Paleobiota of the Chinle Formation

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The Chinle Formation is an extensive geological unit in the southwestern United States, preserving a very diverse fauna of Late Triassic (primarily Norian-age) animals and plants. This is a list of fossilized organisms recovered from the formation.

Contents

Amniotes

Archosauromorphs

Crurotarsans

Other Archosauromorphs

Non-crurotarsan Archosauromorphs of the Chinle Formation
GenusSpeciesStateMemberAbundanceNotesImages

Crosbysaurus [1]

C. harrisae [1]

  • Arizona
  • Utah [1]

An archosauriform represented only by teeth. [1] It is treated as indeterminate archosauriform remains by Irmis in 2005. [1] It was originally thought to be an ornithischian dinosaur.

Crosbysaurus Crosbysaurus hypothetical.png
Crosbysaurus
Doswellia Doswellia kaltenbachi life restoration.png
Doswellia
Trilophosaurus Trilophosaurus NT small.jpg
Trilophosaurus
Vancleavea Vancleavea.jpg
Vancleavea
Doswellia [2] cf. D. kaltenbachi
  • Arizona
Osteoderms, vertebrae, rib and hip fragments.A doswelliid archosauriform.
Puercosuchus [3] P. traverorum
  • Arizona
  • Blue Mesa

Two monodominant bonebeds.

A carnivorous azendohsaurid archosauromorph.

Rugarhynchos [4] R. sixmilensis
  • New Mexico
  • Bluewater Creek
Skull and postcranial fragments.A doswelliid archosauriform. Originally described as a species of Doswellia , [5] but subsequently transferred to a separate genus.
Syntomiprosopus [6] S. sucherorum
  • Arizona

Two to four individuals from a single quarry. [6]

A short-faced archosauriform, possibly an unusual early-diverging crocodylomorph. Appears convergent with some Late Cretaceous notosuchians. [6]

Tanystropheidae [7] Indeterminate
  • New Mexico
  • Petrified Forest
VertebraeModerately-sized tanystropheid vertebrae from the Hayden Quarry, likely representing a new taxon closely related to Langobardisaurus and Tanytrachelos . [7]

Tanytrachelos [8]

Indeterminate [8] / T. ahynis [7]

  • New Mexico
  • Arizona [8]
  • Petrified Forest
  • Mesa Redondo [8]

Cervical rib, [8] calcaneum, etc.

A small tanystropheid represented by several hundred fossil specimens.

Tecovasaurus [9]

T. murryi [9]

  • Mesa Redondo [9]

An unknown amniote represented by scattered teeth formerly believed to be from an ornithischian dinosaur. [9] Later discoveries of similar teeth in pseudosuchians meant that these could no longer be regarded as anything more specific than some kind of archosauriform. [9]

Trilophosaurus [10]

T. buettneri [11]

T. dornorum [12]

T. jacobsi [13]

T. phasmalophos [14]

  • Arizona
  • Sonsela

Vancleavea [15]

V. campi [15]

  • Arizona [15]
  • New Mexico

A strange aquatic carnivorous archosauriform, represented by both articulated skeletons and scattered elements like osteoderms and vertebrae. [15]

Other amniotes

Miscellaneous amniotes of the Chinle Formation
GenusSpeciesStateMemberAbundanceNotesImages

Acallosuchus [17]

A. rectori [17]

Known only from a partial skull. [17]

A strange neodiapsid whose bones were heavily ornamented "with subtriangular knobs... running the length of the bones." Even these ornamentations were ornamented "with additional grooves." It is too bizarre to be currently classified as anything more than a probable diapsid. [17]

Drepanosaurus Drepanosaurus BW.jpg
Drepanosaurus
Placerias Placerias1DB.jpg
Placerias
Ancistronychus [18] A. paradoxus
  • Arizona
  • Sonsela
Manual unguals (hand claws).A drepanosaur related to Drepanosaurus.
Avicranium [19] A. renestoi
  • New Mexico
  • 'Siltstone'
Skull and neck vertebrae.A drepanosaur with a toothless skull and a flexible neck owing to the heterocoelous (saddle-shaped) articular surfaces of the vertebral centrae. The neural spines are anteroposteriorly short and strongly anterodorsally inclined. These features closely resemble those of Drepanosaurus .

Colognathus [20]

C. obscurus [20]

Known only from a jaw fragment and some isolated teeth. [20]

Originally believed to be a fish, Colognathus was a strange amniote with distinctive fluted teeth. [20]

Dolabrosaurus D. aquatilis
  • New Mexico
  • Petrified Forest
Articulated vertebral and limb material.A drepanosaur.
Drepanosaurus [21] D. unguicaudatus
  • New Mexico
  • Petrified Forest
A drepanosaur.

Kataigidodon [22]

K. venetus

  • Arizona
  • Blue Mesa
Partial dentaries.

A non-mammalian eucynodont.

Kraterokheirodon [23]

K. colberti [23]

  • Petrified Forest [23]
  • Blue Mesa or Mesa Redondo [23]

Known only from two teeth. [23]

A possible cynodont. Although they share some similarities with cynodont teeth, the teeth of Kraterokheirodon are very distinctive and can't be confidently referred to a known amniote group. [23]

Palacrodon [24] Indeterminate
  • Arizona
  • Blue Mesa
Jaw fragments.A diapsid reptile of uncertain phylogenetic placement with unusual broadened teeth. More complete fossils of this genus from the Fremouw Formation of Antarctica suggest that it was an arboreal saurian. [25]

Placerias [26]

P. hesternus [26]

Known from several hundred remains, but very rare outside of the highly concentrated Placerias Quarry. [26]

A placeriine stahleckeriid dicynodont.
Skybalonyx [27] S. skapter
  • Arizona
  • Blue Mesa
Manual unguals (hand claws).A drepanosaur which likely had a burrowing lifestyle.

Uatchitodon [28]

U. schneideri [29]

Known in Chinle from only a single tooth. The presence of venom channels is consistent with other known Uatchitodon specimens, although the Chinle specimen's channels are unique in being "completely enclosed under the surface of the crown." [30]

A reptile of unknown affinities, probably a carnivorous archosauromorph with venomous capabilities.
Whitakersaurus [31] W. bermani
  • New Mexico
  • "Siltstone"
A rhynchocephalian found at Ghost Ranch.
Indeterminate procolophonid [32] Indeterminate
  • Utah

Amphibians

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Amphibians of the Chinle Formation
GenusSpeciesStateMemberAbundanceNotesImages

Apachesaurus [33]

A. gregorii [33]

Common in the Owl Rock and Petrified forest members. [33] Blue Mesa remains are fragmentary. [33]

A metoposaurid temnospondyl which is a junior synonym of Anaschisma

Anaschisma Koskinonodon perfectus.jpg
Anaschisma
Funcusvermis Funcusvermis life restoration.jpg
Funcusvermis

Anaschisma [34] [35]

A. browni [36] [35]

A. browni is "possibly the most common tetrapod fossil in the lower Chinle", although its presence in the upper Chinle is "unclear". [36]

A metoposaurid temnospondyl. Koskinonodon was erected for the species "Buettneria" perfecta when it was discovered that the latter genus was preoccupied. Gee et al., 2017 then synonymised it with Anaschisma. [34] [35]

Chinlestegophis [37]

C. jenkinsi

  • Colorado

A temnospondyl in the group Stereospondyli, related to Rileymillerus from the Dockum Group of Texas. Possibly a stem-caecilian according to one analysis, [37] though others have disputed this finding

Funcusvermis [38] F. gilmorei
  • Arizona
  • Blue Mesa
Numerous jaw fragments, as well as a referred maxillopalatine, vertebra, and femurA stem-caecilian

Salientia indet. [39]

Indeterminate

  • Arizona
  • Sonsela Member
  • Blue Mesa Member

Five bones: four ilia and a partial maxilla.

A stem-group frog. Might be more closely related to crown-group frogs (anurans) than to Early Triassic taxa Triadobatrachus and Czatkobatrachus .

Cartilaginous fish

Chondrichthyans of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages

Acrodus [40]

Indeterminate [40]

Only a single tooth is known. [40]

A hybodontiform shark.
Xenacanthus Xenacanth.png
Xenacanthus

Lonchidion [42]

L. humblei [42]

A hybodontiform shark. Lonchidion remains are common throughout the Carnian microvertebrate sites of the American southwest. [42]

Palaeoxyris P. humblei [43]
  • Arizona
  • Blue Mesa
Several specimensAn egg capsule of a freshwater hybodont shark.

Phoebodus [44]

Indeterminate [44]

Only a single specimen has been recovered from the formation. [44]

Reticulodus [45]

R. synergus [45]

The crown of its tooth bears a "reticulating ornamentation on [its] occlusal surface[.]" [45] Reticulodus remains are common throughout the Norian microvertebrate sites of the American southwest. [45]

Xenacanthus [46]

X. moorei [46]

Common in the lower Chinle Formation's microvertebrate localities. [46]

A xenacanthiform shark.

Lobe-finned fish

Coelacanths

Actinistians (coelacanths) of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages

Chinlea [47]

Indeterminate [48]

An actinisitan (coelacanth).
Chinlea Chinlea BW.jpg
Chinlea

Lungfish

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Dipnoans (lungfish) of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotes

Arganodus [49]

A. dorotheae [49]

Indeterminate [49]

Arganodus toothplates are the most common fossil in the formation from a non-tetrapod. [49] They are evenly distributed across strata, although some individual localities have very high concentrations. [49]

Most Chinlean Arganodus fossils are isolated tooth plates. [49]

Ceratodus [49]

C. dorotheae [49]

Named by Case in 1921, in the 1980s it was referred to Arganodus. [49]

Ray-finned fish

Actinopterygians (ray-finned fish) of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages

Australosomus [50]

Indeterminate [51]

Known only from two vertebrae. [51]

Australosomus Australosomus merlei.JPG
Australosomus
Saurichthys Saurichthys (Mensch & Natur-Museum, Munchen).jpg
Saurichthys

Cionichthys [52]

C. dunklei

  • Colorado
  • Utah

A member of Redfieldiiformes.

Hemicalypterus

H. weiri

  • Utah
  • Church Rock Member

A member of Dapediiformes. [53]

Lasalichthys [52] [54]

L. hillsi [52]

A member of Redfieldiiformes.

Indeterminate [55]

Represented by isolated scales. [55]

Lophionotus [56]

L. sanjuanensis [56]

  • Utah
  • Church Rock Member [56]

A member of Semionotiformes.

L. chinleana [57]

  • Utah
  • Church Rock Member

A member of Semionotiformes.

Saurichthys [58]

Indeterminate

  • Arizona
  • Upper Blue Mesa Member

A member of Saurichthyiformes.

Synorichthys [52]

S. stewarti

  • Colorado
  • Utah

A member of Redfieldiiformes.

Tanaocrossus [52]

T. kalliokoskii

  • Colorado

An enigmatic actinopterygian. [53]

Turseodus [52] [59]

T. dolorensis [52]

A member of Palaeonisciformes. [52]

Indeterminate [60]

Common. [60]

Isolated scales from Chinle microvertebrate sites commonly have Turseodus-like ridges, however that feature is not unique to Turseodus and in 2005 Irmis advised researchers to regard them as indeterminate palaeoniscid remains. [60]

Plants

The Chinle Formation has a diverse flora of plant megafossils, though they are concentrated in only a few sites with suitable conditions. One of the most diverse floral communities is found near Fort Wingate, New Mexico. Paleobotanists have traditionally placed the Fort Wingate plant beds into the Monitor Butte Member, though more recently they are placed within the Bluewater Creek Formation, a subunit of the Chinle Formation first defined in 1989. [61] Some Fort Wingate plant fossils belong to the "Lake Ciniza beds", a localized patch of grey mudstone corresponding to an ancient lake. [62]

Another productive areas for plant fossils is Petrified Forest National Park in Arizona. Though petrified wood could be found through the entire stratigraphy of the park, most other plant fossils are exclusive to greenish mudstone layers adjacent to the Newspaper Rock sandstone bed in the Blue Mesa Member (formerly known as the "Lower Petrified Forest").

Conifers are the most common and diverse plants, including petrified wood and leafy branches from massive trees ( Araucarioxylon , Pagiophyllum ) as well as smaller shrubby forms ( Pelourdea ). Cycad and bennettitalean leaves and other remains make up a significant portion of the flora ( Zamites , Nilssoniopteris , Williamsonia , etc.). Ferns ( Cladophlebis , Phlebopteris , Clathropteris , Cynepteris, etc.) are abundant, with a range of growth habits including low shrubs, tree ferns, and palm-like fronds comparable to their modern relatives. Sphenophytes (horsetails: Neocalamites , Equistetites , Schizoneura , etc.) have low diversity but high abundance, and the largest Neocalamites fossils in the Chinle Formation could reach up to 6 meters (20 feet) in height. "Seed ferns" ( Chilbinia , Marcouia ?) ginkgophytes ( Baiera ), and small lycopods ( Chinlea , Selaginella ) were present but uncommon. The flora is rounded out by unusual low-growing gymnosperms such as Sanmiguelia (an angiosperm-like shrub), Dechellyia , and Dinophyton (possible relatives of Gnetales). [63] [64]

The floral composition of the Chinle Formation (and other parts of Late Triassic North America) seem to shift with changes in climate over time. The lowest parts of the Chinle, such as the Shinarump Conglomerate, are dominated by the bennettitalean Eoginkgoites alongside the first occurrence of other persistent plants such as Phlebopteris , Equisetites , and most common conifer species. Subsequent subunits (such as the Blue Mesa Member, Monitor Butte Member, and Bluewater Creek Formation) are much more diverse, with a wide array of humidity-adapted plants making up the typical Chinle flora. This second floral zone is characterized by Dinophyton , a common but enigmatic shrubby gymnosperm. Plant fossils are rare in the upper part of the Chinle Formation, which was presumably much drier than the lower part. In these later layers, by far the most common plant fossils belong to Sanmiguelia (an endemic of southwestern North America) alongside conifers and horsetails. [65] [66]

Gymnosperms

Gymnosperms of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages
Araucariorhiza [67] A. joaeUncommonRoots of conifers similar to modern Araucariaceae. Possibly from the same plant as Araucarioxylon arizonicum .

Araucarioxylon [68]

A. arizonicum,

A. sp. [69]

AbundantPetrified trunks of large conifers possibly related to modern Araucariaceae. [72] State fossil of Arizona.
Araucarioxylon arizonicum Araucarioxylon arizonicum (petrified wood) - National Museum of Natural History, United States - DSC08540.JPG
Araucarioxylon arizonicum
Araucarites A. rudicula [73]
  • Arizona
  • New Mexico
  • Blue Mesa
  • Monitor Butte
Very rareLarge female conifer cones similar to those of araucariacean conifers.
Aricycas [74] A. paulae
  • Arizona
  • Blue Mesa ( = "Lower Petrified Forest")
Moderately common Pinnate cycad leaves
Baiera B. arizonica
  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
  • Bluewater Creek ( = "lower red member", formerly Monitor Butte) [75] [71]
Uncommon Ginkgophyte leaves
Brachyphyllum B. sp,

B. hegewaldia [76]

UncommonConifer leaves and shoots
Carpolithus C. chinleana
  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
RareSeeds of uncertain affinities
Cephalotaxopsis C. sp.Conifer foliage
Charmorgia C. dijolli
  • "Petrified Forest" sensu lato [63]
RareShort cycad stems
Chilbinia [77] C. lichii
  • Arizona
  • Shinarump
RareAn archaic seed fern with seeds and leaves more similar to Carboniferous-Permian seed ferns than to Triassic forms.
Creberanthus C. bealeii [73]
  • Arizona
Very rarePollen-bearing cones similar to those of some extinct "pteridosperms" (seed ferns). Associated with Alisporites opii, a common palynomorph.
Dadoxylon D. chaneyi
  • "Petrified Forest" sensu lato [63]
Very rarePossible cordaitalean conifer wood.
Dechellyia [78] D. gormaniiUncommonAn enigmatic gymnosperm with narrow pinnate leaves, "clasping" leaf-like sporophylls, and winged seeds. Some leaves are affected by galls, similar to those formed by eriophyid mites in modern plants. [79] [80]
Dinophyton D. spinosus [81]
  • Blue Mesa (= "Lower Petrified Forest") [81] [63] [65]
  • Monitor Butte [81]
  • Bluewater Creek ("Ciniza Lake beds", formerly Monitor Butte) [62] [71]
CommonAn unusual gymnosperm combining needle-covered shoots with seed-bearing structures having the form of "pinwheel"-like clusters of tubular needles. Possibly related to Gnetales.
Elatocladus E. puercoensis [80]
  • Arizona
  • Blue Mesa
UncommonLeaf-bearing conifer shoots
Eoginkgoites E. sp.,

E. davidsonii [82]

Common within its small stratigraphic rangeA bennettitalean with palm-shaped fronds similar to some ginkgo species.
Ginkgoites G. sp.RareA ginkgophyte
Lindleycladus L. arizonicus [80]
  • Arizona
  • Blue Mesa
UncommonConifer shoots bearing Podozamites leaves. Formerly known as Podozamites arizonicus.
Lyssoxylon L. grigsbyi
  • "Petrified Forest" sensu lato [63]
  • Bluewater Creek (formerly Monitor Butte) [71]
Rare Cycad trunks
Marcouia M. neuropteroides
  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
  • Bluewater Creek (formerly Monitor Butte) [71]
  • Monitor Butte [79]
UncommonFern-like gymnosperm leaves of uncertain affinities. Some leaves are affected by feeding traces including crescent-shaped marginal incisions and oval-shaped holes. These were probably produced by beetles or orthopterans (grasshoppers and kin). [79]
Masculostrobus M. clathratus [78]
  • Arizona
  • Monitor Butte
Locally commonA pollen-bearing cone associated with lattice-shaped Equisetosporites chinleana pollen.
Nilssoniopteris N. ciniza [62] [71]
  • "Petrified Forest" sensu lato [63]
  • Bluewater Creek ("Ciniza Lake beds", formerly Monitor Butte) [75] [62] [71]
  • Shinarump [63]
UncommonLarge smooth-edged bennettitalean leaves, some of which were originally identified as Macrotaeniopteris magnifola.
Otozamites O. macombii
  • Agua Zarca Sandstone [70]
Uncommon Bennettitalean leaves
Pagiophyllum P. sp.,

P. duttonia, [62]

P. navajoensis, [62]

P. readiana, [62]

P. zuniana, [62]

P. simpsonii [83]

  • "Middle Dolores" [69]
  • "Petrified Forest" sensu lato [63]
  • Sonsela [83] [65]
  • Bluewater Creek ("Ciniza Lake beds", formerly Monitor Butte) [62] [71]
  • Agua Zarca Sandstone [70]
Locally very commonConifer leaves
Palissya P. sp.,

P. diffusa,

P. sphenolepis

  • Monitor Butte [63]
  • Agua Zarca Sandstone [63]
  • Shinarump [63]
UncommonConifer leaves and shoots
Pelourdea P. poleoensisCommonA shrubby conifer with strap-like leaves arranged around a single narrow stem.
Podozamites P. sp.,

P. emmonsi,

P. lanceolatus

  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
  • Shinarump [63]
  • Temple Mountain [63]
UncommonConifer leafs and shoots
Pramelreuthia P. dubielli, [84] P. yazzi [84]
  • Arizona
  • New Mexico
  • Utah
  • Blue Mesa [65]
  • Monitor Butte
RareGymnosperm microsporophylls (pollen-bearing organs)
Pterophyllum P. sp.,

P. braunianum

Uncommon Bennettitalean leaves
Samaropsis S. sp.,

S. puerca

  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
UncommonSeeds of uncertain affinities
Sanmiguelia S. lewisiiCommonAn unusual palm-like shrub, controversially suggested to be a relative or predecessor of angiosperms (flowering plants).

Schilderia

S. adamanica

RarePetrified stems of a conifer or gnetalean [72]
Williamsonia W. nizhonii [87]
  • Bluewater Creek ( = "lower red member", formerly Monitor Butte) [75] [87] [71]
RareA bennettitalean "flower" (female cone)

Woodworthia

W. arizonica

Uncommon

Stems and petrified wood of a conifer related to A. arizonicum. [72] [88]

Zamites Z. sp.,

Z. occidentalis,

Z. powellii

Very common Bennettitalean leaves. Some leaves exhibit feeding traces, including sharp diagonal marginal traces and slot-like non-marginal traces. These traces were probably left by beetles. [79] Zamites powellii was formerly known as Otozamites powellii.

Ferns

Ferns of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages
Apachea A. arizonica
  • "Petrified Forest" [63]
Rare Dipteridacean fern leaves, possibly damaged specimens of Clathropteris walkeri. [91]
Cladophlebis C. daughertyi, [91] C. subfalcata,

C. yazzia, [76]

C. sp.

  • Blue Mesa (= "Lower Petrified Forest") [91] [76] [65]
  • Bluewater Creek (= "lower red member", formerly Monitor Butte) [75] [91] [71]
  • Monitor Butte [63]
  • Shinarump [63]
Very commonLarge sterile fern leaves of uncertain affinities
Clathropteris C. walkeri
  • Blue Mesa (= "Lower Petrified Forest") [91] [65]
  • Bluewater Creek (= "lower red member", formerly Monitor Butte) [75] [91] [71] [63]
Common Dipteridacean fern leaves
Cynepteris [91] C. sp.,

C. lasiophora [91]

  • Church Rock? [90]
  • Owl Rock? [90]
  • Blue Mesa (= "Lower Petrified Forest") [91] [79]
  • Bluewater Creek (= "lower red member", formerly Monitor Butte) [91] [71]
  • Monitor Butte [79]
Common Bipinnate fern leaves previously identified as Lonchopteris . Some leaves are affected by crescent-shaped marginal feeding traces, probably from beetles or orthopterans (grasshoppers and kin). [79]
Itopsidema [92] I. vancleavi
  • Arizona
  • Sonsela
UncommonStems of large osmundacean tree ferns. Some stems show evidence of being bored by oribatid mites. [93]
Phlebopteris P. smithii,

P. utensis

  • Blue Mesa (= "Lower Petrified Forest") [94] [65]
  • Bluewater Creek ( = "lower red member" / "Ciniza Lake beds", formerly Monitor Butte) [75] [91] [62] [71]
  • Shinarump [94]
Common Matoniacean fern leaves with a palmate structure
Sphenopteris S. arizonica
  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
UncommonSterile fern leaves of uncertain affinities. Some show evidence for marginal damage by insect feeding traces. [95]
Todites T. fragilis
  • Blue Mesa (= "Lower Petrified Forest") [91]
  • Bluewater Creek (="lower red member", formerly Monitor Butte) [75] [91] [71]
Uncommon Osmundacean fern leaves
Wingatea [91] W. plumosa
  • Blue Mesa (= "Lower Petrified Forest") [91] [65]
  • Bluewater Creek (="lower red member", formerly Monitor Butte) [91] [71]
Rare Gleicheniacean fern leaves previously named as a species of Coniopteris .

Other plants

Other plants of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages
Chinlea C. sp.,

C. campii

  • "Petrified Forest" sensu lato [63]
UncommonSmall lycopod stems similar to shrubby forms such as Pleuromeia . [96]
Equisetites E. sp.,

E. bradyi

  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
  • Bluewater Creek ("Ciniza Lake beds", formerly Monitor Butte) [62] [71]
  • Shinarump [63]
CommonA horsetail indistinguishable from modern Equisetum .
Equisetocalis [97] E. muirii
  • Arizona
  • Blue Mesa
Concentrated in a narrow stratigraphic range (the Newspaper Rock sandstone bed)Small three-dimensional horsetail stems preserved in pyrite nodules.
Isoetites I. circularis
  • "Petrified Forest" sensu lato [63]
Rare Quillwort shoots
Lycostrobus L. chinleana
  • Blue Mesa (= "Lower Petrified Forest") [63] [65]
RareHorsetail cones sometimes placed in the genus Equicalostrobus
Neocalamites N. sp.,

N. virginiensis

  • "Siltstone" [69]
  • Church Rock? [90]
  • Owl Rock? [90]
  • "Petrified Forest" sensu lato [63]
  • Bluewater Creek ( = "lower red member" / "Ciniza Lake beds", formerly Monitor Butte) [75] [62]
CommonStems and leaves of a giant sphenophyte (horsetail)
Schizoneura S. harrisii
  • Bluewater Creek (formerly Monitor Butte) [71]
UncommonStems and leaves of a large sphenophyte (horsetail) more typical of Southern Hemisphere plant assemblages.
Selaginella S. anasazia [78]
  • Arizona
  • Monitor Butte
UncommonA low-growing lycopsid similar to modern broad-leaved species of Selaginella, such as S. kraussiana

Arthropods

Arthropods of the Chinle Formation
GenusSpeciesStateStratigraphic positionAbundanceNotesImages
Enoplocytia E. porteri [99]
  • Arizona
  • Sonsela?
Single well-preserved fossilAn erymid crayfish

Paleoscolytus [100]

P. divergus

  • Arizona
  • Sonsela

A species of bark beetle, evidenced by trace fossils of tracks made on A. arizonicum specimens.

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<span class="mw-page-title-main">Petrified Forest National Park</span> National park in Arizona, United States

Petrified Forest National Park is an American national park in Navajo and Apache counties in northeastern Arizona. Named for its large deposits of petrified wood, the park covers about 346 square miles, encompassing semi-desert shrub steppe as well as highly eroded and colorful badlands. The park's headquarters is about 26 miles (42 km) east of Holbrook along Interstate 40 (I-40), which parallels the BNSF Railway's Southern Transcon, the Puerco River, and historic U.S. Route 66, all crossing the park roughly east–west. The site, the northern part of which extends into the Painted Desert, was declared a national monument in 1906 and a national park in 1962. The park received 644,922 recreational visitors in 2018.

<i>Revueltosaurus</i> Extinct genus of reptiles

Revueltosaurus is an extinct genus of suchian pseudosuchian from Late Triassic deposits of New Mexico, Arizona and North Carolina, United States. Many specimens, mostly teeth, have been assigned to Revueltosaurus over the years. Currently, three species are included in this genus, all of which were originally thought to represent monospecific genera of basal ornithischian dinosaurs. It was 1 meter long.

<i>Chindesaurus</i> Extinct genus of dinosaurs

Chindesaurus is an extinct genus of basal saurischian dinosaur from the Late Triassic of the southwestern United States. It is known from a single species, C. bryansmalli, based on a partial skeleton recovered from Petrified Forest National Park in Arizona. The original specimen was nicknamed "Gertie", and generated much publicity for the park upon its discovery in 1984 and airlift out of the park in 1985. Other fragmentary referred specimens have been found in Late Triassic sediments throughout Arizona, New Mexico, and Texas, but these may not belong to the genus. Chindesaurus was a bipedal carnivore, approximately as large as a wolf.

<span class="mw-page-title-main">Chinle Formation</span> Geological formation in the western US

The Chinle Formation is an Upper Triassic continental geological formation of fluvial, lacustrine, and palustrine to eolian deposits spread across the U.S. states of Nevada, Utah, northern Arizona, western New Mexico, and western Colorado. In New Mexico, it is often raised to the status of a geological group, the Chinle Group. Some authors have controversially considered the Chinle to be synonymous to the Dockum Group of eastern Colorado and New Mexico, western Texas, the Oklahoma panhandle, and southwestern Kansas. The Chinle Formation is part of the Colorado Plateau, Basin and Range, and the southern section of the Interior Plains. A probable separate depositional basin within the Chinle is found in northwestern Colorado and northeastern Utah. The southern portion of the Chinle reaches a maximum thickness of a little over 520 meters (1,710 ft). Typically, the Chinle rests unconformably on the Moenkopi Formation.

Spinosuchus is an extinct genus of trilophosaurid allokotosaur from the Late Triassic of Texas, southern United States. It has been assigned to a variety of groups over its history, from coelophysid dinosaur to pseudosuchian to uncertain theropod dinosaur and to Proterosuchidae. This uncertainty is not unusual, given that it was only known from a poorly preserved, wall-mounted, partial vertebral column of an animal that lived in a time of diverse, poorly known reptile groups. However, newly collected material and recent phylogenetic studies of early archosauromorphs suggest that it represents an advanced trilophosaurid very closely related to Trilophosaurus.

<i>Saurosuchus</i> Paracrocodylomorph reptile genus from Late Triassic period

Saurosuchus is an extinct genus of large loricatan pseudosuchian archosaurs that lived in South America during the Late Triassic period. It was a heavy, ground-dwelling, quadrupedal carnivore, likely being the apex predator in the Ischigualasto Formation.

<i>Acaenasuchus</i> Genus of reptiles

Acaenasuchus is an extinct genus of pseudosuchian, endemic to what would be presently be known as Arizona during the Late Triassic, specifically during the Carnian and Norian stages of the Triassic. Acaenasuchus had a stratigraphic range of approximately 11.5 million years. Acaenasuchus is further categorized as one of the type fauna that belong to the Adamanian LVF, based on the fauna of the Blue Mesa Member of the Chinle Petrified Forest Formation of Arizona, where Acaenasuchus was initially discovered.

<i>Trilophosaurus</i> Extinct genus of reptiles

Trilophosaurus is a lizard-like trilophosaurid allokotosaur known from the Late Triassic of North America. It was a herbivore up to 2.5 m long. It had a short, unusually heavily built skull, equipped with massive, broad flattened cheek teeth with sharp shearing surfaces for cutting up tough plant material. Teeth are absent from the premaxilla and front of the lower jaw, which in life were probably equipped with a horny beak.

<i>Dromomeron</i> Extinct genus of reptiles

Dromomeron is a genus of lagerpetid avemetatarsalian which lived around 220 to 211.9 ± 0.7 million years ago. The genus contains species known from Late Triassic-age rocks of the Southwestern United States and northwestern Argentina. It is described as most closely related to the earlier Lagerpeton of Argentina, but was found among remains of true dinosaurs like Chindesaurus, indicating that the first dinosaurs did not immediately replace related groups.

<i>Smilosuchus</i> Extinct genus of reptiles

Smilosuchus is an extinct genus of leptosuchomorph parasuchid from the Late Triassic of North America.

The Cooper Canyon Formation is a geological formation of Norian age in Texas and New Mexico. It is one of several formations encompassed by the Dockum Group.

<i>Leptosuchus</i> Extinct genus of reptiles

Leptosuchus is an extinct genus of leptosuchomorph phytosaur with a complex taxonomical history. Fossils have been found from the Dockum Group and lower Chinle Formation outcropping in Texas, New Mexico, and Arizona, USA, and date back to the Carnian stage of the Late Triassic.

<i>Machaeroprosopus</i> Extinct genus of reptiles

Machaeroprosopus is an extinct genus of mystriosuchin leptosuchomorph phytosaur from the Late Triassic of the southwestern United States. M. validus, once thought to be the type species of Machaeroprosopus, was named in 1916 on the basis of three complete skulls from Chinle Formation, Arizona. The skulls have been lost since the 1950s, and a line drawing in the original 1916 description is the only visual record of the specimen. Another species, M. andersoni, was named in 1922 from New Mexico, and the species M. adamanensis, M. gregorii, M. lithodendrorum, M. tenuis, and M. zunii were named in 1930. Most species have been reassigned to the genera Smilosuchus, Rutiodon, or Phytosaurus. Until recently, M. validus was considered to be the only species that has not been reassigned. Thus, Machaeroprosopus was considered to be a nomen dubium or "doubtful name" because of the lack of diagnostic specimens that can support its distinction from other phytosaur genera. However, a taxonomic revision of Machaeroprosopus, conducted by Parker et al. in 2013, revealed that UW 3807, the holotype of M. validus, is not the holotype of Machaeroprosopus, while the species Machaeroprosopus buceros, Machaeroprosopus being a replacement name, with a fixed type species, for Metarhinus, is the combinatio nova of the type species of the genu: Belodon buceros. Therefore, the name Pseudopalatus must be considered a junior synonym of Machaeroprosopus, and all species of the former must be reassigned to the latter. This revised taxonomy was already accepted in several studies, including Stocker and Butler (2013). Stocker and Butler (2013) also treated M. andersoni as a valid species, and not a junior synonym of Machaeroprosopus buceros as was previously suggested by Long and Murry (1995).

Parrishia is an extinct genus of sphenosuchian crocodylomorph known from the Late Triassic Chinle, Dockum, and Santa Rosa Formations in Arizona and New Mexico.

Uatchitodon is an extinct genus of Late Triassic reptile known only from isolated teeth. Based on the structure of the teeth, Uatchitodon was probably a carnivorous archosauromorph. Folded grooves on the teeth indicate that the animal was likely venomous, with the grooves being channels for salivary venom. The teeth are similar to those of living venomous squamates such as Heloderma and venomous snakes. Uatchitodon is the earliest known venomous reptile.

<span class="mw-page-title-main">Epipophyses</span> Bony projections of neck vertebrae in certain reptiles

Epipophyses are bony projections of the cervical vertebrae found in archosauromorphs, particularly dinosaurs. These paired processes sit above the postzygapophyses on the rear of the vertebral neural arch. Their morphology is variable and ranges from small, simple, hill-like elevations to large, complex, winglike projections. Epipophyses provided large attachment areas for several neck muscles; large epipophyses are therefore indicative of a strong neck musculature.

The Colorado City Formation is a Late Triassic geologic formation in the Dockum Group of Texas, United States. It has previously been known as the Iatan Member, Colorado City Member or 'Pre-Tecovas Horizon'.

<i>Anisodontosaurus</i> Extinct genus of reptiles

Anisodontosaurus is an extinct genus of trilophosaurid allokotosaur known from the Middle Triassic Moenkopi Formation of Arizona. The type species, A. greeri, was named and described by Samuel Paul Welles in 1947, and its taxonomic placement was largely unknown until the holotype was reassessed in 1988, when it was recovered as a lepidosauromorph or a trilophosaurid. The holotype, a jaw catalogued as UCMP V3922, was discovered in 1940 and was described seven years later. Apart from the type specimen, Anisodontosaurus is known from the referred specimen UCMP 37815, a right ilium.

Land vertebrate faunachrons (LVFs) are biochronological units used to correlate and date terrestrial sediments and fossils based on their tetrapod faunas. First formulated on a global scale by Spencer G. Lucas in 1998, LVFs are primarily used within the Triassic Period, though Lucas later designated LVFs for other periods as well. Eight worldwide LVFs are defined for the Triassic. The first two earliest Triassic LVFs, the Lootsbergian and Nonesian, are based on South African synapsids and faunal assemblage zones estimated to correspond to the Early Triassic. These are followed by the Perovkan and Berdyankian, based on temnospondyl amphibians and Russian assemblages estimated to be from the Middle Triassic. The youngest four Triassic LVFs, the Otischalkian, Adamanian, Revueltian, and Apachean, are based on aetosaur and phytosaur reptiles common in the Late Triassic of the southwestern United States.

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  69. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 Ash, Sidney R. (1987). "The Upper Triassic Red Bed Flora of the Colorado Plateau, Western United States". Journal of the Arizona-Nevada Academy of Science. 22 (1): 95–105. JSTOR   40024387.
  70. 1 2 3 4 5 6 7 8 9 10 Ash, Sidney R. (1974). "Upper Triassic plants of Canon del Cobre, New Mexico". New Mexico Geological Society Guidebook. 25: 179–184.
  71. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 Ash, Sidney R. (1989). "The upper Triassic Chinle flora of the Zuni Mountains, New Mexico" (PDF). New Mexico Geological Society. 40: 225–230. doi:10.56577/ffc-40.225. S2CID   251985942.
  72. 1 2 3 "Trees to Stone" (PDF). National Park Service. 2006. Archived (PDF) from the original on September 7, 2015. Retrieved October 3, 2010.
  73. 1 2 3 Axsmith, Brian J.; Ash, Sidney R. (2006). "Two rare fossil cones from the Upper Triassic Chinle Formation in Petrified Forest National Park, Arizona, and New Mexico". Museum of Northern Arizona Bulletin. 62: 82–94.
  74. Ash, Sidney R. (1991). "A New Pinnate Cycad Leaf from the Upper Triassic Chinle Formation of Arizona". Botanical Gazette. 152 (1): 123–131. doi:10.1086/337871. ISSN   0006-8071. S2CID   83627771.
  75. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 Ash, Sidney R. (1967). "The Chinle (Upper Triassic) megaflora of the Zuni Mountains, New Mexico" (PDF). New Mexico Geological Society Fall Field Conference Guidebook. 18: 125–131. doi:10.56577/ffc-18.125. S2CID   11630110.
  76. 1 2 3 4 5 6 Ash, Sidney R. (1973). "Two New Late Triassic Plants from the Petrified Forest of Arizona". Journal of Paleontology. 47 (1): 46–53. JSTOR   1302865.
  77. Ash, Sidney R. (2006). "Chilbinia Gen. Nov., an Archaic Seed Fern in the Late Triassic Chinle Formation of Arizona, USA". Palaeontology. 49 (2): 237–245. doi:10.1111/j.1475-4983.2006.00542.x. ISSN   0031-0239. S2CID   129438630.
  78. 1 2 3 4 5 6 Ash, Sidney R. (1972). "Late Triassic plants from the Chinle Formation in north-eastern Arizona" (PDF). Palaeontology. 15 (4): 598–618.
  79. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Ash, Sidney (1996). "Evidence of arthropod-plant interactions in the Upper Triassic of the southwestern United States". Lethaia. 29 (3): 237–248. doi:10.1111/j.1502-3931.1996.tb01657.x. ISSN   0024-1164.
  80. 1 2 3 4 5 6 Ash, Sidney R. (2014-06-01). "Contributions to the Upper Triassic Chinle flora in the American southwest". Palaeobiodiversity and Palaeoenvironments. 94 (2): 279–294. doi:10.1007/s12549-014-0150-3. ISSN   1867-1608. S2CID   129297877.
  81. 1 2 3 4 5 Ash, Sidney R. (1970). "Dinophyton, a problematical new plant genus from the Upper Triassic of the south-western United States" (PDF). Palaeontology. 13 (4): 646–663.
  82. 1 2 3 4 Ash, Sidney R. (1977). "An unusual bennettitalean leaf from the Upper Triassic of the south-western United States" (PDF). Palaeontology. 20 (3): 641–659.
  83. 1 2 3 Ash, Sidney R. (1970). "Pagiophyllum simpsonii, a New Conifer from the Chinle Formation (Upper Triassic) of Arizona". Journal of Paleontology. 44 (5): 945–952. JSTOR   1302730.
  84. 1 2 Ash, Sidney; Litwin, Ronald J. (1996). "Two new species of the pinnate microsporophyll Pramelreuthia from the upper Triassic of the southwestern United States". American Journal of Botany. 83 (8): 1091–1099. doi:10.1002/j.1537-2197.1996.tb12807.x.
  85. 1 2 3 4 5 Ash, Sidney R.; Hasiotis, Stephen T. (2013-04-01). "New occurrences of the controversial Late Triassic plant fossil Sanmiguelia Brown and associated ichnofossils in the Chinle Formation of Arizona and Utah, USA". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 268 (1): 65–82. doi:10.1127/0077-7749/2013/0316. ISSN   0077-7749.
  86. 1 2 Ash, Sidney R. (1982). "Occurrence of the Controversial Plant Fossil Sanmiguelia cf. S. lewisi Brown in the Upper Triassic of Utah". Journal of Paleontology. 56 (3): 751–754. JSTOR   1304404.
  87. 1 2 3 Ash, Sidney R. (1968). "A new species of Williamsonia from the Upper Triassic Chinle Formation of New Mexico". Journal of the Linnean Society of London, Botany. 61 (384): 113–120. doi:10.1111/j.1095-8339.1968.tb00108.x.
  88. "Fossil Trees or Petrified Wood" (PDF). University of Arizona. 2012. Retrieved October 14, 2021.
  89. 1 2 Herrick, Alisa S.; Fastovsky, David E.; Hoke, Gregory D. (1999). "OCCURRENCES OF ZAMITES POWELLII IN OLDEST NORIAN STRATA IN PETRIFIED FOREST NATIONAL PARK, ARIZONA" (PDF). National Park Service Paleontological Research. 4: 91–95.
  90. 1 2 3 4 5 6 7 8 9 Milner, Andrew C. (2006). "Plant fossils from the Owl Rock or Church Rock members, Chinle Formation, San Juan County, Utah". New Mexico Museum of Natural History & Science Bulletin. 37: 410–413.
  91. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 Ash, S.R. (1969). "Ferns from the Chinle Formation (Upper Triassic) in the Fort Wingate area, New Mexico" (PDF). United States Geological Survey, Professional Paper. Professional Paper. 613-D: 1–40. doi:10.3133/pp613d. ISSN   2330-7102.
  92. Daugherty, Lyman H. (1960). "Itopsidema, A New Genus of the Osmundaceae from the Triassic of Arizona". American Journal of Botany. 47 (9): 771–777. doi:10.1002/j.1537-2197.1960.tb07164.x.
  93. Ash, Sidney (2000). "Evidence of oribatid mite herbivory in the stem of a Late Triassic tree fern from Arizona". Journal of Paleontology. 74 (6): 1065–1071. doi:10.1666/0022-3360(2000)074<1065:EOOMHI>2.0.CO;2. ISSN   0022-3360. S2CID   86324641.
  94. 1 2 3 4 Ash, Sidney; Litwin, Ronald J.; Traverse, Alfred (1982). "The Upper Triassic fern Phlebopteris smithii (Daugherty) Arnold and its spores". Palynology. 6 (1): 203–219. doi:10.1080/01916122.1982.9989242. ISSN   0191-6122.
  95. 1 2 Ash, Sidney (1999). "An Upper Triassic Sphenopteris Showing Evidence of Insect Predation from Petrified Forest National Park, Arizona". International Journal of Plant Sciences. 160 (1): 208–215. doi:10.1086/314115. ISSN   1058-5893. S2CID   85020560.
  96. 1 2 Miller, Charles N. (1968). "The Lepidophytic Affinities of the Genus Chinlea and Osmundites Walkeri". American Journal of Botany. 55 (1): 109–115. doi:10.1002/j.1537-2197.1968.tb06950.x.
  97. Rothwell, Gar W.; R. Ash, Sidney (2015). "Internal anatomy of the Late Triassic Equisetocaulis gen. nov., and the evolution of modern horsetails". The Journal of the Torrey Botanical Society. 142 (1): 27–37. doi:10.3159/TORREY-D-14-00042.1. ISSN   1095-5674. S2CID   86841184.
  98. Holt, Edward L. (1947). "Upright Trunks of Neocalamites from the Upper Triassic of Western Colorado". The Journal of Geology. 55 (6): 511–513. doi:10.1086/625462. ISSN   0022-1376. S2CID   129374986.
  99. Miller, Gary L.; Ash, Sidney R. (1988). "The oldest freshwater decapod crustacean, from the Triassic of Arizona" (PDF). Palaeontology. 31 (2): 273–279.
  100. Sidney R. Ash & Geoffrey T. Creber (2000). "The Late Araucarioxylon arizonicum Trees of the Petrified Forest National Park, Arizona, USA". Palaeontology. 43: 22–23. doi: 10.1111/1475-4983.00116 . S2CID   128691956.

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