Tlayúa Formation
PeriodCretaceous
PrilithologyLimestone
OtherlithologyMudstone
NamedforTlayúa Quarry
RegionPuebla
CountryMexico
Coordinates19.1°N 98.2°W
Paleocoordinates17.1°N 61.6°W
SubunitsLower, Middle and Upper Members
UnderliesUnconformity with Eocene-Oligocene Pie de Vaca Formation
OverliesOrizaba Formation
ThicknessLower: 50 m Middle: 35 m Upper: 40 m

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.

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

GenusSpeciesMaterialNotes
Huehuecuetzpalli[14]H. mixtecusNear-complete specimens of an adult and a juvenileA primitive lizard
Pamizinsaurus[15]P. tlayuaensisA single, crushed skull of a juvenileAn osteoderm-covered sphenodontian
Ankylosphenodon[16]A. pachyostosusFront half of a partial skeletonAn aquatic sphenodontian
Tepexisaurus[17]T. tepexiiNear-complete skeleton, minus the tailA basal scincomorph

Fish

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

Fish
GenusSpeciesHigher taxonNotesImages
Amblysemius?cf. A. spCaturidaeOnly non-amiid amiiform from Tlayúa[18]
AraripichthysA. weberiTeleosteiPossibly related to Late Cretaceous genera from North America?[19]
ArmigatusA. felixi, A. carrhenoaeEllimmichthyiformesFirst 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.InapplicableTeleosteiUndescribed species of Vinctifer and Belonostomus have been recorded[18]
AxelrodichthysA. cf. A. araripensisMawsoniidaeOnly known specimen was lost before description[18]
Bananogmius?cf. B. spTselfatiiformesOne of the few Mexican members of the clade other than Tselfatia[18]
CipactlichthysC. scutatusHalecomorphiBears large plate-like scutes along its midline[22]
EllimmichthysE. sp[23]EllimmichthyiformesType genus of its order
Elopomorpha spp.UnapplicableTeleosteiPossible species of Brannerion, Paraelops and Megalops are known[18]
EpaelopsE. martineziElopiformesRelated to the Jurassic Anaethalion[24]
Gonorynchiformes indet.UnapplicableOstariophysiOne specimen reported in the 1990s, but has not been studied since[23]
Lycoptera?cf. L. spLycopteridaeOnly osteoglossiform fossil from Cretaceous Mexico[18]
MacrosemiocotzusM. americanusMacrosemiidaeSimilar to Macrosemius, but differs in a divided dorsal fin[25]
MichinM. csernaiPachyrhizodontidaeLikely the most basal pachyrhizodontid[26]
NeoproscinetesN. sp[18]PycnodontidaeRelated to Proscinetes
NotagogusN. novomundiMacrosemiidaeClosest to Notagogus helenae[27]
NusaviichthysN. nerivelaiPachyrhizodontoideiFormerly misidentified as Notelops fossils[28]
PachyamiaP. mexicanaVidalamiinaeAlso known from the Middle East[29]
ParaclupeaP. seilacheriEllimmichthyiformesFirst fossil of the genus outside of China[30]
RanulfoichthysR. dorsonudusClupeomorphaSomewhat resembles Ellimmichthyiformes, but lacks their dorsal scutes, therefore it is likely a basal clupeomorph[31]
QuetzalichthysQ. perilliataeIonoscopiformes (Halecomorphi)Likely closest to Oshunia[32]
TahnaichthysT. magnuserrataPycnodontidaeBears two humps in front of its dorsal fin, a novel trait in pycnodonts[33]
TeoichthysT. 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]
TepexichthysT. aranguthyorumPycnodontidaeLikely fed on coral, as shown by gut contents and the large amount of wear on its teeth[36]
TlalocbatosT. applegateiRhinopristiformesOnly chondrichthyan known from Tlayúa[37]
TlayuamichinT. iztliSemionotiformesSpecific name translates to "obsidian", after the colour of the scales[38]
UnamichthysU. espinosaiIchthyodectiformesDiscovered alongside two other currently undescribed ichthyodectiforms[39]
Yabrudichthys?cf. Y. sp[18]AulopiformesLikely an enchodontid, mainly known from the Ein Yabrud site (hence its generic name)

Arthropods

Arthropods
GenusSpeciesHigher taxonNotesImages
ArchaeoniscusA. aranguthyorumSphaeromatidea?Bears an unusual axial pouch unlike all extant isopods, may have been a fish ectoparasite or scavenger like modern cymothoids[40]
AtocatleA. ranulfoiMesothelae?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]
IxtahuaI. benjaminiAnisoptera?Only known from a nymph, matches dragonfly nymphs in shape[40]
ProtaeglaP. minisculaAeglidaeEarliest aeglid fossil known[40]
TepexicarcinusT. tlayuaensisTepexicarcinidae (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.UnapplicableTipuloideaOnly known from a wing pair[40]

Echinoderms

Arthropods
GenusSpeciesHigher taxonNotesImages
AstropectenA. spAstropectinidaeKnown from juvenile fossils preserving both dorsal and ventral sides[43]
EchinasterE. spEchinasteridaeOnly known from a fossil in dorsal view[43]
OphiactisO. applegateiOphiactidaeOne of the few articulated ophiuroids from the Early Cretaceous[44]
OphidiasterO. spOphidiasteridaeOne of the few starfish from this formation which is not known from juvenile specimens[43]
PaleopentactaP. alencasteraeCucumariidaeLikely an infaunal suspsension feeder based on extant relatives[45]
ParapsolusP. tlayuensisPsolidaeLikely a suspension-feeder attached to hard substrates based on extant psolids[45]
PlutonasterP. spAstropectinidaeKnown from a juvenile specimen[43]
TamariaT. spOphidiasteridaeKnown from a juvenile[43]

Mollusks

Other invertebrates

Plants

References

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Further reading

  • L. Martin-Medrano and P. Garcia-Barrera. 2006. Fossil Ophiuroids of Mexico. In F. J. Vega, T. G. Nybor, M. D. C. Perrillat, M. Montellano-Ballesteros, S. R. S. Cevallos-Ferriz, S. A. Quiroz-Barroso (eds.), Topics in Geobiology 24:115-131