The origin of hadrosaurid dinosaurs is far from clear, mainly due to the paucity of their early Late Cretaceous close relatives. Compared to numerous Early Cretaceous basal hadrosauroids, which are mainly from Eastern Asia, only six early Late Cretaceous (pre-Campanian) basal hadrosauroids have been found: three from Asia and three from North America.
Here we describe a new hadrosauroid dinosaur, Yunganglong datongensis gen. et sp. nov., from the early Late Cretaceous Zhumapu Formation of Shanxi Province in northern China. The new taxon is represented by an associated but disarticulated partial adult skeleton including the caudodorsal part of the skull. Cladistic analysis and comparative studies show that Yunganglong represents one of the most basal Late Cretaceous hadrosauroids and is diagnosed by a unique combination of features in its skull and femur.
The discovery of Yunganglong adds another record of basal Hadrosauroidea in the early Late Cretaceous, and helps to elucidate the origin and evolution of Hadrosauridae.
Citation: Wang R-F, You H-L, Xu S-C, Wang S-Z, Yi J, et al. (2013) A New Hadrosauroid Dinosaur from the Early Late Cretaceous of Shanxi Province, China. PLoS ONE 8(10): e77058. doi:10.1371/journal.pone.0077058
Editor: David C. Evans, Royal Ontario Museum, Canada
Received: January 14, 2013; Accepted: August 25, 2013; Published: October 18, 2013
Copyright: © 2013 Wang et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: Funding was provided by the National Natural Science Foundation of China, the Hundred Talents Project of the Chinese Academy of Sciences, and the Department of Land and Resources of Shanxi Province. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Hadrosauroids were facultative bipedal dinosaurs that dominated Cretaceous Laurasian megaherbivorous niches , . During the Late Cretaceous, they gave rise to hadrosaurid dinosaurs, which are characterized by duck-like bills and complex grinding dentitions that rival those of horses and bovids . However, the origin of hadrosaurids is far from clear, mainly due to the paucity of early Late Cretaceous close relatives. Basal hadrosauroids are mainly known from the Early Cretaceous of Eastern Asia, and especially northern China . Until now, only six pre-Campanian Late Cretaceous basal hadrosauroids have been reported: three from Asia (Shuangmiaosaurus gilmorei, Levnesovia transoxiana, and Nanyangosaurus zhugeii, see discussion section below on its age) and three from North America (Eolambia caroljonesa, Protohadros byrdi, and Jeyawati rugoculus) –. Therefore, the discovery of new early Late Cretaceous basal hadrosauroids has important phylogenetic and paleobiogeographical significance and can help elucidate the evolution of hadrosauroids, especially the origin of hadrosaurids.
Definitions of relevant taxa follow Sereno : Hadrosauriformes is the least inclusive clade containing Iguanodon bernissartensis Boulenger in Beneden 1881 and Parasaurolophus walkeri Parks 1922, Hadrosauroidea is the most inclusive taxon containing Parasaurolophus walkeri Parks 1922 but not Iguanodon bernissartensis Boulenger in Beneden 1881, and Hadrosauridae is the least inclusive taxon containing Saurolophus osborni Brown 1912 and Parasaurolophus walkeri Parks 1922 and including Hadrosaurus foulkii Leidy 1858. The term “basal hadrosauroids” here refers to all members of non-Hadrosauridae Hadrosauroidea.
In 1958, C. C. Young (Z.-J. Yang)  reported the first dinosaur record in Shanxi Province of northern China. These remains were recovered from two localities in Zuoyun County of northern Shanxi (Fig. 1). The material is fragmentary, and Young did not name any new dinosaur species; rather, he assigned some of them to existing taxa . The first locality (Xinyaogou) yielded theropod (cf. Velociraptor mongoliensis, represented by a single tooth), ceratopsian (cf. Microceratops gobiensis, represented by two partial mandibles, three isolated teeth, several vertebrae, one humerus, one femur, and other fragmentary specimens), and hadrosauroid (Bactrosaurus johnsoni, represented by two isolated teeth, some vertebrae including a series of 25 caudals, one rib, one right humerus, and several manual and pedal bones). The second locality (Zhanmagou) yielded Sauropoda indet. (represented by one partial dorsal and one fragmentary caudal vertebrae) and Allosauridae indet. (represented by one caudal, one partial right scapula, two distal ends of ischia, one proximal end of right tibia, one partial right fibula, one left metatarsal, and one pedal phalanx). Based on the different dinosaur components, Young considered the Xinyaogou dinosaur assemblage to be Late Cretaceous in age and the Zhanmagou dinosaur assemblage to be Early Cretaceous or earlier in age.
(A)-Shanxi Province in China. (B)-Zuoyun County in Shanxi Province.
More than half a century later, the Department of Land and Resources of Shanxi Province initiated a project to find dinosaurs for the Shanxi Museum of Geology (SXMG) now being constructed. In 2011 and 2012, a number of dinosaur localities were discovered and excavated in Zuoyun County. Preliminary observations indicate the existence of hadrosauroid, ankylosaur, and ceratopsian remains from the early Late Cretaceous Zhumapu Formation, and stegosaur and sauropod remains from the late Early Cretaceous Zuoyun Formation. In this paper, a partial associated hadrosauroid skeleton from 2011 Locality 7 (SXMG V 00001, field number ZY007) is described and diagnosed as a new genus and species.
No permits were required for this study, which complied with all relevant regulations. We obtained permission from the Shanxi Museum of Geological and Mineral Science and Technology to access the collections. The specimens were discovered and excavated by the crew (including co-authors of this study) of the Shanxi Museum of Geological and Mineral Science and Technology.
The electronic edition of this article conforms to the requirements of the amended International Code of Zoological Nomenclature, and hence the new names contained herein are available under that Code from the electronic edition of this article. This published work and the nomenclatural acts it contains have been registered in ZooBank, the online registration system for the ICZN. The ZooBank LSIDs (Life Science Identifiers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefix “http://zoobank.org/”. The LSID for this publication is: urn:lsid:zoobank.org:pub:26AD8279-F3F8-4A6F-A16F-B163BB54F7EE.The electronic edition of this work was published in a journal with an ISSN, and has been archived and is available from the following digital repositories: PubMed Central, LOCKSS.
Numerous cladistic analyses have been conducted in order to elucidate the phylogenetic relationships among hadrosauroids in recent years; for example, at least four papers were published in 2012 , –. However, many of these focused on the phylogeny of Hadrosauridae or its subclades; for example, lambeosaurine was the subject of , while saurolophine was the subject of . Although McDonald  and McDonald et al.  included most of the basal hadrosauroids, the results were poorly resolved and most taxa were clustered in a polytomy in the strict consensus tree. Thus, the phylogeny presented in  is based on a maximum agreement subtree that entailed the deletion of 30 operational taxonomic unites, while that of  is based on Adams consensus tree.
In order to assess the phylogenetic position of the new taxon, we performed a cladistic analysis based on Sues and Averianov . This data matrix has been used by one of the authors (YHL) on the study of Jintasaurus . In the current analysis Nanyangosaurus, Shuangmiaosaurus, and Yunganglong were added to the matrix, to increase its taxonomic representation. This new data matrix was compiled in Mesquite 2.72 , and consists of 138 characters and 38 ornithopod taxa (Supporting Information S1). Two character codings were modified: character 37 (Postorbital, length of squamosal process; 0: short, postorbital-squamosal joint reaches point at mid-length of supratemporal fenestra; 1: long, postorbital-squamosal joint near level of posterior border of supratemporal fenestra) is changed from ‘0’ to ‘?’ for Protohadros because the character state is not clear based on the original descriptive paper (i. e., the squamosal process of the postorbital is partially present)  and a new character state (coronoid process orientation: 2, inclined caudally) is added to reflect this unique feature in Shuangmiaosaurus . The data matrix was analyzed by a Traditional search in TNT 1.1  with 100 replications of Wagner trees and tree bisection reconnection (TBR) branch swapping (with 100 trees to save per replicate). All characters were unordered and equally weighted. Hypsilophodon was selected as outgroup, as in the original analysis .
Dinosauria Owen, 1842 
Ornithischia Seeley, 1887 
Ornithopoda Marsh, 1881 
Yunganglong gen. nov.
Yunganglong datongensis sp. nov.
SXMG V 00001 (Shanxi Museum of Geology, Taiyuan, Shanxi Province, China). Associated but disarticulated partial skeleton of one individual, including the caudodorsal part of the skull (ZY007-37 and -38, separated along the floor of the braincase), two cervical vertebrae (-40 and -41), partial dorsal neural arch and neural processes (-36), two caudals (-27, proximal; -19, middle), distal portions of both ischia (-11, left; -12, right), distal end of left femur (-32), proximal portion of right tibia (-1), and distal portion of left tibia with astragalus (-2). See Table 1 for measurements.
The generic name “Yungang” is after “Yungang Grottoes”, a UNESCO World Heritage built in the 5th and 6th centuries about 50 km east of the fossil locality; “long” means “dragon” in Chinese. The specific name reflects “Datong”, the city in which the locality is situated.
Locality and horizon.
In the vicinity of Zuoyun County, Datong City, Shanxi Province, P. R. China. Lower part of Zhumapu Formation, lower Upper Cretaceous .
In the Zuoyun area, the Zhumapu Formation reaches 722 m in thickness. It overlies the Lower Cretaceous Zuoyun Formation with a parallel unconformity relationship and is covered by Tertiary basalts. The age of the Zhumapu Formation is determined by biostratigraphic correlations, including evidences from angiosperm plants, spores and pollens, ostracodes, and bivalves . No radiometric-based age has been obtained for this formation.
Differential diagnosis (for genus and species by monotypy).
Basal hadrosauroid with the following unique combination of four character states: 1) caudal surface of the supraoccipital inclined steeply forward at approximately 450 (present in Yunganglong and more advanced taxa, but nearly vertical in Jintasaurus and less derived Hadrosauriformes); 2) caudolaterally extended horizontal portion of the paroccipital process and accompanying squamosal (present in Yunganglong and more advanced taxa, but laterally extended in Jintasaurus and less derived Hadrosauriformes); 3) pendent portion of the paroccipital process does not curve cranially (observed in Yunganglong and Jintasaurus; the pendant portion does curve cranially in Bactrosaurus and more advanced taxa); 4) intercondylar extensor groove of the femur deep, U-shaped, partially enclosed by expansion of medial and lateral condyles (present in Yunganglong and less derived Hadrosauriformes, but canal fully enclosed by fusion of lateral and medial condyles in Nanyangosaurus and more advanced taxa).
The caudodorsal part of the skull is preserved, including the parietal, paroccipital processes, and the almost complete braincase (Figs. 2, 3). In occipital view, the skull is transversely wide and dorsoventrally low, with the width between the pendent paroccipital processes of 37.0 cm and the height from the apex of the supraoccipital to the ventral edge of the occipital condyle of 17.5 cm.
(A)-Right lateral view. (B)-Dorsal view. (C)-Caudal view. Scale bar = 10 cm.
(A)-Right lateral view. (B)-Dorsal view. (C)-Caudal view. Scale bar = 10 cm. bo = basioccipital, bs = basisphenoid, eo = exoccipital, ls = laterosphenoid, oo = opisthotic, pa = parietal, po = prootic, pop = paroccipital process, ps = parasphenoid, so = supraoccipital, sq = squamosal.
In dorsal view, the preserved parietal length is 14.0 cm, and the narrowest transverse width at the mid-length of the parietals is 6.0 cm. There is a low sagittal crest along the midline of the preserved parietal portion, but whether or not it continued caudally to form a tall nuchal crest as in Levnesovia  and Jintasaurus  is not clear.
The caudal surface of the supraoccipital is steeply inclined rostrally; the bone is nearly horizontal. In occipital view, the dorsal portion of the supraoccipital consists of a median knob-like dorsal process and two dorsolateral projections. Ventrally, the supraoccipital is separated from the exoccipitals by a slit-like transverse groove on the latter, which continues laterally underneath the opisthotics. The ventral edge of this groove forms a strong horizontal ridge, which borders the foramen magnum dorsally. The lateral sides of the foramen magnum are enclosed by the exoccipitals, which bear a knob-like ventral corner on each side. The exoccipitals also meet along the floor of the foramen magnum.
The paroccipital processes strongly bend caudolaterally, enclosing an arc of around 100 degrees in dorsal view and thereby, increasing the length of skull. The longitudinal distance from the caudal end of the parietal to an imaginary point on the midline between the caudal ends of the paroccipital processes is 12.0 cm, almost the same length as the parietal. In lateral view, the straight and vertical pendent portions of the paroccipital processes are set caudal to the occipital condyle, with their ventral tips slightly below the ventral edge of the occipital condyle.
The occipital condyle is formed by the basioccipital and describes a crescent in caudal view. Its caudal surface is vertical and slightly bulging, while its ventral surface is strongly convex. The surface is generally smooth, and one groove is visible on the left half of the caudal surface (Fig. 2C). A short neck divides the occipital condyle and the basal tubera. The basal tubera seem to be formed more by the basisphenoid than by the basioccipital, and those two bones are well fused to each other. The basal tubera are separated by a longitudinal median recess, and a delicate ridge appears along the midline. A round craniolaterally facing fossa exists on the cranial surface of each side of the basal tubera.
The braincase is broken along a line through the exits of the cranial nerves. The positions of these cranial nerve exits are conventional compared to other hadrosauroids, and generally correspond to those in closely related taxa, such as Levnesovia. Three foramina pierce the fused opisthotic and exoccipital laterally for cranial nerves X-XII. The rostral two foramina for cranial nerves X and XI are merged, giving a larger appearance than the caudal one for cranial nerve XII. The auditory recess, which includes the fenestra vestibule (fenestra ovalis of ), exit for cranial nerve IX, and foramen for the jugular vein, is bounded by the fused basisphenoid and parasphenoid ventrally, the prootic dorsally, and the fused opisthotic and exoccipital caudally. Rostral to the auditory recess is the large, round trigeminal foramen.
Two cervicals (ZY007-40, -41) are preserved, and ZY007-40 is almost complete (Fig. 4). The centrum is strongly opisthocoelous, with the round cranial articular condyle more than half the length of the centrum. The cranial-most protruding point is above the midlevel of the centrum. The caudal articular surface is deeply concave and elliptical in caudal view, being wider than high. The lateral side of the centrum is slightly higher than long, and is divided by a midlevel ridge into dorsal and ventral depressions. The large parapophysis occupies the cranial half of this ridge. The ventral surface is slightly convex, especially at the caudal half. The neural canal is large and round, about half the height of the centrum. The prezygapophysis starts from the dorsolateral corner of the cranial half of the neural arch and does not protrude beyond the cranial edge of the articular condyle. The dorsomedially facing smooth articular facet is large, oval, and flat. The short stem of the prezygapophysis also gives rise to the diapophysis, which projects caudoventrolaterally. The robust postzygapophysis is directed more caudally than laterally, with its entire articular facet beyond the caudal edge of the centrum. The neural spine is not well preserved, but seems to have been delicate.
(A)-Cranial view. (B)-Right lateral view. (C)-Dorsal view. (D)-Caudal view. (E)-Left lateral view. (F)-Ventral view. Abbreviations: dia, diapophysis; par, parapophysis; poz, postzygapophysis; prz, prezygapophysis. Scale bar = 6 cm.
A partial dorsal neural arch and neural spine are preserved (ZY007-36) (Fig. 5A, B). The diapophysis projects dorsolaterally and slightly caudally and has a triangular cross section. The long, oval, and flat postzygapophysis articular facet faces lateroventrally. Only the basal portion of the neural spine is preserved; it is plate-like and thin transversely.
(A, B)-Partial dorsal neural arch and neural spine in (A) dorsal and (B) caudal views. (C, E)-Proximal caudal in (C) left lateral and (E) caudal views. (D, F)-Middle caudal in (D) left lateral and (F) caudal views. Abbreviations: chf, chevron facet; dia, diapophysis; ns, neural spine; poz, postzygapophysis; prz, prezygapophysis; transverse process, trp. Scale bar = 6 cm.
One proximal (ZY007-27) (Fig. 5 C, E) and one middle (ZY007-19) (Fig. 5 D, F) caudal are preserved. The proximal caudal's centrum is narrow and slightly amphicoelous. The articular surfaces are elliptical with relatively narrow ventral ends. The partial right transverse process starts at the neurocentral junction and projects laterally. The neural spine is tall, almost double the height of the centrum. The cross section of the neural spine is rectangular, with the transverse width less than half the longitudinal length. The tip of the neural spine expands slightly. The centrum of the middle caudal is dorsoventrally lower but proximodistally longer than that of the proximal caudal, with hexagonal articular surfaces. The transverse process is not present, and the neural spine projects caudodorsally.
The distal portions of both ischia are preserved (ZY007-11 left, -12 right) (Fig. 6). The preserved shaft is triangular in cross section, with a flat medial surface to contact its counterpart. This flat surface continues to the distal end. The craniolateral surface bears a shallow longitudinal depression, while the caudolateral surface is flat. The distal end slightly expands craniolaterally to form a hemispherical expansion. The expanded distal end is about double the width of the shaft diameter.
(A, C)-Distal portion of left ischium in (A) medial and (C) cranial views. (B, D)-Distal portion of right ischium in (C) medial and slightly caudal and (D) distal and slightly dorsal views. Abbreviation: cede, cranially expanded distal end. Scale bar = 10 cm.
The distal end of the left femur is preserved (ZY007-32). The cross section of the preserved proximal end of the shaft is elliptical, and its transverse width is twice its craniocaudal width. The intercondylar extensor groove of the femur is deep, U-shaped, partially enclosed by expansion of medial and lateral condyles. The medial condyle is slightly larger than the lateral. The medial surface of the medial condyle is flat, while the lateral surface of the lateral condyle bears a stout longitudinal ridge. The caudal condyles are strongly developed, fan-shaped, and longer proximodistally than craniocaudally in lateral and medial views. In caudal view, the medial condyle is more expanded than the lateral, about three times wider transversely. On the lateral surface of the medial condyle, a small longitudinal ridge develops close to the shaft (Fig. 7D).
(A)-Cranial view. (B)- Caudal view. (C)-Proximal view. (D)-Distal view (E)-Lateral view. (F)-Medial view. Abbreviations: ieg, intercondylar extensor groove; ifg, intercondylar flexor groove; lc, lateral condyle; mc, medial condyle. Scale bar = 10 cm.
The proximal portion of the right tibia (ZY007-1) (Fig. 8 A–F) and the distal portion of the left tibia with astragalus (ZY007-2) (Fig. 8 G–K) are preserved. The cnemial crest is well developed and protrudes craniolaterally. Two laterally-projecting condyles exist on the caudal half of the proximal end. The midshaft is ovate in cross section. The distal end of the left tibia is articulated with the astragalus. In cranial view, the astragalus is triangular, with a clear short ascending process. In caudal view, the astragalus is also triangular, with a delicate ascending process at its proximolateral corner.
(A–F)-Proximal portion of right tibia in (A) media, (B) cranial, (C) lateral, (D) caudal, (E) proximal, and (F) distal views. (G–K)-Distal portion of left tibia with astragalus in (G) cranial, (H) caudal, (I) medial, (J) lateral, and (K) distal views. Abbreviations: as, astragalus; cc, cnemial crest; cf, concavity for articulation of distal end of fibula; cmc, caudomedial condyle; lc, lateral condyle; lm, lateral malleolus; mm, medial malleolus. Scale bar = 10 cm.
Phylogenetic analysis recovered 303 MPTs (most parsimonious trees) of 294 steps, with a CI (consistency index) of 0.534 and a RI (retention index) of 0.858. The strict consensus tree recovered Yunganglong, Jintasaurus, Protohadros, Nanyangosaurus, Shuangmiaosaurus, Levnesovia, Bactrosaurus, Tanius, and Telmatosaurus in an unresolved polytomy between Probactrosaurus and (Aralosaurus+Hadrosauridae) with poor bootstrap frequencies and bremer supports (Fig. 9).
Bremer supports no less than 1 and bootstrap frequencies more than 50 are indicated above and below relevant branches, respectively. “•” represents node-based definition, and “→” represents branch-based definition.
In the strict consensus tree, the Hadrosauroidea clade is supported by 7 unambiguous synapomorphies (40, parietal sagittal crest long, more than 2/3 length of parietal; 46, antorbital fenestra external opening absent; 57, lacrimal-nasal contact absent; 74, length of basipterygoid processes extending well below level of ventral border of occipital condyle; 75, occipital condyle articular surface vertical; 103, cervical zygapophyseal peduncles on arches elevated, extending well above level of neural canal, zygapophyses long and dorsally arched; 114, humeral distal condyles compressed mediolaterally, flaring little from shaft of humerus), the (Probactrosaurus+more advanced taxa) clade is supported by 4 unambiguous synapomorphies (55, line of alveolar foramina on medial side of maxilla located dorsal to mid-height of maxilla; 83, dentary alveolar trough narrow parallel-sided grooves; 94, at least 2, and often 3, teeth in vertical series contributing to occlusal surface per tooth position; 96, ornamentation on labial surface of maxillary teeth absence of all but primary carina), the clade above Probactrosaurus is strongly supported by 19 unambiguous synapomorphies (37, squamosal process of postorbital long, postorbital-squamosal joint near level of posterior border of supratemporal fenestra; 38, parietal long, length/minimum width ratio greater than 2; 51, jugal process of maxilla reduced to short projection but retaining a distinct facet; 52, location of apex at or anterior to center of maxilla in lateral exposure; 56, ectopterygoid-jugal contact absent, palatine-jugal contact enhanced; 65, quadratojugal foramen absent; 66, well-defined paraquadrate notch of quadrate absent, reduced to poorly defined embayment of quadrate; 72, paroccipital process and accompanying squamosal curved anteriorly; 77, predentary gracile and shovel-shaped, straight to gently rounded anterior margin, numerous nutrient foramina across entire anterior margin, rounded, triangular denticles project anteriorly and fit into a continuous transverse slot on underside of premaxilla; 89, surangular foramen absent; 93, 3 or more replacement teeth per tooth position; 99, dentary tooth crown dominated by on primary ridge on lingual surface, secondary ridges faint if present; 101, 12–13 cervical vertebrae; 106, scapular proximal end dorsoventrally narrow, no wider than distal portion of scapula, acromion process projects horizontally, anteroventral corner notched, articulation restricted; 118, manual digit I absent; 128, pubis obturator foramen fully open, tubercle absent; 131, femoral distal condyles expanded anteriorly, with anterior ends meeting or fusing together and enclosing extensor tunnel; 132, tibia cnemial crest extending on diaphysis; 137, pedal unguals dorsoventrally flattened and broadened, hoof-like), the (Aralosaurus+Hadrosauridae) clade is supported by 8 unambiguous synapomorphies (41, squamosals approaching midline, separated by narrow band of parietal; 54, ectopterygoid ridge of maxilla well developed into lateral and well demarcated border continuous along posterior region of maxilla; 58, jugal expanded dorsoventrally in front of orbit, lacrimal pushed dorsally to lie completely above the level of the maxilla, jugal forms lower portion of orbital rim; 60, free ventral flange of jugal present, jugal dorsoventrally constricted beneath infratemporal fenestra to set off flange anterior to constriction; 61, ventral flange of jugal rounded or lobate; 62, ratio of depth of jugal at constriction below infratemporal fenestra to length of free flange on jugal small, 0.70–0.90; 95, maxillary tooth crown elongate and lanceolate, height/width ratio at least 2.5 at center of tooth row; 98, apex of dentary teeth central, tooth straight and nearly symmetrical), and the Hadrosauridae clade is supported by 5 unambiguous synapomorphies (45, posteroventral surface of squamosal forming deep, nearly vertical, well-exposed face in posterior view; 63, jugal contributed to infratemporal fenestra, acute angle between postorbital bar and jugular bar; 71, ventrolateral corner of supraoccipital inset into exoccipital so that supraoccipital is “locked” between exoccipitals; 92, greater than 32 tooth positions in dentary and maxillary tooth rows; 112, deltopectoral crest of humerus extends at least to midshaft or longer) (Supporting Information S2).
The 50% majority rule tree further resolved (Yunganglong, Jintasaurus, Protohadros, Nanyangosaurus, and Shuangmiaosaurus) as more basal than a trichotomy of Tanius, (Levnesovia+Bactrosaurus), and (Telmatosaurus+more advanced taxa). Mapping synapomorphies onto the majority rule tree showed that the clade (Yunganglong, Jintasaurus, Protohadros, Nanyangosaurus, Shuangmiaosaurus+more advanced taxa) is supported by 9 unambiguous synapomorphies (37, squamosal process of postorbital long, postorbital-squamosal joint near level of posterior border of supratemporal fenestra; 38, parietal long, length/minimum width ratio greater than 2; 51, jugal process of maxilla reduced to short projection but retaining a distinct facet; 65, quadratojugal foramen absent; 66, well-defined paraquadrate notch of quadrate absent, reduced to poorly defined embayment of quadrate; 93, 3 or more replacement teeth per tooth position; 118, manual digit I absent; 132, tibia cnemial crest extending on diaphysis; 137, pedal unguals dorsoventrally flattened and broadened, hoof-like), while the clade ((Levnesovia+Bactrosaurus)+Tanius+(Telmatosaurus+more advanced taxa)) is supported by 8 unambiguous synapomorphies (4, present of premaxillary foramen ventral to anterior margin of external nares that opens onto the palate and connected by a canal to the narial fossa; 52, location of apex at or anterior to center of maxilla in lateral exposure; 56, ectopterygoid-jugal contact absent, palatine-jugal contact enhanced; 72, paroccipital process and accompanying squamosal curved anteriorly; 77, predentary gracile and shovel-shaped, straight to gently rounded anterior margin, numerous nutrient foramina across entire anterior margin, rounded, triangular denticles project anteriorly and fit into a continuous transverse slot on underside of premaxilla; 89, surangular foramen absent; 99, dentary tooth crown dominated by on primary ridge on lingual surface, secondary ridges faint if present; 129, shaft of ischium nearly straight in lateral view) (Supporting Information S3).
The strict consensus tree recovered by our analysis is more resolved than those consensus trees of  and  regarding the phylogeny of basal hadrosauroids, although the relationships among Yunganglong, Jintasaurus, Protohadros, Nanyangosaurus, Shuangmiaosaurus, Levnesovia, Bactrosaurus, Tanius, and Telmatosaurus are still not resolved. The single most parsimonious tree of  recovered Protohadros, Tanius, Bactrosaurus, Gilmoreosaurus, and Telmatosaurus as successively more derived than Probactrosaurus; in contrast, in our analysis, although Probactrosaurus is recovered as more basal than Protohadros, Tanius, Bactrosaurus, and Telmatosaurus, the relationships among the latter four plus Yunganglong, Jintasaurus, Nanyangosaurus, Shuangmiaosaurus, Levnesovia are not resolved. The analysis of  focused on saurolophine hadrosauroids and only used two basal hadrosauroids, with Probactrosaurus more basal than Bactrosaurus.
Comparison and Discussion
In Yunganglong the caudal surface of the supraoccipital is inclined steeply forward at approximately 450. In contrast, the caudal surface is nearly vertical in Jintasaurus and less derived Hadrosauriformes. The condition in Protohadros, Nanyangosaurus, and Shuangmiaosaurus is not known.
Yunganglong has relatively poorly developed cranial expansion of the distal condyles of the femur and a moderately deep and fully opened intercondylar extensor groove. In contrast, in Nanyangosaurus, Bactrosaurus, Levnesovia, Tanius, Telmatosaurus, and Hadrosauridae, the cranial ends of the expanded condyles meet or fuse together and enclose the extensor tunnel. The condition in Jintasaurus, Protohadros, and Shuangmiaosaurus is not known.
Nanyangosaurus is a medium-sized (~4.5 m) basal hadrosauroid represented by a nearly complete post-cervical vertebral column, the distal portions of both ischia, and elements of the fore and hind limbs. The age of the Nanyangosaurus-bearing red beds in the Xiaguan Basin of southern Henan Province was argued to be Early Cretaceous by Xu et al.  based on the evolutionary grade of Nanyangosaurus, which is intermediate between Probactrosaurus and Hadrosauridae. However, the data matrix of Xu  only included seven hadrosauroids (plus Hypsilophodon, Camptosaurus, Iguanodon, and Ouranosaurus), and our results and those of another cladistic analysis  suggest a more derived position for Nanyangosaurus. Furthermore, regional geological workers insist on an early Late Cretaceous age for the Nanyangosaurus-bearing red beds in Xiaguan Basin of southern Henan Province, which is partially equivalent to the famous dinosaur egg-bearing red beds in the neighboring Xixia Basin , . They also prefer the use of the name Xiaguan Formation to refer to the red beds in the Xiaguan Basin based on priority . Therefore, we regard the horizon of Nanyangosaurus to be the Xiaguan Formation of early Late Cretaceous age.
Shuangmiaosaurus was recovered from the Late Cretaceous of Liaoning Province of northeastern China, and is represented by a left maxilla (holotype) and a referred left dentary . The lack of overlapping elements between it and Yunganglong precludes further comparison.
The available information does not allow direct anatomical comparisons between Yunganglong and two other early Late Cretaceous non-hadrosaurids from North America: the Cenomanian Protohadros  and the Turonian Jeyawati . The North American Campanian Glishades is probably an indeterminate member of Hadrosauridae  rather than a non-hadrosaurid hadrosauroid . The late Campanian - early Maastrichtian European Tethyshadros is an insular dwarf with a possible close relationship to Telmatosaurus .
Eolambia caroljonesa from the lower Cenomanian Mussentuchit Member of the Cedar Mountain Formation in eastern Utah recently received a detailed redescription and was recovered as the sister taxon of Probactrosaurus gobiensis from the Early Cretaceous of China . Eolambia is different from Yunganglong in numerous features, such as the nearly vertical caudal surface of the supraoccipital, the rostrally curved distal end of the paroccipital process, the caudoventrally-directed occipital condyle, and the expanded boot-like distal end of the ischium. All these features are absent in Yunganglong.
Young  assigned the hadrosauroid material recovered from the Zuoyun area to Bactrosaurus johnsoni. Unfortunately, no overlapping material can be compared between Young's material and Yunganglong. However, based on the more basal phylogenetic position and lower stratigraphic horizon of Yunganglong compared to Bactrosaurus johnsoni, Young's material probably does not belong to Bactrosaurus but might pertain to Yunganglong.
Synapomorphies of strict consensus.
Synapomorphies of 50 majority.
We are grateful to Mr. Zhi-Lu Tang for arranging this study; to the crew of the Shanxi Museum of Geological and Mineral Science and Technology for discovering, excavating, and preparing the specimen; to Mr. Jing-Tao Yang for processing the photos; to Mrs. Jin-Ling Huang for drawing Figure 3; to Andrew McDonald for improving the draft; to Drs. Andrew McDonald, Pascal Godefroit, and an anonymous reviewer for reviewing the ms; and to Dr. David Evans for handling this ms.
Conceived and designed the experiments: RFW HLY. Analyzed the data: RFW HLY SCX SZW JY LJX YXL LJ. Wrote the paper: HLY. Performed the field work: SCX SZW JY LJX YXL LJ.
- 1. Norman DB (2004) Basal Iguanodontia. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley, CA: University of California Press. pp. 413–437.
- 2. Horner JR, Weishampel DB, Forster CA (2004) Hadrosauridae. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley, CA: University of California Press. pp. 438–463.
- 3. Erickson GM, Krick BA, Hamilton M, Bourne GR, Norell MA, et al. (2012) Complex Dental Structure and Wear Biomechanics in Hadrosaurid Dinosaurs. Science 338: 98–101. doi: 10.1126/science.1224495
- 4. McDonald AT (2012) Phylogeny of Basal Iguanodonts (Dinosauria: Ornithischia): An Update. PLoS ONE 7: e36745. doi: 10.1371/journal.pone.0036745
- 5. You HL, Ji Q, Li JL, Li YX (2003) A new hadrosauroid dinosaur from the mid-Cretaceous of Liaoning, China. Acta Geol Sin-Engl Ed 77: 148–154. doi: 10.1111/j.1755-6724.2003.tb00557.x
- 6. Sues HD, Averianov A (2009) A new basal hadrosauroid dinosaur from the Late Cretaceous of Uzbekistan and the early radiation of duck-billed dinosaurs. Proc R Soc B-Biol Sci 276: 2549–2555. doi: 10.1098/rspb.2009.0229
- 7. Xu X, Zhao XJ, Lü JC, Huang WB, Li ZY, et al. (2000) A new iguanodontian from Sangping Formation of Neixiang, Henan and its stratigraphical implication. Vertebr Palasiat 38: 185–191.
- 8. Kirkland JI (1998) A new hadrosaurid from the Upper Cedar Mountain Formation (Albian-Cenomanian: Cretaceous) of eastern Utah - the oldest known hadrosaurid (Lambeosaurine?). In: Lucas SG, Kirkland JI, Estep JW, editors. Lower and Middle Cretaceous Terrestrial Ecosystems. Albuquerque, NM: New Mexico Museum of Natural History and Science. pp. 283–295.
- 9. Head JJ (1998) A new species of basal hadrosaurid (Dinosauria, Ornithischia) from the Cenomanian of Texas. J Vertebr Paleontol 18: 718–734. doi: 10.1080/02724634.1998.10011101
- 10. McDonald AT, Wolfe DG, Kirkland JI (2010) A new basal hadrosauroid (Dinosauria: Ornithopoda) from the Turonian of New Mexico. J Vertebr Paleontol 30: 799–812. doi: 10.1080/02724631003763516
- 11. Sereno PC (2005) Stem Archosauria Version 1.0. TaxonSearch website. Available: http://wwwtaxonsearchorg/Archive/stem-archosauria-10php. Accessed 2013 Jan 15.
- 12. Young CC (1958) The first record of dinosaurian remains from Shansi. Vertebr Palasiat 2(4): 231–236.
- 13. Prieto-Márquez A, Chiappe LM, Joshi SH (2012) The Lambeosaurine Dinosaur Magnapaulia laticaudus from the Late Cretaceous of Baja California, Northwestern Mexico. PLoS ONE 7: e38207. doi: 10.1371/journal.pone.0038207
- 14. Godefroit P, Bolotsky YL, Lauters P (2012) A New Saurolophine Dinosaur from the Latest Cretaceous of Far Eastern Russia. PLoS ONE 7: e36849. doi: 10.1371/journal.pone.0036849
- 15. McDonald AT, Espilez E, Mampel L, Kirkland JI, Alcala L (2012) An unusual new basal iguanodont (Dinosauria: Ornithopoda) from the Lower Cretaceous of Teruel, Spain. Zootaxa 3595: 61–76. doi: 10.11646/zootaxa.3609.5.8
- 16. You HL, Li DQ (2009) A new basal hadrosauriform dinosaur (Ornithischia: Iguanodontia) from the Early Cretaceous of northwestern China. Can J Earth Sci 46: 949–957. doi: 10.1139/e09-067
- 17. Maddison WP, Maddison DR (2011) Mesquite: a modular system for evolutionary analysis. Version 2.75. website. Available: http://mesquiteprojectorg.org. Accessed 2012 May 30.
- 18. Goloboff PA, Farris JS, Nixon KC (2008) TNT, a free program for phylogenetic analysis. Version 1.1: Willi Hennig Society Edition. Cladistics 24: 774–786 Available: http://www.zmuc.dk/public/phylogeny/TNT.
- 19. Owen R (1842) Report on British fossil reptiles. Report of the British Association of Advanced Sciences 9: 60–204.
- 20. Seeley HG (1887) On the classification of the fossil animals commonly named Dinosauria. Proceedings of the Royal Society of London 43: 165–171. doi: 10.1098/rspl.1887.0117
- 21. Marsh OC (1881) Principal characters of American Jurassic dinosaurs. Part V. American Journal of Science (Third Series) 21: 417–423. doi: 10.2475/ajs.s3-21.125.417
- 22. Dollo L (1888) Iguanodontidae et Camptonotidae. C R Acad Paris 106: 775–777.
- 23. Sereno PC (1986) Phylogeny of the bird-hipped dinosaurs (Order Ornithischia). Natl Geogr Res 2: 234–256.
- 24. Sereno PC (1997) The origin and evolution of dinosaurs. Annu Rev Earth Planet Sci 25: 435–489. doi: 10.1146/annurev.earth.25.1.435
- 25. Sereno PC (1998) A rationale for phylogenetic definitions, with application to the higher-level taxonomy of Dinosauria. Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 210: 41–83.
- 26. Cope ED (1870) Synopsis of the extinct Batrachia, Reptilia, and Aves of North America. Trans Am Philos Soc 14: 1–252. doi: 10.5962/bhl.title.60499
- 27. Shanxi Regional Geological Survey Team (1984) Jurassic and Cretaceous in Shanxi Province: Regional Geological Survey Team of Shanxi Bureau of Geology and Mineral resources. 131 p.
- 28. Feng ZJ, Zhou SQ, Li ZY (1999) The age of the Late Cretaceous red beds in southwestern Henan Province. Regional Geology of China 18(3): 320–328.
- 29. Zhou SQ, Zhu GB, Feng ZJ (2003) The age of Xiaguan Formation in Xiaguan-Gaoqiu Basin of Neixiang County, Henan Province. Resources Survey & Environment 24(1): 69–74.
- 30. Campione NE, Brink KS, Freedman EA, McGarrity CT, Evans DC (2012) ‘Glishades ericksoni’, an indeterminate juvenile hadrosaurid from the Two Medicine Formation of Montana: implications for hadrosauroid diversity in the latest Cretaceous (Campanian-Maastrichtian) of western North America. Palaeobio Palaeoenv doi:10.1007/s12549-012-0097-1.
- 31. Prieto-Marquez A (2010) Global phylogeny of hadrosauridae (Dinosauria: Ornithopoda) using parsimony and Bayesian methods. Zool J Linn Soc 159: 435–502. doi: 10.1111/j.1096-3642.2009.00617.x
- 32. Dalla Vecchia FM (2009) Tethyshadros insularis, a new hadrosauroid dinosaur (Ornithischia) from the upper Cretaceous of Italy. J Vertebr Paleontol 29: 1100–1116. doi: 10.1671/039.029.0428