|
Cryptodidymosphaerites Princetonensis
''Cryptodidymosphaerites'' is an extinct monotypic genus of pleosporale fungus of uncertain family placement. When described it contained the single species ''Cryptodidymosphaerites princetonensis''. The genus is solely known from the Early Eocene, Ypresian aged, Princeton Chert deposit of the Allenby Formation. ''Cryptodidymosphaerites'' is one of only three described fossil fungus species found in the Princeton Chert, and is a hyperparasite of '' Palaeoserenomyces allenbyensis'', itself a tar spot-like parasite of the fossil palm ''Uhlia''. Distribution ''Cryptodidymosphaerites princetonensis'' is known exclusively from the Princeton Chert, a fossil locality in British Columbia, Canada, which comprises an anatomically preserved flora of Eocene Epoch age, with rich species abundance and diversity. The chert is located in exposures of the Allenby Formation on the east bank of the Similkameen River, south of the town of Princeton, British Columbia. Notable in conjunction w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1998 In Paleontology
Flora Lycophytes Lycophyte research *Wehr (1998) reports, without description, ''Selaginella'' species spikemoss fossils occurring in the Eocene Okanagan highlands Klondike Mountain Formation. Fungi Fungal research *Currah, Stockey, & LePage (1998) describe the a phyllachoralean " tar spot" parasitizing ''Uhlia'' palm leaves, and host for a hyperparasitic pleosporalean fungus. They note them to be one of the first occurrences of hyperparasitic relationships in the fossil record. Arthropods Insects Molluscs Bivalves Amphibians newly named anurans Archosauromorpha Dinosaurs * A paper in the journal ''Nature'' is published by Karen Chin and others announcing the earlier discovery of a "king-sized coprolite" attributed to ''Tyrannosaurus rex''. * ''Lourinhasaurus'' gastroliths documented.Dantas et al. (1998). Sanders, Manley, and Carpenter (2001), "Table 12.1" page 167. * ''Cedarosaurus'' gastroliths documented.Sanders and Carpenter (1998). Sanders, Manley, and Car ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uhlia Allenbyensis
''Uhlia'' is an extinct genus of coryphoid palm containing a single species ''Uhlia allenbyensis''. The species is known from permineralized remains recovered from the Princeton Chert in British Columbia, Canada. Leaves of ''Uhlia'' have "tar spot"-like fungal infections of the extinct ascomycete ''Paleoserenomyces'', which in turn are hyperparasitized by the ascomycete ''Cryptodidymosphaerites''. Distribution ''Uhlia allenbyensis'' is known exclusively from the Princeton Chert, a fossil locality in British Columbia, Canada, which comprises an anatomically preserved flora of Eocene Epoch age, with rich species abundance and diversity. The chert is located in exposures of the Allenby Formation on the east bank of the Similkameen River, south of the town of Princeton, British Columbia. Notable in conjunction with the coal seams of the Allenby Formation are sections of chert which formed during silica-rich periods. The rapid cyclical changes from coal to chert and back are not ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil Preparation
Fossil preparation is the act of preparing fossil specimens for use in paleontological research or for exhibition, and involves removing the surrounding rocky matrix and cleaning the fossil. Techniques Acid maceration Acid maceration is a technique to extract organic microfossils from a surrounding rock matrix using acid. Hydrochloric acid or acetic acid may be used to extract phosphatic fossils, such as the small shelly fossils, from a carbonate matrix. Hydrofluoric acid is also used in acid macerations to extract organic fossils from silicate rocks. Fossiliferous rock may be immersed directly into the acid, or a cellulose nitrate film may be applied ( dissolved in amyl acetate), which adheres to the organic component and allows the rock to be dissolved around it. Film pull The film pull technique is a means of recovering carbonaceous compression fossils for study under transmitted light microscopy. An acid is applied to the surface of the rock to etch away the matrix from t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleofauna Of The Eocene Okanagan Highlands
The paleofauna of the Eocene Okanagan Highlands is comprised of Early Eocene arthropods, vertebrates, plus rare nematodes and molluscs found in geological formations of the northwestern North American Eocene Okanagan Highlands. The highlands lake bed series' as a whole are considered one of the great Canadian ''Lagerstätten''. The paleofauna represents that of a late Ypresian upland temperate ecosystem immediately after the Paleocene-Eocene thermal maximum, and before the increased cooling of the middle and late Eocene to Oligocene. The fossiliferous deposits of the region were noted as early as 1873, with small amounts of systematic work happening in the 1880-90s on British Columbian sites, and 1920-30s for Washington sites. Focus and more detailed descriptive work on the Okanagan Highlands site started in the last 1970's. Most of the highlands sites are preserved as compression-impression fossils in "shales", but also includes a rare permineralized biota and an amber biota. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
