka and Rassoulzadegan, 2002; Fukuda et al., 2007), although exceptions dependant upon oceanic region have also been noted (Sohrin et al., 2010).”
- Complex interactions in the microbial world: underexplored key links between viruses, bacteria and protozoan grazers in aquatic environments (2008, background): “Bacterial abundance in the ocean is on the order of 108 to 109 cells l–1, and the typical relative abundance for viruses, bacteria and heterotrophic nanoflagellates (HNF) is 10–1 to 10–3 (Noble & Fuhrman 1998, Tanaka & Rassoulzadegan 2002).”
- Microbial oceanography of the dark ocean's pelagic realm (2009, background): “Viral production, decay rates, and life strategies along a trophic gradient in the North Adriatic Sea.”
- Seasonal variation of bacterial production, respiration and growth efficiency in the open NW Mediterranean Sea (2002, methodology): “Assuming a conversion factor of 15 fg C per bacteria, BB in our study is in agreement with those reported in the literature for the open NW Mediterranean, which ranged from 0.23 to 1.6 µmol C l–1 (e.g. Fernandez et al. 1994, Van Wambeke et al. 1996, Tanaka & Rassoulzadegan 2002).”
- Mesopelagic zone ecology and biogeochemistry - a synthesis (2010, background): “Mediterranean Sea could be due to a higher abundance of ciliates (Tanaka and Rassoulzadegan, 2002).”
- Bacterial response to dust pulses in the western Mediterranean: Implications for carbon cycling in the oligotrophic ocean (2008, background): “…is P-limited, less DOC is mineralized and assimilated into bacterial biomass, thus increasing the amount of bioavailable DOC that can be exported to the ocean interior through vertical winter mixing [Rivkin and Anderson, 1997; Thingstad et al., 1997; Tanaka and Rassoulzadegan, 2002].”