KT boundary
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Recent papers in KT boundary
The Cretaceous-Paleogene boundary~ 65.5 million years ago marks one of the three largest mass extinctions in the past 500 million years. The extinction event coincided with a large asteroid impact at Chicxulub, Mexico, and occurred within... more
The Cretaceous-Paleogene boundary ~65.5 million years ago marks one of the three largest mass extinctions in the past 500 million years. The extinction event coincided with a large asteroid impact at Chicxulub, Mexico, and occurred within... more
Large impacts are credited with the most devastating mass extinctions in Earth’s history and the Cretaceous – Tertiary (K/T) boundary impact is the strongest and sole direct support for this view. A review of the five largest Phanerozoic... more
Impact stratigraphy is an extremely useful correlation tool that makes use of unique events in Earth’s history and places them within spatial and temporal contexts. The K-T boundary is a particularly apt example to test the limits of this... more
The Cretaceous–Tertiary boundary (KTB) mass extinction is primarily known for the demise of the dinosaurs, the Chicxulub impact, and the frequently rancorous thirty-years-old controversy over the cause of this mass extinction. Since 1980... more
Arambourg was the first to conduct methodical vertebrate palaeontological studies in the Oulad Abdoun and Ganntour phosphatic basins of Morocco between the 1930s and 1950s. As early as 1935, he identified the main stratigraphical levels of... more
–The suevite breccia of the Chicxulub impact crater, Yucatàn, Mexico, is more variable and complex in terms of composition and stratigraphy than suevites observed at other craters. Detailed studies (microscope, electron microprobe, SEM,... more
A 40 m stratigraphic section at Gorgonilla Island, Colombia, provides a unique deep-marine, low-latitude, Southern Hemisphere record of events related to the end-Cretaceous Chicxulub impact and the global Cretaceous/Paleogene boundary... more
Twelve fossil species of Proteaceous pollen, predominantly attributable to Proteacidites and Beaupreaidites, were recovered from the MaastrichtianePaleocene sedimentary succession of the Garden Cove Formation on Campbell Island, the... more
Abstract Terrestrial pollen and spores in late Maastrichtian to early Paleocene marine strata at mid-Waipara, New Zealand, permit reconstruction of contemporary vegetation and paleoclimates. During the latest Cretaceous, spore-pollen... more
Bolide impact and flood volcanism compete as leading candidates for the cause of terminal-Cretaceous mass extinctions. High-precision (40)Ar/(39)Ar data indicate that these two mechanisms may be genetically related, and neither can be... more
The Cretaceous–Tertiary boundary (KTB) is one of the easiest epoch boundaries to identify, whether based on lithological changes in the field, geochemical analysis in the laboratory, or fossil content. A set of five KTB-identifying... more
The devastating effect on terrestrial plant communities of a bolide impact at the Cretaceous-Tertiary boundary is shown in fossil pollen and spore assem-blages by a diverse flora being abruptly replaced by one dominated by a few species... more
Dit proefschrift ontrafelde de evolutionaire geschiedenis van de ammonie ten, een uitgestorven groep van uitsluitend mariene dieren behorende tot de Klasse van de Cephalopoda. Ze vormen dé nummer één... more
A new heterosporous fern species, Azolla boliviensis sp. nov., is described from latest Maastrichtian (latest Cretaceous) to Paleocene (earliest Palaeogene) terrestrial sediments of the Eslabón and Flora Formations, Subandean belt,... more
A gavialoid crocodylian from the Maastrichtian of the Oulad Abdoun phosphatic Basin (Morocco) is described, representing the oldest known crocodylian from Africa. The specimen consists of a skull that exhibits several features not found... more
Thanks to an intensive field work undertaken in spring 2000 with the collaboration between various French and Moroccan organisations, numerous Crocodyliformes remains has been recovered from the phosphatic marine layers from the... more