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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 Paleocene. Show all posts
Showing posts with label Paleocene. Show all posts

Wednesday, March 20, 2019

[PaleoOrnithology • 2017] Tsidiiyazhi abini • Early Paleocene Landbird Supports Rapid Phylogenetic and Morphological Diversification of Crown Birds after the K–Pg Mass Extinction ---ScRaBBlE


 Tsidiiyazhi abini 
Ksepka, Stidham & Williamson, 2017 

 Artwork by Sean Murtha @KsepkaLab  DOI: 10.1073/pnas.1700188114 

Significance: 
Molecular (DNA) studies suggest that birds radiated rapidly in the wake of the Cretaceous–Paleogene mass extinction (66 Ma), diversifying into nearly all the major groups we recognize today. However, fossil evidence for this pattern has been difficult to find because of the poor fossilization potential of small, delicate-boned birds. We report a tiny species of bird from ∼62.5 million-year-old rocks in New Mexico. Tsidiiyazhi abini (Navajo for “little morning bird”) is an ancient species of mousebird (Coliiformes). The fossil provides evidence that many groups of birds arose just a few million years after the mass extinction and had already begun evolving specializations of the foot for different ecological roles.

Abstract
Evidence is accumulating for a rapid diversification of birds following the K–Pg extinction. Recent molecular divergence dating studies suggest that birds radiated explosively during the first few million years of the Paleocene; however, fossils from this interval remain poorly represented, hindering our understanding of morphological and ecological specialization in early neoavian birds. Here we report a small fossil bird from the Nacimiento Formation of New Mexico, constrained to 62.221–62.517 Ma. This partial skeleton represents the oldest arboreal crown group bird known. Phylogenetic analyses recovered Tsidiiyazhi abini gen. et sp. nov. as a member of the Sandcoleidae, an extinct basal clade of stem mousebirds (Coliiformes). The discovery of Tsidiiyazhi pushes the minimum divergence ages of as many as nine additional major neoavian lineages into the earliest Paleocene, compressing the duration of the proposed explosive post–K–Pg radiation of modern birds into a very narrow temporal window parallel to that suggested for placental mammals. Simultaneously, Tsidiiyazhi provides evidence for the rapid morphological (and likely ecological) diversification of crown birds. Features of the foot indicate semizygodactyly (the ability to facultatively reverse the fourth pedal digit), and the arcuate arrangement of the pedal trochleae bears a striking resemblance to the conformation in owls (Strigiformes). Inclusion of fossil taxa and branch length estimates impacts ancestral state reconstructions, revealing support for the independent evolution of semizygodactyly in Coliiformes, Leptosomiformes, and Strigiformes, none of which is closely related to extant clades exhibiting full zygodactyly.

Keywords: aves, phylogeny, morphology, fossil, evolution


Fossil bones of Tsidiiyazhi abini, a 62.5 million-year-old fossil representing the oldest arboreal species of crown bird.
photos: Kate Dzikiewicz  

Systematic Paleontology
 Aves Linnaeus, 1758
 Coliiformes Murie, 1872 cf. 
Sandcoleidae Houde and Olson, 1992 

Tsidiiyazhi abini, gen. et sp. nov

Etymology. The genus and species names are derived from the Navajo (Diné Bizaad) language, reflecting the discovery of the fossil within ancestral Navajo lands. The genus name is derived from the words “tsidii” for “bird” and “yazhi” for “little,” in reference to the fossil’s small size. The specific epithet is derived from the Navajo word “abini” for “morning,” referencing the early Paleocene age of the taxon. Pronunciation using International Phonetic Alphabet phonetic symbols is as follows: /tsɪdi:jæʒi:/ /′ɔbɪnɪ/.

Type Locality and Horizon. NMMNH locality L-6898 comprises a relatively thin (<10 cm) muddy siltstone bed of restricted areal extent, representing an exposure of the Ojo Encino Member of the Nacimiento Formation. The site is located on the West Flank of Torreon Wash within the San Juan Basin, in Sandoval County, New Mexico. ....

Diagnosis. Tsidiiyazhi abini is differentiated from all other Coliiformes by the following apomorphies: (i) tubercle on the medial face of cranial end of the scapula, (ii) strongly developed triangular protuberance at the apex of impressio m. sternocoracoidei of the coracoid, (iii) medially displaced distal exit of canalis extensorius of the tibiotarsus, and (iv) arcuate arrangement of the metatarsal trochleae. 

....

Tsidiiyazhi abini life reconstruction by Sean Murtha.


Daniel T. Ksepka, Thomas A. Stidham and Thomas E. Williamson. 2017. Early Paleocene Landbird Supports Rapid Phylogenetic and Morphological Diversification of Crown Birds after the K–Pg Mass Extinction. Proceedings of the National Academy of Sciences. DOI: 10.1073/pnas.1700188114

New species of ancient bird discovered in New Mexico phy.so/418976380 @physorg_com

 

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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.

[PaleoIchthyology • 2016] Eekaulostomus cuevasae • An Ancient Armored Trumpetfish (Aulostomoidea) from Danian (Paleocene) Marine Deposits of Belisario Domínguez, Chiapas, southeastern Mexico ---ScRaBBlE


Eekaulostomus cuevasae 
Cantalice & Alvarado-Ortega,  2016

ABSTRACT
Eekaulostomus cuevasae gen. and sp. nov. is described and identified here as a new member of the superfamily Aulostomoidea. The single specimen known of this species is part of a newly fossil assemblage collected in the marine sediments belonging to the early Paleocene Tenejapa-Lacandón geological unit, exploited in the Belisario Domínguez quarry, near Palenque town, State of Chiapas, southeastern Mexico. E. cuevasae represents the oldest aulostomoid as far known and the first fossil species of this superfamily collected in America. E. cuevasae differs from other aulostomoids in the presence of two spines preceding the soft rays of both dorsal and anal fins; the star-like scales covering the entire body and part of the snout; as well as the relative large number of principal rays in the caudal fin. The recognition of E. cuevasae as the stem group of Aulostomoidea increases the temporal and geographic distribution of this superfamily up to Danian and within the Caribbean region, when a large part of Chiapas was under the sea after the Cretaceous-Tertiary mass extinction event. This finding also provides evidences suggesting the membership of Aulostomoidea within the order Gasterosteiformes, in which the scutes covering the trunk and the robust spines in unpaired fins are recurrent features.

  Keywords: new species; Aulostomoidea; fossil; Paleocene; Chiapas; Mexico

Figure 2: Holotype. IGM 4716, almost complete specimen exposing the right lateral side of the body.  



Systematic Paleontology
Superfamily AULOSTOMOIDEA sensu Greenwood et al., 1966
Family EEKAULOSTOMIDAE fam. nov.
Genus EEKAULOSTOMUS gen. nov.
Type species. Eekaulostomus cuevasae sp. nov.,  

Derivation of name. The genus name includes the Mayan word “Eek” (= star), the Greek word "aulos" (= αὐλός, that is the name of an ancient flute), and the Latin word "stoma" (= mouth). The name refers to a "fish with a star-like scutes and flute-shaped mouth."
Eekaulostomus cuevasae sp. nov.
Derivation of name. The specific epithet of this fish honors our colleague, Martha Cuevas García, whose dedication and newly passion for the fossils led us to find the only specimen of Eekaulostomus cuevasae.

Occurrence. Paleocene (Danian, ≈ 63Ma) marine strata of the Tenejapa-Lacandón geological unit. Belisario Domínguez quarry, Salto de Agua Municipality, State of Chiapas, southeastern Mexico (Alvarado-Ortega et al., 2015).

Diagnosis. Aulostomoidea fish with rigid star-like scutes covering the whole trunk and part of the snout; pelvic fin placed anteriorly, just behind the postcleithrum; two spines in front of the soft rays of dorsal and anal fins; eight soft rays in both anal and dorsal fins; caudal fin formula iv+I+7—5+I+iii.
CONCLUSIONS 
Fossils referring to the superfamily Aulostomoidea had been collected more than 200 years ago in Eocene and younger marine deposits along Europe. Although the extant aulostomoids form part of large modern cladistics essays, some are based on morphological evidences and others on molecular data; unfortunately, the fossil aulostomoids have never been phylogenetically studied. This situation has prevented the generation of a robust classification of the aulostomoids, and at the same time, has fueled the differences and contradictions between the phylogenetic hypotheses already published. It is so, that it is desirable to make these European fossils part of future cladistic studies; however, first we have to fulfill the task of re-describing them accurately using modern and homogeneous criteria. Only up to the present day, the distribution of fossil aulostomoids was restricted to Europe. Although this fact has not interested paleontologists outside of Europe to further collaborate in studies concerning the diversity evolution of aulostomoids; the goal of this paper is to provide the first tangible evidence that in the past, this fish group was also an inhabitant of the American seas.

From now on, we must take more seriously the paleontological surveys on late Cretaceous and early Paleocene sites with marine sediments present throughout the tropical region of America. As present study shows, fossils may exist that allow us to delve into the details of the evolution of the fishes on both sides of Cretaceous-Tertiary mass extinction event. Sadly, during the joint INAH-UNAM project, from which this article was drawn, no other fossil aulostomoid was recovered; however, the collection effort applied in Belisario Domínguez (where Eekaulostomus cuevasae gen. and sp. nov. came) as well as in its coeval and neighbor quarry, División del Norte, both with Danian marine sediments, really is far from reaching saturation.

The re-examination of the relationships of the Aulostomoidea executed here, using datasets previously generated by other authors and including Eekaulostomus cuevasae gen. and sp. nov., might not be the best way to achieve the desired understanding on the evolutionary processes of these fishes; however, this exercise significantly contributes to this goal. On the one side, the undeniable position of this new species as a primitive aulostomoid member, together with its deep morphological differences with other extinct and living taxa formally, or putatively, included in such superfamily, trace possible trends in morphological changes experienced by these fishes since the Paleocene to the present. This essay also widens the geographical scenario where the evolution of these fishes took place, extending from Europe to the tropical region of America.


  Cantalice, Kleyton Magno and Alvarado-Ortega, Jesús. 2016. Eekaulostomus cuevasae gen. and sp. nov., An Ancient Armored Trumpetfish (Aulostomoidea) from Danian (Paleocene) Marine Deposits of Belisario Domínguez, Chiapas, southeastern Mexico. Palaeontologia Electronica. 19.3.53A: 1-24

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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.

[PaleoOrnithology • 2017] Kumimanu biceae • A Paleocene Penguin from New Zealand Substantiates Multiple Origins of Gigantism in Fossil Sphenisciformes ---ScRaBBlE


Kumimanu biceae
Mayr, Scofield, De Pietri & Tennyson, 2017


Abstract
One of the notable features of penguin evolution is the occurrence of very large species in the early Cenozoic, whose body size greatly exceeded that of the largest extant penguins. Here we describe a new giant species from the late Paleocene of New Zealand that documents the very early evolution of large body size in penguins. Kumimanu biceae, n. gen. et sp. is larger than all other fossil penguins that have substantial skeletal portions preserved. Several plesiomorphic features place the new species outside a clade including all post-Paleocene giant penguins. It is phylogenetically separated from giant Eocene and Oligocene penguin species by various smaller taxa, which indicates multiple origins of giant size in penguin evolution. That a penguin rivaling the largest previously known species existed in the Paleocene suggests that gigantism in penguins arose shortly after these birds became flightless divers. Our study therefore strengthens previous suggestions that the absence of very large penguins today is likely due to the Oligo-Miocene radiation of marine mammals.




Systematic paleontology
Aves Linnaeus, 1758
Sphenisciformes Sharpe, 1891

Kumimanu biceae, n. gen. et sp.

  Holotype. NMNZ S.45877: partial skeleton of a single individual including cranial end of left scapula, incomplete right coracoid, cranialmost portion of sternum, partial left humerus, incomplete proximal end of left ulna, right femur, right tibiotarsus lacking proximal end, partial synsacrum, three vertebrae, and various bone fragments.

  Etymology. From kumi (Maori), a large mythological monster, and manu (Maori), bird. The species epithet honors Beatrice (“Bice”) A. Tennyson, the mother of AJDT, who fostered his interest in natural history (pronounced “bee-chee-ae”).

  Type locality and horizon. Hampden Beach, Otago, New Zealand (NZ Fossil Record Number J42/f0956; precise locality information is recorded at NMNZ); Moeraki Formation, late Paleocene (late Teurian, local stratigraphic level NZP522, which has an absolute age of 55.5.-59.5 million years23; a matrix sample taken from the fossil (GNS Science sample L29126) contained a specimen of the dinoflagellate Palaeocystodinium australinum and an unnamed dinoflagellate taxon that support a Teurian age for this sample; C. Clowes, pers. comm.).

  Diagnosis. A very large-sized sphenisciform species, which is characterized by proximodistally low and widely spaced condyles of the tibiotarsus. Distinguished from the late Paleocene Crossvallia and all post-Paleocene Sphenisciformes of which humeri are known in the dorsoventrally narrower humerus shaft, with ratio of maximum width of proximal end of humerus to minimum width of shaft being 2.4 (less than this value in Crossvallia and all post-Paleocene Sphenisciformes of which the humerus is known). Distinguished from Waimanu tuatahi in having the bicipital crest of humerus not forming a distally directed bulge. Distinguished from Waimanu manneringi (the humerus of which is unknown) in having the tibiotarsus with proximodistally lower and more widely spaced condyles.


The humerus (top) and a bone from the shoulder girdle (coracoid, bottom) of the Paleocene giant penguin Kumimanu biceae, compared to the corresponding bones of one of the largest fossil penguins known to date (Pachydyptes ponderosus from the Eocene in New Zealand) and those of an Emperor Penguin (Aptendodytes forsteri).

photo: G. Mayr/Senckenberg Research Institute.


Gerald Mayr, R. Paul Scofield, Vanesa L. De Pietri and Alan J. D. Tennyson. 2017. A Paleocene Penguin from New Zealand substantiates multiple origins of gigantism in fossil Sphenisciformes. Nature Communications. 8, Article number: 1927. DOI:  10.1038/s41467-017-01959-6

A giant human-sized ancient penguin has been discovered  ibt.uk/A6vYD 
Ancient man-sized penguin found in New Zealand beach  zmescience.com/science/news-science/man-sized-penguin-zealand-12122017/ via @zmescience
 「怪物」サイズのペンギン、ニュージーランドで化石発見  afpbb.com/articles/-/3155164?pid=19636136 via @afpbbcom

   

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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] Cicada Fossils (Cicadoidea: Tettigarctidae and Cicadidae) with A Review of the Named Fossilised Cicadidae ---ScRaBBlE


(4) Platypedia primigenia, nearly entire specimen, wings superimposed over ventro-lateral body, in Colorado University Museum of Natural History, USA. (5a) Tibicina gigantea holotype, dorsal, entire specimen, from Boulard & Riou (1989). (5b) Tibicina gigantea close-up of left forewing base, from Boulard & Riou (1989). (6) Tibicina haematodes, forewing, from Wagner (1967). (7) Tibicina sakalai, holotype, including counterpart, female, lateral, from Prokop & Boulard (2000).

(1) Graptopsaltria aff. nigrofuscata forewing; in National Museum of Nature and Science, Japan; NSM-PA12018; image courtesy Yasunari Shigeta. (4) Minyscapheus dominicanus, holotype, whole specimen in amber; in collection George Poinar; image courtesy George Poinar. (5) Miocenoprasia grasseti, holotype, ventral impression; in Riou collection, Musée de Paléontologie, La Voulte-sur-Rhône, France; image courtesy Bernard Riou.  (7) Dominicicada youngi, holotype, hatchling in amber; in collection George Poinar; image courtesy George Poinar.

(2) Tanna? sp. hindwing; in National Museum of Nature and Science, Japan; NSM-PA12017; image courtesy Yasunari Shigeta. (3) Auritibicen bihamatus forewing; in National Museum of Nature and Science, Japan; NSM-PA12045; image courtesy Yasunari Shigeta. (6) Yezoterpnosia nigricosta forewing; in National Museum of Nature and Science, Japan; NSM-PA12019; image courtesy Yasunari Shigeta. (8) Burmacicada protera, holotype, hatchling in amber; in collection George Poinar; image courtesy George Poinar.

in Moulds, 2018. 

Abstract
The Cicadoidea comprise two families, the Cicadidae and the Tettigarctidae. This paper evaluates the status and taxonomy of all named Cicadoidea fossils belonging to the Cicadidae. Shcherbakov (2009) has previously revised the Tettigarctidae. Two new genera are described, Camuracicada gen. n. and Paleopsalta gen. n., for Camuracicada aichhorni (Heer, 1853) comb. n. and Paleopsalta ungeri (Heer, 1853) comb. n. A lectotype is designated for Cicada emathion Heer, 1853.

          Cicada grandiosa Scudder, 1892 is transferred to Hadoa Moulds, 2015 as Hadoa grandiosa comb. n.; Oncotympana lapidescens J. Zhang, 1989 is transferred to Hyalessa China, 1925 as Hyalessa lapidescens comb. n.; Meimuna incasa J. Zhang, Sun & X. Zhang, 1994 and Meimuna miocenica J. Zhang & X. Zhang, 1990 are transferred to Cryptotympana Stål, 1861 as Cryptotympana incasa comb. n. and Cryptotympana miocenica comb. n.; Tibicen sp. aff. japonicus Kato, 1925 is transferred to Auritibicen as Auritibicen sp. aff. japonicus comb. n., and Terpnosia sp. aff. vacua Olivier, 1790 is transferred to Yezoterpnosia Matsumura, 1917 as Yezoterpnosia sp. aff. vacua comb. n. The generic placement of two other fossils is changed to reflect current classification, those species now being Auritibicen bihamatus (Motschulsky, 1861) and Yezoterpnosia nigricosta (Motschulsky, 1866).

         Two species, Davispia bearcreekensis Cooper, 1941 and Lithocicada perita Cockerell, 1906, are transferred from the subfamily Cicadinae to the Tibicininae, tribe Tibicinini. Cicadatra serresi (Meunier, 1915) is also transferred from the Cicadinae to the Cicadettinae because the Cicadatrini have recently been transferred from the Cicadinae to the Cicadettinae (Marshall et al. 2018).

         Miocenoprasia grasseti Boulard and Riou, 1999 is transferred from the tribe Prasiini to the Lamotialnini. Tymocicada gorbunovi Becker-Migdisova, 1954 is transferred from the Dundubiini to the Cryptotympanini; Paracicadetta oligocenica Boulard & Nel, 1990 is transferred from the Cicadettini to the Pagiphorini and Minyscapheus dominicanus Poinar et al., 2011 is assigned to the Taphurini. Names of species once considered to belong in Cicadidae, but now excluded, are listed with explanation.

Keywords: Hemiptera, Eocene, Cretaceous, Jurassic, Miocene, Oligocene, Paleocene, Quaternary, Pleistocene, Pliocene, Tertiary

PLATE 2. (1) Lyristes renei, holotype, from Riou (1995). (2) Auritibicen sp. aff. japonicus comb. n., in Osaka Museum of Natural History, image Shigehiko Shiyake. (3) Paracicadetta oligocenica, holotype, part and counterpart, from Boulard & Nel (1990). (4) Platypedia primigenia, nearly entire specimen, wings superimposed over ventro-lateral body, in Colorado University Museum of Natural History, USA; UCM 29658, not the type; image David Zelagin. (5a) Tibicina gigantea holotype, dorsal, entire specimen, from Boulard & Riou (1989). (5b) Tibicina gigantea close-up of left forewing base, from Boulard & Riou (1989). (6) Tibicina haematodes, forewing, from Wagner (1967). (7) Tibicina sakalai, holotype, including counterpart, female, lateral, from Prokop & Boulard (2000).

PLATE 3. (1) Graptopsaltria aff. nigrofuscata forewing; in National Museum of Nature and Science, Japan; NSM-PA12018; image courtesy Yasunari Shigeta. (2) Tanna? sp. hindwing; in National Museum of Nature and Science, Japan; NSM-PA12017; image courtesy Yasunari Shigeta. (3) Auritibicen bihamatus forewing; in National Museum of Nature and Science, Japan; NSM-PA12045; image courtesy Yasunari Shigeta. (4) Minyscapheus dominicanus, holotype, whole specimen in amber; in collection George Poinar; image courtesy George Poinar. (5) Miocenoprasia grasseti, holotype, ventral impression; in Riou collection, Musée de Paléontologie, La Voulte-sur-Rhône, France; image courtesy Bernard Riou. (6) Yezoterpnosia nigricosta forewing; in National Museum of Nature and Science, Japan; NSM-PA12019; image courtesy Yasunari Shigeta. (7) Dominicicada youngi, holotype, hatchling in amber; in collection George Poinar; image courtesy George Poinar. (8) Burmacicada protera, holotype, hatchling in amber; in collection George Poinar; image courtesy George Poinar.

M. S. Moulds. 2018. Cicada Fossils (Cicadoidea: Tettigarctidae and Cicadidae) with A Review of the Named Fossilised Cicadidae. Zootaxa.  4438(3); 443–470. DOI:  10.11646/zootaxa.4438.3.2



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