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Sakchai Juanngam

    Sakchai Juanngam

    Research Interests:
    Research Interests:
    A small Permian brachiopod fauna is described from new localities in northeastern Thailand. Brachiopods were collected from early Permian (Asselian) limestones of the Nam Maholan Formation and middle Permian (Murgabian) sandstones of the... more
    A small Permian brachiopod fauna is described from new localities in northeastern Thailand. Brachiopods were collected from early
    Permian (Asselian) limestones of the Nam Maholan Formation and middle Permian (Murgabian) sandstones of the Nam Duk Formation
    and limestones of the Khao Khwang Formation. Analyses of taxa conWrm preliminary hypotheses of Cathaysian aYnities for brachiopods
    and fusulinids found in this part of Thailand. Fossils found in sandstones of the Nam Duk molasse facies, however, also show
    possible Gondwanan relationships with brachiopod taxa described in Australia. This has to be further tested with ongoing research in a
    better understanding of the paleobiogeography of this part of Southeast Asia.
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    Five new genera and species are described from brown silty mudstone near Huai Bun Nak, north-east Thailand. New taxa are Prorugaria thailandica n. gen., n. sp. (Family Rugosochonetidae); Tuberculatella tubertella n. gen., n. sp. (Family... more
    Five new genera and species are described from brown silty mudstone near Huai Bun Nak,
    north-east Thailand. New taxa are Prorugaria thailandica n. gen., n. sp. (Family Rugosochonetidae); Tuberculatella
    tubertella n. gen., n. sp. (Family Overtoniidae); Minispina alata n. gen., n. sp. (Family Marginiferidae);
    Aspinosella sinauris n. gen., n. sp. (Family Retariidae) and Mucrospiriferinella undulosa n. gen.,
    n. sp. (Family Xestotrematidae). The age is considered to be younger Carboniferous.
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    This paper deals with Permian brachiopods collected from 7 localities in the Tak Fa Formation of the Rat Buri Group, developed in the Khao Hin Klingarea, about 50 km southwest of Phetchabun. Twenty one species within seventeen genera are... more
    This paper deals with Permian brachiopods collected from 7 localities in the
    Tak Fa Formation of the Rat Buri Group, developed in the Khao Hin Klingarea, about
    50 km southwest of Phetchabun. Twenty one species within seventeen genera are
    described and discussed. Of them four species, Acosarina kanmerai, Orthotetina ruchae,
    HaydeneUa grantiand Nolothyris sakagami, are newly established ones. The Khao Hin
    Kling brachiopod fauna ranges from the Middle to early Late Permian. The faunal
    elements contain close affinities to those of the central and southern Tethyan realms.
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    Several localities of brachiopod faunas have been reported in the Loei area found mostly in late Palaeozoic shales and limestones. Silicifi ed articulate brachiopods were observed in the Pha Dam section east of Loei, in the Nam Suay... more
    Several localities of brachiopod faunas have been reported in the Loei area found mostly in late Palaeozoic shales
    and limestones. Silicifi ed articulate brachiopods were observed in the Pha Dam section east of Loei, in the Nam Suay
    sub-district, Na duang district. This section is part of the Nam Mahoran Formation according to the geological map
    published by DMR. It consists of brown shales and siltstones interbedded with dark grey limestones and the brachiopod
    assemblage includes cf. Chonetinella, Rhipidomella, Phricodothyris, Marginifera, Reticulatia, STROPHOMENIDA
    fam. indet., and SPIRIFERIDA fam. indet.. These specimens are relatively small in size, silicifi ed and mostly consist
    of single-valves. The occurrence and characteristics of the brachiopods in this section differ from those reported by
    previous workers in the area. This locality also contains several other abundant and diverse invertebrate groups such as
    bryozoans, crinoids and solitary corals. The rocks from both sections consist of shale and limestone. The brachiopods,
    corals, bryozoans and crinoids are interpreted as having lived in shallow marine or shelf environments. Preliminary
    age determinations are based mainly on brachiopods and suggest that the rocks should be reassigned to the Lower
    Permian which is compatible with the age assigned in the geological map of Thailand.
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