An enormous Jurassic turtle bone bed from the Turpan Basin of Xinjiang, China

被引:25
作者
Wings, Oliver [1 ,3 ]
Rabi, Marton [3 ,8 ,9 ]
Schneider, Joerg W. [7 ]
Schwermann, Leonie [2 ]
Sun, Ge [4 ]
Zhou, Chang-Fu [5 ]
Joyce, Walter G. [3 ,6 ]
机构
[1] Museum Nat Kunde Berlin, D-10115 Berlin, Germany
[2] Univ Bonn, Steinmann Inst Geol Mineral & Palaontol, D-53115 Bonn, Germany
[3] Univ Tubingen, Dept Geosci, D-72074 Tubingen, Germany
[4] Jilin Univ, Changchun 130023, Jilin, Peoples R China
[5] Shenyang Normal Univ, Inst Paleontol, Shenyang 110034, Peoples R China
[6] Yale Peabody Museum Nat Hist, New Haven, CT 06511 USA
[7] TU Bergakad Freiberg, Lehrstuhl Palaontol, Inst Geol, D-09599 Freiberg, Germany
[8] MTA ELTE Lendulet Dinosaur Res Grp, Budapest, Hungary
[9] Eotvos Lorand Univ, Dept Paleontol, H-1117 Budapest, Hungary
关键词
Middle Jurassic; Taphonomy; Debris flow; Konzentratlagerstatte; Testudines; Xinjiangchelyidae; TESTUDINES BAENIDAE; VERTEBRATE; JUNGGAR; STRATA;
D O I
10.1007/s00114-012-0974-5
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
引用
收藏
页码:925 / 935
页数:11
相关论文
共 35 条
  • [1] [Anonymous], 1970, NEUES JAHRB GEOL P-M
  • [2] [Anonymous], 1980, MEM I VERT PALEONT P
  • [3] Batsch A., 1788, Versuch einer Anleitung, zur KenntniSS und Geschichte der Thiere und Mineralien
  • [4] Taphonomy of turtles in the Middle Eocene Bridger formation, SW Wyoming
    Brand, LR
    Goodwin, HT
    Ambrose, PD
    Buchheim, HP
    [J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2000, 162 (1-2) : 171 - 189
  • [5] Brinkman DB, 2012, MORPHOLOGY EVOLUTION
  • [6] Collinson J.D., 2006, SEDIMENTARY STRUCTUR, V3rd
  • [7] Dong Zhiming, 1997, P96
  • [8] Dong Zhiming., 1992, Dinosaurian faunas of China, Vi-x, P1
  • [9] Dalton Wells: Geology and significance of debris-flow-hosted dinosaur bonebeds in the Cedar Mountain Formation (Lower Cretaceous) of eastern Utah, USA
    Eberth, DA
    Britt, BB
    Scheetz, R
    Stadtman, KL
    Brinkman, DB
    [J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2006, 236 (3-4) : 217 - 245
  • [10] Sequence stratigraphy, paleoclimate patterns, and vertebrate fossil preservation in Jurassic-Cretaceous strata of the Junggar Basin, Xinjiang Autonomous Region, People's Republic of China
    Eberth, DA
    Brinkman, DB
    Chen, PJ
    Yuan, FT
    Wu, SZ
    Li, G
    Cheng, XS
    [J]. CANADIAN JOURNAL OF EARTH SCIENCES, 2001, 38 (12) : 1627 - 1644