Skip to main content

Rapid neck elongation in Sauropterygia (Reptilia: Diapsida) revealed by a new basal pachypleurosaur from the Lower Triassic of China


Neck elongation has appeared independently in several tetrapod groups, including giraffes and sauropod dinosaurs on land, birds and pterosaurs in the air, and sauropterygians (plesiosaurs and relatives) in the oceans. Long necks arose in Early Triassic sauropterygians, but the nature and rate of that elongation has not been documented. Here, we report a new species of pachypleurosaurid sauropterygian, Chusaurus xiangensis gen. et sp. nov., based on two new specimens from the Early Triassic Nanzhang-Yuan’an Fauna in the South China Block. The new species shows key features of its Middle Triassic relatives, but has a relatively short neck, measuring 0.48 of the trunk length, compared to > 0.8 from the Middle Triassic onwards. Comparative phylogenetic analysis shows that neck elongation occurred rapidly in all Triassic eosauropterygian lineages, probably driven by feeding pressure in a time of rapid re-establishment of new kinds of marine ecosystems.

Peer Review reports


Marine tetrapods, mainly mammals, occupy various trophic levels in modern marine ecosystems [1]. The situation was very different in the Mesozoic, when a much wider diversity of reptiles occupied similar trophic roles and show evidence of iterative evolution of similar locomotory and feeding modes [1,2,3]. The similarity of body plan and anatomical characters among different marine tetrapod groups, such as paddle-like limbs or a streamlined body shape, is evidence of morphological convergence in marine adaptation [1, 4, 5]. Various reptile clades invaded the ocean during the Mesozoic, among which Sauropterygia, Ichthyopterygia, and marine clades of Testudinata, are the longest-lasting clades. Both ichthyosaurs and sauropterygians have their first known occurrences in the Early Triassic, while the earliest fossil record of a marine turtle comes from the Late Triassic [6,7,8,9]. Ichthyosaurs evolved large body size rapidly and adopted a thunniform body plan convergent with cetaceans [10, 11]. Sea turtles exist in the modern ocean, but sauropterygians have no living analogue despite the evident success of their body plan body plan in the Mesozoic, especially the extremely long-necked plesiosaurian sauropterygians. A similar body plan could be seen in some other Mesozoic marine reptiles, like tanystropheids, but no living tetrapod has a neck that is longer than its trunk, except giraffes on land and some birds [1, 12].

Sauropterygia diversified and became widespread during the Early-Middle Triassic, but only the long-necked pelagic lineage survived past the Late Triassic. Compared to abundant sauropterygians in the Middle Triassic, reports from the Lower Triassic are limited to a few incomplete specimens, but several clades became long-necked postdating the Late Triassic. While Tanystropheus and Dinocephalosaurus increased the length of each vertebra to attain a long neck, neck length in Sauropterygia shows a different pattern, mostly achieved by increasing the number of vertebrae [13]. Elasmosauroids from the Cretaceous are well known for their extremely elongated necks, sometimes with over 70 cervical vertebrae [14, 15]. The neck elongation in Triassic eosauropterygians is less extreme, but the origin and rate of acquisition of this feature is obscured by the absence of good fossils of basal taxa. Although a handful of eosauropterygian fossils have been reported in the Early Triassic, most of them are too incomplete to allow precise measurements of head and neck, such as the known specimens of Majiashanosaurus discocoracoidis and Lariosaurus sanxiaensis [9, 16, 17]. Nevertheless, the recently reported [18] nearly complete specimen of Hanosaurus hupehensis, as well as some Corosaurus alcovensis specimens [19,20,21], provide the desired measurements, but good quality basal pachypleurosaurids are required to further explore the earliest stages of the neck-elongation trend among different eosauropterygian clades.

Here we report and describe two specimens of a new eosauropterygian taxon from the Early Triassic Nanzhang-Yuan’an Fauna (NYF), Hubei Province, P. R. China, which aid in mapping the evolution of neck elongation in Eosauropterygia. The newly discovered WGSC V 1901 is nearly complete, providing vital material to quantify the body plan of early marine reptiles, such as neck length/trunk length ratio, and to explore the history of neck elongation in Eosauropterygia.


Geological setting

The NYF occurs at several carbonate outcrops between Nanzhang and Yuan’an counties, Hubei Province, P. R. China (Fig. 1). Fossiliferous beds with abundant marine reptile skeletons and bone fragments mainly occur in the upper part of Member II of the Jialingjiang Formation, comprising laminated micritic carbonates [22]. A zircon U-Pb age of 247.8 ± 1.2 Ma [22, 23] from the volcanic tuff at the top of Member II indicates its age is Spathian (late Olenekian; Early Triassic). The sediments indicate a restricted shallow water or lagoonal environment, coinciding with the palaeogeography of the Yangtze Block in the Triassic [22,23,24].

Fig. 1
figure 1

Summary geological maps. (A) The general location of the South China block in the Early Triassic (modified from Benton et al. [24]). (B) Tectonic map showing major blocks of South China [24], with the site of Nanzhang-Yuan’an Fauna (NYF). (C) Simplified geological map of Nanzhang and Yuan’an counties with distributions of Triassic marine reptiles (modified from Li et al. [16] and Yan et al. [22]). ‘Old land’ is coloured orange, shallow seas light blue, and deep marine basins dark blue in A, B. Abbreviations: Є-S, Cambrian-Silurian; D-P, Devonian-Permian; T1d, Daye Formation, Lower Triassic; T1j, Jialingjiang Formation, Lower Triassic; T2b, Badong Formation, Middle Triassic; T3-J, Upper Triassic-Jurassic; K-Q, Cretaceous-Quaternary.

Systematic palaeontology

Superorder Sauropterygia Owen, 1860 [25].

Order Eosauropterygia Rieppel, 1994 [26].

Family Pachypleurosauridae Nopcsa, 1928 [27].

Genus Chusaurus, gen. nov.

(Figs. 2 and 3)

Fig. 2
figure 2

The two specimens of Chusaurus xiangensis gen. et sp. nov. (A) Photograph of WGSC V 1901, mostly in dorsal view. (B) Interpretive drawing of WGSC V 1901. (C) Photograph of WGSC V 1702, dorsally exposed. (D) Mould and part of the skeleton from the counterpart of WGSC V 1702. (E) Interpretive drawing of WGSC V 1702. The black arrow in B indicates the abrupt inversion of the cervical vertebral column. Skull elements are marked by a black dashed line in D, and shadow in E, and represent the shape of the mould in D marked by a white dashed line. White arrows indicate the corresponding parts in C-E. Abbreviations: CdV, caudal vertebra; CV, cervical vertebra; DR, dorsal rib; DV, dorsal vertebra; ph, phalanx; SV, sacral vertebra. Scale bar = 2 cm

Fig. 3
figure 3

Selected details of the two specimens. (A) Skull of the holotype, ventrally exposed. (B) Interpretative drawing of A. (C) Coracoid of WGSC V 1702. (D) Pectoral region of the holotype in dorsal view. (E) Pelvic and anterior caudal region of the holotype in dorsal view. (F) Pelvic and anterior caudal region of WGSC V 1702 in dorsal view. G-J. Forelimb and hindlimb of the holotype in dorsal view. K-N. Forelimb and hindlimb of WGSC V 1702 in dorsal view. Dashed line represents conjectural borderline. Shade in B represents unidentified elements. Abbreviations: ang, angular; as, astragalus; at, atlas; ax, axis; cal, calcaneum; cbr, ceratobranchial; CdR, caudal rib; ch, chevron; cl, clavicle; co, coracoid; CR, cervical rib; d, dentary; dc, distal carpal;dt, distal tarsal; DV, dorsal vertebra; ecg, ectepicondylar groove; enf, entepicondylar foramen; f, femur; fi, fibula; hu, humerus; il, ilium; in, intermedium; j, jugal; m, maxilla; mc, metacarpal; mt, metatarsal; ph, phalanx; pl, palatine; pm, premaxilla; pob/ept?, postorbital or ectopterygoid; pt, pterygoid; pu, pubis; ra, radius; rap, retroarticular process; sc, scapula; SR, sacral rib; SV, sacral vertebra; ti, tibia; ul, ulna; uln, ulnare. v, vomer. Scale bar in B-L, N = 5 mm. Scale division in A, M = 1 mm

Type species

Chusaurus xiangensis, gen. et sp. nov.


Olenekian (Early Triassic), South China.


As for type species, the only known species in this genus.

Chusaurus xiangensis, gen. et sp. nov.


WGSC (Wuhan Centre of China Geological Survey) V 1901, a nearly complete skeleton lacking some cranial and cervical vertebral elements (Fig. 2A–B).

Referred specimen

WGSC V 1702, an articulated skeleton preserving part of the cranial and incomplete postcranial regions, lacking some cervical, shoulder girdle, appendicular, and posterior caudal elements (Fig. 2C–E).

Type locality and horizon

Songshugou Village, Nanzhang County, Xiangyang City, Hubei Province, P. R. China. Member II of the Jialingjiang Formation; Spathian, late Olenekian, Early Triassic.


The generic name is derived from the Chu Kingdom in Chinese history, which dominated around the area of the fossil site. The specific epithet is derived from “Xiang”, referring to Xiangyang City where the fossil was discovered.


A small-sized pachypleurosaurid eosauropterygian with at least 17 cervical, 16 dorsal, 3 sacral, and about 40 caudal vertebrae; neck length about half the trunk length; pterygoid flanges well developed and longitudinally oriented; anteriormost caudal vertebral neural spines obviously heightened compared to presacral and sacral vertebrae; dorsal and anterior caudal ribs highly pachyostotic with expanding proximal end; posteriormost caudal ribs shortened and round; chevron well developed in the caudal region; clavicle short and stout; scapula elongate and without broadly expanded anterior portion; scapular blade is short and robust; coracoid without concave anteromedial margin; iliac blade well developed with a posterior process; little interspace between the manual and pedal digits; the proximal phalanges short and flattened; 6 maximum carpal and tarsal ossifications; manual phalangeal format 2-3-4-5-3; pedal phalangeal format 2-3-4-5-4.

Brief description

Salient morphological features are summarized here, with additional detailed description provided in the Supplemental Information. The skull is ventrally exposed in the holotype, but the preservation is rather poor (Fig. 3A–B). There are indications of anterior rostral narrowing in the premaxillary portion. Both the palatine and the pterygoid develop a lateral flange. The pterygoid is shattered along the flange, exposing the orbit in ventral view. The anteriormost dentary teeth are comparatively large, with a count of 5–6. The orbit is quite large, as in many other small pachypleurosaurs.

In the holotype, the cervical vertebral column shows an unnatural overturn between the fifth and likely the ninth vertebra (Fig. 2B). The vertebrae anterior to this overturn are ventrolaterally exposed, while more posterior elements are dorsally exposed. There are at least 17 cervical vertebrae in the holotype, 16 dorsal vertebrae, 3 sacral vertebrae, and about 40 caudal vertebrae (CdV). WGSC V 1702 shows the same count of sacral vertebrae as the holotype, whereas the presacral and caudal vertebral elements are incomplete (Fig. 3E–F). As seen in both specimens, the neural spine of the dorsal region is very low, however, the height increases in the sacral region and anteriormost caudal region distinctly, reaching its maximum height in the caudal vertebrae CdV2–10 and decreasing posteriorly (Fig. 3E–F). A similar trend in neural spine height is observed in many pachypleurosaurids [28]. The accessory articulation between the dorsal neural arches (Fig. 3D, F) that is widely found in pachypleurosaurids [29] is also present in C. xiangensis, though it is not obvious. Thickening of the curving dorsal ribs, which is indicative of pachyostosis, is obvious in both specimens, as in many other pachypleurosaurs. A groove could be recognized in WGSG V 1702 at the proximal end of the dorsal ribs, which represents the articulation facet with the corresponding vertebra (Fig. 2C, E). Chevrons are developed in the caudal region (Fig. 3E–F). The first chevron appears at CdV5 in the holotype, while in the WGSG V 1702 the chevron could be recognized from CdV8 owing to its preservation. Chevron size decreases along the caudal vertebral column, disappearing in CdV28 in the holotype.

Based on WGSC V 1702, the form of the coracoid in C. xiangensis is like that in Majiashanosaurus discocoracoidis (Fig. 3C–D) [9], and lacks the stronger waisted outline seen in Middle Triassic pachypleurosaurs like Keichousaurus hui, Dianmeisaurus gracilis, and Diandongosaurus acutidentatus [30,31,32]. The humerus is curved, with a convex anterior margin and a concave posterior margin (Fig. 3G–H, K–L), a pattern characteristic of Sauropterygia [33]. Six carpal ossifications are observed in both manus from the holotype (Fig. 3G–H), namely two large elements, the intermedium and the ulnare, and four small distal carpals, while WGSC V 1702 only has the three carpal ossifications (Fig. 3G–H, K–L). This suggests that C. xiangensis bears at least three carpal ossifications. The difference in counting might be caused by taphonomic processes that disarticulated the distal carpals of WGSC V 1702. The manual digits are deflected towards the ulnar side, and the interdigital space between digits 4 and 5 is the widest in the holotype, whereas in WGSC V 1702 all digits are tightly articulated. In general, the phalanges are stout and massive compared to other eosauropterygians.

Viewed dorsally, the ilium develops a pointed posterior process, different to known pachypleurosaurid taxa, which mostly have poorly developed dorsal blades [32, 34]. Six tarsal ossifications are preserved in both hindlimbs of the holotype: the astragalus, the calcaneum, and four distal tarsals, while the referred specimen preserves only three distal tarsals (Fig. 3I–J, M–N). Fewer carpal and tarsal elements probably suggest an earlier ontogenetic stage of WGSC V 1702 than the holotype, though taphonomic effects cannot be excluded. The six tarsal ossifications in the holotype are a relatively high number among pachypleurosaurs, as the count is usually two or three [17, 21, 32, 35, 36]. Notably, even under different preservation conditions, the interspaces between manual and pedal digits are rather limited in both specimens, suggesting a natural morphological character.

Evidence for a new taxon

The anatomical characters of the limbs and dorsal vertebrae suggest that WGSC V 1901 and WGSC V 1702 are a new taxon rather than examples of Keichousaurus yuananensis, which was the first pachypleurosaur discovered from NYF in 1965 [37]. Unfortunately, the original report of K. yuananensis is rather poor; the holotype is just a moulage without clear illustrations, and the whereabouts of the holotype are unknown. According to the original description by Young [37], K. yuananensis resembles K. hui in the plate-like ulna which is shorter than the radius, but the length and width of the two bones are equal in Chusaurus. Further, the shape of the coracoid in K. yuananensis resembles K. hui [37], with a waisted outline, while the counterpart in C. xiangensis shows a smooth anteromedial margin (Fig. 3C–D). In C. xiangensis, all the dorsal ribs have expanded proximal ends, but only the anterior dorsal ribs of K. yuananensis show this character [37]. Moreover, K. yuananensis has slender rod-like phalanges [37], differing distinctly from C. xiangensis, whose phalanges is short and broadened (Fig. 3G–N).

C. xiangensis also show differences from other known pachypleurosaurid taxa. It shows a broadened clavicle that lacks the anterolateral process in Diandongosaurus [38] and Dianmeisaurus [32], or anterolateral expansion in Dawazisaurus [8] and Dianopachysaurus [34]. In addition, many pachypleurosaurs have hourglass-shaped or rod-like slender metacarpals and metatarsals, including K. hui [29], Dactylosaurus [39], and Majishanosaurus [9], whereas C. xiangensis has stout and massive ones. C. xiangensis also has highly pachyostotic dorsal ribs without constriction near the proximal ends, differing from many other pachypleurosaurid taxa (e.g. Anarosaurus [40], Serpianosaurs [28], Honghesaurus [41], and Prosantosaurus [42]). Though poorly preserved, the snout of C. xiangensis is neither the rounded shape in Panzhousaurus [43], nor tapering like Luopingosaurus [44]. Thus, we consider that WGSC V 1901 and WGSC V 1702 are a new taxon from their combination of these morphological characters.

Chusaurus xiangensis gen. et sp. nov. is a basal pachypleurosaur

We identify Chusaurus xiangensis gen. et sp. nov. as a relatively basal member of Pachypleurosauridae based on our cladistic analysis (Fig. 4A; see Fig. S3 for the full version of the tree). Though, regrettably, the relationships within Pachypleurosauridae have not been completely resolved by our phylogenetic analysis, C. xiangensis, gen. et. sp. nov. is regarded as a basal pachypleurosaur, though the polytomy suggests its relationship with two clades, one including Keichousaurus and the other including Panzhousaurus, is currently unknown.

Fig. 4
figure 4

Phylogenetic position of the new taxon and phenograms of relative neck length in selected Triassic eosauropterygians. (A) Strict consensus of four most parsimonious trees (TL = 534, CI = 0.352, RI = 0.613). Bootstrap values ≥ 50% are labelled. Taxa are marked by different colours. (B) Phenograms of neck-trunk length ratio (Chusaurus as sister group to the clade including Panzhousaurus). (C) Phenograms of neck-trunk length ratio (Chusaurus as sister group to the clade including Keichousaurus). Clades: a. Sauropterygia; b. Placodontia; (c) Eosauropterygia; (d) Pachypleurosauridae; (e) Nothosauridae; (f) Pistosauroidea

Morphological trait analysis confirms this phylogenetic placement. The coracoid has a smooth anteromedial margin without a strongly waisted outline, a transition from the rounded coracoid of Hanosaurus hupehensis and Majiashanosaurus discocoracoidis, both of which are Early Triassic sauropterygians [9, 17] to the derived pachypleurosaurs with “coracoid strongly waisted” [30]. Meanwhile, the iliac blade of C. xiangensis, gen. et sp. nov. is well developed, whilst pachypleurosaurs from the Middle Triassic usually have a reduced or even absent iliac blade, like Serpianosaurus, Neusticosaurus, Wumengosaurus, Dianopachysaurus and Panzhousaurus [28, 34, 35, 43, 45] (see Supplemental Information, Fig. S2). More importantly, C. xiangensis already develops a longer humerus than femur, which indicates further aquatic adaptation compared to Hanosaurus [3], the most basal taxon with comparatively short forelimbs [18]. Yet the high level of pachyostosis in C. xiangensis identifies it as a shallow water, even semiaquatic animal [46].


Neck length macroevolution in Eosauropterygia

The Early Triassic was a time of rapid evolution of life in the oceans, following the devastating end-Permian mass extinction, marked especially by the appearance of new animals and new modes of life [2, 4, 24]. In particular, new benthic groups such as bivalves provided food for new predatory gastropods, malacostracans, echinoids and fishes. These in turn provided food for durophagous fishes and marine reptiles and macropredatory reptiles that fed on fishes and other reptiles [47]. Long necks likely evolved as an adaptation to snapping rapidly at the faster swimming fishes of the new ecosystems or dipping for benthic prey in murky seabed sediments [48].

Phenograms of the neck-trunk length ratio (Fig. 4B–C) show a rapid expansion in the first five million years of eosauropterygian evolution, as the ratio increases from 0.4 to 0.9. This is followed by later but slower expansion in the Middle to early Late Triassic when ratios between 0.9 and > 1 occurred for the first time. Our analyses show that the basal eosauropterygian Hanosaurus (ratio = 0.376), the basal pistosauroid Corosaurus (ratio = 0.500), and C. xiangensis (ratio = 0.480) all have relatively short necks compared to the derived taxa in their clades, and lengthening is seen independently in both pistosauroids and pachypleurosaurs.

The long-necked plesiosaurian clades, first occurring in the latest Triassic [49], evolved from Early–Middle Triassic short-necked eosauropterygian predecessors. The number of cervical and dorsal vertebrae is the key factor that influences the relative length of neck in derived plesiosaurians [13, 15], a similar pattern shared by pachypleurosaurids and basal pistosauroids. Hanosaurus (ratio = 0.376), the most basal taxon, has a relative long trunk as an ancestral body plan, with 25 dorsal and 15 cervical vertebrae [18]. The ratio increases to 0.480 in Chusaurus, from the change of vertebral number (17 cervical and 16 dorsal). When it comes to Keichousaurus (ratio = 0.980), the number of cervical vertebrae increases to 25 with 19 dorsal [29]. This is in line with the pistosauroids, as the ratio reached 0.96 by the end of the Middle Triassic, equivalent to the long neck of Keichousaurus. Though the incomplete specimens of the earliest nothosaurid Lariosaurus sanxiaensis cannot provide enough information to track the neck length, the Middle Triassic taxa share a similar neck length in the clade (Supplemental Information, Table S1).

Thus, a relatively short neck is most probably an ancestral character in Eosauropterygia, and neck elongation originated independently in Triassic pachypleurosaurid and pistosauroid clades, but the short neck reappeared in the derived pliosaurians during the Jurassic and polycotylids in the Cretaceous, in which a long head and large body evolved iteratively as adaptations to different niches [50]. The ratio varies greatly among derived plesiosaurian clades (Table S1), often deciphered as homeotic changes [13, 51]. In addition, evolutionary variability in the vertebral column appears in pachypleurosaurids as well. For example, Qianxisaurus chajiangensis [52] from the Middle Triassic Xingyi fauna developed a short neck with 18 cervical and 28 dorsal vertebrae, whose length/trunk length ratio is 0.397, even lower than in C. xiangensis, gen. et sp. nov (Fig. 4B–C).

Convergence of neck elongation among tetrapods

Extreme long necks were not unique to eosauropterygians, but occurred also in some marine archosauromorph taxa, such as Tanystropheus and Dinocephalosaurus [53, 54]. However, their neck length depends on elongation of each cervical vertebra rather than increasing the number. These two genera show various characters as adaptations for ocean life, such as viviparity in Dinocephalosaurus [55], but they did not give rise to a larger clade and were extinct before the end of the Triassic [54].

Neck elongation evolved independently numerous times among extinct marine reptiles, dinosaurs and pterosaurs, and modern mammals and birds, and is generally explained by selection pressure related to feeding strategy [12, 56, 57]. The classic explanation for neck elongation in the giraffe is as an adaptation for browsing high in the tree canopy [12]. Similarly, the long necks of the giant terrestrial sauropod dinosaurs are explained as adaptations to feed high, and at different heights, in the tree canopy [12, 56, 57].

We suggest here that variations in the neck length of eosauropterygians may reflect different feeding strategies as well: a typical short-necked pliosauromorph is regarded as the apex predator in Mesozoic marine ecosystems, while some of the long-necked plesiosaurs were more likely to be mesophagous, with their long neck enabling them to pursue smaller prey such as fast-moving fishes or benthic animals, like bivalves on the seabed [48, 50, 58]. In these cases, the long, flexible neck with many cervical vertebrae, would enable the hunter to flip its head faster in pursuit of fishes than by moving the whole body, or to search for food over a wide area on the murky seabed without constantly moving the body. As for pachypleurosaurids, they are believed to have fed on invertebrates and small fishes in shallow waters, adopting the suction strategy like aquatic chelonians [47]. Therefore, the neck elongation might have contributed to this ‘fast-strike’ feeding strategy, helping to capture the prey in an ambush.


Phylogenetic analysis

To resolve the phylogenetic position of the new specimens, a cladistic analysis was conducted using the morphological data matrix in Lin et al. [59] with the new taxon added. We excluded taxa with coding < 0.33 of characters (Majiashanosaurus and Bobosaurus). The matrix comprises 34 taxa and 148 morphological characters (see Supplemental Information). The matrix was generated using Mesquite version 3.61 [60]. The phylogenetic analysis was performed using TNT version 1.5 [61], employing a traditional search, with 1000 random addition sequences, 10 trees saved per replication and TBR swapping. Then bootstrap values were computed in PAUP*4.0a169 [62] with 100 replicates for resampling. The phylogenetic analysis recovered four most parsimonious trees, each with length 534 steps. Chusaurus xiangensis is identified as one of the most basal taxa within a monophyletic Pachypleurosauridae; Nothosauridae and Pistosauroidea are situated within a monophyletic Eusauropterygia as well, but Germanosaurus and Simosaurus are not within Nothosauridae, which is different from the finding of Lin et al. [59].

Ancestral state estimation

We estimated ancestral states for neck length/trunk length ratios in R, using the package phytools and the fastAnc and phenogram functions [63]. Our consensus topology was cropped to include just Triassic eosauropterygians, and the tree was then geologically time-calibrated using occurrence dates and the function timePaleoPhy in the R package paleotree [64]. Prior to ancestral state estimation we randomly resolved the consensus tree, which resulted in two main topologies, with Chusaurus xiangensis belonging to either of the two pachypleurosaurid sub-clades. The time-calibrated trees were plotted as phenograms reflecting the known neck:trunk length ratios for each taxon and with estimated ancestral states incorporating uncertainty through simulations. The first and last appearance data (FAD and LAD) are based on Gutarra et al. [56] (see Supplemental Information).

Data Availability

All data generated or analysed during this study are included in this published article and its online supplementary information file.

The specimens of Chusaurus xiangensis are stored in the museum of the Wuhan Center of China Geological Survey (Wuhan, Hubei Province, P. R. China) under the collection numbers WGSC V 1901 and WGSC V 1702.


  1. Kelley NP, Pyenson ND. Evolutionary innovation and ecology in marine tetrapods from the Triassic to the Anthropocene. Science. 2015;34:8aaa3716.

    Article  Google Scholar 

  2. Reeves JC, Moon BC, Benton MJ, Stubbs TL. Evolution of ecospace occupancy by mesozoic marine tetrapods. Palaeontology. 2021;64:31–49.

    Article  Google Scholar 

  3. Motani R, Vermeij GJ. Ecophysiological steps of marine adaptation in extant and extinct non-avian tetrapods. Biol Rev. 2021;96:1769–98.

    Article  PubMed  Google Scholar 

  4. Pyenson ND, Kelley NP, Parham JF. Marine tetrapod macroevolution: physical and biological drivers on 250 Ma of invasions and evolution in ocean ecosystems. Palaeogeogr Palaeoclimatol Palaeoecol. 2014;400:1–8.

    Article  Google Scholar 

  5. Kelley NP, Motani R. Trophic convergence drives morphological convergence in marine tetrapods. Biol Lett. 2015;11:20140709.

    Article  PubMed  PubMed Central  Google Scholar 

  6. Li C, Wu X-C, Rieppel O, Wang LT, Zhao LJ. An ancestral turtle from the Late Triassic of southwestern China. Nature. 2008;456:497–501.

    Article  CAS  PubMed  Google Scholar 

  7. Moon BC. A new phylogeny of ichthyosaurs (Reptilia: Diapsida). J Syst Palaeontol. 2017;17:129–55.

    Article  Google Scholar 

  8. Cheng Y-N, Wu X-C, Sato T, Shan H-Y. Dawazisaurus brevis, a new eosauropterygian from the Middle Triassic of Yunnan, China. Acta Geol Sin. 2016;90:401–24.

    Article  Google Scholar 

  9. Jiang DY, Motani R, Tintori A, Rieppel O, Chen GB, Huang JD, Zhang R, Sun ZY, Ji C. The Early Triassic eosauropterygian Majiashanosaurus discocoracoidis, gen. et sp. nov. (Reptilia, Sauropterygia), from Chaohu, Anhui Province, people’s Republic of China. J Vert Paleontol. 2014;34:1044–52.

    Article  Google Scholar 

  10. Sander PM, Griebeler EM, Klein N, Juarbe JV, Wintrich T, Revell LJ, Schmitz L. Early giant reveals faster evolution of large body size in ichthyosaurs than in cetaceans. Science. 2021;374:eabf5787.

    Article  CAS  PubMed  Google Scholar 

  11. Motani R, You H, McGowan C. Eel-like swimming in the earliest ichthyosaurs. Nature. 1996;382:347–8.

    Article  Google Scholar 

  12. Wilkinson DM, Ruxton GD. Understanding selection for long necks in different taxa. Biol Rev. 2012;87:616–30.

    Article  PubMed  Google Scholar 

  13. Soul LC, Benson RBJ. Developmental mechanisms of macroevolutionary change in the tetrapod axis: a case study of Sauropterygia. Evolution. 2017;71:1164–77.

    Article  PubMed  PubMed Central  Google Scholar 

  14. Sachs S, Kear BP, Everhart MJ. Revised vertebral count in the “longest-necked vertebrate” Elasmosaurus platyurus cope 1868, and clarification of the cervical-dorsal transition in Plesiosauria. PLoS ONE. 2013;8:e70877.

    Article  CAS  PubMed  PubMed Central  Google Scholar 

  15. Fischer V, Zverkov NG, Arkhangelsky MS, Stenshin IM, Blagovetshensky IV, Uspensky GN. A new elasmosaurid plesiosaurian from the early cretaceous of Russia marks an early attempt at neck elongation. Zool J Linn Soc. 2020;192:1167–94.

    Article  Google Scholar 

  16. Li Q, Liu J. An Early Triassic sauropterygian and associated fauna from South China provide insights into Triassic ecosystem health. Commun Biol. 2020;3:63.

    Article  PubMed  PubMed Central  Google Scholar 

  17. Cheng L. (2015). The succession of marine reptiles from the Middle to Upper Triassic of Guizhou and Yunnan provinces, southwest China. (China University of Geoscience). PhD Dissertation, pp. 34–38.

  18. Wang W, Shang Q, Cheng L, Wu X-C, Li C. Ancestral body plan and adaptive radiation of sauropterygian marine reptiles. iScience. 2022;25:105635.

    Article  PubMed  PubMed Central  Google Scholar 

  19. Case EC. A nothosaur from the Triassic of Wyoming. Univ Mich Contrib Mus Paleontol. 1936;5:1–36.

    Google Scholar 

  20. Rieppel O. Corosaurus alcovensis Case and the phylogenetic interrelationships of triassic stem-group Sauropterygia. Zool J Linn Soc. 1998;124:1–41.

    Article  Google Scholar 

  21. Storrs G. Anatomy and relationships of Corosaurus alcovensis (Diapsida: Sauropterygia) and the Triassic Alcova Limestone of Wyoming. Bull Peabody Mus Natl Hist. 1991;44:1–151.

    Google Scholar 

  22. Yan C, Li J, Cheng L, Zhao B, Zou Y, Niu D, Chen G, Fang Z. Strata characteristics of the Early Triassic Nanzhang-Yuan’an Fauna in Western Hubei Province. Earth Sci. 2021;46:122–35.

    Google Scholar 

  23. Cheng L, Yan C, Chen X, Zeng X, Motani R. Characteristics and significance of Nanzhang-Yuanan Fauna, Hubei Province. Geol China. 2015;42:676–84.

    Google Scholar 

  24. Benton BMJ, Zhang Q, Hu S, Chen Z-Q, Wen W, Liu J, Huang J, Zhou C, Xie T, Tong J, et al. Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the Permo-Triassic mass extinction (reprinted from Earth-Science Reviews, vol 125, pg 199–243, 2013). Earth-Sci Rev. 2014;137:85–128.

    Article  Google Scholar 

  25. Owen R. Palaeontology, or, a systematic summary of extinct animals and their geological relations. London: and C. Black; 1860. p. 435.

    Book  Google Scholar 

  26. Rieppel O. Osteology of Simosaurus gaillardoti and the relationships of stem-group Sauropterygia. Fieldiana: Geol new Ser. 1994;28:1–85.

    Google Scholar 

  27. Nopcsa F. Palaeontological notes on reptiles. Geol Hung Ser Palaeontol. 1928;1:3–84.

    Google Scholar 

  28. Rieppel O. A new pachypleurosaur (Reptilia: Sauropterygia) from the Middle Triassic of Monte San Giorgio, Switzerland. Philos Trans R Soc Lond Ser B-Biol. 1989;323:1–73.

    Article  Google Scholar 

  29. Lin K, Rieppel O. Functional morphology and phylogeny of Keichousaurus hui (Sauropterygia, Reptilia). Fieldiana: Geol new Ser. 1998;39:1–35.

    CAS  Google Scholar 

  30. Xue YF, Jiang DY, Motani R, Rieppel O, Sun YL. New information on sexual dimorphism and allometric growth in Keichousaurus hui, a pachypleurosaur from the Middle Triassic of Guizhou, South China. Acta Palaeontol Pol. 2013;60:681–7.

    Article  Google Scholar 

  31. Liu XQ, Lin WB, Rieppel O, Sun ZY, Li ZG, Hao L, Jiang DY. A new specimen of Diandongosaurus acutidentatus (Sauropterygia) from the Middle Triassic of Yunnan, China. Vert PalAsiat. 2015;53:1–5.

    Google Scholar 

  32. Shang Q, Li C, Wu X. (2017). New information on Dianmeisaurus gracilis Shang & Li, 2015. Vert. PalAsiat. 55, 145–161.

  33. Rieppel O. Sauropterygia I: Placodontia, Pachypleurosauria, Nothosauroidea, Pistosauroidea. Encyclopedia of Paleoherpetology. (Dr Friedrich Pfeil Publishing). 2000;12:1–134.

    Google Scholar 

  34. Liu J, Rieppel O, Jiang DY, Aitchison JC, Motani R, Zhang QY, Zhou CY, Sun YY. A new pachypleurosaur (Reptilia: Sauropterygia) from the lower Middle Triassic of southwestern China and the phylogenetic relationships of chinese pachypleurosaurs. J Vert Paleontol. 2011;31:292–302.

    Article  Google Scholar 

  35. Wu X-C, Cheng Y-N, Li C, Zhao L-J, Sato T. New information on Wumengosaurus delicatomandibularis Jiang et al., 2008 (Diapsida: Sauropterygia), with a revision of the osteology and phylogeny of the taxon. J Vert Paleontol. 2011;31:70–83.

    Article  Google Scholar 

  36. Liu QL, Yang TL, Cheng L, Benton MJ, Moon BC, Yan CB, An ZH, Tian L. An injured pachypleurosaur (Diapsida: Sauropterygia) from the Middle Triassic Luoping Biota indicating predation pressure in the Mesozoic. Sci Rep. 2021;11:21818.

    Article  CAS  PubMed  PubMed Central  Google Scholar 

  37. Young C-C. On the new nothosaurs from Hupeh and Kweichou, China. Vert PalAsiat. 1965;9:315–67.

    Google Scholar 

  38. Shang Q, Wu XC, Li C. A new eosauropterygian from Middle Triassic of eastern Yunnan Province, southwestern China. Vet PalAsiat. 2011;49:155–71.

    Google Scholar 

  39. Sues HD, Carroll RL. The pachypleurosaurid Dactylosaurus schroederi (Diapsida: Sauropterygia). Can J Earth Sci. 1985;22:1602–8.

    Article  Google Scholar 

  40. Klein N. Postcranial morphology and growth of the pachypleurosaur Anarosaurus heterodontus (Sauropterygia) from the Lower Muschelkalk of Winterswijk, the Netherlands. Paläont Z. 2012;86:389–408.

    Article  Google Scholar 

  41. Xu G-H, Ren Y, Zhao L-J, Liao J-L, Feng D-H. A long-tailed marine reptile from China provides new insights into the Middle Triassic pachypleurosaur radiation. Sci Rep. 2022;12:7396.

    Article  CAS  PubMed  PubMed Central  Google Scholar 

  42. Klein N, Furrer H, Ehrbar I, Torres Ladeira M, Richter H, Scheyer TM. A new pachypleurosaur from the early Ladinian Prosanto Formation in the Eastern Alps of Switzerland. Swiss J Palaeontol. 2022;141:12.

    Article  PubMed  PubMed Central  Google Scholar 

  43. Jiang DY, Lin WB, Rieppel O, Motani R, Sun ZY. (2019). A new Anisian (Middle Triassic) eosauropterygian (Reptilia, Sauropterygia) from Panzhou, Guizhou Province, China. J Vert Paleontol 38, e1480113.

  44. Xu G-H, Shang Q-H, Wang W, Ren Y, Lei H, Liao JL, Zhao LJ, Li C. A new long-snouted marine reptile from the Middle Triassic of China illuminates pachypleurosauroid evolution. Sci Rep. 2023;13.

  45. Sander PM. The pachypleurosaurids (Reptilia: Nothosauria) from the Middle Triassic of Monte San Giorgio (Switzerland) with the description of a new species. Philos Trans R Soc Lond Ser B-Biol. 1989;325:561–666.

    Article  CAS  Google Scholar 

  46. Gutarra S, Rahman IA. The locomotion of extinct secondarily aquatic tetrapods. Biol Rev. 2021;97:67–98.

    Article  PubMed  Google Scholar 

  47. Rieppel O. Feeding mechanics in Triassic stem-group sauropterygians: the anatomy of a successful invasion of Mesozoic Seas. Zool J Lin Soc. 2002;135:33–63.

    Article  Google Scholar 

  48. Noè L, Taylor M, Gómez-Pérez M. An integrated approach to understanding the role of the long neck in plesiosaurs. Acta Palaeontol Pol. 2017;62:137–62.

    Article  Google Scholar 

  49. Wintrich T, Hayashi S, Houssaye A, Nakajima Y, Sander PM. A Triassic plesiosaurian skeleton and bone histology inform on evolution of a unique body plan. Sci Adv 2017;3, e1701144.

  50. Fischer V, Benson RBJ, Zverkov NG, Soul LC, Arkhangelsky MS, Lambert O, Stenshin IM, Uspensky GN, Druckenmiller PS. Plasticity and convergence in the evolution of short-necked plesiosaurs. Curr Biol. 2017;27:1667–76.

    Article  CAS  PubMed  Google Scholar 

  51. Müller J, Scheyer TM, Head JJ, Barrett PM, Werneburg I, Ericson PGP, Pol D, Sánchez-Villagra MR. Homeotic effects, somitogenesis and the evolution of vertebral numbers in recent and fossil amniotes. Proc Natl Acad Sci. 2010;107:2118–23.

    Article  PubMed  PubMed Central  Google Scholar 

  52. Cheng Y-N, Wu X-C, Sato T, Shan H-Y. A new eosauropterygian (Diapsida, Sauropterygia) from the Triassic of China. J Vert Paleontol. 2012;32:1335–49.

    Article  Google Scholar 

  53. Li C. First record of protorosaurid reptile (Order Protorosauria) from the Middle Triassic of China. Acta Geol Sin. 2003;77:419–23.

    Google Scholar 

  54. Spiekman SNF, Fraser NC, Scheyer TM. A new phylogenetic hypothesis of Tanystropheidae (Diapsida, Archosauromorpha) and other “protorosaurs”, and its implications for the early evolution of stem archosaurs. PeerJ. 2021;9: e11143.

    Article  PubMed  PubMed Central  Google Scholar 

  55. Liu J, Organ CL, Benton MJ, Brandley MC, Aitchison JC. Live birth in an archosauromorph reptile. Nat Com. 2017;8:14445.

    Article  CAS  Google Scholar 

  56. Gutarra S, Stubbs TL, Moon BC, Palmer C, Benton MJ. Large size in aquatic tetrapods compensates for high drag caused by extreme body proportions. Commun Biol. 2022;5:380.

    Article  PubMed  PubMed Central  Google Scholar 

  57. Taylor MP, Wedel MJ, Rauhut OWM, Remes K, Fechner R, Cladera G, Puerta P. (2005). Discovery of a short-necked sauropod dinosaur from the Late Jurassic period of Patagonia. Nature 435, 670–672. 10.1038/nature03623.

  58. McHenry CR, Cook AG, Wroe S. Bottom-feeding plesiosaurs. Science. 2005;310:75.

    Article  CAS  PubMed  Google Scholar 

  59. Lin W-B, Jiang D-Y, Rieppel O, Motani R, Tintori A, Sun Z-Y, Zhou M. Panzhousaurus Rotundirostris Jiang, 2019 (Diapsida: Sauropterygia) and the recovery of the monophyly of Pachypleurosauridae. J. Vert. Paleontol., 2021;41, e1901730.

  60. Maddison WP, Maddison DR. (2019) Mesquite: a modular system for evolutionary analysis. 3.61.

  61. Goloboff PA, Catalano SA. TNT version 1.5, including a full implementation of phylogenetic morphometrics. Cladistics. 2016;32:221–38.

    Article  PubMed  Google Scholar 

  62. Swofford DL. (2021) PAUP*. Phylogenetic Analysis Unsing Parsimony (*and Other Methods). Version 4a169.

  63. Revell LJ. Phytools: an R package for phylogenetic comparative biology (and other things). Methods Ecol Evol. 2012;3:217–23.

    Article  Google Scholar 

  64. Bapst DW. Paleotree: an R package for paleontological and phylogenetic analyses of evolution. Methods Ecol Evol. 2012;3:803–7.

    Article  Google Scholar 

Download references


We thank Mr. Dong-Yi Niu for excavation and specimen preparation.


We are grateful for support from Grant DD20230006 from the China Geological Survey, Grant nos. 41972014, 42030513 and 42272361 from the National Natural Science Foundation of China, and Grant NE/P013724/1 from the Natural Environment Research Council of UK, European Research Council Grant 788203 (INNOVATION).

Author information

Authors and Affiliations



L.C. leads the project on NYF with assists of C.Y. L.C. and L.T. design the study. Q.L., B.M. and T.S. conduct and write the description, measurement and cladistic analyses. M.B., L.C. and L.T. improve the manuscript with the efforts of all authors.

Corresponding authors

Correspondence to Long Cheng or Li Tian.

Ethics declarations

Competing interests

The authors declare no competing interests.

Ethic approval and consent to participate

No live animals involved in this study.

Consent for publication


Additional information

Publisher’s Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Supplementary Material 1

Rights and permissions

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit The Creative Commons Public Domain Dedication waiver ( applies to the data made available in this article, unless otherwise stated in a credit line to the data.

Reprints and Permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Liu, QL., Cheng, L., Stubbs, T.L. et al. Rapid neck elongation in Sauropterygia (Reptilia: Diapsida) revealed by a new basal pachypleurosaur from the Lower Triassic of China. BMC Ecol Evo 23, 44 (2023).

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI:


  • Marine reptile
  • Eosauropterygia
  • Mesozoic
  • Body plan
  • Nanzhang-Yuan’an Fauna