SEASONAL PATTERNS AND PLANT‐MEDIATED CONTROLS OF SUBSURFACE WETLAND BIOGEOCHEMISTRY
By S. Neubauer, Kim Givler, Sarahkeith Valentine, J. Megonigal. 2005
200 citations recorded by the source corpus.
Subfields: Ecology, Industrial and Manufacturing Engineering
View Paper: https://www.semanticscholar.org/paper/28c1dc948d9f6de24692d6df07876832e76848e8
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Citations in the corpus
- Characterization of Neutrophilic Fe(II)-Oxidizing Bacteria Isolated from the Rhizosphere of Wetland Plants and Description of Ferritrophicum radicicola gen. nov. sp. nov., and Sideroxydans paludicola sp. nov. (2007, background): “On the other hand, a rhizosphere Fe cycle where Fe(III) is continually being generated for potential Fe(III) reduction may lead to decreased methanogenesis because Fe(III)-reducing bacteria can outcompete methanogens for carbon in the rhizosphere (Roden and Wetzel 1996; Roden and Wetzel 2002; Neubau”
- Using microbial communities and extracellular enzymes to link soil organic matter characteristics to greenhouse gas production in a tidal freshwater wetland (2014, methodology): “Production of CO2 and CH4 was measured using an anaerobic slurry assay (Neubauer et al. 2005).”
- Returning to Their Roots: Iron-Oxidizing Bacteria Enhance Short-Term Plaque Formation in the Wetland-Plant Rhizosphere (2007, background): “By periodically replenishing Fe(II) within the microcosms, we were able to prevent Fe(II) limitation of microbial Fe oxidation and maintain Fe(II) concentrations between ∼100 to 1000 μmol L−1, values that are typical of many wetland environments where FeOB have been observed or dynamic Fe cycles hav”
- Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales (2013, background): “4), and a number of researchers have hypothesized that the microbial reduction in humics may contribute to unexplained high CO2 and low CH4 production in wetland soils (Segers, 1998; Neubauer et al., 2005; Heitmann et al., 2007; Keller & Bridgham, 2007).”
- Plant species traits regulate methane production in freshwater wetland soils (2011, background): “Like most mineral soils, our soils contained abundant iron, which is regenerated in the rhizosphere of wetlands plants through oxidation of ferrous iron (Fe(II)) (Weiss et al., 2003; Neubauer et al., 2005).”