Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In

Total Page:16

File Type:pdf, Size:1020Kb

Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In Appendix 2 Radioisotopic ages used in GTS2020 M.D. SCHMITZ 1285 1286 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Quaternary À not compiled Neogene À not compiled Pliocene Miocene Paleogene Oligocene Chattian Pg36 biotite-rich layer; PAC- Pieve d’Accinelli section, 43 35040.41vN, Scaglia Cinerea Fm, 42.3 m above base of 26.57 0.02 0.04 206Pb/238U B2 northeastern Apennines, Italy 12 29034.16vE section Rupelian Pg35 Pg20 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 145.8 m above base 31.41 0.03 0.04 206Pb/238U 145.8, equivalent to GSSP), northeastern Apennines, Italy 12 28003.83vE of section MCA/84-3 Pg34 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 142.8 m above base 31.72 0.02 0.04 206Pb/238U 142.8 GSSP), northeastern Apennines, Italy 12 28003.83vE of section Eocene Priabonian Pg33 Pg19 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 14.7 m above base of 34.50 0.04 0.05 206Pb/238U 14.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-14.7 Italy Pg32 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.9 m above base of 34.68 0.04 0.06 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E section Italy Pg31 Pg18 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.7 m above base of 34.72 0.02 0.04 206Pb/238U 12.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-12.7 Italy Pg30 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Variegata Fm, 8.0 m above base 35.28 0.03 0.05 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E of section Italy Pg29 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Variegata Fm, 7.2 m above base 35.34 0.03 0.05 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E of section Italy Pg28 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Variegata Fm, 6.5 m above base 35.40 0.03 0.05 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E of section Italy Pg27 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Variegata Fm, 5.8 m above base 35.47 0.03 0.05 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E of section Italy Bartonian Lutetian Pg26 Pg17 Mission Valley ash, La Mesa, California B33N, 117W terrestrial facies of Mission Valley Fm 43.35 6 0.50 6 0.50 40Ar/39Ar SDSNH Loc. 3428 Pg25 Pg16 DSDP Hole 516F DSDP Hole 516F 30 16.590S, 46.24 6 0.50 6 0.50 40Ar/39Ar 35 17.100W Ypresian Pg24 Pg15 68-0-51, 3497; Blue Two-Ocean Plateau and Irish Rock B44N, 109W overlies Aycross Fm 48.41 6 0.21 6 0.21 40Ar/39Ar Point Marker ash locales, Absaroka volcanic province, western USA Pg23 Pg14 CP-1; Continental Peak Bridger Basin, western USA 42 16006.2vN, Bridger Fm 48.96 6 0.28 6 0.33 40Ar/39Ar tuff 108 4307.5vW Appendix 2 1287 Primary radioisotopic age details Zonal range assignment Biostratigraphy Reference clade zonation Zone Weighted mean age of 5 (of 8 with 2 older and 1 Plank. foraminifera; calc. upper Zone O5; lower upper Zone O5; lower NP25; magnetostratigraphic Sahy et al. (2017); Coccioni younger) single zircon crystal analyses, utilizing CA- nannoplankton NP25 control at top of Chron C9n.2n et al. (2008) TIMS and the ET535 spike. Weighted mean age of 6 (of 7 with 1 older) single Plank. foraminifera; calc. middle Zone O2; middle middle Zone O2; mid NP23; magnetostratigraphic Sahy et al. (2017); Coccioni zircon crystal analyses, utilizing CA-TIMS and the nannoplankton NP23 control at upper Chron 12r et al. (2008) ET535 spike. Weighted mean age of 4 (of 5 with 1 younger) single Plank. foraminifera; calc. middle Zone O2; middle middle Zone O2; mid NP23; magnetostratigraphic Sahy et al. (2017); Coccioni zircon crystal analyses, utilizing CA-TIMS and the nannoplankton NP23 control at upper Chron 12r et al. (2008) ET535 spike. Weighted mean age of 3 (of 7 with 4 older) single Plank. foraminifera; calc. lowermost NP21, lowermost NP21, lowermost CP16a; Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton lowermost CP16a magnetostratigraphic control in lower Chron 13r et al. (1991) ET535 spike. Weighted mean age of 3 (of 3) single zircon crystal Plank. foraminifera; calc. uppermost NP19/20, uppermost NP19/20, uppermost CP15b; Sahy et al. (2017); Odin analyses, utilizing CA-TIMS and the ET535 spike. nannoplankton uppermost CP15b magnetostratigraphic control near base of Chron 13r et al. (1991) Weighted mean age of 7 (of 10 with 3 older) single Plank. foraminifera; calc. uppermost NP19/20, uppermost NP19/20, uppermost CP15b; Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton uppermost CP15b magnetostratigraphic control near base of Chron 13r et al. (1991) ET535 spike. Weighted mean age of 7 (of 12 with 5 older) single Plank. foraminifera; calc. lower NP19/20, lower lower NP19/20, lower CP15b; magnetostratigraphic Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton CP15b control in C15r et al. (1991) ET535 spike. Weighted mean age of 5 (of 7 with 2 older) single Plank. foraminifera; calc. lower NP19/20, lower lower NP19/20, lower CP15b; magnetostratigraphic Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton CP15b control in C15r et al. (1991) ET535 spike. Weighted mean age of 6 (of 10 with 4 older) single Plank. foraminifera; calc. lower NP19/20, lower lower NP19/20, lower CP15b; magnetostratigraphic Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton CP15b control in C16n.1n et al. (1991) ET535 spike. Weighted mean age of 6 (of 9 with 3 older) single Plank. foraminifera; calc. lower NP19/20, lower lower NP19/20, lower CP15b; magnetostratigraphic Sahy et al. (2017); Odin zircon crystal analyses, utilizing CA-TIMS and the nannoplankton CP15b control in C16n.1n et al. (1991) ET535 spike. Laser fusion single-crystal sanidine analyses, originally Plank. foraminifera; calc. NP16, CP14a coccoliths Reticulofenestra umbilica (Levin) and Obradovich, unpublished calibrated to TCs 5 28.32 Ma; no analytical data nannoplankton Discoaster distinctus Martini; magnetostratigraphic data cited in Walsh et al. published. control (1996) Laser fusion of biotite and sanidine separates, no Plank. foraminifera; calc. NP15, CP10 NP15, CP10; magnetostratigraphic control Swisher and Montanari, in analytical data published. nannoplankton prep, cited in Berggren et al. (1995) (postscript) Weighted mean of multi-grain feldspar (46.8% of gas) magnetostratigraphy magnetostratigraphic control Hiza (1999); Flynn (1986) and multi-grain hornblende (98.7% of gas) incremental heating plateau ages, originally calibrated using FCs 5 27.84 Ma. Weighted mean age of 12 (of 16) laser fusion analyses magnetostratigraphy magnetostratigraphic control Smith et al. (2008); Clyde on small multi-grain aliquots of sanidine, using FCs as et al. (2001) fluence monitor. 1288 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Pg22 Pg15 GR-416; Sixth tuff Green River Basin, western USA 41 32031.1vN, uppermost Wilkins Peak Member, Green 49.69 6 0.05 6 0.07 206Pb/238U 109 28052.9vW River Fm Pg21 Pg3 Upper Willwood ash; Bighorn Basin, western USA 42 16006.2vN, Willwood Fm 52.93 6 0.23 6 0.23 40Ar/39Ar bed B 108 4307.5vW Pg20 Pg12 Ash-17 DSDP Site 550, north Atlantic 48 30.910N, 55.48 6 0.12 6 0.12 40Ar/39Ar 13 26.370W Pg19 Pg11 SB01-01 bentonite Longyearbyen section, Spitsbergen, B7809010vN, 10.9 m above base of the Gilsonryggen 55.785 6 0.034 6 0.075 206Pb/238U Svalbard Archipeligo 15 01038vE Member, Frysjaodden Fm, within the PETM carbon isotope excursion Paleocene Thanetian Selandian Pg18 Pg10 Belt Ash Southeast Polecat Bench section, 44 51.50N, Silver Coulee beds, Fort Union Fm 59.39 6 0.30 6 0.30 40Ar/39Ar northern Bighorn Basin, Wyoming, 108 45.10W USA Danian Pg17 volcanic tuff in Kiowa Kiowa core, Elbert County 39.35242N, 174.52 m below top of core; D1 sequence 64.52 6 0.03 6 0.08 206Pb/238U core, KJ08-17 Fairgrounds, Kiowa, Colorado 104.46642 W of fluvial/paludal sandstone, mudstone, and lignite beds Pg16 volcanic tuff in Kiowa Kiowa core, Elbert County 39.35242N, 179.26 m below top of core; D1 sequence 64.63 6 0.05 6 0.09 206Pb/238U core, KJ07-63 Fairgrounds, Kiowa, Colorado 104.46642 W of fluvial/paludal sandstone, mudstone, and lignite beds Pg15 U coal tephra Biscuit Butte locality, Garfield 47 29013.1vN, base of Lebo Member of the Fort Union 64.66 6 0.05 6 0.09 40Ar/39Ar County, eastern Montana 107 407.6vW Formation Pg14 V coal tephra Biscuit Butte locality, Garfield 47 29021.8vN, above the Farrand Channel, upper 64.84 6 0.05 6 0.09 40Ar/39Ar County, eastern Montana 107 4023.8vW Tulloch Member of the Fort Union Formation Pg13 W coal tephra Saddle Section locality, Garfield 47 30034.8vN, below the Farrand Channel, upper 64.91 6 0.05 6 0.10 40Ar/39Ar County, eastern Montana 107 4054.9vW Tulloch Member of the Fort Union Formation Pg12 X coal tephra McGuire Creek locality, McCone 47 37047.5vN, capping the Garbani Channel, upper 65.29 6 0.06 6 0.11 40Ar/39Ar County, eastern Montana 106 10012.4vW Tulloch Member of the Fort Union Formation Pg11 Y coal tephra Hell Hollow locality, Garfield 47.53472N,
Recommended publications
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R
    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
    [Show full text]
  • Understanding and Mapping Variability of the Niobrara Formation
    UNDERSTANDING AND MAPPING VARIABILITY OF THE NIOBRARA FORMATION ACROSS WATTENBERG FIELD, DENVER BASIN by Nicholas Matthies A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date________________ Signed:____________________________________ Nicholas Matthies Signed:____________________________________ Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date:_______________ Signed:____________________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Wattenberg Field has been a prolific producer of oil and gas since the 1970s, and a resurgence of activity in recent years in the Niobrara Formation has created the need for a detailed study of this area. This study focuses on mapping regional trends in stratigraphy, structure, and well log properties using digital well logs, 3D seismic data, and core X-ray diffraction data. Across Wattenberg, the Niobrara is divided into the Smoky Hill Member (made up of A Chalk, A Marl, B Chalk, B Marl, C Chalk, C Marl, and Basal Chalk/Marl) and the Fort Hays Limestone Member. Directly beneath the Niobrara, the Codell Sandstone is the uppermost part of the Carlile Formation. Stratigraphic trends in these units are primarily due to differential compaction and compensational sedimentation. The largest structural trend is a paleo-high that runs east-west to northeast-southwest across the middle of the field. It has a relief of about 100 ft, and is 20 mi wide. The A Chalk and A Marl show evidence of submarine erosion over this area. Faults mapped from 3D seismic data are consistent with previously published data on a proposed polygonal fault system in the Denver Basin.
    [Show full text]
  • Ron Blakey, Publications (Does Not Include Abstracts)
    Ron Blakey, Publications (does not include abstracts) The publications listed below were mainly produced during my tenure as a member of the Geology Department at Northern Arizona University. Those after 2009 represent ongoing research as Professor Emeritus. (PDF) – A PDF is available for this paper. Send me an email and I'll attach to return email Blakey, R.C., 1973, Stratigraphy and origin of the Moenkopi Formation of southeastern Utah: Mountain Geologist, vol. 10, no. 1, p. 1 17. Blakey, R.C., 1974, Stratigraphic and depositional analysis of the Moenkopi Formation, Southeastern Utah: Utah Geological Survey Bulletin 104, 81 p. Blakey, R.C., 1977, Petroliferous lithosomes in the Moenkopi Formation, Southern Utah: Utah Geology, vol. 4, no. 2, p. 67 84. Blakey, R.C., 1979, Oil impregnated carbonate rocks of the Timpoweap Member Moenkopi Formation, Hurricane Cliffs area, Utah and Arizona: Utah Geology, vol. 6, no. 1, p. 45 54. Blakey, R.C., 1979, Stratigraphy of the Supai Group (Pennsylvanian Permian), Mogollon Rim, Arizona: in Carboniferous Stratigraphy of the Grand Canyon Country, northern Arizona and southern Nevada, Field Trip No. 13, Ninth International Congress of Carboniferous Stratigraphy and Geology, p. 89 109. Blakey, R.C., 1979, Lower Permian stratigraphy of the southern Colorado Plateau: in Four Corners Geological Society, Guidebook to the Permian of the Colorado Plateau, p. 115 129. (PDF) Blakey, R.C., 1980, Pennsylvanian and Early Permian paleogeography, southern Colorado Plateau and vicinity: in Paleozoic Paleogeography of west central United States, Rocky Mountain Section, Society of Economic Paleontologists and Mineralogists, p. 239 258. Blakey, R.C., Peterson, F., Caputo, M.V., Geesaman, R., and Voorhees, B., 1983, Paleogeography of Middle Jurassic continental, shoreline, and shallow marine sedimentation, southern Utah: Mesozoic PaleogeogÂraphy of west central United States, Rocky Mountain Section of Society of Economic Paleontologists and Mineralogists (Symposium), p.
    [Show full text]
  • High-Resolution Correlation of the Upper Cretaceous Stratigraphy Between the Book Cliffs and the Western Henry Mountains Syncline, Utah, U.S.A
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 5-2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. Drew L. Seymour University of Nebraska, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Seymour, Drew L., "HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A." (2012). Dissertations & Theses in Earth and Atmospheric Sciences. 88. http://digitalcommons.unl.edu/geoscidiss/88 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. By Drew L. Seymour A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Christopher R. Fielding Lincoln, NE May, 2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH. U.S.A. Drew L. Seymour, M.S.
    [Show full text]
  • Abelisaurus Comahuensis 321 Acanthodiscus Sp. 60, 64
    Index Page numbers in italic denote figure. Page numbers in bold denote tables. Abelisaurus comahuensis 321 structure 45-50 Acanthodiscus sp. 60, 64 Andean Fold and Thrust Belt 37-53 Acantholissonia gerthi 61 tectonic evolution 50-53 aeolian facies tectonic framework 39 Huitrin Formation 145, 151-152, 157 Andes, Neuqu6n 2, 3, 5, 6 Troncoso Member 163-164, 167, 168 morphostructural units 38 aeolian systems, flooded 168, 169, 170, 172, stratigraphy 40 174-182 tectonic evolution, 15-32, 37-39, 51 Aeolosaurus 318 interaction with Neuqu6n Basin 29-30 Aetostreon 200, 305 Andes, topography 37 Afropollis 76 Andesaurus delgadoi 318, 320 Agrio Fold and Thrust Belt 3, 16, 18, 29, 30 andesite 21, 23, 26, 42, 44 development 41 anoxia see dysoxia-anoxia stratigraphy 39-40, 40, 42 Aphrodina 199 structure 39, 42-44, 47 Aphrodina quintucoensis 302 uplift Late Cretaceous 43-44 Aptea notialis 75 Agrio Formation Araucariacites australis 74, 75, 76 ammonite biostratigraphy 58, 61, 63, 65, 66, Araucarioxylon 95,273-276 67 arc morphostructural units 38 bedding cycles 232, 234-247 Arenicolites 193, 196 calcareous nannofossil biostratigraphy 68, 71, Argentiniceras noduliferum 62 72 biozone 58, 61 highstand systems tract 154 Asteriacites 90, 91,270 lithofacies 295,296, 297, 298-302 Asterosoma 86 92 marine facies 142-143, 144, 153 Auca Mahuida volcano 25, 30 organic facies 251-263 Aucasaurus garridoi 321 palaeoecology 310, 311,312 Auquilco evaporites 42 palaeoenvironment 309- 310, 311, Avil6 Member 141,253, 298 312-313 ammonites 66 palynomorph biostratigraphy 74,
    [Show full text]
  • PROGRAMME ABSTRACTS AGM Papers
    The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important.
    [Show full text]
  • Upper Cenomanian Foraminifers from the Southern Part of the San Juan Basin, New Mexico
    Upper Cenomanian Foraminifers from the Southern Part of the San Juan Basin, New Mexico U.S. GEOLOGICAL SURVEY BULLETIN 1808-N AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the U.S. Geological Survey Books and Open-File Reports Sales, Box 25286, Denver, CO 80225. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Tech­ Books of the U.S. Geological Survey are available over the niques of Water-Resources Investigations, Circulars, publications counter at the following U.S. Geological Survey offices, all of of general interest (such as leaflets, pamphlets, booklets), single which are authorized agents of the Superintendent of Documents. copies of periodicals (Earthquakes & Volcanoes. Preliminary De­ termination of Epicenters), and some miscellaneous reports, includ­ ANCHORAGE, Alaska-4230 University Dr., Rm.
    [Show full text]
  • Geology and Stratigraphy Column
    Capitol Reef National Park National Park Service U.S. Department of the Interior Geology “Geology knows no such word as forever.” —Wallace Stegner Capitol Reef National Park’s geologic story reveals a nearly complete set of Mesozoic-era sedimentary layers. For 200 million years, rock layers formed at or near sea level. About 75-35 million years ago tectonic forces uplifted them, forming the Waterpocket Fold. Forces of erosion have been sculpting this spectacular landscape ever since. Deposition If you could travel in time and visit Capitol Visiting Capitol Reef 180 million years ago, Reef 245 million years ago, you would not when the Navajo Sandstone was deposited, recognize the landscape. Imagine a coastal you would have been surrounded by a giant park, with beaches and tidal flats; the water sand sea, the largest in Earth’s history. In this moves in and out gently, shaping ripple marks hot, dry climate, wind blew over sand dunes, in the wet sand. This is the environment creating large, sweeping crossbeds now in which the sediments of the Moenkopi preserved in the sandstone of Capitol Dome Formation were deposited. and Fern’s Nipple. Now jump ahead 20 million years, to 225 All the sedimentary rock layers were laid million years ago. The tidal flats are gone and down at or near sea level. Younger layers were the climate supports a tropical jungle, filled deposited on top of older layers. The Moenkopi with swamps, primitive trees, and giant ferns. is the oldest layer visible from the visitor center, The water is stagnant and a humid breeze with the younger Chinle Formation above it.
    [Show full text]
  • Geology of the Shepton Mallet Area (Somerset)
    Geology of the Shepton Mallet area (Somerset) Integrated Geological Surveys (South) Internal Report IR/03/94 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/00 Geology of the Shepton Mallet area (Somerset) C R Bristow and D T Donovan Contributor H C Ivimey-Cook (Jurassic biostratigraphy) The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Somerset, Jurassic. Subject index Bibliographical reference BRISTOW, C R and DONOVAN, D T. 2003. Geology of the Shepton Mallet area (Somerset). British Geological Survey Internal Report, IR/03/00. 52pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects.
    [Show full text]
  • Phylogeny, Diversity, and Ecology of the Ammonoid Superfamily Acanthoceratoidea Through the Cenomanian and Turonian
    PHYLOGENY, DIVERSITY, AND ECOLOGY OF THE AMMONOID SUPERFAMILY ACANTHOCERATOIDEA THROUGH THE CENOMANIAN AND TURONIAN DAVID A.A. MERTZ A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2017 Committee: Margaret Yacobucci, Advisor Andrew Gregory Keith Mann © 2017 David Mertz All Rights Reserved iii ABSTRACT Margaret Yacobucci Both increased extinction and decreased origination, caused by rising oceanic anoxia and decreased provincialism, respectively, have been proposed as the cause of the Cenomanian Turonian (C/T) extinction event for ammonoids. Conflicting evidence exists for whether diversity actually dropped across the C/T. This study used the ammonoid superfamily Acanthoceratoidea as a proxy for ammonoids as a whole, particularly focusing on genera found in the Western Interior Seaway (WIS) of North America, including Texas. Ultimately, this study set out to determine 1) whether standing diversity decreased across the C/T boundary in the WIS, 2) whether decreased speciation or increased extinction in ammonoids led to a drop in diversity in the C/T extinction event, 3) how ecology of acanthoceratoid genera changed in relation to the C/T extinction event, and 4) whether these ecological changes indicate rising anoxia as the cause of the extinction. In answering these questions, three phylogenetic analyses were run that recovered the families Acanthoceratidae, Collignoniceratidae, and Vascoceratidae. Pseudotissotiidae was not recovered at all, while Coilopoceratidae was recovered but reclassified as a subfamily of Vascoceratidae. Seven genera were reclassified into new families and one genus into a new subfamily. After calibrating the trees with stratigraphy, I was able to determine that standing diversity dropped modestly across the C/T boundary and the Early/Middle Turonian boundary.
    [Show full text]
  • Catalog of Type Specimens of Invertebrate Fossils: Cono- Donta
    % {I V 0> % rF h y Catalog of Type Specimens Compiled Frederick J. Collier of Invertebrate Fossils: Conodonta SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 9 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti­ tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com­ mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of profes­ sional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These publications are distributed by mailing lists to libraries, laboratories, and other in­ terested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available.
    [Show full text]
  • Records from the Aalenian–Bajocian of Patagonia (Argentina): an Overview
    Geol. Mag.: page 1 of 11. c Cambridge University Press 2013 1 doi:10.1017/S0016756813000058 Ophthalmosaurian (Ichthyosauria) records from the Aalenian–Bajocian of Patagonia (Argentina): an overview ∗ MARTA S. FERNÁNDEZ † & MARIANELLA TALEVI‡ ∗ División Palaeontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina. CONICET ‡Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, 8332 General Roca, Río Negro, Argentina. CONICET (Received 12 September 2012; accepted 11 January 2013) Abstract – The oldest ophthalmosaurian records worldwide have been recovered from the Aalenian– Bajocian boundary of the Neuquén Basin in Central-West Argentina (Mendoza and Neuquén provinces). Although scarce, they document a poorly known period in the evolutionary history of parvipelvian ichthyosaurs. In this contribution we present updated information on these fossils, including a phylogenetic analysis, and a redescription of ‘Stenopterygius grandis’ Cabrera, 1939. Patagonian ichthyosaur occurrences indicate that during the Bajocian the Neuquén Basin palaeogulf, on the southern margins of the Palaeopacific Ocean, was inhabited by at least three morphologically discrete taxa: the slender Stenopterygius cayi, robust ophthalmosaurian Mollesaurus periallus and another indeterminate ichthyosaurian. Rib bone tissue structure indicates that rib cages of Bajocian ichthyosaurs included forms with dense rib microstructure (Mollesaurus) and forms with an ‘osteoporotic-like’ pattern (Stenopterygius cayi). Keywords: Mollesaurus,‘Stenopterygius grandis’, Middle Jurassic, Neuquén Basin, Argentina. 1. Introduction all Callovian and post-Callovian ichthyosaurs, two different Early Jurassic taxa have been proposed as Ichthyosaurs were one of the main predators in the ophthalmosaurian sister taxa: Stenopterygius (Maisch oceans all over the world during most of the Mesozoic & Matzke, 2000; Sander, 2000; Druckenmiller & (Massare, 1987).
    [Show full text]