Paleontological JournalPaleontological JournalПалеонтологический журнал0031-031X3034-5871The Russian Academy of Sciences67797010.31857/S0031031X24060104QIEOOKArticlesСтатьиResearch ArticleThe fallow deer Dama pontica sp. nov. (Artiodactyla, Cervidae) from the Lower pleistocene of Taurida cave in the Crimea and the early history of the genus DamaЛань Dama pontica sp. nov. (Artiodactyla, Cervidae) из нижнего плейстоцена пещеры Таврида в Крыму и ранняя история рода DamaVislobokovaI. А.ВислобоковаИ. А.
Russian Federation
ivisl@paleo.ruBorissiak Paleontological Institute, Russian Academy of SciencesПалеонтологический институт им. А.А. Борисяка РАН19122024611212401042025Copyright ©; 2024, Russian Academy of SciencesCopyright ©; 2024, Российская академия наук2024Russian Academy of SciencesРоссийская академия наукhttps://journals.eco-vector.com/0031-031X/article/view/677970

A new fallow deer species Dama pontica is described from the late Early Pleistocene of Taurida cave in the Crimea. The antlers of this medium-sized deer had a small first process at the burr and a primitively narrow proximal palmation. The morphology of D. pontica sp. nov. allows it to be referred to a phylogenetic branch of the modern Iranian fallow deer, D. mesopotamica (Brooke, 1875). The fossil remains of Dama from the Taurida cave are the oldest in Europe. The age of the Taurida fauna, according to biochronology, is estimated at 1.8–1.5 Ma. The find indicates that the divergence of the European and Mesopotamian branches of fallow deer occurred no later than 1.5 Ma. Hypotheses about the origin of Dama (s.s.) from ‘Pseudodama’ at the Early – Middle Pleistocene transition require revision.

Новый вид лани Dama pontica sp. nov. описан по материалам из нижнего плейстоцена пещеры Таврида в Крыму. Рога этого оленя средних размеров имели маленький первый отросток у розетки и примитивно узкое проксимальное веерообразное расширение. Морфология D. pontica sp. nov. позволяет отнести этот вид к филогенетической ветви современной иранской лани, D. mesopotamica (Brooke, 1875). Остатки Dama в Тавриде – древнейшие в Европе. Возраст фауны Тавриды, по данным биохронологии, оценивается в пределах 1.8–1.5 млн л. н. Находка свидетельствует, что дивергенция ветвей европейской и месопотамской ланей произошла не позже 1.5 млн л. н. Гипотезы о происхождении ланей oт ‘Pseudodama’ на рубеже раннего и среднего плейстоцена требуют пересмотра.

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