The Süntel Formation, previously known as the Kimmeridge Formation (German: "Mittlerer Kimmeridge"; Middle Kimmeridge),[1] is a geological formation in Germany. It is Late Jurassic in age, spanning the early to late Kimmeridgian stage. It predominantly consists of limestone deposited in shallow marine carbonate ramp conditions.[2]
DfMMh/FV2/19, a small pedal phalanx III-1, DfMMh/FV3/19, proximal part of a small right fibula
Theropoda
Hannover: Lindener Berg, Tönniesberg, and Ahlem, Thüste, Marienhagen, Holzen, Kahlberg and Langenberg Quarry
18 distinct morphotypes of teeth, referred to "Tyrannosauroidea, as well as Allosauroidea, Megalosauroidea cf. Marshosaurus, Megalosauridae cf. Torvosaurus and probably Ceratosauria"[5]
DFMMh/FV 296, "skull part (articulated quadrate, squamosal, basisphenoid, and pterygoid), a disarticulated 40 cm long partial carapace, plastron, and one cervical vertebra."[6]
DFMMh/FV 500, an articulated partial skeleton consisting of "10 thoracic vertebrae, complete pelvis and sacrum, left and right femur" with an associated possible partial right tibia.[9]
^ abcMartin T, Averianov AO, Schultz JA, Schwermann AH, Wings O (2019-08-07). "Late Jurassic multituberculate mammals from Langenberg Quarry (Lower Saxony, Germany) and palaeobiogeography of European Jurassic multituberculates". Historical Biology. 33 (5): 616–629. doi:10.1080/08912963.2019.1650274. S2CID201201555.
^Martin TH, Schultz JA, Schwermann AH, Wings OL (2016). "First Jurassic mammals of Germany: Multituberculate teeth from Langenberg Quarry (Lower Saxony)". Palaeontologia Polonica. 67: 171–9. doi:10.4202/pp.2016.67_171 (inactive 31 January 2024).{{cite journal}}: CS1 maint: DOI inactive as of January 2024 (link)