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dc.contributor.authorKushwaha, Priyanka
dc.contributor.authorNeilson, Julia W.
dc.contributor.authorMaier, Raina M.
dc.contributor.authorBabst-Kostecka, Alicja
dc.date.accessioned2021-09-21T23:20:55Z
dc.date.available2021-09-21T23:20:55Z
dc.date.issued2022-01
dc.identifier.citationKushwaha, P., Neilson, J. W., Maier, R. M., & Babst-Kostecka, A. (2022). Soil microbial community and abiotic soil properties influence Zn and Cd hyperaccumulation differently in Arabidopsis halleri. Science of the Total Environment, 803.en_US
dc.identifier.issn0048-9697
dc.identifier.doi10.1016/j.scitotenv.2021.150006
dc.identifier.urihttp://hdl.handle.net/10150/661849
dc.description.abstractSoil contamination with trace metal(loid) elements (TME) is a global concern. This has focused interest on TME-tolerant plants, some of which can hyperaccumulate extraordinary amounts of TME into above-ground tissues, for potential treatment of these soils. However, intra-species variability in TME hyperaccumulation is not yet sufficiently understood to fully harness this potential. Particularly, little is known about the rhizosphere microbial communities associated with hyperaccumulating plants and whether or not they facilitate TME uptake. The aim of this study is to characterize the diversity and structure of Arabidopsis halleri rhizosphere-influenced and background (i.e., non-Arabidopsis) soil microbial communities in four plant populations with contrasting Zn and Cd hyperaccumulation traits, two each from contaminated and uncontaminated sites. Microbial community properties were assessed along with geographic location, climate, abiotic soil properties, and plant parameters to explain variation in Zn and Cd hyperaccumulation. Site type (TME-contaminated vs. uncontaminated) and location explained 44% of bacterial/archaeal and 28% of fungal community variability. A linear discriminant effect size (LEfSe) analysis identified a greater number of taxa defining rhizosphere microbial communities than associated background soils. Further, in TME-contaminated soils, the number of rhizosphere-defining taxa was 6-fold greater than in the background soils. In contrast, the corresponding ratio for uncontaminated sites, was 3 and 1.6 for bacteria/archaea and fungi, respectively. The variables analyzed explained 71% and 76% of the variance in Zn and Cd hyperaccumulation, respectively; however, each hyperaccumulation pattern was associated with different variables. A. halleri rhizosphere fungal richness and diversity associated most strongly with Zn hyperaccumulation, whereas soil Cd and Zn bioavailability had the strongest associations with Cd hyperaccumulation. Our results indicate strong associations between A. halleri TME hyperaccumulation and rhizosphere microbial community properties, a finding that needs to be further explored to optimize phytoremediation technology that is based on hyperaccumulation.en_US
dc.description.sponsorshipEuropean Commissionen_US
dc.language.isoenen_US
dc.publisherElsevier BVen_US
dc.rights© 2021 Elsevier B.V. All rights reserved.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.subjectMetal accumulationen_US
dc.subjectMicrobial diversityen_US
dc.subjectPlant growth promoting bacteriaen_US
dc.subjectPseudometallophyteen_US
dc.subjectSoil metal contaminationen_US
dc.subjectTrace metal(loid) elementen_US
dc.titleSoil microbial community and abiotic soil properties influence Zn and Cd hyperaccumulation differently in Arabidopsis hallerien_US
dc.typeArticleen_US
dc.contributor.departmentDepartment of Environmental Science, The University of Arizonaen_US
dc.identifier.journalScience of the Total Environmenten_US
dc.description.note24 month embargo; available online: 30 August 2021en_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal accepted manuscripten_US
dc.identifier.piiS0048969721050816
dc.source.journaltitleScience of The Total Environment
dc.source.volume803
dc.source.beginpage150006


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