Shishugou Formation

Coordinates: 44°30′N 90°12′E / 44.5°N 90.2°E / 44.5; 90.2
Source: Wikipedia, the free encyclopedia.

Shishugou Formation
Ma
Type
Approximate paleocoordinates
42°30′N 100°30′E / 42.5°N 100.5°E / 42.5; 100.5
RegionXinjiang
Country China
ExtentNorthern Junggar Basin

The Shishugou Formation (

China
.

Its strata date back to the

theropod fauna.[3]

The Wucaiwan Member, once considered a separate, underlying formation,[4] is now considered the lowest unit of the Shishugou Formation.

Lithology

At the Wuwaican locality, the formation is approximately 380 m thick, the lower 30 metres of the formation predominantly consist of conglomerate, with the majority of the formation consisting of red coloured mudstone with frequent channel/sheet sandstone lenses and occasional tuffaceous deposits.[3] It is laterally equivalent to the Qigu Formation in the southern half of the Junggar Basin.

Shishugou Formation dinosaur traps

The Shishugou Formation dinosaur traps also known as death pits or death traps are pit structures found within the formation that are noted for their fossil content.

Paleontology

These 'traps' or 'bonebeds' are unusual in that they consist of vertically stacked skeletons of numerous non-avian theropods in 1–2 metres (3.3–6.6 ft) deep pits. The pits are filled with a mix of alluvial and volcanic mudstone and sandstone and appear to have been created by the trampling and wallowing of large dinosaurs. Small theropods and vertebrates then became mired in these pits, dying and being forced deeper by the activities of the large dinosaurs and the struggles of later victims. The high quality of preservation suggests a rapid burying of the carcasses. Some scavenging of the bodies took place leading to a dispersal of body parts. Smaller vertebrates were prone to getting stuck in these mudholes, and the small ceratosaur,

Limusaurus inextricabilis, is the most common in the resulting bonebeds.[5]

Excavations since 2000 have revealed a wealth of fossils dating from a period some 165 to 155 million years ago. Palaeontologists James Clark and

tyrannosaurs. Clark joined Xu, from Beijing's Institute of Vertebrate Paleontology and Paleoanthropology, to explore the Junggar Basin, and in particular the Shishugou Formation, where the exposed rocks have been linked to the Middle Jurassic
.

Prehistoric life

Guanlong wucaii

At the time the area was covered by marshland, adjoined a small mountain range peppered with volcanoes, and was inhabited by dinosaurs, small crocodilians and amphibians. Currently it is a sparsely settled region of dry washes, arid badlands and dunes along the

Gobi desert’s western edge. The Shishugou Formation consists of mudstone, siltstone, and sandstone, and is named for the silicified wood or petrified logs found here. ('Shishugou' = 'stone tree valley') These badlands were used for some sequences in the film Crouching Tiger, Hidden Dragon,[6] the genus Yinlong
('hidden dragon') being named for the film.

Mamenchisaurus sinocanadorum

When the site was first excavated, new species of turtles, crocodilians, pterosaurs, and early mammals were revealed. Many of these species showed the rudiments of characteristics that would later become their hallmarks. One of the first fossil skeletons exposed proved to be that of an unknown

Tienshanosaurus chitaiensis. Later expeditions stretched from the 1960s to the 1990s and yielded among others the extremely long-necked Mamenchisaurus and the carnivorous Sinraptor
. In all, some 600 specimens have been collected.

On analysis of the rock matrix, large amounts of volcanic ash were found, hinting at eruptions during that period, the ash raining onto the marsh creating viscous mud and becoming subsequent death traps. To date three of these death pits have been located. In one pit a

tyrannosauroid named Guanlong, sporting a crest running from its nose to the back of its head. Its discovery was hailed by paleontologists as the earliest known remains of the tyrannosauroid clan that culminated with Tyrannosaurus rex
.

Vertebrate paleofauna

Ornithischians

Undescribed stegosaur is present in the Wucaiwan member.

ankylosaurs present in both upper Shishugou and Wucaiwan members.[2]

Genus Species Stratigraphic position Abundance Notes Images
"
Eugongbusaurus
"
"E. wucaiwanensis" Upper An unspecified basal
neornithischian), previously classified as Gongbusaurus wucaiwanensis.[2]
It is estimated at around 1.3 to 1.5 meters (4.3 to 4.9 ft) long.
Hualianceratops H. wucaiwanensis Upper An early
ceratopsian.[7]
Jiangjunosaurus J. junggarensis Upper A
stegosaurid reaching around 6 meters (20 feet) in length and weighed 2.5 metric tons.[8]
It had three distinguishing traits: the crowns of the teeth are symmetrical and in side view wider than tall; the spine of the axis, the second neck vertebra, has a rectangular profile in side view, instead of a triangular one; and the rear neck vertebrae have large vein openings in their sides.
Yinlong Y. downsi Upper A very basal and most primitive ceratopsian (possibly a chaoyangsaurid). It was bipedal and had a total length of about 1.2 meters (3.9 feet) from nose to tail, and a weight of about 15 kilograms (33 pounds).[9]

Pterosaurs

Genus Species Stratigraphic position Abundance Notes Images
Kryptodrakon K. progenitor Upper A basal
pterodactyloid
with an estimated wingspan of 1.47 meters (4.8 feet).
Sericipterus S. wucaiwanensis Upper A
rhamphorhynchid with a wingspan that has been estimated at least 1.73 meters.[10]

Sauropods

Sauropods
of the Shishugou Formation
Genus Species Stratigraphic position Material Notes Images
Bellusaurus B. sui base of Upper A short-necked sauropod only known from juvenile specimens which measured about 4.8 meters (16 feet) long.[4]
Fushanosaurus[11] F. qitaiensis Upper Complete right femur A
titanosauriform
estimated to have been approximately 98 feet long, which would then make it one of the longest known dinosaurs.
Klamelisaurus K. gobiensis Wucaiwan member A eusauropod measuring 15 meters and weighing 5 metric tons.
Mamenchisaurus M. sinocanadorum Upper "Partial skull and skeleton."[12] A
mamenchisaurid with a remarkably long neck which made up half the total body length.[2]
It is one of the largest dinosaurs known, measuring 35 meters (115 feet) in length with an 18-meter-long (59 feet) neck.
Tienshanosaurus T. chitaiensis Upper "Partial postcranial skeleton."[13] A mamenchisaurid known from very few remains.[2]

Theropods

Undescribed

ornithomimosaur-like species.[2] Indeterminate tetanuran remains.[2]

Genus Species Stratigraphic position Abundance Notes Images
Aorun A. zhaoi Wucaiwan member A basal
alvarezsaur that was at best 1 meter (3.3 feet) long and weighed 2 kilograms (4.4 pounds) at most.[3]
Guanlong G. wucaii Upper A
tyrannosaurs, about 3 meters (9.8 feet).[14]
It has a large distinctive crest on its head, a feature seen in many primitive tyrannosaurs
Haplocheirus H. sollers Upper An alvarezsaur that was the largest known definite member of the superfamily, at around 2 meters long. It had an enlarged thumb claw like other alvarezsaurs, but also retained two other functional fingers, unlike more derived alvarezsaurs, where only the thumb was significantly large and clawed.[15]
Limusaurus L. inextricabilis Upper A toothless, omnivorous
Eastern Asia, including China.[16]
Limusaurus had a small slender body measuring about 1.7 meters in length.
Monolophosaurus M. jiangi Wucaiwan member A
tetanuran
named for the single crest on top of its skull. It is estimated to have a length at 5.5 meters (16.4 feet), the weight at 475 kilograms.
Shishugounykus S. inexpectus Upper A little-known early alvarezsaur.
Sinraptor S. dongi Upper A metriacanthosaurine metriacanthosaur theropod standing nearly 3 meters (9.8 feet) tall and measuring roughly 7.6 meters (25 feet) in length.
Zuolong Z. salleei Upper A basal
gray wolf. The specimen known is probably from a juvenile individual and is quite complete.[17]

Crocodylomorphs

After an overview of crocodylomorphs of the Junggar Basin, Wings et al. identified the following species from the Shishugou Formation.[18]

Genus Species Stratigraphic position Abundance Notes Images
Crocodyliformes indet. Upper A single fully articulated skeleton Found on the same slab that also preserved the holotype and an associated specimen of Limusaurus inextricabilis[16][5]
Junggarsuchus J. sloani Upper
Sunosuchus S. junggarensis Upper Goniopholidid
Nominosuchus N. matutinus Upper
Shartegosuchid

Mammaliamorphs

Genus Species Stratigraphic position Abundance Notes Images
Yuanotherium Y. minor Upper A tritylodontid[19]

See also

References