{"title":"俄罗斯哈普罗夫斯基动物群Liventsovka及其他地区的马科动物:订正","authors":"Vera Eisenmann","doi":"10.1016/j.geobios.2021.11.001","DOIUrl":null,"url":null,"abstract":"<div><p><span>The age and homogeneity of the Khaprovskii Faunal Complex have been a matter of debate for a long time. This works provides the most complete information (photographs and numerical data) ever published on the equid remains of this Complex. Evidence is given for the presence of no less than three, possibly six taxa of Equids. Most fossils are referred to </span><em>Equus</em> (<em>Allohippus</em>) aff. <em>major</em> and to <em>Equus</em> (<em>Allohippus</em>) <em>livenzovensis</em>, both redefined on the basis of correlations between cranial and metapodial dimensions. Comparisons with Chinese fossils bring evidence for their age approximating 2.5 Ma. A third very large species is represented by a few teeth and metapodials which may have been intrusive. It is referred to <em>E.</em> (<em>Sussemionus</em>) aff. <em>verae</em> because of similarities with the NE Siberian species believed to be about 1<!--> <span>myr old. Accumulation of fossils during a long period is probably responsible for the large intraspecific variation observed in </span><em>E.</em> (<em>A.</em>) <em>major</em> and <em>E.</em> (<em>A.</em>) <em>livenzovensis</em> and for the occurrence of several other equid forms. Possible intrusions may also explain the abnormal number of observed taxa. Resemblances with Chinese and NE Siberian fossils indicate Asian influences on the composition of the Khaprovskii Faunal Complex.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6000,"publicationDate":"2022-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"The equids from Liventsovka and other localities of the Khaprovskii Faunal Complex, Russia: A revision\",\"authors\":\"Vera Eisenmann\",\"doi\":\"10.1016/j.geobios.2021.11.001\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p><span>The age and homogeneity of the Khaprovskii Faunal Complex have been a matter of debate for a long time. This works provides the most complete information (photographs and numerical data) ever published on the equid remains of this Complex. Evidence is given for the presence of no less than three, possibly six taxa of Equids. Most fossils are referred to </span><em>Equus</em> (<em>Allohippus</em>) aff. <em>major</em> and to <em>Equus</em> (<em>Allohippus</em>) <em>livenzovensis</em>, both redefined on the basis of correlations between cranial and metapodial dimensions. Comparisons with Chinese fossils bring evidence for their age approximating 2.5 Ma. A third very large species is represented by a few teeth and metapodials which may have been intrusive. It is referred to <em>E.</em> (<em>Sussemionus</em>) aff. <em>verae</em> because of similarities with the NE Siberian species believed to be about 1<!--> <span>myr old. Accumulation of fossils during a long period is probably responsible for the large intraspecific variation observed in </span><em>E.</em> (<em>A.</em>) <em>major</em> and <em>E.</em> (<em>A.</em>) <em>livenzovensis</em> and for the occurrence of several other equid forms. Possible intrusions may also explain the abnormal number of observed taxa. Resemblances with Chinese and NE Siberian fossils indicate Asian influences on the composition of the Khaprovskii Faunal Complex.</p></div>\",\"PeriodicalId\":55116,\"journal\":{\"name\":\"Geobios\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2022-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geobios\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S001669952200002X\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geobios","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S001669952200002X","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
The equids from Liventsovka and other localities of the Khaprovskii Faunal Complex, Russia: A revision
The age and homogeneity of the Khaprovskii Faunal Complex have been a matter of debate for a long time. This works provides the most complete information (photographs and numerical data) ever published on the equid remains of this Complex. Evidence is given for the presence of no less than three, possibly six taxa of Equids. Most fossils are referred to Equus (Allohippus) aff. major and to Equus (Allohippus) livenzovensis, both redefined on the basis of correlations between cranial and metapodial dimensions. Comparisons with Chinese fossils bring evidence for their age approximating 2.5 Ma. A third very large species is represented by a few teeth and metapodials which may have been intrusive. It is referred to E. (Sussemionus) aff. verae because of similarities with the NE Siberian species believed to be about 1 myr old. Accumulation of fossils during a long period is probably responsible for the large intraspecific variation observed in E. (A.) major and E. (A.) livenzovensis and for the occurrence of several other equid forms. Possible intrusions may also explain the abnormal number of observed taxa. Resemblances with Chinese and NE Siberian fossils indicate Asian influences on the composition of the Khaprovskii Faunal Complex.
期刊介绍:
Geobios publishes bimonthly in English original peer-reviewed articles of international interest in any area of paleontology, paleobiology, paleoecology, paleobiogeography, (bio)stratigraphy and biogeochemistry. All taxonomic groups are treated, including microfossils, invertebrates, plants, vertebrates and ichnofossils.
Geobios welcomes descriptive papers based on original material (e.g. large Systematic Paleontology works), as well as more analytically and/or methodologically oriented papers, provided they offer strong and significant biochronological/biostratigraphical, paleobiogeographical, paleobiological and/or phylogenetic new insights and perspectices. A high priority level is given to synchronic and/or diachronic studies based on multi- or inter-disciplinary approaches mixing various fields of Earth and Life Sciences. Works based on extant data are also considered, provided they offer significant insights into geological-time studies.