scholarly journals A Miocene pyrgodesmid millipede (Polydesmida: Pyrgodesmidae) from Mexico

PeerJ ◽  
2021 ◽  
Vol 9 ◽  
pp. e10574
Author(s):  
Francisco Riquelme ◽  
Miguel Hernández-Patricio ◽  
Michelle Álvarez-Rodríguez

A new fossil species of pyrgodesmid millipede (Polydesmida: Pyrgodesmidae) placed in the genus Myrmecodesmus Silvestri, 1910 is described. The type materials are two amber inclusions, male and female specimens that come from Miocene strata in Chiapas, Mexico. Myrmecodesmus antiquus sp. nov. has collum with 10 dorsal tubercles; without porosteles or ozopores; legs of the rings 2–9 with a short projection on the prefemur in both the female and male. Myrmecodesmus antiquus sp. nov is the first fossil record of the genus Myrmecodesmus. This is a New World taxon that belongs to the pantropical family Pyrgodesmidae. Thus, Myrmecodesmus antiquus sp. nov expands the range of the genus to the Miocene tropics in Middle America.

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Iwona Kania-Kłosok ◽  
Wiesław Krzemiński ◽  
Antonio Arillo

AbstractFirst record of the genus Helius—long-rostrum cranefly from Maestrazgo Basin (eastern Spain, Iberian Penisula) is documented. Two new fossil species of the genus Helius are described from Cretaceous Spanish amber and compared with other species of the genus known from fossil record with particular references to these known from Cretaceous period. Helius turolensis sp. nov. is described from San Just amber (Lower Cretaceous, upper Albian) Maestrazgo Basin, eastern Spain, and Helius hispanicus sp. nov. is described from Álava amber (Lower Cretaceous, upper Albian), Basque-Cantabrian Basin, northern Spain. The specific body morphology of representatives of the genus Helius preserved in Spanish amber was discussed in relation to the environmental conditions of the Maestrazgo Basin and Basque-Cantabrian Basin in Cretaceous.


2000 ◽  
Vol 31 (2) ◽  
pp. 209-224 ◽  
Author(s):  
Terry A. Wheeler

AbstractMallochianamyia Santos-Neto was proposed as a replacement name for Gayomyia Malloch, 1933 (preoccupied by Gayomyia Banks, 1913), an unplaced genus of acalyptrate Diptera from Chile and Argentina. The genus comprises 12 species: M. cladostyla sp. n.; M. fenestrata sp. n.; M. flavitibia sp. n.; M. furcata sp. n.; M. gallina sp. n.; M. latigena sp. n.; M. magnipalpis sp. n.; M. nigrohalterata (Malloch) comb. n.; M. penai sp. n.; M. setosa sp. n.; M. truncata sp. n.; M. vexans sp. n. All new species are illustrated and a key to species of Mallochianamyia is provided. The monophyly of the genus is supported by three characters of the male and female genitalia. Mallochianamyia is most closely related to the New World genera Paraleucopis Malloch and Schizostomyia Malloch and an undescribed Australian genus. The group cannot be placed in any established family as currently defined, although there are affinities to some families in the Asteioinea sensu J. F. McAlpine (1989). Research on the morphology and relationships of genera related to Mallochianamyia is required to clarify the familial status of the group.


2018 ◽  
Vol 49 (4) ◽  
pp. 399-408
Author(s):  
Sara Gamboa ◽  
Vicente M. Ortuño

Limodromus emetikos sp. n. (Coleoptera: Carabidae) is described and illustrated from Baltic amber (Eocene). Based on its morphological features, the new species is considered a sister taxon of the extant Holarctic assimilis species group. Furthermore, the specimen described here could represent a case of stress-triggered regurgitation, which would represent the first fossil record of such a process in beetles.


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. 


Antiquity ◽  
1940 ◽  
Vol 14 (54) ◽  
pp. 117-137 ◽  
Author(s):  
J. Grahame D. Clark

The dictum of Clark Wissler that ‘New World culture is [thus] a kind of pyramid whose base is as broad as the two Americas and whose apex rests over Middle America’ is one of those brilliant generalizations which at once sum up the conclusions already reached, and point the way to further progress.From the vantage of today one may agree with A. V. Kidder (22, p. 145) that American archaeologists have been unduly neglectful of the broad base of their pyramid. Yet itwould be churlish to blame them when the apex was so enticing, so rich, so bizarre and above all so enigmatic. Indeed, when men first descried the peaks of Maya, Mexican and Peruvian achievement, it seemed hard to connect them with the lowly foot- hills of cultural attainment familiar in the temperate latitudes of the western hemisphere. Until the underlying unity of civilization in the New World was recognized, its pyramidal structure could hardly be appreciated; in default of this it is easy to understand how archaeologists tended to neglect cultures, which, however interesting they may appear to us from the historical angle, must have appeared to them as intrinsically poor and dull. Then again it was only on the edges of the pyramid that the foundation layer was visible; elsewhere it was buried under a superstructure, massive in proportion to its attractiveness.


2017 ◽  
Vol 188 (3) ◽  
pp. 12 ◽  
Author(s):  
Matúš Hyžný ◽  
Sten Lennart Jakobsen ◽  
René H. B. Fraaije

The fossil record of the burrowing lobster Axius is reviewed. A diagnosis based on the characters with preservation potential is supplied. Plioaxius lineadactylus Fraaije et al., 2011, from the Pliocene of Belgium and the Netherlands is considered congeneric with the type species of Axius. As a consequence, Plioaxius is considered a junior subjective synonym of Axius. A newly described species, Axius hofstedtae from the late Oligocene of Denmark is considered the oldest unequivocal representative of Axius. Both fossil species, A. hofstedtae n. sp. and A. lineadactylus n. comb., share numerous morphological characters with extant Axius stirhynchus. Scarcity of the Cenozoic Axiidae is ascribed to lack of study of the fossil record of this group rather than to low fossilization potential of its representatives. A preliminary scenario of the migration of Axius based on the scarce fossil record suggests the origin in the Western Tethys and subsequent dispersal westward into the West Atlantic and eastward into the West Pacific.


2020 ◽  
Vol 25 (10) ◽  
pp. 1754-1764
Author(s):  
Andrés O. Porta ◽  
Daniel N. Proud ◽  
Peter Michalik ◽  
Fabio Akashi Hernandes

A protonymph of the snout mite genus Odontoscirus Thor, 1913, O. cretacico sp. nov., is described and illustrated from Cretaceous amber of Myanmar is described and illustrated, constituting the earliest fossil species described of the family Bdellidae (ca. 99 Ma). After reexamining the literature and recollected specimens from type localities, we conclude that the following five recent species do not belong to the genus Biscirus and should be transferred to Odontoscirus: O. anomalicornis (Berlese 1916) comb. nov., O. symmetricus (Kramer 1898) comb. nov., O. uncinatus (Kramer 1898) comb. nov., O. norvegicus (Thor 1905) comb. nov., and O. insularis (Willmann 1939) comb. nov. The implications of the fossil record of the family is discussed.


2020 ◽  
Vol 94 (4) ◽  
pp. 696-715 ◽  
Author(s):  
Mateusz Zmudzinski

AbstractThe fossil record of the family Camerobiidae has been represented by only one species, Neophyllobius succineus Bolland and Magowski, 1990, described from Eocene Baltic amber. These prostigmatan mites are distinguishable by their distinctly long and slender stilt-like legs, and they are associated with aboveground vegetation where they hunt for other small invertebrates. This paper enhances the knowledge of fossil stilt-legged mites. Two new fossil species, N. electrus new species and N. glaesus new species, are described from samples of Baltic amber, and remarks on their morphology and taphonomy are provided. The discovery is complemented with a discussion on morphological singularities (the shape of the prodorsum, the location of setae h1 and h2 in living specimens, and lengths of genual setae), an anomaly of hypertrophied seta (found in the N. glaesus holotype), and some biogeographical issues.UUID: http://zoobank.org/d1602384-ae4f-4f90-b4a1-6cdedd77c9e1


1978 ◽  
Vol 5 (3) ◽  
pp. 183-190 ◽  
Author(s):  
Anne LaBastille ◽  
Douglas J. Pool

Tropical New World cloud-forest may best be described as the area of persistent cloud contact with tropical mountain vegetation. Cloud-forest exists in at least five life-zones, being characterized, generally speaking, by having high precipitation and humidity, dripping moisture, continuous cloud or mist cover, absence of frost, and trees laden with mosses and epiphytes.


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