Biomass and primary productivity of the cyanobacterium Trichodesmium spp. in the tropical N Atlantic ocean

By E. Carpenter, Ajit Subramaniam, D. Capone. 2004

237 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Oceanography

View Paper: https://www.semanticscholar.org/paper/b63b10c47460524afbd6d396a56c68530815e82e

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Citations in the corpus

Influence of the Amazon River plume on distributions of free‐living and symbiotic cyanobacteria in the western tropical north Atlantic Ocean (2007, methodology): “Most studies of diazotrophy in the WTNA have focused on Trichodesmium (Carpenter et al. 2004; Capone et al. 2005), with the exception of Carpenter et al. (1999).”
Dissolved inorganic and organic phosphorus uptake in Trichodesmium and the microbial community: The importance of phosphorus ester in the Sargasso Sea (2010, methodology): “ATP has previously been used to examine P ester uptake in cultures of Synechococcus (Fu et al. 2006) and in field populations of phytoplankton (Casey et al. 2009). The H 33 3 PO4 and 33P-ATP were sampled in sets, and the differences in incubation time reflect the time needed to sample one set. Data ”
The fate of nitrogen fixed by diazotrophs in the ocean (2007, background): “In some coastal systems, blooms of dinoflagellates and diatoms have been observed during and subsequent to Trichodesmium blooms (Devassy et al., 1978; Revelante et al., 1982; Furnas and Mitchell, 1996). For example, Devassy et al. (1979) found that as blooms of Trichodesmium decayed, Chaetoceras pop”
Phosphate availability controls Trichodesmium spp. biomass in the SW Pacific Ocean (2005, background): “Light, temperature (Carpenter et al. 2004) and nutrient availability, particularly that of phosphate (Sañudo-Wilhelmy et al. 2001, Mulholland et al. 2002, Fu & Bell 2003) and iron (Behrenfeld & Kobler 1999, Kustka et al. 2002), could physiologically control the kinetics of nitrogen fixation.”
Flux capacities and acclimation costs in Trichodesmium from the Gulf of Mexico (2008, methodology): “and acetylene reduction assays, respectively ( Carpenter et al. 2004; Fu and Bell 2003).”
Latitudinal distribution of Trichodesmium spp. and N 2 fixation in the Atlantic Ocean (2010, background): “abundance, over both space and time, most studies have so far focused on regions which tend to show higher abundances of this genus (Carpenter et al., 2004; Capone et al., 2005; Mulholland et al., 2006), or have been conducted during blooms (Karl et al.”
Nitrogen fixation by Trichodesmium spp.: An important source of new nitrogen to the tropical and subtropical North Atlantic Ocean (2005, methodology): “[38] The rate of primary production in the tropical and subtropical North Atlantic is not well constrained in the literature, with estimates ranging between about 17 and 83 mmol C* m 2 d 1 [Carpenter et al., 2004].”
Modeling the distribution of Trichodesmium and nitrogen fixation in the Atlantic Ocean (2004, background): “Similarly, high concentrations of Trichodesmium are most commonly observed in the southern Sargasso Sea in summer and fall [Carpenter and Romans, 1991; Carpenter et al., 2004, and references therein].”
INTERACTIONS BETWEEN NITRATE UPTAKE AND NITROGEN FIXATION IN CONTINUOUS CULTURES OF THE MARINE DIAZOTROPH TRICHODESMIUM (CYANOBACTERIA) 1 (2005, background): “However, at several stations along a subtropical north Atlantic cruise track in April 1996, Carpenter et al. (2004) found Trichodesmium filaments at depths where NO 3 concentrations were between 1.8 and 12.2mM.”
Phosphate availability and the ultimate control of new nitrogen input by nitrogen fixation in the tropical Pacific Ocean (2007, background): “Temperatures above 26◦ C are necessary for Trichodesmium bloom development (Carpenter et al., 2004).”