Early Ageing and Alzheimer's Pterosaurs Shows That the Holotype Is One of the Best-Preserved Individuals in Exis­ SIR - Mattson Et Ai

Total Page:16

File Type:pdf, Size:1020Kb

Early Ageing and Alzheimer's Pterosaurs Shows That the Holotype Is One of the Best-Preserved Individuals in Exis­ SIR - Mattson Et Ai SCIENTIFIC CORRESPONDENCE process was advanced to the point that it ton corresponds almost exactly to that Sharov'sl plate 4. Impressions of the flight had become detached. In the photographs exhibited by complete, undisturbed exam­ membrane, the posterior boundary of (Fig. la of ref. 2), neither wing membrane ples of Rhamphorhynchus, from the Upper which is evident in Sharov'sl plate 5, Fig. clearly indicates where it was attached to Jurassic Solnhofen limestonelO. However, la, show that the right cheiropatagium the leg, although illustrationsl.2 of the the evidence for soft tissues, especially the remained intact and did not undergo any right wing show an imprint identical in extent and structure of the wing mem­ post-mortem transport. The wings occupy shape and position to that of the left wing. branes, is much clearer in Sordes. The wing almost identical positions, as Sharov This observation may be suspect because, membranes of Solnhofen pterosaurs are correctly showedl, but the outline of the 3 as reconstructed here, the left wing may preserved as impressions , ,9,10, but even right cheiropatagium is more difficult to have originally attached near the knee. the best examples can be interpreted in a trace in photographs because of the I can accept that a membrane may have variety of ways3,4.11. The decomposition of patchy preservation of the black, mineral­ spanned from the lateral digits to either Sordes was halted at an earlier stage than ized tissues in this area. side of the tail (it would not impede in Solnhofen pterosaurs: extensive tracts Peters' reconstruction also fails to terrestrial locomotion), but I question of black, mineralized soft tissues8 pick out explain the unusual morphology and 2 how a membrane spanning the legs and impressions left by the wing membranes. position of the fifth toe ,S,12 and is attached medially can also be attached to Outlines of the wings can be traced with contradicted by details of the internal the lateral digits. The image of pterosaurs ease and show, quite unambiguously, the composition of the membranes. The with broad bat-like wing membranes is existence of a uropatagium and attach­ uropatagium, preserved in three other traditional, but at least two Solnhofen ment of the cheiropatagium to the leg as individuals as well as the holotype, con­ 3 l specimens ,4.7 were preserved with very far as the ankle ,2,8. tains relatively short, sinuous, loosely narrow wings stretched only between the Peters' narrow-winged reconstruction packed fibres, clearly distinguishing it elbow and wing finger. Thus, either Sordes of Sordes is based on a highly unreliable from the middle and outer parts of the is different from these specimens, or pre­ technique, interpretation of photographs, cheiropatagium, which is characterized l vious interpretations ,2 are in error. and unfounded suppositions of post­ by much longer, straighter, closely pack­ 2 David Peters mortem disturbance. Central to his argu­ ed fibres • 12812 Wood Valley Court, St Louis, ment is the claim that the uropatagium is David M. Unwin Missouri 63131-2051, USA part of the right cheiropatagium which, Department of Geology, somehow, drifted into a symmetrical posi­ University of Bristol, UNWIN AND BAKHURINA REPLY - Recon­ tion between the hindlimbs, the internal Bristol BS8 1RJ, UK structions of the Upper Jurassic pterosaur fibres fortuitously lining up parallel to the Natasha N. Bakhurina* Sordes pilosus with broad wings attaching lower leg. However, Peters' interpretation Palaeontological Institute, to the hindlimbs and a medial membrane, (his figure b) omits parts of the central Russian Academy of Sciences, the uropatagium, between the legsl), have region of the right cheiropatagium, pre­ Moscow 117647, Russia 4 , been challenged by Peters, and others on served lateral to the right knee and clearly *Present address: Department of Geology, University of the grounds that preservation of the visible together with the uropatagium in Bristol. remains is too poor to permit such infer­ ences. However, comparison of Sordes with other exceptionally preserved Early AGEing and Alzheimer's pterosaurs shows that the holotype is one of the best-preserved individuals in exis­ SIR - Mattson et ai. suggese that in enhances the aggregation of 1: or amy­ tence2,s. As originally interred, the skele­ Alzheimer's disease "glycation is a late loid-~9 into neurofibrillary tangles and ton was complete and fully articulated, event" and that it "results from free senile plaques. Therefore, a contribution with the neck flexed backward as in some radical generation". Despite their cita­ of glycoxidation modifications early, as 9 Solnhofen pterosaurs • Each forelimb is tion of some of our papers to support well as later, in the pathogenesis of 2 4 partially folded and, although parts of the their view - , their opinion is directly Alzheimer's disease should be seriously left forelimb were lost during collection, it contrary to the findings that the protein considered. is evident that, like the hindlimbs, they are PHF-1:/A68, regarded as the precursor Mark A. Smith* S almost perfectly symmetrical with respect to neurofibrillary tangles , is modified Lawrence M. Sayre* to each other, contradicting claims of by advanced glycation end products Michael P. Vitekt post-mortem disturbance. (AGE)2.6. Vincent M. Monnier* Interestingly, the position of the skele- We have also demonstrated that AGE George Perry* epitopes localize to diffuse amyloid-~ *Institute of Pathology, 1. Sharov. A.G. Akad. nauk SSSR pa/eont. Inst. Tr. 130, senile plaques' (lesions that represent Case Western Reserve University, 104-113 (1971). one of the earliest pathological changes Cleveland, Ohio 44106, USA 2. Unwin, D. M. & Bakhurina, N. N. Nature 371, 62-64 7 ), (1994). in Alzheimer's disease as well as tThe Picower Institute, 3. Welinhofer, P. Ann. Naturhist. Mus. Wien 88A, 149-162 neurofibrillary tangles and neuritic senile Manhasset, (1987). plaques. Moreover, the proteins found in New York 11030, USA 4. Padian, K. & Rayner. J. M. V. Am. J. Sci. 293A, 91-166 (1993). these lesions are continuously exposed to 1. Mattson, M. P., Carney, J. W. & Butterfield, D. A. Nature 5. Gekker, R. F. Trudy paleont. Inst. 15, 7-85 (1948) (in glucose in vivo and therefore constantly 373, 481 (1995). Russian). 2. Yan, S. D. et al. Proc. natn. Acad. Sci. U.S.A. 91, 6. Doludenko, M. p" Sakulina, G,V. & Ponomarenko, A.G. subject to Schiff base formation follow­ 7787-7791 (1994). The Geology and Late Jurassic Fauna and Flora of a ed by Amadori rearrangements and Unique Locality, Au/Ie (Karatau Range, Southern 3. Smith, M. A. et al. Proc. natn. Acad. Sci. U.S.A. 91, Kazakhstan) (Inst. Geol., Russian Acad. Sci., Moscow, AGE modification. Of relevance is that 5710-5714 (1994). 1990) (in Russian). intracellular AGE modification, contrary 4. Vitek, M. P. et a/. Proc. natn. Acad. Sci. U.S.A. 91, 7. Welinhofer, P. The Illustrated Encyclopedia of Pterosaurs to popular dogma, often occurs very 4766-4770 (1994). 1-192 (Salamander. London, 1991). 5. Trojanowski, J. Q. & Lee, V. M. Am. J. Path. 144, 8. Bakhurina, N. N. & Unwin, D. M. Hist. Bioi. (in the rapidly8. 449-453 (1994). press). Rather than representing a tombstone 6. Ledesma, M. D. et a/. J. bioi. Chern. 269, 9. Wellnhofer, P Abh. bayer. Akad. Wiss. (N.F.) 141,1-133 21614-21619 (1994). (1970). or late event, the process resulting in gly­ 7. Giaccone, G. et al. Neurosci. Lett. 97, 232-238 (1989). 10. Welinhofer, P. Palaeontographica149, 1-30 (1975). cation-related modification appears to 8. Giardino, I., Edelstein, D. & Brownlee, M. J. elin. Invest. 11. Pennycuick, C. J. Bioi. Rev. 63, 209-231 (1988). 94, 110-117 (1994). 12. Bakhurina, N. N. & Unwin, D. M. J. vert. Pafeont. 12 represent a very early event that pro­ 9. Hunt, J. V. & Wolff, S. P. Free Radie. Res. Commun. 9 (Suppl.), 18A (1992). motes the formation of free radicals and 12-13,115-123 (1991). 316 NATURE· VOL 374 . 23 MARCH 1995 .
Recommended publications
  • The Wingtips of the Pterosaurs: Anatomy, Aeronautical Function and Palaeogeography, Palaeoclimatology, Palaeoecology Xxx (2015) Xxx Xxx 3 Ecological Implications
    Our reference: PALAEO 7445 P-authorquery-v11 AUTHOR QUERY FORM Journal: PALAEO Please e-mail your responses and any corrections to: Article Number: 7445 E-mail: [email protected] Dear Author, Please check your proof carefully and mark all corrections at the appropriate place in the proof (e.g., by using on-screen annotation in the PDF file) or compile them in a separate list. Note: if you opt to annotate the file with software other than Adobe Reader then please also highlight the appropriate place in the PDF file. To ensure fast publication of your paper please return your corrections within 48 hours. For correction or revision of any artwork, please consult http://www.elsevier.com/artworkinstructions. We were unable to process your file(s) fully electronically and have proceeded by Scanning (parts of) your Rekeying (parts of) your article Scanning the article artwork Any queries or remarks that have arisen during the processing of your manuscript are listed below and highlighted by flags in the proof. Click on the ‘Q’ link to go to the location in the proof. Location in article Query / Remark: click on the Q link to go Please insert your reply or correction at the corresponding line in the proof Q1 Your article is registered as a regular item and is being processed for inclusion in a regular issue of the journal. If this is NOT correct and your article belongs to a Special Issue/Collection please contact [email protected] immediately prior to returning your corrections. Q2 Please confirm that given names and surnames have been identified correctly.
    [Show full text]
  • Griffith Park Pterosaurs and Sordes Pilosus,Griffith
    Griffith Park Pterosaurs and Sordes Pilosus The Sordes pilosus has been tied to both sightings, in 2013, near Griffith Park: March 3rd and May 13th. The more striking survey results were from the first sighting, near the Colorado Street bridge for the Interstate-5, and just a little southeast of the Los Angeles Zoo. From the thirty-five silhouette images of pterosaurs, birds, and bats, the anonymous eyewitness chose only one: the Sordes pilosus. She did mention that the head was larger than what she saw in the silhouette image. That March 3rd sighting was also noteworthy for the number of flying creatures: three. Only about 1% of sightings involve more than two apparent pterosaurs, according to the data I compiled late in 2012. Also noteworthy for this sighting is the clarity of the tail observation. The eyewitness clear about those long thin tails that ended with a structure that I associate with the Rhamphorhynchoid tail flange. From the data compiled late in 2012, 28.5% of all the sighting include reference to that tail structure. The second sighting, on May 13th, was by Devin Rhodriquez, about 1.5 miles south of the first one. In this case, the eyewitness was so focused on the head that she did not notice the presence or absence of a tail on the flying creature. She was sure about the absence of feathers, but was open-minded in questioning the possibility that she had observed a pterosaur. Rhodriquez was given the same survey form as the first eyewitness; she chose six images:Sordes pilosus, Campylognathoides, Dimorphodon, Peteinosaurus, Scaphognathus, and Quetzalcoatlus.
    [Show full text]
  • On Two Pterosaur Humeri from the Tendaguru Beds (Upper Jurassic, Tanzania)
    “main” — 2009/10/20 — 22:40 — page 813 — #1 Anais da Academia Brasileira de Ciências (2009) 81(4): 813-818 (Annals of the Brazilian Academy of Sciences) ISSN 0001-3765 www.scielo.br/aabc On two pterosaur humeri from the Tendaguru beds (Upper Jurassic, Tanzania) FABIANA R. COSTA and ALEXANDER W.A. KELLNER Museu Nacional, Universidade Federal do Rio de Janeiro, Departamento de Geologia e Paleontologia Quinta da Boa Vista s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brasil Manuscript received on August 17, 2009; accepted for publication on September 30, 2009; contributed by ALEXANDER W.A. KELLNER* ABSTRACT Jurassic African pterosaur remains are exceptionally rare and only known from the Tendaguru deposits, Upper Jurassic, Tanzania. Here we describe two right humeri of Tendaguru pterosaurs from the Humboldt University of Berlin: specimens MB.R. 2828 (cast MN 6661-V) and MB.R. 2833 (cast MN 6666-V). MB.R. 2828 consists of a three- dimensionally preserved proximal portion. The combination of the morphological features of the deltopectoral crest not observed in other pterosaurs suggests that this specimen belongs to a new dsungaripteroid taxon. MB.R. 2833 is nearly complete, and because of a long and round proximally placed deltopectoral crest it could be referred to the Archaeopterodactyloidea. It is the smallest pterosaur from Africa and one of the smallest flying reptiles ever recorded. These specimens confirm the importance of the Tendaguru deposits for the Jurassic pterosaur record. This potential, however, has to be fully explored with more field work. Key words: Tendaguru, Tanzania, Africa, Upper Jurassic, Pterosauria. INTRODUCTION in providing isolated remains up to now (Kellner and Mader 1997, Wellnhofer and Buffetaut 1999, Mader Africa shows a great potential for pterosaur material and Kellner 1999).
    [Show full text]
  • New Information on the Tapejaridae (Pterosauria, Pterodactyloidea) and Discussion of the Relationships of This Clade
    AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 41 (4): 521-534. Buenos Aires, 30-12-2004 ISSN 0002-7014 New information on the Tapejaridae (Pterosauria, Pterodactyloidea) and discussion of the relationships of this clade Alexander Wilhelm Armin KELLNER1 Abstract. A phylogenetic analysis indicates that the Tapejaridae is a monophyletic group of pterodactyloid pterosaurs, diagnosed by the following synapomorphies: premaxillary sagittal crest that starts at the anterior tip of the premaxilla and extends posteriorly after the occipital region, large nasoantorbital fenestra that reaches over 45% of the length between premaxilla and squamosal, lacrimal process of the jugal thin, distinct small pear- shaped orbit with lower portion narrow, and broad tubercle at the ventroposterior margin of the coracoid. Several cranial and postcranial characters indicate that the Tapejaridae are well nested within the Tapejaroidea, in sister group relationship with the Azhdarchidae. A preliminary study of the ingroup relationships within the Tapejaridae shows that Tupuxuara is more closely related to Thalassodromeus relative to Tapejara. At present tape- jarid remains have been found in the following deposits: Crato and Romualdo members of the Santana Formation (Aptian-Albian), Araripe Basin, Brazil; Jiufotang Formation (Aptian), Jehol Group of western Liaoning, China; and in the redbeds (Cenomanian) of the Kem Kem region, Morocco. An incomplete skull found in the Javelina Formation (Maastrichtian), Texas also shows several tapejarid features and might be a member of this clade. Although information is still limited, the present distribution of the Tapejaridae indicates that this clade of pterosaurs was not exclusive of Gondwana, and was more widespread than previously known. Resumen. NUEVA INFORMACIÓN SOBRE LOS TAPEJARIDAE (PTEROSAURIA, PTERODACTYLOIDEA) Y DISCUSIÓN SOBRE LAS RELACIONES DE ESTE CLADO.
    [Show full text]
  • The Wingtips of the Pterosaurs: Anatomy, Aeronautical Function and Ecological Implications Hone, DWE; Van Rooijen, MK; Habib, MB
    CORE Metadata, citation and similar papers at core.ac.uk Provided by Queen Mary Research Online The wingtips of the pterosaurs: Anatomy, aeronautical function and ecological implications Hone, DWE; Van Rooijen, MK; Habib, MB doi:10.1016/j.palaeo.2015.08.046 For additional information about this publication click this link. http://qmro.qmul.ac.uk/xmlui/handle/123456789/10947 Information about this research object was correct at the time of download; we occasionally make corrections to records, please therefore check the published record when citing. For more information contact [email protected] Our reference: PALAEO 7445 P-authorquery-v11 AUTHOR QUERY FORM Journal: PALAEO Please e-mail your responses and any corrections to: Article Number: 7445 E-mail: [email protected] Dear Author, Please check your proof carefully and mark all corrections at the appropriate place in the proof (e.g., by using on-screen annotation in the PDF file) or compile them in a separate list. Note: if you opt to annotate the file with software other than Adobe Reader then please also highlight the appropriate place in the PDF file. To ensure fast publication of your paper please return your corrections within 48 hours. For correction or revision of any artwork, please consult http://www.elsevier.com/artworkinstructions. We were unable to process your file(s) fully electronically and have proceeded by Scanning (parts of) your Rekeying (parts of) your article Scanning the article artwork Any queries or remarks that have arisen during the processing of your manuscript are listed below and highlighted by flags in the proof.
    [Show full text]
  • Recent Progress in the Study of Pterosaurs from China
    BCAS Vol.24 No.2 2010 Recent Progress in the Study of Pterosaurs from China WANG Xiaolin1*, JIANG Shunxing1, MENG Xi1 and CHENG Xin1,2 1 Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, CAS, Beijing 100044, China 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China terosaurs are the earliest vertebrates known to be in the study of pterosaurs from China. able to fly in the sky. They existed from the Late PTriassic to the end of the Cretaceous (about 220 to 65 The smallest, swallow-sized arboreal million years ago), when the land was ruled by another kind pterosaur of reptile—dinosaurs. Pterosaurs consist of the long-tailed Rhamphorhynchoidea and the short-tailed Pterodactyloidea. Can you imagine a pterosaur as tiny as a swallow? It The former is a basal group and the latter is more derived. did exist about 120 million years ago. Despite representing Before the 1990s, there was sporadic pterosaur record an immature individual, Nemicolopterus crypticus (Wang in China. Young Chung-chien (C. C. Young), the doyen of et al., 2008) is neither a hatching nor a newborn based on Chinese vertebrate paleontology, reported the first Chinese the ossification of the skeleton. With a wingspan of 25 cm, pterosaur bones from Laiyang of Shandong Province in it is only slightly bigger than a newborn from the Solnhofen 1958. Later, a number of pterosaurs were described such Limestone, which has a wingspan of 18 mm. This makes it as Dsungaripterus weii, Noripterus complicidens from the smallest pterosaur so far known in the world.
    [Show full text]
  • Pterosaur Cladogram 233 Taxa
    Pterosaur Cladogram 233 taxa - 184 characters - Peters 2017 78 Jianchangnathus Huehuecuetzpalli Sordes 2585 3 Macrocnemus BES SC111 79 96 Macrocnemus T4822 Pterorhynchus Macrocnemus T2472 67 100 Changchengopterus PMOL Dinocephalosaurus 89 Wukongopterus Amotosaurus 98 89 95 Archaeoistiodactylus Fuyuansaurus 82 97 Kunpengopterus 95 100 Tanystropheus MSNM BES SC1018 Darwinopterus AMNH M8802 Tanystropheus T/2819 81 97 Darwinopterus modularis ZMNH M 8782 82 Langobardisaurus 97 59 Darwinopterus robustodens 41H111-0309A Tanytrachelos 100 Darwinopterus linglongtaensis IVPP V 16049 Darwinopterus YH2000 89 Cosesaurus 100 Sharovipteryx Longisquama Scaphognathus crassirostris 100 62 Scaphognathus SMNS 59395 Bergamodactylus MPUM 6009 Scaphognathus Maxberg sp. 99 Raeticodactylus 97 Austriadactylus SMNS 56342 83 TM 13104 Austriadactylus SC332466 79 Gmu10157 98 BM NHM 42735 77 Preondactylus 100 100 BSp 1986 XV 132 94 MCSNB 2887 ELTE V 256-Pester specimen Dimorphodon macronyx 78 97 95 99 B St 1936 I 50 (n30) Peteinosaurus Ex3359 Cycnorhamphus 94 Carniadactylus 97 99 99 Moganopterus 93 MCSNB 8950 Feilongus 91 74 Dimorphodon? weintraubi 91 71 IVPP V13758 embryo Yixianopterus Mesadactylus holotype 100 77 JZMP embryo 96 100 Haopterus Dendrorhynchoides Boreopterus 96 73 88 97 JZMP-04-07-3 Zhenyuanopterus SMNS 81928 flathead 100 80 98 Hamipterus 97 Anurognathus Arthurdactylus 69 81 CAG IG 02-81 SMNK PAL 3854 95 PIN 2585/4 flightless anurognthid 86 Ikrandraco 87 Batrachognathus 98 98 79 Coloborhynchus spielbergi 89 Daohugoupterus Criorhynchus Jeholopterus 64
    [Show full text]
  • Evolution of Morphological Disparity in Pterosaurs Katherine C
    Journal of Systematic Palaeontology, Vol. 9, Issue 3, September 2011, 337–353 Evolution of morphological disparity in pterosaurs Katherine C. Prentice, Marcello Ruta∗ and Michael J. Benton School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK (Received 9 November 2009; accepted 22 October 2010; printed 15 September 2011) Pterosaurs were important flying vertebrates for most of the Mesozoic, from the Late Triassic to the end of the Cretaceous (225–65 Ma). They varied enormously through time in overall size (with wing spans from about 250 mm to about 12 m), and in features of their cranial and postcranial skeletons. Comparisons of disparity based on discrete cladistic characters show that the basal paraphyletic rhamphorhynchoids (Triassic–Early Cretaceous) occupied a distinct, and relatively small, region of morphospace compared to the derived pterodactyloids (Late Jurassic–Late Cretaceous). This separation is unexpected, especially in view of common constraints on anatomy caused by the requirements of flight. Pterodactyloid disparity shifted through time, with different, small portions of morphospace occupied in the Late Jurassic and Late Cretaceous, and a much larger portion in the Early Cretaceous. This explosion in disparity after 100 Ma of evolution is matched by the highest diversity of the clade: evidently, pterosaurs express a rather ‘top heavy’ clade shape, and this is reflected in delayed morphological evolution, again an unexpected finding. The expansion of disparity among pterodactyloids was comparable across subclades: pairwise comparisons among the four pterodactyloid superfamilies show that, for the most part, these clades display significant morphological separation, except in the case of Dsungaripteroidea and Azhdarchoidea.
    [Show full text]
  • The Earliest Pterodactyloid and the Origin of the Group
    Current Biology 24, 1011–1016, May 5, 2014 ª2014 Elsevier Ltd All rights reserved http://dx.doi.org/10.1016/j.cub.2014.03.030 Report The Earliest Pterodactyloid and the Origin of the Group Brian Andres,1,* James Clark,2 and Xing Xu3 In previous phylogenetic analyses, the Pterodactyloidea 1School of Geosciences, University of South Florida, Tampa, have traditionally had the longest branch in terms of apomor- FL 33620, USA phy number [5] and temporal duration of gaps without fossils 2Department of Biological Sciences, George Washington implied by phylogeny [4]. This long branch was hypothesized University, Washington, DC 10024, USA to be the result of the pterodactyloids originating in terrestrial 3Key Laboratory of Vertebrate Evolution and Human Origins, environments [1, 2], where the pterosaur fossil record has Institute of Vertebrate Paleontology and Paleoanthropology, historically been undersampled [1]. Due in part to the fragile Chinese Academy of Sciences, Beijing 100044, China construction of their skeletons, pterosaurs have been predom- inantly preserved in quiet marine environments [7], to such an extent that they were hypothesized to have been an almost Summary exclusively marine group [8, 9]. A number of terrestrial de- posits from China have yielded new pterosaurs in recent The pterosaurs were a diverse group of Mesozoic flying rep- years [10, 11], but when preservation in terrestrial or marine tiles that underwent a body plan reorganization, adaptive ra- environments is reconstructed for previous pterosaur phy- diation, and replacement of earlier forms midway through logenies, they still support a predominantly marine history their long history, resulting in the origin of the Pterodacty- for the pterosaurs and a marine origin of the Pterodactyloidea loidea, a highly specialized clade containing the largest (see Table S1 available online).
    [Show full text]
  • Pterosaurs Or Flying Reptiles Were the First Vertebrates to Evolve Flight
    Veldmeijer, Witton & Nieuwland André J. Veldmeijer PTEROSAURS Mark Witton & Ilja Nieuwland Pterosaurs or flying reptiles were the first vertebrates to evolve flight. These distant relatives of modern reptiles and dinosaurs lived from the Late Triassic (over 200 million years ago) to the end of the Cretaceous (about 65 million years ago) a span of some 135 million years. When they became extinct, no relatives survived them and as a result these prehistoric animals cannot readily be compared to our modern-day fauna. So what do we know about these highly succsessful animals? The present summary answers this and many more questions based on the most recent results of modern scientific research. After a short introduction into palaeontology as a science, and the history of pterosaur study, it explains what pterosaurs were, when and where they lived, and what they looked like. Topics such as disease, injury and reproduction are also discussed. Separated from this text are ‘Mark explains’ boxes. Each of these explanations puts one specific species in the spotlight and focuses on its lifestyle. They show the diversity of pterosaurs, from small insectivorous animals with a wingspan of nearly 40 centimetres to the biggest flying animals ever to take to the air, with wingspans of over 10 metres and a way of life comparable to modern-day storks. The text is illustrated with many full-colour photographs and beautiful PTEROSAURS palaeo-art prepared by experts in the field. Dr. André J. Veldmeijer is an archaeologist and palaeontologist (PhD Utrecht University, The Netherlands). He is specialised in the big, toothed pterosaurs of the Cretaceous.
    [Show full text]
  • Pterosaur Cladogram 259 Taxa
    Pterosaur Cladogram 260 taxa - 183 characters - Peters 2021 Huehuecuetzpalli Macrocnemus BES SC111 Macrocnemus T4822 Macrocnemus T2472 Dinocephalosaurus Jianchangnathus Amotosaurus Sordes 2585 3 Fuyuansaurus Skye Middle Jurassic pterosaur Tanystropheus MSNM BES SC1018 Pterorhynchus Tanystropheus T/2819 Changchengopterus PMOL Langobardisaurus Wukongopterus Tanytrachelos Hongshanopterus Archaeoistiodactylus Cosesaurus Kunpengopterus sinensis Kyrgyzsaurus Kunpengopterus antipollicatus Sharovipteryx Darwinopterus AMNH M8802 Longisquama Darwinopterus modularis ZMNH M 8782 Darwinopterus robustodens 41H111-0309A Bergamodactylus MPUM 6009 Darwinopterus linglongtaensis IVPP V 16049 Raeticodactylus Darwinopterus YH2000 Austriadactylus SMNS 56342 Seazzadactylus Scaphognathus crassirostris Austriadraco BSp 1994 I51 Scaphognathus SMNS 59395 Scaphognathus Maxberg sp. Austriadactylus SC332466 Preondactylus TM 13104 MCSNB 2887 Gmu10157 Caelestiventus BM NHM 42735 Dimorphodon macronyx Peteinosaurus Ex3359 BSp 1986 XV 132 Carniadactylus ELTE V 256-Pester specimen MCSNB 8950 B St 1936 I 50 (n30) Dimorphodon? weintraubi Cycnorhamphus IVPP V13758 embryo Moganopterus Mesadactylus holotype Feilongus Dendrorhynchoides curvidentatus Luopterus = D. mutoudengensis Yixianopterus SMNS 81928 flathead Mimodactylus Discodactylus NJU-57003 Haopterus Vesperopterylus JZMP embryo Anurognathus Boreopterus Sinomacrops Zhenyuanopterus CAG IG 02-81 Hamipterus PIN 2585/4 flightless anurognthid Arthurdactylus Batrachognathus SMNK PAL 3854 Daohugoupterus Ikrandraco Eudimorphodon
    [Show full text]
  • An Unusual Long-Tailed Pterosaur with Elongated Neck from Western Liaoning of China
    “main” — 2009/10/20 — 22:33 — page 793 — #1 Anais da Academia Brasileira de Ciências (2009) 81(4): 793-812 (Annals of the Brazilian Academy of Sciences) ISSN 0001-3765 www.scielo.br/aabc An unusual long-tailed pterosaur with elongated neck from western Liaoning of China XIAOLIN WANG1, ALEXANDER W.A. KELLNER2, , , SHUNXING JIANG1 3 and XI MENG1 3 1Key Laboratory of Evolutionary Systematics of Vertebrates Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences PO Box 643, Beijing, 100044, China 2Setor de Paleovertebrados, Museu Nacional, UFRJ Quinta da Boa Vista s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brasil 3Graduate University of Chinese Academy of Sciences, Beijing, 100049, China Manuscript received on August 11, 2009; accepted for publication on September 10, 2009; contributed by ALEXANDER W.A. KELLNER* ABSTRACT A new long-tailed pterosaur, Wukongopterus lii gen. et sp. nov, is described based on an almost complete skeleton (IVPP V15113) representing an individual with an estimated wing span of 730 mm. The specimen was discovered in strata that possibly represent the Daohugou Bed (or Daohugou Formation) at Linglongta, Jianchang, Liaoning Province, China. Wukongopterus lii is a non-pterodactyloid pterosaur diagnosed by the first two pairs of premax- illary teeth protruding beyond the dentary, elongated cervical vertebrae (convergent with Pterodactyloidea), and a strongly curved second pedal phalanx of the fifth toe. The specimen further has a broken tibia that indicates anin- jury occurred while the individual was still alive. Taphonomic aspects provide indirect evidence of an uropatagium, supporting the general hypothesis that at least all non-pterodactyloid pterosaurs show a membrane between the hind limbs.
    [Show full text]