{"title":"二连盆地东梅山(中国内蒙古)出土的格利尔斯新材料","authors":"Qian Li","doi":"10.1002/ar.25462","DOIUrl":null,"url":null,"abstract":"East Mesa, an Eocene locality situated east of the Shara Murun River in the Erlian Basin, is characterized by basal lower red mudstones. However, a distinct depositional hiatus has been observed in these red mudstones, leading to their division into layers 1 and 2. Excitingly, recent discoveries respectively in layers 1 and 2 of the lower red mudstones at the East Mesa include new Glires (<jats:italic>Gomphos</jats:italic> sp.) and rodents such as <jats:italic>Asiomys dawsoni</jats:italic>, <jats:italic>Gobiocylindrodon</jats:italic> cf. <jats:italic>G. ulausuensis</jats:italic>, and <jats:italic>Yuomys</jats:italic> sp., marking their first occurrences within these horizons. A comparative analysis of small mammal faunas suggests that layer 1 may correspond to the Arshantan age, while layer 2 indicates a late Irdinmanhan age based on the combination of taxa found.","PeriodicalId":22308,"journal":{"name":"The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2024-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"New Glires materials from the East Mesa, Erlian Basin (Nei Mongol, China)\",\"authors\":\"Qian Li\",\"doi\":\"10.1002/ar.25462\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"East Mesa, an Eocene locality situated east of the Shara Murun River in the Erlian Basin, is characterized by basal lower red mudstones. However, a distinct depositional hiatus has been observed in these red mudstones, leading to their division into layers 1 and 2. Excitingly, recent discoveries respectively in layers 1 and 2 of the lower red mudstones at the East Mesa include new Glires (<jats:italic>Gomphos</jats:italic> sp.) and rodents such as <jats:italic>Asiomys dawsoni</jats:italic>, <jats:italic>Gobiocylindrodon</jats:italic> cf. <jats:italic>G. ulausuensis</jats:italic>, and <jats:italic>Yuomys</jats:italic> sp., marking their first occurrences within these horizons. A comparative analysis of small mammal faunas suggests that layer 1 may correspond to the Arshantan age, while layer 2 indicates a late Irdinmanhan age based on the combination of taxa found.\",\"PeriodicalId\":22308,\"journal\":{\"name\":\"The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-05-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1002/ar.25462\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Anatomical Record: Advances in Integrative Anatomy and Evolutionary Biology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/ar.25462","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
New Glires materials from the East Mesa, Erlian Basin (Nei Mongol, China)
East Mesa, an Eocene locality situated east of the Shara Murun River in the Erlian Basin, is characterized by basal lower red mudstones. However, a distinct depositional hiatus has been observed in these red mudstones, leading to their division into layers 1 and 2. Excitingly, recent discoveries respectively in layers 1 and 2 of the lower red mudstones at the East Mesa include new Glires (Gomphos sp.) and rodents such as Asiomys dawsoni, Gobiocylindrodon cf. G. ulausuensis, and Yuomys sp., marking their first occurrences within these horizons. A comparative analysis of small mammal faunas suggests that layer 1 may correspond to the Arshantan age, while layer 2 indicates a late Irdinmanhan age based on the combination of taxa found.