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[Ornithology • 2017] Myzomela irianawidodoae • A Colourful New Species of Myzomela Honeyeater from Rote Island in eastern Indonesia ---ScRaBBlE

Myzomela irianawidodoae Prawiradilaga, Baveja, Suparno, Ashari, Ng, Gwee, Verbelen & Rheindt, 2017  photo:   Philippe Verbelen  e-journ...

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Showing posts with label Nodosauridae. Show all posts
Showing posts with label Nodosauridae. Show all posts

Wednesday, March 20, 2019

[Paleontology • 2017] Borealopelta markmitchelli • An Exceptionally Preserved Three-Dimensional Armored Dinosaur Reveals Insights into Coloration and Cretaceous Predator-Prey Dynamics ---ScRaBBlE


Borealopelta markmitchelli 
Brown, Henderson, Vinther, Fletcher, Sistiaga, Herrera & Summons, 2017


Highlights
• A new armored dinosaur is described based on an exceptionally preserved specimen
• Abundant in situ osteoderms with keratinous sheaths and scales are preserved
• Reddish-brown coloration and crypsis in the form of countershading are indicated
• Crypsis indicates strong predation pressure on this large, heavily armored dinosaur


Summary
Predator-prey dynamics are an important evolutionary driver of escalating predation mode and efficiency, and commensurate responses of prey. Among these strategies, camouflage is important for visual concealment, with countershading the most universally observed. Extant terrestrial herbivores free of significant predation pressure, due to large size or isolation, do not exhibit countershading. Modern predator-prey dynamics may not be directly applicable to those of the Mesozoic due to the dominance of very large, visually oriented theropod dinosaurs. Despite thyreophoran dinosaurs’ possessing extensive dermal armor, some of the most extreme examples of anti-predator structures, little direct evidence of predation on these and other dinosaur megaherbivores has been documented. Here we describe a new, exquisitely three-dimensionally preserved nodosaurid ankylosaur, Borealopelta markmitchelli gen. et sp. nov., from the Early Cretaceous of Alberta, which preserves integumentary structures as organic layers, including continuous fields of epidermal scales and intact horn sheaths capping the body armor. We identify melanin in the organic residues through mass spectroscopic analyses and observe lighter pigmentation of the large parascapular spines, consistent with display, and a pattern of countershading across the body. With an estimated body mass exceeding 1,300 kg, B. markmitchelli was much larger than modern terrestrial mammals that either are countershaded or experience significant predation pressure as adults. Presence of countershading suggests predation pressure strong enough to select for concealment in this megaherbivore despite possession of massive dorsal and lateral armor, illustrating a significant dichotomy between Mesozoic predator-prey dynamics and those of modern terrestrial systems.

 Systematic Paleontology

Dinosauria Owen, 1842  
Ornithischia Seeley, 1888  

Ankylosauria Osborn, 1923  
Nodosauridae Marsh, 1890  

Borealopelta markmitchelli gen. et sp. nov. 

Etymology: The generic name Borealopelta is derived from “borealis” (Latin, “northern”) and “pelta” (Greek, “shield”), in reference to the northern locality and the preserved epidermal scales and dermal osteoderms. The specific epithet markmitchelli honors Mark Mitchell for his more than 7,000 hours of patient and skilled preparation of the holotype.


An illustration of Borealopelta markmitchelli. The study suggests that it displayed a camouflage effect known as counter-shading.
 Illustration: Julius Csotonyi/Courtesy of the Royal Tyrrell Museum of Palaeontology, Canada. 


 Illustration: Robert Nicholls 


 Illustration: Davide Bonadonna











Figure 1. Photographs of the Holotype of Borealopelta markmitchelli, TMP 2011.033.0001 Top: anterodorsolateral view; bottom: anterodorsal view. Scale bar, 10 cm. 




Holotype: The holotype is Royal Tyrrell Museum of Palaeontology (TMP) 2011.033.0001: an articulated specimen preserving the head, neck, most of the trunk and sacrum, a complete right and a partial left forelimb and manus, partial pes (Figure 1). In situ osteoderms and nearly complete soft tissue integument are preserved across dorsal and lateral surfaces of the axial skeleton, posterodorsal surface of forelimbs, and plantar surfaces of a manus and a pes. Specimen is preserved in multiple large blocks, including slabs and counter-slabs in the sacral region.

Locality and Horizon: Suncor Millennium Mine, Fort McMurray, Alberta, Canada. Wabiskaw Member, Clearwater Formation, Aptian stage. Detailed locality data are available at Royal Tyrrell Museum of Palaeontology.

Diagnosis: A nodosaurid ankylosaur characterized by the following autapomorphies (∗) and suite of characters [character/state]: cranial: dorsal skull ornamentation expressed as a large hexagonal dermal plate in frontoparietal region and multiple (>20) small dermal plates in frontonasal region∗; external nares excluded from view dorsally (shared with Pawpawsaurus) [16:1]; supraorbital ornamentation forming sharp lateral rim dorsal to orbits (shared with Gargoyleosaurus and Kunbarrasaurus) [38:2]; jugal (suborbital) horn triangular with pointed apex (shared with GastoniaGargoyleosaurus, and Polocanthus); jugal (suborbital) horn base longer than orbit length∗; osteoderms: cervical and thoracic osteoderms form continuous (abutting) transverse rows completely separated by continuous transverse rows of polygonal basement scales; parascapular spine is the largest osteoderm, recurved, and projects posterolaterally and horizontally (potentially shared with Sauropelta); osteoderm count for transverse rows: cervicals: C1-3, C2-3, C3-3, transition: TR-2, thoracic: T1-6∗; third and sixth transverse thoracic osteoderm rows expressed medially but pinch out laterally∗.

The new taxon can be further differentiated from Pawpawsaurus based on: dermal plate in frontonasal region (central dermal plates) flat; absence of ciliary osteoderm. Can be further differentiated from Sauropelta based on: parietals flat to slightly convex; cervical half ring has 4–6 osteoderms only; medial cervical osteoderms subequal, hexagonal, and bear prominent median ridge with posterior margin projecting beyond the basal footprint.





Figure 2: Schematic Line Drawing of TMP 2011.033.0001, the Holotype of Borealopelta markmitchelli, Illustrating Preservation of the Different Tissue Types (A) Schematic of complete specimen in dorsal view. (B and C) Skull in dorsal (B) and left lateral (C) views. (D) Close-up view of the neck, illustrating alternating cervical osteoderm bands (and preserved keratinous sheaths) and polygonal scales. (E) Close-up view of flank illustrating lateral thoracic osteoderms (with keratinous coverings) and polygonal scales. (F) Close-up view of sacral shield counterpart illustrating osteoderms and scales. (G) Close-up view of antebrachium including osteoderms and keratinous coverings. (D’–G’) Interpretive line drawings of the corresponding panels (D)–(G). Scale bars in (B)–(G), 10 cm.

Figure 3Time-Calibrated Strict Consensus Tree Showing Position of Borealopelta markmitchelli within Ankylosauria, with Representative Well-Preserved Ankylosaurs Shown Above Bottom: time-calibrated strict consensus tree illustrating position of Borealopelta markmitchelli within Ankylosauria scaled to Jurassic and Cretaceous stages. Top: line drawings of representative well-preserved ankylosaur specimens with in situ armor and/or skin. Scale bars, 1 m.
(A) Kunbarrasaurus, QM F18101. (B) Euoplocephalus, NHMUK 5161. (C) Sauropelta, AMNH 3035 and 3036 composite. (D) Borealopelta, TMP 2011.033.0001 (this study). (E) Edmontonia, AMNH 5665.

Figure 4:  Chart Illustrating the Loss of Countershading as Body Mass Increases in Terrestrial Mammal Herbivores Chart includes pooled data for artiodactyls, perissodactyls, and proboscideans divided into body-mass bins, showing relative proportion of species that exhibit countershading. The diagonally hatched area represents the mass above which significant predation of adults does not occur. Animals illustrated above chart are representative taxa within each mass bin; species names in italics at top indicate body masses of the largest carnivores.

The Making of a Most Extraordinary Fossil

The Making of a Most Extraordinary Fossil

Caleb M. Brown, Donald M. Henderson, Jakob Vinther, Ian Fletcher, Ainara Sistiaga, Jorsua Herrera and Roger E. Summons. 2017. An Exceptionally Preserved Three-Dimensional Armored Dinosaur Reveals Insights into Coloration and Cretaceous Predator-Prey Dynamics. Current Biology. DOI: 10.1016/j.cub.2017.06.071


Despite heavy armor, new dinosaur used camouflage to hide from predators  eurekalert.org/e/7ZWJ via @CellPressNews @EurekAlert

It's Official: Stunning Fossil Is a New Dinosaur Species  on.natgeo.com/2vx0wxD via @NatGeo
This Is the Best Dinosaur Fossil of Its Kind Ever Found on.natgeo.com/2r02aW7 via @NatGeo
Discover How This Dinosaur Became an Extraordinary Fossil  NationalGeographic.com/magazine/2017/06/making-of-a-dinosaur-fossil-nodosaur-illustrations

Heavily armoured dinosaur had ginger camouflage to deter predators – study  theguardian.com/science/2017/aug/03/heavily-armoured-nodosaur-ginger-camouflage-predators-borealopelta-markmitchelli


ติดอยู่ในกาลเวลา  ngthai.com/animals/1703 via  เนชันแนล จีโอกราฟฟิก (National Geographic) ฉบับภาษาไทย

  

  


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روابط التحميل والمشاهدة، الروابط المباشرة للتحميل
او
شاهد هذا الفيديو القصير لطريقة التحميل البسيطة


كيف تحصل على مدونة جاهزة بآلاف المواضيع والمشاركات من هنا
شاهد قناة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على اليوتيوب لمزيد من الشرح من هنا
رابط مدونة منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات في أي وقت حــــتى لو تم حذفها من هنا
شاهد صفحة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على الفيس بوك لمزيد من الشرح من هنا
تعرف على ترتيب مواضيع منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات (حتى لا تختلط عليك الامور) من هنا

ملاحظة هامة: كل عمليات تنزيل، رفع، وتعديل المواضيع الجاهزة تتم بطريقة آلية، ونعتذر عن اي موضوع مخالف او مخل بالحياء مرفوع بالمدونات الجاهزة بآلاف المواضيع والمشاركات، ولكم ان تقوموا بحذف هذه المواضيع والمشاركات والطريقة بسيطة وسهلة. ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــسلامـ.

[Paleontology • 2017] Borealopelta markmitchelli • An Exceptionally Preserved Armored Dinosaur reveals the Morphology and Allometry of Osteoderms and their Horny Epidermal Coverings ---ScRaBBlE


Borealopelta markmitchelli 
Brown, Henderson, Vinther, et al., 2017

Brown​. 2017.  DOI:  10.7717/peerj.4066  @Brown_Caleb_M

Abstract

Although the evolution and function of “exaggerated” bony projections in ornithischian dinosaurs has been subject to significant debate recently, our understanding of the structure and morphology of their epidermal keratinized coverings is greatly limited. The holotype of Borealopelta, a new nodosaurid ankylosaur, preserves osteoderms and extensive epidermal structures (dark organic residues), in anatomic position across the entire precaudal length. Contrasting previous specimens, organic epiosteodermal scales, often in the form of horn-like (keratinous) sheaths, cap and exaggerate nearly all osteoderms, allowing for morphometric and allometric analyses of both the bony osteoderms and their horny sheaths. A total of 172 osteoderms were quantified, with osteoderm spine length and height being positively allometric with respect to basal length and width. Despite tight correlations between the different measures amongst all other osteoderms, the large parascapular spines represent consistent outliers. Thickness and relative contribution of the keratinized epiosteodermal scales/sheaths varies greatly by region, ranging from 2% to 6% for posterior thoracics, to ∼25% (1.3×) for the parascapular spines—similar to horn sheaths in some bovid analogues. Relative to the bony cores, the horny portions of the spines are strongly positively allometric (slope = 2.3, CI = 1.8–2.8). Strong allometric scaling, species-specific morphology, and significant keratinous extension of the cervicoscapular spines is consistent with elaboration under socio-sexual selection. This marks the first allometric analysis of ornithischian soft tissues.


  

Figure 1: Dorsal view of TMP 2011.033.0001, showing both photocomposite and schematic line drawing.
 (A) Photocomposite dorsal view of TMP 2011.033.0001. (B) Schematic line drawing of (A) showing osteoderm regions by color. (C) Inset showing constituent blocks of TMP 2011.033.0001, and their relative position within a body outline in dorsal view. Photocomposite (A), created using separate, orthogonal images of blocks A–C, D, E, F–I, and J and combined digitally to reduce parallax. Blocks F, G, H, and I represent reflected counterpart.
  
Figure 2: Single dorsal photograph of TMP 2011.033.0001.
Sacral region represents original part—reflected counterpart shown in Fig. 4. Scale equals 1 m.

Figure 3: Interpretive scientific illustration of TMP 2011.033.0001 in dorsal view.
Sacral region represents original part—reflected counterpart shown in Fig. 4. Scale equals 1 m.

Figure 4: Composite dorsal view of TMP 2011.033.0001.
Photocomposite created using separate images of blocks A–C, D, E, F–I, and J (see Fig. 1) and combined digitally to both reduce parallax and remove gaps. Blocks F, G, H and I represent reflected counterpart of sacral part in Fig. 2. Photographs of individual blocks were digitally modified (brightness, contrast, etc.) to removed different lighting conditions, and to illustrate an average composite of the entire specimen. Scale equals 1 m.

Figure 15: Comparisons of the size of the bony core and keratinous sheath of the parascapular spine of Borealopelta to modern bovid and squamate analogues.
(A) Absolute size of the bone core (horncore or osteoderm) (yellow) and the overlying keratinous/horn sheath (grey) for the parascapular spine of TMP 2011.033.0001 (top) as well as averages for several bovid and squamate taxa (lower).
 (B) Schematic representations of the relative bony and keratinous components of select spines/horns (adjusted to same size). Data for Oreamnos americanus (n = 6, 20) and Oreamnos harringtoni (n = 10, 13) from Mead & Lawler (1995), Bos (n = 18) from Grigson (1975), Antilocapra (n = 3) and Bison (n = 18) from Borkovic (2013), Ovis nivicola (n = 2), Ovis dalli (n = 2), Ovis ammon (n = 2), Ovis canadensis nelsoni (n = 5), Ovis canadensis canadensis (n = 8), Capra ibex sibirica (n = 4) and Capra ibex ibex (n = 5) from Bubenik (1990), Trioceros (n = 1) from TMP 1990.007.0350, Phrynosoma solare (n = 1) from LACM 123351, and P. asio (n = 1) from WLH 1093.


Conclusion
The combined results showing that the osteoderm spines, and their keratinous coverings, are positively allometric (regionally); and that the anterior portion of the osteoderm series is both highly variable and has species specific morphology, provided new insights into the function and evolution of these structures. Similar results have been obtained from analysis of the exaggerated structures of most other ornithischian clades: Hadrosauridae (Dodson, 1975; Evans, 2010; McGarrity, Campione & Evans, 2013), Ceratopsia (Currie et al., 2016; Dodson, 1976; Hone, Wood & Knell, 2016; Lehman, 1990), Pachycephalosauria (Horner & Goodwin, 2009; Schott et al., 2011). These results in other ornithischian clades have been used to support the hypothesis that these exaggerated structures may have functioned, and evolved, in the context of socio-sexual selection (Hone, Wood & Knell, 2016; Hopson, 1975; Sampson, 1997). Similar hypotheses have been proposed for thyreophoran spines and plates (Carpenter, 1998; Hopson, 1977; Main et al., 2005; Padian & Horner, 2011), but until now had lacked commensurate morphometric backing. This argument is strengthened further when the parascapular spine is considered. Not only does this element show a different pattern of scaling than the rest of the series, but the absolute sizes of the keratin sheath and bony core are similar to the horns of extant bovids, and the relative sizes similar to the horns of some extant squamates, both of which are thought to function in socio-sexual display (Bustard, 1958; Farlow & Dodson, 1975; Geist, 1966). Combined with recent evidence suggesting this spine may, in life, have been pigmented differently than the rest of the osteoderms (Brown et al., 2017), this suggests this spine may have function as a visual socio-sexual display signal with conspecifics.


Caleb M. Brown​. 2017. An Exceptionally Preserved Armored Dinosaur reveals the Morphology and Allometry of Osteoderms and their Horny Epidermal Coverings. PeerJ. 5:e4066.  DOI:  10.7717/peerj.4066

New research analyses body armour of Borealopelta  RoyalTyrrellMuseum.wordpress.com/2017/11/29/new-research-analyses-body-armour-of-borealopelta/ via @RoyalTyrrell

   

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روابط التحميل والمشاهدة، الروابط المباشرة للتحميل
او
شاهد هذا الفيديو القصير لطريقة التحميل البسيطة


كيف تحصل على مدونة جاهزة بآلاف المواضيع والمشاركات من هنا
شاهد قناة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على اليوتيوب لمزيد من الشرح من هنا
رابط مدونة منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات في أي وقت حــــتى لو تم حذفها من هنا
شاهد صفحة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على الفيس بوك لمزيد من الشرح من هنا
تعرف على ترتيب مواضيع منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات (حتى لا تختلط عليك الامور) من هنا

ملاحظة هامة: كل عمليات تنزيل، رفع، وتعديل المواضيع الجاهزة تتم بطريقة آلية، ونعتذر عن اي موضوع مخالف او مخل بالحياء مرفوع بالمدونات الجاهزة بآلاف المواضيع والمشاركات، ولكم ان تقوموا بحذف هذه المواضيع والمشاركات والطريقة بسيطة وسهلة. ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــسلامـ.

[Paleontology • 2018] Acantholipan gonzalezi • Paleodiversity of Late Cretaceous Ankylosauria from Mexico and Their Phylogenetic Significance ---ScRaBBlE


Acantholipan gonzalezi 
Rivera-Sylva, Frey, Stinnesbeck, Carbot-Chanona, Sanchez-Uribe & Guzmán-Gutiérrez, 2018


Abstract
Isolated bones and osteoderms of ankylosaurian dinosaurs recovered from Late Cretaceous sediments of northern Coahuila, northeastern Mexico, have been identified as remains of nodosaurids. Here, we summarize these discoveries and provide a review on Mexican Ankylosauria from a taxonomic perspective. We also present a new taxon, Acantholipan gonzalezi gen. et sp. nov. from the Pen Formation and provide a phylogenetic analysis integrating the new taxon. A. gonzalezi is the first named ankylosaur from Mexico that adds to the currently rare nodosaurid diversity from southern Laramidia.

Keywords: Dinosaur, Nodosauridae, Pen Formation, Mexico, Endemism, Laramidia 


Dinosauria Owen (1842)
Ornithischia Seeley (1887)
Thyreophora Nopcsa (1915)

Ankylosauria Osborn (1923)
Nodosauridae Marsh, 1890



Acantholipan gen. nov.
 Acantholipan gonzalezi sp. nov.

 Etymology: Greek αγκάθι (acanthus) = spine; and the Spanish contraction of Lépai-Ndé (gray people) lipan, a tribe of Apaches from northern Mexico; gonzalezi = in honor of Arturo H. Gonzalez González, for his outstanding support to Mexican paleontology.


Héctor E. Rivera-Sylva, Eberhard Frey, Wolfgang Stinnesbeck, Gerardo Carbot-Chanona, Iván E. Sanchez-Uribe and José Rubén Guzmán-Gutiérrez. 2018. Paleodiversity of Late Cretaceous Ankylosauria from Mexico and Their Phylogenetic Significance. Swiss Journal of Palaeontology DOI: 10.1007/s13358-018-0153-1

 Rivera-Sylva, H.E., Carpenter, K. and Aranda-Manteca, F.J. 2011, Late Cretaceous Nodosaurids (Ankylosauria: Ornithischia) from Mexico. Revista Mexicana de Ciencias Geológicas. 28(3); 271–278.  satori.geociencias.unam.mx/28-3/(04)RiveraSylva.pdf



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روابط التحميل والمشاهدة، الروابط المباشرة للتحميل
او
شاهد هذا الفيديو القصير لطريقة التحميل البسيطة


كيف تحصل على مدونة جاهزة بآلاف المواضيع والمشاركات من هنا
شاهد قناة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على اليوتيوب لمزيد من الشرح من هنا
رابط مدونة منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات في أي وقت حــــتى لو تم حذفها من هنا
شاهد صفحة منتدى مدونات بلوجر جاهزة بألاف المواضيع والمشاركات على الفيس بوك لمزيد من الشرح من هنا
تعرف على ترتيب مواضيع منتدى مدونات بلوجر جاهزة بآلاف المواضيع والمشاركات (حتى لا تختلط عليك الامور) من هنا

ملاحظة هامة: كل عمليات تنزيل، رفع، وتعديل المواضيع الجاهزة تتم بطريقة آلية، ونعتذر عن اي موضوع مخالف او مخل بالحياء مرفوع بالمدونات الجاهزة بآلاف المواضيع والمشاركات، ولكم ان تقوموا بحذف هذه المواضيع والمشاركات والطريقة بسيطة وسهلة. ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــسلامـ.

[Paleontology • 2018] Invictarx zephyri • A New Nodosaurid Ankylosaur (Dinosauria: Thyreophora) from the Upper Cretaceous Menefee Formation of New Mexico ---ScRaBBlE


 Invictarx zephyri 
McDonald​ & Wolfe, 2018

   DOI:  10.7717/peerj.5435 
Illustration by Kara Kelley

Abstract
Nodosauridae is a clade of armored dinosaurs with a rich fossil record and long history of study in North America. Nodosaurid fossils have been collected throughout the western United States and Canada. Here, we report three new nodosaurid specimens from the Upper Cretaceous (lower Campanian) Allison Member of the Menefee Formation, San Juan Basin, northwestern New Mexico. The three specimens belong to a new genus and species, Invictarx zephyri, characterized by a unique combination of features pertaining to the morphology of the osteoderms. Among the three specimens there are representative cervical/pectoral and thoracic osteoderms, as well as components of a probable co-ossified pelvic shield. The new tax on is most similar to Glyptodontopelta mimus from the Maastrichtian of New Mexico.


Figure 1: Stratigraphic occurrences of Invictarx zephyri and other ankylosaurs from the San Juan Basin.
Generalized stratigraphic column of Upper Cretaceous strata in the San Juan Basin, northwestern New Mexico, showing the stratigraphic positions of the nodosaurids I. zephyri and Glyptodontopelta mimus and the ankylosaurids Ahshislepelta minor, Nodocephalosaurus kirtlandensis, and Ziapelta sanjuanensis. Ankylosaur occurrence data are from Sullivan & Lucas (2015).
Nodosaurid silhouette by Scott Hartman (creativecommons.org), and ankylosaurid silhouette by Andrew A. Farke (creativecommons.org), both available from PhyloPic. Stratigraphic column is derived from data in Miller, Carey & Thompson-Rizer (1991), Molenaar et al. (2002), Sullivan & Lucas (2006), and Fowler (2017).



Illustration by Kara Kelley 

Systematic paleontology
Dinosauria Owen, 1842, sensu Baron, Norman & Barrett, 2017
Ornithischia Seeley, 1888, sensu Sereno, 2005

Thyreophora Nopcsa, 1915, sensu Sereno, 2005
Ankylosauria Osborn, 1923, sensu Sereno, 2005
Nodosauridae Marsh, 1890, sensu Sereno, 2005

Invictarx zephyri gen. et sp. nov.

Holotype: WSC 16505, incomplete postcranial skeleton including fragments of a dorsal rib, six complete or partial identifiable osteoderms (WSC 16505.1–WSC 16505.6), and fragments of additional osteoderms.

Referred specimens: Natural History Museum of Utah (UMNH) VP 28350, incomplete postcranial skeleton including three dorsal vertebrae, fragments of dorsal ribs, distal end of left humerus, distal end of left ulna, proximal ends of left and right radii, incomplete metacarpal, numerous incomplete but identifiable osteoderms, and fragments of additional osteoderms; UMNH VP 28351, incomplete postcranial skeleton including fragments of several dorsal centra, fragments of dorsal ribs, numerous incomplete but identifiable osteoderms, and fragments of additional osteoderms.

Etymology: Invictarx is derived from the Latin words invictus (“invincibleunconquerable”) and arx (“fortress”), in reference to the well-armored nature of ankylosaurian dinosaurs. The specific name, zephyri, is the genitive form of the Latin masculine noun zephyrus, “west wind,” in reference to the blustery conditions that prevail among the outcrops where the specimens were discovered. The full name may be translated as “unconquerable fortress of the western wind.”

Locality: All specimens were collected in San Juan County, New Mexico, on land administered by the U.S. BLM. Precise locality data are on file at WSC, UMNH, and the BLM.

Horizon: All specimens were collected from outcrops of the Juans Lake Beds (Miller, Carey & Thompson-Rizer, 1991) (Fig. 1), upper part of the Allison Member, Menefee Formation; lower Campanian, Upper Cretaceous (Molenaar et al., 2002; Lucas et al., 2005).

Specific diagnosis (as for genus by monotypy): nodosaurid ankylosaur distinguished by the following unique combination of characters: (1) observable on WSC 16505, UMNH VP 28350, and UMNH VP 28351 cervical/pectoral, thoracic, and pelvic osteoderms exhibit overall smooth surface texture, with little or no projecting rugosity, with abundant pits distributed randomly over the entire external surface, and with no neurovascular grooves or a small number of bifurcating and non-bifurcating neurovascular grooves distributed randomly, similar to Glyptodontopelta mimus but lacking the dense pattern of dendritic grooves that characterizes that taxon (Burns, 2008; Burns & Currie, 2014); (2) observable on WSC 16505 and UMNH VP 28351 some thoracic osteoderms exhibit a low, rounded keel with a deep groove extending craniocaudally along the apex, also present in the ankylosaurids Anodontosaurus lambei (Fig. 13G in Penkalski (2018)) and Platypelta coombsi (Fig. 13O in Penkalski (2018)) (P. Penkalski, 2018, personal communication), but absent in G. mimus (Burns, 2008); and (3) observable on UMNH VP 28351 probably possessed a co-ossified pelvic shield consisting of polygonal osteoderms of uniform size (Category 3 of Arbour, Burns & Currie (2011)), similar to some other nodosaurids, including Nodosaurus textilis (Lull, 1921), Stegopelta landerensis (Moodie, 1910), G. mimus (Ford, 2000; Burns, 2008), and Europelta carbonensis (Kirkland et al., 2013), as well as the ankylosaurid Aletopelta coombsi (Ford & Kirkland, 2001; Arbour & Currie, 2016).
....



Conclusions: 
The new nodosaurid I. zephyri provides further insight into the poorly known vertebrate fossil record of the Allison Member of the Menefee Formation. Although the known material is fragmentary, the osteoderms exhibit a unique combination of characters. The occurrence of Invictarx in the early Campanian of southern Laramidia aligns with previous hypotheses that nodosaurids were present in Laramidia throughout the Late Cretaceous, even as ankylosaurids suffered a local extinction and later reinvaded from Asia (Arbour, Zanno & Gates, 2016).


Andrew T. McDonald​ and Douglas G. Wolfe. 2018. A New Nodosaurid Ankylosaur (Dinosauria: Thyreophora) from the Upper Cretaceous Menefee Formation of New Mexico. PeerJ. 6:e5435.  DOI:  10.7717/peerj.5435

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