Mostrando postagens com marcador plesiosauria. Mostrar todas as postagens
Mostrando postagens com marcador plesiosauria. Mostrar todas as postagens

sexta-feira, 1 de novembro de 2019

Ossos de enormes predadores do mar jurássico encontrados em milharal

Os ossos do predador gigante do mar foram descobertos por paleontologistas em um campo de milho na vila de Krzyżanowice. Dariusz Nast / Piotr Szczepaniak
Cientistas na Polônia descobriram os ossos de enormes predadores nadadores que vagavam pelas águas há 150 milhões de anos.
 
Com seu corpo maciço e focinho alongado, parecido com um crocodilo, o pliossauro, que viveu na Europa e na América do Sul durante o período Jurássico Final, cerca de 163 a 145 milhões de anos atrás.
Seu nome vem das palavras gregas "plio" e "sauros", que juntas significam "mais lagartos".
As criaturas podem atingir mais de 10 m de comprimento e pesar várias dezenas de toneladas.
 

Os paleontólogos encontraram centenas de ossos, não apenas os pertencentes ao pliosaurus, mas também os dos plesiossauros (outro tipo de réptil marinho; ao contrário do pliosaurus, este tem pescoço longo), tartarugas e enormes crocodilos pré-históricos. Dariusz Nast
 
Eles tinham barbatanas para nadar e grandes dentes pontudos para capturar suas presas, que incluíam peixes e répteis marinhos.
Os paleontologistas poloneses encontraram os ossos em um campo de milho na vila de Krzyżanowice, no centro da Polônia, perto das montanhas Świętokrzyskie, relata a Science na Polônia.
 
Fragmentos de ossos de enormes predadores do mar de 150 milhões de anos atrás descobertos perto de Iłża
 
A descoberta deles é muito rara, enfatizam.
Os paleontologistas encontraram os ossos na vila de Krzyżanowice, perto das montanhas Świętokrzyskie. Nos dias do pliosaurus, essa parte da Polônia era um arquipélago de ilhas tropicais, com lagoas quentes e reservatórios marinhos, onde os animais marinhos viviam. Daniel Tyborowski
"Na Europa, eles foram descobertos até agora em apenas alguns países, mas nunca na Polônia", disse o paleontólogo Daniel Tyborowski, do Museu da Terra da Academia Polonesa de Ciências, em Varsóvia.
 
 Daniel Tyborowski e Błażej Błażejowski, do Instituto de Paleobiologia da Academia Polonesa de Ciências, publicaram suas descobertas em um artigo no 'Proceedings of the Geological Association'. Marcin Obara / PAP
 
Tyborowski e Błażej Błażejowski, do Instituto de Paleobiologia da Academia Polonesa de Ciências, publicaram suas descobertas em um artigo na "Proceedings of the Geological Association", intitulado "Novos fósseis de répteis marinhos do Jurássico tardio da Polônia, com implicações para a paleobiogeografia das faunas de vertebrados".
As criaturas podem atingir mais de 10 m de comprimento e pesar várias dezenas de toneladas. Eotyrannu5
 
Os ossos encontrados são semelhantes aos encontrados nas localidades jurássicas tardias de Kimmeridge Clay, na Grã-Bretanha, e no arquipélago de Svalbard, no Ártico, observam no artigo.
Os ossos pertencem tanto ao pilossauro quanto às criaturas que ele comeu. Dariusz Nast
 
Em Krzyżanowice, eles encontraram centenas de ossos, não apenas os pliosauros, mas também os dos plesiossauros (outro tipo de réptil marinho; ao contrário do pliosaurus, este tem pescoço longo), tartarugas e enormes crocodilos pré-históricos.
 

Daniel Tyborowski, do Museu da Terra da Academia Polonesa de Ciências, em Varsóvia, disse que esta foi a primeira vez que tais ossos foram encontrados na Polônia. Marcin Obara / PAP
 
Nos dias do pliosaurus, essa parte do que hoje é a Polônia parecia muito diferente: era um arquipélago de ilhas tropicais, com lagoas quentes e reservatórios marinhos, onde os animais marinhos viviam.
 
"O poderoso pliosaurus caçava todos os animais cujos fósseis encontramos neste local", acrescentou Tyborowski.
 
Nos próximos meses, os paleontólogos continuarão suas pesquisas em Krzyżanowice, na esperança de encontrar ainda mais ossos de répteis enormes.

sexta-feira, 5 de outubro de 2018

Elasmossauro
    O Elasmossauro (Elasmosaurus platyurus) cujo nome significa elasmos "placa fina" em referências as placas pélvicas finas e sauro "lagarto", viveu há aproximadamente 80,5 milhões de anos atrás durante o período Cretáceo na região central da América do Norte.

    Esta espécie não era um dinossauro, mas sim, um réptil marinho do grupo dos plesiossauros (Ordem Plesiosauria). O seu aspecto poderia ser descrito como o de uma gigantesca serpente unida ao corpo de uma tartaruga marinha sem casco. Seu pescoço era enorme, possuía o comprimento maior do que todo o restante do corpo, isto é, quase 8 metros de comprimento. O corpo todo media 14 metros de comprimento. O Elasmossauro provavelmente se arrastava em praias para por seus ovos em ninhos pouco profundos como as tartarugas marinhas fazem hoje em dia.

Dados:
 
Nome: Elasmossauro
Nome Científico: Elasmosaurus platyurus
Época: Cretáceo
Local onde viveu: América do Norte
Peso: Cerca de 2,2 toneladas
Tamanho: 14 metros de comprimento
Alimentação: Carnívora

Classificação Científica:
Reino: Animalia
Filo: Chordata
Classe: Reptilia
Superordem: Sauropterygia
Ordem: Plesiosauria
Família: Elasmosauridae
Espécie: Elasmosaurus platyurus Bonaparte & Novas, 1985.

Referências:
- Cope, E. D. 1868. "Remarks on a new enaliosaurian, Elasmosaurus platyurus." Proceedings of the Academy of Natural Sciences of Philadelphia, 20: 92-93. (for meeting of March 24, 1868.
- Everhart, M. J. 2005. Oceans of Kansas - A Natural History of the Western Interior Sea. Indiana University Press, 320 pp.

domingo, 10 de janeiro de 2016

[Paleontology • 2016]  

Makhaira rossica • Peculiar Macrophagous Adaptations in A New Cretaceous Pliosaurid

Makhaira rossica
Fischer, Arkhangelsky, Stenshin, Uspensky, Zverkov & Benson, 2015
Abstract
During the Middle and Late Jurassic, pliosaurid plesiosaurs evolved gigantic body size and a series of craniodental adaptations that have been linked to the occupation of an apex predator niche. Cretaceous pliosaurids (i.e. Brachaucheninae) depart from this morphology, being slightly smaller and lacking the macrophagous adaptations seen in earlier forms. However, the fossil record of Early Cretaceous pliosaurids is poor, concealing the evolution and ecological diversity of the group. Here, we report a new pliosaurid from the Late Hauterivian (Early Cretaceous) of Russia. Phylogenetic analyses using reduced consensus methods recover it as the basalmost brachauchenine. This pliosaurid is smaller than other derived pliosaurids, has tooth alveoli clustered in pairs and possesses trihedral teeth with complex serrated carinae. Maximum-likelihood ancestral state reconstruction suggests early brachauchenines retained trihedral teeth from their ancestors, but modified this feature in a unique way, convergent with macrophagous archosaurs or sphenacodontoids. Our findings indicate that Early Cretaceous marine reptile teeth with serrated carinae cannot be unequivocally assigned to metriorhynchoid crocodylomorphs. Furthermore, they extend the known diversity of dental adaptations seen in Sauropterygia, the longest lived clade of marine tetrapods.
Systematic description
Plesiosauria Blainville, 1835  
Pliosauridae Seeley, 1874 
Thalassophonea Benson & Druckenmiller, 2014  
Makhaira rossica gen. et sp. nov.

LSIDs: urn:lsid:zoobank.org:pub:2C95C409-72C0-45FE-BF58-608657D5382F (Publication);
urn:lsid:zoob- ank.org:act:F19A595F-D739-4361-9088-84B7B947DC93 (Makhaira);
urn:lsid:zoobank.org:act:258CFACB-27D3-44CF-8B04-A12FDDECA55C (Makhaira rossica)
Figure 2. Rostrum of YKM 68249/1-10.
(a–c) Right premaxilla, in (a) lateral, (b) medial and (c) ventral views. Numbers indicate the position of each alveolus. The ventral premaxilla–maxilla suture is located at the 6th alveolus. Note the procumbent 1st alveolus. (d–e) Anterior part of the symphysis, in (d) anterior, (e) ventral and (f) posterior views.

Figure 3. Dentition and mandible of YKM 68249/1-10.
 (a) Mandible in dorsal view. (b) Replacement tooth in the 2nd alveolus, showing the trihedral cross section. (c) Base of the 3rd alveolus crown, showing the marked mesiolabial carina (the crown fragment has been glued slightly off its original position). (d) 1st or 2nd post-symphysis replacement tooth, showing distal ridges and serrated carinae. (e,f) Successive zooms of the mesiolabial carinae of a broken off crown lying on the ventral surface of the symphysis (figure 2). (h) Schematic diagram of the carination, drawn from (f). Note the serrated crenulations.

Holotype, Horizon and Locality: YKM 68249/1-10, a slightly immature fragmentary skeleton consisting of a partial right premaxilla, the anterior part of the mandible, several teeth, three dorsal vertebrae in anatomical connection, a partial left ischium and a partial right ilium. It is preserved in three dimensions in a series of pyritic limestone nodules found along the banks of the Volga River, 600 m to the north of Slantsevy Rudnik, Ulyanovsk Oblast, Russian Federation (figure 1). The precise level within the section is unknown, but the section only contains Upper Hauterivian (Lower Cretaceous) strata of the Speetoniceras versicolor Zone in this locality.
Etymology: From Latinized Ancient Greek ‘μάχαɩρα’ (mákhaira): a blade with a curved outline and Latin ‘rossica’: Russian.
Figure 4. Postcranial remains of YKM 68249/1-10.
(a–f) Dorsal centrum, in (a) anterior, (b) right lateral, (c) posterior, (d) left lateral, (e) ventral and (f) dorsal views. (g–k) Right ilium in (g) dorsal, (h) medial, (i) lateral, (j) posterior and (k) ventral views. (l–q) Left ischium in (l) anterolateral (glenoid), (m) dorsal, (n) posterolateral, (o) medial, (p) anteromedial and (q) ventral views. (r) Reconstruction of Makhaira rossica based on Late Jurassic pliosaurids and mid-Cretaceos brachauchenines; the orange coloured parts indicate fossils preserved in YKM 68249/1-10.
.............................

Discussion and Conclusion

Ecology of Early Cretaceous pliosaurids
Makhaira rossica shares morphological features with both Late Jurassic and Mid-Cretaceous pliosaurids, detailing the tempo of morphological evolution in the early history of Brachaucheninae. Osteological features often associated with macrophagy, and widely present in Middle–Late Jurassic pliosaurids such as the spatulate rostrum and the expanded caniniform teeth were seemingly lost early in the evolution of brachauchenines. However, the incompletely resolved phylogenetic position of Makhaira rossica within Brachaucheninae, and the presence of these features in some other Cretaceous pliosaurid specimens whose phylogenetic affinities were not resolved by our analysis raises a number of questions regarding the evolution and biodiversity of early members of that clade. Specifically, it seems that Early Cretaceous pliosaurids exhibit multiple ecomorphologies that are in need of further study. Because of the poor record of Early Cretaceous pliosaurids, it is still unclear whether trihedral, strongly carinated teeth constitute the ancestral condition of derived thalassophoneans or were acquired convergently in Makhaira rossica, Pliosaurus and currently enigmatic taxa such as ‘Pliosaurusrossicus. Parsimony-based methods are ambiguous while likelihood methods suggest that trihedral teeth are a synapomorphy of Pliosaurus + Brachaucheninae, that was subsequently lost within Brachaucheninae. In this scenario, Makhaira rossica thus retained the ancestral state of that trait, but modified it via a unique serration pattern.
Makhaira rossica departs from both Late Jurassic and Cretaceous thalassophoneans by its smaller size: the largest dorsal centrum is 72 mm wide. Nevertheless, fusion of neurocentral suture suggests osteological maturity for this specimen. For comparison, the last cervical centrum of the late Barremian ‘Brachauchenius’ sp. is 117 mm wide, the largest dorsal centrum of Brachauchenius lucasi is 90 mm wide and the width of those of Kronosaurus queenslandicus and ‘Kronosaurusboyacensis exceed 150 mm and 170 mm, respectively. Makhaira rossica markedly differs from Cretaceous thalassophoneans by having relatively large teeth and dental adaptations reminiscent of macrophagous predators such as theropod dinosaurs or thalattosuchians crocodyliforms. Unexpectedly, because of their densely serrated and wave-like pattern, the carinae of YKM 68249/1-10 appear larger and more complex than in other macrophagous marine tetrapods such as Mosasaurus hoffmani (V. Fischer 2015, personal observation on ULg PA.25119), Dakosaurus maximus ([54]; V. Fischer 2015, personal observation on ULg PA.6600) or Geosaurus, the latter being regarded as having ‘hypercarnivorous’ adaptations. Makhaira rossica is also unique among plesiosaurs in having trihedral but moderately widely spaced teeth. Contrary to carination and serration, previous authors have not generally assigned a specific functional interpretation to the presence of wide interalveolar spacing. However, we note that the carinated teeth of macrophagous marine reptiles are usually closely spaced.

Makhaira rossica thus indicates that pliosaurids explored previously unrecognized niches during the Early Cretaceous, with the presence of a smaller bodied taxon possessing clear yet distinctive macrophagous adaptations. By being the first sauropterygian to develop complex serration of its carinae, Makhaira rossica further exemplifies the profound diet-driven morphofunctional convergences that evolved among Mesozoic marine reptiles.
Figure 5. Phylogenetic position of Makhaira rossica and ancestral state reconstructions of character 139, related to crown shape. (a) Strict consensus of the maximum-parsimony analysis of the full dataset. (b) Strict consensus of the maximum-parsimony analysis of the reduced dataset. (c) Results of maximum-parsimony method for ancestral state reconstruction (using MESQUITE). (d) Results of likelihood method for ancestral state reconstruction (using CLADDIS).
 Implications for metriorhynchid extinction
An isolated crown from the Aptian of Sicily (MSNC 4475) has been recently regarded as evidence for the late survival of geosaurine metriorhynchid crocodyliforms, several million years after their supposed extinction [61]. However, although they do not yet co-occur within a single pliosaurid taxon, all the features of MSNC 4475 described in [61] can now be shown to have been present among Cretaceous pliosaurids (‘The conical shape of the tooth crown, noticeable lingual curvature, presence of mesial and distal carinae, and microscopic denticles along the carinae’ [61], p. 610). We also note that MSNC 4475 appears weakly trihedral in apical view ([61]; figure 2f). Moreover, fine, smooth and widely spaced apicobasal ridges restricted to one surface of the tooth and the triangular or approximately triangular cross section of the crown are other features shared between MSNC 4475 and Makhaira rossica. Differences between these two specimens are also present: the apicobasal ridges are not located on the curved side in the large tooth of Makhaira rossica (but such ridges are present in one small replacement tooth (figure 3) and thus possibly variable with dental development in Makhaira rossica), and the weak development of a trihedral cross section in the Sicilian tooth. It is not currently possible to make a definitive statement on the affinities of MSNC 4475, which clearly is an important specimen and potentially illustrates the profound convergence of Makhaira rossica with macrophagous archosaurs. However, future discoveries are likely to clarify whether MSNC 4475 is a late-surviving, low-latitude metriorhynchid or a brachauchenine pliosaurid.
Valentin Fischer, Maxim S. Arkhangelsky, Ilya M. Stenshin, Gleb N. Uspensky, Nikolay G. Zverkov and Roger B. J. Benson. 2015. Peculiar Macrophagous Adaptations in A New Cretaceous Pliosaurid. Royal Society Open Science.   DOI:  10.1098/rsos.150552

terça-feira, 20 de outubro de 2015

Plesiosaur Bites

Mine’s bigger than yours! The Monster of Aramberri, Predator X, and other monster pliosaurs in the media


During the past decade several dramatically named giant pliosaurs have hit the mainstream media, many claiming to be the biggest yet discovered. But only a trickle of peer-reviewed literature has been published to accompany these news stories. The lack of published data makes it really difficult to sift the facts from the fiction, and it’s easy to get the different stories muddled up, especially in the case of two identically sized congeneric pliosaur specimens from Svalbard: ‘The Monster’ and ‘Predator X’. So in an attempt to iron out the details and assess what we really know about all these specimens, here’s a short summary of the main players.

The Monster of Aramberri

Hit the mainstream media: 2002.
Estimated length in media: 18 m.
Conservative estimated length 15 m.
Material: Partial vertebral column, proximal end of a femur, part of the pelvic girdle, and cranial fragments. The fragment of rostrum collected in 1985 is now lost.
Where: Aramberri, Mexico.
Excavation: The original excavation in 1985 yielded a partial rostrum and vertebral column. The excavation site was reidentified in 2001 and additional material was collected during 2001 and 2002.
Peer-reviewed scientific references: Buchy et al. (2003).

Notes: The material was collected over a period of several years, but the discovery only hit the mainstream media in 2002 when more substantial pieces of the skeleton were discovered. An excellent account of the ‘Monster of Aramberri’ is given here by Richard Forrest. Buchy et al. (2003) described UANL-FCT-R2, the partial vertebral column discovered in 1985 [pictured below], but the majority of the skeleton has not been described and is in the process of being prepared. I’ve confirmed with Marie-Celine that the vertebrae described in 2003 are part of the ‘Monster of Aramberri’, but it is worth noting that the 2003 paper doesn’t explicitly mention ‘The Monster of Aramberri’ by name. Originally referred to Liopleurodon, it isn’t considered so any more (Buchy & Frey, 2003).
Monster of Aramberri vertebrae
Part of a figure from Buchy et al. (2003) showing some of the vertebrae and girdle elements of 'The Monster of Aramberri' of the

The Monster

Hit the mainstream media: October 2006
Estimated length in media: 15 metres
Conservative estimated length: 13-15 m
Material: anterior part of rostrum, two cervical and numerous dorsal vertebrae, a nearly complete coracoid and right forelimb, and several dorsal ribs and gastralia.
Where: Svalbard, Norway.
Excavation: Discovered in 2006 and excavated in 2007.
Peer-reviewed scientific literature: none.
Notes: ‘The Monster’, not to be confused with ‘The Monster of Aramberri’, was the first pliosaur from Svalbard to be excavated and the first to make the news. A second giant pliosaur (‘Predator X’, see below) was discovered at the same time, but was excavated the following season. Richard Forrest’s 2008 article on the plesiosaurs from svalbard provides a thorough discussion, including comments on ‘The Monster’, but it was written before the second pliosaur hit the mainstream media.
Paddle of 'the monster'
Partial forelimb of 'The Monster'

Predator X

Hit the mainstream media: March 2009
Estimated length in media:
15 m
Conservative estimated length: 13-15 m
Material: Partial skeleton including posterior skull region and anterior cervical vertebrae.
Where: Svalbard, Norway.
Excavation: Discovered in 2006 and excavated in 2008.
Peer-reviewed scientific literature: none.

Notes. The fossil material attributed to this pliosaur was first mentioned in stories covering “The Monster” in 2008, but the name ‘Predator X’ was coined after the specimen was excavated and it hit the media in 2009. According to an SVP poster by Knutsen et al. (2009) both ‘The Monster’ and ‘Predator X’ belong to the same taxon – they are congeneric and they are closest in their anatomy to Pliosaurus. They are both estimated to be the same size, and they are also both from the same geological formation, so with all these similarities it’s easy to confuse the two. ‘Predator X’ inspired the cover story for the 31 October 2009 issue of New Scientist, and was the main subject of a recent History Channel documentary of the same name, which also featured another giant pliosaur – the Weymouth Bay pliosaur. ‘Predator X’ will also appear in the BBC’s upcoming series Planet Dinosaur. Despite its widespread presence in the news and on TV, I was unable to find a suiatable photograph of the actual material.

The Weymouth Bay pliosaur

Hit the mainstream media: October 2009
Estimated length in the media: 16 m
Conservative estimated length: 12 m.
Material: skull and mandible (missing the tip of the manibular symphysis).
Where: Weymouth Bay, Dorset, UK.
Excavation: Discovered in pieces over a period of time – specific details unclear. The specimen was purchased by Dorset County Museum in Dorchester.
Peer-reviewed scientific literature: none.
Notes:
There is an excellent account of the Weymouth Bay pliosaur here by Richard Forrest. The skull as preserved is 2.1m long.









The Weymouth Bay pliosaur
The Weymouth Bay pliosaur and Richard Forrest


So there we have it, four mega-pliosaurs making big news in the space of a decade. All of them have conservative and realistic length estimates around the 15m mark, with the Weymouth Bay pliosaur possibly slightly smaller and ‘The Monster of Aramberri’ possibly slightly larger. But all the estimates are way too wooly to take seriously just yet. So all these monsters will remain jostling for top spot until the scientific papers are published, and until we have a better understanding of pliosaurid proportions.
There are or course plenty of other giant pliosaurs, which frequently pop up in discussions too, including additional real contenders for ‘biggest pliosaur ever!’. While I do plan to write more on giant pliosaurs in the future, I’ve stuck to the ones in the mainstream media for now. You might have noticed that Liopleurodon was conspicuously omitted from this post. Well, although it is entirely relevant to the present topic, it hasn’t been in the news recently so I decided to leave the magical Liopleurodon alone this time around. It will be nice to write about a pliosaur with an actual scientific name for a change, even if that’s opening a can of worms in itself!

References

Buchy, M.-C. & Frey, E. 2003. Was it really eating granite? We’re searching hard: history of the Monster
of Aramberri (and stories about it). First meeting of the EAVP – abstracts, 39.

Buchy M.-C., Frey E., Stinnesbeck, W. ; López-Oliva J.G. 2003. First occurrence of a gigantic pliosaurid plesiosaur in the Late Jurassic (Kimmeridgian) of Mexico. Bulletin de Societe géologique de France, 174, 271-278.

Knutsen, E., Druckenmiller, P., Hurum, J., Nakrem, H. 2009. Preliminary account of new Late Jurassic pliosaurid material from Svalbard, Norway. Journal of Vertebrate Paleontology, 128A.

Noè, L. F., Smith, D. T. J. & Walton, D. I. 2004. A new species of Kimmeridgian pliosaur (Reptilia; Sauropterygia) and its bearing on the nomenclature of Liopleurodon macromerus. Proceedings of the Geologists’ Association 115, 13-24.

fonte: http://plesiosauria.com