Fossil Species of Boehmerieae Gaudich. (Urticaceae)
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Insects in Amber
Annu. Rev. Entomol. 1993.46:145-59 Copyright © 1993 by Annual Reviews Inc. All righis reserved INSECTS IN AMBER George O. Poinar, Jr. Department of Entomological Sciences, University of California, Berkeley, California 94720 KEY WORDS: fossil insects, tissue preservation, paleoentomology, paleosymbiosis, paleoen vironments Introduction Aside from their beauty, insects in amber represent the finest fossil remains of the Insecta and offer numerous opportunities to study microevolution, biogeography, mimicry, behavior, environmental reconstruction, extinction, paleosymbiosis, and molecular phylogeny. Amberization (changes involved in the process of forming amber from fresh resin) is a gentle process inducive to the preservation of insects that are small, delicate, and soft-bodied. It is the most complete type of fossilization known for insects, and by preserving the three-dimensional form, color pattern, and minute details of the exoskeleton, such fossils can be easily compared with their extant descendants. The study of amber insects was initiated over 200 years ago with the fIrst investigation of the Baltic amber fauna and flora (10). Indeed, most of the descriptions of amber insects today pertain to Baltic deposits. However, in the past 50 years, workers have begun to explore additional amber deposits. These are listed in Table 1. Access provided by Oregon State University on 12/22/16. For personal use only. The oldest amber deposits containing insects are from the Middle East and Annu. Rev. Entomol. 1993.38:145-159. Downloaded from www.annualreviews.org are commonly known as Lebanese amber. They date from the Early Cretaceous and extend back 135 million years. In the past 20 years, attention has centered on the highly fossiliferous Tertiary amber deposits in the Dominican Republic, which are fairly extensive and provide a steady income for Dominican workers primarily through sale for use as jewelry. -
The Origin and Early Evolution of the Legumes Are a Complex
bioRxiv preprint doi: https://doi.org/10.1101/577957; this version posted March 16, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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-NC-ND 4.0 International license. 1 The Origin and Early Evolution of the Legumes are a 2 Complex Paleopolyploid Phylogenomic Tangle closely 3 associated with the Cretaceous-Paleogene (K-Pg) Boundary 4 5 Running head: 6 Phylogenomic complexity and polyploidy in legumes 7 8 Authors: 9 Erik J.M. Koenen1*, Dario I. Ojeda2,3, Royce Steeves4,5, Jérémy Migliore2, Freek T. 10 Bakker6, Jan J. Wieringa7, Catherine Kidner8,9, Olivier Hardy2, R. Toby Pennington8,10, 11 Patrick S. Herendeen11, Anne Bruneau4 and Colin E. Hughes1 12 13 1 Department of Systematic and Evolutionary Botany, University of Zurich, 14 Zollikerstrasse 107, CH-8008, Zurich, Switzerland 15 2 Service Évolution Biologique et Écologie, Faculté des Sciences, Université Libre de 16 Bruxelles, Avenue Franklin Roosevelt 50, 1050, Brussels, Belgium 17 3 Norwegian Institute of Bioeconomy Research, Høgskoleveien 8, 1433 Ås, Norway 18 4 Institut de Recherche en Biologie Végétale and Département de Sciences Biologiques, 19 Université de Montréal, 4101 Sherbrooke St E, Montreal, QC H1X 2B2, Canada 20 5 Fisheries & Oceans Canada, Gulf Fisheries Center, 343 Université Ave, Moncton, NB 21 E1C 5K4, Canada 22 6 Biosystematics Group, Wageningen University, Droevendaalsesteeg 1, 6708 PB, 23 Wageningen, The Netherlands 24 7 Naturalis Biodiversity Center, Leiden, Darwinweg 2, 2333 CR, Leiden, The Netherlands 25 8 Royal Botanic Gardens, 20a Inverleith Row, Edinburgh EH3 5LR, U.K. -
Two New Ripidiine Species in Dominican Amber with Evidence of Aggregative Behaviour of Males “Frozen” in the Fossil Record (Coleoptera: Ripiphoridae)
Eur. J. Entomol. 108: 275–286, 2011 http://www.eje.cz/scripts/viewabstract.php?abstract=1617 ISSN 1210-5759 (print), 1802-8829 (online) Two new ripidiine species in Dominican amber with evidence of aggregative behaviour of males “frozen” in the fossil record (Coleoptera: Ripiphoridae) JAN BATELKA1, MICHAEL S. ENGEL2, ZACHARY H. FALIN2 and JAKUB PROKOP 3 1Nad vodovodem 16, CZ-100 00, Praha 10, Czech Republic; e-mail: [email protected] 2 Divison of Entomology (Paleoentomology), Natural History Museum, and Department of Ecology & Evolutionary Biology, 1501 Crestline Drive – Suite 140, University of Kansas, Lawrence, Kansas 66049-2811, USA; e-mail: [email protected] 3Department of Zoology, Faculty of Science, Charles University in Prague, Viniþná 7, 128 44 Praha 2, Czech Republic; e-mail: [email protected] Key words. Taxonomy, Coleoptera, Ripiphoridae, Ripidiinae, Neorrhipidius, Quasipirhidius, new species, Tertiary, Miocene, Dominican amber, Central America, paleoethology, aggregative behaviour Abstract. Ten amber inclusions of male Ripidiinae (Coleoptera: Ripiphoridae) are reported from Early Miocene deposits of the Dominican Republic and compared with extant species of Neorrhipidius Viana, 1958 from Argentina and Paraguay and Quasipir- hidius Zaragoza Caballero, 1991 from Mexico. Neorrhipidius seicherti sp. n. and Quasipirhidius luzziae sp. n. are described and illustrated. Both species are characterised by 11-segmented antennae with eight distal antennomeres uniflabellate, mouthparts reduced to maxillary palpi represented by long styli with fused basal palpomeres, by metathoracic wings without crossveins and tarsal formula of 5-5-4. Neorrhipidius seicherti sp. n. differs from Quasipirhidius luzziae sp. n. by the presence of postocular omma- tidia and by the shape of metascutellum. -
Rbcl and Legume Phylogeny, with Particular Reference to Phaseoleae, Millettieae, and Allies Tadashi Kajita; Hiroyoshi Ohashi; Yoichi Tateishi; C
rbcL and Legume Phylogeny, with Particular Reference to Phaseoleae, Millettieae, and Allies Tadashi Kajita; Hiroyoshi Ohashi; Yoichi Tateishi; C. Donovan Bailey; Jeff J. Doyle Systematic Botany, Vol. 26, No. 3. (Jul. - Sep., 2001), pp. 515-536. Stable URL: http://links.jstor.org/sici?sici=0363-6445%28200107%2F09%2926%3A3%3C515%3ARALPWP%3E2.0.CO%3B2-C Systematic Botany is currently published by American Society of Plant Taxonomists. Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/about/terms.html. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/journals/aspt.html. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. The JSTOR Archive is a trusted digital repository providing for long-term preservation and access to leading academic journals and scholarly literature from around the world. The Archive is supported by libraries, scholarly societies, publishers, and foundations. It is an initiative of JSTOR, a not-for-profit organization with a mission to help the scholarly community take advantage of advances in technology. For more information regarding JSTOR, please contact [email protected]. -
Palaeoplethodon Hispaniolae Gen
UC Berkeley UC Berkeley Previously Published Works Title Palaeoplethodon hispaniolae gen. n., sp. n. (Amphibia: Caudata), a fossil salamander from the Caribbean Palaeodiversity 8: 21–29; Stuttgart 30 December 2015. Permalink https://escholarship.org/uc/item/1f381770 Authors Wake, David B Poinar, George Publication Date 2021-06-28 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Palaeodiversity 8: 21–29; Stuttgart 30 December 2015. 21 Palaeoplethodon hispaniolae gen. n., sp. n. (Amphibia: Caudata), a fossil salamander from the Caribbean GEORGE POINAR JR. & DAV I D B. WAKE Abstract A salamander hatchling, Palaeoplethodon hispaniolae gen. n., sp. n. (Amphibia: Caudata), is described from Dominican Republic amber. While physical features align the fossil with members of the family Plethodontidae, the short forelimb with the foot lacking distinct digits and the long hind limb with elongated foot and strongly fused digits, as well as its presence in 15–40 mya Dominican amber, distinguish the fossil from previously described sal- amanders. The apparent 13–14 costal grooves and strongly webbed digits are characters shared with members of the extant plethodontid genus Bolitoglossa PETERS, 1879, the most speciose genus of Neotropical salamanders. This is the first salamander recovered from any amber source and the first undisputed salamander reported from the Caribbean region. K e y w o r d s : Salamander, fossil, Palaeoplethodon hispaniolae, Caudata, Plethodontidae, Dominican amber. 1. Introduction 2. Materials and methods Over the years, remains of frogs, lizards, birds and The salamander fossil originated from an amber mine mammals have been found in various amber depos- in the northern mountain range (Cordillera Septentrional) its around the world, but no salamanders have ever been of the Dominican Republic between Puerto Plata and San- reported (POINAR 1992; POINAR & POINAR 1999). -
Historical Biology: an International Journal of Paleobiology
This article was downloaded by: [The Library, University of Witwatersrand] On: 07 August 2014, At: 05:12 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Historical Biology: An International Journal of Paleobiology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ghbi20 Paleotrichius dominicanus n. gen., n. sp. (Coleoptera; Cetoniidae), a flower beetle in Dominican amber George Poinar Jr. a a Department of Zoology , Oregon State University , Corvallis, OR, 97331, USA Published online: 28 Jun 2010. To cite this article: George Poinar Jr. (2011) Paleotrichius dominicanus n. gen., n. sp. (Coleoptera; Cetoniidae), a flower beetle in Dominican amber, Historical Biology: An International Journal of Paleobiology, 23:02-03, 109-113, DOI: 10.1080/08912963.2010.482417 To link to this article: http://dx.doi.org/10.1080/08912963.2010.482417 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. -
Chemical Preservation of Plants and Insects in Natural Resins
Chemical preservation of plants and insects in natural resins B. Artur Stankiewicz1,2{, Hendrik N. Poinar3, Derek E. G. Briggs1, Richard P. Evershed2 and George O. Poinar Jr4 1Biogeochemistry Research Centre, Department of Earth Sciences, University of Bristol, Queen's Road, Bristol BS8 1RJ, UK 2Organic Geochemistry Unit, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK 3Institute of Zoology, University of Munich, PO Box 202136, D-80021 Munich, Germany 4Department of Entomology, Oregon State University, 2046 Cordley Hall, Corvallis, OR 97331, USA The morphological preservation of fossils in amber is remarkable, but their chemical composition is largely unknown. The likelihood of DNA preservation in amber has been questioned but, surprisingly, the fate of more decay-resistant macromolecules such as ligno-cellulose in plants or the chitin^protein complex in insect cuticle has not been investigated. Here we report the results of investigations using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS) of the tissues of insects and the plant Hymenaea from ancient and sub-fossil resins (2^20 ka) from Kenya, and from Dominican amber (25^30 Ma). The volatile components of the resin have penetrated even the internal tissues, resulting in the exceptional three-dimen- sional preservation of amber inclusions. Chitin is preserved in the bee and ligno-cellulose in the Hymenaea leaf from the Kenyan resins. There was no trace, however, of these macromolecules in tissues in Dominican amber. The presence of aliphatic polymer and sulphur-containing moieties in these tissues indicates that they have undergone diagenetic alteration; in view of this, the preservation in Dominican amber of a macromolecule as labile as DNA would be extraordinary. -
Amber! Conrad C
AMBER! CONRAD C. LABANDEIRA! Department of Paleobiology, National Museum of Natural History, Smithsonian Institution Washington, D.C. 20013 USA ˂[email protected]! ˃ and! Department of Entomology, University of Maryland, College Park, MD 20742 USA ABSTRACT.—The amber fossil record provides a distinctive, 320-million-year-old taphonomic mode documenting gymnosperm, and later, angiosperm, resin-producing taxa. Resins and their subfossil (copal) and fossilized (amber) equivalents are categorized into five classes of terpenoid, phenols, and other compounds, attributed to extant family-level taxa. Copious resin accumulations commencing during the early Cretaceous are explained by two hypotheses: 1) abundant resin production as a byproduct of plant secondary metabolism, and 2) induced and constitutive host defenses for warding off insect pest and pathogen attack through profuse resin production. Forestry research and fossil wood-boring damage support a causal relationship between resin production and pest attack. Five stages characterize taphonomic conversion of resin to amber: 1) Resin flows initially caused by biotic or abiotic plant-host trauma, then resin flowage results from sap pressure, resin viscosity, solar radiation, and fluctuating temperature; 2) entrapment of live and dead organisms, resulting in 3) entombment of organisms; then 4) movement of resin clumps to 5) a deposition site. This fivefold diagenetic process of amberization results in resin→copal→amber transformation from internal biological and chemical processes and external geological forces. Four phases characterize the amber record: a late Paleozoic Phase 1 begins resin production by cordaites and medullosans. A pre-mid-Cretaceous Mesozoic Phase 2 provides increased but still sparse accumulations of gymnosperm amber. Phase 3 begins in the mid-early Cretaceous with prolific amber accumulation likely caused by biotic effects of an associated fauna of sawflies, beetles, and pathogens. -
The Origin and Early Evolution of the Legumes Are a Complex
bioRxiv preprint doi: https://doi.org/10.1101/577957; this version posted March 16, 2019. 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-NC-ND 4.0 International license. 1 The Origin and Early Evolution of the Legumes are a 2 Complex Paleopolyploid Phylogenomic Tangle closely 3 associated with the Cretaceous-Paleogene (K-Pg) Boundary 4 5 Running head: 6 Phylogenomic complexity and polyploidy in legumes 7 8 Authors: 9 Erik J.M. Koenen1*, Dario I. Ojeda2,3, Royce Steeves4,5, Jérémy Migliore2, Freek T. 10 Bakker6, Jan J. Wieringa7, Catherine Kidner8,9, Olivier Hardy2, R. Toby Pennington8,10, 11 Patrick S. Herendeen11, Anne Bruneau4 and Colin E. Hughes1 12 13 1 Department of Systematic and Evolutionary Botany, University of Zurich, 14 Zollikerstrasse 107, CH-8008, Zurich, Switzerland 15 2 Service Évolution Biologique et Écologie, Faculté des Sciences, Université Libre de 16 Bruxelles, Avenue Franklin Roosevelt 50, 1050, Brussels, Belgium 17 3 Norwegian Institute of Bioeconomy Research, Høgskoleveien 8, 1433 Ås, Norway 18 4 Institut de Recherche en Biologie Végétale and Département de Sciences Biologiques, 19 Université de Montréal, 4101 Sherbrooke St E, Montreal, QC H1X 2B2, Canada 20 5 Fisheries & Oceans Canada, Gulf Fisheries Center, 343 Université Ave, Moncton, NB 21 E1C 5K4, Canada 22 6 Biosystematics Group, Wageningen University, Droevendaalsesteeg 1, 6708 PB, 23 Wageningen, The Netherlands 24 7 Naturalis Biodiversity Center, Leiden, Darwinweg 2, 2333 CR, Leiden, The Netherlands 25 8 Royal Botanic Gardens, 20a Inverleith Row, Edinburgh EH3 5LR, U.K. -
Molecular Taphonomy of Animal and Plant Cuticles: Selective Preservation and Diagenesis
Molecular taphonomy of animal and plant cuticles: selective preservation and diagenesis Derek E. G. Briggs Biogeochemistry Research Centre, Department of Earth Sciences, University of Bristol, Queen's Road, Bristol BS8 1RJ, UK The nature of organic material and the environment in which it is deposited exert a major in£uence on the extent to which biomacromolecules are preserved in the fossil record. The role of these factors is explored with a particular focus on the cuticle of arthropods and leaves. Preservation of the original chemistry of arthropod cuticles is favoured by their thickness and degree of sclerotization, and the presence of biominerals. Decay and burial in terrestrial as opposed to marine, and anoxic rather than oxygenated conditions, likewise appear to enhance preservation. The most important factor in the long- term preservation of the chemistry of both animal and plant cuticles, however, is diagenetic alteration to an aliphatic composition. This occurs even in amber, which encapsulates the fossil, eliminating almost all external factors. Some plants contain an original decay-resistant macromolecular aliphatic component but this is not the case in arthropods. It appears that the aliphatic components of many plant as well as animal fossils may be the result of diagenetic polymerization. Selective preservation as a result of decay resistance may explain the initial survival of organic materials in sediments, but in many cases longer- term preservation relies on chemical changes. Selective preservation is only a partial explanation for the origin of kerogen. Keywords: cuticle; aliphatic; molecular taphonomy; selective preservation; polymerization; kerogen such as animal cuticles, algal cell walls, plant cuticles, 1. -
Some Types of Fossils Panel (PDF)
Some Types of Plant Fossils THE BOTANIC GARDEN OF SMITH C OLLE G E Much of what we know about the form and structure of extinct plant species comes from fossils. Four major types of plant fossils are: Fossil Pecopteris fronds PHOTO BY PAMELA DODS; SPECIMEN FROM THE BENESKI MUSEUM, AMHERST COLLEGE Compression and impression fossils originate in wet areas where plant parts become quickly buried by sediment, the weight of which squeezes out and flattens the plant material, leaving impressions in the fine-grained sediment. In some cases plant carbon or cuticle (waxy, water-repellent coating) also remain Fossil leaves of Ginkgo Fossil leaves and branches of Sphenophyllum miravallis within the impression. PHOTO BY GHEDOGHEDO PHOTO BY WOUDLOPER Permineralized fossils result from infiltration of the plant tissue by water containing dissolved minerals. Over time, if the minerals precipitate, a rock forms that preserves the plant in three dimensions with detail down to the cellular level. Above: Fossil wood from Madagascar PHOTO BY JAMES ST. JOHN Petrified tree in Petrified Forest National Park in Arizona Man standing next to fossilized Sigillaria trunk in a coal Petrified Calamites trunk Polished petrified wood from Arizona mine in France PHOTOS BY PAMELA DODS; SPECIMENS FROM THE BENESKI MUSEUM, AMHERST COLLEGE ALEXANDER WINCHELL, SKETCHES OF CREATION, NEW YORK, NY: HARPER & BROTHERS, 1870 Unaltered plant remains can occur Right: Flower of Strychnos electri in Dominican Republic where microbial activity, which would amber PHOTO BY GEORGE POINAR normally destroy plant remains, is inhibited by freezing, salinity, or acidity. Below: Hymenaea protera leaf in Dominican Republic amber Examples can be found in deep lake PHOTO BY GEORGE POINAR sediments, in amber (fossilized plant resin), and in pack rat middens, where animal nests made of plants become encased in crystallized urine. -
Elaphoglossum
Dissertation zur Erlangung des Doktorgrades der Naturwissenschaften (Dr. rer. nat.) an der Fakultät für Biologie der Ludwig-Maximilians-Universität München EVOLUTION AND CLASSIFICATION OF ELAPHOGLOSSUM AND ASPLENIUM FERNS ON CUBA, AND DISCOVERY OF A MIOCENE ELAPHOGLOSSUM IN DOMINICAN AMBER Josmaily Lóriga Piñeiro München, 15. Januar 2018 ii A mi familia y mis amigos, donde quiera que estén To my family and my friends, wherever they are iii iv PREFACE Statutory declaration Erklärung Diese Dissertation wurde im Sinne von §12 der Promotionsordnung von Prof. Dr. Jochen Heinrichs betreut. Ich erkläre hiermit, dass die Dissertation nicht einer anderen Prüfungskommission vorgelegt worden ist und dass ich mich nicht anderweitig einer Doktorprüfung ohne Erfolg unterzogen habe. Eidesstattliche Erklärung Ich versichere hiermit an Eides statt, dass die vorgelegte Dissertation von mir selbstständig und ohne unerlaubte Hilfe angefertigt wurde. Josmaily Lóriga, 15. Januar 2018 (Unterschrift) 1. Gutachter: Prof. Dr. Susanne S. Renner 2. Gutachter: Prof. Dr. Reinhard Agerer Tag der Abgabe: 15. Januar 2018 Tag der Disputation: 28. Februar 2018 v vi Declaration of contribution In this thesis, I present the results from my doctoral research, carried out in Munich from March 2013 to January 2018 (maternity leave between February and December 2017) under the guidance of Prof. Dr. Jochen Heinrichs. My thesis resulted in three published manuscripts presented in Chapters 2 to 4. I generated all data and conducted all analyses myself with some exceptions: Chapter 2, Alejandra Vasco produced Fig. 4; Chapter 3, Ledis Regalado conducted the study of gametophytes and generated the drawings of Fig. 1; and Chapter 4, Kathrin Feldberg contributed to the divergence time estimates and Alexander R.