An Early Late Cretaceous Dinosaur Tracksite in Central Yukon Territory,Canada

Dinosaur tracks were first reported from the coal-bearing clastic sequences of the Ross River Block in 1999 by members of a University of Alaska Museum field party, and track sites were confirmed by a joint Alaska-Yukon team in 2000. This fault-bounded sedimentary block is 3 kilometers west of Ross River, in the Yukon Territory. The discovery was followed by two years of field mapping and collection. This research has resulted in the documentation of 251 individual tracks at two separate but stratigraphically related sites, as well as a short (four-footprint) trackway at one of the sites. Six ichnogenera were identified. Ornithomimipus, Amblydactylus, and Gypsichnites were recognized at one site. At a stratigraphically higher site, four ichnogenera were documented including Tetrapodosaurus, Irenesauripus, Amblydactylus, and Columbosauripus. This ichno-assemblage is compared with those of Aptian to Cenomanian age from Alberta, British Columbia, and Alaska.

The discovery of unequivocal dinosaur evidence in a small structural inlier in the Tintina Trench that was previously assumed to be Eocene in age resulted in a restudy of the palynology and biostratigraphy of this coal-bearing sequence and the recent assignment of a middle Albian to early Cenomanian age to the upper part of the dinosaur-bearing interval.     

Blastomycosis: Report of the first case from Alberta,Canada

The first known case of laboratory confirmed blastomycosis in Alberta occurred in 1970. The patient, who is believed never to have left Alberta, presented with of headaches, sore neck and impaired intellect. Initially, tuberculous or cryptococcal meningitis was suspected, but laboratory findings did not support the diagnosis. A fungus resembling Blastomyces dermatitidis was isolated from the venticular cerebrospinal fluid and lung at autopsy. A few yeast cells suggestive of B. dermatitidis were seen in lung and brain tissue sections. Initial attempts at in vitro conversion of the mycelial form of the isolate into yeast form on several enriched media were unsuccessful. The fungus gave ± to ++ reactions with B. dermatitidis specific conjugate by the direct fluorescent antibody technique, it was not pathogenic for mice and guinea pigs, and no asexual spores were produced in slide cultures. Further investigation indicated that the mycelial form of the fungus converted into its yeast form when an actively growing inoculum was used, although the yeast cells varied considerably in size. The yeast form produced disseminated infection in mice within 10 days. Exoantigenic analysis demonstrated an A antigen specific for B. dermatitidis, which revealed the identity of this organism as an atypical strain of B. dermatitidis.

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Zusammenfassung Der erste Fall in Blastomycosis von einem Laboratorium wurde 1970 in Alberta bestätigt. Der Patient — der wahrscheinlich Alberta nie verlassen hat — klagte über Kopfschmerzen, Genickschmerzen und zeigte beeinträchtigte Verstand. Anfänglich wurde TBC — oder cryptococcal meningitis vermutet, laborfunde unterstutzten jedoch nicht die Diagnose. Ein Fungus — ahnlich zum Blastomyces dermatitidis wurde von venticular cerebrospinal Flüssigkeit und von der Lunge nach der Autopsie isoliert. Wenige Hefezellen hinweisend auf B. dermatitidis wurden gewebschnitten von Lunge und Gehirn festgestellt. Anfängliche Versuche die isolierten mycel Form in die Hefe Form in vitro mit Hilfe verschiedener angereicherter Nahrboden was erfolglos. Der Fungus ergab in der Direct Fluorescent Antibody Technik. ± zu ++ Reaktion mit dem B. dermatitidis specifische Konjugate; es war nicht pathogen fur Mause und Meerschweinchen, asexual Sporen wurden in der objecttrage Kultur produziert. Weitere Untersuchungen zeigten, dass sich die mycel Form des Fungus in die Hefeform umwandelte wenn ein gut wachsendes Inoculum gebraucht wurde. Die Hefezellen zeigten jedoch beträchtliche Grossenunterschiede. Die Hefeform verursachte in Mauseneine generallisierte Infektion in inerhalb von 10 Tagen. Exoantigenik Analyse zeigte ein A Antigen, specifisch für B. dermatitidis, welches die Identität des Organismus als atypischen Stamm des B. dermatitidis aufwies.

     

Paleoparasitological records in a canid coprolite from Patagonia, Argentina

In this note, organic remains identified as a canid coprolite were examined. The material was dated at 6540 +/- 110 B.P.; it was collected in the Perito Moreno National Park, Santa Cruz, Argentina. Paleoparasitological analysis was performed following standard procedures. Coprolite fragments were rehydrated in a trisodium phosphate aqueous solution and subjected to spontaneous sedimentation for microscope analysis. Eggs of nematodes identified as Trichuris sp., Capillaria sp., Uncinaria sp., and an ascaridid (probably Toxascaris sp.) or spirurids (presumably Physaloptera sp.), plus a cestode (Anoplocephalidae), presumably Moniezia sp., were found.     

The Late Cretaceous bivalveDidymotis Gerhardt, 1897 from Sergipe,Brazil

PalZ - The geographically widespread Upper Cretaceous bivalve genusDidymotis Gerhardt, 1897 has a short stratigraphie ränge, from the upper Turonian to the lowermost Coniacian. Three acme...     

Soft tissue and cellular preservation in vertebrate skeletal elements from the Cretaceous to the present

Soft tissues and cell-like microstructures derived from skeletal elements of a well-preserved Tyrannosaurus rex (MOR 1125) were represented by four components in fragments of demineralized cortical and/or medullary bone: flexible and fibrous bone matrix; transparent, hollow and pliable blood vessels; intravascular material, including in some cases, structures morphologically reminiscent of vertebrate red blood cells; and osteocytes with intracellular contents and flexible filipodia. The present study attempts to trace the occurrence of these four components in bone from specimens spanning multiple geological time periods and varied depositional environments. At least three of the four components persist in some skeletal elements of specimens dating to the Campanian. Fibrous bone matrix is more altered over time in morphology and less likely to persist than vessels and/or osteocytes. Vessels vary greatly in preservation, even within the same specimen, with some regions retaining pliability and other regions almost crystalline. Osteocytes also vary, with some retaining long filipodia and transparency, while others present with short and stubby filipodia and deeply pigmented nuclei, or are pigmented throughout with no nucleus visible. Alternative hypotheses are considered to explain the origin/source of observed materials. Finally, a two-part mechanism, involving first cross-linking of molecular components and subsequent mineralization, is proposed to explain the surprising presence of still-soft elements in fossil bone. These results suggest that present models of fossilization processes may be incomplete and that soft tissue elements may be more commonly preserved, even in older specimens, than previously thought. Additionally, in many cases, osteocytes with defined nuclei are preserved, and may represent an important source for informative molecular data.     

A new favreine coprolite (Crustacea,Decapoda) from the Jurassic of Iran and the Cretaceous of the Dinarids,Jugoslavia

Favreina tabasensis n. sp., a Crustacean (Decapoda) coprolite with numerous longitudinal canals is described from the Upper Jurassic of the Tabas area, east-central Iran. The same favreine form-species is also recorded and figured from the Neocomian of the Dinarids, Bata, Montenegro, Jugoslavia. Further, a lectotype is proposed forFavreina prusensis (Paréjas) from the Upper Portlandian of the region of Lake Apolyont, Turkey.Favreina montana Elliott from the Albian Qamchuqa formation, Gund-i-Shikavt, Erbil Liwa, northern Iraq, is considered as a nomen dubium non conservandum.     

Reconstruction of Late Cretaceous coastal paleotemperature from halite deposits of the Late Cretaceous Nongbok Formation (Khorat Plateau,Laos)

Cretaceous evaporites of the Maha Sarakhan Formation in Thailand (e.g., the Nongbok Formation, Laos) have been studied for almost a century as the huge potash deposits in the world. The consistently high local paleotemperatures should lead to huge salt deposits during the evaporation process. Primary fluid inclusions in halite can provide surface brine water temperatures directly and quantitatively. Until now, there have been no data published from paleotemperature of primary fluid inclusions of Cretaceous halite. The non-marine halite from the Cretaceous Nongbok Formation (Laos) precipitated from shallow brine waters with temperatures of 17.7–42.3 °C.     

Wood-fall associations from Late Cretaceous deep-water sediments of Hokkaido, Japan

Sunken wood (wood-fall) in the deep sea today is colonized and consumed by diverse invertebrate communities that show phylogenetic relationships to the chemotrophic fauna on whale carcasses, hydrothermal vents and hydrocarbon seeps. Here we document Late Cretaceous examples of wood-fall communities from deep-water sediments of the Yezo Group on Hokkaido, Japan, consisting of provannid, skeneiform, and patelliform gastropods, and thyasirid and nuculanid bivalves. These species are similar or identical to those found on plesiosaur bones and at hydrocarbon seeps in the same sediments, showing that many members of the modern chemotrophic deep-sea fauna colonized this range of habitats at least since Late Cretaceous time. We also document for the first time faecal chimneys in boreholes in these wood fragments, which were presumably built by xylophagain bivalves.     

Nasal bots and lice from white-tailed deer in southern Alberta, Canada

Heads of 64 white-tailed deer (Odocoileus virginianus) fawns, harvested in the vicinity of Magrath, Alberta, Canada, (49 degrees 24'782'N, 112 degrees 52'113'W) were examined for the presence of nasal bots and lice. The deer were collected between 8-30 January 2004 as part of a government-approved herd reduction protocol. The entire surface of each head was scanned visually for the presence of lice. Each head was split longitudinally, and the nasal passages, sinuses, and ethmoid region were washed for recovery of nasal bots. First instar Cephenemyia spp. were recovered from 17 heads (27%). Intensity of infestation ranged from 1-18 larvae (mean intensity 4.8). Among fawns, there were no significant differences in prevalence or mean intensity between the sexes. Two species of nasal bots were identified. Smaller larvae, tentatively identified as C. jellisoni, were present in 16 of 17 infested deer while larger specimens, tentatively identified as C. phobifera, were found in four deer; and in three of the four it co-occurred with C. jellisoni. The presence of C. phobifera in Alberta would represent a range extension for this species, which has not been known to occur west of North Dakota. Thirty-one fawns (48%) were infested with the sucking louse Solenopotes ferrisi. One infested fawn also had one specimen of the chewing louse, Tricholiopeurus lipeuroides.     

An Ornithomimid (Dinosauria) Bonebed from the Late Cretaceous of Alberta,with Implications for the Behavior,Classification, and Stratigraphy of North American Ornithomimids

Bonebeds can provide a wealth of anatomical, taphonomic, and ontogenetic information about the specimens preserved within them, and can provide evidence for inferred behavior. The material described here represents the first known bonebed of ornithomimids in North America, and the fourth record of an ornithomimosaur bonebed in the world. Partial skeletons representing three individuals are preserved in this assemblage, each comprising primarily portions of the posterior postcrania (pelvis, hind limbs and tail). All three individuals are morphologically similar, although one is larger in overall size. Given the stratigraphic position of the site, and the morphology of the postcrania, the preserved material represents a taxon from the clade containing Ornithomimus and Struthiomimus. Pedal ungual morphology is examined and found to be too variable to be useful in distinguishing these species taxonomically. This site provides additional evidence of gregarious behavior in ornithomimids and the first probable record of that behavior in North American forms.     

An enigmatic organism from the 'Exshaw' Formation (Devonian-Carboniferous), Alberta, Canada

Libodiscus ascitus gen. et. sp. nov. (incertae sedis) consists of a flask-like body (mean length of 15 mm; mean maximum width of 9 mm) bearing a flange of plates or flattened tentacles. At one end a pair of arm-like extensions connects with a disc with concentric markings. The flask has transverse structures with prominent relief. Some of these are more or less regularly arranged, but in other specimens they are much more irregular. On what appears to be the inner wall of the flask there are closely spaced striations. Libodiscus is known only from Devonian-Carboniferous transitional strata ('Exshaw' Formation) at Crowsnest Pass, southwest Alberta, Canada. Its affinities are speculative and no secure relationship can be demonstrated with metazoans, plants or other problematica such as chitinozoans. The disc is, however, similar to a number of discoidal fossils that previously have been assigned to chondrophorine medusoid hydrozoans. □ Libodiscus ascitus, Exshaw, Devonian, Carboniferous, problematica.     

Circulation of parasites among fishes from lakes in the Caribou Mountains,Alberta, Canada

Circulation of 24 macroparasite species among 12 species of fish was evaluated within samples of hosts collected from 9 lakes on an isolated plateau in northern Alberta, Canada. Twenty-seven parasite taxa (24 species plus the larval stages of Triaenophorus crassus, T. stizostedionis, and Raphidascaris acus) had the potential to be circulated among hosts. Sixteen parasite taxa were recovered from a single host species within a lake. Of the 11 remaining nonspecialist taxa, 4 were larval stages that matured in fish or birds and 7 were adults. Eight of the 11 cases of circulation among hosts involved lake whitefish, and this host was involved in the transmission of 5 species to piscivorous fishes. Despite evidence for the circulation of 7 taxa among the 4 species of sympatric Salmonidae, 60-99% of all worms were recovered from just 1 species of host. These results indicated that approximately 60% of the parasite taxa that infected fish in these lakes were absolute host specialists. The remaining 40% of parasite taxa had restricted host ranges, with most examples of parasite circulation limited to the 2 species of sympatric coregonid.     

First record of Lipoptena depressa (Diptera: Hippoboscidae) from Alberta, Canada

Lipoptena depressa is reported for the first time from Alberta on a 2 1/2-mo-old white-tailed deer fawn. This ked fly is one of four species occurring on deer in North America. The fawn had severe hemorrhagic enteritis of undetermined cause.     

Adoption Practices of The Blood Indians of Alberta,Canada

Abstract

Adoption is practiced in many parts of the world, but its mechanics are rarely spelled out in detail. The following paper is an effort to correct this lack for the Blood (Blackfoot) Indians living in Alberta in 1939. The introduction of a money economy and life on a reservation brought about certain modifications, but at the time this investigation was made “the Indians themselves” said adoption was “frequent in former times.” There is reason to believe that the motives for adoption and the varying attitudes of those who adopt and of those who are adopted have not changed radically through the years. Many parallels in adoption are apparent, not only in other Blackfoot tribes, but also in such North American Indian groups as the Crow, Omaha, Winnebago and Ojibwa.     

Probable Ankylosaur Ossicles from the Middle Cenomanian Dunvegan Formation of Northwestern Alberta,Canada

A sample of six probable fragmentary ankylosaur ossicles, collected from Cenomanian deposits of the Dunvegan Formation along the Peace River, represent one of the first dinosaurian skeletal fossils reported from pre-Santonian deposits in Alberta. Specimens were identified as ankylosaur by means of a palaeohistological analysis. The primary tissue is composed of zonal interwoven structural fibre bundles with irregularly-shaped lacunae, unlike the elongate lacunae of the secondary lamellar bone. The locality represents the most northerly Cenomanian occurrence of ankylosaur skeletal remains. Further fieldwork in under-examined areas of the province carries potential for additional finds.     

Chloranthaceous floral structures from the Late Cretaceous of Sweden

New chloranthaceous floral structures from the Late Cretaceous (Late Santonian/Early Campanian) of Scania, southern Sweden, have provided important new information on theChloranthistemon plants. The material includes well preserved fragments of inflorescence axes with flowers in situ documenting thatChloranthistemon flowers were bisexual and closely resembled those of extantChloranthus (Chloranthaceae). An emended diagnosis is given for the type species of the genus,Chloranthistemon endressii, and a new species,C. alatus, is described. The flowers ofChloranthistemon are small, perianthless and strongly zygomorphic, consisting of a tripartite and broadened androecium borne in an abaxial to lateral position on the monocarpellate ovary, and arranged in the axils of decussate bracts. Stamens are either completely free (C. alatus), or free at the base and coherent at the apex (C. endressii). The apical connective is extensive in both species; elaborated into conspicuous wing-like structures inC. alatus, or into a massive and shield-like structure inC. endressii. Pollen grains ofC. endressii are spheroidal, and reticulate and spiraperturate, while those ofC. alatus are ellipsoidal, tectate and foveolate with a unique combination of a distal colpus and a proximal furrow (colpus?) perpendicular to each other. Ovaries observed in well preserved flowers of both species are small and undifferentiated. Larger, dispersed fruits of chloranthaceous affinity are abundant and distinct, and probably represent at least two or three species, but cannot be linked with certainty to any of theChloranthistemon species described here.     

A synopsis of lake sturgeon management in Alberta, Canada

The lake sturgeon ( Acipenser fulvescens ) is resident in the North and South Saskatchewan rivers of Alberta. Because of their confined distribution, low abundance, and vulnerability to anthropogenic impacts, lake sturgeon in Alberta have been the focus of specific management actions for nearly 60 years.
Lake sturgeon harvest was prohibited in Alberta from 1940 to 1968, after which a limited harvest was again permitted, but only as a hook-and-line sport fishery. After being reopened the fishery was primarily managed as a "trophy" fishery. Sport fishery harvest statistics have been compiled annually since 1968, through mail-out questionnaires sent to all holders of sturgeon angling licenses.
Few research studies have been undertaken on the life history or habitat requirements of lake sturgeon in the province, and biologists have relied primarily on anglers to provide information for management decisions. Preliminary population information for the South Saskatchewan River, from mark-recapture data, suggests a population size of about 3700 fish. Recent studies in the North Saskatchewan River indicate a population of about 1300 fish. Studies indicate that a portion of the population in both rivers is trans-boundary, moving between the waters of the adjoining provinces of Alberta and Saskatchewan, and creating concerns because of differences in angling regulations. During recent decades, major consumptive uses of water have also contributed to depletion of lake sturgeon habitat in the province.
After reviewing past management strategies and actions, Alberta Environmental Protection implemented a number of regulatory changes in 1987 to further protect lake sturgeon populations in the province while continuing to provide angling opportunities and maintaining a controlled harvest.