A new species of Oviparosiphidae (Hemiptera: Aphidomorpha) from the Lower Cretaceous of China

2017 ◽  
Vol 75 ◽  
pp. 157-161 ◽  
Author(s):  
Ying Fu ◽  
Yunzhi Yao ◽  
Gexia Qiao ◽  
Yunyun Zhao ◽  
Dong Ren
2021 ◽  
pp. 1-9
Author(s):  
Mateo Daniel Monferran ◽  
Flaviana Jorge de Lima ◽  
Alexander Wilhelm Armin Kellner ◽  
Juliana Manso Sayão ◽  
Edilson Bezerra Santos Filho ◽  
...  

2017 ◽  
Vol 91 (4) ◽  
pp. 1200-1214 ◽  
Author(s):  
Peihong JIN ◽  
Teng MAO ◽  
Junling DONG ◽  
Zixi WANG ◽  
Mingxuan SUN ◽  
...  

Zootaxa ◽  
2016 ◽  
Vol 4200 (2) ◽  
pp. 327 ◽  
Author(s):  
PEDRO S. R. ROMANO

Pelomedusoides is the most diverse clade of side-necked turtles and there is an extensive fossil record (de Broin, 1988; Lapparent de Broin, 2000; Gaffney et al., 2006, 2011) that dates back at least to the Barremian (Lower Cretaceous) (Romano et al., 2014). Its large fossil record evidences a greater diversity in the past, particularly at the end of the Mesozoic, and exhibits a good sampling of species that are represented by skull material (Gaffney et al., 2006, 2011). As a consequence, the most complete and recent phylogenetic hypotheses for this clade (e.g. Romano et al., 2014; Cadena, 2015) are based on matrices comprising a great amount of cranial characters derived largely from Gaffney et al. (2006, 2011). In addition, it is well established that shell characters show a lot of phenotypic plasticity, even in the fossil species (Romano, 2008; Gaffney et al., 2006, 2011). In most cases it consequently is not justified to rely on “diagnostic features” of poorly informative shell-only material for describing a new species. Because of that, most authors remark new morphotypes in the literature when such aberrant specimens are recovered, but do not make any nomenclatural act by proposing a new yet poorly supported species (e.g. Romano et al., 2013; Ferreira & Langer, 2013; Menegazzo et al., 2015). Unfortunately, such a supposedly new bothremydid turtle (Pleurodira: Bothremydidae) from the Early Paleocene of Brazil was recently described based on poorly diagnostic remains (Carvalho et al., 2016; hereafter CGB, for the authors initials) and a correction of this unfounded nomenclatural act is required. In addition I present some comments on shell only material from Brazil in order to guide splitter-taxonomists to stop describing poorly preserved fossil specimens as new species. 


Ameghiniana ◽  
2020 ◽  
Vol 57 (6) ◽  
Author(s):  
Maria E. P. Batista ◽  
Lutz Kunzmann ◽  
Artur A. Sá ◽  
Antônio Á. F. Saraiva ◽  
Maria I. B. Loiola

2020 ◽  
Vol 3 (4) ◽  
pp. 352-356
Author(s):  
DANY AZAR ◽  
SIBELLE MAKSOUD

Psychodidae Newman, 1834 is a large family of small, hairy nematoceran dipterans, comprising more than 2,600 described extant species. It is currently subdivided into seven subfamilies: Bruchomyiinae Alexander, 1920, Horaiellinae Enderlein, 1936, Phlebotominae Rondani, 1840, Psychodinae Newman, 1834, Sycoracinae Jung, 1954, Trichomyiinae Tonnoir, 1922, and the fossil subfamily Protopsychodinae Stebner et al., 2015. Some authors consider the group to consist of two families, i.e., Psychodidae and Phlebotomidae (Williams, 1993; Azar et al., 1999). This fact is founded only on the hematophagous and medically important aspects of the phlebotomines, nevertheless this arrangement is unfounded, because the phylogenetic relationships between the psychodid subfamilies remain unresolved, even if there is a possible sister-group relationship between the Phlebotominae and Psychodinae (Curler & Moulton, 2012). We consider recognizing phlebotomines as a separate family would necessitate also giving separate familial status to all the currently recognized subfamilies, which is not adopted here.


Phytotaxa ◽  
2020 ◽  
Vol 449 (2) ◽  
pp. 164-172
Author(s):  
ANDREY O. FROLOV ◽  
IRINA M. MASHCHUK

Study of isolated leaf compressions from Prisayan Formation outcrops on the right side of the Irkutsk reservoir resulted in identification of a new species: Marskea cuspidata sp. nov. The species has a strong morphological affinity with M. heeriana N. Nosova et Kiritchkova and T. ketovae Teslenko. The epidermis original texture differs well the Marskea cuspidata sp. nov. from other representatives of the genus Marskea which are known from the Jurassic and Lower Cretaceous sediments of Europe, Central Asia and Siberia.


2018 ◽  
Vol 85 ◽  
pp. 109-127 ◽  
Author(s):  
Pei-Hong Jin ◽  
Jun-Ling Dong ◽  
Zi-Xi Wang ◽  
Xiu-Cai Yuan ◽  
Yi-Fan Hua ◽  
...  

The osteology of Ornithosuchus is described in some detail. This study is largely based on material discussed by previous workers, but also takes into account specimens hitherto undescribed. It is considered that the species O. taylori Broom 1913 is invalid, being based on larger individuals of the form previously named O. woodwardi by Newton (1894). Furthermore, evidence is presented to show that specimens previously described by Huxley (1877) and Walker (1961) as Dasygnathus longidens are also referable to Ornithosuchus . It is concluded that but one species is present in the material, the correct name for which is Ornithosuchus longidens (Huxley). At least eleven individuals are present with skulls ranging from about 50 to 450 mm in length. Observations on the smaller members of this series suggest that changes in the shape and proportions of the skull took place with growth in a similar manner to those seen in living crocodiles. In the light of new information concerning the osteology of Ornithosuchus it is considered that this reptile is a primitive carnosaur, occupying a position very close to the ancestry of the Jurassic and Cretaceous members of this group. An examination of descriptions and figures of Triassic reptiles referred by von Huene (1932) and later authors to the Carnosauria has led to the conclusion that the great bulk of this material is more properly allocated to the Prosauropoda, and that the only Triassic carnosaurs known at the present time, apart from Ornithosuchus , are Teratosaurus and Sinosaurus , these two names being here used in a restricted sense. It is suggested that Ornithosuchus is close to the common ancestry of both the Megalosauridae and the Tyrannosauridae, and the derivation of the skull patterns of these forms from that of Ornithosuchus is discussed. Additional fenestrations marginal to the preorbital fossa and in the surangular of advanced carnosaurs are held to be related to the development of the pterygoid musculature rather than to the need to lighten the skull. In the course of a brief review of the Carnosauria the view is put forward that Acrocanthosaurus is a Lower Cretaceous representative of the tyrannosaur group, using this term in a broad sense, and is perhaps related to the Cenomanian Spinosaurus and the Wealden Altispinax . As a result of examination of English megalosaurian material, the name Eustreptospondylus oxoniensis gen. et sp.nov. is proposed for the Oxford specimen previously known as ‘ Streptospondylus’ cuvieri , and Metriacanthosaurus gen.nov. for Megalosaurus parkeri . The incomplete cranium from Dives figured by Piveteau (1923) is made the type of a new species, E. divesensis , to which certain other carnosaurian material from Normandy is provisionally allocated. Following Chakravarti (1935), the endoskeletal elements included by Matley (1923) in the type material of the Indian nodosaur Lametasaurus are held to belong to one or other of the two carnosaurs Indosuchus and Indosaurus, but the numerous scutes are not thought to be carnosaurian and the name Lametasaurus is here restricted to them. It is suggested that Indosuchus from the ? Turonian is a tyrannosaund. On the other hand Ceratosaurus and Proceratosaurus are regarded as coelurosaurs. A modified classification of the Infra-order Carnosauria is given, in which two main groups are recognized; Superfamily Megalosauroidea to include the Megalosauridae, and Superfamily Tyrannosauroidea to include the Ornithosuchidae (restricted), Spinosauridae and Tyrannosauridae.


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