Permian and Triassic Radiolaria from Northwest Thailand: Paleogeographical implications

• Main Authors: Feng Q., Malila K., Wonganan N., Chonglakmani C., Helmcke D., Ingavat-Helmcke R., Caridroit M.
• Format: Article
• Language: English
• Published: 2014
• Online Access: http://www.scopus.com/inward/record.url?eid=2-s2.0-29544433707&partnerID=40&md5=a3f086b999a3f7cf7a6eff6e7160a95a; http://cmuir.cmu.ac.th/handle/6653943832/4928
• Institution: Chiang Mai University

Well-preserved radiolarians were recovered from seven sections in the Mae Hong Son-Mae Sariang area, northwestern Thailand. 51 species assigned to 34 genera are identified, including 1 new species (Triassospongosphaera erici Feng sp. nov.) and 19 unidentified species. They are divided into the Late Permian, late Ladinian and middle Carnian radiolarian assemblages. Newly identified radiolarian assemblages, together with the published radiolarian biostratigraphic data from this region, indicate that there was a pelagic basin during the Late Paleozoic and Triassic. This basin was joined to the Chiang Dao and Changning-Menglian oceanic basins, and they represent the main oceanic basin of the Paleotethyan Archipelago Ocean. This main oceanic basin was situated in the traditional "Shan-Thai Block". Therefore, "the Shan-Thai Block" was not a single block during that stage, but composed of the Paleotethyan Ocean and two continental terranes that were affiliated with the Gondwana and Cathaysian domains, respectively. © 2005 Published by Elsevier SAS.