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]
Description
Map of the Lower Saxon Hills with Süntel center-right
DFMMh/FV 296, "skull part (articulated quadrate, squamosal, basisphenoid, and pterygoid), a disarticulated 40 cm long partial carapace, plastron, and one cervical vertebra."[9]
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.[11]
↑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 14 August 2026).{{cite journal}}: CS1 maint: DOI inactive as of August 2026 (link)
1234Diedrich, Cajus (1 June 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. Bibcode:2011PdPe...91..129D. doi:10.1007/s12549-010-0044-y.
Bibliography
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. Bibcode:2017Faci...63...19B. doi:10.1007/s10347-017-0501-4. S2CID135060170.
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. Bibcode:2011PdPe...91..129D. doi:10.1007/s12549-010-0044-y. S2CID140604517.