Bibliographic References to Alaskan Fossils, 1839 - May 1979 Compiled by Carol W
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Insecta: Coleoptera: Leiodidae: Cholevinae), with a Description of Sciaphyes Shestakovi Sp.N
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Arthropod Systematics and Phylogeny Jahr/Year: 2011 Band/Volume: 69 Autor(en)/Author(s): Fresneda Javier, Grebennikov Vasily V., Ribera Ignacio Artikel/Article: The phylogenetic and geographic limits of Leptodirini (Insecta: Coleoptera: Leiodidae: Cholevinae), with a description of Sciaphyes shestakovi sp.n. from the Russian Far East 99-123 Arthropod Systematics & Phylogeny 99 69 (2) 99 –123 © Museum für Tierkunde Dresden, eISSN 1864-8312, 21.07.2011 The phylogenetic and geographic limits of Leptodirini (Insecta: Coleoptera: Leiodidae: Cholevinae), with a description of Sciaphyes shestakovi sp. n. from the Russian Far East JAVIER FRESNEDA 1, 2, VASILY V. GREBENNIKOV 3 & IGNACIO RIBERA 4, * 1 Ca de Massa, 25526 Llesp, Lleida, Spain 2 Museu de Ciències Naturals (Zoologia), Passeig Picasso s/n, 08003 Barcelona, Spain [[email protected]] 3 Ottawa Plant Laboratory, Canadian Food Inspection Agency, 960 Carling Avenue, Ottawa, Ontario, K1A 0C6, Canada [[email protected]] 4 Institut de Biologia Evolutiva (CSIC-UPF), Passeig Marítim de la Barceloneta, 37 – 49, 08003 Barcelona, Spain [[email protected]] * Corresponding author Received 26.iv.2011, accepted 27.v.2011. Published online at www.arthropod-systematics.de on 21.vii.2011. > Abstract The tribe Leptodirini of the beetle family Leiodidae is one of the most diverse radiations of cave animals, with a distribution centred north of the Mediterranean basin from the Iberian Peninsula to Iran. Six genera outside this core area, most notably Platycholeus Horn, 1880 in the western United States and others in East Asia, have been assumed to be related to Lepto- dirini. -
<I>Equisetum Giganteum</I>
Florida International University FIU Digital Commons FIU Electronic Theses and Dissertations University Graduate School 3-24-2009 Ecophysiology and Biomechanics of Equisetum Giganteum in South America Chad Eric Husby Florida International University, [email protected] DOI: 10.25148/etd.FI10022522 Follow this and additional works at: https://digitalcommons.fiu.edu/etd Recommended Citation Husby, Chad Eric, "Ecophysiology and Biomechanics of Equisetum Giganteum in South America" (2009). FIU Electronic Theses and Dissertations. 200. https://digitalcommons.fiu.edu/etd/200 This work is brought to you for free and open access by the University Graduate School at FIU Digital Commons. It has been accepted for inclusion in FIU Electronic Theses and Dissertations by an authorized administrator of FIU Digital Commons. For more information, please contact [email protected]. FLORIDA INTERNATIONAL UNIVERSITY Miami, Florida ECOPHYSIOLOGY AND BIOMECHANICS OF EQUISETUM GIGANTEUM IN SOUTH AMERICA A dissertation submitted in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in BIOLOGY by Chad Eric Husby 2009 To: Dean Kenneth Furton choose the name of dean of your college/school College of Arts and Sciences choose the name of your college/school This dissertation, written by Chad Eric Husby, and entitled Ecophysiology and Biomechanics of Equisetum Giganteum in South America, having been approved in respect to style and intellectual content, is referred to you for judgment. We have read this dissertation and recommend that it be approved. _______________________________________ Bradley C. Bennett _______________________________________ Jack B. Fisher _______________________________________ David W. Lee _______________________________________ Leonel Da Silveira Lobo O'Reilly Sternberg _______________________________________ Steven F. Oberbauer, Major Professor Date of Defense: March 24, 2009 The dissertation of Chad Eric Husby is approved. -
(Foram in Ifers, Algae) and Stratigraphy, Carboniferous
MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract -
Paleozoic Geology of the Dobbin Summit-Clear Creek Area, Monitor
AN ABSTRACT OF THE THESIS OF DIANE CAROL WISE for the degree of MASTER OF SCIENCE in Geology presented on August 13, 1976 Title: PALEOZOIC GEOLOGY OF THE DOBBIN SUMMIT- CLEAR CREEK AREA, MONITOR RANGE, NYiE COUNTY, NEVADA Abstract approved: Redacted for Privacy son Paleozoic limestones, dolomites, quartz arenites, and other clastic rocks were mapped in the vicinity of Dobbin Summit and Clear Creek in the central Monitor Range. Sedimentary rock units present in this area represent the shallow-shelf eastern assemblage and basin and also the basin-slope facies of the traditional limestone- clastic assemblage. The four oldest, Ordovician, units were deposited in shallow shelf environments. The Lower Ordovician Goodwin Formation is composed of about 1200 feet of calcareous shales and thin-bedded limestones. The overlying Antelope Valley Limestone is about 500 feet thick and consists of wackestones, packstones, and rare algal grainstones.The Copenhagen Formation (135 feet thick) is the highest regressive deposit of sandstone, siltstone, and limestone below the transgressive Eureka Quartzite.The Eureka is a quartz arenite 181 feet thick, with an intercalated shallow marine dolomite member. The transition from shallow to deep water conditions can be seen in the change from algal boundstones to laminated lime mud- stones in the Hanson Creek Formation (190 feet thick).The super- jacent Roberts Mountains Formation (285 feet thick) is composed of lime mudstones and allodapic beds deposited in basinal, deep water conditions.During earliest Devonian -
Smithsonian Miscellaneous Collections
-&? SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82. NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University (Publication 3061) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82, NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University Publication 306i i CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 ZU £or& (gafttmore (prees BALTIMORE, MD., U. S. A. THE PAST CLIMATE OF THE NORTH POLAR REGION 1 By EDWARD W. BERRY THE JOHNS HOPKINS UNIVERSITY The plants, coal beds, hairy mammoth and woolly rhinoceros ; the corals, ammonites and the host of other marine organisms, chiefly invertebrate but including ichthyosaurs and other saurians, that have been discovered beneath the snow and ice of boreal lands have always made a most powerful appeal to the imagination of explorers and geologists. We forget entirely the modern whales, reindeer, musk ox, polar bear, and abundant Arctic marine life, and remember only the seemingly great contrast between the present and this subjective past. Nowhere on the earth is there such an apparent contrast between the present and geologic climates as in the polar regions and the mental pictures which have been aroused and the theories by means of which it has been sought to explain the fancied conditions of the past are all, at least in large part, highly imaginary. Occasionally a student like Nathorst (1911) has refused to be carried away by his imagination and has called to mind the mar- velously rich life of the present day Arctic seas, but for the most part those who have speculated on former climates have entirely ignored the results of Arctic oceanography. -
Deep-Time Patterns of Tissue Consumption by Terrestrial Arthropod Herbivores
Naturwissenschaften DOI 10.1007/s00114-013-1035-4 ORIGINAL PAPER Deep-time patterns of tissue consumption by terrestrial arthropod herbivores Conrad C. Labandeira Received: 21 December 2012 /Revised: 26 February 2013 /Accepted: 2 March 2013 # Springer-Verlag Berlin Heidelberg (outside the USA) 2013 Abstract A survey of the fossil record of land-plant tissues from a known anatomy of the same plant taxon in better and their damage by arthropods reveals several results that preserved material, especially permineralisations. The tro- shed light on trophic trends in host-plant resource use by phic partitioning of epidermis, parenchyma, phloem and arthropods. All 14 major plant tissues were present by the xylem increases considerably to the present, probably a end of the Devonian, representing the earliest 20 % of the consequence of dietary specialization or consumption of terrestrial biota. During this interval, two types of time lags whole leaves by several herbivore functional feeding separate the point between when tissues first originated from groups. Structural tissues, meristematic tissues and repro- their earliest consumption by herbivorous arthropods. For ductive tissues minimally have been consumed throughout epidermis, parenchyma, collenchyma and xylem, live tissue the fossil record, consistent with their long lags to herbivory consumption was rapid, occurring on average 10 m.y. after during the earlier Paleozoic. Neither angiosperm dominance the earliest tissue records. By contrast, structural tissues in floras nor global environmental perturbations had any (periderm, sclerenchyma), tissues with actively dividing discernible effect on herbivore trophic partitioning of plant cells (apical, lateral, intercalary meristems), and reproduc- tissues. tive tissues (spores, megagametophytes, integuments) expe- rienced approximately a 9-fold (92 m.y.) delay in arthropod Keywords Angiosperm diversification . -
Holocene Palaeoenvironmental Reconstruction Based on Fossil Beetle Faunas from the Altai-Xinjiang Region, China
Holocene palaeoenvironmental reconstruction based on fossil beetle faunas from the Altai-Xinjiang region, China Thesis submitted for the degree of Doctor of Philosophy at the University of London By Tianshu Zhang February 2018 Department of Geography, Royal Holloway, University of London Declaration of Authorship I Tianshu Zhang hereby declare that this thesis and the work presented in it is entirely my own. Where I have consulted the work of others, this is always clearly stated. Signed: Date: 25/02/2018 1 Abstract This project presents the results of the analysis of fossil beetle assemblages extracted from 71 samples from two peat profiles from the Halashazi Wetland in the southern Altai region of northwest China. The fossil assemblages allowed the reconstruction of local environments of the early (10,424 to 9500 cal. yr BP) and middle Holocene (6374 to 4378 cal. yr BP). In total, 54 Coleoptera taxa representing 44 genera and 14 families have been found, and 37 species have been identified, including a new species, Helophorus sinoglacialis. The majority of the fossil beetle species identified are today part of the Siberian fauna, and indicate cold steppe or tundra ecosystems. Based on the biogeographic affinities of the fossil faunas, it appears that the Altai Mountains served as dispersal corridor for cold-adapted (northern) beetle species during the Holocene. Quantified temperature estimates were made using the Mutual Climate Range (MCR) method. In addition, indicator beetle species (cold adapted species and bark beetles) have helped to identify both cold and warm intervals, and moisture conditions have been estimated on the basis of water associated species. -
Coleoptera, Staphylinidae, Micropeplinae)
A peer-reviewed open-access journal ZooKeys 775: 97–102 (2018)Micropeplus liweiae sp. n., a new species from Sichuan, China... 97 doi: 10.3897/zookeys.775.22620 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research Micropeplus liweiae sp. n., a new species from Sichuan, China (Coleoptera, Staphylinidae, Micropeplinae) Cheng-Bin Wang1, Ri-Xin Jiang2, Jiang Zhu3 1 Innovation College, Mianyang Normal University, 166 Mianxing West Road, Mianyang 621000, Sichuan Province, PR China 2 Department of Biology, Shanghai Normal University, 100 Guilin Road, Shanghai 200234, PR China 3 College of Agriculture and Biology, Zhongkai University of Agriculture and Engineering, 388 Guangxin Road, Guangzhou 510550, Guangdong Province, PR China Corresponding author: Jiang Zhu ([email protected]) Academic editor: A. Brunke | Received 8 May 2018 | Accepted 19 June 2018 | Published 18 July 2018 http://zoobank.org/34D87368-3017-438F-971C-586335DC791D Citation: Wang C-B, Jiang R-X, Zhu J (2018) Micropeplus liweiae sp. n., a new species from Sichuan, China (Coleoptera, Staphylinidae, Micropeplinae). ZooKeys 775: 97–102. https://doi.org/10.3897/zookeys.775.22620 Abstract A new species of micropepline beetle is described from Sichuan, China, Micropeplus liweiae sp. n. (Coleop- tera, Staphylinidae). Important morphological characters of the new species are illustrated by colour plates. Keywords China, Micropeplinae, Micropeplus, new species, Staphylinidae, taxonomy Introduction Micropeplus Latreille, 1809 is the most speciose genus of Micropeplinae (Coleoptera, Staphylinidae), with members distributed in Ethiopian, Nearctic, Neotropical, Orien- tal and Palaearctic Regions. Campbell (1968, 1992, 1995) established eight species- groups to classify the species of the genus. In the fauna of China, 22 species had been recorded before this study (Herman 2001; Schülke and Smetana 2015; Grebennikov and Smetana 2015; Zheng et al. -
Xerox University Microfilms
information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. -
The European Palaeoecological Record of Swedish Red-Listed Beetles
Biological Conservation 260 (2021) 109203 Contents lists available at ScienceDirect Biological Conservation journal homepage: www.elsevier.com/locate/biocon Policy analysis The European palaeoecological record of Swedish red-listed beetles Francesca Pilotto a,*, Mats Dynesius b, Geoffrey Lemdahl c, Paul C. Buckland d, Philip I. Buckland a a Environmental Archaeology Lab, Department of Historical, Philosophical and Religious studies, Umeå University, Umeå, Sweden b Department of Wildlife, Fish, and Environmental Studies, Swedish University of Agricultural Sciences, Umeå, Sweden c Department of Biology and Environmental Science, Linnaeus University, Kalmar, Sweden d Independent Researcher, 20 Den Bank Close, Sheffield S10 5PA, UK ARTICLE INFO ABSTRACT Keywords: Recent global changes have triggered a biodiversity crisis. However, climate fluctuationshave always influenced Coleoptera biodiversity and humans have affected species distributions since prehistoric times. Conservation palaeobiology Conservation palaeobiology is a developing field that aims to understand the long-term dynamics of such interactions by studying the geo Environmental archaeology historical records in a conservation perspective. Case studies exist for vertebrates and plants, but insects have Palaeoentomology largely been overlooked so far. Here, we analysed the current red-listed beetle species (Coleoptera) in Sweden Threatened species and investigated their occurrence and representation in the European Quaternary fossil record. Fossil data currently exist for one third of the Swedish red-listed beetle species. All the red-list conservation classes are represented in the fossil record, which may allow for comparative studies. We found significantly different representations in the fossil records among taxonomic groups and ecological traits, which may depend on the fossil depositional and sampling environments and variation in how difficultspecies are to identify. -
Malaysian Limestone Orchids Status: Diversity, Threat and Conservation
Blumea 54, 2009: 109–116 www.ingentaconnect.com/content/nhn/blumea RESEARCH ARTICLE doi:10.3767/000651909X474168 Malaysian limestone orchids status: diversity, threat and conservation G. Rusea1, M.Y.L. Lim1, S.N. Phoon2, W.S.Y. Yong2, C.H. Tang1, H.E. Khor1, J.O. Abdullah1, J. Abdullah3 Key words Abstract To date, a total of 288 species from 96 genera were identified from the limestone areas in Perlis and Padawan-Bau, Sarawak, of which many of these are restricted to limestone habitat and either endemic to Perlis or conservation to Sarawak. Knowledge and data obtained from the field observation over the past 8 years leads us to report that diversity at least 15 species endemic to limestone has become rare in the wild in Perlis, Bau and Padawan Sarawak. This limestone orchids was mainly attributed by: i) lack of emphasis by the government on understanding and protecting biodiversity in Malaysian this kind of habitat; ii) lack of scientists willing to do research in dangerous and disaster prone limestone habitat; threat and iii) lack of knowledge and awareness among local communities on the importance of conserving and utilizing their natural resources in a sustainable manner. Published on 30 October 2009 INTRODUCTION Material AND METHODS Orchids are the largest flowering plant family in Malaysia In both areas limestone hills and some adjacent landscape (including Sabah and Sarawak) with about 2 000 species, of features were selected for this survey (Table 1). In Sarawak, two which 700 are recorded from limestone. Threats to orchids on rivers were included that flow through the limestone hills and limestone include small-scale logging (extracting timber by valleys. -
Pleistocene) Insect Assemblages from Illinois Kristine D
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 1985 Middle and Late Wisconsinan (Pleistocene) insect assemblages from Illinois Kristine D. Carter University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Carter, Kristine D., "Middle and Late Wisconsinan (Pleistocene) insect assemblages from Illinois" (1985). Theses and Dissertations. 52. https://commons.und.edu/theses/52 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. MIDDLE AND LATE WISCONSINAN (PLEISTOCENE) INSECT ASSEMBLAGES FROM ILLINOIS by Kristine D. Carter Bachelor of Science, North Dakota State University, 1981 B~chelor of Arts, Moorhead State University, 1978 A thesis submitted to the graduate faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Arts Grand Forks, North Dakota May 1985 I" This thesis submitted by Kristine D. Carter in partial fulfillment of the requirements for the degree of Master of Arts from the University of North Dakota is hereby approved by the Faculty Advisory Committee under whom the work was done. This thesis meets the standards for appearance and conforms to the style and format requirements of the Graduate School of the University of North Dakota, and is hereby approved. Dean the Graduate School 55297:1 l.