000			02269nab a2200313 c 4500
001			vtls000644259
003			RU-ToGU
005			20210922095931.0
007			cr |
008			181121|2017 xxu s a eng dd
024	7		_a10.1016/j.cretres.2017.05.004 _2doi
035			_ato000644259
040			_aRU-ToGU _brus _cRU-ToGU
100	1		_aSkutschas, Pavel P. _9100143
245	1	0	_aEarly Cretaceous choristoderes (Diapsida, Choristodera) from Siberia, Russia _cP. P. Skutschas, D. D. Vitenko
504			_aБиблиогр.: с. 91-92
520	3		_aThere are ten known Lower Cretaceous localities for skeletal remains of choristoderes in Siberia (Russia). Choristoderan remains at all these localities are represented by isolated bones, usually by isolated vertebrae of Choristodera indet. Three choristoderan taxa in two geological units were identified: the non-neochoristodere Khurendukhosaurus sp. (possibly closely related to the long-necked Sino-Japanese hyphalosaurids) from the Murtoi Formation, Transbaikalia; cf. Khurendukhosaurus sp. and the “Shestakovo choristodere” with possible neochoristoderan affinities from the Ilek Formation, Western Siberia. All these three choristoderan taxa had a microanatomical organization of vertebrae similar to that of in advanced large neochoristoderes (vertebral centra with tight spongiosa). The Siberian fossil record includes the westernmost (Shestakovo locality, Ilek Formation) and the northernmost (Teete locality, the Sangarian Group) occurrences of the Early Cretaceous choristoderes in Asia. Like in other regions of Asia, Siberian localities are characterized by the absence of neosuchian crocodyliforms.
653			_aСибирь
653			_aхористодеры
653			_aранний меловой период
653			_aокаменелости
655		4	_aстатьи в журналах _9745982
700	1		_aVitenko, Dmitriy D. _9474388
773	0		_tCretaceous research _d2017 _gVol. 77. P. 79-92 _x0195-6671
852	4		_aRU-ToGU
856	7		_uhttp://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000644259
908			_aстатья
999			_c443555