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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. -
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 -
Distribution of the Native Trees of Utah Kimball S
Brigham Young University Science Bulletin, Biological Series Volume 11 | Number 3 Article 1 9-1970 Distribution of the native trees of Utah Kimball S. Erdman Department of Biology, Slippery Rock State College, Slippery Rock, Pennsylvania Follow this and additional works at: https://scholarsarchive.byu.edu/byuscib Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Erdman, Kimball S. (1970) "Distribution of the native trees of Utah," Brigham Young University Science Bulletin, Biological Series: Vol. 11 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/byuscib/vol11/iss3/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Brigham Young University Science Bulletin, Biological Series by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. MU3. CCy.P. ZOOL. LIBRARY DEC 41970 Brigham Young University HARVARD Science Bulletin UNIVERSITY) DISTRIBUTION OF THE NATIVE TREES OF UTAH by Kimball S. Erdman BIOLOGICAL SERIES—VOLUME XI, NUMBER 3 SEPTEMBER 1970 BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN BIOLOGICAL SERIES Editor: Stanley L. Welsh, Department of Botany, Brigham Young University, Provo, Utah Members of the Editorial Board: Tipton, Zoology Vernon J. Feeeon L. Anderson, Zoology Joseph R. Murdock, Botany WiLMER W. Tanner, Zoology Ex officio Members: A. Lester Allen, Dean, College of Biological and Agricultural Sciences Ernest L. Olson, Chairman, University Publications The Brigham Young University Science Bulletin, Biological Series, publishes acceptable papers, particularly large manuscripts, on all phases of biology. Separate numbers and back volumes can be purchased from Pubhcation Sales, Brigham Young University, Provo, Utah. -
A History of Juab County, Utah Centennial County History Series
A HISTORY OF fjuab County Pearl D. Wilson with June McNulty and David Hampshire UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF JuaB County Pearl D. Wilson with June McNulty and David Hampshire luab County, one of Utah's earliest created counties, sits along the strategic north-south corridor of the state. Prehistoric and Native American Indian cultures roamed there, as did early Spanish priests and explorers, who left an important record of the area. Trappers and traders wandered the mountains and deserts that create stark contrasts in this geo graphically diverse county. Mark Twain, an early traveler through parts of luab, penned interesting insights of the county, which contained portions of the Pony Express and Overland Stage routes. Mormon pioneers arrived to establish farms and ranches. This was followed by the build ing of railroads and mineral exploration. Rail traffic for a vast region centered in Nephi, labeled "Little Chicago." To the west, the Tintic Mining District rose as one of Utah's richest gold and silver mining areas, attract ing a more ethnically diverse population. From majestic Mount Nebo to streams and lakes and the vast sand dunes of west Juab, the county contains many recreational possibili ties. Juab County is rich in history, geogra phy, and tradition; this book tells its story. ISBN: 0-913738-20-4 A HISTORY OF Juab County A HISTORY OF ffuaB County Pearl D. Wilson with June McNulty and David Hampshire 1999 Utah State Historical Society Juab County Commission Copyright © 1999 by Juab County Commission -
Genus Hemicystites Hall, 1852 PI. :36, Fig. 8
194 .-\ S1TDY OF NORTH .HIERICAN EDRIOASTEROIDEA 'tlEMOIR 21 Text fig. :34. pl. 36, fig. 1·3. GSC 14680-5. Paratype of Isorophusella pleiadae (Sir;. The holotype is well preserved. Floorplates have been clair and Bolton) (1965, pl, 11, fig. 5, 6 J. 7 mm axial lost from ambulacrum III. which exposes the inner side of by 7.2 mm transverse diameter. the coverplates. A few floorplates are crushed in the other PI. :36, fig. 8. ambulacra. The oral frame is slightly abraded but not This specimen is only slightly disrupted, but lacks the disrupted. The anal structure lies to the right of center of floorplates of ambulacra II and IV. The theca has been interambulacrum 5 (left from the inner surface view J. more deeply etched than the others, and details are 01.. Etching has removed some surficial features, especially the scure. The oral frame and the hydropore structures an' smaller basal ridges of the distal rim plates. relatively well preserved, as is the anal area. GSC 14680-2. Paratype of lsorophusella pleiadae (Sin- clair and BoltonI (1965, pl. 11. fig. 4.5,6). 5.7 mm axial GSC 14680·6. Paratype of Isorophusella pleiadae (Sin .. by 6 mm transverse diameter. clair and Bolton) (1965, pI. 11, fig. 3, 5. 61. 6.1 mm axial PI. 36, fig. 5. by 6.2 mm transverse diameter. This individual, considerably smaller than the holotype, PI. 36. fig. 9. appears to retain thecal proportions characteristic of a In this specimen, ambulacra II and IV are missing sev- young adult. The ambulacral-interambulacral areas are eral f1oorplates, and those of I and III are poorly pre. -
Utah Forest Insect and Disease Conditons Report 2002-2004
Utah State University DigitalCommons@USU Quinney Natural Resources Research Library, The Bark Beetles, Fuels, and Fire Bibliography S.J. and Jessie E. 2005 Utah Forest Insect and Disease Conditons Report 2002-2004 K Matthews V DeBlander L Pederson P Mocettini D Halsey Follow this and additional works at: https://digitalcommons.usu.edu/barkbeetles Part of the Ecology and Evolutionary Biology Commons, Entomology Commons, Forest Biology Commons, Forest Management Commons, and the Wood Science and Pulp, Paper Technology Commons Recommended Citation Matthews, K., DeBlander, V., Pederson, L., Mocettini, P. and Halsey, D. (2005). Utah forest insect and disease conditons report 2002-2004. USDA Forest Service, State and Private Forestry, Forest Health Protection, Intermountain Region, R4-OFO-TR-05012, 58 pp. This Full Issue is brought to you for free and open access by the Quinney Natural Resources Research Library, S.J. and Jessie E. at DigitalCommons@USU. It has been accepted for inclusion in The Bark Beetles, Fuels, and Fire Bibliography by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. United States Department of Agriculture Forest Service Utah State and Private Forestry Forest Health Forest Insect and Disease Protection Intermountain Region Conditions Report R4-OFO-TR-05-12 2002 - 2004 State of Utah Department of Natural Resources Division of Forestry, Fire and State Lands Butterfly Lake, Mirror Lake Highway Darren Blackford, USFS. FOREST HEALTH SPECIALISTS Forest Health Protection -
Proceedings of the United States National Museum
PROCEEDINGS OF THE UNITED STATES NATIONAL MUSEUM issued iMiv\jA, vJ^l ^y '^* SMITHSONIAN INSTITUTION U. S. NATIONAL MUSEUM Vol. 87 Washington: 1939 No. 3068 THE HEDERELLOIDEA, A SUBORDER OF PALEOZOIC CYCLOSTOMATOUS BRYOZOA By Ray S. Bassler The middle and upper Paleozoic strata of North America contain many incrusting, tubular, corallike organisms usually classified as aberrant cyclostomatous Bryozoa. Hederella, Reptaria, and Hernodia are the best-known genera, each represented by a few previously described species some of which have been identified from such widely separated horizons and locaHties that their names have little strati- graphic significance. The care of large collections of these fossils accumulated in the United States National Museum during the past 30 years led me to take up their study and, in 1934,^ to propose the name Hederelloidea as a new order of the Cyclostomata, since the typical bryozoan ancestrula was observed in a number of the species. With the present-day recognition of the Cyclostomata as an order, the Hederelloidea becomes subordinal in rank. At present all the six known genera are classified under a single family—Reptariidae Simpson, 1897. The earliest known forms of cyclostomatous Bryozoa occur in the lowest Ordovician (Buftalo River series) of Arkansas, where several species of Crepipora LHrich, 1882, of the suborder Ceramoporoidea occur. This suborder expands rapidly, particularly in the Devonian and Mississippian periods, with the very abundant development of Fistalipora and its alfies, but so far as known becomes extinct with the close of the Paleozoic. In the Chazyan, following the Buffalo » Proc. Qeol. Soc. America for 1933, p. -
County Grants Easement to Transwest After Concerns Are Allayed
Serving East Juab County - A Nice Place To Live! Volume 117, No. 13 March 27, 2019 Single Copy Price $100 Water from aquifers in Nephi and Mona most likely mix underground By Myrna Trauntvein Times-News Correspondent Does the water from the aquifers in Nephi and Mona mix underground? It is likely that they do be- cause of data from a 1996 study entitled: “Hydrology and Simu- lation of Ground-Water Flow in Juab Valley, Juab County, Utah.” The study was filed with the State of Utah Department of Natural Resources as Techni- cal Publication No. 114 and was written by Susan A. Thi- ros, Bernard J. Stolp, Heidi K. Hadley and Judy I. Steiger and was prepared by the Unit- ed States Geological Survey in cooperation with the Central Utah Water Conservancy Dis- trict and the East Juab Water Conservancy District and is 113 pages long including maps and charts. MONA RESERVOIR ON THE FIRST DAY OF SPRING • This photo taken last Wednesday, the fi rst day of Spring, shows Mount Nebo in “Water discharging from a all it’s winter glory. refl ected in the water of Mona Reservoir as it fi lls during the runoff from this winter’s storms. Photo Mike Davis spring at Burraston Ponds is a mixture of about 70 percent ground water from a hypoth- esized flow path that extends Mona City offi cials want questions answered about down gradient from where Salt Creek enters Juab Valley and 30 percent from a hypothesized Houweling’s operations and plans for the future flow path from the base of the By Myrna Trauntvein man camp and not single fam- toes is projected to pay in the dressed. -
Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1976 Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan Charles Willard Cookman Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, Mineral Physics Commons, and the Sedimentology Commons Recommended Citation Cookman, Charles Willard, "Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan" (1976). Master's Theses. 614. https://scholarworks.wmich.edu/masters_theses/614 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. PETROLOGY OF THE ROCKPORT QUARRY LIMESTONE (MIDDLE DEVONIAN TRAVERSE GROUP) ALPENA, PRESQUE ISLE AND MONTMORENCY COUNTIES, MICHIGAN by Charles Willard Cookman A Thesis Submitted to the Faculty of the Graduate College in partial fulfillment of the Degree of the Master of Science Western Michigan University Kalamazoo, Michigan December 19 76 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT The basal unit of the dominantly carbonate Traverse Group, the Bell Shale, is gradationally overlain by the Rock- port Quarry Limestone which has a thickness of approximately 14 m. The Rockport Quarry Limestone is composed of a dark unrestricted marine subtidal organic-mud packstone facies, comprised of an algal-mat-bearing coral packstone subfacies and a shallower water crinoid-bryozoan grainstone subfacies; a shoal-forming stromatoporoid biolithite facies; and a la- goonal micrite facies comprised of a subtidal dense subfacies containing gastropods, ostracods, and calcispheres, and an intertidal to supratidal fenestral subfacies. -
Ground-Water Resources of Northern Juab Valley, Utah
UTAH STATE ENOI'NEER Technical Publication No. 11 GROUND-WATER RESOURCES OF NORTHERN JUAB VALLEY, UTAH by L. J. Bjorklund Hydrologist, U. S. Geological Survey Prepared by the U. S. Geological Survey in cooperation with The Utah State Engineer 1967 CONTENTS Page Abstract _ 7 Introduction 8 Purpose and scope of the investigation 8 Location, extent, and population of the area __ _ 8 Previous investigations___ 10 Methods of investigation __ 10 Well- and spring-numbering system 11 Acknowledgments __ 11 Physical setting _ 11 Physiography and drainage_______________ __ 11 Climate 13 Geology _ _ 15 Rocks exposed in the area __ 15 Selected geologic formations and their water-bearing properties 15 Rocks of Paleozoic age __ 15 Arapien Shale 17 Indianola Group _ _ 17 Rocks of Tertiary age 17 Valley fill 18 Generalized structure of the valley 19 Ground water_______________________________________ 19 Source and recharge __ _ 19 Infiltration from streams 19 Salt Creek 20 Other perennial streams __ 21 Ephemeral and intermittent streams . ... 22 Infiltration from irrigation systems and water applied to fields 22 Subsurface inflow 22 Potential artificial recharge 23 -1- CONTENTS - (Continued) Page Ground water (continued) Occurrence 24 The valley fill______________ 24 Water-table conditions 24 Artesian conditions_ __ 24 Perched water-table conditions __ 25 Quantity of water in the valley fill 25 Configuration of the water surface __ . 26 Fluctuations of water levels .. 2:7 Long-term fluctuations_____ ..__ .. .. .. 2:7 Seasonal fluctuations __ ...__ 30 Movement . ._ _ _ ...._.... .... __ .. 34 Aquifer tests .. .. .. 35 Discharge ._____ _ . _ .. __ .. __ .. 37 Wells _.__ _ . -
Smithsonian Miscellaneous Collections Volume 148, Number 2
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 2 ffifyarba S. attb Harg Bait* Halrntt THE BRACHIOPOD SUPERFAMILY STENOSCISMATACEA By RICHARD E. GRANT United States Geological Survey (Publication 4569) OS^. C/jp; CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION April 1, 1965 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 2 Barkis S. attb ifflan} Baux Maiwti Steward} iFunJn THE BRACHIOPOD SUPERFAMILY STENOSCISMATACEA By RICHARD E. GRANT United States Geological Survey (Publication 4569) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION April 1, 1965 CONNECTICUT PRINTERS, INC. HARTFORD, CONNECTICUT, U.S.A. CONTENTS Page Introduction 1 Type genus 2 Acknowledgments 3 External morphology 4 Size 4 Commissure 4 Plication 6 Costation 7 Stolidium 8 Delthyrium and deltidial plates 13 Internal morphology 14 Camarophorium 14 Spondylium 16 Musculature 18 Hinge plate and cardinal process 22 Crura 22 Lophophore 23 Pallial markings 23 Shell structure 25 Life habits 26 Phylogeny 29 Classification 33 Key 35 Systematics of superfamily Stenoscismatacea 37 Family Atriboniidae 37 Subfamily Atriboniinae 37 Subfamily Psilocamarinae 77 Family Stenoscismatidae 95 Subfamily Stenoscismatinae 95 Subfamily Torynechinae 152 Species doubtfully Stenoscismatacean 160 Genera no longer included in Stenoscismatacea 162 References cited 166 Explanations of plates 175 Index 187 ILLUSTRATIONS PLATES Exp™ Page 1. Atribonium 175 2. Atribonium 175 3. Atribonium 176 4. Sedenticellula, Septacamera, Camarophorinella 176 5. Sedenticellula 177 6. Cyrolexis 177 7. Cyclothyris, Camarophorina 177 8. Camerisma 178 9. Psilocamara, Coledium 178 10. Coledium 179 11. Coledium 179 12. Coledium 179 13. Coledium 180 14. Coledium 180 15. Coledium 180 16. Coledium 181 17. Coledium 181 18. Coledium 182 19. Stenoscisma 182 20. Stenoscisma 183 21. -
PROGRAMME, ABSTRACTS and AGM Papers
The Palaeontological Association 60th Annual Meeting 14th–17th December 2016 Université Claude Bernard Lyon 1 Lyon, France PROGRAMME, ABSTRACTS and AGM papers ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 60th Annual Meeting 14th–17th December 2016 Université Claude Bernard Lyon 1 Lyon, France The programme and abstracts for the 60th Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. Venue The Conference takes place at the Laënnec Campus, Domaine de la Buire, Université Claude Bernard Lyon 1 (Metro line D, station ‘Laënnec’; tram T2 or T5, stop ‘Ambroise Paré’) in the eastern part of Lyon. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. You should therefore present for only 12 minutes to allow time for questions and switching between speakers. We have a number of parallel sessions in adjacent theatres so timing is especially important. All of the lecture theatres have an A/V projector linked to a large screen. All presentations should be submitted on a memory stick and checked the day before they are scheduled. This is particularly relevant for Mac-based presentations as UCBL is PC-based. Poster presentations Poster boards will accommodate an A0-sized poster presented in portrait format only. Materials to affix your poster to the boards are available at the meeting. Travel grants to student members Students who have been awarded a PalAss travel grant should see the Executive Officer, Dr Jo Hellawell (e-mail <[email protected]>) to receive their reimbursement. Lyon Lyon (<www.onlylyon.com/en/visit-lyon.html>), capital of Gaul, is an ancient Roman city and a UNESCO World Heritage Site.