Iron limits the cell division rate of Prochlorococcus in the eastern equatorial Pacific

By Elizabeth L. Mann, Sallie W. Chisholm. 2000

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Citations in the corpus

Prochlorococcus contributes to new production in the Sargasso Sea deep chlorophyll maximum (2007, background): “…of the influence of temperature, light, nutrients and trace metals on the its growth and physiology in culture and in the field [e.g., Mann and Chisholm, 2000; Moore et al., 2002]; and molecular studies focusing on its genome and genetic diversity [e.g., Rocap et al., 2003; Zinser et…”
A rising tide lifts all phytoplankton: Growth response of other phytoplankton taxa in diatom‐dominated blooms (2006, result): “These results confirm that the iron response of the two major prokaryotic groups is similar to the bulk nondiatom assemblage iron response; that is, they increased modestly in both biomass and chlorophyll-specific net growth rate as also reported by Mann and Chisholm [2000] .”
Cobalt limitation and uptake in Prochlorococcus (2002, methodology): “With the Sherrell and Boyle particulate cobalt value measured in surface waters (1.5 mmol Co mol21 C), a population of 105 cells ml21 Prochlorococcus growing at 0.4 d21 in the Sargasso Sea (Mann 2000) with 53 fg C cell21 (Campbell et al. 1994) would incorporate 0.3 pM d21 of cobalt in new cells, and”
Novel interactions between phytoplankton and microzooplankton: their influence on the coupling between growth and grazing rates in the sea (2002, background): “This seems to be an arena ripe for the application of molecular techniques coupled with flow cytometric or imaging-in-flow analysis, as has been brought to bear successfully on natural intrinsic growth rates of prokaryotes (e.g. Mann & Chisholm, 2000).”
Carbon versus iron limitation of bacterial growth in the California upwelling regime (2000, background): “In contrast to large phytoplankton, population sizes of both heterotrophic and phototrophic picoplankton can be kept in check by mortality (grazing and viral lysis) even when growth rates are greatly enhanced by DOC or iron additions (Mann and Chisholm 2000).”
Microbial community structure and variability in the tropical Pacific (2002, background): “Nonetheless, the growth rates of PRO, SYN and eukaryotic picophytoplankton also responded significantly to the iron additions (Mann and Chisholm, 2000; Landry et al., 2000b), while their grazer-regulated standing stocks did not change significantly (Wells et al.”
Co-limitation of diatoms by iron and silicic acid in the equatorial Pacific (2011, methodology): “Added Fe has been shown to stimulate the growth rate of Prochlorococcus in the EEP when cell cycle-based growth rate methods were applied in microcosm experiments (Mann and Chisholm, 2000).”
Copper toxicity and cyanobacteria ecology in the Sargasso Sea (2002, methodology): “DNA synthesis generally starts after dusk and reaches a peak around 1900 h, followed by the G2 phase and mitosis (Vaulot et al. 1995; Liu et al. 1997; Shalapyonok et al. 1998; Mann 2000a).”
Depth-stratified phytoplankton dynamics in Cyclone Opal, a subtropical mesoscale eddy (2008, background): “In IronEx II, for example, there was little evidence of an iron fertilization effect on biomass or composition of cells less than 10m m( Landry et al., 2000a), but their growth rates and physiological states were clearly stimulated (Cavender-Bares et al., 1999; Landry et al., 2000b; Mann and Chisho”