Also known as James Ross Archipelago
Where: Antarctica (64.3° S, 56.8° W: paleocoordinates 62.6° S, 67.3° W)
• coordinate estimated from map
When: López de Bertodano Formation, Late/Upper Maastrichtian (70.6 - 66.0 Ma)
• “molluscan units”
• bed-level stratigraphic resolution
Environment/lithology: marine; lithified shale and sandstone
Size class: macrofossils
• DJ.953.690, six vertebrae and five associated vertebral fragments
•DJ.953.751, large proximal portion of a rib
Preservation: concretion
Collected by British Antarctic Survey (BAS)
Collection methods: quarrying, surface (in situ), mechanical,
• Collected under the auspices of the British Antarctic Survey (BAS) and reposed in Cambridge.
Primary reference: J. E. Martin and J. A. Crame. 2006. Palaeobiological significance of high-latitude Late Cretaceous vertebrate fossils from the James Ross Basin, Antarctica. Cretaceous-Tertiary high-latitude palaeoenvironments: James Ross Basin, Antarctica 258(1):109-124 [E. Vlachos/F. Aspromonte/F. Aspromonte]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 232783: authorized by Evangelos Vlachos, entered by Franco Aspromonte on 29.12.2023
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
| |
cf. Elasmosauridae indet. Cope 1869 elasmosaur DJ.953.690, six vertebrae and five associated vertebral fragments
|