Picophytoplankton in the equatorial Pacific: vertical distributions in the warm pool and in the high nutrient low chlorophyll conditions
By J. Blanchot, J. André, C. Navarette, J. Neveux, M. Radenac. 2001
106 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/138a76d1fa489b851eabcf64f76779713e5141ef
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In Ecology
In Oceanography
Citations in the corpus
- Assessing the dynamics and ecology of marine picophytoplankton: The importance of the eukaryotic component (2004, methodology): “Using simplified carbon conversion factors, other studies have shown that picoeukaryotes can be responsible for a greater portion of carbon biomass than either Prochlorococcus or Synechococcus (e.g., Partensky et al. 1996; Blanchot et al. 2001).”
- Chemical and Biological Studies of Particulate Organic Matter in the Ocean (2002, background): “It is now widely recognized that small organisms can be major components of the plankton in many oceanic regimes (e.g., Bidigare and Ondrusek, 1996; Binder et al., 1996; Blanchot and Rodier, 1996; Landry et al., 1997; Blanchot et al., 2001).”
- Significance of predation by protists in aquatic microbial food webs (2004, background): “…of prokaryotic and eukaryotic prey biomass are presented in Table 2, based on literature values for typical cell abundances and for cell-specific carbon contents in oligotrophic and mesotrophic marine pelagic ecosystems (Fukuda et al. 1998; Li 1998; Zubkov et al. 2000; Blanchot et al. 2001).”
- Microbial community structure and variability in the tropical Pacific (2002, methodology): “In contrast, only one population of Synechococcus appears to be present in both high- and lownutrient waters of the equatorial Pacific (Neveux et al., 1999; Blanchot et al., 2001).”
- Phytoplankton Assemblage Structure and Primary Productivity Along 170° W in the South Pacific Ocean (2003, background): “Limnol Oceanogr 38:1420–1437 Lindley ST, Bidigare RR, Barber RT (1995) Phytoplankton photosynthesis parameters along 140° W in the Equatorial Pacific.”