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Report on Biodiversity and Tropical Forests in Indonesia
Report on Biodiversity and Tropical Forests in Indonesia Submitted in accordance with Foreign Assistance Act Sections 118/119 February 20, 2004 Prepared for USAID/Indonesia Jl. Medan Merdeka Selatan No. 3-5 Jakarta 10110 Indonesia Prepared by Steve Rhee, M.E.Sc. Darrell Kitchener, Ph.D. Tim Brown, Ph.D. Reed Merrill, M.Sc. Russ Dilts, Ph.D. Stacey Tighe, Ph.D. Table of Contents Table of Contents............................................................................................................................. i List of Tables .................................................................................................................................. v List of Figures............................................................................................................................... vii Acronyms....................................................................................................................................... ix Executive Summary.................................................................................................................... xvii 1. Introduction............................................................................................................................1- 1 2. Legislative and Institutional Structure Affecting Biological Resources...............................2 - 1 2.1 Government of Indonesia................................................................................................2 - 2 2.1.1 Legislative Basis for Protection and Management of Biodiversity and -
Fossil History of Curculionoidea (Coleoptera) from the Paleogene
geosciences Review Fossil History of Curculionoidea (Coleoptera) from the Paleogene Andrei A. Legalov 1,2 1 Institute of Systematics and Ecology of Animals, Siberian Branch, Russian Academy of Sciences, Ulitsa Frunze, 11, 630091 Novosibirsk, Novosibirsk Oblast, Russia; [email protected]; Tel.: +7-9139471413 2 Biological Institute, Tomsk State University, Lenin Ave, 36, 634050 Tomsk, Tomsk Oblast, Russia Received: 23 June 2020; Accepted: 4 September 2020; Published: 6 September 2020 Abstract: Currently, some 564 species of Curculionoidea from nine families (Nemonychidae—4, Anthribidae—33, Ithyceridae—3, Belidae—9, Rhynchitidae—41, Attelabidae—3, Brentidae—47, Curculionidae—384, Platypodidae—2, Scolytidae—37) are known from the Paleogene. Twenty-seven species are found in the Paleocene, 442 in the Eocene and 94 in the Oligocene. The greatest diversity of Curculionoidea is described from the Eocene of Europe and North America. The richest faunas are known from Eocene localities, Florissant (177 species), Baltic amber (124 species) and Green River formation (75 species). The family Curculionidae dominates in all Paleogene localities. Weevil species associated with herbaceous vegetation are present in most localities since the middle Paleocene. A list of Curculionoidea species and their distribution by location is presented. Keywords: Coleoptera; Curculionoidea; fossil weevil; faunal structure; Paleocene; Eocene; Oligocene 1. Introduction Research into the biodiversity of the past is very important for understanding the development of life on our planet. Insects are one of the Main components of both extinct and recent ecosystems. Coleoptera occupied a special place in the terrestrial animal biotas of the Mesozoic and Cenozoics, as they are characterized by not only great diversity but also by their ecological specialization. -
Agathis Macrophylla Araucariaceae (Lindley) Masters
Agathis macrophylla (Lindley) Masters Araucariaceae LOCAL NAMES English (pacific kauri); Fijian (da‘ua,dakua dina,makadri,makadre,takua makadre,dakua,dakua makadre) BOTANIC DESCRIPTION Agathis macrophylla is a tall tree typically to about 30–40 m tall, 3 m in bole diameter, with a broad canopy of up to 36 m diameter. Branches may be erect to horizontal and massive. Mature specimens have wide, spreading root systems whereas seedlings and young specimens have a vigorous taproot with one or more whorls of lateral roots. Leaves simple, entire, elliptic to lanceolate, leathery, and dark green, and shiny above and often glaucous below; about 7–15 cm long and 2–3.5 cm wide, with many close inconspicuous parallel veins. The leaves taper to a more or less pointed tip, rounded at the base, with the margins curved down at the edge. Petioles short, from almost sessile up to 5 mm long. Cones egg-shaped at the end of the first year, about 5 cm long, and 3 cm in diameter, more or less round at the end of the second year, 8–10 cm in diameter. Female cones much larger than males, globular, on thick woody stalks, green, slightly glaucous, turning brownish during ripening. Seeds brown, small, ovoid to globose, flattened, winged, and attached to a triangular cone scale about 2.5 cm across. BIOLOGY Pacific kauri is monoecious and produces cones instead of flowers. The first female cones begin to be produced at about 10 years old and take up to 2 years to mature (more often in 12-15 months). -
Baez NHM 1997.Pdf (3.622Mb)
HERP QL 668 B33 l':iif;,O0i.U'.Z06l("'^ ocxentxpc Papers Natural History Museum The University of Kansas 29 October 1997 Number 4:1^1 Redescription of the Paleogene Shelania pascuali from Patagonia and Its Bearing on the Relationships of Fossil and Recent Pipoid Frogs >. By o O Ana Maria BAez^ and Linda Trueb- o ^Departamento de Geologia, FacuUad de Ciencias Exactas, Universidad de 0) w >. > t- Buenos Aires, Pabellon II, Ciudad Universitaria, 1428 Buenos Aires, Argentina CO !-> >^ ^ £ -^ '^Division of Herpetology, Natural Histoiy Museum, and Department of P Kansas 66045-2454, J3 o, Systematics and Ecology, The University of Kansas, Lawrence, USA a o t3 o CO ^ t. CONTENTS ° CO I ABSTRACT 2 « RESUMEN 2 5S INTRODUCTION 2 Previous Paleontological Work 4 Acknowledgments 4 MATERIALS AND METHODS 5 General Methodology 5 Cladistic Methodology 5 Specimens Examined 6 STRATIGRAPHIC PROVENANCE AND AGE OF MATERIAL 6 REDESCRIPTION OF SHELANIA 8 ANALYSIS OF CHARACTERS 16 RESULTS 31 DISCUSSION 35 Taxonomic Considerations 35 Characters 36 LITERATURE CITED 37 APPENDIX 40 © Natural History Museum, The University of Kansas ISSN No. 1094-0782 — 2 Scientific Papers, Natural History Museum, The University of Kansas 1960, is redescribed on the basis of a series of 30 recently I ABSTIMCT Shdania pascuali Casamiquela, .'-\ ' . discovered specimens, which range in estimated snout-vent length from 30-100 mm, from the Paleo- y ' gene of Patagonia. This large pipoid anuran is distinguished by possessing a long, narrow braincase; an hourglass-shaped frontoparietal; a robust antorbital process on the edentate maxilla; long, straight {/) '/^ I ilia that describe a V-shape in dorsal profile; and a trunk that is long relative to the lengths of the head and limbs. -
Ecological Assessments in the B+WISER Sites
Ecological Assessments in the B+WISER Sites (Northern Sierra Madre Natural Park, Upper Marikina-Kaliwa Forest Reserve, Bago River Watershed and Forest Reserve, Naujan Lake National Park and Subwatersheds, Mt. Kitanglad Range Natural Park and Mt. Apo Natural Park) Philippines Biodiversity & Watersheds Improved for Stronger Economy & Ecosystem Resilience (B+WISER) 23 March 2015 This publication was produced for review by the United States Agency for International Development. It was prepared by Chemonics International Inc. The Biodiversity and Watersheds Improved for Stronger Economy and Ecosystem Resilience Program is funded by the USAID, Contract No. AID-492-C-13-00002 and implemented by Chemonics International in association with: Fauna and Flora International (FFI) Haribon Foundation World Agroforestry Center (ICRAF) The author’s views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States Government. Ecological Assessments in the B+WISER Sites Philippines Biodiversity and Watersheds Improved for Stronger Economy and Ecosystem Resilience (B+WISER) Program Implemented with: Department of Environment and Natural Resources Other National Government Agencies Local Government Units and Agencies Supported by: United States Agency for International Development Contract No.: AID-492-C-13-00002 Managed by: Chemonics International Inc. in partnership with Fauna and Flora International (FFI) Haribon Foundation World Agroforestry Center (ICRAF) 23 March -
The Biogeography of Large Islands, Or How Does the Size of the Ecological Theater Affect the Evolutionary Play
The biogeography of large islands, or how does the size of the ecological theater affect the evolutionary play Egbert Giles Leigh, Annette Hladik, Claude Marcel Hladik, Alison Jolly To cite this version: Egbert Giles Leigh, Annette Hladik, Claude Marcel Hladik, Alison Jolly. The biogeography of large islands, or how does the size of the ecological theater affect the evolutionary play. Revue d’Ecologie, Terre et Vie, Société nationale de protection de la nature, 2007, 62, pp.105-168. hal-00283373 HAL Id: hal-00283373 https://hal.archives-ouvertes.fr/hal-00283373 Submitted on 14 Dec 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. THE BIOGEOGRAPHY OF LARGE ISLANDS, OR HOW DOES THE SIZE OF THE ECOLOGICAL THEATER AFFECT THE EVOLUTIONARY PLAY? Egbert Giles LEIGH, Jr.1, Annette HLADIK2, Claude Marcel HLADIK2 & Alison JOLLY3 RÉSUMÉ. — La biogéographie des grandes îles, ou comment la taille de la scène écologique infl uence- t-elle le jeu de l’évolution ? — Nous présentons une approche comparative des particularités de l’évolution dans des milieux insulaires de différentes surfaces, allant de la taille de l’île de La Réunion à celle de l’Amé- rique du Sud au Pliocène. -
Changes of the Palynobiotas in the Mesozoic and Cenozoic of Patagonia: a Review
Biological Journal of the Linnean Society, 2011, 103, 380–396. With 6 figures Changes of the palynobiotas in the Mesozoic and Cenozoic of Patagonia: a review MIRTA E. QUATTROCCHIO1,2*, WOLFGANG VOLKHEIMER3, ANA MARÍA BORRROMEI1 and MARCELO A. MARTÍNEZ1,2 1INGEOSUR, CONICET, San Juan 670, (8000), Bahía Blanca, Argentina 2Departamento de Geología, Universidad Nacional del Sur, San Juan 670, (8000) Bahía Blanca, Argentina 3IANIGLA, CCT-CONICET, CC330 (5500) Mendoza, Argentina Received 22 February 2011; accepted for publication 22 February 2011bij_1652 380..396 This study describes the compositional changes of Mesozoic–Cenozoic palynologic assemblages in Patagonia, the succession of phytogeographic scenarios and some evolutionary key events. The Triassic ‘Ipswich Microflora’, characterized by bisaccate pollen and high frequencies of trilete spores, represents the warm–temperate province of south-western Gondwana (Dicroidium Flora), followed in time, in Patagonia, near the Triassic/Jurassic bound- ary, by the ‘Classopollis Microflora’, indicating warm and (seasonal) arid conditions. Araucariaceans and podocar- paceans grew on Jurassic uplands. The exclusively Early Cretaceous taxa Cyclusphaera and Balmeiopsis (Coniferae) appeared in the Valanginian. The oldest angiospermous pollen types of Argentina appear in the Barremian–Aptian of southern Patagonia. During the Maastrichtian, the Nothofagaceae and Myrtaceae are incoming. In the Palaeocene, a vegetation dominated by tropical elements would have developed in Patagonia. Increasing Nothofagidites frequency in northern Patagonia during the Middle to Late Eocene indicates climatic change from warm to temperate. Of three Early to Middle Miocene phytogeographic provinces (Neotropical– Transitional and Austral), the Transitional one was replaced during the Late Miocene–Pliocene by the xerophytic Proto Espinal/Steppe with a shrubby–herbaceous vegetation. -
Geologica Acta, Vol.4, N°4, 2006, 409-438 |415| Ce
'geológica FOmS^Y ACTA GEOLÓGICA HISPAfilCA Geológica acta: an international earth science journal Universidad de Barcelona [email protected] ISSN (Versión impresa): 1695-6133 ESPAÑA 2006 C.C. Labandeira THE FOUR PHASES OF PLANT-ARTHROPOD ASSOCIATIONS IN DEEP TIME Geológica acta: an international earth science journal, december, año/vol. 4, número 004 Universidad de Barcelona Barcelona, España pp. 409-438 Red de Revistas Científicas de América Latina y el Caribe, España y Portugal ®re¿!alyc^ Universidad Autónoma del Estado de México http://redalyc.uaemex.mx Geológica Acta, Vol.4, N° 4, 2006, 409-438 Appendix l-IX geología acta Available online at www.geologica-acta.com The Four Phases of Plant-Arthropod Associations in Deep Time C.C. LABANDEIRA |1||2| 111 Smithsonian Institution, National Museum of Natural History P.O. Box 37012, MRC-121 Department of Paleobiology, Washington, D.C., USA 200137012. E-mail: [email protected] 121 University of Maryland, Department of Entomology College Park, Maryland, USA 20742 1 ABSTRACT I Vascular-plant hosts, their arthropod herbivores, and associated functional feeding groups are distributed spa- tiotemporally into four major herbivore expansions during the past 420 m.y. They are: (1) a Late Silurian to Late Devonian (60 m.y.) phase of myriapod and apterygote, hexapod (perhaps pterygote) herbivores on several clades of primitive vascular-plant hosts and a prototaxalean fungus; (2) a Late Mississippian to end-Permian (85 m.y.) phase of mites and apterygote and basal pterygote herbivores on pteridophyte and basal gymnospermous plant hosts; (3) a Middle Triassic to Recent (245 m.y.) phase of mites, orthopteroids (in the broadest sense) and hemipteroid and basal holometabolan herbivores on pteridophyte and gymnospermous plant hosts; and (4) a mid Early Cretaceous to Recent (115 m.y.) phase of modern-aspect orthopteroids and derived hemipteroid and holometabolous herbivores on angiospermous plant hosts. -
Fossil Pollen Records Indicate That Patagonian Desertification Was Not Solely a Consequence of Andean Uplift
ARTICLE Received 25 Oct 2013 | Accepted 4 Mar 2014 | Published 28 Mar 2014 DOI: 10.1038/ncomms4558 Fossil pollen records indicate that Patagonian desertification was not solely a consequence of Andean uplift L. Palazzesi1,2, V.D. Barreda1, J.I. Cuitin˜o3, M.V. Guler4, M.C. Tellerı´a5 & R. Ventura Santos6 The Patagonian steppe—a massive rain-shadow on the lee side of the southern Andes—is assumed to have evolved B15–12 Myr as a consequence of the southern Andean uplift. However, fossil evidence supporting this assumption is limited. Here we quantitatively estimate climatic conditions and plant richness for the interval B10–6 Myr based on the study and bioclimatic analysis of terrestrially derived spore–pollen assemblages preserved in well-constrained Patagonian marine deposits. Our analyses indicate a mesothermal climate, with mean temperatures of the coldest quarter between 11.4 °C and 16.9 °C (presently B3.5 °C) and annual precipitation rarely below 661 mm (presently B200 mm). Rarefied richness reveals a significantly more diverse flora during the late Miocene than today at the same latitude but comparable with that approximately 2,000 km further northeast at mid-latitudes on the Brazilian coast. We infer that the Patagonian desertification was not solely a consequence of the Andean uplift as previously insinuated. 1 Museo Argentino de Ciencias Naturales ‘Bernardino Rivadavia’, Angel Gallardo 470 (C1405DJR), Buenos Aires, Argentina. 2 Jodrell Laboratory, Royal Botanic Gardens, Kew, Richmond, Surrey TW9 3DS, UK. 3 Universidad de Buenos Aires, Departamento de Ciencias Geolo´gicas, Facultad de Ciencias Exactas y Naturales. Intendente Gu¨iraldes 2160 (C1428EHA), Buenos Aires, Argentina. -
Evolution of the Female Conifer Cone Fossils, Morphology and Phylogenetics
DEPARTMENT OF BIOLOGICAL AND ENVIRONMENTAL SCIENCES EVOLUTION OF THE FEMALE CONIFER CONE FOSSILS, MORPHOLOGY AND PHYLOGENETICS Daniel Bäck Degree project for Bachelor of Science with a major in Biology BIO602, Biologi: Examensarbete – kandidatexamen, 15 hp First cycle Semester/year: Spring 2020 Supervisor: Åslög Dahl, Department of Biological and Environmental Sciences Examiner: Claes Persson, Department of Biological and Environmental Sciences Front page: Abies koreana (immature seed cones), Gothenburg Botanical Garden, Sweden Table of contents 1 Abstract ............................................................................................................................... 2 2 Introduction ......................................................................................................................... 3 2.1 Brief history of Florin’s research ............................................................................... 3 2.2 Progress in conifer phylogenetics .............................................................................. 4 3 Aims .................................................................................................................................... 4 4 Materials and Methods ........................................................................................................ 4 4.1 Literature: ................................................................................................................... 4 4.2 RStudio: ..................................................................................................................... -
2. DACRYCARPUS (Endlicher) De Laubenfels, J. Arnold Arbor. 50: 315
Flora of China 4: 79. 1999. 2. DACRYCARPUS (Endlicher) de Laubenfels, J. Arnold Arbor. 50: 315. 1969. 鸡毛松属 ji mao song shu Podocarpus L’Héritier ex Persoon sect. Dacrycarpus Endlicher, Syn. Conif. 221. 1847; Bracteocarpus A. V. Bobrov & Melikyan. Trees or shrubs evergreen, dioecious (very rarely monoecious); trunk straight; main branches spreading or drooping; branchlets drooping or ascending, dense. Leaves dimorphic: juvenile leaves 2-ranked and forming an oblong-ovate branchlet outline, linear, not scalelike; adult leaves needlelike or scalelike, falcate, bilaterally or bifacially flattened, or not flattened, 0.8–1.5 mm. Pollen cones lateral (rarely terminal), solitary or few together; microsporophylls numerous, imbricate; microsporangia 2, abaxial. Seed-bearing structures terminal and often borne on short, lateral branchlets, pedunculate, with appressed or spreading, bractlike leaves at base of peduncle; apical 1 or 2 bracts fertile; basal bracts fused to form a succulent, warty receptacle; ovule inverted. Epimatium wholly enveloping seed, united with fertile bract(s) and together bearing a short, free apex forming an asymmetrically projecting crest on immature seed-bearing structure. Seed large. Nine species: from China and Myanmar to Fiji Islands and New Zealand; one species in China. 1. Dacrycarpus imbricatus (Blume) de Laubenfels var. patulus de Laubenfels, J. Arnold Arbor. 50: 320. 1969. 鸡毛松 ji mao song Bracteocarpus kawaii (Hayata) A. V. Bobrov & Meli- kyan; Podocarpus kawaii Hayata. Trees to 40 m tall; trunk to 2 m d.b.h.; bark superficially dark brown or blackish, weathering gray, red-brown and granular fibrous within, flaking in thin strips; crown spreading; branchlets stiff, erect. Juvenile leaves borne at 60–75° to branchlet axis, 0.2– 0.7 mm apart (branchlets 3–4 × 1.2–1.6 cm in outline), sessile, green or ± glaucous, linear, falcate to “S”- shaped, 6–10(–17) × 0.9–1.2 mm, stomata arranged in 2 whitish rows on abaxial surface, base decurrent, margin entire, apex obliquely incurved-apiculate, apiculus 0.2–0.3 mm. -
Fossil Ants (Hymenoptera: Formicidae): Ancient Diversity and the Rise of Modern Lineages
Myrmecological News 24 1-30 Vienna, March 2017 Fossil ants (Hymenoptera: Formicidae): ancient diversity and the rise of modern lineages Phillip BARDEN Abstract The ant fossil record is summarized with special reference to the earliest ants, first occurrences of modern lineages, and the utility of paleontological data in reconstructing evolutionary history. During the Cretaceous, from approximately 100 to 78 million years ago, only two species are definitively assignable to extant subfamilies – all putative crown group ants from this period are discussed. Among the earliest ants known are unexpectedly diverse and highly social stem- group lineages, however these stem ants do not persist into the Cenozoic. Following the Cretaceous-Paleogene boun- dary, all well preserved ants are assignable to crown Formicidae; the appearance of crown ants in the fossil record is summarized at the subfamilial and generic level. Generally, the taxonomic composition of Cenozoic ant fossil communi- ties mirrors Recent ecosystems with the "big four" subfamilies Dolichoderinae, Formicinae, Myrmicinae, and Ponerinae comprising most faunal abundance. As reviewed by other authors, ants increase in abundance dramatically from the Eocene through the Miocene. Proximate drivers relating to the "rise of the ants" are discussed, as the majority of this increase is due to a handful of highly dominant species. In addition, instances of congruence and conflict with molecular- based divergence estimates are noted, and distinct "ghost" lineages are interpreted. The ant fossil record is a valuable resource comparable to other groups with extensive fossil species: There are approximately as many described fossil ant species as there are fossil dinosaurs. The incorporation of paleontological data into neontological inquiries can only seek to improve the accuracy and scale of generated hypotheses.