Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties

Storage of soil samples prior to metagenomic analysis presents a problem. If field sites are remote or if samples are collected by third parties, transport to analytical laboratories may take several days or even weeks. The bulk of such samples and requirement for later homogenisatio...

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Autores principales: Lina A. Clasen, Andrew P. Detheridge, John Scullion, Gareth W. Griffith
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Publicado: Pensoft Publishers 2020
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spelling oai:doaj.org-article:dbacfef9275f4d3d89a19f526cf994f52021-12-02T11:21:54ZSoil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties10.3897/mbmg.4.583652534-9708https://doaj.org/article/dbacfef9275f4d3d89a19f526cf994f52020-11-01T00:00:00Zhttps://mbmg.pensoft.net/article/58365/download/pdf/https://mbmg.pensoft.net/article/58365/download/xml/https://mbmg.pensoft.net/article/58365/https://doaj.org/toc/2534-9708 Storage of soil samples prior to metagenomic analysis presents a problem. If field sites are remote or if samples are collected by third parties, transport to analytical laboratories may take several days or even weeks. The bulk of such samples and requirement for later homogenisation precludes the convenient use of a stabilisation buffer, so samples are usually cooled or frozen during transit. There has been limited testing of the most appropriate storage methods for later study of soil organisms by eDNA approaches. Here we tested a range of storage methods on two contrasting soils, comparing these methods to the control of freezing at -80 °C, followed by freeze-drying. To our knowledge, this is the first study to examine the effect of storage conditions on eukaryote DNA in soil, including both viable organisms (fungi) and DNA contained within dying/dead tissues (plants). For fungi, the best storage regimes (closest to the control) were storage at 4 °C (for up to 14 d) or active air-drying at room temperature. The worst treatments involved initial freezing, followed by thawing which led to significant later spoilage. The key spoilage organisms were identified as Metarhizium carneum and Mortierella spp., with a general increase in saprotrophic fungi and reduced abundances of mycorrhizal/biotrophic fungi. Plant data showed a similar pattern, but with greater variability in community structure, especially in the freeze-thaw treatments, probably due to stochastic variation in substrates for fungal decomposition, algal proliferation and some seed germination. In the absence of freeze drying facilities, samples should be shipped refrigerated, but not frozen if there is any risk of thawing. Lina A. ClasenAndrew P. DetheridgeJohn ScullionGareth W. GriffithPensoft PublishersarticleEcologyQH540-549.5ENMetabarcoding and Metagenomics, Vol 4, Iss , Pp 135-147 (2020)
institution DOAJ
collection DOAJ
language EN
topic Ecology
QH540-549.5
spellingShingle Ecology
QH540-549.5
Lina A. Clasen
Andrew P. Detheridge
John Scullion
Gareth W. Griffith
Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
description Storage of soil samples prior to metagenomic analysis presents a problem. If field sites are remote or if samples are collected by third parties, transport to analytical laboratories may take several days or even weeks. The bulk of such samples and requirement for later homogenisation precludes the convenient use of a stabilisation buffer, so samples are usually cooled or frozen during transit. There has been limited testing of the most appropriate storage methods for later study of soil organisms by eDNA approaches. Here we tested a range of storage methods on two contrasting soils, comparing these methods to the control of freezing at -80 °C, followed by freeze-drying. To our knowledge, this is the first study to examine the effect of storage conditions on eukaryote DNA in soil, including both viable organisms (fungi) and DNA contained within dying/dead tissues (plants). For fungi, the best storage regimes (closest to the control) were storage at 4 °C (for up to 14 d) or active air-drying at room temperature. The worst treatments involved initial freezing, followed by thawing which led to significant later spoilage. The key spoilage organisms were identified as Metarhizium carneum and Mortierella spp., with a general increase in saprotrophic fungi and reduced abundances of mycorrhizal/biotrophic fungi. Plant data showed a similar pattern, but with greater variability in community structure, especially in the freeze-thaw treatments, probably due to stochastic variation in substrates for fungal decomposition, algal proliferation and some seed germination. In the absence of freeze drying facilities, samples should be shipped refrigerated, but not frozen if there is any risk of thawing.
format article
author Lina A. Clasen
Andrew P. Detheridge
John Scullion
Gareth W. Griffith
author_facet Lina A. Clasen
Andrew P. Detheridge
John Scullion
Gareth W. Griffith
author_sort Lina A. Clasen
title Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
title_short Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
title_full Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
title_fullStr Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
title_full_unstemmed Soil stabilisation for DNA metabarcoding of plants and fungi. Implications for sampling at remote locations or via third-parties
title_sort soil stabilisation for dna metabarcoding of plants and fungi. implications for sampling at remote locations or via third-parties
publisher Pensoft Publishers
publishDate 2020
url https://doaj.org/article/dbacfef9275f4d3d89a19f526cf994f5
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