Back Matter (PDF)

Total Page:16

File Type:pdf, Size:1020Kb

Back Matter (PDF) Items listed in order of radiometric age Radiometric ages in this list have been arranged in order of increasing magnitude. If every age were exact, the list would correspond to the stratigraphical order of the Items, but since some determinations are imprecise or anomalous the list is only a first approximation to a true chronological order. Its purpose is to provide a summary of data, including that basic for the construction of a time-scale, and to assist in finding data in the Items when the approximate stratigraphical or radiometric age is known. Each entry gives the Item number, stratigraphical range (with the youngest rocks first), age (in millions of years), method used, and mineral (or rock) on which the determination was made. The abbreviations used are listed overleaf. Determinations on metamorphic or intrusive igneous rocks are indicated by an oblique stroke that separates the stratigraphical range of the metamorphosed and igneous rocks from that of any overlying rocks; e.g., Pliocene/Jurassic. This con- vention has not been adopted in the Items themselves. The values used have been standardized wherever possible (see the introduc- tion to the Items for details), and the Rb-Sr age listed is that determined from the A = I "47 × I0--11 Year-1 decay constant. In a given entry, ages determined by different methods have not been combined into a single average or mean age (as they may have in some parts of Part 4) but have been given separately. If, however, several approximately concordant ages have been found by the same method, the figure given for the age under that entry is the mean of these values. When ages are widely scattered, their range is generally listed, with the youngest age first. A few very anomalous ages have been omitted. In the latest stages of preparation, improvements in presentation of data sug- gested themselves, and it was decided that it would be helpful to adopt them, even though consistency between different parts of the volume would be reduced. Thus the presentation of the following data, although based on the Items, differ in several respects from them. The Geological Society Phanerozoic time-scale 1964 is summarized on pp. 260-3. 443 Items listed in order of increasing age ABBREVIATIONS USED FOR MINERALS AND ROCKS ab, albite hb, hornblende or, orthoclase ur, uraninite an, anorthoclase il, illite pl, plagioclase vat., various minerals, ad, adularia km, kolm pt, pitchblende rocks bi, biotite lp, lepidolite py, pyroxene xn, xenotime br, brannerite mb, molydenite sd, sanidine zr, zircon fi, feldspar mu, muscovite sy, sylvine ?, not stated gl, glauconite mz, monazite TR, total rock Note: Although/.7, M, and L generally correspond to the formally recognized stratigraphical sub- divisions Upper, Middle, and Lower respectively, they may also stand for the following: U, upper, late, top; M, mid-; L, lower, early, basal. Age Item Stratigraphical range (m.y.) Method Mineral lO 7 Plio-Pleistocene o" 95 K-Ar sat 243 Pleistocene (Irvingtonian) i- 36 K-Ar TR i o8 --/Plio-Plelstocene (?U. Blancan) i. 53 K-Ar bi 244 L. Pleistocene (Villafranchian)-Pliocene (Astian) 1.6i K-Ar TR 245 L. Pleistocene (Villafranchian) I75 K-Ar an 246 --/Plio--Pleistocene (?U. Blancan) I9 K-Ar bi 247 Plio-Pleistocene (?U. Blancan) 2 05 K-Ar bi 248 Plio-Pleistocene (U. Blancan) 225 K-Ar bi 3o9 Plio- Pleistocene (Blancan) 32 K-Ar TR 3o8 Plio-Pleistocene (Blancan) 33 K-Ar TR 249 Plio--Pleistocene (?U. Blancan) 33 K-Ar pl 250 Plio-Pleistocene (Blancan) 3"48 K-At pt, py 251 Pliocene (L. Blancan-U. Hemphillian) 4. I K-Ar TR 25 U. Pliocene 5.2 K-At gl 252 Pliocene (U. Hemphillian) 5.2 K-Ar fi 318 U. Miocene (~ Pontian) 6.1-7.6 K-Ar ? 253 Mio-Pliocene (Hemphillian) 6"4 K-Ar sd Io9 L. Pliocene (Tabanian)/U. Eocene 7.0 K-At ? Io9 L. Pliocene (Tabanian)/U. Eocene 7-o Rb---Sr var. 317 U. Miocene (L. Hemphillian-U. Clarendonian) 7'7 K-Ar ? 36 Pliocene (Scaldisian) 8"o5 K-At gl 254 Mio-Pliocene (Hemphillian) 8-i K-Ar pl 27 ° ~/U. Miocene (Clarendonian) 8- 9 K-Ar sd 255 Mio-Pliocene (Hemphillian) 8"9 K-At sd 256 Mio--Pliocene (Hemphillian) 9"2 K-Ar TR 28 U. Miocene (L. Hemphillian) 9.2 K-Ar bi 1 Io U. Miocene 9-6 K-Ar gl 271 U. Miocene (Clarendonian) 9"8 K-Ar TR 272 U. Miocene (Clarendonian) 9"8 K-Ar TR 258 U. Miocene (U. Clarendonian) 9"89 K-Ar pl 259 U. Miocene (Clarendonian) 9"9 K-Ar bi 257 U. Miocene (L. Hemphillian) 10"0 K-Ar TR 264 U. Miocene (L. Clarendonian) IO.6 K-Ar TR 26 U. Miocene (U. Clarendonian) lO- 7 K-Ar bi 26o U. Miocene (Clarendonian) lO- 7 K-Ar sd 266 U. Miocene (L. Clarendonian) lO. 7 K-Ar bi AAA Items in order of increasing age Age Item Stratigraphical range (m.y.) Method Mineral 265 U. Miocene (L. Clarendonian) xo.8 K-Ar bi 262 U. Miocene (L. Clarendonian) IO'85 K-Ar bi 261 U. Miocene (Clarendonian) I I "o K-Ar sd 263 U. Miocene (L. Clarendonian) I I "o K-Ar bi 268 U. Miocene (L. Clarendonian) x I. I K-Ar bi 27 U. Miocene (L. Clarendonian) I I. 1-I2 K-Ar bi 274 U. Miocene (Clarendonian) I x '4 K-Ar TR 269 U. Miocene (L. Clarendonian) x I "4 K-Ar bi 267 U. Miocene (L. Clarendonian) ix. 5 K-Ar sd 273 U. Miocene (Clarendonian) x x. 7 K-Ar TR 275 U.-M. Miocene (L. Clarendonian-U. Barstovian) i x .8 K-Ar bi, pl 314 - 'U. Tertiary' x3"4 K-Ar 313 'L. Pliocene' 14" o K-Ar 276 M. Miocene (Barstovian) x4" 6 K-At TR, pl 277 ) 312 L. Pliocene-L. Miocene x4" 6-15" 9 K-At ? 278 M. Miocene (U. Barstovian) x4. 7 K-Ar TR 279 M. Miocene ( ?L. Barstovian) x5" o5 K-At sd 38 M. Miocene (Barstovian) x5" 2 K-Ar bi 39 M. Miocene (Barstovian) 15" 2 K-Ar bi i28 L. Miocene (Hutchinsonian) 15" 4 K-Ar gl 28o M.-L. Miocene (Barstovian-Hemingfordian) 15" 4 K-Ar TR 28[ M. Miocene (Barstovian) x5" 4 K-Ar sd 282 M. Miocene ( ?L. Barstovian) x5" 6 K-Ar sd I3I 'U. Miocene' I6 Pb-a zr, mz, xn 40 ~/U. Oligocene x7" o K-Ar bi 79 M.-L. Miocene (U. Hemingfordian) 17 • 2 K-Ar bi 15o U.-M. Eocene 18 K-Ar gl I27 L. Miocene (Waitakian) x9" 4 K-Ar gl I29 M. Miocene (Waiauan) x9" 9 K-Ar gl i26 Oligocene (Duntroonian-Whaingaroan) 2o'8 K-Ar gl 8o L. Miocene (U. Arikareean) 2 I- 45 K-Ar bi I97 Oligocene (Whitneyan-Orellan) 2 I. 6 K-Ar ad 3IO L. Miocene (Santacrucian) 2 I- 7 K-Ar pl 8i L. Miocene-U. Oligocene (L. Zemorrian) 22"5 K-At gl 315 L. Miocene (L. Arikareean) 23"3 K-Ar 82 L Miocene (Burdigalian) 24"8 K-Ar gl 283 L. Miocene (L. Arikareean) 24"9 K-Ar ab I48 U.-M. Eocene 25 K-At gl 284 L. Miocene (Arikareean) 25"3 K-Ar TR 285 L. Miocene (L. Arikareean) 25"6 K-Ar TR 83 U. Oligocene (Whitneyan) 25"7 K-Ar sd I34 'U. Miocene' 26-24 ° Pb-a zr x49 U.-M. Eocene 27 K-At gl 286 L. Miocene (L. Arikareean) 29"5 K-At TR 287 Recent-L. Oligocene (U. Chadronian) 29"7 K-At I35 U. Miocene (Tongaporutuan) 3 °. 2-35" 8 K-Ar gl I46 U.-M. Eocene 31 K-Ar gl 23I L. Cretaceous (Upper Hauterivian) 31 K-Ar gl 288 U.-L. Oligocene (Whitneyan-Chadronian) 3 x. [ K-Ar sd III U. Eocene 3 i. 4 K-Ar gl 289 U.-L. Oligocene (Whitneyan-Chadronian) 3 I" 5 K-At sd 445 Items in order of increasing age Age Item Stratigraphical range (m.y.) Method Mineral 296 L. Oligocene (Chadronian) 3 I. 6 K-Ar bi 3xI L. Oligocene 3 I. 6 K-Ar TR I55 Oligocene 32 K-Ar bi 295 L. Oligocene (M. Chadronian) 32" 6 K-Ar bi 297 Oligocene 32" 8 K-Ar bi I5I U.-M. Eocene 33 K-Ar gl 84 L. Oligocene (Chadronian) 33" x K-Ar sd 292 L. Oligocene (L. Chadronian) 33"3 K-Ar bi 293 L. Oligocene (M. Chadronian) 33"7 K-Ar bi 85 L. Oligocene/M. Eocene 35 K-Ar bi I3O L. Oligocene 35 K-Ar sy 29 x L. Oligocene (L. Chadronian) 35"2 K-Ar sd, pl 23 U. Eocene (Kiev stage) 35" 6 K-Ar gl 294 L. Oligocene (M. Chadronian) 35"7 K-Ar sd, pl x47 U.-M. Eocene 36 K-Ar gl 299 L. Oligocene-U. Eocene (L. Chadronian- U. Duchesnean) 36" 5 K-Ar sd 125 U. Eocene (Kaiatan) 36" 6 K-Ar gl 29 ° L. Oligocene (L. Chadronian) 36"8 K-Ar fs 3oo L. Oligocene-U. Eocene (Duchesnean) 37' o K-Ar sd, bi, TR 298 L. Oligocene-U. Eocene (L. Chadronian- U. Duchesnean) 37" 5 K-Ar TR I32 'Oligocene-U. Eocene' 38 Pb--a zr, mz, xn I52 L. Eocene-Palaeocene 38 K-Ar gl I23 M. Eocene (Claibornian) 39 K-Ar gl I I 4 U. Eocene (Jacksonian) 39"4 K-Ar gl x x5 M. Eocene (~ Lutetian) 4 x "8 K-Ar gl 2 i8 L. Cretaceous (U. Albian) 42-82 K-Ar gl 124 M.
Recommended publications
  • South Dakota to Nebraska
    Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska.
    [Show full text]
  • Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)
    St. Cloud State University theRepository at St. Cloud State Culminating Projects in Cultural Resource Management Department of Anthropology 10-2019 Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) Samantha Mills Follow this and additional works at: https://repository.stcloudstate.edu/crm_etds Part of the Archaeological Anthropology Commons Recommended Citation Mills, Samantha, "Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)" (2019). Culminating Projects in Cultural Resource Management. 28. https://repository.stcloudstate.edu/crm_etds/28 This Thesis is brought to you for free and open access by the Department of Anthropology at theRepository at St. Cloud State. It has been accepted for inclusion in Culminating Projects in Cultural Resource Management by an authorized administrator of theRepository at St. Cloud State. For more information, please contact [email protected]. Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) by Samantha M. Mills A Thesis Submitted to the Graduate Faculty of St. Cloud State University in Partial Fulfillment of the Requirements for the Degree of Master of Science in Functional Morphology October, 2019 Thesis Committee: Matthew Tornow, Chairperson Mark Muñiz Bill Cook Tafline Arbor 2 Abstract Toward the end of the Middle Eocene (40-37mya), the environment started to decline on a global scale. It was becoming more arid, the tropical forests were disappearing from the northern latitudes, and there was an increase in seasonality. Research of the Chadronian (37- 33.7mya) in the Great Plains region of North America has documented the persistence of several mammalian taxa (e.g. primates) that are extinct in other parts of North America.
    [Show full text]
  • Rodents (Mammalia) from the Pilgrim Creek Local Fauna, Wyoming: a Mixed Eocene and Oligocene Assemblage (Duchesnean to Whitneyan)
    Paludicola 11(2):51-72 March 2017 © by the Rochester Institute of Vertebrate Paleontology RODENTS (MAMMALIA) FROM THE PILGRIM CREEK LOCAL FAUNA, WYOMING: A MIXED EOCENE AND OLIGOCENE ASSEMBLAGE (DUCHESNEAN TO WHITNEYAN) William W. Korth Rochester Institute of Vertebrate Paleontology, 265 Carling Road, Rochester, New York 14610 <[email protected]> ABSTRACT Previously, only the non-eomyid rodents from the Pilgrim Creek fauna of Wyoming have been described (Sutton and Black, 1975; Korth, 1981; Korth and Emry, 2013). This fauna has been considered as Chadronian in age since its first description. Twenty-seven species of rodents are recognized here from this fauna. There is a predominance of Chadronian species (13 taxa); however, the presence of three species known elsewhere from the Duchesnean (“Leptotomus” guildayi, Metanoiamys korthi, Griphomys cf. alecer), four from the Orellan (“Prosciurus” sp., cf. relictus, Eumys elegans, “Scottimus” viduus, Protosciurus sp., cf. P. mengi), and two from the Whitneyan (Leptodontomys douglassi, Ansomys sp., cf. A. cyanotephrus,) demonstrates that the fauna is clearly mixed with elements from four different horizons. INTRODUCTION either earlier or later horizons, demonstrating the evident mixing of faunas. Over 40 years ago, Sutton and Black (1975) _________________________________________ identified 11 species of rodents from the Pilgrim Creek fauna of Wyoming (Table 1). However, TABLE 1. Previously identified rodents from the Pilgrim Creek specimens of the family Eomyidae were not local fauna, Wyoming (Sutton and Black, 1975). described or listed. The locality from which the Ischyromyidae fossils were collected is in the Teton National Forest Ischyromys cf. veterior in Jackson County, Wyoming along Pilgrim Creek Cylindrodontidae (Sutton and Black, 1975).
    [Show full text]
  • Paleogene and Neogene Time Scale of GTS 2012 Paleogene Neogene N
    Paleogene and Neogene Time Scale of GTS 2012 Paleogene Neogene N. Vandenberghe 1, F.J. Hilgen 2 and R.P. Speijer 3 F.J. Hilgen 1, L.J. Lourens 2 and J.A. Van Dam 3 1. Department of Earth and Environmental Sciences, K. U. Leuven, Celestijnenlaan 200E, B - 3001 Leuven, Belgium, [email protected] 1. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands, [email protected] 2. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands, [email protected] 2. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3508 TA Utrecht, The Netherlands, [email protected] 3. Department of Earth and Environmental Sciences, K. U. Leuven, Celestijnenlaal 200E, B - 3001 Leuven, Belgium, [email protected] 3. Institut Català de Paleontologia Miquel Crusafont (ICP), Campus de la UAB, Mòdul ICP, E-08193 cerdanyola del Vallès, Spain, [email protected] Of the 9 Paleogene stages, only 3 remain to be formally defined: the Bartonian and Priabonian stages of upper Paleogene Time Scale Eocene and the Chattian (base of upper Oligocene). Larger 18 13 AGE Epoch/Age Polarity Mega- Dinoflagellate Cysts North American O C AGE -1.0 -0.5 -0.5 Of the 8 Neogene stages, only 2 remain to be formally defined: the Burdigalian and Langhian stages of lower and middle Mio- (Ma) Chron Cycles Planktonic Foraminifera Benthic Calcareous Nannofossils Radiolarians NALMA MP European Mammals ALMA SALMA 0.0 0.5 1.0 1.5 2.0 0.0 0.5 1.0 1.5 2.0 2.5 Age (Stage) (Ma) During the Paleogene, the global climate, being warm (Stage) Northwestern Europe Mammals other zones Foraminifera ELMA R T low latitude southern high latitude until the late Eocene, shows a significant cooling trend cene.
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • Deep Sea Drilling Project Initial Reports Volume 6
    39. PLANKTONIC MICROFOSSIL BIOSTRATIGRAPHY OF THE NORTHWESTERN PACIFIC OCEAN David Bukry1, U.S. Geological Survey, La Jolla, California, Robert G. Douglas, Case Western Reserve University, Cleveland, Ohio, Stanley A. Kling, Cities Service Oil Company, Tulsa, Oklahoma, and Valeri Krasheninnikov, Academy of Sciences of the U.S.S.R., Moscow CONTENTS Page Page Introduction 1253 Regional Correlation 1281 Zonal Comparison 1254 Calcareous Nannoplankton 1281 Planktonic Foraminifera, Mesozoic 1281 Upper Cretaceous-Paleocene Boundary 1255 California 1281 Paleocene-Eocene Boundary 1259 Japan 1285 Eocene-Oligocene Boundary 1259 West Pacific 1286 Oligocene-Miocene Boundary 1259 Australia 1287 Miocene-Pliocene Boundary 1260 Planktonic Foraminifera, Cenozoic 1288 Pliocene-Pleistocene Boundary 1261 Solomon Islands 1288 Zonal Summary 1261 Mariana Islands 1288 The Philippines 1288 Paleoecology 1261 Taiwan 1289 Calcareous Nannoplankton 1261 Japan 1289 Radiolaria 1267 Kamchatka Penisula 1290 California 1290 Preservation 1267 Radiolaria 1291 Calcareous Nannoplankton 1267 Sedimentation Rates 1291 Foraminifera 1269 Relationship to Acoustostratigraphy 1294 Radiolaria 1279 References 1296 INTRODUCTION A comparison of zonal units of calcareous nannoplank- ton, foraminifera, and radiolarians in the same strata Biostratigraphic evidence obtained from the north- shows only few cases of exact coincidence of zonal western Pacific Ocean as a result of coring carried out limits, especially if coincidences at the top or bottom by the Glomar Challenger during Leg 6 of the Deep of the standard 9-meter coring runs are dismissed as Sea Drilling Project from Hawaii to Guam is considered artificially induced owing to gaps in sediment recovery. here mainly from the standpoint of three dominant Exact coincidence of zonal limits within coring runs marine planktonic microfossil groups—calcareous nan- are most notable for the Upper Paleocene sediment of noplankton, foraminifers, and radiolarians.
    [Show full text]
  • Interim Geologic Map of the Enoch Quadrangle, Iron County, Utah
    Interim Geologic Map of the Enoch Quadrangle, Iron County, Utah by Tyler R. Knudsen DISCLAIMER This open-file report makes information available to the public during the review and production period necessary for a formal UGS publication. The map may be incomplete, and inconsistencies, errors, and omissions have not been resolved. While the document is in the review process, it may not conform to UGS standards; therefore it may be premature for an individual or group to take actions based on its contents. Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. For use at 1:24,000 scale only. This geologic map was funded by the Utah Geological Survey and the U.S. Geological Survey, National Cooperative Geologic Mapping Program through USGS STATEMAP award numbers G11AC20249 and G12AC20226. The views and conclusions contained in this document are those of the author and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. OPEN-FILE REPORT 628 UTAH GEOLOGICAL SURVEY a division of Utah Department of Natural Resources 2014 MAP UNIT DESCRIPTIONS QUATERNARY Alluvial deposits Qal1 Stream deposits (Holocene) – Stratified, moderately to well-sorted gravel, sand, silt, and clay deposited in stream channels, floodplains, and man-made flood conveyance channels; includes small alluvial-fan and colluvial deposits, and minor terraces less than 10 feet (3 m) above modern base level; 0 to 30 feet (0–10 m) thick.
    [Show full text]
  • (Whitneyan) Rhinocerotid from Northeastern California
    Journal of Paleontology, 89(1), 2015, p. 135–139 Copyright © 2015, The Paleontological Society 0022-3360/15/0088-0906 doi: 10.1017/jpa.2014.11 A mid-Oligocene (Whitneyan) rhinocerotid from northeastern California Jen A. Bright,† Bruce H. Tiffney, and André R. Wyss Department of Earth Science, University of California – Santa Barbara, Santa Barbara, California 93106, USA; 〈[email protected]〉, 〈[email protected]〉 Abstract.—Rhinoceroses were important in North American mammal faunas from the late middle Eocene to the Miocene, but the group’s poor sampling outside the High Plains and eastern Rocky Mountain regions during their early evolution significantly hinders understanding of their biogeography. This limited geographic sampling is parti- cularly true of early–middle Oligocene time, with the vast majority of Whitneyan localities occurring in the White River Badlands of South Dakota. Thus, any rhinocerotid from outside the High Plains during this period is significant. We describe two new rhinocerotid specimens from the middle Oligocene Steamboat Formation of the northeastern Warner Mountains of California. Although the Steamboat Formation is well known for fossil plants, this is the first report of mammalian fossils from the area: an isolated lower molar recovered in 1974 but not previously described or illustrated, and a mandibular fragment recovered approximately 20 years later and bearing two molar teeth, most likely pertaining to the same taxon and horizon. The lack of distinctive morphological characters suggests both fossils be conservatively referred to Rhinocerotidae incertae sedis. Based on published tooth measurement data, Trigonias osborni represents the closest size match, but that species is currently only known from the Chadronian.
    [Show full text]
  • Aplodontid, Sciurid, Castorid, Zapodid and Geomyoid Rodents of the Rodent Hill Locality, Cypress Hills Formation, Southwest Saskatchewan
    APLODONTID, SCIURID, CASTORID, ZAPODID AND GEOMYOID RODENTS OF THE RODENT HILL LOCALITY, CYPRESS HILLS FORMATION, SOUTHWEST SASKATCHEWAN A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon By Sean D. Bell © Copyright Sean D. Bell, December 2004. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Master’s degree from the University of Saskatchewan, I agree that the libraries of the University of Saskatchewan may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professors who supervised my thesis work or, in their absence, by the Head of the Department of Geological Sciences or the Dean of the College of Graduate Studies and Research. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences 114 Science Place University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2 i ABSTRACT The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan.
    [Show full text]
  • 2014BOYDANDWELSH.Pdf
    Proceedings of the 10th Conference on Fossil Resources Rapid City, SD May 2014 Dakoterra Vol. 6:124–147 ARTICLE DESCRIPTION OF AN EARLIEST ORELLAN FAUNA FROM BADLANDS NATIONAL PARK, INTERIOR, SOUTH DAKOTA AND IMPLICATIONS FOR THE STRATIGRAPHIC POSITION OF THE BLOOM BASIN LIMESTONE BED CLINT A. BOYD1 AND ED WELSH2 1Department of Geology and Geologic Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota 57701 U.S.A., [email protected]; 2Division of Resource Management, Badlands National Park, Interior, South Dakota 57750 U.S.A., [email protected] ABSTRACT—Three new vertebrate localities are reported from within the Bloom Basin of the North Unit of Badlands National Park, Interior, South Dakota. These sites were discovered during paleontological surveys and monitoring of the park’s boundary fence construction activities. This report focuses on a new fauna recovered from one of these localities (BADL-LOC-0293) that is designated the Bloom Basin local fauna. This locality is situated approximately three meters below the Bloom Basin limestone bed, a geographically restricted strati- graphic unit only present within the Bloom Basin. Previous researchers have placed the Bloom Basin limestone bed at the contact between the Chadron and Brule formations. Given the unconformity known to occur between these formations in South Dakota, the recovery of a Chadronian (Late Eocene) fauna was expected from this locality. However, detailed collection and examination of fossils from BADL-LOC-0293 reveals an abundance of specimens referable to the characteristic Orellan taxa Hypertragulus calcaratus and Leptomeryx evansi. This fauna also includes new records for the taxa Adjidaumo lophatus and Brachygaulus, a biostratigraphic verifica- tion for the biochronologically ambiguous taxon Megaleptictis, and the possible presence of new leporid and hypertragulid taxa.
    [Show full text]
  • Alphabetical List
    LIST E - GEOLOGIC AGE (STRATIGRAPHIC) TERMS - ALPHABETICAL LIST Age Unit Broader Term Age Unit Broader Term Aalenian Middle Jurassic Brunhes Chron upper Quaternary Acadian Cambrian Bull Lake Glaciation upper Quaternary Acheulian Paleolithic Bunter Lower Triassic Adelaidean Proterozoic Burdigalian lower Miocene Aeronian Llandovery Calabrian lower Pleistocene Aftonian lower Pleistocene Callovian Middle Jurassic Akchagylian upper Pliocene Calymmian Mesoproterozoic Albian Lower Cretaceous Cambrian Paleozoic Aldanian Lower Cambrian Campanian Upper Cretaceous Alexandrian Lower Silurian Capitanian Guadalupian Algonkian Proterozoic Caradocian Upper Ordovician Allerod upper Weichselian Carboniferous Paleozoic Altonian lower Miocene Carixian Lower Jurassic Ancylus Lake lower Holocene Carnian Upper Triassic Anglian Quaternary Carpentarian Paleoproterozoic Anisian Middle Triassic Castlecliffian Pleistocene Aphebian Paleoproterozoic Cayugan Upper Silurian Aptian Lower Cretaceous Cenomanian Upper Cretaceous Aquitanian lower Miocene *Cenozoic Aragonian Miocene Central Polish Glaciation Pleistocene Archean Precambrian Chadronian upper Eocene Arenigian Lower Ordovician Chalcolithic Cenozoic Argovian Upper Jurassic Champlainian Middle Ordovician Arikareean Tertiary Changhsingian Lopingian Ariyalur Stage Upper Cretaceous Chattian upper Oligocene Artinskian Cisuralian Chazyan Middle Ordovician Asbian Lower Carboniferous Chesterian Upper Mississippian Ashgillian Upper Ordovician Cimmerian Pliocene Asselian Cisuralian Cincinnatian Upper Ordovician Astian upper
    [Show full text]
  • Geology and Vertebrate Paleontology of Western and Southern North America
    OF WESTERN AND SOUTHERN NORTH AMERICA OF WESTERN AND SOUTHERN NORTH PALEONTOLOGY GEOLOGY AND VERTEBRATE Geology and Vertebrate Paleontology of Western and Southern North America Edited By Xiaoming Wang and Lawrence G. Barnes Contributions in Honor of David P. Whistler WANG | BARNES 900 Exposition Boulevard Los Angeles, California 90007 Natural History Museum of Los Angeles County Science Series 41 May 28, 2008 Magnetic stratigraphy of the Eocene to Miocene Sespe and Vaqueros formations, Los Angeles and Orange counties, California Gino Calvano,1 Donald R. Prothero,2,3 Joshua Ludtke,4 and E. Bruce Lander1,3 ABSTRACT. The middle Eocene to lower Miocene age Sespe and Vaqueros formations in northern Orange County and northwestern Los Angeles County, California, USA, yield many important vertebrate and invertebrate fossils. These include Uintan (late middle Eocene) and Arikareean to Hemingfordian (late Oligocene to early Miocene) land mammals in the Sespe Formation, and important marine mammals (including the oldest sirenians and desmostylians in California and many early whales) and mollusks of the Turritella inezana Zone in the Vaqueros Formation. Paleomagnetic analyses of five important fossil-bearing sections in northern Orange County and one in Los Angeles County were undertaken to determine the age of these fossils and to supplement previous paleomagnetic studies of the Sespe and Vaqueros sequence. More than 225 samples were collected and subjected to both thermal and alternating field demagnetization. Although most samples had a slight chemical remanence overprint resulting from goethite, their characteristic remanence was held mostly in magnetite with little hematite (despite the red color of many rocks). Both normal and reversed polarities were documented and passed reversal tests, demonstrating that the overprints had been removed and a primary or characteristic remanence revealed.
    [Show full text]