Also known as Beth Zayit
Where: Jerusalem, Israel (31.8° N, 35.2° E: paleocoordinates 8.0° N, 29.7° E)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Gallic to Gallic (125.8 - 93.5 Ma)
• "track-bearing layer...is below the Mozza marls, which present the lowest part of a fossiliferous series of Middle to Upper Cenomanian; the complex of which the dinosaur beds are part is 200-250 m thick and is underlined by marine layers of Albian age." Formation is not named, but is below the "middle Cenomanian Acanthoceras beds." (Note that "Mozza marls" = "Moza marl".)
• bed-level stratigraphic resolution
Environment/lithology: lacustrine; yellow, argillaceous limestone
Size class: macrofossils
Preservation: trace
Collected by M. Sofer
Collection methods: surface (in situ),
• Tracks occur on an 80 sq-m slab.
Primary reference: M. Avnimelech. 1962. Dinosaur tracks in the Lower Cenomanian of Jerusalem. Nature 196(4851):264 [M. Carrano/M. Carrano/M. Carrano]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 28227: authorized by Matthew Carrano, entered by Matthew Carrano on 30.01.2003
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
Theropoda indet. theropod single individual trackway with 20+ prints; others alongside in slab; author claims tracks perhaps made by Elaphrosaurus bambergi
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Aves | |
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