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Sarcosaurus

January 01, 1970

Not to be confused with Sarcolestes or Sarcosuchus.

Sarcosaurus (Latin: "flesh lizard") is a genus of basal neotheropod dinosaur, roughly 3.5 metres (11 ft) long. It lived in what is now England and maybe Ireland and Scotland during the Hettangian-Sinemurian stages of the Early Jurassic, about 199-196 million years ago. Sarcosaurus is one of the earliest known Jurassic theropods, and one of only a handful of theropod genera from this time period. Along with Dracoraptor hanigani it is one of the two described neotheropods from the lowermost Jurassic of the United Kingdom.[1]

Sarcosaurus
Temporal range: Hettangian-Sinemurian
~200–194 Ma
Skeletons of the known specimens of Sarcosaurus woodi (restored as a ceratosaur)
Scientific classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Clade: Neotheropoda
Genus: †Sarcosaurus
Andrews, 1921
Type species
†Sarcosaurus woodi
Andrews, 1921
Synonyms

Description edit

 
Size comparison of the two known partial skeletons of Sarcosaurus woodi (restored as a basal neotheropod)

The holotype is NHMUK PV R4840 a partial skeleton that includes a posterior dorsal vertebra, partial left and right ilia, that are fused to the proximal portion of the pubis, lacking the femoral head. The specimen shows some evidence of skeletal maturity, meaning it is not an early juvenile, but its exact ontogenetic stage cannot be ascertained.[1] Referred specimens include the non mature NHMUK PV R3542 (holotype of Sarcosaurus andrewsi) that includes a complete right tibia; WARMS G667–690, a partial skeleton of a single individual that includes posterior dorsal vertebra, middle caudal vertebra, dorsal rib fragments, left ilium, right and left pubes, femora and tibiae, proximal end of left fibula, probable distal half of fibula, distal portions of metatarsals IV, II or III proximal half of left pedal phalanx II-1, and three indeterminate bone fragments.[1][2] Sarcosaurus shares certain morphological conditions with other neotheropods, including Liliensternus liliensterni (collateral fossae of the metatarsal II with similar development and shape on both sides, larger ratio on the centrum) and Dilophosaurus wetherilli (lateral collateral fossa is bigger than the medial one in the metatarsal, middle caudal series proportionately lower and narrower than the middle−posterior dorsal vertebra). Sarcosaurus was a bipedal predator, probably able to run fast and catch small prey. The holotype belonged to a 3.5-metre-long animal whose weight was no greater than 50–60 kg. NHMUK PV R3542 belonged to a larger animal, estimated to have had a maximum length of 5 m and a weight of 140 kg.[3]

History of discovery edit

 
Pelvis and parts of femur and dorsal vertebra

The fossils of Sarcosaurus were found in the Lower Lias of England. The type species, Sarcosaurus woodi, was first described by Charles William Andrews in 1921 shortly after a partial skeleton had been found by S.L. Wood near Barrow-on-Soar, in the Scunthorpe Mudstone. The generic name is derived from Greek sarx, "flesh". The specific name honours Wood. The holotype, BMNH 4840/1, consists of a pelvis, a vertebra and the upper part of a femur. The preserved length of the femur is 31.5 centimetres (12.4 in).[4] A second species, Sarcosaurus andrewsi, was named by Friedrich von Huene in 1932,[5] based on a 445-millimetre (17.5 in) tibia, BMNH R3542, described by Arthur Smith Woodward in 1908 and found near Wilmcote.[6] Confusingly von Huene in the same publication named the very same fossil Magnosaurus woodwardi. Later he made a choice for S. andrewsi to be the valid name.[7] Huene also discussed WARMS G667–690, a partial skeleton also from Wilmcote, both specimens are from the Blue Lias. In 1974 S. andrewsi was reclassified as Megalosaurus andrewsi by Michael Waldman, on the probably erroneous assumption it was a megalosaurid.[8] A later study concluded the two species to be indistinguishable except for size, but other authors consider any identity to be unprovable as there are no comparable remains and conclude both species to lack autapomorphies and therefore to be nomina dubia.[9] Von Huene in 1932 referred a partial skeleton from the collection of the Warwick Museum to S. woodi but the identity was unproven; in 1995 it was given the informal name "Liassaurus"[10] but this has remained a nomen nudum. The specimen is likely one individual, located in the same stratiagraphic position as the holotypic specimen. Unfortunately, there are few available overlapping elements from the specimen and the holotype. Both specimens preserve a relatively complete femur: however, the features of both (an anteromedially directed head, a relatively long fourth trochanter and a trochanteric shelf) are plesiomorphic and thus do not indicate conspecifity or clade membership. It is noted, however, that there are no features which are present in one specimen but not the other. In 2020 WARMS G667–690 was given a comprehensive redescription, which proposed that all three specimens belonged to the same species, Sarcosaurus woodi.[1]

Between the years 1980 and 2000, three fossils were discovered on a beach near The Gobbins in Northern Ireland by palaeontologist Roger Byrne. Exact geologic provenance is not reported for any of the specimens, but the very dark colouration of the specimens indicate (through means of comparison to marine fossils in other Northern Irish localities) they hail from Lias Group rocks, likely from either the Planorbis Zone or the Pre-planorbis Zone of the Waterloo Mudstone Formation. Along specimens referred to Scelidosaurus a tibia was recovered, BELUM K12493, referred to an indeterminate neotheropod, probably related to Sarcosaurus or from an indeterminate megalosauroid. The scelidosaur femur and theropod tibia are the only known remains of dinosaurs from Ireland, which has a poor Mesozoic fossil record entirely consisting of marine localities, and the scelidosaur specimen was the first ever reported from the island.[11]

In 2023, a partial Theropod Specimen recovered from the lower Sinemurian Broadford Beds Formation of the Isle of Skye, previously referred to a Coelophysoid-grade theropod, was reclassified as Cf.Sarcosaurus, clading with Tachiraptor as a branch leading to Averostra. This specimen, NMS G.1994.10.1, consists on an isolated left tibia lacking its proximal region.[12]

Phylogeny edit

 
Sarcosaurus restored as a basal neotheropod

Andrews originally assigned Sarcosaurus to the Megalosauridae. The first to suggest a more basal position was Samuel Paul Welles who placed it in the Coelophysidae.[13] Later analyses resulted in either a position in the Ceratosauria,[14] or in the Coelophysoidea.[15] Ezcurra (2012) found Sarcosaurus to be the most basal ceratosaur in a large unpublished analysis.[16] In 2018, Andrea Cau in the large analysis of Saltriovenator found Sarcosaurus to be a dilophosaurid with good amount of support in the data.[17] In 2020, Ezcurra et al. recovered Sarcosaurus as a close relative of Averostra due to the presence of shared characters including an anteroventrally oriented ventral margin of the preacetabular process in lateral view on the ilium and a femur with a poorly posteriorly developed fourth trochanter. Their cladogram is shown below:[1] A latter work reinforced that clade made of Sarcosaurus woodi + (Tachiraptor admirabilis + Averostra).[12]

Palaeoenvironment edit

Holotype specimen was collected from strata (bucklandi zone, Sinemurian) that were deposited in epicontinental, shallow, marine settings affected by sea-level fluctuations and a warm, predominantly humid climate.[18] In south-western Warwickshire, is represented by the upper part of the Rugby Limestone Member (Hettangian-Sinemurian) of the Blue Lias Formation. with typical lithofacies of alternating mudrocks and generally fine-grained and frequently highly fossiliferous limestones.[19] the Rugby Limestone Member was deposited at a palaeolatitude of approximately 35° N in a storm-influenced offshore setting.[20] Wilmcote was related to the eastern margin of the Worcester Graben during the Early Jurassic and adjacent to the East Midlands Shelf.[21] The western margin of the emergent London Platform at 60–80 km to the south-east was probably the principal source of terrestrial biodebris.[22]

See also edit

References edit

  1. ^ a b c d e Ezcurra, M. D.; Butler, R. J.; Maidment, S. C. R.; Sansom, I. J.; Meade, L. E.; Radley, J. D. (2020). "A revision of the early neotheropod genus Sarcosaurus from the Early Jurassic (Hettangian–Sinemurian) of central England". Zoological Journal of the Linnean Society. 191: 113–149. doi:10.1093/zoolinnean/zlaa054. hdl:11336/160038.
  2. ^ Carrano, Matthew T.; Sampson, Scott D. (2004-09-27). "A review of coelophysoids (Dinosauria: Theropoda) from the Early Jurassic of Europe, with comments on the late history of the Coelophysoidea". Neues Jahrbuch für Geologie und Paläontologie – Monatshefte. 2004 (9): 537–558. doi:10.1127/njgpm/2004/2004/537. ISSN 0028-3630.
  3. ^ "List of Theropods", Dinosaur Facts and Figures, Princeton University Press, pp. 248–285, 2019-06-25, doi:10.2307/j.cdb2hnszb.15, S2CID 243596687, retrieved 2023-10-19
  4. ^ Andrews, Charles W. (1921). "LVI.—On some ramins of a Theropodous dinosaur from the Lower Lias of Barrow-on-Soa". Annals and Magazine of Natural History. 8 (47): 570–576. doi:10.1080/00222932108632620. ISSN 0374-5481.
  5. ^ Von Huene, F. (1932). "Die fossile Reptil-Ordnung Saurischia, ihre Entwicklung und Geschichte". Monographien zur Geologie und Paläontologie. 1 (4): 361. Retrieved 19 October 2023.
  6. ^ Woodward, A. Smith (1908). "Note on a Megalosaurian tibia from the lower Lias of Wilmcote, Warwickshire". Annals and Magazine of Natural History. 1 (3): 257–259. doi:10.1080/00222930808692397. ISSN 0374-5481.
  7. ^ Savage, Jay M.; von Huene, Friedrich R. Freiherr (1957-04-05). "Palaontologie und Phylogenie der Niederen Tetrapoden". Copeia. 1957 (1): 68. doi:10.2307/1440541. ISSN 0045-8511. JSTOR 1440541.
  8. ^ Waldman, M. (1974). "Megalosaurids from the Bajocian (Middle Jurassic) of Dorset". Paleontology. 17 (2): 325–339. Retrieved 19 October 2023.
  9. ^ Naish, Darren; Martill, David M. (2008-04-09). "Dinosaurs of Great Britain and the role of the Geological Society of London in their discovery: basal Dinosauria and Saurischia". Journal of the Geological Society. 165 (3): 613–623. doi:10.1144/0016-76492007-154. ISSN 0016-7649. S2CID 129624992.
  10. ^ Pickering, S. (1995). Jurassic Park: Unauthorized Jewish Fractals in Philopatry. A Fractal Scaling in Dinosaurology Project (2 ed.). Capitola. p. 478.{{cite book}}: CS1 maint: location missing publisher (link)
  11. ^ Simms, Michael J.; Smyth, Robert S.H.; Martill, David M.; Collins, Patrick C.; Byrne, Roger (2021). "First dinosaur remains from Ireland". Proceedings of the Geologists' Association. 132 (6): 771–779. Bibcode:2021PrGA..132..771S. doi:10.1016/j.pgeola.2020.06.005. S2CID 228811170.
  12. ^ a b Ezcurra, Martín D.; Marke, Daniel; Walsh, Stig A.; Brusatte, Stephen L. (2023). "A revision of the 'coelophysoid-grade' theropod specimen from the Lower Jurassic of the Isle of Skye (Scotland)". Scottish Journal of Geology. 59 (1): 012. Bibcode:2023ScJG...59...12E. doi:10.1144/sjg2023-012. hdl:20.500.11820/c9cde9ec-b458-42d3-a002-2b03ec6dbe54. S2CID 264343748.
  13. ^ Welles, S.P. (1984). "Dilophosaurus wetherilli (Dinosauria, Theropoda): osteology and comparisons". Palaeontographica Abteilung A. 185: 85–180. Retrieved 19 October 2023.
  14. ^ Gauthier, J. A. (1986). "Saurischian monophyly and the origin of birds". Memoirs of the California Academy of Sciences. 8 (1): 1–55. Retrieved 19 October 2023.
  15. ^ Carrano, Matthew T.; Hutchinson, John R.; Sampson, Scott D. (2005-12-30). "New information onSegisaurus halli, a small theropod dinosaur from the Early Jurassic of Arizona". Journal of Vertebrate Paleontology. 25 (4): 835–849. doi:10.1671/0272-4634(2005)025[0835:niosha]2.0.co;2. ISSN 0272-4634. S2CID 30039789.
  16. ^ Ezcurra, M. (2012). "Phylogenetic analysis of Late Triassic – Early Jurassic neotheropod dinosaurs: Implications for the early theropod radiation". Journal of Vertebrate Paleontology. Program and Abstracts. 32: 1–91.
  17. ^ Dal Sasso, Cristiano; Maganuco, Simone; Cau, Andrea (2018). "The oldest ceratosaurian (Dinosauria: Theropoda), from the Lower Jurassic of Italy, sheds light on the evolution of the three-fingered hand of birds". PeerJ. 6: e5976. doi:10.7717/peerj.5976. PMC 6304160. PMID 30588396.
  18. ^ Hesselbo, Stephen P. (2008). "Sequence stratigraphy and inferred relative sea-level change from the onshore British Jurassic". Proceedings of the Geologists' Association. 119 (1): 19–34. Bibcode:2008PrGA..119...19H. doi:10.1016/s0016-7878(59)80069-9. ISSN 0016-7878.
  19. ^ Ambrose, Keith (2001). "The lithostratigraphy of the Blue Lias Formation (Late Rhaetian—Early Sinemurian) in the southern part of the English Midlands". Proceedings of the Geologists' Association. 112 (2): 97–110. Bibcode:2001PrGA..112...97A. doi:10.1016/s0016-7878(01)80020-1. ISSN 0016-7878.
  20. ^ Weedon, Graham P.; Jenkyns, Hugh C.; Page, Kevin N. (2017-01-30). "Combined sea-level and climate controls on limestone formation, hiatuses and ammonite preservation in the Blue Lias Formation, South Britain (uppermost Triassic – Lower Jurassic)". Geological Magazine. 155 (5): 1117–1149. doi:10.1017/s001675681600128x. hdl:10026.1/8505. ISSN 0016-7568. S2CID 133014351.
  21. ^ Radley, J.D. (2003). "Warwickshire's Jurassic geology, past,present and future" (PDF). Mercian Geologist. 15 (1): 209–218. Retrieved 19 October 2023.
  22. ^ Cox, BM; Sumbler, MG; Ivimey-Cook, HC (1999). "A formational framework for the Lower Jurassic of England and Wales (onshore area)". British Geological Survey Research Report. 99 (1): 1–28. Retrieved 19 October 2023.

External links edit

  • Sarcosaurus in the Dino Directory

January 01, 1970
sarcosaurus, confused, with, sarcolestes, sarcosuchus, latin, flesh, lizard, genus, basal, neotheropod, dinosaur, roughly, metres, long, lived, what, england, maybe, ireland, scotland, during, hettangian, sinemurian, stages, early, jurassic, about, million, ye. Not to be confused with Sarcolestes or Sarcosuchus Sarcosaurus Latin flesh lizard is a genus of basal neotheropod dinosaur roughly 3 5 metres 11 ft long It lived in what is now England and maybe Ireland and Scotland during the Hettangian Sinemurian stages of the Early Jurassic about 199 196 million years ago Sarcosaurus is one of the earliest known Jurassic theropods and one of only a handful of theropod genera from this time period Along with Dracoraptor hanigani it is one of the two described neotheropods from the lowermost Jurassic of the United Kingdom 1 SarcosaurusTemporal range Hettangian Sinemurian 200 194 Ma PreꞒ Ꞓ O S D C P T J K Pg N Skeletons of the known specimens of Sarcosaurus woodi restored as a ceratosaur Scientific classification Domain Eukaryota Kingdom Animalia Phylum Chordata Clade Dinosauria Clade Saurischia Clade Theropoda Clade Neotheropoda Genus SarcosaurusAndrews 1921 Type species Sarcosaurus woodiAndrews 1921 Synonyms Magnosaurus woodi Andrews 1921 Huene 1932 Magnosaurus woodwardiHuene 1932 Megalosaurus Magnosaurus woodwardiHuene 1932 Sarcosaurus andrewsi Huene 1932 Megalosaurus andrewsi Huene 1932 Waldman 1972 Contents 1 Description 2 History of discovery 3 Phylogeny 4 Palaeoenvironment 5 See also 6 References 7 External linksDescription edit nbsp Size comparison of the two known partial skeletons of Sarcosaurus woodi restored as a basal neotheropod The holotype is NHMUK PV R4840 a partial skeleton that includes a posterior dorsal vertebra partial left and right ilia that are fused to the proximal portion of the pubis lacking the femoral head The specimen shows some evidence of skeletal maturity meaning it is not an early juvenile but its exact ontogenetic stage cannot be ascertained 1 Referred specimens include the non mature NHMUK PV R3542 holotype of Sarcosaurus andrewsi that includes a complete right tibia WARMS G667 690 a partial skeleton of a single individual that includes posterior dorsal vertebra middle caudal vertebra dorsal rib fragments left ilium right and left pubes femora and tibiae proximal end of left fibula probable distal half of fibula distal portions of metatarsals IV II or III proximal half of left pedal phalanx II 1 and three indeterminate bone fragments 1 2 Sarcosaurus shares certain morphological conditions with other neotheropods including Liliensternus liliensterni collateral fossae of the metatarsal II with similar development and shape on both sides larger ratio on the centrum and Dilophosaurus wetherilli lateral collateral fossa is bigger than the medial one in the metatarsal middle caudal series proportionately lower and narrower than the middle posterior dorsal vertebra Sarcosaurus was a bipedal predator probably able to run fast and catch small prey The holotype belonged to a 3 5 metre long animal whose weight was no greater than 50 60 kg NHMUK PV R3542 belonged to a larger animal estimated to have had a maximum length of 5 m and a weight of 140 kg 3 History of discovery edit nbsp Pelvis and parts of femur and dorsal vertebra The fossils of Sarcosaurus were found in the Lower Lias of England The type species Sarcosaurus woodi was first described by Charles William Andrews in 1921 shortly after a partial skeleton had been found by S L Wood near Barrow on Soar in the Scunthorpe Mudstone The generic name is derived from Greek sarx flesh The specific name honours Wood The holotype BMNH 4840 1 consists of a pelvis a vertebra and the upper part of a femur The preserved length of the femur is 31 5 centimetres 12 4 in 4 A second species Sarcosaurus andrewsi was named by Friedrich von Huene in 1932 5 based on a 445 millimetre 17 5 in tibia BMNH R3542 described by Arthur Smith Woodward in 1908 and found near Wilmcote 6 Confusingly von Huene in the same publication named the very same fossil Magnosaurus woodwardi Later he made a choice for S andrewsi to be the valid name 7 Huene also discussed WARMS G667 690 a partial skeleton also from Wilmcote both specimens are from the Blue Lias In 1974 S andrewsi was reclassified as Megalosaurus andrewsi by Michael Waldman on the probably erroneous assumption it was a megalosaurid 8 A later study concluded the two species to be indistinguishable except for size but other authors consider any identity to be unprovable as there are no comparable remains and conclude both species to lack autapomorphies and therefore to be nomina dubia 9 Von Huene in 1932 referred a partial skeleton from the collection of the Warwick Museum to S woodi but the identity was unproven in 1995 it was given the informal name Liassaurus 10 but this has remained a nomen nudum The specimen is likely one individual located in the same stratiagraphic position as the holotypic specimen Unfortunately there are few available overlapping elements from the specimen and the holotype Both specimens preserve a relatively complete femur however the features of both an anteromedially directed head a relatively long fourth trochanter and a trochanteric shelf are plesiomorphic and thus do not indicate conspecifity or clade membership It is noted however that there are no features which are present in one specimen but not the other In 2020 WARMS G667 690 was given a comprehensive redescription which proposed that all three specimens belonged to the same species Sarcosaurus woodi 1 Between the years 1980 and 2000 three fossils were discovered on a beach near The Gobbins in Northern Ireland by palaeontologist Roger Byrne Exact geologic provenance is not reported for any of the specimens but the very dark colouration of the specimens indicate through means of comparison to marine fossils in other Northern Irish localities they hail from Lias Group rocks likely from either the Planorbis Zone or the Pre planorbis Zone of the Waterloo Mudstone Formation Along specimens referred to Scelidosaurus a tibia was recovered BELUM K12493 referred to an indeterminate neotheropod probably related to Sarcosaurus or from an indeterminate megalosauroid The scelidosaur femur and theropod tibia are the only known remains of dinosaurs from Ireland which has a poor Mesozoic fossil record entirely consisting of marine localities and the scelidosaur specimen was the first ever reported from the island 11 In 2023 a partial Theropod Specimen recovered from the lower Sinemurian Broadford Beds Formation of the Isle of Skye previously referred to a Coelophysoid grade theropod was reclassified as Cf Sarcosaurus clading with Tachiraptor as a branch leading to Averostra This specimen NMS G 1994 10 1 consists on an isolated left tibia lacking its proximal region 12 Phylogeny edit nbsp Sarcosaurus restored as a basal neotheropod Andrews originally assigned Sarcosaurus to the Megalosauridae The first to suggest a more basal position was Samuel Paul Welles who placed it in the Coelophysidae 13 Later analyses resulted in either a position in the Ceratosauria 14 or in the Coelophysoidea 15 Ezcurra 2012 found Sarcosaurus to be the most basal ceratosaur in a large unpublished analysis 16 In 2018 Andrea Cau in the large analysis of Saltriovenator found Sarcosaurus to be a dilophosaurid with good amount of support in the data 17 In 2020 Ezcurra et al recovered Sarcosaurus as a close relative of Averostra due to the presence of shared characters including an anteroventrally oriented ventral margin of the preacetabular process in lateral view on the ilium and a femur with a poorly posteriorly developed fourth trochanter Their cladogram is shown below 1 A latter work reinforced that clade made of Sarcosaurus woodi Tachiraptor admirabilis Averostra 12 Theropoda Tawa Chindesaurus Eodromaeus Neotheropoda Coelophysoidea Zupaysaurus Gojirasaurus Cryolophosaurus Dilophosaurus Sarcosaurus Tachiraptor AverostraPalaeoenvironment editHolotype specimen was collected from strata bucklandi zone Sinemurian that were deposited in epicontinental shallow marine settings affected by sea level fluctuations and a warm predominantly humid climate 18 In south western Warwickshire is represented by the upper part of the Rugby Limestone Member Hettangian Sinemurian of the Blue Lias Formation with typical lithofacies of alternating mudrocks and generally fine grained and frequently highly fossiliferous limestones 19 the Rugby Limestone Member was deposited at a palaeolatitude of approximately 35 N in a storm influenced offshore setting 20 Wilmcote was related to the eastern margin of the Worcester Graben during the Early Jurassic and adjacent to the East Midlands Shelf 21 The western margin of the emergent London Platform at 60 80 km to the south east was probably the principal source of terrestrial biodebris 22 See also edit nbsp Dinosaurs portal Timeline of coelophysoid researchReferences edit a b c d e Ezcurra M D Butler R J Maidment S C R Sansom I J Meade L E Radley J D 2020 A revision of the early neotheropod genus Sarcosaurus from the Early Jurassic Hettangian Sinemurian of central England Zoological Journal of the Linnean Society 191 113 149 doi 10 1093 zoolinnean zlaa054 hdl 11336 160038 Carrano Matthew T Sampson Scott D 2004 09 27 A review of coelophysoids Dinosauria Theropoda from the Early Jurassic of Europe with comments on the late history of the Coelophysoidea Neues Jahrbuch fur Geologie und Palaontologie Monatshefte 2004 9 537 558 doi 10 1127 njgpm 2004 2004 537 ISSN 0028 3630 List of Theropods Dinosaur Facts and Figures Princeton University Press pp 248 285 2019 06 25 doi 10 2307 j cdb2hnszb 15 S2CID 243596687 retrieved 2023 10 19 Andrews Charles W 1921 LVI On some ramins of a Theropodous dinosaur from the Lower Lias of Barrow on Soa Annals and Magazine of Natural History 8 47 570 576 doi 10 1080 00222932108632620 ISSN 0374 5481 Von Huene F 1932 Die fossile Reptil Ordnung Saurischia ihre Entwicklung und Geschichte Monographien zur Geologie und Palaontologie 1 4 361 Retrieved 19 October 2023 Woodward A Smith 1908 Note on a Megalosaurian tibia from the lower Lias of Wilmcote Warwickshire Annals and Magazine of Natural History 1 3 257 259 doi 10 1080 00222930808692397 ISSN 0374 5481 Savage Jay M von Huene Friedrich R Freiherr 1957 04 05 Palaontologie und Phylogenie der Niederen Tetrapoden Copeia 1957 1 68 doi 10 2307 1440541 ISSN 0045 8511 JSTOR 1440541 Waldman M 1974 Megalosaurids from the Bajocian Middle Jurassic of Dorset Paleontology 17 2 325 339 Retrieved 19 October 2023 Naish Darren Martill David M 2008 04 09 Dinosaurs of Great Britain and the role of the Geological Society of London in their discovery basal Dinosauria and Saurischia Journal of the Geological Society 165 3 613 623 doi 10 1144 0016 76492007 154 ISSN 0016 7649 S2CID 129624992 Pickering S 1995 Jurassic Park Unauthorized Jewish Fractals in Philopatry A Fractal Scaling in Dinosaurology Project 2 ed Capitola p 478 a href Template Cite book html title Template Cite book cite book a CS1 maint location missing publisher link Simms Michael J Smyth Robert S H Martill David M Collins Patrick C Byrne Roger 2021 First dinosaur remains from Ireland Proceedings of the Geologists Association 132 6 771 779 Bibcode 2021PrGA 132 771S doi 10 1016 j pgeola 2020 06 005 S2CID 228811170 a b Ezcurra Martin D Marke Daniel Walsh Stig A Brusatte Stephen L 2023 A revision of the coelophysoid grade theropod specimen from the Lower Jurassic of the Isle of Skye Scotland Scottish Journal of Geology 59 1 012 Bibcode 2023ScJG 59 12E doi 10 1144 sjg2023 012 hdl 20 500 11820 c9cde9ec b458 42d3 a002 2b03ec6dbe54 S2CID 264343748 Welles S P 1984 Dilophosaurus wetherilli Dinosauria Theropoda osteology and comparisons Palaeontographica Abteilung A 185 85 180 Retrieved 19 October 2023 Gauthier J A 1986 Saurischian monophyly and the origin of birds Memoirs of the California Academy of Sciences 8 1 1 55 Retrieved 19 October 2023 Carrano Matthew T Hutchinson John R Sampson Scott D 2005 12 30 New information onSegisaurus halli a small theropod dinosaur from the Early Jurassic of Arizona Journal of Vertebrate Paleontology 25 4 835 849 doi 10 1671 0272 4634 2005 025 0835 niosha 2 0 co 2 ISSN 0272 4634 S2CID 30039789 Ezcurra M 2012 Phylogenetic analysis of Late Triassic Early Jurassic neotheropod dinosaurs Implications for the early theropod radiation Journal of Vertebrate Paleontology Program and Abstracts 32 1 91 Dal Sasso Cristiano Maganuco Simone Cau Andrea 2018 The oldest ceratosaurian Dinosauria Theropoda from the Lower Jurassic of Italy sheds light on the evolution of the three fingered hand of birds PeerJ 6 e5976 doi 10 7717 peerj 5976 PMC 6304160 PMID 30588396 Hesselbo Stephen P 2008 Sequence stratigraphy and inferred relative sea level change from the onshore British Jurassic Proceedings of the Geologists Association 119 1 19 34 Bibcode 2008PrGA 119 19H doi 10 1016 s0016 7878 59 80069 9 ISSN 0016 7878 Ambrose Keith 2001 The lithostratigraphy of the Blue Lias Formation Late Rhaetian Early Sinemurian in the southern part of the English Midlands Proceedings of the Geologists Association 112 2 97 110 Bibcode 2001PrGA 112 97A doi 10 1016 s0016 7878 01 80020 1 ISSN 0016 7878 Weedon Graham P Jenkyns Hugh C Page Kevin N 2017 01 30 Combined sea level and climate controls on limestone formation hiatuses and ammonite preservation in the Blue Lias Formation South Britain uppermost Triassic Lower Jurassic Geological Magazine 155 5 1117 1149 doi 10 1017 s001675681600128x hdl 10026 1 8505 ISSN 0016 7568 S2CID 133014351 Radley J D 2003 Warwickshire s Jurassic geology past present and future PDF Mercian Geologist 15 1 209 218 Retrieved 19 October 2023 Cox BM Sumbler MG Ivimey Cook HC 1999 A formational framework for the Lower Jurassic of England and Wales onshore area British Geological Survey Research Report 99 1 1 28 Retrieved 19 October 2023 External links editSarcosaurus in the Dino Directory Retrieved from https en wikipedia org w index php title Sarcosaurus amp oldid 1220047819, wikipedia, wiki, book, books, library,

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