In-game article clicks load inline without leaving the challenge.
The Süntel Formation, previously known as the Kimmeridge Formation (German: "Mittlerer Kimmeridge"; Middle Kimmeridge), 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.
Description
Map of the Lower Saxon Hills with Süntel center-right
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"
DFMMh/FV 296, "skull part (articulated quadrate, squamosal, basisphenoid, and pterygoid), a disarticulated 40 cm long partial carapace, plastron, and one cervical vertebra."
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.
Bai, Hua-Qing; Betzler, Christian; Erbacher, Jochen; Reolid, Jesús; Zuo, Fanfan (2017). "Sequence stratigraphy of Upper Jurassic deposits in the North German Basin (Lower Saxony, Süntel Mountains)". Facies. 63 (3) 19. doi:. S2CID .
Lallensack, Jens N.; Sander, P. Martin; Knötschke, Nils; Wings, Oliver (2015). (PDF). Palaeontologia Electronica. 18.
Diedrich, C (2011). "Upper Jurassic tidal flat megatracksites of Germany - coastal dinosaur migration highways between European islands, and a review of the dinosaur footprints". Palaeobiodiversity and Palaeoenvironments. 91 (2): 129–155. doi:. S2CID .