Tlayúa Formation

Geologic formation in Mexico From Wikipedia, the free encyclopedia

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.

Sub-unitsLower, Middle and Upper Members
OverliesOrizaba Formation
Quick facts Type, Sub-units ...
Tlayúa Formation
Stratigraphic range: Albian–Cenomanian
Cipactlichthys scutatus, one of the fossil fish from Tlayúa Formation
TypeGeological formation
Sub-unitsLower, Middle and Upper Members
UnderliesUnconformity with Eocene-Oligocene Pie de Vaca Formation
OverliesOrizaba Formation
ThicknessLower: 50 m Middle: 35 m Upper: 40 m
Lithology
PrimaryLimestone
OtherMudstone
Location
Coordinates19.1°N 98.2°W / 19.1; -98.2
Approximate paleocoordinates17.1°N 61.6°W / 17.1; -61.6
RegionPuebla
CountryMexico
Type section
Named forTlayúa Quarry
Tlayúa Formation is located in Mexico
Tlayúa Formation
Tlayúa Formation (Mexico)
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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

Undescribed turtle, exhibited in Tepexi Museum, Tepexi de Rodríguez

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

More information Genus, Species ...
GenusSpeciesMaterialNotes
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
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Fish

Mainly after González-Rodríguez (2016)[18] and Applegate et al. (2006)[3]

More information Fish, Genus ...
Fish
Genus Species Higher taxon Notes Images
Amblysemius? cf. A. sp Caturidae Only non-amiid amiiform from Tlayúa[18]
Fossil of Amblysemius from Solnhofen
Araripichthys A. weberi Teleostei Possibly related to Late Cretaceous genera from North America?[19]
Fossil of A. castilhoi
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]
Fossil of A. brevissimus from Lebanon
Aspidorhynchidae spp. Inapplicable Teleostei Undescribed species of Vinctifer and Belonostomus have been recorded[18]
Fossil of Vinctifer comptoni
Axelrodichthys A. cf. A. araripensis Mawsoniidae Only known specimen was lost before description[18]
A. araripensis fossil from Brazil
Bananogmius? cf. B. sp Tselfatiiformes One of the few Mexican members of the clade other than Tselfatia[18]
Reconstruction of B. aratus
Cipactlichthys C. scutatus Halecomorphi Bears large plate-like scutes along its midline[22]
C. scutatus holotype
Ellimmichthys E. sp[23] Ellimmichthyiformes Type genus of its order
Illustration of E. goodi
Elopomorpha spp. Unapplicable Teleostei Possible species of Brannerion, Paraelops and Megalops are known[18]
The extant Atlantic tarpon, a species in the genus Megalops
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]
The extant milkfish, a modern gonorynchiform
Lycoptera? cf. L. sp Lycopteridae Only osteoglossiform fossil from Cretaceous Mexico[18]
L. davidii reconstruction
Macrosemiocotzus M. americanus Macrosemiidae Similar to Macrosemius, but differs in a divided dorsal fin[25]
M. americanus reconstruction
Michin M. csernai Pachyrhizodontidae Likely the most basal pachyrhizodontid[26]
Neoproscinetes N. sp[18] Pycnodontidae Related to Proscinetes
Fossil of N. penalvai from the Santana Group
Notagogus N. novomundi Macrosemiidae Closest to Notagogus helenae[27]
Reconstruction of N. denticulatus
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]
Fossil of Q. perrilliatae under UV light
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]
Fossil of T. kallistos under UV light
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)
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Arthropods

More information Arthropods, Genus ...
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]
Speculative life restoration of Archaeoniscus coreaensis
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]
An Aegla individual of unknown species from Argentina
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]
The extant tipulid Tipula paludosa
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Echinoderms

More information Arthropods, Genus ...
Arthropods
Genus Species Higher taxon Notes Images
Astropecten A. sp Astropectinidae Known from juvenile fossils preserving both dorsal and ventral sides[43]
Specimen of the extant A. duplicatus
Echinaster E. sp Echinasteridae Only known from a fossil in dorsal view[43]
An Echinaster sepositus found in Arrábida National Park, Portugal
Ophiactis O. applegatei Ophiactidae One of the few articulated ophiuroids from the Early Cretaceous[44]
An extant Ophiactis savignyi from Mexico
Ophidiaster O. sp Ophidiasteridae One of the few starfish from this formation which is not known from juvenile specimens[43]
An Ophidiaster ophidianus found in Cabo de Palos, Spain
Paleopentacta P. alencasterae Cucumariidae Likely an infaunal suspsension feeder based on extant relatives[45]
The extant cucumariid Pentacta lutea
Parapsolus P. tlayuensis Psolidae Likely a suspension-feeder attached to hard substrates based on extant psolids[45]
The extant psolid Psolus phantapus
Plutonaster P. sp Astropectinidae Known from a juvenile specimen[43]
A Plutonaster observed on Kelvin Seamount
Tamaria T. sp Ophidiasteridae Known from a juvenile[43]
A Tamaria observed near the Mariana Islands
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Mollusks

Other invertebrates

Plants

References

Further reading

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