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Relevant bibliographies by topics / Cedar Mountain Formation

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Academic literature on the topic 'Cedar Mountain Formation'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Cedar Mountain Formation"

1

Harris, Elisha B., and Nan Crystal Arens. "A mid-Cretaceous angiosperm-dominated macroflora from the Cedar Mountain Formation of Utah, USA." Journal of Paleontology 90, no. 4 (July 2016): 640–62. http://dx.doi.org/10.1017/jpa.2016.44.

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AbstractAngiosperms first appeared in the fossil record as pollen during the Valanginian–Hauterivian; they spread out of the tropics in the Aptian and Albian, and radiated in the Late Cretaceous. Despite these general patterns, details of the taxonomic, geographic, and ecological evolution of Cretaceous angiosperms are relatively poorly known because only a handful of Early and mid-Cretaceous macrofloras have been reported. This is the first detailed report of a fossil leaf flora from the Cedar Mountain Formation from the mid-Cretaceous of the Western Interior. We describe a flora that is overwhelmingly dominated by angiosperms (152 of 153 identified specimens are angiosperms) from the Albian–Cenomanian transition that is preserved in a clay- and carbonate-rich, lacustrine mudstone from the uppermost Cedar Mountain Formation of Emery County, Utah. We recognize 18 leaf morphotypes, all of which are dicotyledonous angiosperms. The majority of the Cedar Mountain morphotypes have taxonomic affinities with forms of similar age described from the Atlantic and Gulf coastal plains and other localities from the Western Interior. From this, we infer that a relatively diverse angiosperm flora grew along the margins of a small pond on the coastal plain. Palynological preparations of the fossil matrix were barren; however, previous studies of other facies within the formation showed that both conifers and ferns were important components of the regional vegetation during Cedar Mountain time. The effective absence of conifers and ferns in this macroflora and low leaf mass per area values among the angiosperms measured suggests that even at the Early–Late Cretaceous transition, angiosperms had come to dominate some sites, particularly those that were disturbed or seasonally ephemeral, where fast-growth or seasonal deciduousness would have been favored.

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Britt, Brooks B., Rodney D. Scheetz, Donald B. Brinkman, and David A. Eberth. "A Barremian neochoristodere from the Cedar Mountain Formation, Utah, U.S.A." Journal of Vertebrate Paleontology 26, no. 4 (December 11, 2006): 1005–8. http://dx.doi.org/10.1671/0272-4634(2006)26[1005:abnftc]2.0.co;2.

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3

Joeckel, R. M., G. A. Ludvigson, A. Möller, C. L. Hotton, M. B. Suarez, C. A. Suarez, B. Sames, J. I. Kirkland, and B. Hendrix. "Chronostratigraphy and terrestrial palaeoclimatology of Berriasian–Hauterivian strata of the Cedar Mountain Formation, Utah, USA." Geological Society, London, Special Publications 498, no. 1 (October 17, 2019): 75–100. http://dx.doi.org/10.1144/sp498-2018-133.

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AbstractThis paper presents breakthroughs in the chronostratigraphy of the heretofore poorly constrained Yellow Cat Member of the Cedar Mountain Formation, which is an important record of terrestrial environments, ecosystems and global change in the ancient North American Cordilleran foreland. Zircon populations from 10 stratigraphic horizons in the Yellow Cat Member yield youngest single-grain ages ranging from 142.5 ± 2.7 to 133.7 ± 2.7 Ma (Berriasian–late Valanginian); those from one mudstone palaeosol yield a robust Concordia Age of 136.3 ± 1.3 (Valanginian). Additionally, a new palynoflora – one of a few to be published from the Cedar Mountain Formation – is assigned to the middle Berriasian to early Hauterivian stages, based on the presence of Foraminisporis wonthaggiensis and Trilobosporites sp. cf. T. canadensis, and the absence of F. asymmetricus, Appendicisporites spp. and angiosperms. Furthermore, these chronostratigraphic data allow us to interpret part of the so-called ‘Weissert Event’ C-isotope excursion (Valanginian) in a new C-isotope profile through a palaeosol-bearing alluvial succession in the Yellow Cat Member. This research extends a firm understanding of the formation further back into the Early Cretaceous than was the case previously (except for ostracod biostratigraphy) and sets the stage for future advancements.

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Taylor, Michael P., Mathew J. Wedel, and Richard L. Cifelli. "A New Sauropod Dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA." Acta Palaeontologica Polonica 56, no. 1 (March 2011): 75–98. http://dx.doi.org/10.4202/app.2010.0073.

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5

Lockley, Martin G., Diane White, James Kirkland, and Vince Santucci. "Dinosaur Tracks from the Cedar Mountain Formation (Lower Cretaceous), Arches National Park, Utah." Ichnos 11, no. 3-4 (July 2004): 285–93. http://dx.doi.org/10.1080/10420940490428742.

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SHAPIRO, R. S., H. C. FRICKE, and K. FOX. "DINOSAUR-BEARING ONCOIDS FROM EPHEMERAL LAKES OF THE LOWER CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH." PALAIOS 24, no. 1 (January 1, 2009): 51–58. http://dx.doi.org/10.2110/palo.2008.p08-013r.

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7

Lorenz, John C., Scott P. Cooper, and William A. Olsson. "Natural fracture distributions in sinuous, channel-fill sandstones of the Cedar Mountain Formation, Utah." AAPG Bulletin 90, no. 9 (September 2006): 1293–308. http://dx.doi.org/10.1306/03300605137.

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8

Nydam, Randall L., and Richard L. Cifelli. "A new teiid lizard from the Cedar Mountain Formation (Albian–Cenomanian boundary) of Utah." Journal of Vertebrate Paleontology 22, no. 2 (July 8, 2002): 276–85. http://dx.doi.org/10.1671/0272-4634(2002)022[0276:antlft]2.0.co;2.

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9

Carpenter, Kenneth, Jeff Bartlett, John Bird, and Reese Barrick. "Ankylosaurs from the Price River Quarries, Cedar Mountain Formation (Lower Cretaceous), east-central Utah." Journal of Vertebrate Paleontology 28, no. 4 (December 12, 2008): 1089–101. http://dx.doi.org/10.1671/0272-4634-28.4.1089.

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10

Kirkland, James, Marina Suarez, Celina Suarez, and ReBecca Hunt-Foster. "The Lower Cretaceous in east-central Utah—The Cedar Mountain Formation and its bounding strata." Geology of the Intermountain West 3 (January 1, 2016): 101–228. http://dx.doi.org/10.31711/giw.v3.pp101-228.

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Although only recognized as a discrete stratigraphic unit since 1944, the Cedar Mountain Formation represents tens of millions of years of geological and biological history on the central Colorado Plateau. This field guide represents an attempt to pull together the results of recent research on the lithostratigraphy, chronostratigraphy, sequence stratigraphy, chemostratigraphy, and biostratigraphy of these medial Mesozoic strata that document the dynamic and complex geological history of this region. Additionally, these data provide a framework by which to examine the history of terrestrial faunas during the final breakup of Pangaea. In fact, the medial Mesozoic faunal record of eastern Utah should be considered a keystone in understanding the history of life across the northern hemisphere. Following a period of erosion and sediment bypass spanning the Jurassic–Cretaceous boundary, sedimentation across the quiescent Colorado Plateau began during the Early Cretaceous. Thickening of these basal Cretaceous strata across the northern Paradox Basin indicate that salt tectonics may have been the predominant control on deposition in this region leading to the local preservation of fossiliferous strata, while sediment bypass continued elsewhere. Thickening of overlying Aptian strata west across the San Rafael Swell provides direct evidence of the earliest development of a foreland basin with Sevier thrusting that postdates geochemical evidence for the initial development of a rain shadow.

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Dissertations / Theses on the topic "Cedar Mountain Formation"

1

Greenhalgh, Brent W. "A Stratigraphic and Geochronologic Analysis of the Morrison Formation/Cedar Mountain Formation Boundary, Utah." Diss., CLICK HERE for online access, 2006. http://contentdm.lib.byu.edu/ETD/image/etd1392.pdf.

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Ayers, James D. "Lithologic Evidence of Jurassic/Cretaceous Boundary Within the Nonmarine Cedar Mountain Formation, San Rafael Swell, Utah." Ohio University / OhioLINK, 2004. http://www.ohiolink.edu/etd/view.cgi?ohiou1097256637.

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Roca, Xavier Argemi. "Tectonic and Sequence Stratigraphic Implications of the Morrison Formation-Buckhorn Conglomerate Transition, Cedar Mountain, East-central Utah." Ohio University / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1079297057.

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Mori, Hirotsugu. "Dinosaurian Faunas of the Cedar Mountain Formation and LA-ICP-MS Detrital Zircon Ages for Three Stratigraphic Sections." BYU ScholarsArchive, 2009. https://scholarsarchive.byu.edu/etd/2000.

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The Cedar Mountain Formation contains the most diverse record of Early Cretaceous dinosaurs in the western hemisphere. However, analyses of its faunas have been hindered because 1) most taxa are based on incomplete/fragmentary materials or incomplete descriptions, 2) most sites and some horizons preserve few taxa, and 3) the stratigraphy and geochronology are poorly understood. To help resolve these stratigraphic and correlation problems U-Pb LA-ICP-MS detrital zircon ages were obtained at significant sites and horizons. These dates indicate all sites at or near the base of the formation are no older than 122 to 124 Ma, thus all basal stratigraphic packages are time equivalent. Detrital zircons coarsely bracket the temporal span of the Ruby Ranch Member between about 115 Ma to 111 Ma while the base of the Mussentuchit Member is dated between 108 to 104 Ma and the top of the member is Cenomanian in age. Multivariate analyses utilizing Simpson and Raup-Crick similarity index and pair-group moving algorithms reveal that formationfs faunas fall into two groups. These groups are compared statistically with European, Asian, and Morrison faunas. Results indicate (1) that there is no close relationship between the Yellow Cat fauna and the Morrison Formation fauna and (2) corroborate long-standing hypotheses that the Yellow Cat fauna has European ties and the Mussentuchit fauna has Asian ties. Detrital zircon LA-ICP-MS U-Pb ages were used in this study to approximate the time of deposition of strata because volcanic ashes are rarely preserved in the formation. The ability to select the youngest crystals in a sample prior to applying analytical methods could substantially reduce the number of crystals and cost required to obtain these dates. To this end, the hypothesis that the most pristine, unabraded crystals should be younger than abraded crystals was tested by imaging detrital zircons via SEM, ranking the crystals by the degree of abrasion, and determining their ages. Results of this study partly corroborate the hypothesis in that there is a correlation between the degree of abrasion and ages – obviously abraded crystals are most likely the oldest while pristine to slightly abraded crystals are usually the youngest in a given sample.

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Knight, John A. II. "Quantifying Climate Change Over the Early Cretaceous Ruby Ranch Member of the Cedar Mountain Formation, East-Central Utah." Thesis, The University of Texas at San Antonio, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10813710.

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The age of the Ruby Ranch Member (RRM) of the Cedar Mountain Formation in East-Central Utah was recently constrained using carbon isotope chemostratigraphy to span known excursions associated with the late Aptian. The RRM is characterized by calcrete horizons that are thought to occur across the C10 carbon isotope excursion. Along with carbonate stable isotope analyses and the region’s paleo-position in a depositional basin on the leeward rain shadow of the Sevier Orogenic belt, this interval is hypothesized to coincide with an aridification event. Our research objective is to quantify the extent of this aridity using clumped isotope paleothermometry (n = 7) and paleoprecipitation proxies (n = 51) for samples collected across the C10 chemostratigraphic interval. Two weathering indices, CIA-K and CALMAG, were applied to data obtained using X-ray fluorescence spectrometry. Using these proxies, we determined mean annual precipitation across the RRM at its type section. Precipitation values ( n = 27) obtained through CIA-K for identified paleosol horizons ranged between 795 and 1275 mm/year, and through CALMAG ranged between 735 and 1042 mm/year. Precipitation values decreased through the C10 interval which may indicate increased aridity. Clumped isotopes provided ?47 values ranging from 0.647 to 0.693‰. Paleotemperature measurements (n = 4) from accepted carbonate samples were between 27.9 and 46.3 °C. Isotopic compositions of water calculated from carbonates ranged between -4.4‰ and -1.9‰ VSMOW. Precipitation values and temperatures were not lowest during the C10 interval. Temperatures peaked at the end of the C10 interval and decreased afterward, indicating a potential for cooler, more arid conditions. These results suggest that carbon cycle changes during the mid-Cretaceous may have influenced paleoclimate conditions experienced in terrestrial settings.

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Sorensen, Amanda Elizabeth MacKay. "Geologic mapping of exhumed, mid-Cretaceous paleochannel complexes near Castle Dale, Emery County, Utah: On the correlative relationship between the Dakota Sandstone and the Mussentuchit Member of the Cedar Mountain Formation." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2727.

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Numerous well-preserved, exhumed paleochannels in the Morrison, Cedar Mountain and Dakota Sandstone formations are exposed east of Castle Dale, Utah. These channels consist primarily of point bar complexes and scattered, low sinuosity channels. To determine the vertical and lateral relationships of these channels within the Cedar Mountain and Dakota Sandstone formations, a 1:24,000 scale geologic map covering ~140 km2 was created showing the fluvial sandstones. In the study area the Cedar Mountain Formation consists, from bottom to top, of 2.5-10 m of Buckhorn Conglomerate Member equivalent units, ~80 m of the Ruby Ranch Member, and ~30 m of the Mussentuchit Member. The Dakota Sandstone consists of conglomeratic to sandy, meandering channel fills within the Mussentuchit Member. The Ruby Ranch-Mussentuchit member contact is diagnosed as the top of a laterally extensive, ~10 meter thick, maroon paleosol with calcrete horizons and root traces. When deeply weathered the contact is discernable as a shift from maroon mudstone to a pale green-white, silty mudstone. Like the balance of the Mussentuchit Member overbank deposits, the white-green mudstone is rich in smectitic clays. In the southern one-third of the mapped area, Ruby Ranch Member sandstones are thin, discontinuous channel segments surrounded by floodplain deposits. In the middle to northern area, point bar complexes dominate, some of which are laterally amalgamated. Flow direction data from four meander complexes and a low sinuosity channel indicate an average northeast flow. Dakota Sandstone channels all of which are within the Mussentuchit Member also flowed to the northeast but point bar complexes are both more numerous and more laterally continuous than in the Ruby Ranch Member, indicating deposition in an area with less accommodation space than during Ruby Ranch Member time. The data indicate the Dakota Sandstone consists exclusively of fluvial sandstones encased within the Mussentuchit Member of the Cedar Mountain Formation. Therefore, these units are coeval and simply different facies of the same depositional system. Consequently the Mussentuchit Member is considered a member facies of the Dakota Formation.

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Hokanson, William H. "Identifying Complex Fluvial Sandstone Reservoirs Using Core, Well Log, and 3D Seismic Data: Cretaceous Cedar Mountain and Dakota Formations, Southern Uinta Basin, Utah." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2597.

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The Cedar Mountain and Dakota Formations are significant gas producers in the southern Uinta Basin of Utah. To date, however, predicting the stratigraphic distribution and lateral extent of potential gas-bearing channel sandstone reservoirs in these fluvial units has proven difficult due to their complex architecture, and the limited spacing of wells in the region. A new strategy to correlate the Cedar Mountain and Dakota Formations has been developed using core, well-log, and 3D seismic data. The detailed stratigraphy and sedimentology of the interval were interpreted using descriptions of a near continuous core of the Dakota Formation from the study area. The gamma-ray and density-porosity log signatures of interpreted mud-dominated overbank, coal-bearing overbank, and channel sandstone intervals from the cored well were used to identify the same lithologies in nearby wells and correlate similar stratal packages across the study area. Data from three 3D seismic surveys covering approximately 140 mi2 (225 km2) of the study area were utilized to generate spectral decomposition, waveform classification, and percent less-than-threshold attributes of the Dakota-Cedar Mountain interval. These individual attributes were combined to create a composite attribute that was merged with interpreted lithological data from the well-log correlations. The overall process resulted in a high-resolution correlation of the Dakota-Cedar Mountain interval that permitted the identification and mapping of fluvial-channel reservoir fairways and channel belts throughout the study area. In the future, the strategy employed in this study may result in improved well-success rates in the southern Uinta Basin and assist in more detailed reconstructions of the Cedar Mountain and Dakota Formation depositional systems.

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Books on the topic "Cedar Mountain Formation"

1

Stikes, Mathew W. Fluvial facies and architecture of the poison strip sandstone lower cretaceous Cedar Mountain Formation, Grand County, Utah. Salt Lake City, Utah: Utah Geological Survey, 2007.

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2

McPherson, Mary L. Reservoir characterization of the Cretaceous Cedar Mountain and Dakota Formations, Southern Uinta Basin: Year-one report. Salt Lake City, Utah: Utah Geological Survey, 2006.

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Fluvial facies and architecture of the poison strip sandstone lower cretaceous Cedar Mountain Formation, Grand County, Utah. Utah Geological Survey, 2007. http://dx.doi.org/10.34191/mp-06-2.

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4

Reservoir characterization of the lower Cretaceous Cedar Mountain and Dakota Formations, Northern Uinta Basin, Utah. Utah Geological Survey, 2012. http://dx.doi.org/10.34191/ofr-597.

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Reservoir characterization of the Cretaceous Cedar Mountain and Dakota Formations, southern Uinta Basin : Year-one report. Utah Geological Survey, 2006. http://dx.doi.org/10.34191/ofr-492.

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Reservoir characterization of the Cretaceous Cedar Mountain and Dakota Formations, southern Uinta Basin, Utah : year-one report, year-two report. Utah Geological Survey, 2008. http://dx.doi.org/10.34191/ofr-516.

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7

Cedar Mountain and Dakota formations around Dinosaur National Monument : evidence of the first incursion of the Cretaceous western interior seaway into Utah. Utah Geological Survey, 2012. http://dx.doi.org/10.34191/ss-143.

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Book chapters on the topic "Cedar Mountain Formation"

1

Weiss, Malcolm P., and Michael G. Roche. "The Cedar Mountain Formation (Lower Cretaceous) in the Gunnison Plateau, central Utah." In Geological Society of America Memoirs, 557–70. Geological Society of America, 1988. http://dx.doi.org/10.1130/mem171-p557.

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Suarez, M. B., C. A. Suarez, A. H. Al-Suwaidi, G. Hatzell, J. I. Kirkland, J. Salazar-Verdin, G. A. Ludvigson, and R. M. Joeckel. "Terrestrial Carbon Isotope Chemostratigraphy in the Yellow Cat Member of the Cedar Mountain Formation." In Terrestrial Depositional Systems, 303–36. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-803243-5.00008-x.

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Conference papers on the topic "Cedar Mountain Formation"

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Keebler, Abby, Edward Simpson, Michael Wizevich, Willow R. Reichard-Flynn, Issac Diljohn, Lara Ilsemann, Abigail C. Underwood, and Isabelle Kisluk. "HYPERCONCENTRATED FLOWS IN THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, EAST-CENTRAL UTAH." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-333873.

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Ryan, Allison Aileen. "DETERMINING THE CHEMOSTRATIGRAPHIC RECORD OF THE CEDAR MOUNTAIN FORMATION USING δ13CORG ISOTOPES." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289273.

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Paige, Mark R., and Marina B. Suarez. "ISOTOPE GEOCHEMISTRY OF LACUSTRINE DEPOSITS IN THE CRETACEOUS CEDAR MOUNTAIN FORMATION, EASTERN UTAH." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289200.

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Martin, Anthony J., James I. Kirkland, Donald D. DeBlieux, Vincent L. Santucci, Andrew R. C. Milner, Celina Suarez, and Marina B. Suarez. "PROBABLE AVIAN FEEDING TRACE FOSSILS FROM THE CEDAR MOUNTAIN FORMATION (LOWER CRETACEOUS), UTAH USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318336.

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Kisluk, Isabelle, Willow R. Reichard-Flynn, Shannon N. Evans, Abby Keebler, Michael C. Wizevich, and Edward Simpson. "DIAGENETIC HISTORY OF CRYPTALGAL CARBONATES IN THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, EASTERN UTAH." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324481.

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Lee, Jacquelin Diane, Andreas Möller, G. Ludvigson, Marina B. Suarez, Noah McLean, R. M. Joeckel, Julie Maxson, and ReBecca Hunt-Foster. "VOLCANOGENIC ZIRCONS FROM MUDROCKS AND CHRONOSTRATIGRAPHIC REFINEMENT OF THE CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH." In Joint 55th Annual North-Central / 55th Annual South-Central Section Meeting - 2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021nc-362848.

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Topping, Leah, and Brett T. McLaurin. "SILCRETE DEVELOPMENT WITHIN FLUVIAL CHANNELS OF THE CEDAR MOUNTAIN FORMATION (EARLY CRETACEOUS), GREEN RIVER, UTAH." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344842.

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Lee, Jacquelin Diane, Andreas Möller, G. A. Ludvigson, Marina B. Suarez, Noah McLean, R. M. Joeckel, and Julie Maxson. "REFINING THE CHRONOSTRATIGRAPHY OF THE CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH USING VOLCANOGENIC ZIRCON FROM MATURE PALEOSOLS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355167.

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Reichard-Flynn, Willow R., Shannon N. Evans, Isabelle Z. Kisluk, Abigail C. Underwood, Edward L. Simpson, and Michael C. Wizevich. "A PROBABLE EARLY CRETACEOUS PARACOPID DUNG BEETLE NEST, UPPER YELLOW CAT MEMBER, CEDAR MOUNTAIN FORMATION, EAST-CENTRAL UTAH." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310932.

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Wizevich, Michael C., Isabelle Kisluk, Willow R. Reichard-Flynn, Abby Keebler, Shannon N. Evans, and Edward Simpson. "FLUVIAL ARCHITECTURE OF EXHUMED AND INVERTED PALEOCHANNELS OF THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION OF EAST-CENTRAL UTAH." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328242.

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