VDRARY FEB / Marine Science Laboratory Oregon State University
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Geologic Formations of Western Oregon
BULLETIN 70 GEOLOGIC fORMATION§ OF WESTERN OREGON WEST OF LONGITUDE 121° 30' STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1971 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 Stal·e Office Building Portland, Oregon 97201 BULLETIN 70 GEOLOGIC FORMATIONS OF WESTERN OREGON (WEST OF LONGITUDE 12 1 °30') By John D. Beaulieu 1971 GOVERNING BOARD Fayette I. Bristol, Rogue River, Chairman R. W. deWeese, Portland Harold Banta, Baker STATE GEOLOGIST R. E. Corcoran CONTENTS Introduction . Acknowledgements 2 Geologic formations 3 Quadrang I es. 53 Corre I ation charts. 60 Bibliography. 63 ii GE OLOGIC FORMA T IONS OF WESTERN OR EGON (W E ST OF LONG ITUD E 12 1°30') By John D. Beaulieu* INTRODUCTION It is the purpose of th is publi cation to provide a concise , yet comprehensive discussion of the for mations of western Oregon. It is the further aim that the data for each of the formations be as current as possi ble. Consequently, the emphasis has been placed on th e recent literature . Although this paper should not be viewed as a discussion of the historical development of each of the fo rmations, the original reference for each of the units is given . Also, in cases where the historical development of the formation has a direct bearing on present-day problems it is included in the discussion . A wide variety of published literature and unpublished reports , theses, and dissertations was con sul ted and several professional opin ions regarding specific problems were so licited . In recent years re search has been concentrated in the Klamath Mountains and the southern Coast Range and for these regions literature was volumi nous. -
Groundwater and Biodiversity Conservation
GROUNDWATER AND BIODIVERSITY CONSERVATION: A methods guide for integrating groundwater needs of ecosystems and species into conservation plans in the Pacific Northwest DECEMBER 2007 JENNY BROWN ABBY WYERS ALLISON ALDOUS LESLIE BACH photos credits (from top): springs at Borax Lake © Allison Aldous/TNC; Whychus Creek © Jim Yuskavitch; spring on Lower Crooked River © Marshall Gannett Acknowledgements: We are grateful to the Northwest Conservation Fund for financial support of this work. Additionally, this guide would not have been possible without the time and contributions of numerous colleagues. Our thanks goes to: • Brad Nye (Deschutes Basin Land Trust) for field trip to Camp Polk to see springs and groundwater-dependent ecosystems of Whychus Creek drainage • Colin Brown for retrieving literature from the Oregon State University library • Don Sada (Desert Research Institute) for review of KEAs for springs • Eloise Kendy (The Nature Conservancy) for review of earlier version of document • Jack Williams (Trout Unlimited) for review of KEAs for springs and Borax Lake chub and review of document • James Newton for review of groundwater-dependent species in Whychus Ck • Jason Dedrick (Crooked River Watershed Council) for field trip to the Lower Crooked • Jen Newlin-Bell (The Nature Conservancy) for design of the cover • John Crandall (The Nature Conservancy) for field testing the methods guide at Moses Coulee Conservation Area in WA • Jonathan Higgins (The Nature Conservancy) for review of KEAs for lakes and discussions of methods development -
Paleogene Marine Bivalves of the Deep-Water Keasey Formation in Oregon, Part IV: the Anomalodesmatans
UC Berkeley PaleoBios Title Paleogene marine bivalves of the deep-water Keasey Formation in Oregon, part IV: The anomalodesmatans Permalink https://escholarship.org/uc/item/6vf3t60q Journal PaleoBios, 31(3) ISSN 0031-0298 Author Hickman, Carole S. Publication Date 2014-12-16 DOI 10.5070/P9313025099 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Peer Reviewed Title: Paleogene marine bivalves of the deep-water Keasey Formation in Oregon, part IV: The anomalodesmatans Journal Issue: PaleoBios, 31(3) Author: Hickman, Carole S., University of California Publication Date: 2014 Permalink: http://escholarship.org/uc/item/6vf3t60q Acknowledgements: Documentation of the Keasey bivalve fauna would not have been possible without the encouragement of the late Harold Vokes, who generously turned over the specimens and considerable research effort he originally invested in anticipation of publishing monographic treatments of mollusks of the Keasey Formation. For collecting assistance in the field, I am grateful to James C. Hickman and to the following undergraduate students from the 1979 invertebrate paleontology class at the University of Oregon: Janet Baldridge, Les Boyer, Scott Larson, Greg Miles, Gordy Miller, Diane Searcy, Gary Smith, and Barbara Zeller. Digital photography of specimens illustrated in color is the work of UCMP photographer and Associate Dave Strauss, and the exceptional quality of his morphological documentation of specimens is the most important single contribution to this monographic treatment. Micrographs of very small transparent shells were recorded digitally with the Hitachi S-r800 Field Emission Scanning Electron Microscope at the Biological Scanning Electron Microscope Facility of the University of Hawaii with advice and assistance from Tina Weatherby Carvalho. -
Wynoochee Valley Quadrangle Grays Harbor County, Washington
State of Washington Department of Natural Resources BERT L. COLE, Commissioner of Public Lands DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 56 GEOLOGY OF THE WYNOOCHEE VALLEY QUADRANGLE GRAYS HARBOR COUNTY, WASHINGTON By WELDON W. RAU STATE PRINTING PLANT. OLYMPIA, WASH. 1967 For sale by Department of Natural Resources, Olympia, Washington. Price, $1 .50. CONTENTS Page Abstract . 5 Introduction . 6 Location and general geography. 6 Purpose and scope. 8 Previous work . 9 Field work and acknowledgments. 10 Stratigraphy . 10 Tertiary rocks . 10 Crescent Formation . .......................................... 10 Age and correlation . 11 Sedimentary rocks of late Eocene age. 13 Age and correlation ...................................... 14 Lincoln Creek Formation ......................... .. ......... 16 Age and correlation. 17 Astoria(?) Formation ........... .............. ............ 21 Age and correlation. 23 Montesano Formation . 28 Age and correlation .. ..................................... 34 Quaternary deposits .............................................. 38 Deposits of Pleistocene (?) age. 38 Landslide debris . 39 Alluvium .......................... .. ....................... 39 Structure . 39 Folds ...................................... .................... 40 Faults ............... .... .. ................. ................... 42 Unconformities . 43 Economic geology . 45 Oil and gas possibilities. 45 Other commodities ............ ........................... .. .... 47 References . 49 ILLUSTRATIONS -
The Stratigraphy and Depositional Setting of the Spencer
AN ABSTRACT OF THE THESIS OF Linda J. Baker for the degree of Master of Science in Geology presented on March 3, 1988. Title: The Stratigraphy and Depositional Setting of the Spencer Formation, West-central Willamette Valley, Oregon; a Surface-subsurface Analysis Abstract approved: Redacted for Privacy Dr. Kieth F. Oles The late Eocene Spencer Formation crops out in the low hills on the western edge of the central Willamette Valley, Oregon.Surface exposures in eastern Benton and southeastern Polk Counties and oil/gas well records and cuttings in Polk, Marion and Linn Counties were studied to determine Spencer stratigraphy, regional lithologic variations, and depositional environment. Methods used include: study of outcrops, petrography, texture, and well cuttings, as well as the correlation of well logs and microfossil data of McKeel (1984, 1985). The distribution of the underlying early-late Eocene Yamhill Formation is also briefly considered. The Yamhill Formation consists of the Miller sandstone member enclosed between mudstones. The lower and middle Yamhill record shoaling from bathyal to marginal marine depths, and they are overlain by bathyal upper Yamhill mudstones. The Miller sandstone is lens-shaped, trends parallel to the Corvallis fault, and reaches a maximum thickness of approximately 2,000 feet on the east side of the fault. The Miller sandstone grades westward into bathyal mudstones, and eastward into volcanic tuffs and flows. Thinning of the Miller sandstone and upper Yamhill mudstone along the Corvallis fault suggests movement during early late Eocene. The absence of Yamhill strata along the outcrop belt to the southwest may be related to this tectonic activity. -
Paleogene Marine Bivalves of the Deep-Water Keasey
Peer Reviewed Title: Paleogene marine bivalves of the deep-water Keasey Formation in Oregon, Part III: The heteroconchs Journal Issue: PaleoBios, 32(1) Author: Hickman, Carole S., Department of Integrative Biology and Museum of Paleontology, University of California, Berkeley Publication Date: 2015 Permalink: http://escholarship.org/uc/item/603017mr Acknowledgements: People and institutions providing invaluable assistance with the Keasey bivalve project are acknowledged at the end of the anomalodesmatan chapter (Hickman 2014). This monographic treatment of the bivalve fauna is dedicated to the late Harold Vokes in grateful recognition of the material that he collected and for encouraging me many years ago to undertake completion of a project in which he had already invested considerable effort. Paul Valentich-Scott has generously shared his enthusiasm and encyclopedic knowledge of the living bivalve fauna of the Northeastern Pacific as well as providing access to important collections in the Santa Barbara Museum of Natural History. John Armentrout, Casey Burns, Dave Jablonski, Liz Nesbitt, Graham Oliver, and Winston Ponder responded to queries with helpful information. Excavation and field work at the Rock Creek cold seep was undertaken jointly with Dave Taylor, who discovered the site, and Liz Nesbitt; and we are grateful to Richard Wysong for access to the site as well as to the Keasey family and friends in Vernonia, Oregon for their interest in the project. Casey Burns has continued to provide specimens that normally would have been overlooked in the field. I am especially thankful to UCMP Associate and Photographer Dave Strauss, for his volunteered time and exceptional expertise with the digital photography and finalization of the figures. -
Oregon Natural Areas Plan
Portland State University PDXScholar Institute for Natural Resources Publications Institute for Natural Resources - Portland 2010 Oregon Natural Areas Plan Oregon Natural Heritage Advisory Council Let us know how access to this document benefits ouy . Follow this and additional works at: http://pdxscholar.library.pdx.edu/naturalresources_pub Part of the Natural Resources and Conservation Commons, and the Sustainability Commons Citation Details Oregon Natural Heritage Advisory Council. 2010. Oregon Natural Areas Plan. Oregon Biodiversity Information Center, Institute for Natural Resources – Portland, Portland State University, Portland, OR. 198pp. This Technical Report is brought to you for free and open access. It has been accepted for inclusion in Institute for Natural Resources Publications by an authorized administrator of PDXScholar. For more information, please contact [email protected]. Oregon Natural Areas Plan 2010 Natural Heritage Advisory Council to the State Land Board State Land Board Kate Brown Ted Kulongoski Ted Wheeler Secretary of State Governor State Treasurer Natural Heritage Advisory Council Voting Members Richard Brown Robert Chandler Stuart Garrett Charles Carter Alan Dickman Cathy Macdonald Ex-Officio Members Agriculture Director: Katy Coba, represented by Rebecca Currin Fish and Wildlife Director: Roy Elicker, represented by Holly Michaels Forestry Director: Marvin Brown, represented by Andrew Yost Higher Education Chancellor: George Pernsteiner, represented by Scott Heppell Parks and Recreation Director: Tim Wood, -
Geology of Oregon Orr Orr.Pdf
Fifth Edition Geology of Oregon Elizabeth L. Orr William N. Orr University of Oregon Cover: Ripple-marked sand dunes on the Oregon Coast resemble a gigantic fingerprint (photo by Gary Tepfer). Copyright ® 1964 by Ewart M. Baldwin Copyright ® 1976, 1981, 1992, 2000 by Kendall/Hunt Publishing Company ISBN 0-7872-6608-6 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written permission of the copyright owner. Printed in the United States of America 10 98765432 Table of Contents Introduction 1 History of geologic study in Oregon 9 Blue Mountains 21 Klamath Mountains 51 Basin and Range 79 High Lava Plains 103 Deschutes-Columbia Plateau 121 Cascade Mountains 141 Coast Range 167 Willamette Valley 203 Bibliography 223 Glossary 245 Index 251 iii Dedicated to the graduates Acknowledgments Between the fourth and fifth editions of Geology of Oregon, the importance of global tectonics to the state has been ingrained even deeper. Riding on the leading edge of the moving North American plate, Oregon reflects the underlying mecha- nism of the plate collision boundary in virtually all aspects of its geology. In the seven years since the fourth edition was written, an irregular but continuing drumbeat of earthquakes reminds us of the forces beneath our feet and the need to prepare for catastrophic changes be they quakes, volcanoes, tsunamis, floods, or massive earth movements. Most profound is the discovery of irrefutable evidence that these catastrophes have been visited on the state quite regularly over the past few thousands of years as well as the absolute surety that similar disasters will oc- cur in the near and distant future. -
Ble of Information Contained in DOE's Research and Development Reports to Business, Industry, the Academic Community, and Federal, State and Local Governments
A major purpose of the Techni- cal Information Center is to provide / the broadest dissemination possi- ble of information contained in DOE's Research and Development Reports to business, industry, the academic community, and federal, state and local governments. Although a small portion of this report is not reproducible, it is being made available to expedite the availability of information on the research discussed herein. ORNL/Sub—84-64794/1 )DE8.5 010453 SHALES AND OTHER ARGILLACEOUS STRATA IN THE UNITED STATES *3erge Gonzales Earth Resource Associates, Inc. Athens, Georgia 30601 Kenneth S. Johnson University of Oklahoma P i Norman, Oklahoma 73069 s. q. r SI- BT3 <S g5 WHfs-g 5' g s -3 n. sn? f ffP g S- 5" — > a ii 8 3 a 3 I g- Date Published: March 1985 1 - — G2 3 ^ S 5 2 3 - J! sg o=r a. 3a ^I» t» I © 3 3. 55 8 ^ n A ••55 Report Prepared by 5FF a. 8B bG c <8 Earth Resources Associates, Inc. Q o _ 3. 2 o Athens, Georgia hmr=> 3 5 8 I ; under 3 E- « i P9 Subcontract No. 11X-64794V S^l 8 1- for ^ u fi* i o g ft- ~ 2. J S g to Ef >< Oak Ridge National Laboratory _ vN; o BSO. o 1I Oak Ridge, Tennessee 37831 operated by if»s s s MARTIN MARIETTA ENERGY SYSTEMS, INC. lllil for the Mftl U.S. DEPARTMENT OF ENERGY under Contract No. DE-AC05-840R21400 s1 I is-?: \ DISTRIBUTION CF T11IS DOCUMENT IS UUUMITta iii FOREWORD In 1976 the National Waste Terminal Storage (NWTS) Program was established by the U.S. -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1975
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1975 GEOLOGICAL SURVEY BULLETIN 1422-A Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1975 By GEORGE V. COHEE and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1422-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Cohee, George Vincent, 1907- Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1975. (Contributions to Stratigraphy) (Geological Survey Bulletin 1422-A) Bibliography: p. A74-A84. 1. Geology, Stratigraphic Nomenclature United States. I. Wright, WilnaB., joint author. II. Title. III. Series. IV. Series: United States Geological Survey Bulletin 1422-A. QE75.B9no. 1422-A [QE645] 557.3'08s [551.7'001'4] 76-608278 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-02896-4 CONTENTS Page Listing of nomenclatural changes _________________________ Al Restoration of the name Cove Creek Limestone for the area of the Greendale syncline in southwest Virginia, by Wallace de Witt, Jr _______________ 46 Abandonment of the Indian Trail Formation and distribution of certain equiva lent ash-flow tuffs, eastern Nevada Test Site by G. L. Dixon, K. A. Sargent, and W. J. Carr _________________________________________ 49 Correlation chart of Carboniferous rocks in Arkansas and Oklahoma, by Macken zie Gordon, Jr _________________________________ 54 Cooper Marl in the Coastal Plain of South Carolina and Georgia, by Joseph E. Hazel _____________________________________________ 54 Paleobiogeography of Jurassic deposits in the conterminous United States, by Ralph W. -
[Italic Page Numbers Indicate Major References] Abajo Mountains, 314
Index [Italic page numbers indicate major references] Abajo Mountains, 314 andesite, 70, 82, 86, 267, 295, 297, terranes, 36, 644 Abert Lake-Goose Lake area, 343 299, 303, 305, 308, 310, 343, volcanic. See volcanic arcs Abert Rim area, 303, 377 345, 350, 371, 375, 483, 527, volcanism, 74, 81, 89, 299, 300, Absaroka Range, 290, 354 543, 644, 654 320, 385, 482, 491, 642 Absaroka system, 592 Aneth Formation, 45 waning, 643 Absaroka thrust, 172, 219, 594, 599, Angora Peak member, 316 See also specific arcs 601 Angustidontus, 34 Archean, 629, 632, 651, 652 Absaroka volcanic field, 218, 297, Anita Formation, 275 arches, 15, 46 300, 486, 491 anorthosite, 412, 633 archipelago, volcanic, 453 accretion, 36, 111, 127, 128, 131, Antelope Mountain Quartzite, 38, 40, arenite, 142 141, 168, 242, 252, 254, 262, 420 argillite, 11, 16, 31, 34, 38, 41, 62, 265, 273, 450, 468, 534, 545, Antelope Range Formation, 28 70, 81, 85, 87, 89, 111, 128, 555, 636, 646, 664, 677, 693 Antelope Valley Limestone, 22, 23, 24 130, 133, 136, 138, 141, 160, accretionary prism, 37, 127, 141, 241, anticlines, 213, 319, 340 162, 164, 281, 434, 543, 547, 281, 422, 423, 432, 436, 468, antimony, 643, 644 635, 658, 663, 671, 676 471, 621, 654, 676 Antler allochthon, 422, 431 Argus Range, 365, 600 actinolite, 528, 637 Antler assemblage, 419, 422, 450 Arikaree Formation, 286 Adams Mine, 632 Antler foredeep basin, 35, 61, 62, 74, Arizona, 140, 597 Adaville Formation, 219 94, 96, 420, 425, 430, 471 south-central, 323 Adel Mountain volcanic field, 218, Antler foreland basin, 28, 42,