|Statement||Charles A. Sandberg and David L. Clark, editors.|
|Series||Brigham Young University geology studies ; v. 26, pt. 3|
|Contributions||Sandberg, Charles A 1929-, Clark, David Leigh, 1931-, Geological Society of America. Rocky Mountain Section., Pander Society.|
|The Physical Object|
|Pagination||v, 190 p. :|
|Number of Pages||190|
General Information. Title: Youngest Permian conodont faunas from the Great Basin and Rocky Mountain regions Author(s): Wardlaw, B.R., and Collinson, J.W. Publishing Organization: Brigham Young University Department of Geology Series and Number: Brigham Young University Geology Studies v. 26 [pt. 3, p. ] Larger Work: Conodont biostratigraphy of the Great Basin and Rocky Mountains. Conodont fossils preserving features of the soft tissues of both the head and trunk are known from only two places in the world. The Upper Ordovician Soom Shale of Cape Province, South Africa, has yielded a single specimen that displays structures of the head and of the anterior portion of the trunk (Figure 2), as well as more than one hundred specimens that preserve paired head structures. Upper Paleozoic strata of the Pre-Uralian Foredeep in the southern Ural Mountain region of Russia and Kazakhstan comprise the type area of the Cisuralian Series (Lower Permian), consisting of Asselian, Sakmarian, Artinskian, and Kungurian stages. Current studies in the region will establish stratotypes and precise chronostratigraphic stage and substage boundaries of the Cisuralian based on Cited by: 1. Significant advances in refining the Upper Devonian conodont zonation and in establishing biofacies of conodont zones have been made for the northern Rocky Mountains, Great Plains, and Great Basin.
The temporal constraints established by conodont biostratigraphy allow correlation to the Grizzly Bear Formation, a regionally restricted Lower to Middle Devonian unit in the Selwyn Basin to the north. Résumé: Une nouvelle unité de bassin du Groupe de Road River, Dévonien inférieur à moyen, ci-après désigné formellement sous le nom de. Devonian and Lower Mississippian conodont zonation of the Great Basin and Rocky Mountains, In SANDBERG, C.A. & CLARK, D.L. (eds) Conodont biostratigraphy of the Great Basin and Rocky Mountains, Brigham Young University Geology Studies 26(3). Conodont biostratigraphy and depositional history of the Middle Devonian to Lower Carboniferous in the Cantabrian zone (Cantabrian Mountains, Spain). Conodont biostratigraphy of the Great Basin and Rocky Mountains. Brigham Young Univ. Geol. Stud. ; pp., many figs./plts. Orig. wrps., small libr. stamp on title page only, 4to. Aspects of Middle and Upper Ordovician conodont biostratigraphy of carbonate facies in Nevada and southeast California and comparison with some Appalachian successions. - [In:] Sandberg, C. A. & Clark, D. L. (eds.) Conodont biostratigraphy of the Great Basin and Rocky Mountains.
The purpose of this study is to 1) document new δ 13 C carb curves from Lower–Middle Ordovician carbonate rocks at Shingle Pass (South Egan Range, NV) and the Ibex area (western UT) in the Great Basin region, USA, 2) examine local or regional sources of variability related to diagenesis and sea-level change, and 3) evaluate the global significance of these new data by comparison to δ 13 C. Permian conodont biostratigraphy in the Great Basin. In Sandberg, C. A., and Clark, D. L. (eds.), Conodont biostratigraphy of the Great Basin and Rocky Mountains: Brigham Young University Geology Studies, Scientific Bookseller. Determination Guides. Geological Guide Books. Versandbuchhandlung Dr. Frank Rudolph Books on Fossils, Palaeontology, Geology, Rocks, Minerals and more. Home > Systematics > Invertebrates > Conodonta. Conodonta! Brachiopods and conodont biostratigraphy of the Famennian from the Dębnik anticline, southern Poland. Conodont biostratigraphy of the Bakken and lower Lodgepole Formations (Devonian and Mississippian), Williston Basin, North Dakota and their respective equivalents in the northern Rocky Mountains and northern midcontinent 27 skeletal limestone near the Basin margins. Conodonts were recovered from the three members of the Bakken, by.