FIRST UPPER CRETACEOUS DINOSAUR TRACK ASSEMBLAGE FROM JORDAN (MIDDLE EAST) - PRELIMINARY RESULTS

被引:3
|
作者
Klein, Hendrik [1 ]
Gierlinski, Gerard [2 ]
Lallensack, Jens N. [3 ]
Abu Hamad, Abdalla [4 ]
Al-Mashakbeh, Habes [5 ]
Alhejoj, Ikhlas [4 ]
Konopka, Marcin [6 ]
Blonski, Marcin [7 ]
机构
[1] Saurierwelt Palaontol Museum, Alte Richt 7, D-92318 Neumarkt, Germany
[2] Polish Geol Inst, Rakowiecka 4, PL-00975 Warsaw, Poland
[3] Liverpool John Moores Univ, Sch Nat Sci & Psychol, James Parsons Bldg,Bryon St, Liverpool L3 3AF, Merseyside, England
[4] Univ Jordan, Environm & Appl Geol Dept, Amman 11942, Jordan
[5] Al al Bayt Univ, Dept Appl Earth & Environm Sci, Mafraq, Jordan
[6] Med Univ Warsaw, Dept Sports Cardiol & Noninvas Cardiovasc Imaging, Kondratowicza 8, PL-03242 Warsaw, Poland
[7] Ctr Postgrad Med Educ, Dept Musculoskeletal Trauma Surg & Orthopaed, Konarskiego 13, PL-05400 Otwock, Poland
关键词
Ajlun Group; Na'ur Formation; Cenomanian; footprints; theropod; sauropod; ornithopod; CROUCHING THEROPOD; SAUROPOD; ORNITHOPOD; PROVINCE;
D O I
10.14241/asgp.2020.10
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Dinosaur tracks from Jordan (Middle East) have only been briefly reported in geological overview papers and books. We present here the first description and documentation of Jordanian dinosaur tracks based on a new tracksite from the south-central part of the country. The track-bearing strata belong to marginal marine (tidal flat) deposits of the Na'ur Formation (Upper Cretaceous, Cenomanian). This unit largely consists of well-bedded limestones, dolomites and marls that contain abundant marine invertebrate fossils such as bivalves, ammonites and foraminifers. The dinosaur ichnofauna occurs on four different levels and comprises abundant theropod tracks and trackways as well as isolated sauropod and ornithopod tracks. Theropod trackways consist of two different morphotypes. Morphotype 1 is tridactyl (26 cm pes length) and with a broad, but short metatarsal area and resembles the ichnogenus Picunichnus from the Lower Cretaceous (Albian) of Argentina. Morphotype 2 (36 cm pes length) has extensive and narrow metatarsal impressions continuously occurring along regularly-spaced trackways. This suggests either a plantigrade movement of the trackmaker or reflects preservational factors. By their overall-shape with thin digits, Morphotype 2 resembles described penetrative tracks suggesting a strong influence of the substrate. Sauropod tracks are relatively small (40 cm pes length) and show low heteropody with a kidney-shaped manus imprint, pointing to a Sauropodichnus-like form. The single ornithopod pes track (18 cm in length) is similar to material described as Ornithopodichnus from the Lower Cretaceous of Korea. Due to the incomplete material of sauropod and ornithopod prints, no concrete assignment is given to this material and further study is needed. The presence of dinosaur tracks proves a temporary subaerial exposure of the surface whereas the main part of the Na'ur Formation is dominated by subaqueous activity of marine faunas.
引用
收藏
页码:331 / 342
页数:12
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