Montemarcello Formation
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The Montemarcello Formation is a
Late Triassic The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch ...
( Carnian) geologic
formation Formation may refer to: Linguistics * Back-formation, the process of creating a new lexeme by removing or affixes * Word formation, the creation of a new word by adding affixes Mathematics and science * Cave formation or speleothem, a secondar ...
in
Liguria Liguria (; lij, Ligûria ; french: Ligurie) is a Regions of Italy, region of north-western Italy; its Capital city, capital is Genoa. Its territory is crossed by the Alps and the Apennine Mountains, Apennines Mountain chain, mountain range and is ...
,
Italy Italy ( it, Italia ), officially the Italian Republic, ) or the Republic of Italy, is a country in Southern Europe. It is located in the middle of the Mediterranean Sea, and its territory largely coincides with the homonymous geographical re ...
.Montemarcello Formation
in the
Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals, plants, and microorganisms. History The Paleobiology Database (PBDB) originated in the NCEAS-funded Phanerozoic Marine Pale ...
Fossil
prosauropod Sauropodomorpha ( ; from Greek, meaning "lizard-footed forms") is an extinct clade of long-necked, herbivorous, saurischian dinosaurs that includes the sauropods and their ancestral relatives. Sauropods generally grew to very large sizes, had lon ...
tracks have been reported from the formation.Weishampel et al., 2004, pp.517-607


Description

The formation comprises arenites with a few thin clayey inter-beds. The sands overlie micro-conglomeratic bodies up to thick. Two-dimensional ripple marks (with wavelengths of nearly ), larger ripples (wavelengths of ), interference ripples, and mud cracks were recognized. The arenitic beds are also characterized by internal structures such as accretionary laminae, coalescent bodies, low-angle lamination, and cross stratification. Some arenitic levels are deeply bioturbated, both by simple vertical tubes and by larger horizontal ones. Rare small wood fragments were recognized. Small channels, up to over a very short distance, cut the arenitic bodies.Lerici
in the
Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals, plants, and microorganisms. History The Paleobiology Database (PBDB) originated in the NCEAS-funded Phanerozoic Marine Pale ...


Fossil content

The following fossils were reported from the formation: * '' Evazoum sirigui''Nicosia & Loi, 2003 * '' Anomoepus sp.''Leonardi, 2000 * '' Eosauropus sp.''Lockley et al., 2006 * '' Grallator (Eubrontes)'' * Chirotheriidae indet.


See also

*
List of dinosaur-bearing rock formations This list of dinosaur-bearing rock formations is a list of geologic formations in which dinosaur fossils have been documented. Containing body fossils * List of stratigraphic units with dinosaur body fossils ** List of stratigraphic units with few ...
** List of stratigraphic units with sauropodomorph tracks *** Prosauropod tracks * List of fossiliferous stratigraphic units in Italy


References


Bibliography

* * * * * {{cite LSA , last=Dalla Vecchia , first=F.M , year=1995 , title=I dinosauri in Italia: stato delle conoscenze - Dinosaurs in Italy: state of knowledge , journal= Natura Nascosta , volume=11 , pages=29–35 Geologic formations of Italy Triassic System of Europe Triassic Italy Carnian Stage Sandstone formations Shale formations Fluvial deposits Ichnofossiliferous formations Paleontology in Italy