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Article: Early Ordovician conodonts from Tarutao Island, southern peninsular Thailand

Publication: Palaeontology
Volume: 51
Part: 6
Publication Date: November 2008
Page(s): 1435 1453
Author(s): Sachiko Agematsu, Katsuo Sashida, Sirot Salyapongse and Apsorn Sardsud
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How to Cite

AGEMATSU, S., SASHIDA, K., SALYAPONGSE, S., SARDSUD, A. 2008. Early Ordovician conodonts from Tarutao Island, southern peninsular Thailand. Palaeontology51, 6, 1435–1453.

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Early Ordovician conodont faunas of the Thung Song Formation on Tarutao Island, southern peninsular Thailand, consist of 14 known species belonging to 17 genera, and eight undescribed species. Utahconus tarutaoensis and Filodontus tenuis are new species. Three conodont zones: the Rossodus manitouensis Zone, the Utahconus tarutaoensis Zone and the Filodontus tenuis Zone, in ascending order, are defined in the study sections. These are coeval with the interval from the Rossodus manitouensis Zone to the Acodus deltatus-Oneotodus costatus Zone of the standard zonation in the North American Midcontinent. Based on the conodonts studied here and fossils previously reported from Tarutao Island, the Thung Song Formation is early Tremadocian to middle Arenig (Ibexian) in age. This formation is lithostratigraphically subdivided into the S1 to S5 members, and our study sections consist of the S1 to S3 members. These strata accumulated on a shelf in the Early Ordovician. The depositional environments of the limestones making up the S1 and S3 members were in deeper-shelf conditions. Limestone and shale of the S2 member formed in a shallow-water, high-energy environment.
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