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Pakisaurus balochistani

Reptilia - Pakisauridae

Taxonomy
Pakisaurus balochistani was named by Malkani (2004). It is a 3D body fossil. Its type locality is Kinwa Kali Kakor, DL-4 (southern sites), which is in a Maastrichtian fluvial claystone in the Vitakri Formation of Pakistan.

Synonymy list
YearName and author
2004Pakisaurus balochistani Malkani p. 71
2006Pakisaurus balochistani Malkani p. 111
2007Pakisaurus balochistani Malkani
2008Pakisaurus balochistani Malkani p. 51
2010Pakisaurus balochistani Malkani p. 40
2014Pakisaurus balochistani Malkani p. 56
2015Pakisaurus balochistani Malkani p. 4
2016Pakisaurus balochistani Malkani p. 129
2017Pakisaurus balochistani Malkani p. 116
2019Pakisaurus balochistani Malkani p. 635
2020Pakisaurus balochistani Malkani p. 418–420

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
Osteichthyes()
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
Tetrapoda
Reptiliomorpha
Anthracosauria
subclassAmphibiosauriaKuhn 1967
Cotylosauria()
Amniota
Sauropsida
classReptilia
subclassEureptilia()
Romeriida
Diapsida()
RankNameAuthor
Archosauromorpha(Huene 1946)
Crocopoda
ArchosauriformesGauthier 1986
Eucrocopoda
Archosauria()
informalAvemetatarsalia
Ornithodira
Dinosauromorpha
Dinosauriformes
Dinosauria()
Saurischia()
Sauropoda()
Gravisauria
Eusauropoda
Neosauropoda
Macronaria
Titanosauriformes
Titanosauria
PoripuchiaMalkani 2020
familyPakisauridae
genusPakisaurus
speciesbalochistani

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

Pakisaurus balochistani Malkani 2004
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Diagnosis
ReferenceDiagnosis
M. S. Malkani 2019Pakisaurus balochistani sharing with Titanosauria as procoelous caudals; forward insertion of neural arches on caudals; prominent olecranon process on ulna and vertebrae lacking hyposphene-hypantrum articulations Pakisauridae characters are same as genus and species. Pakisaurus balochistani is recognised as more derived lithostrotian titanosaur based on procoelous anterior and middle caudal vertebrae. Pakisaurus balochistani is recognised as most derived Poripuch lithostrotian titanosaur based on procoelous anterior, middle and posterior caudal vertebrae. Pakisaurus balochistani is characterised by long slender legs and tall tail; narrow, long and recurved teeth with constant thickness from base to tip (except tip); large sized braincase with D-shaped occipital condyle; basal tubera breadth narrower than occipital condyle; caudals are tall quadrangular shape except a few anteriormost caudals which are broad; distal most caudal centrum anterior articular face shape procoelous while posterior face ball is biconvex cone with a horizontal transverse groove in the middle; distal scapula relatively less expanded than Gspsaurus; distal scapula with relatively anteroposteriorly long glenoid; distal scapular articular length for coracoid is relatively small (unlike Isisaurus); acromian process is narrow; expanded radial condyle exposed on the anterior aspect of distal humerus (unlike Isisaurus); femoral shaft, lateral margin shape, proximal one-third deflected medially with wavy style (and not straight as in Isisaurus); transversely narrow proximal Tibia with arc shaped lateral fibular condylar ridge ended just below cnemial crest; and osteoderms spikes on ramus.
M. S. Malkani 2020Pakisaurus balochistani is a large sized gracile bodied pakisaurid Poripuchia titanosaurian sauropod sharing with the Titanosauria as procoelous caudals, forward insertion of neural arches on caudals, vertebrae lacking hyposphene-hypantrum articulations, prominent olecranon process on ulna and neural spine single and not bifid. Pakisaurus balochistani shares with Poripuchia [4] [27] as procoelous all caudal vertebrae except first biconvex in some taxa (because in Poripuchia anterior, middle and distal caudals found are all procoelous, while in lithostrotian distal caudals are not procoelous). Pakisaurus balochistani sharing with the Pakisauridae (characters same as genus and species Pakisaurus balochistani) as straight and slightly recurved slender teeth which have almost same thickness (diameter) except tip (opposite of gspsaurids teeth which are conical and con- verge and taper on all sides from base to tip); ratio of mid transverse width above and below of mid caudal centrum is about 1 i.e. the ventral view of mid caudal centra are not compressed or slightly compressed; transversely (relatively) thin bone of proximal tibia; proximal tibia, anteroposteriorly twice wide than transverse width (in Gspsauridae stocky tibia anteroposteriorly 1 to 1.5 times than transverse width); distal tibia is anteroposteriorly more wider than transverse width (while in Gspsauridae distal stocky tibia is transversely more wide than anteroposterior width). Pakisauridae is the most inclusive clade of Titanosauria containing Pakisaurus balochistani and Isisaurus colberti but not Saraikimasoom vitakri and Gspsaurus pakistani.
Pakisaurus balochistani is characterized by long slender legs and tall tail; nar- row, long and recurved teeth with constant thickness from base to tip (except tip) and slender indices more than 5 (while Gspsaurus and Saraikimasoom have moderate and small teeth respectively with gradually decreasing thickness from base to tip, and have rounded and pointed tips and slender indices vary from 3 - 5); large sized braincase with D-shaped occipital condyle (Figure 5) (while Gspsaurus and Saraikimasoom have rectangular occipital condyle with sagital dorsoventral groove and constriction); basal tubera breadth narrower than occipital condyle; caudals are tall (Figure 1) quadrangular shape (without significant ventral reduction) except a few anteriormost caudals which are broad; vertically oriented neural spine (Figure 1) on anterior and mid caudals (unlike Isisaurus colberti show inclined neural spine); distal most caudal centrum anterior articular face shape procoelous while posterior face ball has a horizontal transverse groove in the middle (posterior ball is folded like upper and lower anticlines al- ternated or sandwiched by a mid syncline) (Figure 5) unlike the slight and very feeble vertical groove on posterior ball of distal caudal centrum of Lirainosaurus astibiae [47] from Spain, Europe and U-shaped groove on posterior ball of distal caudal centrum of Epachthosaurus sciutoi [48] from Patagonia, Argentina, South America; Anterolateral bicleavage of sternal or two longitudinal transverse crest separated by a trough and medially convex profile (Figure 3); distal scapula relatively less expanded (Figure 2) than Gspsaurus pakistani and Saraikimasoom vitakri; distal scapula with relatively anteroposteriorly long glenoid (Figure 2); distal scapular articular length for coracoid is relatively small (Figure 2) (unlike Isisaurus which have long articular surface for coracoid); acromian process is narrow (Figure 2); expanded radial condyle exposed on the anterior aspect of distal humerus (Figure 1) (Figure 4) (unlike Isisaurus colberti which have no expanded radial condyle); femoral shaft, lateral margin shape, proximal one-third deflected medially with wavy style (Figure 4) (and not straight as in Saraikimasoom vitakri); slender flattened and transversely compressed proximal tibia with anteroposteriorly quite broad distal tibia (Figure 4), (while Gspsaurus pakistani have stocky biconvex lense shaped tibia with transversely broad distal ends, Sa- raikimasoom vitakri have stocky subsquare shaped proximal tibia of equal transverse and anteroposterior widths, Isisaurus colberti have slender flattened and transversely compressed proximal tibia with anteroposteriorly relatively less broad distal tibia; Figure 7); and dorsoposterior to lateroventrally oriented crest or ridge on the medial aspect of proximal fibula; and dorsoventrally straight parallel rugose structures on proximal fibula (Figure 2).
Measurements
No measurements are available
Composition: hydroxyapatiteinfrao
Entire body: yesinfrao
Adult length: 10 to < 100infrao
Adult width: 10 to < 100infrao
Adult height: 10 to < 100infrao
Thickness: thickinfrao
Architecture: compact or denseinfrao
Form: sphericalinfrao
Ontogeny: accretion, modification of partsinfrao
Grouping: gregariousinfrao
Environment: terrestrialinfrao
Locomotion: actively mobileinfrao
Life habit: ground dwellinginfrao
Diet: herbivoreinfrao
Reproduction: oviparousinfrao
Dispersal: direct/internalinfrao
Dispersal 2: mobileinfrao
Created: 2004-12-14 12:49:10
Modified: 2004-12-14 14:49:10
Source: infrao = infraorder
Reference: Marsh 1875

Age range: Late/Upper Maastrichtian or 70.60000 to 66.00000 Ma

Collections (11 total)


Time interval Ma Country or state Original ID and collection number
Maastrichtian72.1 - 66.0India (Gujarat) Pakisaurus balochistani (34725)
Late/Upper Maastrichtian70.6 - 66.0Pakistan (Balochistan) Balochisauridae indet. (220166) Pakisaurus balochistani (53153 78055 79427 type locality: 79428 79665 79669 220154 220160) Titanosauria indet. (79668)