A new fossil plant of probable intermediate affinities (Trimerophyte–Progymnosperm)

1975 ◽  
Vol 53 (16) ◽  
pp. 1719-1728 ◽  
Author(s):  
Henry N. Andrews ◽  
Patricia G. Gensel ◽  
Andrew E. Kasper
Keyword(s):  
New Brunswick ◽  
Middle Devonian ◽  
New Genus ◽  
Second Order ◽  
Central Axis ◽  
New Genus And Species ◽  
Fossil Plant ◽  
Linear Distance

Oocampsa catheta, new genus and species, comes from the early Middle Devonian of New Brunswick about ½ mi west of Dalhousie Junction. The plant is known from a central axis with spirally arranged first-and second-order branches; the latter dichotomize some what irregularly to produce ultimate fertile branchlets, located at varied distances along the second-order axes, so that the terminal, erect sporangia occur over a linear distance rather than in dense terminal clusters. The sporangia are ovoid with pointed apices and contain spores that are trilete, zonate, and ornamented with cones and spines. The spores are compared with dispersed spores known as Samarisporites or Grandispora.

Adaptive function and phylogenetic significance of novel skeletal features of a new Devonian microconchid tubeworm (Tentaculita) from Wyoming, USA

2021 ◽  
pp. 1-15
Author(s):  
Michał Zatoń ◽  
Mingxi Hu ◽  
Mercedes di Pasquo ◽  
Paul M. Myrow
Keyword(s):  
Middle Devonian ◽  
New Genus ◽  
Adaptive Strategy ◽  
Phylogenetic Significance ◽  
New Genus And Species ◽  
Adaptive Function ◽  
Faunal Assemblage ◽  
Early Devonian ◽  
Narrow Channels ◽  
Algal Thalli

Abstract A new genus and species of microconchid tubeworm, Aculeiconchus sandbergi n. gen. n. sp., is described from the Givetian (Devonian) Maywood Formation of Cottonwood Canyon, Wyoming, USA. It possesses unique hollow spines of various lengths on the tube underside, a position previously undocumented for these fossils. Like some cyclostome bryozoans possessing basal tubular extensions, the basal spines of Aculeiconchus n. gen. were presumably also used for fixation to flexible substrata, e.g., algal thalli, which is a previously undocumented adaptive strategy in microconchids. Together with other skeletal features, such basal spines could suggest that ‘lophophorate’ microconchids, unlike the other tentaculitoids, might be phylogenetically not as distant from bryozoans as previously thought. The Maywood Formation, which contains a few-millimeters thick, monospecific shell accumulation of the microconchids described herein, records deposition in an estuarine brackish setting within narrow channels that were cut into underlying strata. The microconchids were opportunistic taxa that repeatedly colonized these salinity-stressed estuarine channels, leading to a series of adaptive innovations, including colonization of plant stems during the Early Devonian (Beartooth Butte Formation) and possibly flexible, soft-algal substrata during the Middle Devonian (Maywood Formation, this study). Tectonic quiescence during the Early and Middle Devonian indicates that erosion and subsequent deposition of the Maywood and the underlying Beartooth Butte Formation channels were responses to major eustatic events. Over a span of nearly 30 Myr, channels were cut successively during lowstand conditions and a distinctive faunal assemblage with microconchids tracked marine transgressions into the channels. UUID: http://zoobank.org/394c8b32-d5e7-411e-8e56-6fb9f55bbb8a

Gigantocharinus szatmaryi, a new trigonotarbid arachnid from the Late Devonian of North America (Chelicerata, Arachnida, Trigonotarbida)

2000 ◽  
Vol 74 (1) ◽  
pp. 25-31 ◽  
Author(s):  
William A. Shear
Keyword(s):  
North America ◽  
Middle Devonian ◽  
New Genus ◽  
Upper Devonian ◽  
Late Carboniferous ◽  
Late Devonian ◽  
New Genus And Species ◽  
Significant Time ◽  
The Family ◽  
Time Gap

A new trigonotarbid arachnid, Gigantocharinus szatmaryi new genus and species, is described from Upper Devonian (Late Famennian) sediments in Pennsylvania. Devonian trigonotarbids were known before from only a single North American locality and several European ones. The new trigonotarbid occurs in what had previously been a significant time gap between the faunas of the Middle Devonian and the late Carboniferous. Gigantocharinus szatmaryi is assigned with some hesitation to the family Palaeocharinidae.

Canadian Nymphomyiidae (Diptera)

1975 ◽  
Vol 53 (6) ◽  
pp. 853-866 ◽  
Author(s):  
D. Keith McE. Kevan ◽  
Felicity E. A. Cutten-Ali-Khan
Keyword(s):  
New Brunswick ◽  
New Genus ◽  
Systematic Position ◽  
Compound Eyes ◽  
New Genus And Species

A new genus and species, Oreadomyia albertae, is described from the mountains of western Alberta. This differs in several important adult characters from the three previously known genera and species of Nymphomyiidae, particularly in the possession of mouthparts (which are rather unlike those of other Diptera), in the form of the compound eyes, and in the virtually apterous condition. It is placed in a new subfamily, Oreadomyiinae. Further records of Palaeodipteron walkeri Ide are given for New Brunswick. These include examples of the previously unknown, fully alate adults. The systematic position of the Nymphomyioidea is briefly discussed. The group is retained in a separate suborder, Archaeodiptera. An appendix gives a list of arthropods trapped at the same site as O. albertae.

The new Devonian (Givetian) heteractinid sponge Gondekia from Ontario, Canada, and evolution of the astraeospongiids and eiffeliids

1991 ◽  
Vol 65 (1) ◽  
pp. 38-44 ◽  
Author(s):  
J. Keith Rigby
Keyword(s):  
Middle Devonian ◽  
New Genus ◽  
New Genus And Species ◽  
Thickened Wall

The new genus and species, Gondekia hastula, are described from the Middle Devonian (Givetian) Hungry Hollow Formation of southwestern Ontario. Astraeospongium lancifer Reimann, 1945, is also included in the new genus and A. acicularis is considered a synonym of that species. Gondekia has a flat saucer-like form and a felted, but thin, skeleton composed of at least three orders of regularly spaced and oriented simple sexiradiates. Gondekia is placed in the Eiffeliidae but is convergent toward the Astraeospongiidae in having a somewhat thickened wall.

A NEW GENUS AND SPECIES OF PHORID FLY FROM CANADA (DIPTERA: PHORIDAE)

1967 ◽  
Vol 99 (2) ◽  
pp. 221-223 ◽  
Author(s):  
Thomas Borgmeier
Keyword(s):  
New Brunswick ◽  
New Genus ◽  
New Genus And Species ◽  
Phorid Fly

AbstractCrinophleba rostrata, a new genus and species of a phorid fly from New Brunswick, Canada, is described.

Devonian cladid crinoids: Families Glossocrinidae Goldring, 1923, and Rutkowskicrinidae new family

2001 ◽  
Vol 75 (4) ◽  
pp. 783-807 ◽  
Author(s):  
George C. McIntosh
Keyword(s):  
Middle Devonian ◽  
Western Europe ◽  
New Genus ◽  
Type Specimen ◽  
New Combination ◽  
Late Devonian ◽  
New Genus And Species ◽  
Median Ridge ◽  
New Family ◽  
Anal Sac

The cladid crinoid order Poteriocrinida Jaekel, 1918 is a polyphyletic group that includes a variety of independent lineages united solely by the presence of ramulate or pinnulate arms. One of these lineages is the Rutkowskicrinidae new family herein assigned to the order Dendrocrinida, Bather 1899. Genera assigned to this new family include Rutkowskicrinus new genus, Decorocrinus new genus, Iteacrinus, Nassoviocrinus, Quantoxocrinus, Sacrinus, Sostronocrinus, ?Propoteriocrinus, and ?Schmidtocrinus. Members of this family are characterized by low conical cups with ridged thecal plates, U-shaped peneplenary radial facets bearing faint transverse ridges, a proximal median ridge on the posterior side of a long, narrow, predominantly straight anal sac, and pentagonal columns with one to two cirri per nodal. Arms in this family are highly variable, ranging from isotomous to heterotomous and pinnulate. The arms in the type specimen of Rutkowskicrinus patriciae n. sp. preserve all these various arm stages. The oldest presently known rutkowskicrinids occur in the Late Silurian (Ludlovian) of Australia and the Early Devonian (Pragian) of western Europe. The family diversified during the Middle Devonian (Givetian) in northeastern North America, and declined in numbers and diversity throughout the Late Devonian before going extinct in the Early Mississippian (Tournaisian).The Glossocrinidae Goldring, 1923, containing Glossocrinus, Charientocrinus, Catactocrinus, and Liparocrinus, is also reviewed. This family, distinguished by a strongly recumbent anal sac in the B-E plane and a prominent median ridge extending the entire length of the anal sac, was derived from the Rutkowskicrinidae during the Middle Devonian (Givetian) and diversified in the Late Devonian before going extinct at the Frasnian-Famennian boundary.The previously described rutkowskicrinid and glossocrinid genera listed above were assigned by Moore et al. (1978) to the dendrocrinid family Mastigocrinidae and poteriocrinid families Rhenocrinidae, Poteriocrinitidae, and Scytalocrinidae. Studied taxa include Rutkowskicrinus patriciae new genus and species, Rutkowskicrinus collieri new genus and species, Nassoviocrinus costatus (Goldring, 1954) new combination, Nassoviocrinus schultzei (Haarmann, 1921) new combination, Nassoviocrinus? duluki (Kesling, 1969) new combination, Nassoviocrinus? ornatus (Goldring, 1954) new combination, Nassoviocrinus? chilmanae new species, Decorocrinus arkonensis (Goldring, 1950) new combination, Decorocrinus cooperi (Goldring, 1926) new combination, Quantoxocrinus clarkei (Williams, 1882) new combination, Glossocrinus halli (Goldring, 1923) new combination, and Charientocrinus bellitubatus (Kesling, 1973) new combination.

New chonostrophiid brachiopods from the Famennian (Late Devonian) of the Santanghu Basin, Xinjiang, northwest China

2002 ◽  
Vol 76 (2) ◽  
pp. 229-238
Author(s):  
Zhong-Qiang Chen ◽  
Neil W. Archbold
Keyword(s):  
Middle Devonian ◽  
New Genus ◽  
Early Carboniferous ◽  
Northwest China ◽  
Late Devonian ◽  
New Genera ◽  
New Genus And Species ◽  
Early Devonian ◽  
Median Septum ◽  
Devonian Age

Two new genera of the Chonostrophiidae are proposed herein to accommodate the resupinate shells from the Famennian sediments of the Late Devonian in the Santanghu Basin of the Balikun area, Xinjiang Province, northwestern China. Santanghuia santanghuensis new genus and species is distinguishable from other chonostrophiids by the possession of a pair of long dorsal anderidia and absence of a dorsal median septum. Balikunochonetes liaoi new genus and species is distinct because of the presence of a pair of anderidia with secondary anderidia, and a dorsal median septum. Santanghuia new genus is considered to be phylogenetically related to Chonostrophia of late Early to Middle Devonian age, while Balikunochonetes has possibly given rise to Chonostrophiella of Early Devonian age and is a likely ancestor of Tulcumbella of Early Carboniferous age.

Morphology, systematics, and evolution of Middle Devonian Ambocoeliidae (Brachiopoda), western New York

1990 ◽  
Vol 64 (1) ◽  
pp. 79-99 ◽  
Author(s):  
Daniel Goldman ◽  
Charles E. Mitchell
Keyword(s):  
New York ◽  
Middle Devonian ◽  
Type Species ◽  
New Genus ◽  
New Genus And Species ◽  
Median Septum ◽  
Internal Morphology ◽  
Apical Plate ◽  
Hamilton Group ◽  
Shape And Size

The internal morphology of ambocoeliid brachiopods from the Middle Devonian Hamilton Group of western New York indicates a need for several taxonomic revisions. “Ambocoelia” praeumbona is transferred to Emanuella. “Ambocoelia” spinosa and “A.” nana represent Crurispina n. gen. Specimens of species belonging to Crurispina have moderately well developed crural plates, and, accordingly, they are assigned to the subfamily Rhynchospiriferinae. Crural plates are small and obscure but clearly present in Ambocoelia umbonata, the type species of Ambocoelia. Thus, the diagnosis of the subfamily Ambocoeliinae is emended to include species with tiny crural plates.Ambocoeliid specimens from the Levanna Shale Member of the Skaneateles Formation, formerly referred to Echinocoelia, reveal several elaborate features in the pedicle valve, including an apical plate and a hollow tube supported by a median septum. These specimens represent a new genus and species, Mucroclipeus eliei. The homeomorphy found in the shape and size of these ambocoeliids may be the result of paedomorphosis. Additionally, their pattern of occurrence and minute size suggest that they attained their paedomorphic state through progenesis. The taxa Ambocoelia tuberculata n. sp., Crurispina n. gen., and Mucroclipeus eliei n. gen. and sp. are established.

scholarly journals The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada – a review of previously described taxa and a description of a new genus and species

Fossil Record ◽  
2017 ◽  
Vol 20 (1) ◽  
pp. 47-67 ◽  
Author(s):  
Kathryn E. Mickle
Keyword(s):  
New Brunswick ◽  
New Genus ◽  
New Genus And Species ◽  
Type Specimens ◽  
Lower Carboniferous ◽  
Taxonomic History ◽  
Dorsal Ridge ◽  
History Of ◽  
Shale Formation ◽  
Being Moved

Abstract. The Lower Carboniferous Albert shale formation of New Brunswick, Canada, is well-known for the preservation of countless articulated lower actinopterygian palaeoniscoid fishes. This site is at the boundary between the Devonian and the Lower Carboniferous, making the lower actinopterygians preserved at this site important. The taxonomic history of previously described Albert shale formation actinopterygians is reviewed here. Many of the earliest described actinopterygian taxa from the Albert Formation are represented by poorly preserved type specimens and have the distinction of being moved from one paraphyletic genus to another paraphyletic genus. While these taxa are in need of major redescriptions, such work is premature until the large paraphyletic or polyphyletic genera they have been placed in, Palaeonicus[m], †Rhadinichthys, and †Elonichthys, are redescribed. But there is new diversity within the Albert shale formation. Here, a new lower actinopterygian species, †Lambeia pectinatus, is described from one well-preserved specimen. This new species is characterized by dorsal ridge scales with pectinated posterior margins, body scales inserted between adjacent dorsal ridge scales, body scales with pectinated posterior and ventral margins, the presence of a ventral rostro-premaxilla and a median rostral bone, a separate and distinct antorbital bone, and a single supraorbital bone. This newly described species is distinct from previously described fishes from the Albert Formation, and the morphology of this newly described species is more similar to later Carboniferous fishes rather than Devonian fishes. This suggests that morphological features commonly seen in Carboniferous fishes and rarely seen in Devonian fishes were present early in the Carboniferous.

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