scholarly journals A boring foraminiferan from the Upper Jurassic of England and Northern France

1993 ◽  
Vol 12 (1) ◽  
pp. 83-89 ◽  
Author(s):  
C. R. Plewes ◽  
T. J. Palmer ◽  
J. R. Haynes
Keyword(s):  
New Genus ◽  
Substrate Surface ◽  
Upper Jurassic ◽  
New Genus And Species ◽  
Southern England ◽  
Northern France

Abstract. Small rosette borings, consisting of an excavated pit from which is subtended a system of branching galleries, are common in carbonate skeletal substrates in the Upper Jurassic Oxford Clay (Callovian-Oxfordian) and Kimmeridge Clay (Kimmeridgian) of southern England and northern France. The opening of the pit onto the substrate surface is surrounded by an agglutinated collar, which suggests that they may be the work of Foraminifera. The new genus and species, Globodendrina monile, are erected to accommodate them. Other examples of boring in the Foraminiferida are reviewed. It is proposed that other similar rosette boring ichnogenera may also be the work of foraminiferans.

The second species of the cnemidolestid genus Piesbergopterum from the Upper Carboniferous of Avion, Northern France (Archaeorthoptera: Cnemidolestidae)

2021 ◽  
Vol 4 (4) ◽  
Author(s):  
ANDRÉ NEL ◽  
PATRICK ROQUES
Keyword(s):  
New Genus ◽  
New Genus And Species ◽  
Upper Carboniferous ◽  
Northern France ◽  
The Family ◽  
Triangular Area

The Palaeozoic archaeorthopteran order Cnemidolestodea Handlirsch, 1937 (sensu Béthoux, 2005; not sensu Aristov, 2014) currently comprises only the family Cnemidolestidae Handlirsch, 1906. They are easily characterized by the presence of a more or less triangular area delimited by the vein MA and the first anterior fork of MP+CuA+CuPa, this last vein having several parallel posterior branches. Dvořák et al. (2021) listed the included genera, and described the new genus and species Piesbergopterum punctatum from the Moscovian of Piesberg (Germany), characterized by the presence of a pattern of rounded spots in numerous cells all over the forewings. Nel & Poschmann (in press) noticed that the Cnemidolestidae show an important diversity of patterns of coloration on their forewings, possibly related to cryptic behaviors in the vegetation.

Glabrimycetoporus amoenus, a new tachyporine genus and species of Mesozoic Staphylinidae (Coleoptera) from Liaoning, China

Zootaxa ◽  
2009 ◽  
Vol 2225 (1) ◽  
pp. 63-68 ◽  
Author(s):  
YANLI YUE ◽  
YUNYUN ZHAO ◽  
DONG REN
Keyword(s):  
Lower Cretaceous ◽  
New Genus ◽  
Abdominal Tergite ◽  
Upper Jurassic ◽  
Yixian Formation ◽  
Liaoning Province ◽  
New Genus And Species ◽  
Ne China

A new genus and species of well-preserved fossil Staphylinidae is described and illustrated. Glabrimycetoporus amoenus Yue, Zhao & Ren, gen. et sp. nov. is assigned to the tribe Mycetoporini in the subfamily Tachyporinae based on the following characters: head more or less inserted into prothorox, the tenth abdominal tergite broad and oblong; antennal insertions exposed and located anterior to a line drawn between anterior edges of eyes; body strongly tapered to the narrow head and abdominal apex. The specimen was discovered in the Upper Jurassic–Lower Cretaceous Yixian Formation of Beipiao City, Liaoning Province, NE China.

A new Unionoidea (Mollusca, Bivalvia) from the Tacuarembó Formation (Upper Triassic–Upper Jurassic), Uruguay

1993 ◽  
Vol 67 (6) ◽  
pp. 962-965 ◽  
Author(s):  
Sergio Martinez ◽  
Alfredo Figueiras ◽  
Jorge S. da Silva
Keyword(s):  
New Genus ◽  
Upper Jurassic ◽  
Upper Triassic ◽  
New Genus And Species ◽  
Large Size

A new genus and species of Unionoidea, Tacuaremboia caorsii, are described from the Tacuarembó Formation (Upper Triassic–Upper Jurassic) of Uruguay. The genus is distinguished from other Unionoidea by its large size, thickness, edentulous hingeline, and the presence of claustra. It has some similarities with the Anodontinae and the Archanodontacea, but it cannot be assigned to any of the known family units.

An asteroid (Echinodermata) faunule from the Oxfordian Swift Formation (Upper Jurassic) of Montana

2016 ◽  
Vol 90 (6) ◽  
pp. 1160-1168
Author(s):  
Daniel B. Blake ◽  
Thomas E. Guensburg
Keyword(s):  
New Genus ◽  
Upper Jurassic ◽  
Wide Distribution ◽  
Time Interval ◽  
New Genus And Species ◽  
The North ◽  
Class Level ◽  
Regional Location ◽  
Favorable Conditions ◽  
Continental Interior

AbstractA new Late Jurassic (Oxfordian) asteroid (Echinodermata) faunule from the Swift Formation of Montana includes representatives of four genera including the new genus and speciesAtalopegaster gundersoni(Stichasteridae),Eokainastersp. indet. (Astropectinidae), an indeterminate probable member of the Goniasteridae, and a species indeterminate beyond the class level. Because of weathering at the outcrop, preservation is poor.Although representing an unusual depositional occurrence, overall faunule composition appears comparable to that found in a similar modern environment. The faunule is comparable in age and regional location to earlier Jurassic asteroid discoveries, suggesting wide distribution during a geologically brief time interval of favorable conditions. Asteroids are only rarely reported from the Mesozoic of the North American continental interior, and co-occurrence of multiple fossil taxa is unusual on a global basis.

A new rhamphorhynchid (Pterosauria: Rhamphorhynchidae) from the Middle/Upper Jurassic of Qinglong, Hebei Province, China

Zootaxa ◽  
2012 ◽  
Vol 3158 (1) ◽  
pp. 1 ◽  
Author(s):  
JUNCHANG LÜ ◽  
DAVID M. UNWIN ◽  
BO ZHAO ◽  
CHUNLING GAO ◽  
CAIZHI SHEN
Keyword(s):  
Late Jurassic ◽  
New Genus ◽  
Upper Jurassic ◽  
Hebei Province ◽  
New Taxon ◽  
New Genus And Species ◽  
Skeletal Morphology ◽  
Unique Character ◽  
Distal Process ◽  
Nasal Process

A heavily compressed, but nearly complete fossil skeleton recovered from the Middle/Upper Jurassic Tiaojishan Forma-tion of Mutoudeng, Qinglong County, Hebei Province, China, represents a new genus and species of long-tailed pterosaur,Qinglongopterus guoi gen. et sp. nov. The holotype and only known specimen has an estimated forelimb length of 0.18m. The new taxon is distinguished by a relatively short skull, a remarkably short pteroid with a distinctive knob-like distalexpansion, and a prepubis with a relatively slender distal process. Phylogenetic analysis demonstrates that Qinglongopter-us is a member of Rhamphorhynchidae, exhibiting many of the unique character states found in members of this clade.Qinglongopterus is strikingly similar to Rhamphorhynchus and more closely related to this taxon than to any other rham-phorhynchine, this pairing is supported by morphometric data and several synapomorphies (short, broad nasal process ofthe maxilla; forelimb length more than four times that of the hind limb; wing-phalanx one more than twice the length ofthe tibia). Qinglongopterus demonstrates that the highly derived skeletal morphology of Rhamphorhynchus, known onlyfrom the latest Jurassic (Tithonian) of Europe, had already appeared by the start of the Late Jurassic. This hints at evolu-tionary stasis in Rhamphorhynchinae, a phenomenon seemingly also present in two other clades of basal pterosaurs,Anurognathidae and Scaphognathinae, and contrasting sharply with basal monofenestratans which appear to have undergone extensive evolutionary change during the same interval.

A North American freshwater sponge (Eospongilla morrisonensis new genus and species) from the Morrison Formation (Upper Jurassic), Colorado

1999 ◽  
Vol 73 (3) ◽  
pp. 389-393 ◽  
Author(s):  
Stan P. Dunagan
Keyword(s):  
North American ◽  
New Genus ◽  
Upper Jurassic ◽  
Morrison Formation ◽  
Freshwater Sponge ◽  
New Genus And Species ◽  
East Central ◽  
North American Freshwater ◽  
Lacustrine Carbonate

Eospongilla morrisonensis n. gen. and sp., the oldest-described freshwater sponge (Demospongea: Spongillidae), is found in the Upper Jurassic (?Oxfordian/Kimmeridgian to Tithonian) Morrison Formation, east-central Colorado, U.S.A. Eospongilla morrisonensis occurs within the well-developed lacustrine carbonate succession of the Morrison Formation, and is represented by two micritic body fossils with calcite-replaced megascleres that range in length from 180 to 300 μm and in diameter from 20 to 35 μm. Megascleres are simple oxeas and strongyles and lack apparent ornamentation, possibly due to the diagenetic replacement. The oxeas are straight but the strongyles display a slight curvature. Microscleres are absent; gemmoscleres were not observed.

The description and phenetic relationships of a new Ichthyosaur genus from the Upper Jurassic of England

1976 ◽  
Vol 13 (5) ◽  
pp. 668-683 ◽  
Author(s):  
C. McGowan
Keyword(s):  
New Genus ◽  
Middle Triassic ◽  
Upper Jurassic ◽  
Evolutionary Trends ◽  
Phenetic Analysis ◽  
New Genus And Species ◽  
The North ◽  
Phenetic Relationships ◽  
Principal Coordinates ◽  
Temporal Sequences

A large and previously unknown ichthyosaur is reported from the Kimmeridge Clay (Upper Jurassic) of Stowbridge, Norfolk, England. The only valid genera described from the Upper and Middle Jurassic are considered to be Ophthalmosaurus Seeley and Nannopterygius von Huene, and since the Stowbridge specimen is distinct from these, a new genus and species, Grendelius mordax gen. et sp. nov., are erected. Using cluster and principal coordinates analyses, G. mordax was found to have closest phenetic affinities with Platypterygius americanus (Nace) of the North American Cretaceous, and with an undescribed ichthyosaur from the Middle Triassic of Switzerland, and least phenetic affinity with Ophthalmosaurus discus (Marsh).The phenetic analysis also revealed that the division of the Ichthyosauria into latipinnates and longipinnates is questionable. Stenopterygius quadriscissus (Quenstedt), long considered a longipinnate, is herein shown to have closer phenetic affinity with latipinnate ichthyosaurs. The close phenetic affinity between the skulls of P. americanus and the undescribed Swiss ichthyosaur is inconsistent with currently held views of cranial evolution in ichthyosaurs, and points to the shortcomings of tracing evolutionary trends in temporal sequences of fossils.

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