2012Unpublished venueRequires access

CRETACEOUS TETRAPOD FOOTPRINT BIOSTRATIGRAPHY, BIOCHRONOLOGY, AND ICHNOFACIES

Martin G. Lockley, Spencer G. Lucas, Masaki Matsukawa, Jerald D. Harris

Open publisher page 18 citations

Abstract

The global record of Cretaceous tetrapod footprints is dominated by the tracks of non-avian dinosaurs and birds; fewer tracks are known of pterosaurs, crocodylians, turtles, mammals, and other tetrapods. The Cretaceous track record is best known from East Asia (especially China and Korea) and western North America. A moderately extensive record is also known from South America (primarily Argentina and Brazil), but Cretaceous track assemblages from Europe, Africa, and Australia are much more poorly known. Here, we re-examine two global footprint biochrons based on the Cretaceous tetrapod footprint record. An Early Cretaceous biochron is characterized by sauropod and ornithopod tracks. A Late Cretaceous biochron has fewer sauropod tracks but adds the tracks of hadrosaurs, tyrannosaurids, and

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The global record of Cretaceous tetrapod footprints is dominated by the tracks of non-avian dinosaurs and birds; fewer tracks are known of pterosaurs, crocodylians, turtles, mammals, and other tetrapods. The Cretaceous track record is best known from East Asia (especially China and Korea) and western North America. A moderately extensive record is also known from South America (primarily Argentina and Brazil), but Cretaceous track assemblages from Europe, Africa, and Australia are much more poorly known. Here, we re-examine two global footprint biochrons based on the Cretaceous tetrapod footprint record. An Early Cretaceous biochron is characterized by sauropod and ornithopod tracks. A Late Cretaceous biochron has fewer sauropod tracks but adds the tracks of hadrosaurs, tyrannosaurids, and

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Available abstract

The global record of Cretaceous tetrapod footprints is dominated by the tracks of non-avian dinosaurs and birds; fewer tracks are known of pterosaurs, crocodylians, turtles, mammals, and other tetrapods. The Cretaceous track record is best known from East Asia (especially China and Korea) and western North America. A moderately extensive record is also known from South America (primarily Argentina and Brazil), but Cretaceous track assemblages from Europe, Africa, and Australia are much more poorly known. Here, we re-examine two global footprint biochrons based on the Cretaceous tetrapod footprint record. An Early Cretaceous biochron is characterized by sauropod and ornithopod tracks. A Late Cretaceous biochron has fewer sauropod tracks but adds the tracks of hadrosaurs, tyrannosaurids, and

Key concepts: Tetrapod (structure), Cretaceous, Paleontology, Geology, Ichnofacies, Footprint, Biochronology, Biostratigraphy

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