Also known as Goniopholis kiplingi type locality
Where: England, United Kingdom (50.6° N, 1.9° W: paleocoordinates 41.5° N, 7.9° E)
• coordinate stated in text
• small collection-level geographic resolution
When: Stair Hole Member (Durlston Formation), Late/Upper Berriasian (145.0 - 140.2 Ma)
• Bed 129b (Clements, 1993), Intermarine beds sensu Wimbledon in Benton & Spencer(1995; = Intermarine Member sensu Clements, 1993), Stair Hole Member sensu Westhead & Mather (1996), Purbeck Limestone Group; Berriasian, Lower Cretaceous (Salisbury et al., 1999; Milner & Batten, 2002).
•
•Durlston Formation is likely upper Berriasian in age based on magnetostratigraphy (Ogg et al. 1994; Ogg et al. 2008) and correlates to other upper Berriasian assemblages in Europe (e.g. Wimbledon and Hunt 1993).
• bed-level stratigraphic resolution
Environment/lithology: terrestrial; fine-grained, gray, white, sandy limestone and calcareous mudstone
Size class: macrofossils
Primary reference: M. B. d. Andrade, R. Edmonds, M. J. Benton and R. Schouten. 2011. A new Berriasian species of Goniopholis (Mesoeucrocodylia, Neosuchia) from England, and a review of the genus. Zoological Journal of the Linnean Society 163:S66-S108 [P. Mannion/P. Mannion]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 123271: authorized by Philip Mannion, entered by Philip Mannion on 17.01.2012
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Plantae indet. Haeckel 1866 | |
Reptilia | |
Goniopholis kiplingi n. sp.
Goniopholis kiplingi n. sp. Andrade et al. 2011 crocodilian DORCM 12154 - type (well-preserved skull, dorsoventrally flattened, lacking mandibles and most teeth)
| |
"Chelonia indet." = Testudines
"Chelonia indet." = Testudines Batsch 1788 turtle | |
Bivalvia | |
Bivalvia indet. Linnaeus 1758 clam |