Kyana Events -- Members Only! Rhabdosomes Including the Sicula and Spinose Thecae

Total Page:16

File Type:pdf, Size:1020Kb

Kyana Events -- Members Only! Rhabdosomes Including the Sicula and Spinose Thecae http://www.amfed.org/sfms/index.html The KYANA Geological Society video produced by member Dave Shuffett can also be found on KET EncyloMedia internet site: http://www.ket.org/itvvideos/offering/science/ksroc.htm Electronic Edition of "LODESTAR" http://www.amfed.org/sfms/pdf/lodestar_may-june09.pdf MEETING TIME: 3rd Tuesday of each month - Social/Swap at 7:00 p.m. Meeting Starts at 7:30. Go To: http://www.kyanageo.org LOCATION: The Louisville Nature Center 3745 Illinois Avenue, Louisville, KY 40213 handicap accessible facility - visitors welcome http://www.louisvillenaturecenter.org DIRECTIONS: From the Watterson Expressway (I-264) -Take Exit 14 to Poplar Level Road North. Take Poplar Level Road to Trevilian Way (1.0 mi). Turn Right on to Trevilian Way. Take Trevilian Way to Illinois Avenue (0.2 mile) (to your left, Illinois Avenue is the first intersecting KYANA’s mission is to provide educational, road just before the Zoo entrance). recreational and social opportunities to those Turn left on to Illinois Avenue. interested in geological sciences and lapidary arts. Take Illinois Avenue to the Louisville Nature Center parking lot on your right (0.2 mile). Except for items specifically copyrighted by authors, other non-profit societies may use material in this newsletter. KYANA GEOLOGICAL SOCIETY Indiana and Kentucky / Volume 44, Number 9 THE GEMSCOOP c/o Sherry Lindle 6004 Highplace Dr Louisville, KY 40291 Revised July 7, 1999 at the AFMS Annual Meeting KYANA GEOLOGICAL SOCIETY Member of the The Southeast Federation of Mineralogical Societies, Inc. and American Federation of Mineralogical Societies “Code of Ethics” I will respect both private and public property and will do no collecting I will cause no willful damage to collecting materials and will take home only on privately owned land without the owner’s permission. what I can reasonably use. I will keep informed on all laws, regulations or rules governing I will practice conservation and undertake to utilize fully and well the materials I collecting on public lands and will observe them. have collected and will recycle my surplus for the pleasure and benefit of others. I will to the best of my ability, ascertain the boundary lines of property I will support the Rockhound project H.E.L.P. (Help Eliminate Litter Please) and on which I plan to collect. will leave all collecting areas devoid of litter, regardless of how found. I will use no firearms or blasting material in collecting areas. I will cooperate with field trip leaders and those in designated authority in all I will cause no willful damage to property of any kind, such as fences, collecting areas. signs, buildings, etc. I will report to my club or federation officers, Bureau of Land Management or I will leave all gates as found. other authorities any deposit of petrified wood or other materials on public land I will build fires in designated or safe places only and will be certain which should be protected for the enjoyment of future generations for public they are completely extinguished before leaving the area. educational and scientific purposes. I will discard no burning material - matches, cigarettes, etc. I will appreciate and protect our heritage of natural resources. I will fill all excavation holes which may be dangerous to livestock. I will observe the “Golden Rule,” will use “Good Outdoor Manners” and will at I will not contaminate wells, creeks or other water supplies. all times conduct myself in a manner which will add to the stature and public image of Rockhounds everywhere. 2009 BOARD OR DIRECTORS (with area code = long distance from Louisville) President Past President Director Betty Hansel (451-6953) Maryann Collings (502-257-2412) Luther Peak (239-8656) Vice-President Past President Director Herb Miracle (231-4154) Charlie Oldham (241-8755) Bill Beasy (245-5335) Treasurer Director Show Chair Michael Popp (797-0255) Kenny Popp (812-256-4764) Mike Whitehouse (905-4988) Secretary Director Newsletter Editor Blythe Collings (502-633-7644) Leo Gallaher (968-5535) Sherry Lindle (231-2268) Collect Cancelled Stamps for KYANA GEOLOGICAL SOCIETY Scholarship Program Membership Form Make check payable to: KYANA Geological Society Mail To: KYANA, c/o Treasurer Michael Popp, 4402 Birch View Drive, Louisville, KY 40299 Name: ___________________________________________________ Date Pd: _________ Address: _________________________________________________ Ck #__________ City: _________________________ State: ________ ZIP: ___________ E-mail Address for news: __________________________________________________ Telephone: Home (____) ______________ Business/Cell (____) __________________ Circle: Individual ($15 per yr) Family ($20 per yr) Student ($10 per yr) If family membership, list each name (include ages of children just for our info.): _______________________ _______________________ _______________________ _______________________ _______________ ___________________ Annual Dues are due by 1st of the year. 1 THE KYANA GEMSCOOP Monthly newsletter of the KYANA Geological Society in Louisville, Kentucky http://www.kyanageo.org/ Volume 44, Number 9 September 2009 Page 1 NEXT MEETING Tuesday, September 15th, 7:00 Social/Swap & 7:30 Program Program for September 15, 2009 by Herb Miracle, Vice-President Speaker: Dr. Katherine Bulinski is a Professor of Earth Science at Bellarmine University, Louisville, Kentucky. She teaches an “Evolution and Creationism” class at Bellarmine. Topic: “The Nature of Creationism and Evolution in Our Society” Message from the Prez. by Betty Hansel Greetings, the Lapidary Arts, and other subjects related to the Well we are all entering the “Fall Season”. It is Earth Sciences. (KYANA Video, fieldtrips, monthly a busy time for “Rock hounds”. There is so much programs and Club Show) going on; we should all find plenty to do. By the time we hold our next KYANA meeting, Section II many of you will have tales to share about the To cooperate with educational and scientific Cumberland trip with Kenny Popp. Charlie and I institutions and other clubs engaged in increasing the (and hopefully some of you) will have enjoyed the knowledge and public interest in the Earth Sciences Greenfield show. and in the conservation of our natural resources The weekend after our meeting Sept. 19-20, will (KYANA Video, outreach at “Falls”, shared fieldtrips be the “Falls Fossil Festival”. I hope you are and Club Show.) planning to attend and to donate some of your time to work in the KYANA booth. Please let Maryann Section III Collings know if you can take a two hour shift or To provide a means for exhibiting collections at more or just help when you can. See page 6 for all public gatherings. (KYANA Club Show and the goings on and Festival times. This is a great time Louisville Nature Center) to share your enjoyment of KYANA with others. We always gain a number of new members at the “Falls I believe the strength of KYANA is our of the Ohio”. It is a wonderful opportunity. diversity. Our members are interested in many facets When I share my thoughts on KYANA I tend to of “Our Earth”. We have members talented and revert to our Constitution to help me sum up what expert in many areas. Our members have been KYANA is all about. generous in sharing their expertise, by presenting I hope you have all had time to read our programs for us. We have also had programs Constitution for yourselves. It is on our website presented by guest speakers, to enrich our various under “Members Only” section. Let me quote from interests. the purposes: While there are many clubs specializing in one area, I think KYANA does an excellent job of Section I meeting our member’s interests in Fossils, Minerals To provide educational, recreational, and social and Lapidary Arts. I personally am glad to have been opportunities to those interested in the subjects of introduced to KYANA almost two decades ago by Geology, Mineralogy, Archaeology, Paleontology, David Horn at the St. James Art Fair. I know many 2 of you have been brought into KYANA by a member Special Announcement: who spoke highly of our club. Word of mouth is Cosby Keys the FIRST PRESIDENT and Life probably our best recruiter. Please continue to share Member of KYANA has built a beautiful table for your enthusiasm about KYANA with your friends our KYANA Auction. He cut cabs from Flint and acquaintances. You are our best ambassadors. Ridge, Ohio material and placed them in the Speaking of experts in our club, Shevvy Baker center of the beautiful hand built table he has had another drawing published in “Jewelry constructed. This is an amazing donation to Artist” (Formally Lapidary Journal) and a photograph KYANA. We will ask Cosby to set a minimum bid of a pin she created from one of her previous for the table. See picture on page 4. drawings. Way to go Shevvy!!!! I received a call from a former student of Allen On behalf of KYANA I want to express our Jewell’s trying to reach him. He could not say sincere appreciation to Cosby for his incredible enough good things about his classes with Allen at generosity. I know it will be a treasure for some William Holland. Allen is among the best when it lucky person in our club. comes to teaching silversmithing. He has also done some great presentations for our club on lapidary arts I hope we have a great turn out for our October over the years. auction. I know I am looking forward to it. Look How nice to be able to brag on our members a forward to seeing you all at the Sept 15th meeting. little! Our Auction is coming up in October. I hope Betty you are saving all your good STUFF to bring in and saving your pennies to buy goodies for yourself. The The next board meeting is scheduled for auction is always a favorite program.
Recommended publications
  • G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine
    DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GEOLOGY OF THE CRAIG QUADRANGLE, ALASKA By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Open-File Report 83-91 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and strati graphic nomenclature Menlo Park, California 1983 Geology of the Craig Quadrangle, Alaska By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Introduction This report consists of the following: 1) Geologic map (1:250,000) (Fig. 1); includes Figs. 2-4, index maps 2) Description of map units 3) Map showing key fossil and geochronology localities (Fig. 5) 4) Table listing key fossil collections 5) Correlation diagram showing Silurian and Lower Devonian facies changes in the northwestern part of the quadrangle (Fig. 6) 6) Sequence of Paleozoic restored cross sections within the Alexander terrane showing a history of upward shoaling volcanic-arc activity (Fig. 7). The Craig quadrangle contains parts of three northwest-trending tectonostratigraphic terranes (Berg and others, 1972, 1978). From southwest to northeast they are the Alexander terrane, the Gravina-Nutzotin belt, and the Taku terrane. The Alexander terrane of Paleozoic sedimentary and volcanic rocks, and Paleozoic and Mesozoic plutonic rocks, underlies the Prince of Wales Island region southwest of Clarence Strait. Supracrustal rocks of the Alexander terrane range in age from Early Ordovician into the Pennsylvanian, are unmetamorphosed and richly fossiliferous, and aopear to stratigraphically overlie pre-Middle Ordovician metamorphic rocks of the Wales Group (Eberlein and Churkin, 1970).
    [Show full text]
  • Silurian Rugose Corals of the Central and Southwest Great Basin
    Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation-------------------------------­ 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ----------------------------------------------­ 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study-------------------------------------------------------­ 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum
    [Show full text]
  • Some Reflections on the Beginning of the Oldest Corals Rugosa
    Latypov Y, Archiv Zool Stud 2019, 2: 008 DOI: 10.24966/AZS-7779/100008 HSOA Archives of Zoological Studies Original Article form a calcareous skeleton could occur at the beginning of the Early Some Reflections on the Cambrian (skeletal evolution during the Cambrian explosion). And from that moment it began a rapid development rugosa and wide- Beginning of the Oldest spread dissemination. In the early Caradoc already known genera of 5-6 separate taxonomically and morphologically groups – streptelas- Corals Rugosa ma tin, Cystiphyllum and columnar in. On average, Caradoc number genera doubled and by the end of the Ordovician have risen to 30 with Yuri Latypov* the dominance of single forms [3-5]. National Scientific Center of Marine Biology, Vladivostok, Russia First rugosa had only simple septa and full bottom with single additional plates, but by the beginning of the Late Ordovician plate tabulae acquire the ability to very wide variation, and by the end of Abstract the Late Ordovician kaliko blastes basal surface polyp’s single rugosa acquired the ability to secrete peripheral convex skeletal elements - Provides a conceptual theory of origin Rugosa. Discusses the septum (Paliphyllum). By the beginning of the Late Ordovician all possibility of the oldest single corals from the Cambrian forebears. With specific examples showing ways of their development and types of microstructures - lamellar, fibrous, monakant, golokant, rab- transmission of hereditary traits. Discusses the validity of the terms dakant, dimorfakant participated in the construction of the tabulae, “Tetracorallia” and “Rugosa” and their bilaterally. septa, plate and akanthin septa. The ability to secrete lamellar scleren- chyma vertical and horizontal skeletal elements like thickening until Keywords: Cambrian; Development; Origin; Rugosa their mutual fusion, was developed from the beginning rugosa stories and observed in many genera, or lesser greater extent until the end of their existence.
    [Show full text]
  • Mass Occurrence of the Large Solitary Rugose Coral Phaulactis Angusta at the Boundary Lower/Upper Visby Formation in The
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/290510570 Mass occurrence of the large solitary rugose coral Phaulactis angusta at the boundary Lower/Upper Visby Formation in the... Article in Gff -Uppsala- · January 2016 DOI: 10.1080/11035897.2015.1103780 CITATIONS READS 0 247 3 authors, including: Axel Munnecke Friedrich-Alexander-University of Erlangen-Nürnberg 116 PUBLICATIONS 2,597 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Paleobiology of graptolites View project All content following this page was uploaded by Axel Munnecke on 02 February 2016. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. GFF, 2016 http://dx.doi.org/10.1080/11035897.2015.1103780 Article Mass occurrence of the large solitary rugose coral Phaulactis angusta at the boundary Lower/Upper Visby Formation in the Silurian of Gotland, Sweden: palaeoecology and depositional implications FRIEDERIKE ADOMAT12, AXEL MUNNECKE1 and ERIKA KIDO3 Adomat F., Munnecke A.& Kido E., 2016: Mass occurrence of the large solitary rugose coral Phaulactis an- gusta at the boundary Lower/Upper Visby Formation in the Silurian of Gotland, Sweden: Palaeoecology and depositional implications. GFF, Vol 00, pp. 1–17. © Geologiska Föreningen. doi: http://dx.doi.org/10.1080/1 1035897.2015.1103780. Abstract: The boundary between the Lower and Upper Visby formations on Gotland (Sweden), which roughly correlates with the Llandovery–Wenlock boundary, is characterised by a mass occurrence of the large solitary rugose coral Phaulactis angusta.
    [Show full text]
  • Paleozoic Corals of Alaska
    Paleozoic Corals of Alaska Geologic and Paleogeographic Setting of Paleozoic Corals in Alaska Ordovician, Silurian, and Devonian Corals of Alaska Carboniferous Corals of Alaska A Preliminary Report Stratigraphic Distribution of Permian Corals in Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 823-A, B, C, D Paleozoic Corals of Alaska Geologic and Paleogeographic Setting of Paleozoic Corals in Alaska By MICHAEL CHURKIN, JR. Ordovician, Silurian, and Devonian Corals of Alaska By WILLIAM A. OLIVER, JR., CHARLES W. MERRIAM, and MICHAEL CHURKIN, JR. Carboniferous Corals of Alaska A Preliminary Report By AUGUSTUS K. ARMSTRONG Stratigraphic Distribution of Permian Corals in Alaska By CHARLES L. ROWETT GEOLOGICAL SURVEY PROFESSIONAL PAPER 823-A, B, C, D UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1975 UNITED STATES DEPARTMENT OF THE INTERIOR STANLEY K. HATHAWAY, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Paleozoic corals of Alaska. (Geological Survey professional paper ; 823) CONTENTS: Churkin, M. Jr. Geologic and paleogeographic setting of Paleozoic corals in Alaska. Oliver, W. A. Jr., Merriam, C. W. and Churkin, M., Jr. Ordovician, Silurian, and Devonian corals of Alaska, [etc.] Includes bibliographies and indexes. Supt. of Docs, no.: I 19.16:823-A,B,C,D 1. Corals, Fossil. 2. Paleontology Paleozoic. 3. Paleiontology Alaska. I. Churkin, Michael, 1932- II. Series: United States. Geological Survey. Professional paper ; 823. QE778.P34 563'.6'09798 75-619102 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02666-0 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Geologic and paleogeographic setting of Paleozoic corals in Alaska, by Michael Churkin, Jr.
    [Show full text]
  • Rugose Corals from the Upper Silurian of Scania, Sweden
    Title Rugose Corals from the Upper Silurian of Scania, Sweden Author(s) Kato, Makoto; Ezaki, Yoichi Citation 北海道大学理学部紀要, 21(4), 483-504 Issue Date 1986-02 Doc URL http://hdl.handle.net/2115/36740 Type bulletin (article) File Information 21_4_p483-504.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Jour. Fac. Sci., Hokkaido Univ., Ser. IV , vo l. 21 . no. 4, Feb ., 1986, pp.483-504. RUGOSE CORALS FROM THE UPPER SILURIAN OF SCAN lA, SWEDEN by Makoto Kato and Yoichi Ezaki (with 5 text-figures and 3 plates) Abstract Four species of rugose corals including (wo new species, Pilopliyllum keimorii and Phaulactis variabilis are described from (he upper Ludlovian Oved-Ramsasa Group of Scania, somhern Sweden. An aHemp( is made at re-classifyi ng and synonymizing genera belonging to the Streptelasmatidae, Lykophyllidae and Kyphophyllidae. Introduction In Scania, southern Sweden, Silu rian sediments are extensivel y developed along NW-SE trending outcrop belts (Text-fig. 1). Shales are predominant, and they have been stratigraphically classified as below (Regnell, 1960): Oved-Ramsasa Group ) """ Ludlow Colonus Shale Cyrtograptus Shale """ Wenlock Rastrites Shale """ Llandovery The topmost sequence, the Oved-Ramsasa Group is further divided into 4 units. The lowermost unit, di vision 1, the Bjorsjolagard limestone and shale, is composed of gray marls with lenses of limestone. Rugose and tabulate corals are known to occur in division 1, but none has been described as yet. In 1968 Mori collected some foss ils from a fossiliferous layer of division 1 rocks ex­ posed along a ditch about 30 m WNW of the bridge on the road from Bjorsjolagitrd to Ojupadal, Scania.
    [Show full text]
  • Stratigraphy and Structure of the Horseshoe Gulch Area, Etna and China Mountain Quadrangles, California
    AN ABSTRACT OF THE THESIS OF TED ANDREW ZDANOWICZ for theMASTER OF SCIENCE (Name of student) (Degree) in Geology presented on (Major) (Date) Title: STRATIGRAPHY AND STRUCTURE OF THE HORSESHOE GULCH AREA, ETNA AND CHINA MOUNTAIN QUADRANGLES, CALIFORNIA Redacted for Privacy Abstract approved: Dr. -"A.J. Boucot The Horseshoe Gulch area includes 16 square miles in the Eastern Paleozoic Belt of the Klamath Mountains geologic province north of Callahan, California.Fossiliferous Late Ordovician and Silurian limestones and unfossiliferous greywackes, arkoses, shales, mudstones, schists, and phyllites, and other terrigenous clastic rocks are exposed in a broad fault zone in the area of study.It is concluded that the limestones represent a clear, stable, and rela- tively shallow water environment of deposition.These limestones are found associated with a geosynclinal sequence of rock units. Eleven mappable units grouped into upper and lower thrust plates, are recognized. The fault zone in the Horseshoe Gulch area, approximately one mile wide, is characterized by a prominent folded thrust fault that is part of the Mallethead Thrust. The Mallethead Thrust, whose age is at least post-Late Silurian in the area, has placed upper plate unfossiliferous, pre-Cretaceous age chlorite grade metamorphic rocks over the Early Paleozoic unmetamorphosed limestones and clastics of the lower plate.The trace of the Mallethead Thrust is very sinuous and irregular. Stratigraphy and Structure of the Horseshoe Gulch Area, Etna and China Mountain Quadrangles, California
    [Show full text]
  • SILURIAN and DEVONIAN CORALS of JAPAN in Terms of Geotectonics
    ACT A PALA EON T 0 LOG ICA POLONICA Vol. 25 1980 No. 3-4 MAKOTO KATO, MASAO MINATO, ISAO NIIKAWA, MAKOTO KAWAMURA, HITOSHI NAKAI and SOlCHI HAGA SILURIAN AND DEVONIAN CORALS OF JAPAN KATO, M., MINATO, M., NIIKAWA, 1., KAWAMURA, M., NAKAI, H. and HAGA, S.: Silurian and Devonian corals of Japan. Acta Palaeont. Polonica, 25, 3/4, 557-566. January 1981. Coral assemblages and their faunal sequence for the Silurian and Devonian in four major regions of Japan are reviewed. In Yokokurayama the G, fauna with Hatysttes is Early to Middle Silurian and the G. fauna with Schedohatysttes is mainly Late Silurian. The Kawauchi Formation of Hikoroichi corresponds to G, and a part of G,. The Okuhinotsuchi Formation of Arisu is mainly correlatable with the G,. The Ohno fauna of Hikoroichi with Xystrtphyttum and the FUkuji fauna are both Early Devonian in age, but their composition is quite different from each other. The Nakazato fauna of Hikoroichi is Middle Devonian. These faunas are composed mostly of cosmopolitan genera. The development of coral faunas may indicate the strong contrast in litho- and biofacies between the Pacific side (outer zone of Southwest Japan and Northeast Japan) and the Japan Sea side (inner zone of Southwest Japan) during the Silurian and Devonian. Key w 0 r d s: coral biostratigraphy, paleogeography, Silurian, Devonian, Japan. Makoto Kato, Masao Mtnato, lsao Nttkawa, Makoto Kawamura, Httosht Nakat and Sotcht Haga, Department of Geology and Mtneralogy, Facutty of Sctence, Hokkatdo Untverstty, Sapporo, Japan. Received: September 1979. INTRODUCTION In terms of geotectonics, Japan has customarily been divided into Northeast and Southwest Japan, the latter being divided into the inner zone and outer zone.
    [Show full text]
  • Палеонтологічний Збірник 2018. № 50. С. 51–59
    ПАЛЕОНТОЛОГІЧНИЙ ЗБІРНИК PALEONTOLOGICAL REVIEW 2018. № 50. С. 51–59 2018. N 50. P. 51–59 UDC 563.3:51.733 (477.4) SOME REMARKS ON PALEOBIOLOGY OF CNIDARIA - CASE OF STUDY SILURIAN FOSSIL CORALS FROM PODILLIA, UKRAINE V. Grytsenko National natural history museum of NAS of Ukraine [email protected] Abstract. The article deal with paleobiological features of Silurian fossil corals re- constructed on study its taphonomy, structure of the skeletons with using paleoenvironment affinities and literature resources. Diversity Silurian Cnidarians was shown on many exam- ples studying samples. There were used many years collections of author. Special attention was paid on morphology and microstructure of the skeleton elements of different Cnidari- ans. Canadian researchers discovered fossil polyps of tabulate corals which show features provide probably exact their connection with modern Alcyonarians. Key words: Silurian, Cnidarians, structure, microstructure, diversity, Podollian Silurian geological sequence is well outcropped in the Dniester valley [1, 12, 14-16 etc.]. Part of the collections cropped from boreholes cores in the west part of Ukraine. Silurian fossil corals are relatively well studied. Many paleontologists paid an attention on the biologi- cal affinities of fossil cnidarians such as shape, measurements, speed of their increase, mode of the biomineralization, ways of classification, and so on. In the last time occurs some publica- tion deal with shape and structure of coral polyps. N.N. Jakovlev [6] thought that hornlike shape of the rugosans corals depend on currents and it is reason of bilateralism. The conduct of life of fossil corals was discussed in investigations of B.S. Sokolov [12 etc], B.V.
    [Show full text]
  • UNIVERSITY of CALIFORNIA RIVERSIDE Molecular Organic
    UNIVERSITY OF CALIFORNIA RIVERSIDE Molecular Organic Geochemical Records of Late Ordovician Biospheric Evolution ADissertationsubmittedinpartialsatisfaction of the requirements for the degree of Doctor of Philosophy in Geological Sciences by Megan Kimberly Rohrssen December 2013 Dissertation Committee: Dr. Gordon D. Love, Chairperson Dr. Timothy W. Lyons Dr. Woodward W. Fischer Copyright by Megan Kimberly Rohrssen 2013 The Dissertation of Megan Kimberly Rohrssen is approved: Committee Chairperson University of California, Riverside Acknowledgments Thank you, Gordon for introducing me to this field, in all its potential and pitfalls, and for giving me tools to work in it. Thank you to my committee members Tim Lyons and Woody Fischer, and co-authors David Fike and Seth Finnegan. Anything written here that’s worth reading probably is so because of your help. I am grateful to the entire faculty in UCR Earth Sciences for helping build such a positive environment, and for being so generous with your time and knowledge. Thank you Chao Li for so much patience in helping me grow less afraid of breaking things by teaching me to fix them. Mark Williams, thank you for putting up with my novice mentorship at the beginning and dissertation angst towards the end. Thanks, Steve Bates for all the help with the lab, like figuring out the dozen ways to break a rock powdering machine. Thank you Lidya Tarhan, Lucas Joel, Natascha Riedinger, Kayla Kroll, Jacqui Gilchrist, Eli Brewer, Julian Lozos, Cassy Rose, Amy Kelly, Corrie Neighbors, Kenny Ryan, Leanne Hancock, Robyn Dahl, Sarah Henry, and Joanna Oseguera for comradeship, commiseration, and occasional cat-sitting. Thank you Carina Lee and Emily Haddad (and Alex Zumberge, even though you just started!) for taking over the lab so ably.
    [Show full text]
  • Catalogue of Type Specimens of Fossils in the Australian Museum
    AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Fletcher, Harold O., 1971. Catalogue of type specimens in the Australian Museum, Sydney. Australian Museum Memoir 13: 1–167. [31 December 1971]. doi:10.3853/j.0067-1967.13.1971.423 ISSN 0067-1967 Published by the Australian Museum, Sydney nature culture discover Australian Museum science is freely accessible online at http://publications.australianmuseum.net.au 6 College Street, Sydney NSW 2010, Australia THE AUSTRALIAN MUSEUM, SYDNEY MEMOIR 13 Catalogue of Type Specimens in the Australian Museum, Sydney By H. O. FLETCHER Published by Order of the Trustees of the Australian Museum Sydney, New South Wales, Australia 1971 95540-1 ABSTRACT This catalogue is a classified list of all type specimens of the fossil plants, invertebrates, and vertebrates, including specimens mentioned in literature, in the collections of the Australian Museum, Sydney. Also included are plaster replicas (plastotypes) of important type specimens, and, when known, the institution in which the original specimen is stored is given. Genera and species are arranged in alphabetical order in their appropriate larger biological groups. The cata­ logue, containing almost 4,000 specimens, is complete to December, 1968. INTRODUCTION Type specimens are listed in alphabetical order according to genera and species in their various groups such as Foraminifera, Anthozoa, Pelecypoda, etc. Terminology of the types fol­ lows generally accepted usage-holotypes, paratypes, lectotypes, paralectotypes, syntypes, neo­ types, and hypotypes. The latter may include any described specimen which does not fall into the preceding ,categodes. When a new species has been based on a single specimen it has been listed as a holotype.
    [Show full text]
  • Silurian Rugose Corals of the Klamath Mountains Region, California
    Silurian Rugose Corals of the Klamath Mountains Region, California GEOLOGICAL SURVEY PROFESSIONAL PAPER 738 Silurian Rugose Corals of the Klamath Mountains Region, California By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 738 A descriptive, taxonomic, and stratigraphic study of Klamath Mountains Silurian Rugosa UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600033 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1 (paper cover) Stock Number 2401-2077 CONTENTS Page Geologic correlation, etc. Continued page Abstract. _ --_-_--_----_--_______-__________________ 1 Correlation with Silurian rocks in the Great Basin __ 20 Introduction. ______________________________________ 1 Correlation with eastern North America, Europe, Objectives and scope. ___________________________ 2 and Australia._________----__________--___-__ 20 History of investigation. ________________________ 2 Eastern North America____________________ 20 Methods of study______ _________________________ 3 Europe ____________________________________ 21 Acknowledgments. __ _ ___________________________ 4 Australia-___----------------_----------__ 22 Distribution of Paleozoic rocks in the Klamath Moun­ Geologic age of Paleozoic rocks in the northeastern Kla­ tains region. _____________________________________ 4 math subregion___--______________________________ 22 Paleozoic strata of the northeastern Klamath subregion_ 6 Gazelle Formation of Silurian age, Willow Creek Depositional environment and origin of the northeastern Klamath subregion coral-bearing deposits.___________ 24 6 Coral-bearing limestone conglomerate.____________ 25 Bonnet Rock section- _--___-___-_-___-______ 10 Origin of coralline limestones in the Gazelle For­ Chastain Ridge section- _____________________ 11 mation- -_-_--_-_________-____-___------_____ 26 Mallethead Ridge section.
    [Show full text]