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From Wikipedia, the free encyclopedia
The Tlayúa Formation is an Early Cretaceous (late Albian) geological formation near Tepexi de Rodríguez, Puebla.[1]
Tlayúa Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Sub-units | Lower, Middle and Upper Members |
Underlies | Unconformity with Eocene-Oligocene Pie de Vaca Formation |
Overlies | Orizaba Formation |
Thickness | Lower: 50 m Middle: 35 m Upper: 40 m |
Lithology | |
Primary | Limestone |
Other | Mudstone |
Location | |
Coordinates | 19.1°N 98.2°W |
Approximate paleocoordinates | 17.1°N 61.6°W |
Region | Puebla |
Country | Mexico |
Type section | |
Named for | Tlayúa Quarry |
The formation contains a diverse array of vertebrate and invertebrate fossils. About 70% of the macrofossils are osteichthyan fish.[2] Other vertebrates include chelonians, pterosaurs, lepidosaurs, and crocodiles.[3] Cyanobacteria, foraminifera, algae, gymnosperms, sponges, cnidarians, annelids, gastropods, ammonites, bivalves, arachnids, insects, isopods, anomurans, brachyurans, crinoids, echinoids, holothuroids, stelleroids, and ophiuroids, have also been recovered from the Tlayúa Formation.[3][4][5]
Genus | Species | Abundance | Notes |
---|---|---|---|
Huehuecuetzpalli | H. mixtecus | A primitive lizard | |
Pamizinsaurus | P. tlayuaensis | An osteoderm-covered sphenodontian | |
Ankylosphenodon[6] | A. pachyostosus | An aquatic sphenodontian | |
Tepexisaurus[7] | T. tepexii | A basal scincomorph | |
Mainly after González-Rodríguez (2016)[8] and Applegate et al. (2006)[9]
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