Additions and Comments on the Fossil Birds of Agate Fossil Beds National Monument, Sioux County, Nebraska
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1991 ADMINISTRATION BOARD of DIRECTORS President Dr
FEB 91 THE GEOLOGICAL NEWSLETTER I GEOLOGICAL SOCIETY OF THE OREGON COUNTRY I .. GEOLOGICAL SOCIETY Non-Profit Org. OF THE OREGON COUNTRY U.S. POSTAGE P.O. BOX 907 PAID Portland, Oregon PORTLAND, OR 97207 Permit No. 999 \ 1Ett£ 13" .\. J!l CIJ" \ \. GEOLOGICAL SOCIETY OF THE OREGON COUNTRY 1990-1991 ADMINISTRATION BOARD OF DIRECTORS President Dr. Ruth Keen 222-1430 Directors 4138 SW 4th Ave Donald Barr (3 years) 246-2785 Portland, OR 97201 Peter E. Baer (2 years) 661-7995 Vice President Charlene Holzwarth (1 year) 284-3444 Dr. Walter Sunderland 625-6840 Immediate Past Presidents 7610 NE Earlwood Rd. Rosemary Kenney 221-0757 Newberg, OR 97132. Joline Robustelli 223-2852 Secretary Cecelia Crater 235-5158 THE GEOLOGICAL NEWSLETTER 3823 SE lOth Editor: Sandra Anderson 775-5538 Portland, OR 97202 Calendar: Joline Robustelli 223-2852 Treasurer Business Mgr. Joline Robustelli 223-2852 Archie Strong 244-1488 Assist: Cecelia Crater 235-5158 6923 SW 2nd Ave Portland, OR 97219 ACTIVITIES CHAIRS Calligrapher Properties and PA System .. Wallace R. McClung 637-3834 (Luncheon) Donald Botteron 245-6251 Field Trips (Evening) Walter A. Sunderland 625-6840 Alta B. Fosback 641-6323 Publications Charlene Holzwarth 284-3444 Margaret Steere 246-1670 Geology Seminars Publicity Margaret Steere 246-1670 Roberta L. Walter 235 -3579 Historian Refreshments Phyllis G. Bonebrake 289-8597 (Friday Evening) Hospitality Donald and Betty Turner 246-3192 (Luncheon) Margaret Fink 289-0188 (Geology Seminars) (Evening) Gale Rankin and Freda and Virgil Scott 771-3646 Manuel Boyes 223-6784 Telephone Library: Frances Rusche 6_54-5975 Cecelia Crater 235-5158 Esther Kennedy -287-3091 Volunteer Speakers Bureau Lois Sato 654-7671 Robert Richmond 282-3817 Past Presidents Panel Annual Banquet Rosemary Kenney 221-0757 Esther Kennedy 287-3091 Programs Gale Rankin 223-6784 (Luncheon) Helen E. -
Geologic Studies of Union County, New Mexico
Bulletin 63 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Geologic Studies of Union County, New Mexico by Brewster Baldwin and William R. Muehlberger SOCORRO 1959 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY KENNETH W. FORD, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director GEORGE S. Austin, Deputy Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, Secretary-Treasurer, 1961-1985, Hobbs Judy Floyd, President, 1977-1981, Las Cruces Owen Lopez, 1977-1983, Santa Fe Dave Rice, 1972-1983, Carlsbad Steve Torres, 1967-1985, Socorro BUREAU STAFF Full Time MARLA D. ADKINS, Assistant Editor LYNNE MCNEIL, Staff Secretary ORIN J. ANDERSON, Geologist NORMA J. MEEKS, Department Secretary RUBEN ARCHULETA, Technician I ARLEEN MONTOYA, Librarian/Typist WILLIAM E. ARNOLD, Scientific Illustrator SUE NESS, Receptionist ROBERT A. BIEBERMAN, Senior Petrol. Geologist ROBERT M. NORTH, Mineralogist LYNN A. BRANDVOLD, Chemist JOANNE C. OSBURN, Geologist CORALE BRIEBLEY, Chemical Microbiologist GLENN R. OSBURN, Volcanologist BRENDA R. BROADWELL, Assoc. Lab Geoscientist LINDA PADILLA, Staff Secretary FRANK CAMPBELL, Coal Geologist JOAN C. PENDLETON, Associate Editor RICHARD CHAMBERLIN, Economic Geologist JUDY PERALTA, Executive Secretary CHARLES E. CHAPIN, Senior Geologist BARBARA R. Popp, Lab. Biotechnologist JEANETTE CHAVEZ, Admin. Secretary I ROBERT QUICK, Driller's Helper/Driller RICHARD R. CHAVEZ, Assistant Head, Petroleum MARSHALL A. REITER, Senior Geophyicist RUBEN A. CRESPIN, Laboratory Technician II JACQUES R. RENAULT, Senior Geologist Lois M. DEVLIN, Director, Bus.-Pub. Office JAMES M. ROBERTSON, Mining Geologist KATHY C. EDEN, Editorial Technician GRETCHEN H. -
Monophyly and Interrelationships of Snook and Barramundi (Centropomidae Sensu Greenwood) and five New Markers for fish Phylogenetics ⇑ Chenhong Li A, , Betancur-R
Molecular Phylogenetics and Evolution 60 (2011) 463–471 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Monophyly and interrelationships of Snook and Barramundi (Centropomidae sensu Greenwood) and five new markers for fish phylogenetics ⇑ Chenhong Li a, , Betancur-R. Ricardo b, Wm. Leo Smith c, Guillermo Ortí b a School of Biological Sciences, University of Nebraska, Lincoln, NE 68588-0118, USA b Department of Biological Sciences, The George Washington University, Washington, DC 200052, USA c The Field Museum, Department of Zoology, Fishes, 1400 South Lake Shore Drive, Chicago, IL 60605, USA article info abstract Article history: Centropomidae as defined by Greenwood (1976) is composed of three genera: Centropomus, Lates, and Received 24 January 2011 Psammoperca. But composition and monophyly of this family have been challenged in subsequent Revised 3 May 2011 morphological studies. In some classifications, Ambassis, Siniperca and Glaucosoma were added to the Accepted 5 May 2011 Centropomidae. In other studies, Lates + Psammoperca were excluded, restricting the family to Available online 12 May 2011 Centropomus. Recent analyses of DNA sequences did not solve the controversy, mainly due to limited taxonomic or character sampling. The present study is based on DNA sequence data from thirteen Keywords: genes (one mitochondrial and twelve nuclear markers) for 57 taxa, representative of all relevant Centropomidae species. Five of the nuclear markers are new for fish phylogenetic studies. The monophyly of Centrop- Lates Psammoperca omidae sensu Greenwood was supported by both maximum likelihood and Bayesian analyses of a Ambassidae concatenated data set (12,888 bp aligned). No support was found for previous morphological hypothe- Niphon spinosus ses suggesting that ambassids are closely allied to the Centropomidae. -
Sankey, J.T. 2002. Vertebrate Paleontology And
SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS. IDAHO Table 2. Stratigraphic level and geologic unit of fossils discussed in this paper. See Systematic Paleontology section (this paper) for referenced specimens and their corresponding IMNH locality. GF, upper Glenns Ferry Formation (normal polarity, upper Olduvai subchron); B, lower Bruneau Formation (lowest Bruneau Formation, normal polarity, uppermost Olduvai subchron; remaining Bruneau Formation, reversed polarity; Fig. 5). IMNH 158 and 159 (collected by the John Tyson family) have imprecise locations, and a wide range of elevations are shown for these two localities. xxxx x x ¥f XX x X XXX a mw Eiychocheilus arcifems Mcheilus --Gila milleri ~u~yes&us -sp. cf. & tierinurn cf. WQsp. &ma SP- d. && sp. cf. *lopolus sp. Colubridae-indeterminate cf. Qm sp. d. sp. d. & sp. sp. cf. M.kptc-stomus param"lodon Taxidea taxus htimiun pid~nrn sp. d. C. &xg&gs Q& sp. cf. c. priscolatrans Felis lacustrjs EAk SP. -v Jhnlwu SP. fdbQmy3Q.1 patus sbdaka- lYlkmV3- I3Ywmu .SP. d-LsEia Leporidae-indeterminate sp. cf. E. sirn~licidm I3aY!ws- cf. Qglntocamelus Sp. '3. QE%!Qps sp. cf. J-Iemiauche0Ul sp. QdQQihsSP. saYs SP. d-- AND WHEREAS.. Honoring John A. White T.3S. Fo Snake River (5 km) Figure 3. Tyson Ranch. Topographic map with locations of the three measured sections (Sinker Butte 7.5' U.S.G.S. Quadrangle). Photograph of TRl (view to Sinker Butte) with arrow pointing to the phreatic tuff near the Glenns Ferry-Bruneau Formational contact. SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS, IDAHO Figure 4. Three Mile East. Topographic map with locations of measured section (Silver City 4 NE and Sinker Butte 7.5' U.S.G.S. -
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field June 12, 2007 ABSTRACT This is compilation of a technical analysis of existing paleontological data and a limited, selective paleontological field survey of the geologic bedrock formations that will be impacted on Federal lands by construction associated with energy development in the Jonah Field, Sublette County, Wyoming. The field survey was done on approximately 20% of the field, primarily where good bedrock was exposed or where there were existing, debris piles from recent construction. Some potentially rich areas were inaccessible due to biological restrictions. Heavily vegetated areas were not examined. All locality data are compiled in the separate confidential appendix D. Uinta Paleontological Associates Inc. was contracted to do this work through EnCana Oil & Gas Inc. In addition BP and Ultra Resources are partners in this project as they also have holdings in the Jonah Field. For this project, we reviewed a variety of geologic maps for the area (approximately 47 sections); none of maps have a scale better than 1:100,000. The Wyoming 1:500,000 geology map (Love and Christiansen, 1985) reveals two Eocene geologic formations with four members mapped within or near the Jonah Field (Wasatch – Alkali Creek and Main Body; Green River – Laney and Wilkins Peak members). In addition, Winterfeld’s 1997 paleontology report for the proposed Jonah Field II Project was reviewed carefully. After considerable review of the literature and museum data, it became obvious that the portion of the mapped Alkali Creek Member in the Jonah Field is probably misinterpreted. -
Spring 2010 Newsletter
National Association of Geoscience Teachers Pacific Northwest Section Spring 2010 President Ralph Dawes, Earth Sciences Dept. This Issue Includes: Wenatchee Valley College 2010 PNW Section Annual Meeting, Twin Falls, ID 1300 Fifth Street , Wenatchee, WA 98801 PNW Section Election Ballot [email protected] Ron Kahle Travel Grants for K-12 teachers- apply Vice President Ron Metzger From the President Southwestern Oregon Community College As I hand over the Pacific Northwest section presidency to 1988 Newmark Avenue, Coos Bay, OR 97420 [email protected] Ron Metzger, there are three things I want to leave you with. Secretary/Treasurer Robert Christman-Department of Geology First, this is the century of earth science, not just for Western Washington University knowledge, but for our future on planet earth. Together, we Bellingham, WA 98225 humans are measurably changing the earth and altering the [email protected] course of earth history. The decisions we make and the Newsletter Editor Cassandra Strickland, Physical Sciences, S-1 actions we take during this century will determine how many Columbia Basin College people will be able to live on planet earth in the future, and how they live. To shape this Pasco, WA 99301 future, we will have to solve problems such as limits on energy and material resources; [email protected] reduced biodiversity and its effect on survival of remaining species ; climate change; and State Councilors increased human exposure to earthquakes, eruptions, floods, storms, wildfires, AK Cathy Connor, Univ. of Alaska Southeast, Juneau landslides, and more. Solving these problems will require the special methods of [email protected] gaining and refining knowledge that we have as earth scientists. -
The Origin and Biogeographic Diversification of Fishes in the Family Poeciliidae
RESEARCH ARTICLE The origin and biogeographic diversification of fishes in the family Poeciliidae David N. Reznick1*, Andrew I. Furness2, Robert W. Meredith3, Mark S. Springer1 1 Department of Biology, University of California Riverside, Riverside, California, United States of America, 2 Department of Ecology and Evolutionary Biology, University of California Irvine, Irvine, California, United States of America, 3 Department of Biology and Molecular Biology, Montclair State University, Montclair, New Jersey, United States of America * [email protected] a1111111111 a1111111111 a1111111111 Abstract a1111111111 a1111111111 The fish subfamily Poeciliinae (sensu Parenti, 1981) is widely distributed across the West- ern Hemisphere and a dominant component of the fish communities of Central America. Poeciliids have figured prominently in previous studies on the roles of dispersal and vicari- ance in shaping current geographic distributions. Most recently, Hrbek et al. combined a OPEN ACCESS DNA-based phylogeny of the family with geological models to provide a biogeographic per- spective that emphasized the role of both vicariance and dispersal. Here we expand on that Citation: Reznick DN, Furness AI, Meredith RW, Springer MS (2017) The origin and biogeographic effort with a database enlarged in the quantity of sequence represented per species, in the diversification of fishes in the family Poeciliidae. number of species included, and in an enlarged and more balanced representation of the PLoS ONE 12(3): e0172546. doi:10.1371/journal. order Cyprinodontiformes. We combine a robust timetree based upon multiple fossil calibra- pone.0172546 tions with enhanced biogeographic analyses that include ancestral area reconstructions to Editor: Axel Meyer, University of Konstanz, provide a detailed biogeographic history of this clade. -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
The Lost World of Fossil Lake
Snapshots from Deep Time THE LOST WORLD of FOSSIL LAKE lance grande With photography by Lance Grande and John Weinstein The University of Chicago Press | Chicago and London Ray-Finned Fishes ( Superclass Actinopterygii) The vast majority of fossils that have been mined from the FBM over the last century and a half have been fossil ray-finned fishes, or actinopterygians. Literally millions of complete fossil ray-finned fish skeletons have been excavated from the FBM, the majority of which have been recovered in the last 30 years because of a post- 1970s boom in the number of commercial fossil operations. Almost all vertebrate fossils in the FBM are actinopterygian fishes, with perhaps 1 out of 2,500 being a stingray and 1 out of every 5,000 to 10,000 being a tetrapod. Some actinopterygian groups are still poorly understood be- cause of their great diversity. One such group is the spiny-rayed suborder Percoidei with over 3,200 living species (including perch, bass, sunfishes, and thousands of other species with pointed spines in their fins). Until the living percoid species are better known, ac- curate classification of the FBM percoids (†Mioplosus, †Priscacara, †Hypsiprisca, and undescribed percoid genera) will be unsatisfac- tory. 107 Length measurements given here for actinopterygians were made from the tip of the snout to the very end of the tail fin (= total length). The FBM actinop- terygian fishes presented below are as follows: Paddlefishes (Order Acipenseriformes, Family Polyodontidae) Paddlefishes are relatively rare in the FBM, represented by the species †Cros- sopholis magnicaudatus (fig. 48). †Crossopholis has a very long snout region, or “paddle.” Living paddlefishes are sometimes called “spoonbills,” “spoonies,” or even “spoonbill catfish.” The last of those common names is misleading because paddlefishes are not closely related to catfishes and are instead close relatives of sturgeons. -
Winter 2010 Newsletter
National Association of Geoscience Teachers Pacific Northwest Section WINTER 2010 President Ralph Dawes, Earth Sciences Dept. This Issue Includes: Wenatchee Valley College 2010 PNW Section Annual Meeting, Twin Falls, ID 1300 Fifth Street , Wenatchee, WA 98801 PNW Section Election Information [email protected] Summer Opportunities and more.. Vice President Ron Metzger From the President Southwestern Oregon Community College How can we teach geoscience using information 1988 Newmark Avenue, Coos Bay, OR 97420 [email protected] technology? The Internet is being used as a learning tool by Secretary/Treasurer most students, not just those taking online classes. The Robert Christman-Department of Geology question is: how can we as geoscience teachers make the Western Washington University best use of this information technology to help students learn Bellingham, WA 98225 [email protected] geoscience? What would a freely available portal of digital Newsletter Editor geoscience learning resources, one that can be used at the Cassandra Strickland, Physical Sciences, S-1 college level, look like? Columbia Basin College Pasco, WA 99301 Investigators have looked into the efficacy of digital learning and determined that [email protected] learning results can be similar in purely online classes when compared with purely in- State Councilors person classes, and can be better in “hybrid” courses that combine online and in-person AK Cathy Connor, Univ. of Alaska Southeast, Juneau teaching and learning methods. The Andes physics tutoring program from Carnegie [email protected] Mellon University has been a key component of some hybrid physics courses. Students Michael Collins using Andes do their algebra-based physics homework assignments online. -
The Diatom Genus Actinocyclus in the Western United States
The Diatom Genus Actinocyclus in the Western United States A, Aciinocyclm Species from Lacustrine Miocene Deposits pf the Western United States B, Geologic Ranges of Lacustrine Species, Western SnltS States 0 ; SU G E Q L Q G S U PR O F E,S g- 1 PA P::B - B AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications re leased prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may no longer be available. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices listed below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications of over the counter at the following U.S. Geological Survey offices, all general interest (such as leaflets, pamphlets, booklets), single copies of which are authorized agents of the Superintendent of Documents. -
Black Mesa State Park and Preserve Resource Management Plan 2013 [Updated April 2015]
Black Mesa State Park and Preserve Resource Management Plan 2013 [Updated April 2015] Cimarron County, Oklahoma Lowell Caneday, Ph.D. Hung Ling (Stella) Liu, Ph.D. Kaowen (Grace) Chang, Ph.D. Michael Bradley, Ph.D. This page intentionally left blank. Acknowledgements The authors acknowledge the assistance of numerous individuals in the preparation of this Resource Management Plan (RMP). On behalf of the Oklahoma Tourism and Recreation Department’s Division of State Parks, staff members were extremely helpful in providing access to information and in sharing of their time. The essential staff providing assistance for the development of the RMP included Bruce Divis, Regional Manager of the Western Region, with assistance from other members of the staff throughout OTRD. In particular, assistance was provided by Deby Snodgrass, Kris Marek, and Doug Hawthorne – all from the Oklahoma City office of the Oklahoma Tourism and Recreation Department. Significant information was also provided by individuals from the Kenton Museum, from the Cimarron County Historical Society, and from Ron Mills, a former manager of Black Mesa State Park. It is the purpose of the Resource Management Plan to be a living document to assist with decisions related to the resources within the park and the management of those resources. The authors’ desire is to assist decision-makers in providing high quality outdoor recreation experiences and resources for current visitors, while protecting the experiences and the resources for future generations. Lowell Caneday, Ph.D., Regents Professor Leisure Studies Oklahoma State University Stillwater, OK 74078 i Abbreviations and Acronyms ADAAG ................................................. Americans with Disabilities Act Accessibility Guidelines CDC .....................................................................................................