Инд. авторы:	Foronova I.V.
Заглавие:	Early Quaternary History of the Genus Archidiskodon (Proboscidea, Elephantidae) in Western Siberia: to the Question of Intermediate Links in Mammoth Lineage
Библ. ссылка:	Foronova I.V. Early Quaternary History of the Genus Archidiskodon (Proboscidea, Elephantidae) in Western Siberia: to the Question of Intermediate Links in Mammoth Lineage // Proceedings of the Zoological Institute RAS. - 2018. - Т.322. - № 3. - С.241-258.
Идентиф-ры:	РИНЦ: 36290689;
Реферат:	rus: Статья посвящена ранним представителям линии Archidiskodon-Mammuthus из отложений нижнего плейстоцена юга Западной Сибири (Кузнецкая котловина). В пределах рода Archidiskodon описаны формы (A. meridionalis, A. m. tamanensis, A. m. voigtstedtensis, A. aff. wüsti), представляющие собой последовательные стадии прогрессивного преобразования линии на раннем этапе ее развития. Морфометрические данные коренных зубов (М3) изучены с помощью авторского метода исследования группы, что позволило уточнить систематическую принадлежность рассматриваемых таксонов и их положение в структуре филетической мамонтовой линии. Показано, что форма, выделявшаяся ранее под названием «слон Вюста», но впоследствии отнесенная к виду M. trogontherii, значимо отличается от последнего по частоте и длине пластин. Она также хорошо выделяется статистически, и рассматривается, как самостоятельный и самый поздний таксон в составе архидискодонтной группы слонов. В структуре филетической мамонтовой линии A. wüsti занимает четкую позицию промежуточной формы (своеобразного моста, по словам Г. Полига) между родами Archidiskodon и Mammuthus. Таким образом, с помощью многомерных диаграмм используемого авторского метода стало возможным приблизиться к выявлению так называемых промежуточных звеньев в мамонтовой линии. Обсуждаются также направление филетического развития и некоторые адаптации группы во второй половине раннего плейстоцена. Приводятся сведения о сопутствующей фауне и времени существования описанных видов на рассматриваемой территории. eng: The paper is concerned with the early representatives of the Archidiskodon-Mammuthus lineage from the sediments of Lower Pleistocene of the South of Western Siberia (Kuznetsk Basin). Several forms were being described within the genus Archidiskodon (A. meridionalis, A. m. tamanensis, A. m. voigtstedtensis, A. aff. wüsti) which represent consecutive steps of progressive development of the lineage on the early stage of its evolution. Morphometric features of molars (M3) have been studied using the author's original method designed for this group, which allowed specifying systematic attribution of the taxa under study and their position in the structure of the mammoth lineage. It was demonstrated that the form previously distinguished as Wüst's elephant and later attributed to the species M. trogontherii significantly differs from the latter in frequency and length of the plates. This form also stands out well statistically and is regarded as a separate and the latest taxon among the archidiskodon group of elephants. A. wüsti occupies a distinct position of an intermediate form (a ‘bridge' as H. Pohlig put it) between the genera Archidiskodon and Mammuthus in the structure of the mammoth lineage. Thus, the multi-dimensional diagrams used in our method permit to take a step close to revealing of so-called intermediate links in the mammoth lineage. Direction of phyletic development and some adaptations of the group in the second half of Early Pleistocene are also discussed. Account is also given to the accompanying fauna and the existence period of these species on the territory under study.
Ключевые слова:	early Pleistocene; Kuznetsk Basin; lineage; molars; western Siberia; биостратиграфия; ранний плейстоцен; кузнецкая котловина; biostratigraphy; Archidiskodon; западная Сибирь; моляры; филетическая линия;
Издано:	2018
Физ. хар-ка:	с.241-258
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