DOCSLIB.ORG

Interim Geologic Map of the Durst Mountain Quadrangle, Morgan and Weber Counties, Utah

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Interim Geologic Map of the Durst Mountain Quadrangle, Morgan and Weber Counties, Utah Utah Geological Survey, a division of Open-File Report 498 Utah Department of Natural Resources Interim Geologic Map of the in cooperation with U.S. Geological Survey Durst Mountain 7.5' Quadrangle T Cou S 85 Qc 68 51 23 37 Keh Qmc 70 U Keh Qc Qmc Zi Keh Qms Qms Tw Qms Qal R Qac Qac Qmc Cm Qdlb Qmc Keh Qmc Qmc Qms Qms Qmc H Zkc 48 26 Keh Qmc Tw 78 Cm T Zm 2 Qmc Qac Zcc Keh Keh Tw Qmc Qmc Qms 66 D Qmc 40 44 37 Keh Qac R Qmc Qms 88 Qms(TK) Qms Qat2 Cm A Tw Qa2? Tw L Keh Qmc Qmc Qmc L 42 6 Tw B I 7 Tw Qmc Qms?(Tw) Qa Qafo Cn Zkc Keh Qafy Qmc W Qmc Qmc Qmc Tw Qmc Qal Qdlb 70 10 Qao Cn Qac Qc Qms Qal Qmc Cn Qms Qac 39 Qms Qal2 Qlg? Qmc Qmc Qmc Qmc Qmc Qms Qla/Qms Keh Qmc Qmc Qc Qms Qmc Ql Qc 15 Qms Qlg 15 27 Qmc Qms Qal Qac Qac Qms Qmc Qmc Qmc Ql/Qms Qms Keh Tw Qmc Qmc Qac Qaf Qmc Keh 12 Tw Keh 54 Tw Tw Qms Qms Qms Qac Qao Qafy Qc Qms Qmc Qa Qms?(Tw) Qay Ql Qms Qmc 7 Qmc Qal2 Qmc Tw Qafy Qla Qmso?(Tw) Qmc Tcg Ql Qms Qmc Qla 5 Tw Qmc Qay Qay Keh Qmc Tw Qmc Qmc Qmc Tw Keh Tw Ql/Tcg Qmc Qmc 4 Qc Ql/Tcg 5 Qmc Qafy Qla Ql Keh Qmc Qac Qms Qafy Qmc Qmc Qac Qafy 5 Qac Tcg Keh 34 Tw 5 4 Qac Ql/Tcg Ql Qla Tw Qms Qmc Qmdf Qms Qh Qmc 5 Keh 2 Qmc Qmc Qms Qafy Keh Qmc Tw Qac Qms Ql Ql 2 Qa2 Qmc Qc Qa2? Qac Qmc Qms Qmc Ql/Tcg B 4 Tw Tw Ql/Tcg Keh Qmc Keh Qmc Tcg Ql Qafy Qmc 84 Qmc Qmc 10 7 Qmdf Qc B Tcg Qla Jn Qmc Keh Qmc Tcg Qlg? 11 Keh 21 Tw Tw Qms? B X B Jn Keh 2 Tw Keh? Qa Qc Qms Qmc Qms?(Tcg) Qc 64 Qms Qla Ql Qmc Keh Qmc Tw Qmdf Qac Keh? Qac Qac 28 Keh B Keh? Qmc Qc Qmc Qms Tcg Qdlb Jn 25 Qac Qmc Qc Qmc Qmc Qab? Qms Qac Qafp? B 12 Qay Keh Qms Qla 53 16 Keh Qc Qng Qms Qmc Qmc Keh Qap? Tw Qc Qmc Qmc X Jn Keh Qms Qc Qcg 8 Qmc/Qa 2 2 Qmc Ql? Jn Qfdb Keh? Qmc Tw Qc 31 34 Qc Qafp? Qc Qmc Qc Qmc B 22 Qmc Qac Ql/Thv Keh Qap? 2 Qmc Tw Qms Qdlb Qcg Qa Qac Qc Qms(Tcg) Qdlb? Keh? Qmc Qmc Qmso Qms Keh Tw Qms 3 Qc Qc Qafy Thv Qap? Qms Qc Qla? Qmc Qmc Qc Qms Qac B Keh Qmc Qmc Qc Qmc Qms Qac TRt 46 Qmc 15 Qms Tcg Jn 78 Qmc Qcg Tcg Tcg Qms Keh Qmc/Qap Qac Qac Qmc Qmc Qmc Qms Qc Qac 4 Tw Qms Qal Qmc Qmso Qafy Qac TRa Qms?(Tw) Qc Qfdb Qaf Thv Qmso Qmc Qms Qms?(Tcg) Qms?(Tcg) Qms Qcg Qap Qmc Qmc Qmc B Qmc Qc Qms?(Tcw?) B Qa 22 Qms Qac Qmc Qms 42 Qcg Qmc Qmc Keh Qap Qcg Qc 2 Qmc TRt Qaf Qmc Qc Qmc Qmc Qms 17 Qmc 1 Qmc Qms Thv 16 6 Tcg Qms Qfdb Qmc Qac Qmc 46 Keh 0.5 Qms B Qmc 3 Qmc 14 13 Qaf TRt Keh 16 Qmc 3 Qmc Qc 29 Qc Qa Qac Tcg Qms Thv Qap Keh Qms Qmc TRt Qmc Qmc Qc Qay 3 Qafo Qmc 2 Qmc Qmc 23 Thv Qms BENNETT CREEK THRUST Qap Qaf Qmc 2 Pp Qms Qac Qac Qmc 2 Tcg 19 Tcg Qmc Tcg Qmc Qab? Qmc Qcg Qac 4 18 Qms Qms?(Ts) Qms Qmc 41 Qms Qcg Qac Qmc 6 Qms Thv Mhu Qms Qms Qmc 3 Tcg Qms Tcw Qmdf Qmc Qac Qmc Thv Qmc Qms Qmc 46 10 Qms 4 Qms 43 35 Qms 59 Keh Keh 11 Tw 15 Qms Keh Keh Qmc Qmc Keh Qc Qac Qmc Tcg Qc Qc Thv 21 Mhl Mdl Qac Qmc Qac Qc Qms Qms?(Tcg) Qac Qms Qc Qmc Mde Mdu Qmso Mdl Qmc Qmc Qmc Qmc Qmc Qac Qms Qmc 27 Qmc Qc Qc Qc Qmc Qmc Qms Qms Qng Keh 26 8 Qmc Tcw Qmdf 26 20 44 Qc Qao 31 Qc Qay Qms?(Tcg) 22 Mdl Keh 2 Qmc Qmc Mhu Qmc Tcg 12 Qmc Qms Qmc Qab Qab? Qmc Tcw 35 25 Qc Qmc Qms Qmc Tcg Thv Mde Qmc Qao Qmc Qmc Qc Qc Qmc Qmc 36 55 Tw? Qa Qms Qmso Tcg Thv 11 Qmc Qmc Qap Tw? Qms 1 Qmc Qac Qafb? 25 Keh Qms Qcg Mdu Qc Qmc Qafb? Ml Qc Qa Qap Qmc Cm Qms Qmc Qmc Cn Mde 36 37 Qmc Qmc Tcw 26 Qms 19 Qa/Tw? Qmc 25 26 Qmc Mdl Keh Qc 22 Qmc Cm 40 Ml 20 9 Tw Tw Tcg Tcg Qms?(Tcg) 46 Mhl Qafy Qa/Tw? Tw Qms Qmc 44 Thv Qay? Qmc Qmc 70 Qafy 55 70 Qa Qmc Tw Qmc Qmc Qmc Qms?(Tcg) Qms Qms Mde Qap Qmc/Qa Qc Tw Qmc Qms 50 Qms/Qafb? Qms 35 Qa 29 Qmc Qms Qmc Qmc/Qa Qms?(Tcg) Qmc Qms 28 Qal Qmc Tcg Qmc Ml Qmc Qms Qmc/Qafo? 3 Qmc Qmc 29 Qac Qms Qmdf Qms Qmc Qab? Cm 45 Qap Qac Tcg Cn Qms 35 Qmc Tcw Qmc Qmc 2 Tw Tw Qms Qmc Qmc 12 Qa Qa Qmc Tcg Qmc 18 Cm Dwc 14 Qac Qac Qmc Qms Keh Keh? Qms?(Tcg) Qmc Ml Qmc Tw? Qac 29 Qmc wm Tcw Tcw Qms Dh Qmc Tcg Qmc 33 Mhu Qay Qmc Qms Tw Qmso? Thv? 42 Qms Qac 6 Qmc Qc Qms?(Tcg) Qms 12 Qaf Mdl? 11 Qmc Tw Qmc (Tcg) Qms 29 Qms Qmc Tcw 3 19 Qc Mhl 55 31 Qap Qaf 1 pimple mounds Tw Qmc Tcy? 10 Qmc Mde Qmc 2 Qmc 3 86 3 Qmc Qms?(Tcg) 7 Qc Keh Qmc Qc Qaf Qa 35 Qmc Qmc Qmc Tcy? Ml Qafy Qmc Qms Qmc Tcw Qaf Qmc 8 Qmc Qmc Qc Qc 30 Qap Qms Qms Qa 10 Thv Ml Qa Qafp 2 Qms Dh Qap Qmc Qc Qms Qms Qmc Qms?(Keh) Tcg Tcg 24 Qms Thv Db Tw Tn Thv Qmc 3 Qmc 21 37 Qaf Qng Qay Qac Qms?(Tcg) Qac Qms Thv? Qay Qafy Qc Keh pimple mounds Qa Qmc Qc Qms Qmc Qmdf Qmc Qc Qac Dh Ml Qmc Tn Qmc 33 Qms Tw Qmc Qc Tcg 26 Qac Qms Qaf Qms Qafp Tw Qms Dwc Qms 21 Qac Qmc Qms Dh Qms Qay Qc Qac Qms?(Tcg) Qms Qms Qa Ts Ml Qc 28 Tcg Qaf Qmc Tw Qmc Tcw TRd TRw 21 Qmc Ts 44 37 Ppm Qms Tw Qc 34 Qac PIPwl Qmc 8 Qms?(Tw) pimple mounds Qc stone stripes? 36 Qmc Db Qmc 42 Qac 10 9 Qms Keh Tw Tcw Ml Qa2 42 Qms Qms Ppf Qmc Qms Thv Ts/Ml 70 Keh Qmc Qc Tcg Qmc QaQao? 4 Tw Qmc Qcg Pwu 32 43 Qms TRd Qms 12 Ts 74 Qc Qmc 24 Qms Ppg Qc Qao Qc Qc Tn Qmc Tcy? Qms Qay 9 Tcg Qmc Dh PIPwl Ppm 33 Qmc 30 29 Qaf Keh Qac Qmc Tcg Qmso 54 Qmc Qmc pimple mounds Qmc 25 36 Qmc 3 41 N 35 66 Qms?(Pp) Qmc Qmc stone stripes? O Dh Tcg Tcw R 9 18 Qa Qmc Qafo? Tn wm? M Qc Keh Qmc Qc Qc Qac A Ts 37 Qms Tw Qmc Qms?(Tcw) L TRd Qmc F Qms A Db 14 Qms 29 U Qc 2 Qac Qmc L Qaf Qc Qms Tn Qcg T 38 Tn Qms Qmc Qc ? Qac Ml 44 Qms Qaf Pwu 25 22 Qms Ppf 19 Qms Tcg Qmc Ppg Tw Tn Tcg Qms?(Tcw) Ppm 23 Qms Dh Db Ppm Keh 30 Qafo PIPwl 13 21 Qmc Qms Qms Ppg 4 Qcg Dwc 20 Tw Qmc 24 Qmc Qms Pwu Qac Tn Qc Qmc Qmc Qms?(Tcg) Qms Dh Ml Qms Qmc Qmc Qac Qmc 32 Qmc Dh Qa Pwu Keh Tcg Dwc? Dh Db Qmc Dh Qmc Qap? Qmc 33 Qms Db Db Qmc Qmc Tcg Dwc? Dwc Db 62 Qms Qmc Qms Tw 23 Qmc Qmdf Ct 28 48 Qac Qac Db Qac Qac Tca Ts Db Qac Qms Qmc Qap? Tcg 26 33 Tca 75 63 Dh Tcg Tcw? Qms 7 Qmc Qac 31 Qmc Ts Dh 63 Cn Dh Keh Qms Qac Qmso Qmc Qmso Tcw Qms?(Tcw) 27 58 35 75 Ml Keh Qmc Dh Mhl Keh C Tn Cn 2 O Qmc Tca? Ts Dwc N wm? Qmc Cm 54 Cn 2 C Qms?(Tcg) Tcy? 13 Db E Qms?(Ts) Ts 32 25 Cm 57 64 Qms A Qac Tn Qmc Qmc 39 68 Qms LE Qmc Qmc Qmc Qms?(Tct) 14 18 Dh D Qmc Qms Cou 49 56 Cn TK? Qmc W Tcg Qms Qmc 19 Qmso Qmc Tcg Ml 23 Mde Tw IL LA 24 Qmc Qms Qmc 30 Com Cm Keh R Tn Qmc Qms Tcw D Qac Qmso Qc Qms Qac Col 44 T Qms 26 Tca? 17 37 55 41 H Qmc 37 45 42 60 R 28 Tca Tct Qms Col Db Qac Mdd U Qac Tcg 23 Com Cou S Qmc 21 Tcw Tcy? 52 72 T Qmc Ct 58 Db Qmc Tw Tcg Qc Tcg Tcg Tct Qmc 52 Ml Qac 5 Qmso Tcg Tcg Qng 44 71 Qac 26 Qms Qmc Qmso?(Tcg) Qmc Tct Qa 52 Col 62 Mhl Tcg Qmc Qms Qc Qac Qmc Tcg 34 Qms 59 Qms Qac Tcg Tca Qmc Ct 62 Qmc Qmc Qmc 7 73 Tcg 19 Tcw? Qmc 53 Tct Col Qms 57 28 11 Qmc Qac 18 Tcg Tcg 26 Tct 87 Qmc 66 Qc Tcg Qmc Qmdf Ct 86 Mhl Qc 20 30 Qng Qafy Qmc 85 Qmc Qc Tcg Qmc Ct Qa Tw Tcg Tcg 20 Qmc Qng 88 62 Qms Qms Qc Qmc Tcg Qc 57 Keh Qmc Qmc 50 53 63 26 Qmc 54 Db 21 28 Tcg Tct Tct 14 54 Mhl Qmc/Qatp Tn Tcg 30 Tct Qms Col Mde Qafo Qac Tn Tn Qms Qmc 11Qmc Ct 55 37 Qmc 30 25 Qmc Tca 23 Qmc Qmc/Qatp Tcg Tcg Tcg Qms?(Tcg) Qc 37 64 Qaf1 63 Qms?(Tcw) Qms Qmc Tct 8 Tct Cou Db Ml 24 Qms Qc Tn 33 Xf? 45 3 Keh Qms Qac 23 Qmc 18 Qafoe Qatp Qmc 21 Qac 31 Tcy? Qms 49 Mde Qmc Ct 21 Tct Qmc 67 Keh Tcg Tcg Tcw 26 18 22 55 Qms 25 Qal Qafy Qafo Qms Qmc Qafo Tn Tn 36 Qms 70 52 Dh 7 Keh Keh Qc Qac Qafo Tct Qmc Keh Qaf1 Keh Qab Tn Tcw Qmc Qms(Tct) Qng Qmc Db Ml Qmc Qaf1 Qmc Qatp Tw? Qac Tcw Xf 54 70 Keh Tcw 6 81 Dwc Qac Qmc Qac Tn Qms?(Tcg?) 7 Qms Mde Qc Qmc 24 Xf 72 Qac 4 Tw Qmso Qc Xf Cn Dh Db Qaf1 Qat2 Tw Tw Qc 27 Tcw Qac Qmc Tct 47 Qmc Qmc Tn Tct 41 69 75 Qmc Qmc Qms Tw Qms Qmc Qafo 21 40 Qms Cm Qmc Qmc Keh Qms Tw Qmso Qac Qms Tcw Qms(Xf) 81 Qaf1 Keh Tct Cou Dh Db Tw 12 29 Tcw 53 Qmc Ml Qms?(Tn) Qms?(Tn) 43 Qms(Xf) Qms Qmc Qaf1 Qms Tn Tw Xf Dwc Qa? 26 Tw Qmc Qmc Tcw Qms?(Xf) Xf Com Qat2 Qmc Qmso?(Tn) Tn Qc Tw? Qmc Col Cm Dh Qmc Qal Qafo Qms Qms Tct Keh Qa Qmc Qmc Qac Qafoe? Qmc Qms Qmso Qmt Cn 72 Qc Qac Tcg? Qmc Qc Qafo Qato Qmc 20 Xf Ct Cm Dwc Keh Qc/QTao/ Qmc Qms Tcg? 79 Qac Qmso 43 Qms?(Tw?) Xf Xf Qac 3 QTay? Tw Qafo Com Cn 29 Tw Qmc 28 Tw Qaf Qmc Qms 12 15 Tw? Qms Ct Cou Cm Qmc Qafy Qms Qms Tw Qmc Xf Qal2 Keh Qmso?(Tn) Tw Qaoe? Col QTay? Tn Qc Qng/Xf Tw Qmc Qao Qaf1 Qmso Tn 45 Qms?(Tw) 85 Qafy Qac 7 Qmc Xf Qafy Qms Qac Qafo 50 Qms Qms Qc Qmt Ct Xf Qmc Qac Qac 44 51 79 Qmc Qms?(Keh) Tn 45 24 42 Qms Qmc 84 Qmc Qac Qmc Qaoe 55 Qao Qms Ct Qmt Tw Qaoe Ct Qafb Qafy Qao? Db Qmc Qms Qms Ct Qa Qaf 88 Qmc Qab Qmso Qac Cou Qac Qms Qac 35 88 Qmc/Qaoe Keh Qms Qac 77 34 Qafy Qatp Xf Qmc Qms Com Qafo Qafy Qmc Qa Qao? 64 Qmc/QTa Qac Qab Qal Cm or Com Qms Qmc 79 Qms Keh Tw Qaf Qms 7 Qmc Qms Qafy Qafy Qaf Qafy Ct 87 Col Qmc Qap? 8 Qc Qmc Xf Qms Xfpg 60 Qmdf 72 Ml Qms Tw Qafo Qmc Xf 73 Qmc/Qap? Qmc Qafy QmXsf Xf Qms Qms Qmsy Qafy Qms Qaf 88 Qmc/Qat Qmc 81 Qmc Qms1 Qafy Qmc 26 Qms 38 Qmc Qms?(Tn) Qaoe? Qmsy Qms Xf Dh Db O Qms Qms Xf Qms Qms G Qmc Xf Qms?(Xf) Com 71 Qafb? Qat2 D 10 83 43 70 74 Dwc E Qms Qms Keh Qac Qms N Qms Xf Xf QTay? 71 Cn Qab Qal Qms Qms 81 23 Qat Qmc 75 Qmc Qdlb 43 Qms 40 Cou Qmc Qmc Qafy Xf Qac Qmc Cm Qmc Qdlb Tcg? Qmc Tcg 41 Qms Qms(Xf) Qmrf Col QTay Tw Qab Qmc Qmc 26 Qmc Tw Qms RO 60 Cm? 52 Tcg O Qms Qmc Qmc Ct 68 62 Qmc Tcg Qms F Qac 60 86T Xf 68 Qms(Xf) Qms Qafy 6 Qmc Xf H Qms Qms?(Xf) Xf Qmc Qms RU Qms 10 S Qms Qms?(Xf) Qms Qmc Qms 83 65 34 55 Qc 7 Qms T 42 75 Qfdb Tcy? Xf Qmc Qmc Qms Tcg Qmc Qms Col Cou Qmc Ct Tcg? Xf 80 32 Qms Xf 53 50 Qmc/QTay? Qafy Qmc Tcy? Qms Xf 82 2 Tw Xf Xf Qms 61 Qdlb Qms Qms Qms 69 80 50 14 Qmc Qac Xf Qms Qms Col Qms?(Ts) 6 76 Qmc 77 Ct Keh Qmc Tcg 5 Qms?(Xf) Qms(Xf) Qms 59 Tcg? Ct Qac Cm 75 Keh 12 Tw 57 Qms Qms?(Xf) 73 Qmdf Qmc Qao 13 82 40 Qms Qms 60 Qmc Tcy? Qms Ct 64 77 Qms Qmc Xf 72 55 73 46 89 Qaf1 Thv Qms Qms 78 45 Col 70 Keh Qmc 40 Qms Qms Qmso(Xf) 36 Qmc 76 Qms Qms Qms 75 Qmc QTay? 2 Thv Qms Qms Qmc Xf 70 45 Col 70 Qms?(Keh) Qms Qmc Qmc Tcg 8 58 54 Cm 69 78 59 Mde Keh Qms Qms Ct 73 Tcg Qc Qms?(Ts) Thv? Qmc Qms Cn Tw Tcg Thv Qac Thv Qmc Cou Qafy Tcy? 59 82
Load more

Recommended publications
  • The World at the Time of Messel: Conference Volume
    T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203.
    [Show full text]
  • The Paromomyidae (Primates, Mammalia): Systematics, Evolution, and Ecology
    The Paromomyidae (Primates, Mammalia): Systematics, Evolution, and Ecology by Sergi López-Torres A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Department of Anthropology University of Toronto © Copyright by Sergi López-Torres 2017 The Paromomyidae (Primates, Mammalia): Systematics, Evolution, and Ecology Sergi López-Torres Doctor of Philosophy Department of Anthropology University of Toronto 2017 Abstract Plesiadapiforms represent the first radiation of Primates, appearing near the Cretaceous- Paleogene boundary. Eleven families of plesiadapiforms are recognized, including the Paromomyidae. Questions surrounding this family explored in this thesis include its pattern of extinction, its phylogeny and migration, and its dietary ecology. Firstly, there is a record of misclassifying small-sized omomyoid euprimates as late-occurring paromomyid plesiadapiforms. Here, a new omomyoid from the Uintan of California is described. This material was previously thought to pertain to a paromomyid, similar to previously named supposed paromomyids Phenacolemur shifrae and Ignacius mcgrewi. The new Californian species, Ph. shifrae, and I. mcgrewi are transferred to Trogolemurini, a tribe of omomyoids. The implications of this taxonomic change are that no paromomyids are found between the early Bridgerian and the Chadronian, suggesting that the group suffered near-extinction during a period of particularly warm climate. Secondly, migration of paromomyids between North America and Europe is poorly understood. The European material (genus Arcius) is taxonomically reassessed, including emended diagnoses for all four previously named species, and description of two new Arcius species. A cladistic ii analysis of the European paromomyids resolves Arcius as monophyletic, implying that the European radiation of paromomyids was a product of a single migration event from North America.
    [Show full text]
  • Revised Tertiary Stratigraphy and Paleontology of the Western Beaver Divide, Fremont County, Wyoming
    SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY . NUMBER25 Revised Tertiary Stratigraphy and Paleontology of the Western Beaver Divide, Fremont County, Wyoming Robert J. Emry ISSUED SMITHSONIAN INSTITUTION PRESS City of Washington 1975 ABSTRACT Emry, Robert J. Revised Tertiary Stratigraphy and Paleontology of the West- ern Beaver Divide, Fremont County, Wyoming. Smithsonian Contributions to Paleobiology, number 25, 20 pages, 6 figures, 1975.•In the western Beaver Divide area in west-central Wyoming, a lens of coarse Tertiary volcanic conglomerate and tuff disconfqrmably overlies Uintan rocks of the Wagon Bed Formation. The coarse volcaniclastic rocks were previously regarded as a faciès of the Beaver Divide Conglomerate Member of the Chadronian White River Formation, although fossil mammals from the volcaniclastic unit are species known other- wise only from Uintan rocks. Reexamination of field relations has shown that the White River Formation disconformably overlies the volcaniclastic unit. The "lower Uinta C" temporal equivalence indicated by the fossils from the volcani- clastic unit is no longer anomalous; the underlying Wagon Bed Formation has fossil mammals indicating "Uinta B" equivalence, and the overlying White River Formation has a fairly diverse Chadronian fauna. The Uintan volcaniclastic unit is assigned to the Wiggins Formation. The Beaver Divide Conglomerate Mem- ber is restricted to conglomerate in the lower part of the White River Forma- tion. It is composed predominantly of clasts of locally derived Precambrian crystalline rocks. OFFICIAL PUBLICATION DATE is handstamped in a limited number of initial copies and is recorded in the Institutions annual report, Smithsonian Year. SI PRESS NUMBER 6013. SERIES COVER DESICN: The trilobite Phacops rana Green. Library of Congress Cataloging in Publication Data Emry, Robert J.
    [Show full text]
  • The Baca Formation and the Eocene-Oligocene Boundary in New Mexico Spencer G
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/34 The Baca Formation and the Eocene-Oligocene boundary in New Mexico Spencer G. Lucas, 1983, pp. 187-192 in: Socorro Region II, Chapin, C. E.; Callender, J. F.; [eds.], New Mexico Geological Society 34th Annual Fall Field Conference Guidebook, 344 p. This is one of many related papers that were included in the 1983 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • An Assessment of the Vertebrate Paleoecology and Biostratigraphy of the Sespe Formation, Southern California
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY AN ASSESSMENT OF THE VERTEBRATE PALEOECOLOGY AND BIOSTRATIGRAPHY OF THE SESPE FORMATION, SOUTHERN CALIFORNIA by Thomas M. Bown1 Open-File Report 94-630 1994 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 USGS, Denver, Colorado Abstract Fossil vertebrates occurring in the continental Sespe Formation of southern California indicate that deposition of the upper third of the lower member and the middle and upper members of the formation took place between Uintan (middle Eocene) and late early or early late Arikareean (latest Oligocene or earliest Miocene) time. Chadronian (latest Eocene) mammalian faunas are unknown and indicate a period of intraformational erosion also substantiated by sedimentologic data. The Sespe environment was probably savannah with gallery forest that formed under a climate with wet and dry seasons. More detailed knowledge of Sespe sediment accumulation rates and paleoclimates can be obtained through paleosol and alluvial architecture studies. Introduction The continental Sespe Formation (Watts, 1897) consists of over 1,650 m of coarse to fine lithic sandstone, pebble to cobble conglomerate, and variegated mudrock and claystone that is best exposed in the Simi Valley area of the Ventura Basin, southern California. It is unconformably underlain by the largely marine Llajas Formation (lower to middle Eocene; Squires, 1981), and is variously overlain conformably (gradationally) by the Vaqueros Formation (?upper Oligocene to lower Miocene; Blake, 1983), or unconformably by the Calabasas or Modelo Formations (middle Miocene), or the Pliocene Saugus Formation (Taylor, 1983).
    [Show full text]
  • Geological Survey
    DEPARTMENT OF THE IHTBEIOE BULLETIN OF THE UNITED STATES GEOLOGICAL SURVEY WASHINGTON G-UVEltNMENT PRINTING OFFICE 1900 [JOTTED STATES GEOLOGICAL StJKVEY (JHAKLES D. WALCOTT. DIEECTOK BIBLIOGRAPHY AND INDEX OF AND MI FOR THE YEA.R 1899 BY FRED BOTJGHTON WEEKS WASHINGTON GOVERNMENT PRINTING OFFICE 1900 CONTENTS. Page. Letter of transmittal...................................................... 7 Introduction............................................................. 9 List of publications examined ...............'.......................;...... 11 Bibliography............................................................. 15 Addenda to bibliographies for previous years............................... 90 Classified key to the index................................................ 91 Index................................................................... 97 LETTER OF TRANSMITTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washmgton, D. <?., June 1%, 1900. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the Year 1899, and to request that it l)e published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Directs United States Geological Survey. 7 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1899. By FEED BOUGHTON WEEKS. INTRODUCTION. The method of preparing and arranging the material of the Bibliog­ raphy
    [Show full text]
  • Vertebrate Paleontological Resources of Death Valley National Park, California
    NEVADA STATE MUSEUM PALEONTOLOGICAL PAPERS NUMBER 1 Field Trip Guide Book 71st Annual Meeting of the Society of Vertebrate Paleontology Paris Las Vegas, Las Vegas, Nevada November 2-5, 2011 by Joshua W. Bonde and Andrew R.C. Milner, Editors NEVADA DEPARTMENT OF TOURISM AND CULTURAL AFFAIRS DIVISION OF MUSEUMS AND HISTORY CARSON CITY, NEVADA NOVEMBER 2011 CONFERENCE EDITION i VERTEBRATE PALEONTOLOGICAL RESOURCES OF DEATH VALLEY NATIONAL PARK, CALIFORNIA Vincent L. Santucci1*, Torrey Nyborg2*, Paul H. Buchheim2, and Kevin E. Nick2 1 National Park Service, Geologic Resources Division, Washington, D.C. 20005 [email protected] 2 Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, California, 92354 [email protected] *Corresponding Authors 127 INTRODUCTION 1800 m (5905 feet) of basin fill fluvial to lacustrine Death Valley National Park (DEVA), sediments containing rich and diverse mammal and California, is administered by the National Park bird ichnofossils. The second stop will visit another Service and was originally proclaimed as a national vertebrate track locality of similar age and monument by President Hoover on February 11, depositional environment as the Copper Canyon 1933. The park boundary was expanded by Formation. The third and final stop of the field trip 1,200,000 acres and redesignated a national park on will examine a classic vertebrate collecting locality October 31, 1994 with the passage of the California in the Titus Canyon Formation which has yielded an Desert Protection Act. Death Valley National Park is assemblage of Eocene fossil mammals. the largest unit in the National Park System in the lower 48 states consisting of more than 3.6 million PHYSIOGRAPHY acres, much of which is designated wilderness.
    [Show full text]
  • Mammals of the Middle Eocene Uinta Formation
    MAMMALS OF THE MIDDLE EOCENE UINTA FORMATION D. Tab Rasmussen Department of Anthropology, Washington University, St. Louis, Missouri 63130 Glenn C. Conroy Department of Anthropology, Washington University, St. Louis, Missouri 63130 Anthony R. Friscia Department of Biology, University of California, Los Angeles, California 90024 K. Elizabeth Townsend Department of Anthropology, Washington University, St. Louis, Missouri 63130 Mary D. Kinkel Department of Anatomy, Northeastern Ohio Universities College of Medicine, Rootstown, Ohio, 44272 ABSTRACT INTRODUCTION Fossil mammals from the Uinta Formation, Uinta Fossils from the Uinta Formation (UF) of northeast- Basin, northeastern Utah, served as the primary basis for ern Utah have played a prominent role in our understand- establishing the Uintan North American Land Mammal ing of middle Eocene mammalian evolution in North “Age.” These Uintan mammals still remain of central America. O. C. Marsh of the Yale Peabody Museum importance in understanding mammalian evolution and first explored the fossil-bearing terrestrial sediments of paleoecology of the middle Eocene in North America. the Uinta Basin in 1870 (Betts, 1871; Marsh, 1875a, The Uintan fauna represents a transition between the rel- 1875b). He collected fossil mammals from gray bad- atively stable, tropical conditions of the earlier Eocene, lands near the White River that clearly belong to today's and the more arid and cooler conditions of the later UF (figure 1). This same area was collected more exten- Eocene. Among the key mammalian events during the sively by Francis Speir in the 1880s, working for Prince- Uintan are the appearance and radiation of selenodont ton University. Speir's fossils were studied by the great artiodactyls, and the great family-level diversification of paleontologists W.
    [Show full text]
  • Evolutionsstadien Der Kaufunktionen Früher Artiodactyla
    Evolutionsstadien der Kaufunktionen früher Artiodactyla Dissertation zur Erlangung des Doktorgrades (Dr. rer. nat.) der Mathematisch‐Naturwissenschaftlichen Fakultät der Rheinischen Friedrich‐Wilhelms‐Universität Bonn vorgelegt von Leonie C. Schwermann, geb. Lenssen aus Münster Bonn 2016 Anfertigung mit Genehmigung der Mathematisch‐Naturwissenschaftlichen Fakultät der Rheinischen Friedrich‐Wilhelms‐Universität Bonn 1. Gutachter: Prof. Dr. Thomas Martin 2. Gutachter: Prof. Dr. em. Wighart von Koenigswald Tag der Promotion: 12.07.2016 Erscheinungsjahr: 2016 Inhaltsverzeichnis 5 Inhaltsverzeichnis 1. Kurzfassung ...................................................................................................................................................... 7 2. Zielsetzung ..................................................................................................................................................... 13 3. Einleitung........................................................................................................................................................ 14 3.1. Rezente und fossile (Cet)Artiodactyla und ihre Phylogenie ......................................... 14 3.1.1. Untersuchte Taxa ................................................................................................................. 18 3.2. Zahnform‐ und ‐funktion der Mammalia und speziell der Artiodactyla ................. 33 3.3. Facetten ..............................................................................................................................................
    [Show full text]
  • Paleobios 35 Supplement: 1–25, March 20, 2018 Paleobios
    PaleoBios 35 Supplement: 1–25, March 20, 2018 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY WESTERN ASSOCIATION OF VERTEBRATE PALEONTOLOGISTS ANNUAL MEETING BJ Nicholls PROGRAM WITH ABSTRACTS Dixie State University, St. George, Utah FEBRUARY 16–19, 2018 Host Committee Tracy J. Thomson, Jerry Harris, University of California-Davis Andrew R. C. Milner, Dixie State University Jim Kirkland, St. George Dinosaur Discovery Site at Johnson Farm 0 Utah State Geological Survey Citation: Thomson, T.J., J. Harris, A.R.C. Milner, and J. Kirkland (eds.). 2018. Western Association of Vertebrate Paleontology Annual Meeting: Program with Abstracts. PaleoBios 35 Supplement. ucmp_paleobios_38376 Permalink: https://escholarship.org/uc/item/1935d40d Copyright: Items in eScholarship are protected by copyright, with all rights reserved, unless otherwise indicated. PALEOBIOS, VOL. 35, SUPPLEMENT, MARCH 2018 TABLE OF CONTENTS Map of Dixie State University ..........................................................................................3 Schedule of Events ..............................................................................................................4 Field Trip Summaries ........................................................................................................6 Keynote Abstract .................................................................................................................7 Abstracts of Oral Presentations .....................................................................................8
    [Show full text]
  • PALEONTOLOGY and STRATIGRAPHY of MIDDLE EOCENE ROCK UNITS in the SOUTHERN GREEN RIVER and UINTA BASINS, WYOMING and UTAH Paul C
    GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 4 2017 PALEONTOLOGY AND STRATIGRAPHY OF MIDDLE EOCENE ROCK UNITS IN THE SOUTHERN GREEN RIVER AND UINTA BASINS, WYOMING AND UTAH Paul C. Murphey, K.E. Beth Townsend, Anthony R. Friscia, James Westgate, Emmett Evanoff, and Gregg F. Gunnell A Field Guide Prepared For SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA Post-Meeting Field Trip October 30–November 1, 2016 © 2017 Utah Geological Association. All rights reserved. For permission to copy and distribute, see the following page or visit the UGA website at www.utahgeology.org for information. Email inquiries to [email protected]. GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 4 2017 Editors UGA Board Douglas A. Sprinkel Thomas C. Chidsey, Jr. 2016 President Bill Loughlin [email protected] 435.649.4005 Utah Geological Survey Utah Geological Survey 2016 President-Elect Paul Inkenbrandt [email protected] 801.537.3361 801.391.1977 801.537.3364 2016 Program Chair Andrew Rupke [email protected] 801.537.3366 [email protected] [email protected] 2016 Treasurer Robert Ressetar [email protected] 801.949.3312 2016 Secretary Tom Nicolaysen [email protected] 801.538.5360 Bart J. Kowallis Steven Schamel 2016 Past-President Jason Blake [email protected] 435.658.3423 Brigham Young University GeoX Consulting, Inc. 801.422.2467 801.583-1146 UGA Committees [email protected]
    [Show full text]
  • A Glyptosaurine Lizard from the Eocene
    East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 8-2013 A Glyptosaurine Lizard from the Eocene (late Uintan) of San Diego, California, and Implications for Glyptosaurine Evolution and Biogeography David Moscato East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Biodiversity Commons, Evolution Commons, and the Paleontology Commons Recommended Citation Moscato, David, "A Glyptosaurine Lizard from the Eocene (late Uintan) of San Diego, California, and Implications for Glyptosaurine Evolution and Biogeography" (2013). Electronic Theses and Dissertations. Paper 1176. https://dc.etsu.edu/etd/1176 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. A Glyptosaurine Lizard from the Eocene (late Uintan) of San Diego, California, and Implications for Glyptosaurine Evolution and Biogeography _________________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences _________________________ by David A. Moscato August 2013 _________________________ Jim I. Mead, Chair Blaine W. Schubert Steven C. Wallace Keywords: Glyptosaurinae, Glyptosaurus sylvestris, San Diego County, Santiago Formation Uintan, biogeography ABSTRACT A Glyptosaurine Lizard from the Eocene (late Uintan) of San Diego, California, and Implications for Glyptosaurine Evolution and Biogeography by David Moscato Glyptosaurine lizards (family Anguidae) are known exclusively from the Paleogene of North America and Eurasia.
    [Show full text]