Early Triassic conodonts of Jiarong, Nanpanjiang Basin, southern Guizhou Province, South China

• Published in: Journal of Asian earth sciences 2015-06, Vol.105, p.104-121
• Main Authors: Chen, Yanlong, Jiang, Haishui, Lai, Xulong, Yan, Chunbo, Richoz, Sylvain, Liu, Xiaodan, Wang, Lina
• Format: Article
• Language: English
• Subjects: Biostratigraphy; Conodont; Early Triassic; Jiarong sections
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2015.03.014

•Thirteen conodont zones are identified for the Early Triassic Jiarong sections (South China).•The Induan/Olenekian boundary is recognised by Nv. w. eowaageni.•Microfacies analyses indicate toe-of-slope to basinal sedimentological facies.•Segminiplanate conodonts occur in the late Griesbachian and early Spathian.•Occurrences of segminiplanate conodonts may have been related to oxygenated seawater. Jiarong (Huishui County, Guizhou Province, South China) is a key locality for the study of the Early Triassic recovery after the end-Permian mass extinction. The size reduction of conodonts at the Smithian/Spathian transition was first documented in Jiarong, and it is also a locality that contributes to the documentation of the Early Triassic paleo-seawater temperatures. In the Jiarong sections, thirteen conodont zones were identified for the Early Triassic; in ascending order, they are Hindeodus parvus Zone, Hindeodus sosioensis Zone, Clarkina krystyni Zone, Neoclarkina discreta Zone, Neospathodus cristagalli–Eurygnathodus costatus assemblage zone, Novispathodus waageni eowaageni Zone, Novispathodus waageni waageni Zone, Discretella discreta Zone, Pachycladina–Parachirognathus assemblage zone, Novispathodus pingdingshanensis Zone, Icriospathodus collinsoni Zone, Triassospathodus homeri Zone, Triassospathodus triangularis Zone. These conodont zones in the Jiarong sections improve the global correlation of Early Triassic sections and also provide better regional age constraints in an area that is important for studies of recovery from the extinction. Based on the first appearance of Nv. waageni eowaageni, the Induan/Olenekian boundary is recognized at 3.6m above the base of the Jiarong III Section. The dominance of blade-shaped (segminate) conodonts was replaced by gondola-shaped (segminiplanate) conodonts twice; the first time was in the late Griesbachian, and the second time was in the early Spathian. The dominance of segminiplanate conodonts probably indicates that the deeper seawater environment became more oxygenated during the late Griesbachian and early Spathian for short time intervals, as it is believed that the Griesbachian segminiplanate conodonts favored deeper oxygenated water habitats. A new genus, Spathogondolella gen. nov., and a new species, Spathogondolella jiarongensis sp. nov., have been recognized.