Showing posts with label Maniraptors. Show all posts
Showing posts with label Maniraptors. Show all posts

Tuesday, 21 November 2023

Jaculinykus yaruui: A new species of Alvarezsaurid Dinosaur from the Late Cretaceous of Mongolia.

The Alvarezsaurids are a poorly understood group of Maniraptoran Theropod Dinosaurs, in which later members became miniaturized and independently obtained a number of features associated with Birds, including s a lightly built, kinetic skull, a keeled sternum, a fused carpometacarpus, and a retroverted pubis and ischium. This was combined with several features unique to the group which have been hard to interpret functionally, including a short robust forelimb with a greatly elongated first finger, which has been suggested as a possible adaptation to digging and hunting burrowing Insects, combined with elongate hind limbs, apparently adapted to fast running. It has also been suggested that the group show adaptations towards vision in low-light environments and highly acute hearing, possibly comparable to that of modern Barn Owls, which is likely an indication of nocturnal behaviour.  

The Alvarezsaurids had a global distribution, but the majority of fossils are known from South America or Asia. The most derived Alvarezsaurids are known from the Late Cretaceous Nemegt Basin of Mongolia, from where eight species have been described to date, although most of these are known from fragmentary remains, of little help in reconstructing the ecology of the living Dinosaurs, or the way in which they were related to one-another.

In a paper published in the journal PLoS One on 15 November 2023, Kohta Kubo of the Department of Natural History and Planetary Sciences at Hokkaido University, Yoshitsugu Kobayashi of the Hokkaido University Museum, Tsogtbaatar Chinzorig of the Department of Biological Sciences at North Carolina State University and the Institute of Paleontology of the Mongolian Academy of Sciences, and Khishigjav Tsogtbaatar, also of the Institute of Paleontology of the Mongolian Academy of Sciences, describe a new species of Alvarezsaurid Dinosaur from the Nemegt Basin.

The new species is described from a single nearly complete and articulated skeleton, from the Baruungoyot-Nemegt interfingering interval at the Nemegt locality of the Nemegt Basin in the Gobi Desert of Mongolia. It is named Jaculinykus yaruui, where 'Jaculinykus' is a combination of 'Jaculus' a small Dragon from Greek mythology, and 'onykus', meaning 'claw', while 'yaruui'- derives from the Mongolian word 'yaruu', meaning 'speedy'.

Holotype of Jaculinykus yaruui (MPC-D 100/209). (A) Photograph of the specimen. (B) Explanatory drawing of (A). Highlighted areas refer to the indication of the skeletal elements; skull in green, tail in grey, pectoral girdle and forelimbs in red, pelvis and hind limbs in purple. (C) Reconstruction of Jaculinykus yaruui. Grey areas are missing parts. Kubo et al. (2023).

The specimen comprises is a nearly complete skeleton with a skull, missing the vomers, nasals, postorbitals, and supraoccipitals, and a post-cranial skeleton missing the eighth or ninth cervical vertebra, posterior dorsal vertebrae, seven anterior caudal vertebrae, sternum, furcula, right manual phalanx (II-2), right manual ungual and left fibula. 

Surprisingly, it was discovered with the neck curved posteriorly on the right side of the body; the tail positioned on the left side and curled around the flexed hind limbs to the right. This is very different from the typical 'flexed' position seen in small Theropod Dinosaur remains, and closely resembles the sleeping posture in Birds, where the head is tucked under the wing. Such a posture has previously been recorded in numerous Troodontids, Dinosaurs closely related to Birds. However, Alvarezsaurids are much less closely related within the Maniraptora. This raises two possibilities; either this sleeping posture arose before or with the emergence of the first Maniraptorans, and can be expected in all members of the group, or is a convergent adaptation to heat conservation in sleeping small feathered Dinosaurs.

Evolution of Avian-like sleeping posture in Theropod Dinosaurs. Skeletal disposition of Jaculinykus yaruui  (MPC-D 100/209) in dorsal (A) and ventral (reversed) (B) views. (C), Interpretive line drawing of skeletal disposition. (D), Life restoration of sleeping posture of Jaculinykus yaruui . (E), Simplified coelurosaurian phylogeny represents presence for evidence of avian ‘tuck-in’ posture. Kubo et al. (2023).

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Thursday, 14 September 2023

Fujianvenator prodigiosus: A novel Avialan Theropod from the Late Jurassic of Fujian Province, China.

The clade Avialae is defined as containing all living Birds, plus anything more closely related to them than either Deinonychus or Troodon. This group appeared in the Middle-to-Late Jurassic, but pre-Cretaceous fossils are rare and limited to a small number of locations, making the early history of the Avialans somewhat unclear. The oldest known Avialan fossils probably come from the Yanliao Biota in northeast China, where they first appear about 166 million years ago, with slightly younger specimens, including Archaeopterix, coming from the Solnhofen Limestones of Germany, although these have not been precisely dated. Following these two fossil lagerstatten there is a gap of about 30 million years before further Avialan fossils appear in the Early Cretaceous Huajiying Formation of Hainan Island, South China. Clearly, understanding the nature of these Jurassic stem-Birds is a key to understanding the global Avialan diversification at the beginning of the Cretaceous. 

In a paper published in the journal Nature on 6 September 2023, Liming Xu of the Fujian Institute of Geological Survey, Min Wang of the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences, Runsheng Chen, also of the Fujian Institute of Geological Survey, Liping Dong, also of the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences,  Min Lin, again of the Fujian Institute of Geological Survey, Xing Xu, again of the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences,  and of the Centre for Vertebrate Evolutionary Biology at Yunnan University, and of the Paleontological Museum of Liaoning at Shenyang Normal University, Jianrong Tang, again of the Fujian Institute of Geological Survey, Hailu You, again of the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences, Guowu Zhou, Linchang Wang, Wenxing He, and Yujuan Li, all of the Fujian Institute of Geological Survey, and Chi Zhang and Zhonghe Zhou, again of the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences, describe a new species of Avialan Theropod from an outcrop the Late Jurassic (149.9–150.2 million years old) Nanyuan Formation near Yangyuan Village in Zhenghe Country in Fujian Province, China, the first Avialan to be described from this recently discovered locality, which has to date yielded more than 100 well-preserved Vertebrate fossils, and shows signs of becoming a significant Late Jurassic fossil lagerstatten.

The new species is descried from a single partial skeleton, preserved on a slab and counter slab. It is given the name Fujianvenator prodigiosus, where 'Fujianvenator' means 'Fujian hunter', and 'prodigiosus' is intended to mean 'bizarre', in reference to the unusual nature of the specimen. The single known specimen is not considered to be skeletally mature, on the basis of its unfused metacarpals and tibiotarsus, although it does have a fused astragalus and calcaneum and an ossified sternum, implying that it was close to maturity when it died.

Morphology, phylogenetic and palaeogeographical position of Fujianvenator prodigiosus, IVPP V31985. (a), (b) Photograph (a) and line drawing (b) of the holotype of Fujianvenator prodigiosus (composite drawing based on both the slab and the counter slab). (c) Time-scaled phylogenetic tree showing the position of Fujianvenator prodigiosus (red star), with a palaeomap of the Late Jurassic (150  million years ago) showing the distribution of the known Jurassic Avialan fossils. The green and blue stars denote the Yanliao Biota and the Solnhofen Limestones, respectively. Abbreviations: ch, chevron; cv, caudal vertebra; dv, dorsal vertebra; gs, gastralia; lf, left femur; lfi, left fibula; lh, left humerus; li, left ilium; lis, left ischium; lr, left radius; ls, left scapula; lt, left tibia; lu, left ulna; mI to mV, metatarsal I to V; mcI to III, metacarpal I to III; pd, pedal digit; pt, proximal tarsal; pu, pubis; rh, right humerus; ra, radiale; rc, right coracoid; rf, right femur; rfi, right fibula; ri, right ilium; ris, right ischium; rr, right radius; rs, right scapula; rt, right tibia; ru, right ulna; st, sternum; un, ulnare; ?sv, possible sacral vertebra; I-1 to I-2, manual phalanx I-1 and I-2; II-1 to II-3, manual phalanx II-1 to II-3; III-1 to III-4, manual phalanx III-1 to III-4. Scale bars are 20 mm. Xu et al. (2023).

Fujianvenator prodigiosus has a mosaic combination of Theropod, Avialan, and unique features, including vertebrae increase in length increases further back on the spine, with the fifth vertebra twice as long as the first, something seen in Cretaceous Avialans such as Jeholornis, but not Jurassic forms such as Archaeopterix, a scapula significantly shorter than the humerus, something not found in other Theropods or early Avialans, a humerus significantly longer than the scapula, something seen in among Theropods only in Cretaceous Avialans and the Scansoriopterygids (a group of Jurassic Maniraptors believed to have evolved flight independently of the Birds), an ossified sternum, again seen in Cretaceous Avialans and Scansoriopterygids, a small deltopectoral crest on the humerus, seen in other Jurassic Avialans, an ulna shorter than the humerus, typical of non-Avialan Theropods, a straight ulna, seen in some early Avialans, but absent in others, and in most closely related Theropods.

A phylogenetic analysis recovered Fujianvenator prodigiosus as a member of the e Anchiornithidae, the sister group to all other Avialans (including Archaeopterix and all Cretaceous Avialans), and which until has contained only species from the Yanliao Biota. Fujianvenator prodigiosus is ten million years younger than the Yanliao Biota Avialans, and the most southerly Jurassic Avialan discovered to date, and therefore represents a significant increase to our knowledge of Jurassic Avialans. It the proportions of its manual phalanges (hands) are similar to those of Archaeopterix, while its pevis appears closer to those of Anchiornis and Troodontids, while its feet show a range of mixture of features seen in Archaeopteryx, Anchiornis, Troodontids, and Dromaeosaurids.

Counter slab of holotype of Fujianvenator prodigiosus, IVPP V31985. (a) Photograph. (b) Line drawing. Abbreviations: ch, chevron; cv, caudal vertebra; dv, dorsal vertebra; gs, gastralia; lf, left femur; lfi, left fibula; lh, left humerus; li, left ilium; is, ischium; lr, left radius; ls, left scapula; lt, left tibia; lu, left ulna; mI to mV, metatarsal I to V; mcI to III, metacarpal I to III; pt, proximal tarsal; pu, pubis; rh, right humerus; ra, radiale; rc, right coracoid; rf, right femur; rfi, right fibula; ri, right ilium; rs, right scapula; rt, right tibia; st, sternum; un, ulnare; ?sv, possible sacral vertebra; I-1 to I-2, manual phalanx I-1 and I-2; II-1 to II-3, manual phalanx II-1 to II-3; III-1 to III-4, manual phalanx III-1 to III-4. Scale bars are 20 mm. Xu et al. (2023).

The evolution of early Avialans has long thought to have been driven by adaptation for flight, however, Fujianvenator prodigiosus does not appear particularly suited to flying, and a morphometric analysis suggests that it was probably better suited to a terrestrial lifestyle. Its hands appear to have been quite flexible, which would be good for grasping prey, but would lessen the ability to support weight on wing feathers during flight, while its hindlimbs were long and its feet well adapted for running.

In fact, the morphometric analysis suggested that the hindlimbs of Fujianvenator prodigiosus were uniquely well suited to running, compared to other Mesozoic Theropods, although Xu et al. note that long limbs in a modern Bird can be an indicator of a wading lifestyle rather than a running one, and the preservation of the lower limbs of the specimen is not sufficiently good to eliminate either possibility. The Nanyuan Formation, from which the specimen was obtained, comprises a mixture of mudstones and shales, and many of the fossils recovered from it are of species aquatic or semi-aquatic in nature, implying a wetland environment, quite different from the environments recorded by the Yanliao Biota and the Solnhofen Limestones, increasing our knowledge of the ecosystems in which the earliest Avialans lived.

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Sunday, 10 September 2023

Tyrannomimus fukuiensis: A new Ornithomimosaur from the Early Cretaceous of Japan, and its implications for the origins of the Ornithomimosauria.

The Ornithomimosaurs are a group of Theropod Dinosaurs with notably long and slender hindlimbs, thought to have been capable of sustained high-speed running in a similar fashion to modern Ostriches. This Ostrich-like appearance is accentuated by their having feathers, long necks, small heads, and often-toothless beak-like jaws. The earliest known Ornithomimosaurs date from the Early Cretaceous, with the two major subdivisions of the group, the Ornithomimidae and Deinocheiridae apparently having already diverged by this time, implying a deeper 'ghost' history to the clade, which has not been detected in the fossil record.

In a paper published in the journal Scientific Reports on 7 September 2023, Soki HattoriMasateru ShibataSoichiro KawabeTakuya Imai,  Hiroshi Nishi, and Yoichi Azuma of the Institute of Dinosaur Research at Fukui Prefectural University, and the Fukui Prefectural Dinosaur Museum, describe a new species of Ornithomimosaur from the Early Cretaceous Kitadani Formation exposure at Kitadani Dinosaur Quarry.

Kitadani Dinosaur Quarry is a notable Dinosaur-producing site in Fukui Prefecture, which has previously produced a number of new Dinosaur species, including the Therizinosaur, Fukuivenator paradoxus, which is the most complete non-Avian Dinosaur known from Japan, the Titanosaur, Fukuititan nipponensis, the Megaraptor, Fukuiraptor kitadaniensis, and the Iguanodontian, Fukuisaurus tetoriensis.

Bonebed 1 is a distinct layer within the Kitadani Formation at Kitadani Dinosaur Quarry containing a large number of disassociated Dinosaur bones interpretted as having come from a single species of Ornithomimosaur, which Hattori et al. formally describe as a new species, under the name Tyrannomimus fukuiensis, where 'Tyrannomimus' refers to the similarity of the species to some (small) Tyrannosaurs, in particular its possession of a vertical ridge on the ilium, a feature previously interpreted as a defining Tyrannosaur trait, and 'fukuiensis' means 'from Fukui'.

Locality, horizon, and overview of the Ornithomimosaur materials. Regional map for the location of Fukui in Japan, and the Kitadani Dinosaur Quarry in Fukui (a), stratigraphic section of the part of the Kitadani Formation in the Kitadani Dinosaur Quarry (b), photograph of the Kitadani Dinosaur Quarry in 2019 with an arrowhead indicating where the studied specimens were discovered (c), and overview of the Ornithomimosaur material (d). Fossil specimens shown in (d) are not in the same scale while the bar is scaled for the paratype (FPDM-V-10295). The holotype (FPDM-V-11333) and paratype in (d) are colored in red anb blue, respectively. Right femur in (d) is mirrored from a left femur (FPDM-V-11338). Hatorri et al. (2023).

Tyrannomimus fukuiensis is described from a holotype, FPDM-V-11311, a disarticulated but associated skeleton including two parts of the braincase, several dorsal, sacral and caudal vertebrae, and fragments of ilium, and paratype, FPDM-V-10295, a disarticulated but associated hindlimb skeleton including a partial lef femur, left metatarsal II, lef and right metatarsal IV, right pedal phalanx I-1 and a pedal ungual, with reference to several other specimens.

Cranial elements of Tyrannomimus fukuiensis. Left frontal of FPDM-V-11313 (a)–(c) and right prootic (mirrored) (d)–(f), osseous labyrinth (mirrored) (g)–(i) and basioccipital (j)–(l) of FPDM-V-11311 in dorsal (a), (g), lateral (b), (f), (i), (j), ventral (c), (l), dorsolateral (d), anterior (e), (h) and posterior (k) views. Abbreviations: br, basisphenoid recess; bt, basal tuber; cd, cochlear duct; dtr, dorsal tympanic recess; if, infracondylar fossa; lc, lacrimal contact; ls, lateral semicircular canal; lsc, laterosphenoid contact; om, orbital margin; or, orbitonasal ridge; pfc, prefrontal contact; poc, postorbital contact; pop, postorbital process; rs, rostral semicircular canal; sf, supratemporal fossa; sr, subcondylar recess; V, trigeminal nerve opening; VII, facial nerve opening. Scale bars are equal to 10 mm. Hatorri et al. (2023).

Bonebed 1 contains a very large number of detached bones, but this appears to be a monospecific assemblage, with little variation among any of the individual skeletal elements. The holotype of Tyrannomimus fukuiensis does not appear to be fully mature, which might raise the possibility that it is a juvenile of another species, notably Fukuiraptor kitadaniensis, which is also present at Kitadani Dinosaur Quarry and of nearly identical age. However, the holotype of Tyrannomimus does not show any of the diagnositic features of Fukuiraptor, while it shows a number of diagnostic features of the Ornithomimosaurs and is clearly monospecific with the other material from Bonebed 1, effectively ruling out such a hypothesis.

A phylogenetic analysis recovered Tyrannomimus fukuiensis as a member of the Deinocheiridae, forming a sister taxon to the Mongolian Harpymimus okladnikovi. This analysis also makes Tyrannomimus fukuiensis the oldest known member of the Deinocheiridae, and the first member of that group from East Asia. This close relationship between the Japanese Tyrannomimus fukuiensis and the Mongolian Harpymimus okladnikovi is noteworthy, as other Early Cretaceous Japanese fossils, including Hadrosaurs and Cockroaches have also shown closer affinity to Mongolian groups than to Chinese ones, suggesting an ecological link between the two areas.

Phylogenetic position of Tyrannomimus fukuiensis within Ornithomimosauria. A coloured bar in the strict consensus tree represents the time and region of occurrence for each taxon and a number represents Bremer support value for each node. Note that the dataset for the phylogenetic analysis that yielded this consensus tree did not include Aviatyrannis. Hatorri et al. (2023).

The presence of a vertical ridge on the ilium of Tyrannomimus fukuiensis makes it very similar to the ilium of Aviatyrannis jurassica, a Theropod Dinosaur from the Late Cretaceous of Portugal, currently assumed to be a Tyrannosaurid, largely due to the possession of this feature. Aviatyrannis jurassica has a number of other features, such as a brevis fossa which becomes mediolaterally broader towards the posterior end, which are typical of Ornithomimosaurs. A phylogenetic analysis of the Ornithomimosauria with Aviatyrannis jurassica included recovered this Jurassic 'Tyrannosaur' as the sister taxon to Tyrannomimus fukuiensis. If this is correct then Aviatyrannis jurassica is in fact both the earliest known Ornithomimosaur and the earliest known Deinocheirid, although without having inspected the holotype of Aviatyrannis jurassica themselves, Hatorri et al. are cautious in this assessment.

Strict consensus tree of 2640 MPTs with a length of 3019 steps (CI = 0.217; RI = 0.608) resulted by the phylogenetic analysis conducted with Aviatyrannis jurassica being added. Numbers associated with nodes represent Bremer support values. Hatorri et al. (2023).

The oldest known specimens currently recognised as Ornithomimosaurs are un-named fragmentary specimens from the Kirkwood Formation of South Africa, followed by fragmentary specimens assigned to Valdoraptor oweni, un-named fragmentary specimens from France, and some fragmentary material from Thailand described as Kinnareemimus khonkaenensis. A putative Ornithomimosaur, Lepidocheirosaurus natatilis, has previously been described from the Late Jurassic  Kulinda Deposits of Zabaykalsky Krai, Russia, but it is now considered doubtful that this is even a Theropod. If Lepidocheirosaurus natatilis is not an Ornithomimosaur, and Aviatyrannis jurassica is, then Aviatyrannis jurassica would be the oldest known and only Jurassic member of the Ornithomimosauria. This is not implausible, as the Ornithomimosauria are considered to be the sister taxon to the Maniraptora, a group which appeared in the Middle Jurassic, making it unlikely that the Ornithomimosauria are significantly younger. Furthermore, the distribution of the earliest known Ornithomimosaurs suggests that the group appeared before the break-up of Pangea, making a Cretaceous origin improbable. 

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Saturday, 24 June 2023

Shri devi: The (previously unknown) skull of a Dromaeosaurid Dinosaur from the Late Cretaceous Baruungoyot strata of Mongolia.

The Dromaeosaurs were a group of small-to-medium sized Theropod Dinosaurs, closely related to the earliest Birds. They are noted for the presence of an enlarged and highly curved claw on their second toe, a long, straight tail formed from tightly interlocked caudal vertebrae, and the presence of feathers. The group were widespread, with numerous fossils from the Cretaceous of Asia, North and South America, and Europe, although their Bird-like, often delicate skeletons did not usually preserve well, so most species are known only from fragmentary remains. One area where more complete Dromaeosaur skeletons are more frequently found is the Djadokhta strata of the Gobi Desert, Mongolia, an area which has produced several fairly complete skeletons of the Late Cretaceous Dromaeosaur, Velociraptor mongoliensis

These Upper Cretaceous deposits of the Gobi desert have produced a range of other Velociraptorine Dromaeosaurs, including Adasaurus mongoliensisTsaagan mangas, 'VelociraptorosmolskaeLinheraptor exquisitusShri devi, and Kuru kulla, although most of these are known only from a single specimen.

In a paper published in the journal Acta Paleontologica Polonica on 21 June 2023, Łukasz Czepiński of the  Institute of Palaeobiology of the Polish Academy of Sciences, describes a new Dromaeosaur specimen from the Late Cretaceous Baruungoyot strata  of the Gobi Desert, which he assigns to the species Shri devi.

The new specimen, ZPAL MgD-I/97, was collected in 1970 by a Polish-Mongolian Palaeontological Expedition, and initially described and illustrated as Velociraptor sp., then later redescribed as a specimen of Velociraptor mongoliensis. However, upon re-examination of the specimen, Czepiński disagrees with this diagnosis, noting that the skull is much less elongated than in that species.

(A) Map of Mongolia and Inner Mongolia of China with the Upper Cretaceous sites yielding remains of dromaeosaurid dinosaurs. (B) Photograph of Khulsan locality, from where the specimen described in this paper was collected, photographed in the 1970 during the Polish-Mongolian Paleontological Expeditions (from the Collections of the Institute of Palaeobiology of the Polish Academy of Sciences). Czepiński (2023).

Specimen ZPAL MgD-I/97 comprises a partial skull, including the left jugal, left lacrimal, left maxilla, fragment of the right maxilla, palatine elements, both dentaries lacking the anteriormost portions, both splenials, surangulars, and angulars, in close association with a distal portion of the left hindlimb, containing the distal parts of the left fibula and tibia, astragalus and complete pes, with four metatarsals and all phalanges. The holotype specimen of Shri devi, MPC-D 100/980, is a partial articulated skeleton including cervical, dorsal, and proximal caudal vertebrae, the right femur, the right and left tibiotarsa, and the right pes but lacking a skull, There is almost no overlap in the bones of the two specimens, with ZPAL MgD-I/97 being about 20% smaller than MPC-D 100/980, but both specimens preserve a single hind foot (left in ZPAL MgD-I/97 and right in MPC-D 100/980), and Czepiński is confident that these are similar enough to assign the two specimens to the same species.

Reconstruction of the Dromaeosaurid Dinosaur Shri devi, based on ZPAL MgD-I/97 and MPC-D 100/980. (A) Skull; missing elements reconstructed on the base of Velociraptor mongoliensis (MPC-D 100/25 and MPC-D 100/54). (B) Whole body silhouette with known remains of the holotype and referred material. Czepiński (2023).

The skull of Shri devi is apparently much shorter than in other Mongolian Dromaeosaurids, based upon the shape of the antorbital fenestra (opening in the skull in front of the eye), which is almost round in Shri devi, but elongated in most Mongolian Dromaeosaurids, despite Shri devi otherwise being very similar, and presumably closely related to, Velociraptor mongoliensis. A similar short-snouted condition is seen in many North American Dromaeosaurids, though these are not thought to be closely related to Shri devi, suggesting that this is an ecological adaptation, rather than an indicator of relatedness.

Dromaeosaurid Dinosaur Shri devi (ZPAL MgD-I/97) from the Upper Cretaceous, Khulsan, Ömnögovi, Gobi Desert, Mongolia. Photographs (A₁), (A₂), (A₄), and (A₅) and 3D model (A₃), (A₆), and (A₇) obtained from the CT scan of the left side of the skull in dorsal (A₁), medial (A₂, A₃), anterior (A₆), and lateral (A₇) views. Elements of the left palate in dorsal (A₄) and ventral (A₅) views. Right maxilla in the lateral (A₈, A₉) and anterior (A₁₀) views, with the margin of the antorbital fenestra indicated by dashed lines, and the close up of the fifth (A₁₁) and the second (A₁₂) preserved tooth in labial views showing very weakly developed denticles on the mesial carina. Right mandible in the lateral (A₁₃) and (A₁₄) and medial (A₁₅) and (A₁₆) views. (B) Explanatory drawings of the skull in left (B₁) and right (B₂) lateral views with the preserved bones (in grey). Czepiński (2023).

Most of the Dromaeosaurid Dinosaurs from Mongolia, particularly those with very long snouts, are found in palaeodesert environments, covered by aeolian sands. Both specimens of Shri devi, on the other hand, comes from a more mixed environment, with a mixture of aeolian and fluvial deposits, suggesting a wetter (though still fairly arid) environment. The available prey to a small predatory Dinosaur would appear to have been similar in both environments, including Lizards, Mammals, Protoceratopsids, Oviraptorosaurs, and Birds (larger Ankylosaurids were also present, but unlikely to have been hunted by small Dromaeosaurs), suggesting that the variation in snout length is unlikely to be related to feeding. Instead, Czepiński suggests that an elongated snout may have been related to an elongated sinus, something which would have improved thermoregulation in Dromaeosaurs living in exposed, arid environments.

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Thursday, 22 December 2022

Microraptor zhaoianus: The stomach contents of a small Dromaeosaurid Dinosaur, and the implications for this on its diet and ecology.

Determining the diets of extinct Animals is remarkably problematic, and can generally only be accomplished where clearly identifiable feeding traces or stomach contents can be found. Even where Animals thought likely to be predatory are found in close proximity to those thought likely to be their prey, it is impossible to state with any confidence that this reflects the behaviour of the living Animals, and is not a postmortem association. Stomach contents are only very rarely preserved, and then only at sites with exceptional fossil preservation, meaning that most known examples come from a very small number of locations. Furthermore, the stomach contents of an Animal can usually only tell us what it has consumed, and provides little information about its wider behaviour. We cannot, for example assume that an Animal directly hunted another species based upon its stomach contents, as almost all carnivorous Animals will consume carrion given the opportunity.

Theropod Dinosaurs are generally assumed to have hunted prey smaller than themselves. This is true of most modern Mammals, Birds and Crocodilians. Other than Mustelids, which regularly hunt prey larger than themselves, predatory Mammals generally hunt large prey only when in packs, so that the total mass of the predators outstrips that of the prey, even if the individuals do not. Large Theropods are likely to have mostly hunted other Dinosaurs, as these would have represented most of the large prey available in their environments. Small Theropods, on the other hand, are likely to have had a much wider range of suitably sized prey, including even smaller Dinosaurs, Lizards, small Amphibians, small Mammals, Arthropods, and Molluscs, and are likely to have fed on all of these. 

Very few Dinosaurs have more than one specimen known with preserved stomach contents, giving us a very limited conception of their diet. However, the small Early Cretaceous Dromaeosaurid Microraptor has four known individuals with preserved stomach contents, providing the opportunity for an analysis of its diet not really possible for any other Dinosaur. Individuals of Microraptor have previously been shown to have consumed a Bird, a Lizard, and a Fish.

In a paper published in the Journal of Vertebrate Paleontology on 20 December 2022, David Hone of the School of Biological and Behavioural Sciences at Queen Mary University of London, Alexander Decechhi of the Division of Natural Sciences at Mount Marty College, Corwin Sullivan of the Department of Biological Sciences at the University of Alberta, and the Philip J. Currie Dinosaur Museum, Xu Xing of the Key Laboratory of Vertebrate Evolution and Human Origins at the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences, and Hans Larsson of the Redpath Museum at McGill University, describe the stomach contents of the fourth specimen of Microraptor in which this is known, the holotype of Microraptor zhaoianus, and discuss the implications of this for our understanding of the diet of the species.

The specimen, IVPP V 12330, is a compression fossil broken into a number of fragments, with most of the part and counterpart present, showing the incomplete but articulated skeleton of the small Dinosaur. The abdominal and thoracic cavities show no signs of having been ruptured, and, visible within the rib-cage of the Animal, is the articulated pes (foot) of a small Mammal. This visibly overlies the ribs of the left side of the thoracic cavity, and is in turn overlain by the ribs of the right side. The visible part of the foot includes ll tarsals and metatarsals and most phalanges,including unguals of digits I and probably III. A number of long bones are also present, beneath and beside the pes, which hint that more of the Mammal might be present but obscured.

Holotype specimen of Microraptor zhaoianus (IVPP V12330) with Mammal foot gut contents. (A) Entire specimen. Box inset indicates the location of (B) and (C). (B) Close-up view of Mammal foot. (C) Illustration of visible bones: dark gray elements are Microtaptor ribs, yellow bones are the articulated Mammalian foot and light gray are unidentified bones. Note the juxtaposition of the foot over the inside of the left ribs and the overlap of the right ribs over the foot, particularly over digits II and III. Abbreviations: ast, astragalus; cal, calcaneum; mtI, metatarsal 1; nav, navicular; lr, left rib; rr, right rib. Scale bar in (A) equals 100 mm and in (B) and (C) equals 5 mm. Hone et al. (2022).
The phalanges of the foot are slender, resembling those of the Early Cretaceous Mammals Eomaia and Sinodelphys, both of which come from the same deposits as Microraptor. However, they are neither as elongate nor as curved as seen in these species, suggesting that this is another, unknown, Mammal, and that it was a primarily ground dwelling species (Eomaia and Sinodelphys are both thought to have been arboreal in nature).

The first digit is 8.1 mm in length excluding the ungual (claw), or 9 mm in length if the ungual is included. This is roughly equivalent to those of Sinodelphys, Yanoconodon, and Eomaia, and may therefore indicate an Animal of similar size, although if this Mammal did have a different ecological role, then the possible size bracket can be expanded somewhat. Nevertheless, Hone et al. estimate a size in the range 13-43 g (the range that includes most modern Mice, Voles, and Shrews).

Numerous examples of Microraptor have been recovered from the beds which make up the Jehol Biota, and many studies have been done on this Dinosaur's ecology. Nevertheless, considerable controversy remains about the lifestyle of Microraptor, with different researchers having suggested that it might be nocturnal, diurnal, capable of gliding flight, capable of powered flight, arboreal in habit, and terrestrial in habit. What is generally accepted is that Microraptor was capable of some-sort of areal locomotion, and probably able to climb reasonably well (although there is considerable doubt as to whether it was capable of living in arboreal environments with small-diameter branches, an environment which the only non-Avian Theropods thought likely to have colonised are the Scansoriopterygians. 

Over 300 specimens of Microraptor are known, which have been divided into three separate species, of different sizes and with slightly different anatomical traits, although it is still possible that this represents different growth stages and variability within a single species. Whatever the taxonomic implications, this physical variation probably represents a degree of ecological difference between the morphotypes, which may indicate differences in diet. The four specimens of Microraptor for which stomach contents are known belong to two different species, Microraptor zhaoianus, of which a previous specimen was shown to have consumed a Lizard, while Hone et al.'s study shows consumption of a small, terrestrial, Mammal, and Microraptor gui, in which two specimens have been shown to have consumed a Fish, and a small Bird, respectively. This may, therefore, represent two different species with slightly different dietary habits, but is also likely just to represent a degree of flexibility in feeding habits.

Most modern predators take food items considerably smaller than themselves, and this is unlikely to have been different in the Early Cretaceous. With the exception of Mustelids, modern Mammals of 21 kg or less typically target prey no more than 40% of their own size. This rule appears to be applicable to Microraptor, with all four specimens with stomach contents having consumed Animals significantly smaller themselves. The Bird known from the stomach contents of a specimen of Microraptor gui had an ulna length of 10.5 mm, while the ulna of the Dinosaur that had eaten it was 80 mm long. The Lizard eaten by a specimen of Microraptor zhaoianus had femur 13.4 mm long, while its consumer's was 75 mm in length. The Fish appears to have been of a similar proportion to the Dinosaur which ate it, based upon rib size, while Hone et al. estimate that the small Mammal from their study was about 10% of the size of the Microraptor.

Any consideration of the diet of an Animal should also take into account its jaw morphology. Typically, Vertebrates with shorter, more robust jaws tend to consume larger prey, which needs to be subdued and processed before consumption, whereas those with longer jaws tend to consume smaller prey, with an emphasis on shovelling down as many prey items as quickly as possible. 

This principle has previously been applied to the Eudromaeosauria, with the group found to split conveniently into three clusters, species with short deep jaws, such as Deinonychus and Atrociraptor, species with intermediate-lengthed jaws, such as AchillobatorSaurornitholestes, Bambiraptor, and Acheroraptor, and long-snouted forms such as Linheraptor, Tsaagan, and Velociraptor. Interestingly, all of the species known to have short jaws are from North America, as are most of those with intermediate jaws, while most of the long-jawed species are Asian, although, with the jaws of many species unknown or known only from fragmentary remains, it is unclear how significant this is.

While many specimens of Microraptor are known, it has proven hard to fit it into this matrix, as in the majority of specimens both maxillae are absent, unexposed, damaged, or difficult to fully demarcate from adjacent bones. However, two specimens, BMNHC PH881 and IVPP V 13475, both identified as Microraptor sp., have maxillae which appear to fit into the intermediate group, possible suggesting prey fairly easy to seize, but requiring some force to subdue. Since Microraptor is itself a small Animal, probably massing under 1 kg, Mouse-sized Mammals and similar small Vertebrates would seem to fit into this category, while most Insects would be too small.

The Mammal consumed by Microraptor IVPP V 12330 is thought to have been ground dwelling, and about the right size for the presumed prey of Microraptor, which is itself also thought to have been ground dwelling. This would seem, at first sight, to be fairly good evidence for Microraptor having predated this Mammal. However, Hone et al. caution against making such an assumption, observing that almost all carnivorous Animals will consume carrion if it is available, rather than hunting, and that, therefore, an Animal having consumed another Animal cannot be taken as direct evidence of a predator-prey relationship.

Hone et al. also not that, while Dromaeosaurs are generally assumed to have been capable of swallowing quite large items, all of the known stomach contents of Microraptor have been quite small, in this case the foot only of a Mammal, which is a low-nutrition part of the body, and generally among the last parts consumed. This makes it quite conceivable that the majority of the Mammal might have been consumed by another Animal, with the Microraptor, subsequently consuming an overlooked portion of the carcass. 

It has previously been suggested that Microraptor might have been capable of actively hunting small Birds in the treetops, based upon the presence of a partial wing and both feet of an Enantiornithine Bird within the body cavity of another specimen. However, these are again low nutrition parts of the body, likely to have been left by another Animal eating the majority of the Bird. What remains of the wing, and the feet, are themselves articulated, appears to suggest that Microraptor was incapable of any further processing of its food; either tearing these pieces of a carcass then swallowing them, or finding them left behind after the majority of the Bird has been eaten by something else. Whichever is the case, the specimen does not seem to be, in itself, sufficient evidence to claim Microraptor was able to hunt small Birds. Even if the Bird could be assumed to have been killed and then consumed by the Dinosaur, this does not indicate that the predation event took place above the ground. Even the most arboreal of modern Birds spends a considerable amount of time on the ground, and many modern predators, such as Hyenas, Cheetahs, and Foxes, hunt them there.

The presence of a Fish in within the body cavity of Microraptor specimen has also been taken as evidence of direct predation on Fish, within an aquatic environment, although in that case scavenging was not ruled out. 

Hone et al. note that the suggestion that Microraptor was capable of hunting both in the treetops and in the water as highly dubious, noting that modern Animals which can do this tend to be very specialist predators, something that there is no evidence for in the case of Microraptor. They caution that such stories are attractive, but are not supported by the evidence, and that the presence of a wide range of consumed Animals within the stomach contents of a species is probably more indicative of it being a generalist scavenger that a specialist hunter.

The range of Animals now known to have been consumed by Microraptor is wider than for any other known non-Avian Theropod, although this is clearly related to the fact that more specimens with stomach contents are known than for any other Dinosaur. However, the assumption that Microraptor, whilst probably capable of hunting, would consume a wide range of Animals opportunistically, is probably also true for most Theropods. Furthermore, most Theropods are thought likely to have changed the Animals they consumed quite significantly over their long growth-cycles, and it is likely that members of the same species in different regions would have consumed different food items, and that individuals would have consumed different items at different times of year, all of which would have favoured a more generalist approach to feeding. Insects and other Invertebrates are likely to have made up a proportion of the diet of the smallest Theropods. These have never been found in any stomach contents, but this is probably reflective of their low preservation potential rather than their not being consumed.

Specimen IVPP V 12330, the holotype of Microraptor zhaoianus, provides direct evidence of the direct consumption of a Mammal by Microraptor, only the second time this has been demonstrated for a non-Avian Dinosaur. However, this does not provide evidence of a direct predation event, but rather adds to the mounting evidence that Microraptor was a generalist carnivore, largely eating small Vertebrates, but not necessarily hunting them.

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Wednesday, 7 December 2022

Fossil eggshells from the Early Cretaceous Okurodani Formation of Gifu Prefecture, Japan.

The past three decades have seen the discovery of a large quantity of fossil eggs from several Lower Cretaceous deposits in Japan, notably the Yezo Group of Hokkaido, the Kuwajima Formation of Ishikawa Prefecture, and the Ohyamashimo Formation in Hyōgo Prefecture. These include eggs which are thought to have come from Ornithopod and Theropod Dinosaurs (including Oviraptosaurs, Troodontids, and Birds). These findings add to the known palaeobiodiversity of these areas, by indicating the presence of groups not known from the skeltal fossil record. However, the majority are of Aptian or Albian age (121.4-100.5 million years old), with earlier examples being much rarer.

The Okurodani Formation outcrops in the Shokawa area of northwestern Gifu Prefecture, and is considered to be of Hauterivian age (i.e. between 132.9 and 129.4 million years old). This formation has produced a variety of Vertebrate remains, including Dinosaurs, aquatic Tetrapods and Fish, as well as a number of fragmentary egg pieces, which have been assumed to have been of Dinosaurian origin, but never formally investigated.

In a paper published in the journal Historical Biology on 24 November 2022, Rina Uematsu of the Graduate School of Science and Technology at the University of TsukubaKohei Tanaka of the Faculty of Life and Environmental Sciences at the University of Tsukuba, Shohei Kozu of the Gifu Prefectural Museum, Shinji Isaji of the Natural History Museum and Institute of Chiba, and Shizuo Shimojima of Takayama City, describe the known egg material from the Okurodani Formation, and discuss the implications this has for the known biodiversity of the environment which produced these strata.

All the fossils examined in the study were collected between 1988 and 2009 by Shizuo Shimojima, Masatoshi Okura and Satoru Sakamoto, from the Okurodani Formation, a 220 m thick sequence of shale, alternating sandstone and mudstone, and sandstone beds, which forms part of the Itoshiro Subgroup of the Middle Jurassic to Lower Cretaceous Tetori Group, which has been dated to between 133 and 129 million years old, based upon uranium-lead dates obtained from layers of volcanic tuff within the formation.

Map of the eggshell locality. (A) Distribution of the Tetori Group in Japan formed of three subgroups. (B) Stratigraphic position of the Okurodani Formation in the Shokawa area. (C) Detail of the boxed area in (A), showing the distribution and the stratigraphic sequence of the Okurodani Formation with the locations where eggshell materials were collected. GPM-Fo-1923, 09/Cr/89/01 and 09/Cr/88/07 were found in debris of fallen rocks and their location is not specified in the stratigraphy. Uematsu et al. (2022).

Sevem fragments of eggshell and two eggshell impressions were found within black mudstone layers within the Okurodani Formation. These mudstone layers are also rich in Plant fossils and freshwater Molluscs, and are interpretted as having been laid down in a network of stagnant pools or oxbow lakes within a floodplain environment. Vertebrate remains, predominantly Fish scales and Turtle shells, but also including Frogs, small Lizards, and Choristoderes (Crocodile-like Diapsids of uncertain affinities) are typically preserved in three dimensions (i.e. not compressed),  which implies rapid burial with minimal movement. Dinosaur fossils are rare in these layers, but the teeth of Ornithopods, Sauropods, and Verociraptorines have been found, as well as the tarsometatarsus of an Enantiornithine Bird.

The first two eggshell fragments discussed, GPM-Fo-1923 and 09/Cr/89/01, are assigned to the Oofamily Testudoolithidae (i.e. Turtle Eggs). These fragments are approximately 5 x 6 mm and 3 x 3 mm, respectively, and are assumed to have come from the same egg, based upon cross-sections of the joint and the overall  shape of the fragments when jointed. However their precise origin is unclear, because they were collected by Masatoshi Okura, who has since passed away, and are now housed in separate museums. The outer surfaces of both shells are strongly abraded and show nodular patterns composed of tightly packed shell units. Based upon the curvature of the eggshell, the original egg would have been about 22 mm in diameter.

Eggshell assigned to Testudoolithidae. (GPM-Fo-1923). (A) Nodular outer surface with exposed shell units. (B) Radial thin section under normal light, showing discrete shell units (bracket), tubular pore canals (white arrowheads) and cratered bases (black arrowhead). The shell appears two-layered with an undulating boundary (arrow). (C) The same view as (B) under polarised light, exhibiting irregular extinction patterns. (D) Radial view, scanning electron microscope, showing discrete shell units (bracket) with ill-preserved ultrastructure. Uematsu et al. (2022).

These shells show two separate layers, separated by an undulating horizontal boundary. In the upper layer, needle-like crystals radiate outward from the boundary. Although less prominent, such acicular crystals are also found in the lower layer; the crystals develop concentrically from the organic cores, making the basal parts of the shell units rounded in shape. Under polarised light, the eggshell exhibits irregular extinction patterns. 

Turtle eggs typically have only a single layer, so the structure of the these eggshells, with two distinct layers, each with a different type of crystals, is distinctly unTestudine. Apparently double-layered Turtle eggshells can be produced taphonomically, by when two shell fragments happen to come to rest with one sitting inside the other, or as a result of a pathology - gravid female Turtles, suffering from some king of environmental stress, can retain eggs instead of laying them, depositing additional layers of minerals on the surface of the egg during the process. Neither of these appears to be the case in this instance, rather the eggs appear to have been altered diagenetically, with the outer portion of the shell having been recrystalised as a result of contact with external chemistry.

Based upon the morphology of these eggshell fragments, it is estimated that they were laid by a small Cryptodiran Turtle, with a carapace length of less than 200 mm.

The next five specimens, GPM-Fo-1294, 1295, 1296, 1297, and 1298 are placed within the Oofamily Prismatoolithidae, which is typified by a two-layered structure and an ornamented shell surface. They are assigned to a new oospecies, with GPM-Fo-1925 as the holotype, and given the name Ramoprismatoolithus okurai, where 'Ramoprismatoolithus' derives from 'Ramo-' from the Latin 'ramus', meaning branch, plus '-prismatoolithus', from the oofamily name, in reference to the reticulate ridges on the other surface of the eggshell, and 'okurai', honours the late Masatoshi Okura who pioneered the discovery of fossil eggshells and other Vertebrate remains in Shokawa.

All of these specimens are fragmentary; no intact examples of this new oospecies are known. The outer surface of these shells is distinctly sculpted, with low ridges arranged in elaborate reticulated patterns. The shells range from 0.31 to 0.61 mm in thickness, with the average being 0.46 mm. Seen under a scanning electron microscope, a near-vertical, unbranching, pore canal could be observed, increasing slightly in width towards the surface of the egg.

Ramoprismatoolithus. (A), (B) Eggshell outer surfaces showing the well-sculpted reticulation: (A) holotype: GPM-Fo-1925 and (B) a cast of GPM-Fo-1924 made of  silicone rubber. (C) Radial thin section under normal light, showing a mammillary layer (ML) and a prismatic layer (PL) with a gradual boundary (horizontal bar on the left side) (holotype: GPM-Fo-1925). (D) the same view as (C) under PLM, showing columnar extinction patterns. (E)–(G) Radial view under Scanning Electron Microscope (holotype: GPM-Fo-1925), displaying (E) ML and PL, (F) numerous vesicles (arrowhead) over the eggshell and (G) acicular crystals at the base of mammillae. (H) Straight pore canal under Scanning Electron Microscope (GPM￾Fo-1928). Uematsu et al. (2022).

These eggshells show two layers, which appears to be an original feature rather than something produced by diagenetic alteration, with a lower mammillary layer (the inner layer of many eggs, which is made up of small calcium carbonate crystals, which are easily disolved and provide a source of calcium for the growing embryo) and the upper prismatic layer (made up of larger crystals, which provides structural strength to the egg) observable. These are separated by a gradual boundary. The mammillary layer makes up about one fifth to one sixth of the shell's thickness, and is comprised of  acicular crystals radiating from what were presumably organic cores. The base of this layer is abraded, probably due to absorption of calcium by the growing embryo. The prismatic layer is made up of narrow, columnular crystals, visible under polarised light. Vesicles can be seen in this layer under the scanning electron microscope.

Based upon the thickness of the shell fragments, the original Ramoprismatoolithus okurai eggs are calculated to have had an average mass of 99.39 g, which assuming an egg twice as long as it is wide, would give an original size of about 57 x 133 mm.

Prismatoolithid eggs are generally accepted to have been laid by Troodontid Dinosaurs, as intact eggs assigned to the oofamily have been found with Troodontid embryos inside. However, it has been suggested that some eggs assigned to this oofamily might have been laid by early Birds.

The small estimated size of the Ramoprismatoolithus okurai eggs leads Uematsu et al. to conclude the Animal which laid them weighed somewhere between twelve and seventeen kilograms, small for a Theropod Dinosaur, but not implausible for a non-Avian Maniraptoran.

The final two specimens described are GPM-Fo-1929, an impression of part of an outer eggshell surface measuring 6 × 7 mm, and 09/Cr/88/07, a possible impression of part of an inner eggshell surface, measuring 2 x 2 mm. Neither of these specimens preserves any of the original eggshell material. The outer surface impression GPM-Fo-1929 bears a strong resemblance to the outer surface of the Ramoprismatoolithus okurai egg fragments, with reticulate ornamentation and the remains of several pore openings. The inner shell fragment impression, 09/Cr/88/07, is smooth, with no discerning features which would allow it to be associated with any known egg fossil.

Indeterminate eggshell impressions. (A) Outer surface impression (GPM-Fo-1929). (B) Cast of (A) made of silicone rubber, showing reticulate ornamentation similar to Ramoprismatoolithus and remains of pore openings (arrowheads) between the ridges. (C) Inner? surface impression with a smooth appearance (09/Cr/88/07). Uematsu et al. (2022).

The specimens described by Uematsu et al. are the oldest known fossil eggshells from Japan, and provide additional information on biodiversity within the Early Cretaceous Tetori Group, within which skeletal material is scarce, demonstrating that Turtles and small Dinosaurs were nesting in the area. 

The eggs assigned to Ramoprismatoolithus okurai are likely to have been laid by a Troodontid, or closely related Maniraptoran Theropod. Okurodani Formation yields teeth of possible Velociraptorinae, and other strata within the Tetori Group (likely to be roughly co-eval, but laid down in different environments within the same landscape) have produced possible Oviraptorosauria and Dromaeosauridae, as well as the Therizinosaur-related Fukuivenator paradoxus. However, all of these groups are known to produce non-prismatic shells with microstructures unlike that of the Oofamily Prismatoolithidae. This strongly suggests that the Ramoprismatoolithus okurai eggs were produced by a small Maniraptoran Theropod not represented in the skeletal fossil record of the Tetori Group. 

Troodontids, and basal Paravians (the group that includes Troodontids, Birds, and Dromaeosaurs) in general are scarce in Early Cretaceous deposits, both as skeletal and egg remains. Examples are known from the US, Spain, and China, and all Early Cretaceous small non-Avian Theropods known from East Asia come from two formations in northeastern China, the Yixian and Huajiying. Thus the discovery of the Ramoprismatoolithus okurai eggs in Japan is a significant contribution to our understanding of the distribution of mall non-Avian Theropods from the early Early Cretaceous of East Asia.

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