Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings

© 2018 Ivarsson et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Garnets from disparate geographical envir...

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Main Authors: Magnus Ivarsson, Henrik Skogby, Bongkot Phichaikamjornwut, Stefan Bengtson, Sandra Siljeström, Prayote Ounchanum, Apichet Boonsoong, Mingkhwan Kruachanta, Federica Marone, Veneta Belivanova, Sara Holmström
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Published: 2018
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http://cmuir.cmu.ac.th/jspui/handle/6653943832/58024
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Institution: Chiang Mai University
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spelling th-cmuir.6653943832-580242018-09-05T04:21:14Z Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings Magnus Ivarsson Henrik Skogby Bongkot Phichaikamjornwut Stefan Bengtson Sandra Siljeström Prayote Ounchanum Apichet Boonsoong Mingkhwan Kruachanta Federica Marone Veneta Belivanova Sara Holmström Agricultural and Biological Sciences Biochemistry, Genetics and Molecular Biology © 2018 Ivarsson et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Garnets from disparate geographical environments and origins such as oxidized soils and river sediments in Thailand host intricate systems of microsized tunnels that significantly decrease the quality and value of the garnets as gems. The origin of such tunneling has previously been attributed to abiotic processes. Here we present physical and chemical remains of endolithic microorganisms within the tunnels and discuss a probable biological origin of the tunnels. Extensive investigations with synchrotron-radiation X-ray tomographic microscopy (SRXTM) reveal morphological indications of biogenicity that further support a euendolithic interpretation. We suggest that the production of the tunnels was initiated by a combination of abiotic and biological processes, and that at later stages biological processes came to dominate. In environments such as river sediments and oxidized soils garnets are among the few remaining sources of bio-available Fe2+, thus it is likely that microbially mediated boring of the garnets has trophic reasons. Whatever the reason for garnet boring, the tunnel system represents a new endolithic habitat in a hard silicate mineral otherwise known to be resistant to abrasion and chemical attack. 2018-09-05T04:19:07Z 2018-09-05T04:19:07Z 2018-08-01 Journal 19326203 2-s2.0-85051426408 10.1371/journal.pone.0200351 https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85051426408&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/58024
institution Chiang Mai University
building Chiang Mai University Library
country Thailand
collection CMU Intellectual Repository
topic Agricultural and Biological Sciences
Biochemistry, Genetics and Molecular Biology
spellingShingle Agricultural and Biological Sciences
Biochemistry, Genetics and Molecular Biology
Magnus Ivarsson
Henrik Skogby
Bongkot Phichaikamjornwut
Stefan Bengtson
Sandra Siljeström
Prayote Ounchanum
Apichet Boonsoong
Mingkhwan Kruachanta
Federica Marone
Veneta Belivanova
Sara Holmström
Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
description © 2018 Ivarsson et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Garnets from disparate geographical environments and origins such as oxidized soils and river sediments in Thailand host intricate systems of microsized tunnels that significantly decrease the quality and value of the garnets as gems. The origin of such tunneling has previously been attributed to abiotic processes. Here we present physical and chemical remains of endolithic microorganisms within the tunnels and discuss a probable biological origin of the tunnels. Extensive investigations with synchrotron-radiation X-ray tomographic microscopy (SRXTM) reveal morphological indications of biogenicity that further support a euendolithic interpretation. We suggest that the production of the tunnels was initiated by a combination of abiotic and biological processes, and that at later stages biological processes came to dominate. In environments such as river sediments and oxidized soils garnets are among the few remaining sources of bio-available Fe2+, thus it is likely that microbially mediated boring of the garnets has trophic reasons. Whatever the reason for garnet boring, the tunnel system represents a new endolithic habitat in a hard silicate mineral otherwise known to be resistant to abrasion and chemical attack.
format Journal
author Magnus Ivarsson
Henrik Skogby
Bongkot Phichaikamjornwut
Stefan Bengtson
Sandra Siljeström
Prayote Ounchanum
Apichet Boonsoong
Mingkhwan Kruachanta
Federica Marone
Veneta Belivanova
Sara Holmström
author_facet Magnus Ivarsson
Henrik Skogby
Bongkot Phichaikamjornwut
Stefan Bengtson
Sandra Siljeström
Prayote Ounchanum
Apichet Boonsoong
Mingkhwan Kruachanta
Federica Marone
Veneta Belivanova
Sara Holmström
author_sort Magnus Ivarsson
title Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
title_short Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
title_full Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
title_fullStr Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
title_full_unstemmed Intricate tunnels in garnets from soils and river sediments in Thailand – Possible endolithic microborings
title_sort intricate tunnels in garnets from soils and river sediments in thailand – possible endolithic microborings
publishDate 2018
url https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85051426408&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/58024
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