Carbon versus iron limitation of bacterial growth in the California upwelling regime

By David L. Kirchman, B. Meon, Matthew T. Cottrell, D. Hutchins, Debra A. Weeks, K. Bruland. 2000

158 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Oceanography

View Paper: https://www.semanticscholar.org/paper/f99e33671dc63db09dbecdcc6352584bf571df2e

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Citations in the corpus

Phosphorus and trace metal limitation of algae and bacteria in Lake Superior (2004, result): “Similar results have been reported for the California upwelling system (Kirchman et al. 2000), but until now freshwater bacterial response to metal availability has not been evaluated.”
Glucose fluxes and concentrations of dissolved combined neutral sugars (polysaccharides) in the Ross Sea and Polar Front Zone, Antarctica (2001, background): “, 2000, 2001) since DOC fluxes often limit bacterial growth (Church et al., 2000; Kirchman et al., 2000) even in the iron-poor waters of Antarctic seas (Martin et al.”
Rapid bacterial mineralization of organic carbon produced during a phytoplankton bloom induced by natural iron fertilization in the Southern Ocean (2008, background): “…experiments demonstrating that carbon is the primary limiting factor for heterotrophic bacterial growth in lowiron waters (Church et al., 2000; Kirchman et al., 2000), while only one study reports direct iron-limitation of heterotrophic bacteria in coastal Antarctic waters (Pakulski et al.,…”
Viral release of iron and its bioavailability to marine plankton (2004, background): “Macrellis et al. (2001) have demonstrated that the marine Fe-ligand pool is a complicated mixture of many different organic complexes.”
Single-cell analysis of bacterial growth, cell size, and community structure in the Delaware estuary (2004, background): “Heterotrophic bacteria are typically carbon-limited in marine environments (Ducklow 2000, Kirchman et al. 2000), although inorganic nutrients, such as phosphorous, can be limiting as well (Cotner et al. 1997).”
Exopolysaccharides produced by bacteria isolated from the pelagic Southern Ocean - Role in Fe binding, chemical reactivity, and bioavailability (2011, unknown): “associated with heterotrophic bacteria, production of storage carbohydrates) known to be Fe-responsive (Kirchman et al., 2000; van Oijen et al., 2005).”
Community structure of marine bacterioplankton: patterns, networks, and relationships to function (2008, unknown): “Yet such nutrients are thought to limit bacterial growth (even heterotrophic bacteria) in many parts of the sea (Pomeroy et al. 1995, Pakulski et al. 1996, Cotner et al. 1997, Thingstad et al. 1998, Kirchman et al. 2000).”
Response of bacterioplankton to iron fertilization in the Southern Ocean (2004, background): “However, the current view is that, at least in some HNLC areas, bacterioplankton are not directly Fe limited, but rather carbon-limited as a consequence of the low primary productivity of Fe-limited phytoplankton (Hutchins et al. 1998; Church et al. 2000; Kirchman et al. 2000).”