Tlayúa Formation
Geologic formation in Mexico
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The Tlayúa Formation is an Cretaceous Konservat-Lagerstätte near Tepexi de Rodríguez, Puebla, Central Mexico.[1] It consists of three members (Lower, Middle and Upper), spanning the lower Albian of the Early Cretaceous to the lower Cenomanian of the Late Cretaceous. It consists of a series of limestone quarries that preserve lagoonal palaeoenvironments, such as a shelf lagoon, a shallow lagoon surrounded by a peneplain, and a tidal flat. It is notable for preserving high quantities of vertebrate and invertebrate fossils, and is thus considered a Lagerstätte.
| Tlayúa Formation | |
|---|---|
| Stratigraphic range: | |
Cipactlichthys scutatus, one of the fossil fish from Tlayúa Formation | |
| 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 |
Description
The Tlayúa Formation was first described by Jerjes Pantoja-Alor in 1992.[2] It is located in the Tlayúa ravine, which itself lies in the southern portion of Puebla, Central Mexico, near Tepexi de Rodríguez,[1] and consists of a series of limestone quarries that has seen commercial use for decades.[3]
Stratigraphy
The Tlayúa Formation consists of two stratigraphic units (Tlayúa and Barranca Abuelo)[4] and three members. The Lower Member is lower Albian in age. It consists of bioturbated limestones, and is characterised by the presence of the non-rudist bivalve Chondrodonta and the rudist bivalve Toucasia polygyra. The Middle Member, corresponding to the Tlayúa Quarry, is the most fossiliferous.[3] Its age has been difficult to ascertain, as the foraminiferan Spiroloculina cretacea is known exclusively from lower Cenomanian strata,[5] though it has since been determined to be Upper Albian.[3] The Middle Member consists of fine-grained lithographic limestones, interspersed with hematitic layers that preserve its vertebrate fauna. The Upper Member is Cenomanian in age, and consists of a sequence of dolomites. It is characterised by the presence of the miliolid foraminiferan Dicyclina schlumbergi.[3]
Depositional environments
The depositional environment of the Tlayúa Formation was likely a shallow, coastal lagoon,[6] with some freshwater influence, as indicated by the presence of crocodilian and turtle fossils.[6][7] The Lower Member of the Tlayúa Formation represents a carbonate environment which apparently had stressed biodiversity.[4] The depositional environment of the Middle Member was likely arid for much of the year, with the exception of seasonal rains and storms.[7] The Upper Member likely represents a tidal flat.[4] The Tlayúa Formation may have been part of an island, though a connection to the North American mainland cannot be discounted.[7]
Paleobiota
The formation contains a diverse array of vertebrate and invertebrate fossils. For this reason, it is considered a Konservat-Lagerstätte.[4][7] About 70% of the macrofossils are osteichthyan fish.[8] Other vertebrates include chelonians, pterosaurs, lepidosaurs, and crocodiles.[9] 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.[9][10][11]
Archelosaurs

The remains of several indeterminate archelosaur taxa have been recovered from the Tlayúa Formation. Indeterminate crocodilians and turtles have been identified.[6][7] Partial, articulated wings of an unidentified pterosaur have been discovered from the formation. Though tentatively assigned to Pteranodon sp. and Nyctosaurus sp. in 2008,[12] they likely represent either an early azhdarchoid or an indeterminate ornithocheiromorph.[13]
Lepidosaurs
| Genus | Species | Material | Notes |
|---|---|---|---|
| Huehuecuetzpalli[14] | H. mixtecus | Near-complete specimens of an adult and a juvenile | A primitive lizard |
| Pamizinsaurus[15] | P. tlayuaensis | A single, crushed skull of a juvenile | An osteoderm-covered sphenodontian |
| Ankylosphenodon[16] | A. pachyostosus | Front half of a partial skeleton | An aquatic sphenodontian |
| Tepexisaurus[17] | T. tepexii | Near-complete skeleton, minus the tail | A basal scincomorph |
Fish
Mainly after González-Rodríguez (2016)[18] and Applegate et al. (2006)[3]
| Fish | |||||
|---|---|---|---|---|---|
| Genus | Species | Higher taxon | Notes | Images | |
| Amblysemius? | cf. A. sp | Caturidae | Only non-amiid amiiform from Tlayúa[18] | ||
| Araripichthys | A. weberi | Teleostei | Possibly related to Late Cretaceous genera from North America?[19] | ||
| Armigatus | A. felixi, A. carrhenoae | Ellimmichthyiformes | First records of Armigatus from America, alongside the oldest species in the genus,[20] the two species from Tlayúa also seem to clade closest to each other[21] | ||
| Aspidorhynchidae spp. | Inapplicable | Teleostei | Undescribed species of Vinctifer and Belonostomus have been recorded[18] | ||
| Axelrodichthys | A. cf. A. araripensis | Mawsoniidae | Only known specimen was lost before description[18] | ||
| Bananogmius? | cf. B. sp | Tselfatiiformes | One of the few Mexican members of the clade other than Tselfatia[18] | ||
| Cipactlichthys | C. scutatus | Halecomorphi | Bears large plate-like scutes along its midline[22] | ||
| Ellimmichthys | E. sp[23] | Ellimmichthyiformes | Type genus of its order | ||
| Elopomorpha spp. | Unapplicable | Teleostei | Possible species of Brannerion, Paraelops and Megalops are known[18] | ||
| Epaelops | E. martinezi | Elopiformes | Related to the Jurassic Anaethalion[24] | ||
| Gonorynchiformes indet. | Unapplicable | Ostariophysi | One specimen reported in the 1990s, but has not been studied since[23] | ||
| Lycoptera? | cf. L. sp | Lycopteridae | Only osteoglossiform fossil from Cretaceous Mexico[18] | ||
| Macrosemiocotzus | M. americanus | Macrosemiidae | Similar to Macrosemius, but differs in a divided dorsal fin[25] | ||
| Michin | M. csernai | Pachyrhizodontidae | Likely the most basal pachyrhizodontid[26] | ||
| Neoproscinetes | N. sp[18] | Pycnodontidae | Related to Proscinetes | ||
| Notagogus | N. novomundi | Macrosemiidae | Closest to Notagogus helenae[27] | ||
| Nusaviichthys | N. nerivelai | Pachyrhizodontoidei | Formerly misidentified as Notelops fossils[28] | ||
| Pachyamia | P. mexicana | Vidalamiinae | Also known from the Middle East[29] | ||
| Paraclupea | P. seilacheri | Ellimmichthyiformes | First fossil of the genus outside of China[30] | ||
| Ranulfoichthys | R. dorsonudus | Clupeomorpha | Somewhat resembles Ellimmichthyiformes, but lacks their dorsal scutes, therefore it is likely a basal clupeomorph[31] | ||
| Quetzalichthys | Q. perilliatae | Ionoscopiformes (Halecomorphi) | Likely closest to Oshunia[32] | ||
| Tahnaichthys | T. magnuserrata | Pycnodontidae | Bears two humps in front of its dorsal fin, a novel trait in pycnodonts[33] | ||
| Teoichthys | T. kallistos, T. brevipina[34] | Ophiopsidae (Halecomorphi) | Name of the type species (Teoichthys kallistos) translates to "God's most beautiful fish", in reference to the exquisite preservation[35] | ||
| Tepexichthys | T. aranguthyorum | Pycnodontidae | Likely fed on coral, as shown by gut contents and the large amount of wear on its teeth[36] | ||
| Tlalocbatos | T. applegatei | Rhinopristiformes | Only chondrichthyan known from Tlayúa[37] | ||
| Tlayuamichin | T. iztli | Semionotiformes | Specific name translates to "obsidian", after the colour of the scales[38] | ||
| Unamichthys | U. espinosai | Ichthyodectiformes | Discovered alongside two other currently undescribed ichthyodectiforms[39] | ||
| Yabrudichthys? | cf. Y. sp[18] | Aulopiformes | Likely an enchodontid, mainly known from the Ein Yabrud site (hence its generic name) | ||
Arthropods
| Arthropods | |||||
|---|---|---|---|---|---|
| Genus | Species | Higher taxon | Notes | Images | |
| Archaeoniscus | A. aranguthyorum | Sphaeromatidea? | Bears an unusual axial pouch unlike all extant isopods, may have been a fish ectoparasite or scavenger like modern cymothoids[40] | ||
| Atocatle | A. ranulfoi | Mesothelae? | Indeterminate family due to poor preservation, likely within Mesothelae due to its distinct abdominal segments,[40] but more recently its affinity as a spider is questioned[41] | ||
| Ixtahua | I. benjamini | Anisoptera? | Only known from a nymph, matches dragonfly nymphs in shape[40] | ||
| Protaegla | P. miniscula | Aeglidae | Earliest aeglid fossil known[40] | ||
| Tepexicarcinus | T. tlayuaensis | Tepexicarcinidae (basal Eubrachyura) | Formerly assigned questionably to Homolidae due to an absence of clear carapace regions,[40] but then separated into its own family as a basal eubrachyuran[42] | ||
| Tipulidae indet. | Unapplicable | Tipuloidea | Only known from a wing pair[40] | ||
Echinoderms
| Arthropods | |||||
|---|---|---|---|---|---|
| Genus | Species | Higher taxon | Notes | Images | |
| Astropecten | A. sp | Astropectinidae | Known from juvenile fossils preserving both dorsal and ventral sides[43] | ||
| Echinaster | E. sp | Echinasteridae | Only known from a fossil in dorsal view[43] | ||
| Ophiactis | O. applegatei | Ophiactidae | One of the few articulated ophiuroids from the Early Cretaceous[44] | ||
| Ophidiaster | O. sp | Ophidiasteridae | One of the few starfish from this formation which is not known from juvenile specimens[43] | ||
| Paleopentacta | P. alencasterae | Cucumariidae | Likely an infaunal suspsension feeder based on extant relatives[45] | ||
| Parapsolus | P. tlayuensis | Psolidae | Likely a suspension-feeder attached to hard substrates based on extant psolids[45] | ||
| Plutonaster | P. sp | Astropectinidae | Known from a juvenile specimen[43] | ||
| Tamaria | T. sp | Ophidiasteridae | Known from a juvenile[43] | ||
Mollusks
- Inoceramus sp.
- Pectinidae indet.
- Osteridae indet.
- Gastropoda indet.
- Neohibolites minimus obtusus
- Neohibolites minimus pinguis
- Neohibolites minimus claviformis
- Neohibolites praeultimus
- Mesohibolites semicanaliculatus
- Martoniceras sp.
- Hysteroceras sp.
- Anisoceras sp.
Other invertebrates
Plants
- cf. Araucaria sp.
- cf. Frenolopsis
- Brachyphyllum sp.
- Podozamites sp.
- Zamites sp.
- Phaeophyceae




















