Where: Libya (31.1° N, 13.2° E: paleocoordinates 19.6° N, 10.2° E)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Omphalocyclus macroporus foram zone, Lower Tar Member (Zimam Formation), Late/Upper Maastrichtian (70.6 - 66.0 Ma)
• Upper portion (unit 8 of Salaj & Nairn 1987) of the Lower Tár Member (Zimam Formation), of late Maastrichtian age (Omphalocyclus macroporus Zone). Corresponds to the Gansserina gansseri, Abathomphalus mayaroensis and Falsotruncana falsocalcarata zones of the planktic foraminifera scheme. Located about 35 m below the base of massive limestones of the Danian Hád Member.
• bed-level stratigraphic resolution
Environment/lithology: open shallow subtidal; lithified, shelly/skeletal packstone
Size class: macrofossils
Collection methods: Repository: Institute of Paleobiology, Polish Academy of Sciences, Warszawa
Primary reference: M. Machalski, J. W. M. Jagt, N. H. Landman and J. Uberna. 2009. First record of the North American scaphitid ammonite Discoscaphites iris from the upper Maastrichtian of Libya. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 254:373-378 [M. Clapham/M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 208625: authorized by Matthew Clapham, entered by Matthew Clapham on 07.04.2020
Creative Commons license: CC BY (attribution)
Taxonomic list
Cephalopoda | |
Discoscaphites iris Conrad 1858 ammonite |