{"title":"华北地区孙家沟组最年轻的栓子化石(四足目:人类龙)","authors":"Jianye Chen, Jun Liu","doi":"10.5194/fr-23-205-2020","DOIUrl":null,"url":null,"abstract":"Abstract. Embolomeri were semiaquatic predators prevalent in the Carboniferous, with\nonly two species from the early Permian (Cisuralian). A new embolomere,\nSeroherpeton yangquanensis gen. et sp. nov. (Zoobank Registration number:\nurn:lsid:zoobank.org:act:790BEB94-C2CC-4EA4-BE96-2A1BC4AED748, registration: 23 November 2020), is named based on a partial right upper jaw and palate\nfrom the Sunjiagou Formation of Yangquan, Shanxi, China, and is late\nWuchiapingian (late Permian) in age. It is the youngest embolomere known to\ndate and the only embolomere reported from North China Block. Its\nphylogenetic position within Embolomeri is confirmed by the strongly\ndeveloped descending flange on the quadrate ramus of the pterygoid. The new\ntaxon is unique among embolomeres by features like a partial coverage of a\ndenticle shagreens on the pterygoid; presence of a cylindrical shaft on the\npterygoid, and two pairs of very large ectopterygoid tusks. Phylogenetic\nanalysis shows Seroherpeton as being the sister group of a clade consisting of\nProterogyrinus, Archeria, and Pholiderpeton. We hypothesize that the dispersal and decline of the embolomeres\nfrom Carboniferous to late Permian (Lopingian) is related to the climate\nchanges, especially aridification, of the paleotropical regions.","PeriodicalId":48830,"journal":{"name":"Fossil Record","volume":"23 1","pages":"205-213"},"PeriodicalIF":1.9000,"publicationDate":"2020-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"The youngest occurrence of embolomeres (Tetrapoda: Anthracosauria) from the Sunjiagou Formation (Lopingian, Permian) of North China\",\"authors\":\"Jianye Chen, Jun Liu\",\"doi\":\"10.5194/fr-23-205-2020\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Embolomeri were semiaquatic predators prevalent in the Carboniferous, with\\nonly two species from the early Permian (Cisuralian). A new embolomere,\\nSeroherpeton yangquanensis gen. et sp. nov. (Zoobank Registration number:\\nurn:lsid:zoobank.org:act:790BEB94-C2CC-4EA4-BE96-2A1BC4AED748, registration: 23 November 2020), is named based on a partial right upper jaw and palate\\nfrom the Sunjiagou Formation of Yangquan, Shanxi, China, and is late\\nWuchiapingian (late Permian) in age. It is the youngest embolomere known to\\ndate and the only embolomere reported from North China Block. Its\\nphylogenetic position within Embolomeri is confirmed by the strongly\\ndeveloped descending flange on the quadrate ramus of the pterygoid. The new\\ntaxon is unique among embolomeres by features like a partial coverage of a\\ndenticle shagreens on the pterygoid; presence of a cylindrical shaft on the\\npterygoid, and two pairs of very large ectopterygoid tusks. Phylogenetic\\nanalysis shows Seroherpeton as being the sister group of a clade consisting of\\nProterogyrinus, Archeria, and Pholiderpeton. We hypothesize that the dispersal and decline of the embolomeres\\nfrom Carboniferous to late Permian (Lopingian) is related to the climate\\nchanges, especially aridification, of the paleotropical regions.\",\"PeriodicalId\":48830,\"journal\":{\"name\":\"Fossil Record\",\"volume\":\"23 1\",\"pages\":\"205-213\"},\"PeriodicalIF\":1.9000,\"publicationDate\":\"2020-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Fossil Record\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.5194/fr-23-205-2020\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fossil Record","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/fr-23-205-2020","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
The youngest occurrence of embolomeres (Tetrapoda: Anthracosauria) from the Sunjiagou Formation (Lopingian, Permian) of North China
Abstract. Embolomeri were semiaquatic predators prevalent in the Carboniferous, with
only two species from the early Permian (Cisuralian). A new embolomere,
Seroherpeton yangquanensis gen. et sp. nov. (Zoobank Registration number:
urn:lsid:zoobank.org:act:790BEB94-C2CC-4EA4-BE96-2A1BC4AED748, registration: 23 November 2020), is named based on a partial right upper jaw and palate
from the Sunjiagou Formation of Yangquan, Shanxi, China, and is late
Wuchiapingian (late Permian) in age. It is the youngest embolomere known to
date and the only embolomere reported from North China Block. Its
phylogenetic position within Embolomeri is confirmed by the strongly
developed descending flange on the quadrate ramus of the pterygoid. The new
taxon is unique among embolomeres by features like a partial coverage of a
denticle shagreens on the pterygoid; presence of a cylindrical shaft on the
pterygoid, and two pairs of very large ectopterygoid tusks. Phylogenetic
analysis shows Seroherpeton as being the sister group of a clade consisting of
Proterogyrinus, Archeria, and Pholiderpeton. We hypothesize that the dispersal and decline of the embolomeres
from Carboniferous to late Permian (Lopingian) is related to the climate
changes, especially aridification, of the paleotropical regions.
期刊介绍:
Fossil Record (FR) is the palaeontological journal of the Museum für Naturkunde Berlin. This journal was founded in 1998 under the name Mitteilungen aus dem Museum für Naturkunde Berlin, Geowissenschaftliche Reihe and appears with two issues each year. Fossil Record publishes original papers in all areas of palaeontology including the taxonomy and systematics of fossil organisms, biostratigraphy, palaeoecology, and evolution. All taxonomic groups are treated, including invertebrates, microfossils, plants, and vertebrates.