Tetrapod footprints have a fossil record in rocks of Devonian-Neogene age. Three principal
factors limit their use in biostratigraphy and biochronology (palichnostratigraphy): invalid …

Rugose corals are one of the major fossil groups in shallow-water environments. They
played an important role in dividing and correlating Carboniferous strata during the last …

Tetrapod trace fossils (primarily footprints) provide significant insight into some major events
of the Paleozoic evolution of tetrapods. The oldest fossils of tetrapods are Middle Devonian …

Well-preserved fish and tetrapod trace fossils occur in Carboniferous (Stephanian C) beds at
Puertollano. They represent the first evidence of vertebrate ichnites in the Carboniferous of …

The Carboniferous record of tetrapod footprints is mostly of Euramerican origin and provides
the basis for a footprint biostratigraphy and biochronology of Carboniferous time that …

Well established distribution patterns for Late Silurian-Early Devonian vertebrates indicate
two basic provinces for the Gondwana supercontinent–an East Gondwana Province …

The Lower Permian ichnofauna in the Collio Formation (Artinskian) in the Val Trompia
(Brescian Prealps, North Italy) has been studied for a long time, but the studies have focused …

The stratigraphic record, distribution, associated faunal elements and environment of the
typical hybodontiform form taxon Lissodus (comprising Lissodus BROUGH, 1935 and …

Numerous tetrapod footprints have been found in the Permian deposits of the Western
Orobic Prealps (Upper Gerola Valley, Sondrio and Lecco Provinces, Lombardy, Italy). The …

The Late Permian mass extinction occurring at 252.6±0.2 Ma is the most severe
Phanerozoic extinction event and was preceded and followed by additional disturbances …