Adrian Przemysław Marciszak, Wiktoria Marianna Gornig, Lena Matyaszczyk, Krzysztof Demidziuk, Marek Kasprzak
{"title":"来自 Południowa 洞穴(波兰西南部苏台德山脉)的犬科和鼬科遗骸","authors":"Adrian Przemysław Marciszak, Wiktoria Marianna Gornig, Lena Matyaszczyk, Krzysztof Demidziuk, Marek Kasprzak","doi":"10.7306/gq.1751","DOIUrl":null,"url":null,"abstract":"<p>Południowa Cave is a locality that has been known for more than 500 years, where at least three or even four different faunal assemblages have been found. The oldest faunal elements are represented by the rodent <em>Baranomys loczyi</em>, and the carnivores <em>Baranogale helbingi</em> and <em>Mustela pliocaenica</em>, being the only Pliocene finds in the Sudetes Mts caves. The second faunal assemblage is dated back to the early Middle Pleistocene and consists of the following taxa: <em>Sorex</em> sp., <em>Rhinolophus</em> aff. <em>ferrumequinum</em>, <em>Glis sackdilligensis</em>, <em>Pliomys coronensis</em>, <em>Pliomys episcopalis</em>, <em>Mimomys</em> sp., <em>Lycaon lycaonoides</em>, <em>Canis mosbachensis</em>, <em>Vulpes vulpes</em>, <em>Ursus deningeri</em>, <em>Ursus arctos </em>ssp., <em>Ursus </em>cf. <em>thibetanus</em>, <em>Gulo gulo schlosseri</em>, <em>Meles meles atavus</em>, <em>Martes vetus</em>, <em>Mustela strandi</em>, <em>Mustela palerminea</em>, <em>Mustela praenivalis</em>, <em>Panthera spelaea fossilis</em>, <em>Homotherium latidens latidens</em>, <em>Panthera gombaszoegensis gombaszoegensis</em>, <em>Acinonyx pardinensis intermedius</em>, <em>Felis</em> cf. <em>silvestris</em>, <em>Pachycrocuta brevirostris</em> and <em>Capreolus</em> sp. The third assemblage is dated back to the Late Pleistocene (MIS 3), and consists of <em>Glis glis</em>, <em>Arvicola</em> sp., <em>Canis lupus spealeus</em>, <em>Ursus </em>ex. gr. <em>spelaeus</em>, and <em>Martes martes</em>. Finally, the youngest fauna, dated as MIS 1, is represented by <em>Arvicola</em> sp., <em>Apodemus</em> sp., <em>Lepus</em> sp., <em>Cricetus cricetus</em>, <em>Ursus arctos arctos</em>, <em>Meles meles</em>, <em>Martes martes</em>, and <em>Capreolus capreolus</em>. Possible relationships that may be inferred include the impact of new species in the disappearance of ancient carnivores.</p>","PeriodicalId":12587,"journal":{"name":"Geological Quarterly","volume":"65 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2024-07-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Remains of Canidae and Felidae from Południowa Cave (Sudetes Mts, SW Poland)\",\"authors\":\"Adrian Przemysław Marciszak, Wiktoria Marianna Gornig, Lena Matyaszczyk, Krzysztof Demidziuk, Marek Kasprzak\",\"doi\":\"10.7306/gq.1751\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Południowa Cave is a locality that has been known for more than 500 years, where at least three or even four different faunal assemblages have been found. The oldest faunal elements are represented by the rodent <em>Baranomys loczyi</em>, and the carnivores <em>Baranogale helbingi</em> and <em>Mustela pliocaenica</em>, being the only Pliocene finds in the Sudetes Mts caves. The second faunal assemblage is dated back to the early Middle Pleistocene and consists of the following taxa: <em>Sorex</em> sp., <em>Rhinolophus</em> aff. <em>ferrumequinum</em>, <em>Glis sackdilligensis</em>, <em>Pliomys coronensis</em>, <em>Pliomys episcopalis</em>, <em>Mimomys</em> sp., <em>Lycaon lycaonoides</em>, <em>Canis mosbachensis</em>, <em>Vulpes vulpes</em>, <em>Ursus deningeri</em>, <em>Ursus arctos </em>ssp., <em>Ursus </em>cf. <em>thibetanus</em>, <em>Gulo gulo schlosseri</em>, <em>Meles meles atavus</em>, <em>Martes vetus</em>, <em>Mustela strandi</em>, <em>Mustela palerminea</em>, <em>Mustela praenivalis</em>, <em>Panthera spelaea fossilis</em>, <em>Homotherium latidens latidens</em>, <em>Panthera gombaszoegensis gombaszoegensis</em>, <em>Acinonyx pardinensis intermedius</em>, <em>Felis</em> cf. <em>silvestris</em>, <em>Pachycrocuta brevirostris</em> and <em>Capreolus</em> sp. The third assemblage is dated back to the Late Pleistocene (MIS 3), and consists of <em>Glis glis</em>, <em>Arvicola</em> sp., <em>Canis lupus spealeus</em>, <em>Ursus </em>ex. gr. <em>spelaeus</em>, and <em>Martes martes</em>. Finally, the youngest fauna, dated as MIS 1, is represented by <em>Arvicola</em> sp., <em>Apodemus</em> sp., <em>Lepus</em> sp., <em>Cricetus cricetus</em>, <em>Ursus arctos arctos</em>, <em>Meles meles</em>, <em>Martes martes</em>, and <em>Capreolus capreolus</em>. Possible relationships that may be inferred include the impact of new species in the disappearance of ancient carnivores.</p>\",\"PeriodicalId\":12587,\"journal\":{\"name\":\"Geological Quarterly\",\"volume\":\"65 1\",\"pages\":\"\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2024-07-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geological Quarterly\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.7306/gq.1751\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geological Quarterly","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.7306/gq.1751","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOLOGY","Score":null,"Total":0}
Remains of Canidae and Felidae from Południowa Cave (Sudetes Mts, SW Poland)
Południowa Cave is a locality that has been known for more than 500 years, where at least three or even four different faunal assemblages have been found. The oldest faunal elements are represented by the rodent Baranomys loczyi, and the carnivores Baranogale helbingi and Mustela pliocaenica, being the only Pliocene finds in the Sudetes Mts caves. The second faunal assemblage is dated back to the early Middle Pleistocene and consists of the following taxa: Sorex sp., Rhinolophus aff. ferrumequinum, Glis sackdilligensis, Pliomys coronensis, Pliomys episcopalis, Mimomys sp., Lycaon lycaonoides, Canis mosbachensis, Vulpes vulpes, Ursus deningeri, Ursus arctos ssp., Ursus cf. thibetanus, Gulo gulo schlosseri, Meles meles atavus, Martes vetus, Mustela strandi, Mustela palerminea, Mustela praenivalis, Panthera spelaea fossilis, Homotherium latidens latidens, Panthera gombaszoegensis gombaszoegensis, Acinonyx pardinensis intermedius, Felis cf. silvestris, Pachycrocuta brevirostris and Capreolus sp. The third assemblage is dated back to the Late Pleistocene (MIS 3), and consists of Glis glis, Arvicola sp., Canis lupus spealeus, Ursus ex. gr. spelaeus, and Martes martes. Finally, the youngest fauna, dated as MIS 1, is represented by Arvicola sp., Apodemus sp., Lepus sp., Cricetus cricetus, Ursus arctos arctos, Meles meles, Martes martes, and Capreolus capreolus. Possible relationships that may be inferred include the impact of new species in the disappearance of ancient carnivores.
期刊介绍:
The policy of the Geological Quarterly is to publish significant contributions of information and geological insight relevant to an international readership. The journal has been issued since 1957 at the Polish Geological Institute - National Research Institute and, at present, is the leading Earth sciences journal in Poland. All aspects of Earth and related sciences, and universal and broad regional rather than locally oriented topics are covered.
The journal is intended to be an international forum for the exchange of information and ideas, particularly on important geological topics of Central Europe.