Lecidea rubrocastanea, a new lichen species from conifer bark and wood in interior western North America (Lecanorales, lichenized ascomycetes)

2007 ◽  
Vol 39 (4) ◽  
pp. 339-347 ◽  
Author(s):  
Toby SPRIBILLE ◽  
Christian PRINTZEN
Keyword(s):  
British Columbia ◽  
North America ◽  
Morphological Traits ◽  
Washington State ◽  
Lichen Species ◽  
Western North America ◽  
Lichenized Ascomycetes ◽  
Lichen Substances ◽  
Thin Walled

Abstract:Lecidea rubrocastanea T. Sprib. & Printzen is described as new from conifer bark and wood in montane valleys of inland British Columbia, Idaho, Montana, Oregon and Washington State. It is characterized by its combination of a crustose olivaceous thallus lacking secondary lichen substances, small, dark burgundy-red or maroon apothecia, dark-capped paraphyses, Lecidella-type ascus, small, thin-walled ascospores, and bacilliform conidia. The generic affinities of the species based on analysis of ITS DNA are unclear, but it has numerous morphological traits in common with Japewia.

Early Eocene (Ypresian) birds from the Okanagan Highlands, British Columbia (Canada) and Washington State (USA)

2019 ◽  
Vol 56 (8) ◽  
pp. 803-813
Author(s):  
Gerald Mayr ◽  
S. Bruce Archibald ◽  
Gary W. Kaiser ◽  
Rolf W. Mathewes
Keyword(s):  
British Columbia ◽  
North America ◽  
Fossil Record ◽  
Washington State ◽  
Fossil Birds ◽  
Early Eocene ◽  
Western North America ◽  
Postcranial Skeleton ◽  
The North ◽  
Okanagan Highlands

We survey the known avian fossils from Ypresian (early Eocene) fossil sites of the North American Okanagan Highlands, mainly in British Columbia (Canada). All specimens represent taxa that were previously unknown from the Eocene of far-western North America. Wings from the McAbee site are tentatively referred to the Gaviiformes and would constitute the earliest fossil record of this group of birds. A postcranial skeleton from Driftwood Canyon is tentatively assigned to the Songziidae, a taxon originally established for fossils from the Ypresian of China. Two skeletons from Driftwood Canyon and the McAbee site are tentatively referred to Coliiformes and Zygodactylidae, respectively, whereas three further fossils from McAbee, Blakeburn, and Republic (Washington, USA) are too poorly preserved for even a tentative assignment. The specimens from the Okanagan Highlands inhabited relatively high paleoaltitudes with microthermal climates (except Quilchena: lower mesothermal) and mild winters, whereas most other Ypresian fossil birds are from much warmer lowland paleoenvironments with upper mesothermal to megathermal climates. The putative occurrence of a gaviiform bird is particularly noteworthy because diving birds are unknown from other lacustrine Ypresian fossil sites of the Northern Hemisphere. The bones of the putative zygodactylid show a sulphurous colouration, and we hypothesize that this highly unusual preservation may be due to the metabolic activity of sulphide-oxidizing bacteria.

Cascadiacarpa exilis sp. nov.: new fruits of Fagaceae from the Eocene of British Columbia

Botany ◽  
2014 ◽  
Vol 92 (5) ◽  
pp. 377-387 ◽  
Author(s):  
Randal A. Mindell ◽  
Ruth A. Stockey ◽  
Graham Beard
Keyword(s):  
British Columbia ◽  
North America ◽  
Cellulose Acetate ◽  
Transverse Section ◽  
Vancouver Island ◽  
Washington State ◽  
Western North America ◽  
Single Seed ◽  
Fossil Genus ◽  
Shape And Size

More than 800 permineralized fagaceous fruits have been studied from the Eocene Appian Way locality of Vancouver Island, British Columbia. These cupulate nuts are the most common fruits preserved at the locality. They occur in calcareous concretions and were studied using the cellulose acetate peel technique. Cupules are borne on a spiny stalk and are broadly ovate in both longitudinal and transverse section. Cupules are evalvate and have both branching and simple spines. A single, ovoid, sclerotic nut is enclosed entirely by the cupule, except at the apex, where a stylar protrusion is free from any surrounding tissues. The nut is bilocular with a glabrous endocarp lining. At maturity, a single seed occupies the locular cavity. The embryo is straight and no endosperm is evident. The single-fruited, spiny cupule is most similar to fruits of Fagaceae subfamily Castaneoideae. Bicarpellate fruits and a glabrous endocarp place them within the fossil genus Cascadiacarpa; however, they differ from Cascadiacarpa spinosa in nut wall anatomy, cupule ornamentation, shape, and size. Fruits of Cascadiacarpa exilis sp. nov. are compared with spiny, small compression and impression fossil fruits from the Eocene Taneum Creek locality of Washington State. The characters of the Washington State fossils overlap with those observed in the anatomically preserved Appian Way cupulate fruits and, as such, may represent compression and impression fossils of the same genus. The permineralized fruits document that evalvate, spiny, cupulate nuts of Fagaceae were present and common in the Eocene of western North America.

Schaereria dolodes (Nyl. ex Hasse) Schmull & T. Sprib.: a second corticolous species in the genus

2005 ◽  
Vol 37 (6) ◽  
pp. 527-533 ◽  
Author(s):  
Michaela SCHMULL ◽  
Toby SPRIBILLE
Keyword(s):  
British Columbia ◽  
North America ◽  
Lichen Species ◽  
Western North America ◽  
Epiphytic Lichen

Schaereria dolodes (Nyl. ex Hasse) Schmull & T. Sprib. comb. nov., an epiphytic lichen species known from western North America was originally described as a member of the genus Lecidea sensu lato. However, its morphology is very characteristic of the genus Schaereria Körb. Here, we lectotypify the species and propose its placement in the latter genus. It is also reported as new to Canada from British Columbia.

Phaeocollybia in western North America. I. ThePhaeocollybia kauffmanii complex

2000 ◽  
Vol 78 (8) ◽  
pp. 1055-1076 ◽  
Author(s):  
Lorelei L Norvell
Keyword(s):  
British Columbia ◽  
New Species ◽  
North America ◽  
Morphological Characters ◽  
Western North America ◽  
Temperate Rainforest ◽  
Emended Description ◽  
Thin Walled

Morphological and molecular investigations during a taxonomic reevaluation of the genus Phaeocollybia revealed four new agaric species from British Columbia, Washington, Oregon, and California that are morphologically similar to Phaeocollybia kauffmanii (Smith) Singer. All five species produce large basidiomes with brown pilei, stipes with cartilaginous rinds surrounding dense pith, vertical-monopodial pseudorhizae, large, verrucose or verruculose, apically beaked basidiospores, and thin-walled, clavate cheilocystidia. The most salient morphological characters distinguishing the new species from P. kauffmanii include abundant clamp connections (Phaeocollybia ammiratii), a pink- or purple-brown pileus lacking encrusting pigments in the pileipellis (Phaeocollybia benzokauffmanii), a nonviscid, fibrillose, ochraceous pileus with a trilaminate pileipellis (Phaeocollybia luteosquamulosa), and unusually large basidiospores and subglobose subcapitate pedicellate cheilocystidia (Phaeocollybia redheadii). An emended description of P. kauffmanii accompanies technical descriptions and a key to the five species and newly revealed complex.Key words: Agaricales, Basidiomycota, Cortinariaceae, RFLPs, temperate rainforest.

Japewia Subaurifera, A New Lichen Genus and Species From North-West Europe and Western North America

1990 ◽  
Vol 22 (3) ◽  
pp. 205-212 ◽  
Author(s):  
T. Tønsberg
Keyword(s):  
British Columbia ◽  
North America ◽  
Western North America ◽  
Coniferous Trees ◽  
North West

AbstractThe genus Japewia Tønsb. is introduced to accommodate three species including J. subaurifera Muhr & Tønsb. sp. nov. based on material from Norway, Sweden, Finland, Scotland, Canada (British Columbia) and U.S.A. (Washington). This species is closely related to Lecidea tornoensis Nyl. but is distinguished in being sorediate and by the production of lobaric acid (accessory) and acetone-soluble pigments. It grows on bark of deciduous and coniferous trees. Lecidea carrollii Coppins & P. James and L. tornoensis Nyl. are transferred to Japewia.

The Lower Jurassic phosphorites of southeastern British Columbia and terrane accretion to western North America

1989 ◽  
Vol 26 (8) ◽  
pp. 1612-1616 ◽  
Author(s):  
T. P. Poulton ◽  
J. D. Aitken
Keyword(s):  
British Columbia ◽  
North America ◽  
Oceanic Crust ◽  
West Coast ◽  
Cold Water ◽  
Lower Jurassic ◽  
Depositional Model ◽  
Western North America ◽  
The West ◽  
Terrane Accretion

Sinemurian phosphorites in southeastern British Columbia and southwestern Alberta conform with the "West Coast type" phosphorite depositional model. The model indicates that they were deposited on or near the Early Jurassic western cratonic margin, next to a sea or trough from which cold water upwelled. This suggests that the allochthonous terrane Quesnellia lay well offshore in Sinemurian time. The sea separating Quesnellia from North America was partly floored by oceanic crust ("Eastern Terrane") and partly by a thick sequence of rifted, continental terrace wedge rocks comprising the Purcell Supergroup and overlying Paleozoic sequence. This sequence must have been depressed sufficiently that access of upwelling deep currents to the phosphorite depositional area was not impeded.

Atropellis piniphila. [Distribution map].

1981 ◽  
Author(s):  
Keyword(s):  
British Columbia ◽  
New Mexico ◽  
North America ◽  
South Dakota ◽  
Geographical Distribution ◽  
Washington State ◽  
Distribution Map ◽  
New Distribution

Abstract A new distribution map is provided for Atropellis piniphila (Weir) Lohman & Cash. Hosts: Pine (Pinus). Information is given on the geographical distribution in NORTH AMERICA, Canada (Alberta, British Columbia, Saskatchewan), USA (Alabama, Arizona, Montana, New Mexico, Oregon, South Dakota, Washington State), (Idaho).

NEW NEARCTIC CRANE-FLIES (TIPULIDAE, DIPTERA), PART XIX

1943 ◽  
Vol 75 (8) ◽  
pp. 139-145 ◽  
Author(s):  
Charles P. Alexander
Keyword(s):  
British Columbia ◽  
North America ◽  
Type Material ◽  
Western North America ◽  
Crane Flies ◽  
The Individual

The crane-flies considered herewith are all from Western North America, from British Columbia to California. The names of the collectors and the location of the type material are indicated at the end of the individual specific accounts; where not stated to the contrary, such types are preserved in my own collection of these flies.

scholarly journals A new milliped of the genus Stenozonium Shelley 1998 from Washington State, U. S. A.: first record of the genus and family from North of the Columbia River (Polyzoniida: Polyzoniidae)

Zootaxa ◽  
2005 ◽  
Vol 1017 (1) ◽  
pp. 25
Author(s):  
ROWLAND M. SHELLEY ◽  
WILLIAM A. SHEAR
Keyword(s):  
New Species ◽  
North America ◽  
Columbia River ◽  
First Record ◽  
Washington State ◽  
Western North America ◽  
Olympic Peninsula

The new species, Stenozonium leonardi, the northernmost representative of the Polyzoniidae in western North America and the only one north of the Columbia River, is described from the Olympic Peninsula of Washington; it is isolated by some 180 mi (288 km) from S. benedictae Shelley, 1998, in coastal Oregon. Stenozonium alone among the four polyzoniidan genera in western North America consists of entirely allopatric and widely separated species, with one apiece in California, Oregon, and Washington-evidence that it diversified earlier than its ordinal counterparts.

A New Gunnel, Pholis clemensi, from the Coast of Western North America

1964 ◽  
Vol 21 (5) ◽  
pp. 933-939 ◽  
Author(s):  
Richard H. Rosenblatt
Keyword(s):  
British Columbia ◽  
New Species ◽  
North America ◽  
North American ◽  
North American Species ◽  
Western North America ◽  
The North ◽  
The Family ◽  
Juan De Fuca ◽  
A New Species

A new species, Pholis clemensi, referred to the family Pholidae, is named and described from 12 specimens taken in southern British Columbia waters and the Strait of Juan de Fuca. Pholis clemensi is compared with other members of the genus, and a key is given to the North American species.

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