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1000 Titel
  • Microbial-, fusulinid limestones with large gastropods and calcareous algae: an unusual facies from the Early Permian Khao Khad Formation of Central Thailand
1000 Autor/in
  1. Ketwetsuriya, Chatchalerm |
  2. Nose, Martin |
  3. Charoentitirat, Thasinee |
  4. Nützel, Alexander |
1000 Erscheinungsjahr 2020
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2020-07-14
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1000 Quellenangabe
  • 66(4):21
1000 Copyrightjahr
  • 2020
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s10347-020-00605-w |
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1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>The Early Permian (Kungurian) Khao Khad Formation of Central Thailand consists mostly of carbonates deposited on the western margin of the Indochina Terrane. This formation has yielded unusual microbial-fusulinid limestones with large gastropods which contribute most to the rock volume. With a height of more than 6 cm, the gastropods are amongst the largest Early Permian gastropods ever reported. Gastropods as major rock formers are rare in the Palaeozoic. This, and other recently reported invertebrate faunas from Thailand show that gastropods may dominate Permian fossil assemblages not only in diversity, but also regarding abundance and in some cases also regarding biomass. Besides gastropods, fusulinids, various calcareous algae, intraclasts and thick microbial-cyanobacterial (<jats:italic>Girvanella</jats:italic> and <jats:italic>Archaeolithoporella</jats:italic>) coatings and reticular microbial patches as well as thick inter- and intragranular radial fibrous cement crusts are present. The gastropods represent at least four species and belong probably to undescribed taxa. The fusulinid genus <jats:italic>Pseudofusulina</jats:italic> and <jats:italic>Misellina</jats:italic> (<jats:italic>M</jats:italic>.) <jats:italic>termieri</jats:italic> are reported from the Khao Khad Formation for the first time and indicate a Bolorian age. Calcareous algae are dominated by dasycladaceans followed by gymnocodiaceans and solenoporaceans. The studied limestone almost completely lacks metazoan reef builders such as corals and sponges. Likewise, brachiopods and bivalves are absent in the studied samples and echinoderms are very scarce. The carbonate is interpreted as product of shallow water, back-reef lagoonal platform community with a high productivity providing the large gastropods with sufficient food. However, conditions were too eutrophic for sessile filter feeders including metazoan reef builders.</jats:p>
1000 Sacherschließung
lokal Original Article
lokal Microbialites
lokal Khao khad formation
lokal Large gastropods
lokal Saraburi group
lokal Dasyclads
lokal Permian
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  1. https://orcid.org/0000-0001-9362-6421|https://frl.publisso.de/adhoc/uri/Tm9zZSwgTWFydGlu|https://frl.publisso.de/adhoc/uri/Q2hhcm9lbnRpdGlyYXQsIFRoYXNpbmVl|https://frl.publisso.de/adhoc/uri/TsO8dHplbCwgQWxleGFuZGVy
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