Xitun Formation

Last updated
Xitun Formation
Stratigraphic range: Early Devonian (Lochkovian)
Type Geological formation
Unit of Cuifengshan Group [1]
Underlies Guijiatun Formation [2]
Overlies Xiaxishancun Formation [2]
Lithology
PrimaryCalciferous mudstones [2]
Location
Coordinates 25°29.853'N and 103°46.309'E [2]
Region Yunnan Province
CountryFlag of the People's Republic of China.svg  China
Extent Qujing
Type section
Named forXitun village

The Xitun Formation is a palaeontological formation which is named after Xitun village in Qujing, a location in South China. This formation includes many remains of fossilized fish and plants of the Early Devonian period (Late Lochkovian). [1] [2] It was originally referred to as the Xitun Member of the Cuifengshan Formation (now the Cuifengshan Group). [3]

Contents

Fossil content

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.

Vertebrates

Acanthodians

Acanthodians reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Ischnacanthidae Genus indet. Qujing. [3] 4 isolated scales (V7218.1, 3, 6 & 8) & 2 longitudinal sections (V7218.4 & 7). [3] Similar to Ischnacanthus & Acanthodes , may be referrable to Youngacanthus .
Nostolepis N. amplificaXitun, Xishan subdistrict, Qujing. [4] 43 trunk scales. [4]
N. consuetaXitun, Xishan subdistrict, Qujing. [4] Around 25 trunk scales. [4]
N. digitusXitun , Xishan subdistrict, Qujing. [4] 28 trunk scales. [4]
N. qujingensisXitun, Xishan subdistrict, Qujing. [4] 19 trunk scales. [4]
N. striataXitun, Xishan subdistrict, Qujing. [4] 69 trunk scales. [4]
N. sp. indet. Qujing. [3] Body scales. [3]
Youngacanthus Y. gracilis Qujing. [3] Jaw elements & teeth. [3] An ischnacanthid.

Actinopterygians

Actinopterygians reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Meemannia M. eosXitun village, Qujing. [5] An early ray-finned fish, formerly thought to be a lobe finned fish. [6]

Chondrichthyes

Chondrichthyes reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Changolepis C. tricuspidus Qujing. [3] 10 scales of various growth stages. [3]
Chondrichthyes Genus indet. Qujing. [3] 4 isolated teeth (V7221.1, 2, 3 & 4).May belong to Gualepis or Changolepis .
Gualepis G. elegansXitun, Qilin district, Qujing. [7] Thousands of isolated scales. [3] [7]
Ohiolepis?O.? xitunensis Qujing. [3] A complete scale (V7233.1) & an incomplete scale (V7223.2). [3]
Peilepis P. solida Qujing. [3] A body scale (V7222). [3]

Jawless fish

Jawless fish reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Parathelodus P. asiaticusQilin district, Qujing. [8] Body scales. [8] A thelodont also known from the Xishancun Formation.
P. cornuformisQilin district, Qujing. [8] Body scales. [8] A thelodont also known from the Xishancun Formation.
P. liaokuoensisQilin district, Qujing. [8] Body scales. [8] A thelodont also known from the Xishancun Formation.
P. scitulusQilin district, Qujing. [8] A complete body scale (IVPP V 12156.1). [8] A thelodont also known from the Xishancun Formation.
P. trilobatusQilin district, Qujing. [8] Body scales. [8] A thelodont also found in the Xishancun Formation.
P. wangiQilin district, Qujing. [8] Body scales. [8] A thelodont also known from the Xishancun Formation.
P. xitunensisQilin district, Qujing. [8] A complete body scale (IVPP V 26113.1). [8] A thelodont.
Turinia T. asiatica Qujing. [3] Multiple scales. [3] A thelodont.
Turinia pagei.jpg
Xitunaspis X. magnus Qujing. [9] 4 headshields. [9] A galeaspid.

Placoderms

Placoderms reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Antiarchi Unnamed antiarch Qujing. [1] MNHN-CHD02 & V10515. [1] Originally referred to ?Xichonelepis.
Asterosteidae Gen. et. sp. indet. Qujing. [10] Part of the head shield. [10] Very similar to Gemuendina . [10]
Chuchinolepis C. gracilis Qujing. [1] Detached plates. [1] A chuchinolepidid also known from the Xishancun Formation.
C. qujingensisPlates. [1] A chuchinolepidid also known from the Xishancun Formation.
C. robusta Qujing. [1] A detached AVL plate (V10512). [1] A chuchinolepidid.
C. sulcata Qujing. [1] Trunkshield, plates & incomplete pectoral fin. [1] A chuchinolepidid.
Gavinaspis G. convergens Qujing. [11] Skull remains. [11] A phyllolepid.
Parayunnanolepis P. xitunensisAlmost-complete specimen. [12] A yunnanolepidid.
Parayunnanolepis xitunensis.jpg
Phymolepis P. cuifengshanensisCuifengshan and Liaokuoshan, Qujing. [1] [13] Plates. [1] [13] A yunnanolepidid also known from the Xishancun Formation.
Phymolepis cuifengshanensis.PNG
P. guoruii Qujing. [1] Trunk-shields & plates. [1] A yunnanolepidid.
Szeaspis S. yunnanensis Qujing. [14] Neurocranium & associated skull roof (IVPP V 5810a-b). [14] Preoccupied genus name, renamed Szelepis .
Szelepis S. yunnanensis Qujing. [14] Neurocranium & associated skull roof (IVPP V 5810a-b). [14] An actinolepid originally named Szeaspis.
Yunnanolepis Y. porifera Qujing. [1] A yunnanolepidid also known from the Xishancun Formation.
Y. sp. Qujing. [1] A trunk-shield associated with part of skull roof (V10514). [1] A yunnanolepidid, specimen formerly assigned to Vanchienolepis .
Zhanjilepis Z. aspratilis Qujing. [1] Plates. [1] A yunnanolepidid also known from the Xishancun Formation.
Zhanjilepis aspartilis.jpg

Sarcopterygians

Sarcopterygians reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Achoania A. jarvikii Qujing. [15] Anterior cranial portion. [15] A basal lobe finned fish.
Diabolepis D. speratusXichong, Qujing. [16] Multiple specimens. [16] [17] A dipteriform originally named Diabolichthys .
Psarolepis P. romeriXichong, Qujing. [18] 4 anterior cranial portions, a posterior cranial portion, 2 complete lower jaws & an incomplete lower jaw. [18] A basal lobe finned fish.
Psarolepis BW.jpg
Styloichthys S. changae Qujing. [19] Multiple specimens. [19] A basal coelacanth. [20]
Snout-orbitalregion-stylo2.jpg
Youngolepis Y. praecursorNumerous specimens. [21] A basal lobe finned fish also known from the Bac Bun Formation.
Youngolepis praecursor Fig1.jpg

Plants

Plants reported from the Xitun Formation
GenusSpeciesPresenceMaterialNotesImages
Gen. nov. AHuaguo Hill, Shengfeng district of Qujing city. [2] Numerous specimens. [2]
aff. Huia aff. H. sp.Huaguo Hill, Shengfeng district of Qujing city. [2] PKU-XH214. [2] A lycophyte.
Unnamed spikeHuaguo Hill, Shengfeng district of Qujing city. [2] A poorly preserved terminal spike (PKU-XH215a, 215b). [2] Probably from a zosterophyll.
Xitunia X. spinitheca Qujing. [22] A zosterophyll.
Zosterophyllum Z. minorstachyum Qujing. [22] A zosterophyll.
Zosterophyllum sp. - MUSE cropped.jpg
Z. shengfengenseA building site at Huaguo Hill, Shengfeng District, Qujing City. [23] A nearly entire individual plant preserved as a compression (PUH-QXI01-1), and its counterpart (PUH-QXI01-1’). [23] A zosterophyll.

See also

Related Research Articles

<span class="mw-page-title-main">Chondrichthyes</span> Class of jawed cartilaginous fishes

Chondrichthyes is a class of jawed fish that contains the cartilaginous fish or chondrichthyians, which all have skeletons primarily composed of cartilage. They can be contrasted with the Osteichthyes or bony fish, which have skeletons primarily composed of bone tissue. Chondrichthyes are aquatic vertebrates with paired fins, paired nares, placoid scales, conus arteriosus in the heart, and a lack of opecula and swim bladders. Within the infraphylum Gnathostomata, cartilaginous fishes are distinct from all other jawed vertebrates.

<span class="mw-page-title-main">Gnathostomata</span> Infraphylum of vertebrates

Gnathostomata are the jawed vertebrates. Gnathostome diversity comprises roughly 60,000 species, which accounts for 99% of all living vertebrates, including humans. In addition to opposing jaws, living gnathostomes have true teeth, paired appendages, the elastomeric protein of elastin, and a horizontal semicircular canal of the inner ear, along with physiological and cellular anatomical characters such as the myelin sheaths of neurons, and an adaptive immune system that has the discrete lymphoid organs of spleen and thymus, and uses V(D)J recombination to create antigen recognition sites, rather than using genetic recombination in the variable lymphocyte receptor gene.

<span class="mw-page-title-main">Acanthodii</span> Class of fishes (fossil)

Acanthodii or acanthodians is an extinct class of gnathostomes. They are currently considered to represent a paraphyletic grade of various fish lineages basal to extant Chondrichthyes, which includes living sharks, rays, and chimaeras. Acanthodians possess a mosaic of features shared with both osteichthyans and chondrichthyans. In general body shape, they were similar to modern sharks, but their epidermis was covered with tiny rhomboid platelets like the scales of holosteians.

<span class="mw-page-title-main">Placodermi</span> Class of fishes (fossil)

Placodermi is a class of armoured prehistoric fish, known from fossils, which lived from the Silurian to the end of the Devonian period. Their head and thorax were covered by articulated armoured plates and the rest of the body was scaled or naked, depending on the species. Placoderms were among the first jawed fish; their jaws likely evolved from the first of their gill arches.

<i>Mizia</i> Extinct genus of fishes

Mizia is a genus of primitive antiarch placoderm found in Emsian-aged marine strata of Early Devonian China.

<span class="mw-page-title-main">Arthrodira</span> Extinct order of fishes

Arthrodira is an order of extinct armored, jawed fishes of the class Placodermi that flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. Arthrodires were the largest and most diverse of all groups of placoderms.

Meemannia is a genus of extinct bony fish from the early Devonian period. It was initially classified as a lobe-finned fish; however, a restudy conducted by Lu et al. (2016) indicates that it was actually an early-diverging ray-finned fish. It was found in Yunnan, China. As preserved, it consists mainly of skull roofing bones and a partial otic region of the braincase. Its anatomy is unique in a number of features that resemble ray-finned fishes (Actinopterygii), and more generalized jawed vertebrates.

<i>Psarolepis</i> Extinct genus of fishes

Psarolepis is a genus of extinct bony fish which lived around 397 to 418 million years ago. Fossils of Psarolepis have been found mainly in South China and described by paleontologist Xiaobo Yu in 1998. It is not known certainly in which group Psarolepis belongs, but paleontologists agree that it probably is a basal genus and seems to be close to the common ancestor of lobe-finned and ray-finned fishes. In 2001, paleontologist John A. Long compared Psarolepis with onychodontiform fishes and refer to their relationships.

<i>Youngolepis</i> Extinct genus of fishes

Youngolepis is a genus of prehistoric coelocanth which lived during the Early Devonian period. Fossils of Y. praecursor have been found in the Xitun Formation of China & the Bac Bun Formation of Trang Xa, Vietnam. Some additional fossil specimens from the Xishancun Formation of China have been referred to Youngolepis sp. & represent the oldest known occurrence of the genus. In addition, Y. praecursor is also found in the Xujiachong formation

<i>Minicrania</i> Extinct genus of fishes

Minicrania is an extinct genus of tiny antiarch fish, with armor averaging up to about 2 centimetres (0.79 in) long, which lived during the Lochkovian epoch in Early Devonian Yunnan Province, China and northern Vietnam.

Gavinaspis is a phyllolepid placoderm which lived during the Early Devonian period, of Qujing, Yunnan province, south China.

Achoania is an extinct genus of primitive bony fish which lived during the Early Devonian period. It is known from a skull discovered in the Xitun Formation of Yunnan, China. While originally originally considered to be a lobe-finned fish, later studies suggested that it may be a stem-group Osteichthyes instead.

Guiyu oneiros is one of the earliest articulated bony fish discovered. Fossils of Guiyu have been found in what is now Qujing, Yunnan, China, in late Silurian marine strata, about 425 million years old.

<i>Silurolepis</i> Extinct genus of fishes

Silurolepis platydorsalis is a species of Silurian-aged "maxillate" early placoderm that has been described from (mostly) articulated remains. Although it has been known for several years, it was finally described by Zhang, et al., in 2010.

<i>Entelognathus</i> Placoderm fish from the late Ludlow epoch of the Silurian period

Entelognathus primordialis is a early placoderm from the late Silurian of Qujing, Yunnan, 419 million years ago.

<i>Parayunnanolepis</i> Extinct genus of fishes

Parayunnanolepis xitunensis is an extinct, primitive antiarch placoderm. The fossil specimens, including a marvelously preserved, intact specimen, are known from the Lochkovian Epoch-aged Xitun Formation of Early Devonian Yunnan. The armor is very similar to that of Yunnanolepis, but is distinguished by being comparatively more flattened.

Meemann Chang also known as Zhang Miman, is a Chinese paleontologist at the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP). She completed her undergraduate studies at Moscow University and completed her PhD thesis entitled 'The braincase of Youngolepis, a Lower Devonian crossopterygian from Yunnan, south-western China' at Stockholm University. She was the first woman to become head of IVPP in 1983. For her many career achievements, she received an honorary degree from the University of Chicago in 2011 and the Romer-Simpson Medal from the Society of Vertebrate Paleontology in 2016.

<i>Phymolepis</i> Extinct genus of fishes

Phymolepis is an extinct genus of yunnanolepidid placoderm from the Early Devonian of China. The type species, P. cuifengshanensis, was named by Zhang Goroui in 1978 and was re-evaluated in 2018, while a second species, P. guoruii, was named and described in 1996.

<i>Houia</i> Extinct genus of arthropods

Houia is an extinct genus of dekatriatan, a clade of chelicerate arthropods. Fossils of Houia have been discovered in deposits of the Early Devonian period in Guangxi and Yunnan, both in China. The genus contains two species: H. guangxiensis, from the Pragian to Emsian epoch of Guangxi; and H. yueya, the type species, from the Lochkovian epoch of Yunnan. The name of the genus is derived from the Chinese character (hòu), meaning "horseshoe crab".

References

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