6533b82dfe1ef96bd12912c0

RESEARCH PRODUCT

Emsian (Lower Devonian) conodonts from the Daliantang Formation at Daliantang, southeastern Yunnan, China

Jau-chyn LiaoHong-he XuWenkun QiePeter KönigshofYi WangJian-feng LuJian-feng LuJosé Ignacio Valenzuela-ríos

subject

010506 paleontologybiologyStratigraphyFaunaPaleontologyPelagic zoneSubspecies010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesDevonianPaleontologyTaxonBenthic zoneFaciesConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences

description

Abstract The lower/upper Emsian boundary witnessed prominent diversification of biostratigraphically important genera Polygnathus Hinde, Caudicriodus Bultynck, and Latericriodus Muller. In contrast, conodonts previously reported around this boundary from the South China Block were characterized by relatively low species or subspecies diversity, and only a few widely distributed and extensively studied zone-defining taxa were recorded. In this paper, conodonts from the Daliantang Formation at the Daliantang section (Guangnan, southeastern Yunnan), one of the representative sections of the transitional facies between the benthic Xiangzhou facies and the pelagic Nandan facies, are investigated. The conodont fauna shows a remarkably high species or subspecies diversity, with fourteen taxa that are assignable to the notoperbonus Zone and inversus Zone. Five polygnathid species are described: P. gronbergi Klapper and Jonson, P. inversus Klapper and Jonson, Polygnathus sp. B, P. luciae Martinez-Perez and Valenzuela-Rios, and P. mashkovae Bardashev. The latter two are reported for the first time from the South China Block. Additionally, three icriodontid taxa are also described, of which L. guangnanensis n. sp. is characterized by distinctly chevron-shaped transverse rows in the anterior part and a well-developed process branching off to the outer side. The new conodont record increases our understanding of the diversification and faunal composition around the lower/upper Emsian boundary in the South China Block. It contributes to the regional and inter-regional biostratigraphical correlation between shallower- and deeper-water facies and also furnishes important South China material for future discussion and deliberation on the position of the lower/upper Emsian boundary.

https://doi.org/10.1016/j.palwor.2020.11.003