@article{MTMT:3165393,
	title = {A toothed turtle from the Late Jurassic of China and the global biogeographic history of turtles},
	url = {https://m2.mtmt.hu/api/publication/3165393},
	author = {Joyce, WG and Rabi, Márton and Clark, JM and Xu, X},
	doi = {10.1186/s12862-016-0762-5},
	journal-iso = {BMC EVOL BIOL},
	journal = {BMC EVOLUTIONARY BIOLOGY},
	volume = {16},
	unique-id = {3165393},
	year = {2016},
	eissn = {1471-2148}
}

@article{MTMT:2575619,
	title = {OSTEOLOGY, RELATIONSHIPS, AND ECOLOGY OF ANNEMYS ( TESTUDINES, EUCRYPTODIRA) FROM THE LATE JURASSIC OF SHAR TEG, MONGOLIA, AND PHYLOGENETIC DEFINITIONS FOR XINJIANGCHELYIDAE, SINEMYDIDAE, AND MACROBAENIDAE},
	url = {https://m2.mtmt.hu/api/publication/2575619},
	author = {Rabi, Márton and Sukhanov, VB and Egorova, VN and Danilov, I and Joyce, AG},
	doi = {10.1080/02724634.2013.807274},
	journal-iso = {J VERTEBR PALEONTOL},
	journal = {JOURNAL OF VERTEBRATE PALEONTOLOGY},
	volume = {34},
	unique-id = {2575619},
	issn = {0272-4634},
	abstract = {A complete description of the xinjiangchelyid turtles Annemys levensis and A. latiens is provided, based on all available material from the Upper Jurassic type locality of Shar Teg, Mongolia. Annemys latiens was previously known almost exclusively from shell material, but an undescribed skull from Shar Teg is referable to this species and its distinct morphology confirms the presence of two taxa at this locality. Annemys latiens has an elongated skull that markedly differs in proportions from those of A. levensis and resembles the shape of some recent, piscivorous turtles. The overall similarity of the shells of the two Annemys species combined with significant differences in the skull indicate that these turtles probably partitioned the aquatic niche by exploring different feeding strategies. Among xinjiangchelyids, at least three different skull morphotypes can be differentiated, which implies a moderate level of ecological diversification among Late Jurassic Asian turtles. Phylogenetic analysis weakly supports the inclusion of Annemys spp. into Xinjiangchelyidae and places xinjiangchelyids at the stem of Testudines, but the latter result is considered tentative. Phylogenetic definitions of Xinjiangchelyidae, Sinemydidae, and Macrobaenidae are provided for nomenclatural clarity and precision. SUPPLEMENTAL DATASupplemental materials are available for this article for free at www.tandfonline.com/UJVP},
	keywords = {EVOLUTION; INNER-MONGOLIA; Reptilia; XINJIANG; Junggar basin; SICHUAN BASIN; QIGU FORMATION; EXTANT TURTLES; MESOZOIC TURTLES; BASIN NW-CHINA},
	year = {2014},
	eissn = {1937-2809},
	pages = {327-352}
}

@article{MTMT:2141870,
	title = {An enormous Jurassic turtle bone bed from the Turpan Basin of Xinjiang, China},
	url = {https://m2.mtmt.hu/api/publication/2141870},
	author = {Wings, O and Rabi, Márton and Schneider, JW and Schwermann, L and Sun, G and Zhou, CF and Joyce, WG},
	doi = {10.1007/s00114-012-0974-5},
	journal-iso = {SCI NAT-HEIDELBERG},
	journal = {NATURWISSENSCHAFTEN},
	volume = {99},
	unique-id = {2141870},
	issn = {0028-1042},
	abstract = {A spectacular new terrestrial Konzentratlagerstatte is introduced from the Turpan Basin of Xinjiang, China that probably belongs to the late Middle Jurassic Qigu Formation. It contains a mass accumulation of "xinjiangchelyid" turtles preliminarily identified as Annemys sp. In the zone with the highest turtle concentration, complete and articulated turtle skeletons are tightly packed at a density of up to 36 turtles per square meter. The fossiliferous layer is thickened here and shows an erosional base. This high concentration zone outcrops approximately 10 m in length and shows no decrease in turtle density after exposing 2 m of the layer into the hillside. Adjacent is a more expansive zone of at least 10 m by 30 m. In this region, the fossiliferous layer is evenly thick, and approximately five, fully disarticulated turtles are present per square meter. A conservatively estimated 1,800 turtles may, therefore, have been deposited at this site. It is likely that these aquatic turtles gathered in a retreating water hole in a riverine environment during a drought, much as some aquatic turtles will do today, but perished when the habitat dried up completely. A following catastrophic rainfall event caused a debris flow, possibly channelized in a dry river bed, which transported complete turtles, disarticulated turtles, and mudstone clasts and deposited them after a short distance. This taphonomic model is consistent with previous environmental reconstructions of the Turpan Basin during the late Middle Jurassic in predicting the episodic breakdown of regional monsoonal circulation resulting in a seasonally dry climate with severe episodic droughts.},
	keywords = {debris flow; Middle Jurassic; vertebrate; Testudines; taphonomy; STRATA; JUNGGAR; TESTUDINES BAENIDAE; DEPOSITIONAL-ENVIRONMENTS; Xinjiangchelyidae; Konzentratlagerstatte},
	year = {2012},
	eissn = {1432-1904},
	pages = {925-935}
}