Cretaceous) Mass Extinction Earle G

Total Page:16

File Type:pdf, Size:1020Kb

Cretaceous) Mass Extinction Earle G http://www.nap.edu/catalog/4762.html We ship printed books within 1 business day; personal PDFs are available immediately. Effects of Past Global Change on Life Panel on Effects of Past Global Change on Life, National Research Council ISBN: 0-309-55261-3, 272 pages, 8.5 x 11, (1995) This PDF is available from the National Academies Press at: http://www.nap.edu/catalog/4762.html Visit the National Academies Press online, the authoritative source for all books from the National Academy of Sciences, the National Academy of Engineering, the Institute of Medicine, and the National Research Council: • Download hundreds of free books in PDF • Read thousands of books online for free • Explore our innovative research tools – try the “Research Dashboard” now! • Sign up to be notified when new books are published • Purchase printed books and selected PDF files Thank you for downloading this PDF. If you have comments, questions or just want more information about the books published by the National Academies Press, you may contact our customer service department toll- free at 888-624-8373, visit us online, or send an email to [email protected]. This book plus thousands more are available at http://www.nap.edu. Copyright © National Academy of Sciences. All rights reserved. Unless otherwise indicated, all materials in this PDF File are copyrighted by the National Academy of Sciences. Distribution, posting, or copying is strictly prohibited without written permission of the National Academies Press. Request reprint permission for this book. ue r i ease l P are t ed. STUDIES IN GEOPHYSICS insert age breaks ally P Effects of Past Global Change on Life iles. ng f i t peset y http://www.nap.edu/catalog/4762.html Effects ofPastGlobalChangeonLife y have been accident a m Board on Earth Sciences and Resources he original t t Commission on Geosciences, Environment, and Resources errors om r National Research Council f not pographic y t e som and riginal paper book, ned, i a he o t om r f be ret ed Copyright © National Academy ofSciences. Allrights reserved. cannot creat iles L f M X however, ng, i om t r f at rm o posed ic f ng-specif ion. i t been recom ibut r t has peset y t r at o f her and ot original work e ive version h t at yles, horit ion of at he aut heading st as t represent ion l a digit publicat word breaks, is hs, h t is new h of T ile: f line lengt F version D is P h t NATIONAL ACADEMY PRESS he print t he original; t bout o Washington, D.C. 1995 A use t Effects of Past Global Change on Life http://www.nap.edu/catalog/4762.html ii NATIONAL ACADEMY PRESS 2101 Constitution Avenue, N.W. Washington, DC 20418 NOTICE: The project that is the subject of this report was approved by the Governing Board of the National Research Council, whose mem- bers are drawn from the councils of the National Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine. The members of the committee responsible for the report were chosen for their special competencies and with regard for appropriate balance. This report has been reviewed by a group other than the authors according to procedures approved by a Report Review Committee consisting of members of the National Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine. The National Academy of Sciences is a private, nonprofit, self-perpetuating society of distinguished scholars engaged in scientific and engi- neering research, dedicated to the furtherance of science and technology and to their use for the general welfare. Upon the authority of the charter granted to it by the Congress in 1863, the Academy has a mandate that requires it to advise the federal government on scientific and technical matters. Dr. Bruce Alberts is president of the National Academy of Sciences. The National Academy of Engineering was established in 1964, under the charter of the National Academy of Sciences, as a parallel organiza- tion of outstanding engineers. It is autonomous in its administration and in the selection of its members, sharing with the National Academy of Sciences the responsibility for advising the federal government. The National Academy of Engineering also sponsors engineering pro- grams aimed at meeting national needs, encourages education and research, and recognizes the superior achievements of engineers. Dr. Robert M. White is president of the National Academy of Engineering. The Institute of Medicine was established in 1970 by the National Academy of Sciences to secure the services of eminent members of appro- priate professions in the examination of policy matters pertaining to the health of the public. The Institute acts under the responsibility given to the National Academy of Sciences by its congressional charter to be an adviser to the federal government and, upon its own initiative, to identify issues of medical care, research, and education. Dr. Kenneth I. Shine is president of the Institute of Medicine. The National Research Council was organized by the National Academy of Sciences in 1916 to associate the broad community of science and technology with the Academy's purposes of furthering knowledge and of advising the federal government. Functioning in accordance with general policies determined by the Academy, the Council has become the principal operating agency of both the National Academy of Sciences and the National Academy of Engineering in providing services to the government, the public, and the scientific and engineering communities. The Council is administered jointly by both Academies and the Institute of Medicine. Dr. Bruce Alberts and Dr. Robert M. White are chairman and vice chairman, respectively, of the National Research Council. Support for this activity was provided by the Department of Energy, the National Science Foundation, the U.S. Geological Survey, and the riginal paper book, not the from original typesetting breaks files. Page are true National Oceanic and Atmospheric Administration. ned, andned,typographic some errors may have been accidentally inserted. Please Library of Congress Cataloging-in-Publication Data Effects of past global change on life / Board on Earth Sciences and Resources, Commission on Geosciences, Environment, and Resources, National Research Council. p. cm. Includes bibliographical references and index. ISBN 0-309-05127-4 1. Paleoecology. 2. Paleoclimatology. I. National Research Council (U.S.). Board on Earth Sciences and Resources. QE720.E32 1994 560'.45—dc20 94-38695 Copyright 1995 by the National Academy of Sciences. All rights reserved. Printed in the United States of America About this This PDF newfile: representation digital of original work the has been recomposed from createdXML files the from o the line lengths, word breaks,to original; heading styles,typesetting-specific and other formatting, however, cannot be retai use the print version of this publication as the authoritative version for attribution. Copyright © National Academy of Sciences. All rights reserved. Effects of Past Global Change on Life http://www.nap.edu/catalog/4762.html iii Panel on Effects of Past Global Change on Life STEVEN M. STANLEY, The Johns Hopkins University, Chairman JAMES P. KENNETT, University of California, Santa Barbara, Co-Vice Chairman ANDREW H. KNOLL, Harvard University, Co-Vice Chairman ROSEMARY A. ASKIN, University of California, Riverside ERIC J. BARRON, Pennsylvania State University WILLIAM B. BERRY, University of California, Berkeley DAVID C. CHRISTOPHEL, University of Adelaide, Australia WILLIAM A. DIMICHELE, National Museum of Natural History, Smithsonian Institution BENJAMIN P. FLOWER, University of California, Santa Barbara ERLE G. KAUFFMAN, University of Colorado GERTA KELLER, Princeton University WILLIAM F. RUDDIMAN, Lamont-Doherty Earth Observatory ROBERT A. SPICER, Oxford University, U.K. S. DAVID WEBB, University of Florida THOMPSON WEBB III, Brown University Staff THOMAS M. USSELMAN, Associate Director riginal paper book, not the from original typesetting breaks files. Page are true JUDITH ESTEP, Administrative Assistant ned, andned,typographic some errors may have been accidentally inserted. Please About this This PDF newfile: representation digital of original work the has been recomposed from createdXML files the from o the line lengths, word breaks,to original; heading styles,typesetting-specific and other formatting, however, cannot be retai use the print version of this publication as the authoritative version for attribution. Copyright © National Academy of Sciences. All rights reserved. iv http://www.nap.edu/catalog/4762.html Effects ofPastGlobalChangeonLife riginal paper book, not the from original typesetting breaks files. Page are true ned, andned,typographic some errors may have been accidentally inserted. Please Copyright © National Academy ofSciences. Allrights reserved. About this This PDF newfile: representation digital of original work the has been recomposed from createdXML files the from o the line lengths, word breaks,to original; heading styles,typesetting-specific and other formatting, however, cannot be retai use the print version of this publication as the authoritative version for attribution. Effects of Past Global Change on Life http://www.nap.edu/catalog/4762.html v Board on Earth Sciences and Resources FREEMAN GILBERT, Scripps Institution of Oceanography, La Jolla, Calif., Chair GAIL M. ASHLEY, Rutgers University, Piscataway, N.J. THURE CERLING, University of Utah, Salt Lake City MARK P. CLOOS, University of Texas at Austin NEVILLE G.W. COOK, University of California, Berkeley JOEL DARMSTADTER, Resources for the Future, Washington, D.C. DONALD J. DEPAOLO, University of California, Berkeley MARCO EINAUDI, Stanford University, Stanford, Calif. NORMAN H. FOSTER, Independent Petroleum Geologist, Denver, Colo. CHARLES G. GROAT, Louisiana State University, Baton Rouge DONALD C. HANEY, Kentucky Geological Survey, Lexington ANDREW H. KNOLL, Harvard University, Cambridge, Mass. PHILIP E. LAMOREAUX, P.E. LaMoreaux and Associates, Inc., Tuscaloosa, Ala. SUSAN LANDON, Thomasson Partner Associates, Denver, Colo. MARCIA K.
Recommended publications
  • Coal and Francis Creek Shale
    University of Pennsylvania ScholarlyCommons Department of Earth and Environmental Departmental Papers (EES) Science January 1970 A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale R. A. Peppers Illinois State Geological Survey Hermann W. Pfefferkorn University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/ees_papers Recommended Citation Peppers, R. A., & Pfefferkorn, H. W. (1970). A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale. Retrieved from https://repository.upenn.edu/ees_papers/18 This material has been published in Smith, W.H., Nance, R.B., Hopkins, Johnson, R.G., and Shabica, C.W. Depositional environments in parts of the Carbondale formation, western and northern Illinois: Francis Creek Shale and associated strata and Mazon Creek biota, Illinois State Geological Survey Field Guidebook Series, No. 8, p. 61-74, 1970 NOTE: At the time of publication, author Hermann W. Pfefferkorn was affiliated with the Illinois State Geological Survey. Currently (September 2005) he is a faculty member in the Department of Earth and Environmental Science at the University of Pennsylvania. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/ees_papers/18 For more information, please contact [email protected]. A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale Abstract Abundant data from spore studies of the Colchester (no. 2) Coal Member and from investigations of plant compressions in the Francis Creek Shale provide an opportunity to compare the flora of the coal with that of the overlying shale in the northeastern part of the Illinois Basin.
    [Show full text]
  • Bedrock Geology of Carbondale Quadrangle
    BEDROCK GEOLOGY OF CARBONDALE QUADRANGLE Prairie Research Institute JACKSON AND WILLIAMSON COUNTIES, ILLINOIS Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY IGQ Carbondale-BG W. John Nelson 2013 89°15' 12'30" 10' 89°07'30" 720 000FEET (IL E) 3 000mE 3 3 3 3 3 3 R. 1 W. 2 590 000 FEET (IL W) R. 1 E. 3 37°45' 03 04 05 06 07 08 10 12 37°45' 51 4180 7 8 9 10 11 12 7 8 000m &c 4180 N 13 &c Creek d r a & h t c m r C CG 508 O &c k" m r a U.S. 366 41 b e" 79 Fish and 18 17 16 15 &t 18 17 &c 13 Wildlife Ho g an 14 Po i n t 4179 m O b r a c r h Pine C a Lo n g Vi ew Island 390000 r 13 d Park FEET (IL E) Sk" 98 390 000 Ck" 322 k" 97 FEET (IL W) m 152 E 4178 k e" K r o A F L 41 ¿ S 273 78 k" PO D ¿ m R e 13 A l C t H t r i CARBONDALE C L R EXPLANATION O 19 22 19 20 20 23 24 B m A 21 R ¿ C Holocene sm Surface mine 4177 k" 105 &t ¿ m c s ¿ 41 e &t 77 Univ ersity l i &c Carbondale Formation School P m » m Desmoinesian Tradewater Formation s s, Stonefort Limestone Member m m, Murphysboro Coal Member Pennsylvanian c c, Curlew Member Southern Illinois ¿ University S 62 &t k" &t-mb Murray Bluff Sandstone Member » &t s 4176 Atokan ¿ &t &t-o olive shale member 27 4176 29 &t-g Grindstaff Sandstone Member 29 C s am e 28 30 pus Lak À 26 25 30 42'30" À 42'30" ¿ 270 m À k" S 1201 &t 290 270 Ü k" k" ªNorth uthern Hill s m So 4175 s k"317 k" 137 s 4175 &t-mb ¿ Symbols Marberry Arboretum 40 Strike and dip of bedding; number indicates degree of dip Carbondale &t r ¿ Reservoi m Horizontal bedding &t r sm ¿ 31 Evergreen Terrace C 32 Vertical joints 4174 31 34 35 36 32 k r 33 ¿ c o ¿ » Shaft mine Sk" 250 F 51 4174 ¿ S ¿ y ¿ Slope mine &t-mb c a m o ¿ À » r m Drift mine c e s m le ¿ ¿ i & ¿ t-mb m ¿ P sm ( À T.
    [Show full text]
  • Terrestrial Impact Structures Provide the Only Ground Truth Against Which Computational and Experimental Results Can Be Com­ Pared
    Ann. Rev. Earth Planet. Sci. 1987. 15:245-70 Copyright([;; /987 by Annual Reviews Inc. All rights reserved TERRESTRIAL IMI!ACT STRUCTURES ··- Richard A. F. Grieve Geophysics Division, Geological Survey of Canada, Ottawa, Ontario KIA OY3, Canada INTRODUCTION Impact structures are the dominant landform on planets that have retained portions of their earliest crust. The present surface of the Earth, however, has comparatively few recognized impact structures. This is due to its relative youthfulness and the dynamic nature of the terrestrial geosphere, both of which serve to obscure and remove the impact record. Although not generally viewed as an important terrestrial (as opposed to planetary) geologic process, the role of impact in Earth evolution is now receiving mounting consideration. For example, large-scale impact events may hav~~ been responsible for such phenomena as the formation of the Earth's moon and certain mass extinctions in the biologic record. The importance of the terrestrial impact record is greater than the relatively small number of known structures would indicate. Impact is a highly transient, high-energy event. It is inherently difficult to study through experimentation because of the problem of scale. In addition, sophisticated finite-element code calculations of impact cratering are gen­ erally limited to relatively early-time phenomena as a result of high com­ putational costs. Terrestrial impact structures provide the only ground truth against which computational and experimental results can be com­ pared. These structures provide information on aspects of the third dimen­ sion, the pre- and postimpact distribution of target lithologies, and the nature of the lithologic and mineralogic changes produced by the passage of a shock wave.
    [Show full text]
  • Columnals (PDF)
    2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown.
    [Show full text]
  • Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy 201 Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy
    Published in "SEPM Special Publication No. 78: 201-217, 2003" which should be cited to reference this work. UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY 201 UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY ELIAS SAMANKASSOU Université de Fribourg, Département de Géosciences, Géologie et Paléontologie, Pérolles, CH-1700 Fribourg, Switzerland e-mail: [email protected] ABSTRACT: A variety of buildup types occur in the upper Paleozoic Auernig and Rattendorf Groups, Carnic Alps, at the present-day Austrian–Italian border, including coral, diverse algal (Anthracoporella, Archaeolithophyllum, Rectangulina, and phylloid green), bryozoan, brachiopod, and sponge buildups. Thin mounds and banks have a diverse fossil association (e.g., Archaeolithophyllum–bryozoan– brachiopod mounds) and occur in siliciclastic-dominated intervals, as do coral buildups. Some of the biodiverse thin mounds occur in strata that were deposited in cooler water. However, the thickest mounds are nearly monospecific (e.g., Anthracoporella mounds) and grew in carbonate-dominated, warm-water environments. Most of the mounds considered in this paper, particularly algal mounds, grew in quiet-water environments below wave base but within the photic zone. Mound growth was variously stopped by siliciclastic input, e.g., auloporid coral mounds, sea-level rise, e.g., the drowning of Anthracoporella mounds of the Rattendorf Group, influence of cool water, e.g., algal mounds of the Auernig Group overlain by limestone of cool-water biotic association, or sea-level fall, e.g., phylloid algal mounds that were subsequently exposed subaerially. There is no indication of ecological succession during mound growth. Growth, dimensions, biotic association, and termination of mounds seem to have been controlled by extrinsic factors, mainly sea level and water temperature.
    [Show full text]
  • Exploring Phylogenomic Relationships Within Myriapoda: Should High Matrix Occupancy Be the Goal?
    bioRxiv preprint doi: https://doi.org/10.1101/030973; this version posted November 9, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Exploring phylogenomic relationships within Myriapoda: should high matrix occupancy be the goal? ROSA FERNÁNDEZ1, GREGORY D. EDGECOMBE2 AND GONZALO GIRIBET1 1Museum of Comparative Zoology & Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 2Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK 1 bioRxiv preprint doi: https://doi.org/10.1101/030973; this version posted November 9, 2015. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Abstract.—Myriapods are one of the dominant terrestrial arthropod groups including the diverse and familiar centipedes and millipedes. Although molecular evidence has shown that Myriapoda is monophyletic, its internal phylogeny remains contentious and understudied, especially when compared to those of Chelicerata and Hexapoda. Until now, efforts have focused on taxon sampling (e.g., by including a handful of genes in many species) or on maximizing matrix occupancy (e.g., by including hundreds or thousands of genes in just a few species), but a phylogeny maximizing sampling at both levels remains elusive. In this study, we analyzed forty Illumina transcriptomes representing three myriapod classes (Diplopoda, Chilopoda and Symphyla); twenty-five transcriptomes were newly sequenced to maximize representation at the ordinal level in Diplopoda and at the family level in Chilopoda.
    [Show full text]
  • Geology for Planning in St. Clair County, Illinois
    465 � JSGS-- -OIL & 6AS s SECJIGN--=fltES 14.GS: STATE OF ILLINOIS CIR465 c.4 DEPARTMENT OF REGISTRATION AND ED UCATION GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ILLINOIS ST ATE GEOLOGIC AL SURVEY John C. Frye, Chief Urbana, IL 61801 CIRCULAR 465 1971 GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ABSTRACT St. Clair County lies in southwestern Illinois across the Mississippi River from St. Louis, Missouri . One-fifth of the total land surface of 673 square miles is on flood­ plains of the Mississippi and Kaskaskia Rivers and Silver Creek. The floodplains are underlain by as much as 120 feet of gravel, sand, silt, and clay. The remaining fo ur­ fifths of the land surface is on uplands that contain flat or dissected plains, low ridges and mound-shaped hills, about 20 square miles of strip mines , and an area of karst topog­ raphy. The uplands are underlain by as much as 75 feet of till and sand and gravel, and generally 12 to 3 0 feet of loess and related silt; however, near the Mississippi River bluffs there are more than 100 feet of loes s and related silt. These deposits have been redistributed into spoil piles in the strip mines. Ben<ilath these deposits or cropping out in places are gently sloping beds of limestone, shale, sand­ stone, siltstone, clay stone, and coal. Thinly layered, frac­ tured limestone underlies the area of karst topography. Mineral and water resources are abundant in the county . Limestone of the St.
    [Show full text]
  • Rocks, Soils and Surfaces: Teacher Guide
    National Aeronautics and Space Administration ROCKS, SOILS, AND SURFACES Planetary Sample and Impact Cratering Unit Teacher Guide Goal: This activity is designed to introduce students to rocks, “soils”, and surfaces on planetary worlds, through the exploration of lunar samples collected by Apollo astronauts and the study of the most dominant geologic process across the Solar System, the impact process. Students will gain an understanding of how the study of collected samples and impact craters can help improve our understanding of the history of the Moon, Earth, and our Solar System. Additionally, this activity will enable students to gain experience with scientific practices and the nature of science as they model skills and practices used by professional scientists. Objectives: Students will: 1. Make observations of rocks, “soil”, and surface features 2. Gain background information on rocks, “soil”, and surface features on Earth and the Moon 3. Apply background knowledge related to rocks, soils, and surfaces on Earth toward gaining a better understanding of these aspects of the Moon. This includes having students: a. Identify common lunar surface features b. Create a model lunar surface c. Identify the three classifications of lunar rocks d. Simulate the development of lunar regolith e. Identify the causes and formation of impact craters 4. Design and conduct an experiment on impact craters 5. Create a plan to investigate craters on Earth and on the Moon 6. Gain an understanding of the nature of science and scientific practices by: a. Making initial observations b. Asking preliminary questions c. Applying background knowledge d. Displaying data e. Analyzing and interpreting data Grade Level: 6 – 8* *Grade Level Adaptations: This activity can also be used with students in grades 5 and 9-12.
    [Show full text]
  • (A) Placement Above Uppermost Aquifer
    AECOM 502-569-2301 tel 500 W Jefferson St. 502-569-2304 fax Suite 1600 Louisville, KY 40202 www.aecom.com October 17, 2018 Big Rivers Electric Corporation Sebree Generating Station 9000 Highway 2096 Robards, Kentucky 42452 Engineer’s Certification of Placement Above the Uppermost Aquifer Existing Green CCR Surface Impoundment EPA Final CCR Rule Sebree Station Robards, Kentucky 1.0 PURPOSE The purpose of this document is to certify that the Placement above Sebree “Green” Existing CCR Surface Impoundment is in compliance with the Placement above the Uppermost Aquifer requirement of the Final CCR Rule at 40 CFR §257.60. Presented below is the project background, summary of findings, limitations and certification. 2.0 BACKGROUND In accordance with 40 CFR §257.60, the owner/operator of an existing CCR Surface Impoundment must demonstrate that the base of the unit is located no less than 1.52 meters (five feet) above the upper limit of the uppermost aquifer, or must demonstrate that there will not be an intermittent, recurring, or sustained hydraulic connection between any portion of the base of the CCR unit and the uppermost aquifer due to normal fluctuations in groundwater elevations (including the seasonal high water table). In accordance with 40 CFR §257.60(c)(1), the demonstration must be made by October 17, 2018. If such demonstration cannot be made, the unit is subject to the closure or retrofit requirements of 40 CFR §257.101 3.0 SUMMARY OF FINDINGS Available data regarding site groundwater, site geology, and physical limits of the unit for the Green Surface Impoundment do not evidence a 5-foot separation between the base of the impoundment and the uppermost limit of the uppermost aquifer and they do not support a lack of hydraulic connectivity between the unit and the aquifer as specified in 40 CFR §257.60(a).
    [Show full text]
  • B2150-B FRONT Final
    Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 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 Library of Congress Cataloging-in-Publication Data Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract ..........................................................................................................................
    [Show full text]
  • Cca) Treated Lumber Along a Topohydrosequence
    University of Kentucky UKnowledge University of Kentucky Master's Theses Graduate School 2010 CHROMIUM, COPPER, AND ARSENIC CONCENTRATION AND SPECIATION IN SOIL ADJACENT TO CHROMATED COPPER ARSENATE (CCA) TREATED LUMBER ALONG A TOPOHYDROSEQUENCE Donald Roy Schwer III University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Schwer, Donald Roy III, "CHROMIUM, COPPER, AND ARSENIC CONCENTRATION AND SPECIATION IN SOIL ADJACENT TO CHROMATED COPPER ARSENATE (CCA) TREATED LUMBER ALONG A TOPOHYDROSEQUENCE" (2010). University of Kentucky Master's Theses. 68. https://uknowledge.uky.edu/gradschool_theses/68 This Thesis is brought to you for free and open access by the Graduate School at UKnowledge. It has been accepted for inclusion in University of Kentucky Master's Theses by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF THESIS CHROMIUM, COPPER, AND ARSENIC CONCENTRATION AND SPECIATION IN SOIL ADJACENT TO CHROMATED COPPER ARSENATE (CCA) TREATED LUMBER ALONG A TOPOHYDROSEQUENCE Arsenic (As), Chromium (Cr), and Copper (Cu) are ubiquitous in soils as a result of anthropogenic and geogenic processes. The fate of As, Cr, and Cu in the environment is largely governed by their speciation, which is influenced by soil physiochemical properties. This study investigated the influence of soil physiochemical properties and landscape position on As, Cr, and Cu concentration and speciation in soils adjacent to Chromated Copper Arsenate (CCA) treated lumber fence posts. Concentration gradients showed elevated total As and Cu adjacent to the three fence posts, which decreased with increasing distance from the posts.
    [Show full text]
  • Fossil Calibrations for the Arthropod Tree of Life
    bioRxiv preprint doi: https://doi.org/10.1101/044859; this version posted June 10, 2016. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. FOSSIL CALIBRATIONS FOR THE ARTHROPOD TREE OF LIFE AUTHORS Joanna M. Wolfe1*, Allison C. Daley2,3, David A. Legg3, Gregory D. Edgecombe4 1 Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 2 Department of Zoology, University of Oxford, South Parks Road, Oxford OX1 3PS, UK 3 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PZ, UK 4 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author: [email protected] ABSTRACT Fossil age data and molecular sequences are increasingly combined to establish a timescale for the Tree of Life. Arthropods, as the most species-rich and morphologically disparate animal phylum, have received substantial attention, particularly with regard to questions such as the timing of habitat shifts (e.g. terrestrialisation), genome evolution (e.g. gene family duplication and functional evolution), origins of novel characters and behaviours (e.g. wings and flight, venom, silk), biogeography, rate of diversification (e.g. Cambrian explosion, insect coevolution with angiosperms, evolution of crab body plans), and the evolution of arthropod microbiomes. We present herein a series of rigorously vetted calibration fossils for arthropod evolutionary history, taking into account recently published guidelines for best practice in fossil calibration.
    [Show full text]