New dicynodonts (Therapsida, Anomodontia) from near the Permo-Triassic boundary of Laos: implications for dicynodont survivorship across the Permo-Triassic mass extinction and the paleobiogeography of Southeast Asian blocks

被引:20
作者
Olivier, Chloe [1 ]
Battail, Bernard [1 ]
Bourquin, Sylvie [2 ]
Rossignol, Camille [3 ]
Steyer, J-Sebastien [1 ]
Jalil, Nour-Eddine [1 ,4 ]
机构
[1] Sorbonne Univ, CNRS, Museum Natl Hist Nat, CR2P, 57 Rue Cuvier,CP 38, F-75005 Paris, France
[2] Univ Rennes, CNRS, Geosci Rennes UMR 6118, F-35000 Rennes, France
[3] Univ Sao Paulo, Dept Geofis, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226,Cidade Univ, BR-05508090 Sao Paulo, SP, Brazil
[4] Univ Cadi Ayyad, Fac Sci Semlalia, Lab Biodiversite & Dynam Ecosyst, Blvd Prince My Abdellah, Marrakech 40000, Morocco
基金
巴西圣保罗研究基金会;
关键词
LUANG PRABANG BASIN; TRUONG SON BELT; KAROO BASIN; SUTURE ZONE; TECTONIC IMPLICATION; STRATIGRAPHIC RANGE; INDOSINIAN OROGENY; NORTHERN VIETNAM; BONE-HISTOLOGY; LIFE-STYLE;
D O I
10.1080/02724634.2019.1584745
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The dicynodonts are an emblematic group of herbivorous therapsids that survived the Permo-Triassic (P-Tr) crisis. Laotian dicynodonts from stratigraphically constrained beds, recently dated using the U-Pb zircon method, yield new insights into terrestrial faunas of Southeast Asia during the latest Permian and earliest Triassic. Summarily described, they were originally attributed to the genus Dicynodon. We provide a new phylogenetic analysis for Laotian dicynodonts, based on three well-preserved skulls, indicating that they belong to two new taxa: Counillonia superoculis, gen. et sp. nov., and Repelinosaurus robustus, gen. et sp. nov. Our phylogenetic analysis of Dicynodontia indicates that (1) Counillonia is closely related to some 'Dicynodon'-grade taxa and (2) Repelinosaurus is a kannemeyeriiform. The phylogenetic affinities of these new Laotian dicynodonts allow discussion of the survivorship of multiple lineages (Kannemeyeriiformes and 'Dicynodon'-grade dicynodontoids) across the P-Tr crisis. The Laotian dicynodonts also shed new light on the paleobiogeography of Southeast Asia from the late Paleozoic to the early Mesozoic, particularly the timing of collisions between the Indochina, the South China, and the North China blocks. The presence of dicynodonts in Laos, most likely in the Early Triassic, thus implies that the connection between the Indochina Block and the South China Block occurred no later than the latest Permian or earliest Triassic (i.e., when the dicynodonts provide direct evidence for a connection).
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页数:22
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