State of the Park Report, John Day
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Timing of In-Water Work to Protect Fish and Wildlife Resources
OREGON GUIDELINES FOR TIMING OF IN-WATER WORK TO PROTECT FISH AND WILDLIFE RESOURCES June, 2008 Purpose of Guidelines - The Oregon Department of Fish and Wildlife, (ODFW), “The guidelines are to assist under its authority to manage Oregon’s fish and wildlife resources has updated the following guidelines for timing of in-water work. The guidelines are to assist the the public in minimizing public in minimizing potential impacts to important fish, wildlife and habitat potential impacts...”. resources. Developing the Guidelines - The guidelines are based on ODFW district fish “The guidelines are based biologists’ recommendations. Primary considerations were given to important fish species including anadromous and other game fish and threatened, endangered, or on ODFW district fish sensitive species (coded list of species included in the guidelines). Time periods were biologists’ established to avoid the vulnerable life stages of these fish including migration, recommendations”. spawning and rearing. The preferred work period applies to the listed streams, unlisted upstream tributaries, and associated reservoirs and lakes. Using the Guidelines - These guidelines provide the public a way of planning in-water “These guidelines provide work during periods of time that would have the least impact on important fish, wildlife, and habitat resources. ODFW will use the guidelines as a basis for the public a way of planning commenting on planning and regulatory processes. There are some circumstances where in-water work during it may be appropriate to perform in-water work outside of the preferred work period periods of time that would indicated in the guidelines. ODFW, on a project by project basis, may consider variations in climate, location, and category of work that would allow more specific have the least impact on in-water work timing recommendations. -
A NEW SABER-TOOTHED CAT from NEBRASKA Erwin H
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Conservation and Survey Division Natural Resources, School of 1915 A NEW SABER-TOOTHED CAT FROM NEBRASKA Erwin H. Barbour Nebraska Geological Survey Harold J. Cook Nebraska Geological Survey Follow this and additional works at: http://digitalcommons.unl.edu/conservationsurvey Part of the Geology Commons, Geomorphology Commons, Hydrology Commons, Paleontology Commons, Sedimentology Commons, Soil Science Commons, and the Stratigraphy Commons Barbour, Erwin H. and Cook, Harold J., "A NEW SABER-TOOTHED CAT FROM NEBRASKA" (1915). Conservation and Survey Division. 649. http://digitalcommons.unl.edu/conservationsurvey/649 This Article is brought to you for free and open access by the Natural Resources, School of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Conservation and Survey Division by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 36c NEBRASKA GEOLOGICAL SURVEY ERWIN HINCKLEY BARBOUR, State Geologist VOLUME 4 PART 17 A NEW SABER-TOOTHED CAT FROM NEBRASKA BY ERWIN H. BARBOUR AND HAROLD J. COOK GEOLOGICAL COLLECTIONS OF HON. CHARLES H. MORRILL 208 B A NEW SABER-TOOTHED CAT FROM NEBRASKA BY ERWIN H. BARBOUR AND HAROLD J, COOK During the field season of 1913, while exploring the Pliocene beds of Brown County, Mr. A. C. \Vhitford, a Fellow in the Department of Geology, University of Nebraska, discovered the mandible of a new mach.erodont cat. His work in this region was in the interest of the ~ebraska Geological Survey and the Morrill Geological Expeditions.1 The known fossil remains of the ancestral Felid.e fall into two nat ural lines of descent, as pointed out by Dr. -
(Barbourofelinae, Nimravidae, Carnivora), from the Middle Miocene of China Suggests Barbourofelines Are Nimravids, Not Felids
UCLA UCLA Previously Published Works Title A new genus and species of sabretooth, Oriensmilus liupanensis (Barbourofelinae, Nimravidae, Carnivora), from the middle Miocene of China suggests barbourofelines are nimravids, not felids Permalink https://escholarship.org/uc/item/0g62362j Journal JOURNAL OF SYSTEMATIC PALAEONTOLOGY, 18(9) ISSN 1477-2019 Authors Wang, Xiaoming White, Stuart C Guan, Jian Publication Date 2020-05-02 DOI 10.1080/14772019.2019.1691066 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of Systematic Palaeontology ISSN: 1477-2019 (Print) 1478-0941 (Online) Journal homepage: https://www.tandfonline.com/loi/tjsp20 A new genus and species of sabretooth, Oriensmilus liupanensis (Barbourofelinae, Nimravidae, Carnivora), from the middle Miocene of China suggests barbourofelines are nimravids, not felids Xiaoming Wang, Stuart C. White & Jian Guan To cite this article: Xiaoming Wang, Stuart C. White & Jian Guan (2020): A new genus and species of sabretooth, Oriensmilusliupanensis (Barbourofelinae, Nimravidae, Carnivora), from the middle Miocene of China suggests barbourofelines are nimravids, not felids , Journal of Systematic Palaeontology, DOI: 10.1080/14772019.2019.1691066 To link to this article: https://doi.org/10.1080/14772019.2019.1691066 View supplementary material Published online: 08 Jan 2020. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tjsp20 Journal of Systematic Palaeontology, 2020 Vol. 0, No. 0, 1–21, http://dx.doi.org/10.1080/14772019.2019.1691066 A new genus and species of sabretooth, Oriensmilus liupanensis (Barbourofelinae, Nimravidae, Carnivora), from the middle Miocene of China suggests barbourofelines are nimravids, not felids a,bà c d Xiaoming Wang , Stuart C. -
First Nimravid Skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1
www.nature.com/scientificreports OPEN First nimravid skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1 Maofelis cantonensis gen. and sp. nov. is described based on a complete cranium from the middle- upper Eocene Youganwo Formation of Maoming Basin, Guangdong Province, China. The new taxon Received: 08 September 2015 has characters diagnostic for Nimravidae such as a short cat-like skull, short palate, ventral surface of petrosal dorsal to that of basioccipital, serrations on the distal carina of canine, reduced anterior Accepted: 21 April 2016 premolars, and absence of posterior molars (M2-3). It is plesiomorphic nimravid taxon similar to Published: 10 May 2016 Nimravidae indet. from Quercy (France) in having the glenoid pedicle and mastoid process without ventral projections, a planar basicranium in which the lateral rim is not ventrally buttressed, and P1 present. The upper canine is less flattened than in other Nimravidae.Maofelis cantonensis gen. and sp. nov. exemplifies the earliest stage of development of sabertooth specialization characteristic of Nimravidae. This taxon, together with other middle-late Eocene nimravid records in South Asia, suggests origin and initial diversification of Nimravidae in Asia. We propose that this group dispersed to North America in the late Eocene and to Europe in the early Oligocene. The subsequent Oligocene diversification of Nimravidae took place in North America and Europe, while in Asia this group declined in the Oligocene, likely because of the earlier development of open habitats on that continent. Nimravids are cat-like hypercarnivores that developed saber-tooth morphology early in the Cenozoic and were top predators in the late Eocene – late Oligocene mammal communities of the Northern Hemisphere1–3. -
John Day Fossil Beds National Monument
ISSUE VIII JANUARY 2007 NARG Newsletter North America Research Group Northwest Fossil Fest Recap Last August NARG held it's first annual Northwest Fossil Fest held at INSIDE THIS ISSUE the Rice Museum in Hillsboro Oregon. The goal of the Fest was to NW Fossil Fest Recap 1 promote, educate, showcase fossils Radiocarbon Dating Fund 3 from the Pacific NW, and to have John Day Fossil Beds fun, all of which was accomplished. National Monument 3 Taxonomy Report #6 5 The tagline for the Fest is “Inspire, Inquire, Interact” and nothing What is “Fossil Search and Rescue? inspires more than displaying some of the amazing fossils specimens that Oregon Fossils have been found in the Pacific NW. Plants of the Jurassic Period 7 Tami Smith making a batch of Trilobite Cookie Many guests where surprised at the Trilobite Morphology 8 wide range of life forms that once lived where we do today. Inquiry minds want to know and we had a top-notch line up of guest speakers such as Dr. Dr. Ellen Morris Bishop, Dr. Jeffrey A. Myers, and Dr. William. N. Orr. This was a great opportunity for guest not only to learn more about the paleontology and geology of Oregon but also to meet 3 of the leading professionals in these fields. More Trilobite Cookie making There were many ways to interact, from the fossil preparation area where demonstrations took place on tools and techniques used to prepare fossils, to fossil identification, and of course all the kids activities that NARG setup. The Screen for Shark Teeth was probably the biggest hits and over 1000 Bone Valley shark teeth where given away. -
The Fossil Frontier John Day Fossil Beds National Monument
National Park Service U.S. Department of the Interior The Fossil Frontier John Day Fossil Beds National Monument Paleontologists (from left) Furlong, Stock, Merriam, and Chaney Paleontology became popular in the 19th century. Thomas Jefferson told Lewis and Clark to look for living giant sloths in the west. The term ‘paleontology’ was coined in the 1820s to describe the new branch of science dedicated to the study of ancient life. Charles Darwin published On the Origin of the Species in 1859, giving voice to a new idea that plants and animals evolve by way of natural selection in an ever-changing world. A growing awareness for the long age of the earth riveted minds from university halls to street corners. Scientists sought fossils to answer difficult questions about the nature of life. The Oregon Discovery In 1862 gold was found near present-day Condon found a stunning abundance of Canyon City. While guarding wagons of gold ancient life. He returned to the area frequently, destined for ships on the Columbia River, eventually hiring men to help prospect for Union calvary troops noticed fossils along him. In what is now the Blue Basin area of the the way. They collected what they could Sheep Rock Unit, he found so many fossils and took their fossils to Thomas Condon, that he named part of the valley The Cove. a congregationalist minister in The Dalles. He even sent some of the fossils he found to Condon was well known to locals as an avid prominent east coast paleontologists. These geologist. Condon recognized the importance paleontologists were tantalized by the potential of the fossils and joined the soldiers on their for their own great finds just waiting for return to the fossil beds. -
BOOK REVIEWS DON MCCORNACK. (Eugene, Oregon: University of Oregon Press, 1928. Pp. 355. $2.50.)
BOOK REVIEWS Thomas Condon, Pioneer Geologist of Oregon.. By ELLEN CON DON MCCORNACK. (Eugene, Oregon: University of Oregon Press, 1928. Pp. 355. $2.50.) Few recent books on any subject have been freighted with such an abundance of tender sentiment and downright love as has this biography of Thomas Condon, Pioneer Geologist of Ore gon. Thomas Condon was "Oregon's Grand Old Man of Sci ence." The author of the book is his beloved daughter, his pupil and his legatee. Most of the materials with which Professor Condon worked were as hard as flint but through his long years he was himself as soft as a baby's cheek. Not in any maudlin sense is this ut tered for he was a manly man. He was a Christian gentleman and a scientist. In the years of his prime he faced with splendid wurage the then prevailing con:flict between science and religion. His fame as a scholar is secure, not alone in the archives of geology, but in the respect of those who know. As a man he is enshrined in countless memories as a fond and wise parent, as a staunch and helpful friend, as a model citizen, as a loving and loved teacher. Henry Fairfield Osborn, senior Geologist of the United States Geological Survey and President of the American Museum of Natural History, says in the Foreword: "Among these names, bright in the scientific history of America, is that of Thomas Condon. The romantic life of this theist and naturalist stretched across the American continent during the formative period of the sciences of geology and palaeontology and his eighty-four well spent years as a high priest of nature qualify him to rank among the immortals." The story of Professor Condon's life-work first appeared in his book, quaintly entitled: Two Islands and What Carne of Them. -
Person, J.J. 2012. Saber Teeth. Geo News 39(2)
Saber Teeth Jeff J. Person Carnivores of all kinds have always been of interest to me. Arguably Smilodon is only the last iteration of saber-teeth in the fossil it is a much more difficult lifestyle to hunt and kill another animal record. Carnivorous mammals with large sabers have appeared than it is to browse or graze on non-mobile plants. Carnivorous four times across unrelated groups of carnivorous mammals over animals have evolved to stalk and kill their prey in many, many the last 60 million years (or so) of Earth’s history. varied ways. Just think of the speed of a frog’s tongue or the speed of a cheetah, the stealth and camouflage of an octopus, Types of Saber-teeth or the intelligence of some birds. These are only a few examples Not only were there four different groups of mammals that of modern carnivores; the variety of carnivores through time is evolved saber-teeth separately, there are also two different kinds broader and even more fascinating. of saber-teeth. There are the dirk-toothed forms, and the scimitar- toothed forms. The scimitar-toothed animals tended to be more Convergent evolution is the reappearance of the same solution lightly built with coarsely serrated and somewhat elongated to a biological problem across unrelated groups of animals. This canines (fig. 1) (Martin, 1998a). The dirk-toothed animals tended has happened many times throughout Earth’s history. The similar to be more powerfully built with long, finely serrated, dagger-like body shapes of sharks, fish, ichthyosaurs (a group of swimming canines which sometimes included a large flange on the lower jaw reptiles) and dolphins is a great example of unrelated groups of (fig. -
The Geology and Mineral Resources of the John Day Region by Arthur J
VOLUME I NUMBER 3 MARCH, 1914 THE MINERAL RESOURCES OF OREGON Published Monthly By The Oregon Bureau of Mines and Geology Small'? Ranch and Field's Mountain on John Day River. CONTENTS. The Geology and Mineral Resources of the John Day Region by Arthur J. Collier Entered aa second clam matter at Corvallis, Ore. on Feb 10, 1914, according to the Act of Aug. 24, 1912. OREGON BUREAU OF MINES AND GEOLOGY COMMISSION Omci or THE COMMISSION tit YEON BUILDING, PORTLAND, OREGON Omci or THE DlHECTOB CORVALLI8. OREGON OSWALD WEST, Governor STAFF COMMISSION HENBT M. PARES, Director ARTHUR M. SWABTLET, Mining Eng'r H. N. LAWBIE, Portland IRA A. WILLIAMS, Ceramist W. C. Fraxows, VVhitney SIDNEY W. FRENCH, Metallurgist I. ¥ RSDDT, Medford C. T. PBALL, Ontario FIELD PARTY CHIEFS T. 8. MANN, Portland P. L. CAMPBELL, Eugene A. N. WlNCHBLL W. J. KERB, Corvallis U. 8. GBAHT A J. COLLIEB SOLON SHEDD GSOBOB D. LOUDBBBACE VOLUME I NUMBER 3 MARCH, 1914 THE MINERAL RESOURCES OF OREGON A Periodical Devoted to the Development of all her Minerals PUBLISHED MONTHLY AT CORVALLIS BY THE OREGON BUREAU OF MINES AND GEOLOGY H. M. PARKS, Director *THE GEOLOGY AND MINERAL RESOURCES OF THE JOHN DAY REGION. By Arthur J. Collier. The John Day river basin in the north central part of Oregon has been for many years a favorite place for geologic exploration, on account of the occurrence there of vertebrate fossils. In recent years, however, attention has been further directed to this region from time to time by reports of the discovery of coal, oil, gas and other mineral resources. -
Locomotor Evolution in the Carnivora (Mammalia): Evidence from the Elbow Joint
Locomotor evolution in the Carnivora (Mammalia): evidence from the elbow joint Ki Andersson Thesis for the degree of Filosofie Licentiat, 2003 Department of Earth Sciences Historical Geology and Paleontology Uppsala University Norbyvägen 22, SE-752 36 Uppsala, Sweden 2 Locomotor evolution in the Carnivora (Mammalia): evidence from the elbow joint KI ANDERSSON Introduction .................................................................................................................... 5 Forearm function ........................................................................................................ 5 Skeletal scaling in mammals ......................................................................................... 5 Body mass estimation ................................................................................................. 6 Carnivore hunting strategy and cursoriality ................................................................... 7 Pursuit predators in the past ........................................................................................ 7 Shape analysis ............................................................................................................ 9 Summary of papers ......................................................................................................... 9 Paper I ....................................................................................................................... 9 Paper II ................................................................................................................... -
Irrigation and Streamflow Depletion in Columbia River Basin Above the Dalles, Oregon
Irrigation and Streamflow Depletion in Columbia River Basin above The Dalles, Oregon Bv W. D. SIMONS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1220 An evaluation of the consumptive use of water based on the amount of irrigation UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 50 cents (paper cover) CONTENTS Page Abstract................................................................................................................................. 1 Introduction........................................................................................................................... 2 Purpose and scope....................................................................................................... 2 Acknowledgments......................................................................................................... 3 Irrigation in the basin......................................................................................................... 3 Historical summary...................................................................................................... 3 Legislation................................................................................................................... 6 Records and sources for data..................................................................................... 8 Stream -
4. Lower Oregon Columbia Gorge Tributaries Watershed Assessment
4. Lower Oregon Columbia Gorge Tributaries Watershed Assessment 4.1 Subbasin Overview General Description Location and Size The Lower Oregon Columbia Gorge Tributaries Watershed consists of the 19 small Columbia River tributaries located between Bonneville Dam and the Hood River. Its major streams are Herman and Eagle creeks. The watershed is located in Hood River County, except for a small part of the Eagle Creek drainage, and includes the City of Cascade Locks and part of the City of Hood River. The watershed covers a drainage area of 63,714 acres or 99.6 square miles. Geology Volcanic lava flows, glaciers, and flooding were the key forces forming the Columbia Gorge landscape of basalt cliffs, waterfalls, talus slopes and ridges. Land elevations rise rapidly from 72 feet above sea level to approximately 5,000 feet. Mt. Defiance is the highest peak at 4,960 feet. Landslides are the dominant erosional process in recent history (USFS, 1998). Debris torrents and ice and snow avalanches are not uncommon in the winter months. Alluvial fan deposits at the mouths of the steeper, more constricted creeks suggest the frequent routing of debris torrents down these channels. The lower mile or so of creeks have gradients of about 5 percent, rising steeply at middle elevations, with lower gradient channels in glaciated headwater valleys. Climate and Weather The watershed lies in the transition zone between the wet marine climate to the west and the dry continental climate to the east. Precipitation amounts vary dramatically from east to west and with elevation, ranging from 40 to 125 to inches annually.