Temperature and substrates as interactive limiting factors for marine heterotrophic bacteria

By L. Pomeroy, W. Wiebe. 2001

600 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/66522d80893d83428d7fc55aa716f62c36351034

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In Ecology

In Global and Planetary Change

In Oceanography

Citations in the corpus

Potential Effects of Elevated Sea-Water Temperature on Pelagic Food Webs (2005, background): “In addition, heterotrophic bacteria have been shown to be temperature controlled during the spring bloom (Pomeroy & Wiebe, 2001).”
Effects of rising temperature on the formation and microbial degradation of marine diatom aggregates (2009, background): “Temperature has been proposed as a principally limiting or supporting factor for microbial processes (Pomeroy & Wiebe 2001).”
Microbial structuring of marine ecosystems (2007, background): “It has been proposed that there is a low-temperature–low-substrate restriction in the Arctic Ocea”
Nutritional ecology of marine herbivorous fishes: ten years on (2009, background): “Heterotrophic bacteria, such as gastrointestinal symbionts, can thus adapt to different temperature conditions given time (Pomeroy & Wiebe 2001), but obviously herbivorous reptiles are subject to diurnal and probably seasonal fluctuations in temperature (e.g. Schall & Dearing 1994) that subtidal…”
Comparison of free-living, suspended particle, and aggregate-associated bacterial and archaeal communities in the Laptev Sea (2009, background): “The cold temperatures of Arctic waters are already understood to constrain microbial activity (Pomeroy & Wiebe 2001), but our result is notable because the evaluated microbial feature was community richness, not activity.”
Modeling the temperature effect on the specific growth rate of phytoplankton: a review (2017, background): “When limiting, these nutrients strongly impact the thermal growth curve (Pomeroy and Wiebe 2001; Thomas 2013; Thomas and Litchman 2016).”
Bacterial Extracellular Enzymatic Activity in Globally Changing Aquatic Ecosystems (2010, background): “However, adding to the direct effects of temperature on the rates of biological processes, warming is also expected to affect pelagic ecosystems by changing the patterns of vertical mixing and nutrient allocation in the water column [70].”
Changes in bacterial activity and community structure in response to dissolved organic matter in the Hudson River, New York (2004, background): “Biotic mineralization of dissolved organic material (DOM) in aquatic ecosystems is carried out by a diverse community of heterotrophic microbes, potentially consisting of representatives from over 50 divisions (or phyla) of bacteria and Archaea (Rappé & Giovannoni 2003).”
Copepods as microbial hotspots in the ocean: effects of host feeding activities on attached bacteria (2005, background): “The marine water column is usually regarded as a nutritionally dilute environment and the growth of free-living bacteria is limited by available organic substrates (Kirchman & Rich 1997, Church et al. 2000, Pomeroy & Wiebe 2001).”
Variations of the abundance and nucleic acid content of heterotrophic bacteria in Beaufort Shelf waters during winter and spring (2008, background): “Complex interactions between substrate limitation and temperature effects are now viewed as the key to the understanding of the relatively low bacterial growth rate and growth efficiency often observed in polar waters (Pomeroy and Wiebe, 2001).”
Large scale importance of sea ice biology in the Southern Ocean (2004, background): “…from within the ice, although as discussed by Brierley & Thomas (2002) and Thomas & Papadimitriou (2003) the production of DOM is closely linked with the production of EPS by algae and bacteria (Krembs et al. 2002), as well as low temperature effects on substrate affinity (Pomeroy & Wiebe 2001).”