Results 91 to 100 of about 9,024 (216)
X-ray fluorescence analyses of the Maastrichtian interval of IODP Site 342-U1403
X-ray fluorescence analyses of the Maastrichtian interval of IODP Site 342 ...
Batenburg, Sietske J +33 more
core +1 more source
Fossils of the type Maastrichtian
The south-western Indian Ocean islands, excluding the microcontinent of Madagascar, are geologically complex and diverse. They have been subject to drastic sea level changes, volcanic events and anthropogenic changes, all of which have contributed to confuse understanding of their avian biogeography.
Jagt, J.W.M. (John) +2 more
openaire +1 more source
Maastrichtian planktic foraminifera of the South Atlantic Ocean
Stratigraphic, faunal and isotopic analyses of the Maastrichtian at DSDP sites 525A and 21 in the South Atlantic reveal a planktic foraminiferal fauna characterized by two major events, an early late Maastrichtian diversification and end-Maastrichtian ...
Gerta Keller (6886058) +3 more
core +1 more source
Campanian and Maastrichtian ammonites from East and North-East Greenland
Newly collected ammonites from Campanian and Maastrichtian strata in East and North-East Greenland are described. An early early Campanian fauna from Hold with Hope includes Neophylloceras, Pseudophyllites, Gaudryceras (Gaudryceras) mite (Hauer 1866) and
W. James Kennedy +2 more
doaj +1 more source
BackgroundThe earliest crocodylians are known primarily from the Late Cretaceous of North America and Europe. The representatives of Gavialoidea and Alligatoroidea are known in the Late Cretaceous of both continents, yet the biogeographic origins of ...
Eduardo Puértolas +2 more
doaj +1 more source
Upper Maastrichtian bivalve faunas from the Crimea, Maastricht and Mangyshlak [PDF]
Upper (but not uppermost) Maastrichtian bivalve faunas in the stratotypical Maastrichtian area and in the Crimea are extremely diverse and species rich, and represent a very littoral shallow and warm environment.
Dhondt, A.
core
Two hyperthermal events with different carbon cycle perturbations occurred across the Cretaceous-Palaeogene boundary, i.e., the late Maastrichtian Warming Event and the Early Danian Dan-C2 event.
Mingming Ma +3 more
doaj +1 more source
(Table 2) Distribution of Manumiella seelandica in Maastrichtian sediments of the Bass River Section in the southern New ...
Saeedi, Farnosh +3 more
core +1 more source
(Appendix A) Size-related isotopic trends in the Maastrichtian planktic foraminifera Planoglobulina multicamerata of DSDP Core 44 ...
Huber, Brian T +5 more
core +1 more source
(Appendix A) Size-related isotopic trends in the Maastrichtian planktic foraminifera Planoglobulina acervulinoides of DSDP Core 44 ...
Huber, Brian T +5 more
core +1 more source

