Soil bacterial diversity in the Arctic is not fundamentally different from that found in other biomes.

By Haiyan Chu, Noah Fierer, Noah Fierer, C. Lauber, J. Gregory Caporaso, Rob Knight, P. Grogan. Environmental Microbiology, 2010

609 citations recorded by the source corpus.

Subfields: Ecology, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/d28a3e81e61495ea1065330389fceef3a0d24a40

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Citations in the corpus

The bacterial biogeography of British soils. (2011, background): “…between pH and diversity in temperate and Arctic biomes have failed to identify reduced diversity at high pH (Hartman et al., 2008b; Rousk et al., 2009; Chu et al., 2010), illustrating that more widespread surveys are required to provide a global synthesis on the exact nature of this relationship.”
Bacterial communities in soil mimic patterns of vegetative succession and ecosystem climax but are resilient to change between seasons (2013, background): “…been studied as an important determinant of bacterial communities (Castro et al., 2009), and though it cannot be completely ruled out, biogeographical studies suggest that climate is not a major factor influencing bacterial community structure in soil (Lauber et al., 2009; Chu et al., 2010).”
CoNet app: inference of biological association networks using Cytoscape (2016, positive): “In our example, we will demonstrate how to build an association network from microbial count data obtained from arctic soil samples (Chu et al. , 2010).”
Permafrost Meta-Omics and Climate Change (2016, background): “Similarly, a survey of nonpermafrost Arctic soils showed that community composition was dependent on pH (Chu et al. 2010).”
Soil fertility is associated with fungal and bacterial richness, whereas pH is associated with community composition in polar soil microbial communities (2014, methodology): “In addition, to externally validate the models, we utilised a set of 33 dry heath tundra ecosystem soils that had been collected from a wide range of locations across the North American and European Arctic (Chu et al., 2010) (Supplemental Table S1).”
Environmental and ecological factors that shape the gut bacterial communities of fish: a meta‐analysis (2012, background): “ity (Lozupone & Knight 2007), pH (Fierer & Jackson 2006; Chu et al. 2010), seasonality (Gilbert et al.”
Soil pH mediates the balance between stochastic and deterministic assembly of bacteria (2018, background): “tributed soil samples that were collected without regard for successional age [29, 31].”
High throughput sequencing analysis of biogeographical distribution of bacterial communities in the black soils of northeast China (2014, methodology): “It should be noted that the samples involved in the studied by Lauber et al. (2009) and Chu et al. (2010) were collected from nonagricultural soils and the samples of this study were from agricultural soils, the differences of relative abundances of bacterial groups in this study with those…”
The Influence of Vegetation Type on the Dominant Soil Bacteria, Archaea, and Fungi in a Low Arctic Tundra Landscape (2011, methodology): “Since soil DON, mineral N and N mineralization diff er considerably among vegetation types (Chu and Grogan, 2010), these results together suggest that diff erences in soil N availability associated with the vegetation types may be one of main drivers of bacterial community structure in low Arctic…”
Strong elevational trends in soil bacterial community composition on Mt. Halla, South Korea (2014, background): “Encouraging progress has been made recently on the horizontal distribution of microbial communities (Chu et al., 2010; Griffiths et al., 2011; Lauber et al., 2009; Lozupone and Knight, 2007; Nemergut et al., 2011; Rousk et al., 2010), but few studies have investigated elevational trends in microbial”
Scaling laws predict global microbial diversity (2016, background): “Represented in this compilation were samples from arctic aquatic systems (130 sites; MG-RAST ID: mgp138), hydrothermal vents (123 sites; MG-RAST ID: mgp327) (48), freshwater lakes in China (187 sites; MG-RAST ID: mgp2758) (49), arctic soils (44 sites; MG-RAST ID: mgp69) (50), temperate soils (84 sit”