Plant Microfossils from the Bruhn Lignite

Total Page:16

File Type:pdf, Size:1020Kb

Plant Microfossils from the Bruhn Lignite University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 6-1957 Plant Microfossils from the Bruhn Lignite Robert E. McLaughlin University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Botany Commons Recommended Citation McLaughlin, Robert E., "Plant Microfossils from the Bruhn Lignite. " PhD diss., University of Tennessee, 1957. https://trace.tennessee.edu/utk_graddiss/3251 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Robert E. McLaughlin entitled "Plant Microfossils from the Bruhn Lignite." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Doctor of Philosophy, with a major in Botany. A. J. Sharp, Major Professor We have read this dissertation and recommend its acceptance: Royal E. Shanks, Gordon Hunt, Harry Klepsen, George Swingle Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) May 21, 1957 To the Graduate Council: I am submitting herewith a thesis written by Robert E. McLaughlin entitled 11Plant Microfossils from the Bruhn Lignite." I recommend that it be accepted partial fulfillment of the requirements for the degree in · of Doctor of Philosophy, with a major in Botaqr. We have read this thesis and recommend its acceptanc • Accepted'�ua�r for the Council: PLANT THE MICROFOSSILS FROM BRUHN LIGNITE A THESIS Submitted to The Graduate Council of I The University of Tennessee in Partial Fulfillment of the Requirements for the degree of Doctor of Philosophy Robert E. �IcLaughlin June 1957 - .. ..-· ·-.. .' ACKNOWLEDGEMENTS During the developmental stages of the project described in these pages, and in the preparation of the manuscript, many persons guided the writer1 s efforts and otherwise made material contributions. To those listed below, the writer is especially indebted and hereby expresses his appreciation. To A. Sharp and members of the Cornmittee for their valuable Dr. J. criticisms and suggestions, and, particularly for their continuing faith in the ultimate realization of objectives, the writer is profoundly grate­ ful. Professor H. K. Brooks, now at the University of Florida, was an original member of the Committee and, along with Dr. Sharp, accompanied the writer on initial field reconnaissance. Alfred Traverse,· during the Swruner of 19.54, made available Dr. the accumulated products of his own research, including unpublished manu­ script, reference material, and a wealth of information. Dean L. R. Hesler, College of Liberal Arts, The University of Tennessee, made it possible to accept Dr. Traverse's invitation to visit the Bureau u. s. of Mines Lignite Laboratory, Grand Forks, North Dakota, by providing travel expenses. Later association with Traverse, now with Shell Dr. Development Corporation, has increased the writer•s obligation to him in ways. many The Southern Fellowships Fund, an agency of the Council of Southern Universities, Inc., granted the writer a generous fellowship award that permitted him to spend the academic year 1955-1956 at The Biological Laboratories, Harvard Universi'tzy'. At the latter institution, it was the 381.296 iii writer's distinct privilege to share the laboratory facilities and to participate in the research activities of Elso Barghoorn, his Dr. s. associates, and students. The vast experience and knowledge of Dr. Barghoorn and Bailey in paleobotany and related botanical fields, Dr. I. W. including pollen and spore research, were drawn upon freely by the writer during that time and continue to be an inspiration. At the same institu­ tion, officials of the Gray Herbarium and the Arnold Arboretum graciously offered the use of their facilities. Stephenson and F. Stearms MacNeill, United States Dr. L. w. Geological Survey, Washington and Denver, respective:cy, offered valuable suggestions and supplied information through correspondence for which the writer is indebted. E. Cushing, District Engineer, and R. M. Richardson, 14. Geologist, with the United States Geological Survey, Ground Water Branch, Memphis, and Richard G. Stearns, Tennessee DiVision of Geology, Dr. Nashville, provided the opportunity for examining revised maps and other unpublished data during the early stages of the investigation, and were particular:cy encouraging. Raymond L. Schreurs, Geologist, former:cy with the Memphis office, accompanied the writer in the field and was especia.J.4r helpful in making stratigraphic determinations as well as in bringing the whole geologic problem into focus. For technical assistance rendered to the writer at various times and in several places, all of which contributed directly or indirectly to the completion of this manuscript, the writer is obligated to the follow­ ing fellow students and associates: Herbert A. Tiedemann, now with the Tennessee Division of Geology, Knoxville; Eduard Shaw, now at the r. iv University of Kansas; Donald R. Whitehead and Jack A· Wolfe, Harvard University; Charles L. n-otter, now with the Shell Development Corpora­ tion, Houston; and Edward E. c. Clebsch andWilliam M. McMaster, The University of Tennessee, Knoxville . TABLE OF CONTENTS PAGE INTRODUCTION • • • • • • • • • • • • • • • • • • • • l GEOLOGICAL SETTING • • • • • • • • • • • • 3 Tertiar,y Deposits •••••••• • • • • • • • • • • • • • • • 12 • • • • • • • • • • • • • • • • • • 15 THE BRUHN PIT Location • • • • • • • • • • • • • • • • • • • • • • • • • 15 Lithology o • • • • • • • • • • • • • • • • • • • • 0 15 Sampling • • • • • • • • • • • • • • • • • 18 Stratigraphic Considerations • • • • • • • • • • • • • • 19 Paleobotanical Relationships • • • • • • • • • • • • • • 22 METHODOLOGY • • • • • • • • • • • • • • • • • • • • • • • 25 Previous Applications • • • • 0 • • • • • • • • • • • • • 25 Triassic • • • • • • • • • • • • • • • • • • • • • • 28 Jurassic • • • • • • • • • • • • • • • • • • • • • 29 Cretaceous • • • • • • • • • • • • • • • • • • • • • • 0 • 32 Tertiary • • • • • • • • • • • • • • • • • • • • • • • • • 46 Quaternar,y • • • • • • • • • • • • • • • • • • • • • • • 48 Separatory Technique • • • • • • • • • • • • • • • • • • • 49 Comparison of Results • • • o • • • • • • • • • • • • • • 0 • • 53 SYSTEMATIC DESCRIPTION • • • • • • • • • • • • • • • • • • • 59 S,ystematic Methods • • • • • • • • • • • • • • • • • • • • • • 59 Sporomorphs from the Bt-ubn Lignite • • • • • • • • • • • • • 71 DISCUSSION OF RESULTS • • • • 0 • • • • • • • • • • • • • 115 other Plant Microfossils • • • • • • • • • • • • • • • • l23 vi PAGE Comparison With other Cretaceous Microfossil Studies • • • • • • 123 SUMMARY AND CONCLUSIONS • • • • • • • • • • • • • • • • • • • • • • 125 LIST OF REFERENCES • • • • • • • • • • • • • • • • • • • • • • • • 128 APPENDIX A • • • • • • • • • • • • • • • • • • • • • • • • • • • • 14.3 APPENDIX B • • • • • • • • • • • • • • • • • • • • • • • • • • • • 158 APPENDIX C • • • • • • • • • • • • • • • • • • • • • • • • • • • • 173 LIST OF ILLUSTRATIONS FIGURE PAGE 1. Cyclic interpretation of geomorphological development in the Mississippi Embayment Region • • • • • • • • • • • 4 2. Generalized areal geology of the Upper Nississippi Embayment (after Stearms and Armstrong, 1955) • • • • • • 6 3. Distribution of Upper Cretaceous deposits in �lest Tennessee with generalized stratigraphical relation- ships based on Wade (1926) • • • • . • • . • . • . • • 8 4. Location and stratigraphical position of the Bruhn lignite • • . • . • . • . • . • . • • . • • 16 5. Photograph of the Bruhn pit • . • . • . • • • • • . • 17 6. Illustration of master key and sample analysis card. used to systematize morphological data ••• . • • • • 81 1. Frequency distribution of plant microfossils in the Bruhn lignite and comparative representation of higher taxonomic categories • • • • • • • • • • • • • • • 113 PLATE • • 143 I-VII. Photomicrographs of Bruhn microfossils (Appendix A) INTRODUCTION The collection and preliminary examination of fossiliferous materials from West Tennessee, begun in the fall of 1952 with the aid an d encouragement of Dr. A. J. Sharp, convinced the writer that the opportunity to extend present knowledge of early vegetational history in the area was substantial. Despite the fact that the region west of the Tennessee River has yielded a considerable amount of plant fossil evidence, mainly in the form of lea£ impressions, man;y unsolved problems remain. From the botanical point of view, the identification of fossil plants based on the single criterion of leaf morphology, as has been attempted in many cases, has serious limitations {Odell, 1932; Arnold.t 1947, pp. 338-339). Furthermore, the restricted representation inherent with this mode o£ fossilization, and the special set o£ conditions under which it is operative have led to qualitative and quantitative interpre­ tations that are questionable. In recent years, the vulnerability of time-honored correlation procedures has been recognized by many geologists. Paleontology developed as a stratigraphic tool with
Recommended publications
  • A Stable Isotopic Investigation of Resource Partitioning Among Neosauropod Dinosaurs of the Upper Jurassic Morrison Formation
    A stable isotopic investigation of resource partitioning among neosauropod dinosaurs of the Upper Jurassic Morrison Formation Benjamin T. Breeden, III SID: 110305422 [email protected] GEOL394H University of Maryland, College Park, Department of Geology 29 April 2011 Advisors: Dr. Thomas R. Holtz1, Jr., Dr. Alan Jay Kaufman1, and Dr. Matthew T. Carrano2 1: University of Maryland, College Park, Department of Geology 2: National Museum of Natural History, Department of Paleobiology ABSTRACT For more than a century, morphological studies have been used to attempt to understand the partitioning of resources in the Morrison Fauna, particularly between members of the two major clades of neosauropod (long-necked, megaherbivorous) dinosaurs: Diplodocidae and Macronaria. While it is generally accepted that most macronarians fed 3-5m above the ground, the feeding habits of diplodocids are somewhat more enigmatic; it is not clear whether diplodocids fed higher or lower than macronarians. While many studies exploring sauropod resource portioning have focused on differences in the morphologies of the two groups, few have utilized geochemical evidence. Stable isotope geochemistry has become an increasingly common and reliable means of investigating paleoecological questions, and due to the resistance of tooth enamel to diagenetic alteration, fossil teeth can provide invaluable paleoecological and behavioral data that would be otherwise unobtainable. Studies in the Ituri Rainforest in the Democratic Republic of the Congo, have shown that stable isotope ratios measured in the teeth of herbivores reflect the heights at which these animals fed in the forest due to isotopic variation in plants with height caused by differences in humidity at the forest floor and the top of the forest exposed to the atmosphere.
    [Show full text]
  • Critical Review of Research on the Lower Jurassic Flora of Poland
    Acta Palaeobotanica 53(2): 141–163, 2013 DOI: 10.2478/acpa-2013-0015 Critical review of research on the Lower Jurassic flora of Poland GRZEGORZ PACYNA Department of Palaeobotany and Palaeoherbarium, Institute of Botany, Jagiellonian University, Lubicz 46, 31-512 Kraków, Poland; e-mail: [email protected] Received 7 October 2013; accepted for publication 5 December 2013 ABSTRACT. The Lower Jurassic plant macrofossils of Poland are poorly known. Relatively rich sources of fossils are found in only a few outcrops in the Holy Cross Mountains. Other described plant remains come from drill cores taken from most areas of Poland, but as a rule these are single specimens. The only professional descriptions of Lower Jurassic macroflora are papers by Raciborski, Makarewiczówna, and a team of researchers consisting of Reymanówna, Barbacka, Ziaja, and Wcisło-Luraniec. Raciborski’s fossil collection is still available for research and revision. Such work is in progress. The collection described by Makarewiczówna contained many interesting speci- mens but unfortunately the majority of them are now missing. Stratigraphic research by geologists has provided some new specimens from drill cores and outcrops in the Holy Cross Mountains but these have not been subjected to detailed palaeobotanical analysis. The palynology of the Lower Jurassic was focused on biostratigraphy from the outset of that research. As an outcome it provided spore-pollen and megaspore zonations for Lower Jurassic strata in Poland. The Polish Lower Jurassic flora is comprised of ferns (very numerous), lycopsids, sphenopsids, cycadaleans, bennettitaleans, gnetaleans, ginkgoaleans, and conifers. This flora is taxonomically poorer than the equally old and geographically close floras of Denmark, Sweden, and Germany.
    [Show full text]
  • Tiof\Lal ORGANIZATION of PALAEOBOTANY
    I p INTERN,~TIOf\lAL ORGANIZATION OF PALAEOBOTANY INTERNATlONAL UNION Of BIOLOGICAL SC1ENCES Secr"tary: Dr. M. C. BOULTER ·SECTION FOR PALAEOBOTANY N. E. London Polytechnic, ? ..sident: Prot. W.G. CHALONEI'\. UK Romfoyo Road, Vice Presidents: !>cof. c. 30UREAU, FRANCE London, E15 412. England. Dr. S. ARCHANGHSKY, ARGENTINA Dr. S.V. MEYEN, USSR DECEMBER 1'383 lOP NE\~S .......................................... REPORTS OF RECENT MEETINGS ......................... 1 FORTHCOMING ,'1EETINGS .......... , .................... 4 OBITUI\RIES ......................................... 5 REQUESTS FeR HE!...? ................................. 7 NE',.,IS OF ! ND! VI JU)1,LS ............................ " .. 7 SALES OF FOSS I LS .................................... 8 BiaLIOGRAPHIES ......... , ........................... 8 RE'/!SION OF INDI)1,N SPEC,ES OF Gl')ssopteris ......... l0 RECENT °UBL I CAT IONS ............................... .11 SOOK REV I E'WS .................... , ... , .... " ........ 11 PLEASE MAIL NEWS AND CORRESPONDENCE TO YOUR REGIONAL REPRESENTATIVE OR TO THE SECRETARY FOR THE NEXT NEWSLETTER 23. The views expressed in the newsletter are those of its correspondents and do not necessarily refiect the pOI icy of iOP. lOP NEWS Many members of lOP are behind with their pay~ent5 of dues now set at £4.00 or us~3.i)O 3 year. Please use the attached form when making your payment. If you pay in £ sterling directly to London please remember to use a cheque which can be negotiated at a London bank. I!\FOPJ-I!\L BUSINESS r;EUI~IG OF lOP, Edmonton, Canada, August 1384 ThE:r'e is to he 2n inforrlal business meeting of lOP during the seco;:d lOP conference next summer. As at ReDding in 1980 its purpose is tC give the membership a chance to 2xpress its views on how lOP is operating; the Executive Committee must be accoun:ab:e to the membership and these informal meetings are one way of achieving ·:his.
    [Show full text]
  • A Reappraisal of Mississippian (Tournaisian and Visean) Adpression Floras from Central and Northwestern Europe
    Zitteliana A 54 (2014) 39 A reappraisal of Mississippian (Tournaisian and Visean) adpression floras from central and northwestern Europe Maren Hübers1, Benjamin Bomfleur2*, Michael Krings3, Christian Pott2 & Hans Kerp1 1Forschungsstelle für Paläobotanik am Geologisch-Paläontologischen Institut, Westfälische Zitteliana A 54, 39 – 52 Wilhelms-Universität Münster, Heisenbergstraße 2, 48149 Münster, Germany München, 31.12.2014 2Swedish Museum of Natural History, Department of Paleobiology, Box 50007, SE-104 05, Stockholm, Sweden Manuscript received 3Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Ludwig- 01.02.2014; revision Maximilians-Universität, and Bayerische Staatssammlung für Paläontologie und Geologie, Richard- accepted 07.04.2014 Wagner-Straße 10, 80333 Munich, Germany ISSN 1612 - 412X *Author for correspondence and reprint requests: E-mail: [email protected] Abstract Mississippian plant fossils are generally rare, and in central and northwestern Europe especially Tournaisian to middle Visean fossil floras are restricted to isolated occurrences. While sphenophytes and lycophytes generally are represented by only a few widespread and long-ranging taxa such as Archaeocalamites radiatus, Sphenophyllum tenerrimum and several species of Lepidodendropsis and Lepido- dendron, Visean floras in particular show a remarkably high diversity of fern-like foliage, including filiform types (Rhodea, Diplotmema), forms with bipartite fronds (Sphenopteridium, Diplopteridium, Spathulopteris, Archaeopteridium), others with monopodial, pinnate fronds (Anisopteris, Fryopsis) and still others characterized by several-times pinnate fronds (e.g., Adiantites, Triphyllopteris, Sphenopteris, Neu- ropteris). Most of these leaf types have been interpreted as belonging to early seed ferns, whereas true ferns seem to have been rare or lacking in impression/compression floras. In the upper Visean, two types of plant assemblages can be distinguished, i.e., the northern Kohlenkalk-type and the south-eastern Kulm-type assemblage.
    [Show full text]
  • Transformative Paleobotany
    Chapter 6 Lower Permian Flora of the Sanzenbacher Ranch, Clay County, Texas William A. DiMichele1, Robert W. Hook2, Hans Kerp3, Carol L. Hotton1,4, Cindy V. Looy5 and Dan S. Chaney1 1NMNH Smithsonian Institution, Washington, DC, United States; 2The University of Texas at Austin, Austin, TX, United States; 3Westfälische Wilhelms-Universität Münster, Münster, Germany; 4National Institutes of Health, Bethesda, MD, United States; 5University of California Berkeley, Berkeley, CA, United States 1. INTRODUCTION 1985; Broutin, 1986; Popa, 1999; Steyer et al., 2000; Wagner and Mayoral, 2007; Bercovici and Broutin, 2008; Since 1989, field parties supported by the U.S. National Barthel, 2009; Wagner and Álvarez-Vázquez, 2010; Museum of Natural History have obtained large collections Barthel and Brauner, 2015). Furthermore, because this of mainly Permian plant fossils from north central Texas. locality was collected on three occasions over a time period This work was undertaken to study known localities and to of 50 years and by different parties, comparative analysis of find new fossiliferous deposits that would contribute to a the Sanzenbacher collections provides a basis for assessing better understanding of floral and paleoenvironmental sites that have comparable histories. changes within the region during the early Permian. From the outset, the effort was interdisciplinary and grew, through the contributions of nearly 20 paleobotanists, 2. GEOLOGY palynologists, invertebrate and vertebrate paleontologists, Clay County is the only county in the Permo-Carboniferous and sedimentary geologists of several subdisciplines, to be outcrop belt of north central Texas that lacks marine rocks. quite comprehensive. Our reporting of results, however, has These alluvial sediments accumulated east of a broad been influenced by unexpected developments, including the coastal plain that bordered the Eastern Shelf of the Midland discovery of new plant-fossil assemblages in areas once Basin.
    [Show full text]
  • Botanical Investigations Into the Fossil Flora of Eriksdal in Fyledalen, Scania
    SVERIGES GEOLOGISKA UNDERSOKNING SER C NR 633 AVHANDLINGAR OCH UPPSATSER ARSBOK 62 NR 4 HANS TRALAU BOTANICAL INVESTIGATIONS INTO THE FOSSIL FLORA OF ERIKSDAL IN FYLEDALEN, SCANIA II. THE MIDDLE JURASSIC MICROFLORA STOCKHOLM 1968 SVERIGES GEOLOGISKA UNDERSOKNING SER C NR 633 ARSBOK 62 NR 4 HANS TRALAU BOTANICAL INVESTIGATIONS INTO THE FOSSIL FLORA OF ERIKSDAL IN FYLEDALEN, SCANIA Il. THE MIDDLE JURASSIC MICROFLORA STOCKHOLM 1968 Editors: Hans Tralau and Per H. Lundegårdh C. DAVIDSONS BOKTRYCKERI AB, VÄXJÖ 1968 BOTAN!CAL !NVEST!GAT!ONS IN ERIKSDAL 3 CONTENTS I. Abstract . 4 II. Preface . 5 III. Introduction . 5 IV. Systematic description of microspores found in situ . 10 V. Systematic description of dispersed microspores and pollen grains 18 VI. Presurned re-bedded specimens of microspores and pollen grains . 98 VII. Stratigraphical results . 99 VIII. Acknowledgements . 105 IX. References . 106 X. Index of genus and species names . 126 XI. Plates I to XXVI . 132 4 HANS TRALAU I. ABSTRACT Mesozoic sediments at Eriksdal in the valley of the Fyle river, SE Scania, southern Sweden have been investigated with regard to their contents of microspores and pollen grains. The microflora found confines the age of the sediments to the Bajocian and Bathonian. The first group of pollen grains and microspores, which confines the age deter­ mination to the Bajocian and Bathonian, is widely distributed in the Liassic but has its uppermost occurrence in different stages, preferably in the Bajocian or the Bathonian, of the Middle Jurassic in Europe. These are Concavisporites subgranu­ losus, Leptolepidites major, Lycopodiacidites rugulatus, Todisporites major, Cala­ mospora mesozoica, Trilites rariverrucatus, Eucommiidites granulosus, and Chas­ matosporites apertus.
    [Show full text]
  • 1485 Haug.Vp
    Arthropod cuticles from the upper Viséan (Mississippian) of eastern Germany JOACHIM T. HAUG, MAREN HÜBERS, CAROLIN HAUG, ANDREAS MAAS, DIETER WALOSZEK, JÖRG W. SCHNEIDER & HANS KERP Arthropod cuticles from the Mississippian (Early Carboniferous, Viséan) Hainichen Subgroup, Erzgebirge Basin, have been encountered in bulk-macerated samples from a roadcut exposure in Chemnitz-Glösa, eastern Germany. The cuti- cles are described in detail and compared with larger faunal components known from the same horizons. Part of the spec- imens represent remains of arthropod appendages, while others, though exhibiting fine detail of surface texture, could not be assigned to certain body regions. In all cases it remains difficult to assign the fragments from Chemnitz-Glösa to taxa known from the Hainichen Subgroup or from other localities yielding arthropod remains of similar preservation. However, it is suggested that several specimens may represent scorpion remains, either limb parts (piece of the pedipalp, distal claw of walking limb) or fragments of the body surface. One specimen, a single appendage element, could repre- sent the first insect fragment from this locality. All fragments appear to be terrestrial faunal components. Chemnitz-Glösa is one of the very few Lower Carboniferous localities to yield remains of terrestrial arthropods and the only one outside Scotland. • Key words: Mississippian, Lower Carboniferous, arthropod cuticles, Erzgebirge Basin. HAUG, J.T., HÜBERS, M., HAUG, C., MAAS, A., WALOSZEK, D., SCHNEIDER,J.W.&KERP, H. 2014. Arthropod cuti- cles from the upper Viséan (Mississippian) of eastern Germany. Bulletin of Geosciences 89(3), 541–552 (7 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received September 20, 2013; accepted in revised form January 13, 2014; published online May 6, 2014; issued June 9, 2014.
    [Show full text]
  • Field Trip 2 Late Paleozoic and Mesozoic Terrestrial Environments in the Dolomites and Surrounding Areas 71-116 Geo.Alp, Vol
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Geo.Alp Jahr/Year: 2016 Band/Volume: 013 Autor(en)/Author(s): Kustatscher Evelyn, Bernardi Massimo, Petti Fabio Massimo, Avanzini Marco, Tomasoni Riccardo Artikel/Article: Field trip 2 Late Paleozoic and Mesozoic terrestrial environments in the Dolomites and surrounding areas 71-116 Geo.Alp, Vol. 13 2016 71 - 116 Field trip 2 Late Paleozoic and Mesozoic terrestrial environments in the Dolomites and surrounding areas Evelyn Kustatscher1,2, Massimo Bernardi3,4, Fabio Massimo Petti3,5, Marco Avanzini3 & Riccardo Tomasoni3 1 Naturmuseum Südtirol, Bindergasse 1, 39100 Bozen/Bolzano, Italy; e-mail: [email protected]; 2 Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Ludwig-Maximilians- Universität and Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 München, Germany; 3 Museo delle Scienze di Trento, Corso del Lavoro e della Scienza 3, 38123 Trento, Italy; e-mail: [email protected], [email protected], [email protected], [email protected]; 4 School of Earth Sciences, University of Bristol, Bristol BS81RJ, UK; 5 PaleoFactory, Dipartimento di Scienze della Terra, Sapienza Università di Roma, P.le Aldo Moro 5, 00185, Roma, Italy. 1 Topics and highlights of the excursion Mojsisovics, 1879, 1882; Mojsisovics et al., 1895; Bittner, 1892; Brack et al., 2005, Mietto & Man- The Southern Alps represent
    [Show full text]
  • An Overview of the Fossil Record of Climbers: Bejucos, Sogas, Trepadoras, Lianas, Cipós, and Vines
    Rev. bras. paleontol. 12(2):149-160, Maio/Agosto 2009 © 2009 by the Sociedade Brasileira de Paleontologia doi:10.4072/rbp.2009.2.05 AN OVERVIEW OF THE FOSSIL RECORD OF CLIMBERS: BEJUCOS, SOGAS, TREPADORAS, LIANAS, CIPÓS, AND VINES ROBYN J. BURNHAM Museum of Paleontology, University of Michigan 1109 Geddes Avenue, Ann Arbor, MI 48109-1079, USA. [email protected] ABSTRACT – One of the most obvious life forms in tropical forests today is the liana, which laces together tree canopies and climbs the dark interiors of forests with snake-like stems. Lianas are ecologically important in extant, forested ecosystems, both intact and disturbed. Their contribution to forest diversity, food resources, structural complexity, and plant-animal interactions are recognized, but rarely studied. Climbers (woody lianas and herbaceous vines) are viewed as everything from diversity contributors to forest growth inhibitors by modern ecologists and systematists. Climbers take advantage of the structural support of trees to invest proportionately more in vegetative and reproductive organs, resulting in proliferation at the individual and species level. Today the climbing habit is dominated by angiosperm species, with only a minor contribution from ferns plus a single non-angiosperm seed plant genus, Gnetum. This contribution reports the establishment of the newly established database, Fossil Record of Climbers (FRC) that documents more than 1100 records of climbing plants from the Paleozoic to the Quaternary using published literature on the fossil record. The diversity of climbers in the fossil record prior to the evolution of angiosperms is explored, posing the hypothesis that climbers of the past had a similarly important role in tropical forests, at least in the Paleozoic.
    [Show full text]
  • Agora Paleobotanica Un Hommage À / a Tribute to Bernard Renault (1836-1904)
    Agora Paleobotanica Un hommage à / A tribute to Bernard Renault (1836-1904) 6-9/07/2015, Autun (France) Résumés - Abstracts Agora Paleobotanica Un hommage à / A tribute to Bernard Renault (1836-1904) 6-9/07/2015, Autun (France) Comité d’organisation / Organizing Committee Anais BOURA – Université Pierre et Marie Curie, Paris Jean BROUTIN – Université Pierre et Marie Curie, Paris Dominique CHABARD – Muséum d’Histoire Naturelle Jacques de La Comble, Autun Anne-Laure DECOMBEIX – CNRS-UMR AMAP, Montpellier Jean GALTIER – CNRS-UMR AMAP, Montpellier Georges GAND – Université de Bourgogne, Dijon Evelyne JONDOT– Muséum d’Histoire Naturelle Jacques de La Comble, Autun Brigitte MEYER-BERTHAUD – CNRS-UMR AMAP, Montpellier LUNDI/MONDAY Museum d’Histoire Naturelle Jacques de La Comble 16h00-17h30 Accueil des participants Participant arrival 17h30-18h Conférence introductive/ Opening talk Georges GAND. Le Bassin Permien d’Autun 18h-19h30 Allocution de bienvenue du maire - Apéritif de bienvenue Welcome address by the mayor - Welcome drinks MARDI /TUESDAY Salon d’honneur de la mairie d’Autun/ City Hall Session 1: PALEOZOÏQUE I Modérateurs/Chairs: Philippe GERRIENNE & Evelyn KUSTATSCHER 8h30-9h00 Jean GALTIER. Keynote: Bernard Renault (1836-1904), his life, works and paleobotanical heritage. 9h-9h20 Christine STRULLU-DERRIEN & P. KENRICK. Palaeozoosporites renaultii, a new fungus in the rooting system of the Rhynie Chert plant Asteroxylon mackiei. 9h20-9h40 ∗ Gonzalo RIAL, B. CASCALES-MIÑANA, R. GOZALO & J.B. DIEZ. Discovery of a new spore assemblage in the Middle Devonian of Iberian Peninsula. 9h40-10h Brigitte MEYER-BERTHAUD, A.-L. DECOMBEIX, R. DUNSTONE, P. GERRIENNE, N. MOMONT & G. YOUNG. First record of aneurophytalean progymnosperms in Australia.
    [Show full text]
  • (Revised with Costs), Petrified Forest National Park
    National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Natural Resource Condition Assessment Petrified Forest National Park (Revised with Costs) Natural Resource Report NPS/PEFO/NRR—2020/2186 The production of this document cost $ 112,132, including costs associated with data collection, processing, analysis, and subsequent authoring, editing, and publication. ON THE COVER Milky Way over Battleship Rock, Petrified Forest National Park Jacob Holgerson, NPS Natural Resource Condition Assessment Petrified Forest National Park (Revised with Costs) Natural Resource Report NPS/PEFO/NRR—2020/2186 J. Judson Wynne1 1 Department of Biological Sciences Merriam-Powell Center for Environmental Research Northern Arizona University Box 5640 Flagstaff, AZ 86011 November 2020 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. The series supports the advancement of science, informed decision-making, and the achievement of the National Park Service mission. The series also provides a forum for presenting more lengthy results that may not be accepted by publications with page limitations. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner.
    [Show full text]
  • Lyginopteris Royalii Sp. Nov. from the Upper Mississippian of North America
    Review of Palaeobotany and Palynology 116 (2001) 159±173 www.elsevier.com/locate/revpalbo Lyginopteris royalii sp. nov. from the Upper Mississippian of North America Alexandru Mihail Florian Tomescu*, Gar W. Rothwell, Gene Mapes Department of Environmental and Plant Biology, Ohio University, Athens, OH 45701, USA Received 22 August 2000; accepted for publication 6 February 2001 Abstract A new species of the seed fern Lyginopteris is described from a nodule in Upper Mississippian (middle Chesterian-Namurian A) shales of the Fayetteville Formation in northwestern Arkansas. The pyritized stem is 29 cm long and slightly compressed, with a diameter of about 11 £ 5 mm, and shows seven diverging leaf bases. The primary xylem of the specimen is eustelic. Foliar bundles extend through ®ve internodes before entering the rachis bases; they do not divide along their trajectory through the stem. Phyllotaxis of the specimen approaches 2/5. Longitudinally oriented sclerenchyma strands accompany the diverging foliar vascular bundles adaxially in the cortex, and are incorporated in the outer cortex above the level of foliar rachis divergence. In contrast to previously described Lyginopteris species, this species lacks capitate epidermal glands. A Lygino- pteris type rachis with a paired vascular bundle is preserved in the same nodule. Coprolites probably produced by oribatid mites are present in different tissues of the stem. The study of the leaf trace divergence necessitated the use of a deformation model to help reconstruct the original position of the cauline bundles in the compressed stele. This occurrence of Lyginopteris con®rms earlier reports of the genus from North America and emphasizes that it was not restricted to Western Europe.
    [Show full text]