Kitadani Formation

Kitadani Formation
Stratigraphic range: Barremian-Aptian
~125–115 Ma
The Kitadani Dinosaur Quarry Bonebed I, where an outcrop of the Kitadani Formation can be found; the white arrow indicates the location of the type locality of Tyrannomimus fukuiensis. Photographed in c. 2023.
TypeGeological formation
Unit ofTetori Group
UnderliesOmichidani Formation
OverliesAkaiwa Formation
Thickness~100 m (330 ft)[1]
Lithology
PrimaryTuff, sandstone, shale
OtherCoal
Location
Coordinates36°06′N 136°36′E / 36.1°N 136.6°E / 36.1; 136.6
Approximate paleocoordinates47°18′N 137°42′E / 47.3°N 137.7°E / 47.3; 137.7
Region Fukui Prefecture
Country Japan
Type section
Named byUnknown[1]
Kitadani Formation is located in Japan
Kitadani Formation
Kitadani Formation (Japan)

The Kitadani Formation (Japanese: 北谷層 Kitadani-sō) is a unit of Lower Cretaceous sedimentary rock which crops out near the city of Katsuyama in Fukui Prefecture, Japan, and it is the primary source of Cretaceous-aged non-marine vertebrate fossils in Japan. Dinosaur remains are among the fossils that have been recovered from the formation, but it also preserves a diverse assemblage of plants, invertebrates, and other vertebrates.[2] Most, if not all, of the fossil specimens collected from the Kitadani Formation are reposited at the Fukui Prefectural Dinosaur Museum.[3]

The Kitadani Formation is a unit within the Tetori Group, a major sequence of Lower Cretaceous rocks that is distributed across Fukui, Ishikawa, and Gifu prefectures of western-central Honshu. The Tetori Group exhibits marked lateral variation, and the Kitadani Formation is only present in Fukui Prefecture.[1] The Kitadani Formation comprises interbedded tuffs, sandstones, and shales and reaches a maximum thickness of approximately one hundred meters (~328 feet).[1] It conformably overlies the Akaiwa Formation and is unconformably overlain by the Omichidani Formation.[4] The Kitadani Formation is significant because it is the major source of dinosaur fossils in Japan and because of Japan's unique position along the northeastern margin of Eurasia during the Early Cretaceous.

Geology

The Kitadani Formation is a unit within the Tetori Group, a Lower Cretaceous sequence of predominantly sedimentary rock which crops out in the Fukui, Ishikawa, and Gifu prefectures of west-central Honshu, Japan in the region surrounding Mount Haku.[1][5]

The formations present within the Tetori Group vary laterally, and the Kitadani Formation crops out only in the Kuzuryū River district of Fukui Prefecture. In this region, the sequence comprises, in ascending stratigraphic order: Gomijima Formation, the Kuwajima Formation, the Akaiwa Formation, and Kitadani Formation.[1] The Kitadani Formation comprises alternating horizons of red-brown tuffs, blackish shales and sandstones, and thin coal beds. The sandstones within the Kitadani Formation are light gray and green and range in clast size from fine to coarse. The type section of the Kitadani Formation occurs along the Nakanomatadani branch of the Takinami River [ja] near the city of Katsuyama, where it is approximately 100 m (~328 feet) in thickness. The Kitadani Formation conformably overlies the Akaiwa Formation and is unconformably overlain by the Omichidani Formation.[1]

The palaeoclimate during the deposition of the formation was noticeably warmer and drier than that of the older Kuwajima and Okurodani Formations, as evidenced by oxygen isotope records as well as by the presence of crocodylomorph fossils in the former in contrast to their absence in the latter.[6]

The Kitadani Formation has had varying nomenclature throughout the history of its study.[1] In the early stratigraphic literature on the Tetori Group, the Kitadani Formation was variably referred to as the "Lower part of the Omichidani Formation",[7] the "Chinaboradani Alternation of Tuff, Shale, and Sandstone",[8] the "Kitadani Alternation of Sandstone, Shale, and Tuff",[9] and simply the "Kitadani Alternation"[10] prior to its designation as a formation.[1]

Age

The Kitadani Formation was biostratigraphically dated to the late Barremian and early Aptian ages of the Early Cretaceous Epoch in 2002 based upon the presence of the freshwater bivalve Nippononaia ryosekiana.[11] In 2005, part of the Kitadani Formation was biostratigraphically dated to the Barremian Age based upon the occurrence of the charophyte gyrogonite Clavator harrisii reyi in association with other charophytes.[12] These biostratigraphic age assignments are supported by zircon fission track radioisotopic ages of tuff, which date the Kitadani Formation to 127-115 Ma.[13]

Fossil assemblage

The Kitadani Formation preserves a diverse assemblage of plant fossils; invertebrate fossils; and vertebrate body and trace fossils, including mammals, turtles, crocodylomorphs, and dinosaurs. Many vertebrate specimens from the Kitadani Formation are incomplete and poorly preserved, so taxonomic diversity is likely higher than it seems.

Plant fossils

The plant fossil assemblage of the Kitadani Formation is characterized by a rarity of ferns and an abundance of cycadales and conifers represented mostly by cones and shoots.[14] A palynological study in 2013 resulted in the identification of greater than 40 species of spores, pollen grains, and plant fragments from the Kitadani Formation representing gymnosperms, freshwater algae, and epiphyllous fungus; however, no angiosperm pollen was identified.[15] Branches of the conifer Brachyphyllum obesum have been recovered, which was interpreted to represent the warming and possible drying of the climate toward the upper Tetori Group.[16] This interpretation is supported by the lack of plants from lower in the Tetori Group, such as ginkgos, in the Kitadani Formation.[17]

Invertebrate fossils

The invertebrate fossil assemblage of the Kitadani Formation mostly comprises freshwater and brackish water bivalve and gastropod mollusks.[18]

Molluscs reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Unio U (?). ogamigoensis Unionid bivalve
Plicatounio P. naktongensis naktongensis
P. naktongensis multiplicatus
Nagdongia N. soni (or Nakamuranaia chingshanensis)
Pseudohyria P. matsumotoi
P. sp. cf. matsumotoi
Nippononaia N. ryosekiana
N. tetoriensis
Trigonioides T. (Wakinoa) tetoriensis
Viviparus V. onogoensis Architaenioglossan gastropod
Planorbidae Indeterminate Hygrophilan gastropod
Insects reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
?Morphna ?M. sp. Blaberidae
Petropterix P. fukuiensis Umenocoleidae
Praeblattella P. inexpecta Mesoblattinidae
P. arcuata
?Vitisma ?V. sp. Umenocoleidae
Ostracods reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Cypridea C. angusticaudata Ostracod
C. (Morinia) monosulcata zhejiangensis
C. (Bisulcocypridea) sp.
Timiriasevia Indeterminate

Vertebrate fossils

Actinopterygii

Fishes reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Amiiformes[18] indeterminate Kitadani Dinosaur Quarry Bonebed I Scales
?Lepidotes ?L. sp. Scales

Mammaliaformes

Mammaliaformes reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Symmetrolestes S. parvus[19] North of Kitadani Dinosaur Quarry Bonebed Fragmentary right mandible Spalacotheriid
Eobaataridae Indeterminate[20] Kitadani Dinosaur Quarry Bonebed I A left p4 crown
?Triconodontidae Indeterminate[20] Kitadani Dinosaur Quarry Bonebed I "a fragment of possible right dentary with a damaged molariform crown and roots"

Testudines

Turtles are represented mostly by shell fragments within the Kitadani Formation.[21][22]

Turtles reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Adocidae Indeterminate Shell Different with Adocus from the same formation
Adocus A. sp. Kitadani Dinosaur Quarry Bonebed I Shell
Nanhsiungchelyidae Indeterminate Kitadani Dinosaur Quarry Bonebed I Shell Had been tentatively classified as Basilemys sp. by Hirayama (2002)
?Sinemydidae Indeterminate Kitadani Dinosaur Quarry Bonebed I Shell
Testudinoidea Indeterminate Kitadani Dinosaur Quarry Bonebed I Shell
Trionychidae Indeterminate Kitadani Dinosaur Quarry Bonebed I Shell
Xinjiangchelyidae Indeterminate Shell

Crocodylomorpha

A nearly complete skeleton of goniopholidid has been discovered from the Kitadani Formation, but this material remains undescribed.[23]

Crocodylomorpha reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Goniopholididae indeterminate Kitadani Dinosaur Quarry (Unspecified) Partial skeleton including cranial remains Phylogenetic analysis suggests that it a basal member of the group similar in position to Siamosuchus and Sunosuchus.[24]
Undescribed Kitadani goniopholidid

Dinosauria

Dinosaurs are among the most well-known vertebrate taxa from the Kitadani Formation. Taxa from all three major dinosaurian clades — Theropoda, Sauropodomorpha, and Ornithischia — have been recovered.[2]

Dinosaurs reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Ankylosauria Indeterminate Teeth Family unknown
Fukuipteryx[25] F. prima Kitadani Dinosaur Quarry (Unspecified) Associated disarticulated partial skeleton Avialan
Fukuiraptor[26][27] F. kitadaniensis Kitadani Dinosaur Quarry Bonebed I Multiple individuals showing different ontogenetic stages Basal megaraptoran

Fukuisaurus[28][29] F. tetoriensis Kitadani Dinosaur Quarry Bonebed I Multiple specimens representing a partial skeleton Hadrosauroid
Fukuititan[30] F. nipponensis Kitadani Dinosaur Quarry Bonebed II Associated partial skeleton Titanosauriform
Fukuivenator[31] F. paradoxus Kitadani Dinosaur Quarry Partial skeleton with skull Basal therizinosaur or some other kind of basal maniraptoran
Koshisaurus[29] K. katsuyama Kitadani Dinosaur Quarry Bonebed IV Partial skeleton Hadrosauroid
Spinosauridae[32] Indeterminate Kitadani Dinosaur Quarry Bonebed I 18 Teeth Subfamily unknown
Tyrannomimus[33] T. fukuiensis Kitadani Dinosaur Quarry Bonebed I Isolated remains from multiple individuals The earliest definitive deinocheirid

Ichnofossils

Undescribed tracks of ankylosaurs and sauropods have been discovered from the Kitadani Formation.[34]

Ichnofossils reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Amblydactylus A. isp.[34] Ornithopod tracks.
Aquatilavipes A. isp.[35] Bird tracks
Asianopodus A. isp.[36] Small to medium-sized tridactyl theropod tracks.
Caririchnium C. isp.[34] Ornithopod tracks
Eubrontidae Indeterminate[36] Large tridactyl theropod tracks.
Grallatoridae Indeterminate[36] Small to medium-sized tridactyl theropod tracks
cf. Gyeongsangornipes cf. G. isp.[35] Bird tracks.
Minisauripus M. isp.[36] The smallest theropod track from the Kitadani Formation.
Ornithomimipodidae Indeterminate[36] Slender-toed tridactyl theropod tracks.
Pteraichnus P. nipponensis[37] Pterosaur tracks; The first pterosaur ichnofossil reported in Japan.

Eggs

Eggs reported from the Kitadani Formation
Genus Species Location Stratigraphic position Material Notes Images
Plagioolithus[38] P. fukuiensis Three-layered eggshell interpreted as a fossil avian egg.

See also

References

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  2. ^ a b Weishampel, D.B.; et al. (2004). "Dinosaur distribution (Early Cretaceous, Asia)." In: Weishampel, D.B.; Dodson, P.; and Osmólska, H. (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 563-570. ISBN 0-520-24209-2.
  3. ^ "FPDM: Fukui Prefectural Dinosaur Museum".
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  5. ^ Yamada, Toshihiro; Sano, Shin-ichi (2018). "Designation of the Type Section of the Tetori Group and Redefinition of the Kuzuryu Group distributed in Central Japan". Memoir of the Fukui Prefectural Dinosaur Museum. 17: 89–94. Retrieved 25 February 2023.
  6. ^ Amiot, Romain; Kusuhashi, Nao; Saegusa, Haruo; Shibata, Masateru; Ikegami, Naoki; Shimojima, Shizuo; Sonoda, Teppei; Fourel, François; Ikeda, Tadahiro; Lécuyer, Christophe; Philippe, Marc; Wang, Xu (January 2021). "Paleoclimate and ecology of Cretaceous continental ecosystems of Japan inferred from the stable oxygen and carbon isotope compositions of vertebrate bioapatite". Journal of Asian Earth Sciences. 205: 104602. Bibcode:2021JAESc.20504602A. doi:10.1016/j.jseaes.2020.104602. S2CID 228820808.
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  38. ^ Imai, Takuya; Azuma, Yoichi (2015). "The oldest known avian eggshells, Plagioolithus fukuiensis, from the Lower Cretaceous (upper Barremian) Kitadani Formation, Fukui, Japan". Historical Biology. 27 (8): 1090–1097. Bibcode:2015HBio...27.1090I. doi:10.1080/08912963.2014.934232. S2CID 129113738.