2005
DOI: 10.3354/meps301303
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Bloom of the marine diazotrophic cyanobacterium Trichodesmium erythraeum in the Northwest African Upwelling

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Cited by 69 publications
(41 citation statements)
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“…In terms of the Cyanobacteria-like sequences that were detected, both Trichodesmium and Lyngbya spp. have been reported to occur in blooms in coastal environments, including in corals, during the warmest seasons (O'Neil and Dennison, 2005;Paul et al, 2005;Ramos et al, 2005;Hewson et al, 2007;O'Neil and Capone, 2008;Paerl and Huisman, 2008). The results reported here highlight the importance of certain diazotroph groups in corals and their proliferation under high-temperature stress conditions.…”
Section: Discussionsupporting
confidence: 55%
“…In terms of the Cyanobacteria-like sequences that were detected, both Trichodesmium and Lyngbya spp. have been reported to occur in blooms in coastal environments, including in corals, during the warmest seasons (O'Neil and Dennison, 2005;Paul et al, 2005;Ramos et al, 2005;Hewson et al, 2007;O'Neil and Capone, 2008;Paerl and Huisman, 2008). The results reported here highlight the importance of certain diazotroph groups in corals and their proliferation under high-temperature stress conditions.…”
Section: Discussionsupporting
confidence: 55%
“…toxicity are available, related to more than one compound. Ramos et al [16] found 0.1-1 µg g -1 microcystins (MCs) in a bloom of Trichodesmium erythraeum, which was recorded for the first time in 2004 in the Canary Islands Archipelago, during the warmest period recorded since 1912. Samples from a Trichodesmium erythraeum bloom off the Brazilian coast were analyzed for MCs, saxitoxins analogues and cylindrospermopsin [17].…”
Section: Marine Planktonic Cyanobacteriamentioning
confidence: 99%
“…Nevertheless, highfrequency sampling in the Sainte Marie Bay shows that increase in the T. erythraeum population is often consecutive to dissolved combined nitrogen (NO 3 − ) pulses with a 3-7 day time lag [45]. Accumulations of T. erythraeum are also frequent in the lagoon of the Australian Great Barrier Reef [42] and other coastal regions (i.e, Brazil, [46]; India [47], Canary Island [48]). The population decay can provide readily available organic material for the other phytoplankton components and coral reef.…”
Section: Natural and Anthropogenic Eutrophicationmentioning
confidence: 99%