The Fossil Record of Plant-Insect Dynamics
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Early Jurassic Microbial Mats—A Potential Response to Reduced Biotic Activity in the Aftermath of the End-Triassic Mass Extinction Event
Palaeogeography, Palaeoclimatology, Palaeoecology 464 (2016) 76–85 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Early Jurassic microbial mats—A potential response to reduced biotic activity in the aftermath of the end-Triassic mass extinction event Olof Peterffy a, Mikael Calner a, Vivi Vajda a,b,⁎ a Department of Geology, Lund University, SE-22362 Lund, Sweden b Swedish Museum of Natural History, P.O. Box 50007, SE-104 05 Stockholm, Sweden article info abstract Article history: Wrinkle structures are microbially induced sedimentary structures (MISS) formed by cyanobacteria and are com- Received 6 June 2015 mon in pre-Cambrian and Cambrian siltstones and sandstones but are otherwise rare in the Phanerozoic geolog- Received in revised form 4 December 2015 ical record. This paper reports the first discovery of Mesozoic wrinkle structures from Sweden. These are Accepted 22 December 2015 preserved in fine-grained and organic-rich heterolithic strata of the Lower Jurassic (Hettangian) Höganäs Forma- Available online 30 December 2015 tion in Skåne, southern Sweden. The strata formed in a low-energy, shallow subtidal setting in the marginal parts fi Keywords: of the Danish rift-basin. Palynological analyses of ne-grained sandstones hosting the wrinkle structures show Hettangian that the local terrestrial environment probably consisted of a wetland hosting ferns, cypress and the extinct co- Mass extinction nifer family Cheirolepidaceae. Palynostratigraphy indicates a Hettangian age, still within the floral recovery phase Microbial mat following the end-Triassic mass extinction event. The finding of wrinkle structures is significant as the presence Cyanobacteria of microbial mats in the shallow subtidal zone, (in a deeper setting compared to where modern epibenthic mi- Wrinkle structures crobial mats grow) suggests decreased benthic biodiversity and suppressed grazing in shallow marine environ- Sweden ments in the early aftermath of the end-Triassic mass extinction event. -
UFRJ a Paleoentomofauna Brasileira
Anuário do Instituto de Geociências - UFRJ www.anuario.igeo.ufrj.br A Paleoentomofauna Brasileira: Cenário Atual The Brazilian Fossil Insects: Current Scenario Dionizio Angelo de Moura-Júnior; Sandro Marcelo Scheler & Antonio Carlos Sequeira Fernandes Universidade Federal do Rio de Janeiro, Programa de Pós-Graduação em Geociências: Patrimônio Geopaleontológico, Museu Nacional, Quinta da Boa Vista s/nº, São Cristóvão, 20940-040. Rio de Janeiro, RJ, Brasil. E-mails: [email protected]; [email protected]; [email protected] Recebido em: 24/01/2018 Aprovado em: 08/03/2018 DOI: http://dx.doi.org/10.11137/2018_1_142_166 Resumo O presente trabalho fornece um panorama geral sobre o conhecimento da paleoentomologia brasileira até o presente, abordando insetos do Paleozoico, Mesozoico e Cenozoico, incluindo a atualização das espécies publicadas até o momento após a última grande revisão bibliográica, mencionando ainda as unidades geológicas em que ocorrem e os trabalhos relacionados. Palavras-chave: Paleoentomologia; insetos fósseis; Brasil Abstract This paper provides an overview of the Brazilian palaeoentomology, about insects Paleozoic, Mesozoic and Cenozoic, including the review of the published species at the present. It was analiyzed the geological units of occurrence and the related literature. Keywords: Palaeoentomology; fossil insects; Brazil Anuário do Instituto de Geociências - UFRJ 142 ISSN 0101-9759 e-ISSN 1982-3908 - Vol. 41 - 1 / 2018 p. 142-166 A Paleoentomofauna Brasileira: Cenário Atual Dionizio Angelo de Moura-Júnior; Sandro Marcelo Schefler & Antonio Carlos Sequeira Fernandes 1 Introdução Devoniano Superior (Engel & Grimaldi, 2004). Os insetos são um dos primeiros organismos Algumas ordens como Blattodea, Hemiptera, Odonata, Ephemeroptera e Psocopera surgiram a colonizar os ambientes terrestres e aquáticos no Carbonífero com ocorrências até o recente, continentais (Engel & Grimaldi, 2004). -
Fish, Various Invertebrates
Zambezi Basin Wetlands Volume II : Chapters 7 - 11 - Contents i Back to links page CONTENTS VOLUME II Technical Reviews Page CHAPTER 7 : FRESHWATER FISHES .............................. 393 7.1 Introduction .................................................................... 393 7.2 The origin and zoogeography of Zambezian fishes ....... 393 7.3 Ichthyological regions of the Zambezi .......................... 404 7.4 Threats to biodiversity ................................................... 416 7.5 Wetlands of special interest .......................................... 432 7.6 Conservation and future directions ............................... 440 7.7 References ..................................................................... 443 TABLE 7.2: The fishes of the Zambezi River system .............. 449 APPENDIX 7.1 : Zambezi Delta Survey .................................. 461 CHAPTER 8 : FRESHWATER MOLLUSCS ................... 487 8.1 Introduction ................................................................. 487 8.2 Literature review ......................................................... 488 8.3 The Zambezi River basin ............................................ 489 8.4 The Molluscan fauna .................................................. 491 8.5 Biogeography ............................................................... 508 8.6 Biomphalaria, Bulinis and Schistosomiasis ................ 515 8.7 Conservation ................................................................ 516 8.8 Further investigations ................................................. -
COMMONWEALTH of VIRGINIA DEPARTMENT of CONSERVATION and ECONOMIC DEVELOPMENT DIVISION of MINERAL RESOURCES Robert C
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 20 GEOLOGY OF THE OAK GROVE CORE . e- 1lg**** - rlrl""*"-*-lq j4;i; s" r "e .-e l;"* l* - :-* l,i.l-1" -*"4{ ' *-q-S''q-"_ l -a,T-,! - !:: ts"--l ::9: : ::5 :e 'l I ." t::::,:1,a::-:d:; r--" 4 f-d;:s ,:,S r,! ,:a:16:":, 9:-4:-:r:: -':"-lii;3? -F - d,* COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1980 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 20 GEOLOGY OF THE OAK GROVE CORE COMMONWEALTH OF VI RGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHAR LOTTESVI LLE, VI RGI N IA 1980 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 20 GEOLOGY OF THE OAK GROVE CORE COMMONWEALTH OF VI RGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1980 COMMONWEALTH OT VIRGINIA DEPARTMENT OF PURCHASES AND SUPPLY . RICHMOND 1980 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia FRED W. WALKER, Director JERALDF. MOORE, Deputy Director BOARD J. H. JOHNSON, West Point, Chairman A. R. DUNNING, Millwood, Vice Chairman MYRON P. ERKILETIAN, Alexandria ARTHUR P. FLIPPO. Doswell HENRY T. N. GRAVES, Luray MILDRED LAYNE, Williamsburg FREDERIC S. REED, Manakin-Sabot GEORGE P. SHAFRAN, Arlington SHELDON H. SHORT,III, Chase City NICHOLAS D. STREET, Grundy SHERMAN WALLACE, Cleveland E. FLOYD YATES, Powhatan CONTENTS' Page Part 1. -
9/3/2019 1 Bonnie Fine Jacobs Curriculum Vitae Address
9/3/2019 BONNIE FINE JACOBS CURRICULUM VITAE ADDRESS: Roy M. Huffington Department of Earth Sciences P.O. Box 750395 Southern Methodist University Dallas, Texas 75275-0395 EDUCATION: Ph.D. 1983, Geosciences, University of Arizona. Past Vegetation and Climate of the Mogollon Rim Area, Arizona. M.S. 1978, Geosciences, University of Arizona. Vegetation and Modern Pollen Spectra in Sinaloa and Nayarit, Mexico. B.A. 1974, Geology/Anthropology, State University of New York at Buffalo. EMPLOYMENT: 2013 – Present. Professor, Roy M. Huffington Department of Earth Sciences, Southern Methodist University. 2006 – 2013. Associate Professor, Roy M. Huffington Department of Earth Sciences, Southern Methodist University. 2009 – 2010. Founding Director, SMU Center for the Environment, Southern Methodist University. 2000 – 2010. Director, Environmental Science Program; 2008 – 2010 founding Director Environmental Studies Program, Southern Methodist University. 2000 – 2006. Assistant Professor Southern Methodist University. 2001- Present. Research Associate Professor II of Biological Sciences, Southern Methodist University. 1995 - 2000. Adjunct Associate Professor, Departments of Anthropology and Geological Sciences, Southern Methodist University. 1986 - 1995. Adjunct Assistant Professor, Southern Methodist University, Department of Geological Sciences, Southern Methodist University. 1 9/3/2019 1985 – Present. Scientist, and Director of Palynology Laboratory, Southern Methodist University. 1984 - 2000. Adjunct Assistant Professor, Department of Biological -
Body-Enlarging Effect of Royal Jelly in a Non-Holometabolous Insect Species, Gryllus Bimaculatus
© 2016. Published by The Company of Biologists Ltd | Biology Open (2016) 5, 770-776 doi:10.1242/bio.019190 RESEARCH ARTICLE Body-enlarging effect of royal jelly in a non-holometabolous insect species, Gryllus bimaculatus Atsushi Miyashita, Hayato Kizaki, Kazuhisa Sekimizu and Chikara Kaito* ABSTRACT (Conlon and Raff, 1999; Otto, 2007). These studies have provided Honeybee royal jelly is reported to have body-enlarging effects in significant insight into the principles of size regulation of living holometabolous insects such as the honeybee, fly and silkmoth, but organisms, although recent concerns over genetically modified its effect in non-holometabolous insect species has not yet been organisms have led researchers to evaluate other types of strategies examined. The present study confirmed the body-enlarging effect in to enlarge animals for industrial purposes. silkmoths fed an artificial diet instead of mulberry leaves used in the As a non-genetic size manipulation, oral ingestion of royal jelly previous literature. Administration of honeybee royal jelly to silkmoth by larvae of the honeybee, Apis mellifera, a holometabolous from early larval stage increased the size of female pupae and hymenopteran insect, induces queen differentiation, leading to adult moths, but not larvae (at the late larval stage) or male pupae. enlarged bodies. Royal jelly contains 12-15% protein, 10-16% We further examined the body-enlarging effect of royal jelly in a sugar, 3-6% lipids (percentages are wet-weight basis), vitamins, non-holometabolous species, the two-spotted cricket Gryllus salts, and free amino acids (Buttstedt et al., 2014). Royal jelly bimaculatus, which belongs to the evolutionarily primitive group contains proteins, named major royal jelly proteins (MRJPs), which Polyneoptera. -
Open Thesis Currano Final.Pdf
The Pennsylvania State University The Graduate School Department of Geosciences VARIATIONS IN INSECT HERBIVORY ON ANGIOSPERM LEAVES THROUGH THE LATE PALEOCENE AND EARLY EOCENE IN THE BIGHORN BASIN, WYOMING, USA A Dissertation in Geosciences by Ellen Diane Currano © 2008 Ellen D. Currano Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy August 2008 The dissertation of Ellen D. Currano was reviewed and approved* by the following: Peter Wilf Associate Professor of Geosciences John T. Ryan, Jr., Faculty Fellow Dissertation Advisor Chair of Committee Russell W. Graham Director of the Earth and Mineral Sciences Museum Associate Professor of Geosciences Conrad C. Labandeira Curator of Paleoentomology, Smithsonian Institution Chairman of the Department of Paleobiology, Smithsonian Institution Special Member Lee Ann Newsom Associate Professor of Anthropology Member Scientist of the Penn State Institutes of the Environment Mark E. Patzkowsky Associate Professor of Geosciences Scott L. Wing Curator of Paleobotany, Smithsonian Institution Special Member Katherine H. Freeman Associate Department Head of Graduate Programs Professor of Geosciences *Signatures are on file in the Graduate School ii ABSTRACT Climate, terrestrial biodiversity, and distributions of organisms all underwent significant changes across the Paleocene-Eocene boundary (55.8 million years ago, Ma). However, the effects of these changes on interactions among organisms have been little studied. Here, I compile a detailed record of insect herbivory on angiosperm leaves for the Bighorn Basin of Wyoming and investigate the causes of variation in insect herbivory. I test whether the changes in temperature, atmospheric carbon dioxide, and floral diversity observed across the Paleocene-Eocene boundary correlate with changes in insect damage frequency, diversity, and composition. -
From the Middle Jurassic of Daohugou, Inner Mongolia, China
Two new kalligrammatids (Insecta, Neuroptera) from the Middle Jurassic of Daohugou, Inner Mongolia, China QING LIU*, DARAN ZHENG, QI ZHANG, BO WANG, YAN FANG and HAICHUN ZHANG LIU, Q., ZHENG, D.R., ZHANG, Q., WANG, B., FANG,Y.&ZHANG, H.C., iFirst article. Two new kalligrammatids (Insecta, Neuroptera) from the Middle Jurassic of Daohugou, Inner Mongolia, China. Alcheringa 38, XX–XX. ISSN 0311-5518. A new genus and two new species of kalligrammatid lacewings (Insecta, Neuroptera), Kalligramma paradoxum sp. nov. and Huiyingogramma formosum gen. et sp. nov., are described and figured, based on two well-preserved forewings from the Middle Jurassic of Daohugou, Inner Mongolia, China. Kalligramma paradoxum sp. nov. can be distinguished from other known Kalligramma species based on forewing characters (e.g., wing shape, costal space, branches of Rs, eye-spot). Huiyingogramma gen. nov. is characterized by a distinct humeral recurrent vein, relatively broad costal space with well-forked costal veinlets, well-developed eye-spot and dense crossveins over the entire wing. Qing Liu (corresponding author) [[email protected]; [email protected]], Daran Zheng [[email protected]], Qi Zhang [[email protected]], Bo Wang [[email protected]], Yan Fang [[email protected]] and Haichun Zhang [[email protected]], State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, PR China; secondary address of Daran Zheng & Qi Zhang, University of Chinese Academy of Sciences, Beijing, 100049, PR China. Received 15.4.2013, revised 9.6.2013, accepted 24.6.2103. Key words: Neuroptera, Kalligrammatidae, Kalligramma, Huiyingogramma, eye-spot, Middle Jurassic, China. -
FOLIAR MORPHOLOGY and ANATOMY of the GIGANTOPTERID PLANT DELNORTEA ABBOTTIAE, from the LOWER PERMIAN of WEST Texasl
Arner. J. Bot. 75(9): 1409-1433. 1988. FOLIAR MORPHOLOGY AND ANATOMY OF THE GIGANTOPTERID PLANT DELNORTEA ABBOTTIAE, FROM THE LOWER PERMIAN OF WEST TEXASl SERGIUS H. MAMAY,2 JOHN M. MILLER,3 DAVID M. ROHR,4 AND WILLIAM E. STEIN, JR.5 'Department of Paleobiology, Smithsonian Institution, Washington, DC 20560; 'Department of Botany, Oregon State University, Corvallis, Oregon 97331; 4Department ofGeology, SuI Ross State University, Alpine, Texas 79832; and 'Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 48109 ABSTRACT Delnortea is a monotypic genus (type-species: D. abbottiae) ofLower Permian gymnosperms based on leaves from uppermost Leonardian deltaic sediments exposed in the Del Norte Moun tains, West Texas. The leaves are simple, symmetrical, mostly oblong or elliptical, and vary in length from 1.2 to about 35 ern. The petioles are short and stout, with a basally enlarged abscission zone. The margins are crenate, with a narrow, indurated border. Venation is in 4 orders: the secondaries and tertiaries are robust, unbranched, and pinnately arranged in a precise "herringbone" pattern, with the secondaries ending in the marginal sinuses; the quaternaries divide sparingly and fuse with others to form a dense reticulum ofsmall meshes. Permineralized petiole and midrib material reflects a bifacial cambium, shown by a semicircular vascular arc, irregularly divided into several collateral bundles with secondary xylem and phloem. Delnortea is referable to the Gigantopteridaceae, a probably artificial family of gymnosperms incertae sedis with important venation features in common, but without known diagnostic reproductive organs. With Delnortea. the North American gigantopterids now include 5 genera, but Gigan topteris itselfis lacking. -
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. -
Divergence in Gut Bacterial Community Among Life Stages of the Rainbow Stag Beetle Phalacrognathus Muelleri (Coleoptera: Lucanidae)
insects Article Divergence in Gut Bacterial Community Among Life Stages of the Rainbow Stag Beetle Phalacrognathus muelleri (Coleoptera: Lucanidae) 1,2, 1,2, 1,2, Miaomiao Wang y, Xingjia Xiang y and Xia Wan * 1 School of Resources and Environmental Engineering, Anhui University, Hefei 230601, China; [email protected] (M.W.); [email protected] (X.X.) 2 Anhui Province Key Laboratory of Wetland Ecosystem Protection and Restoration, Hefei 230601, China * Correspondence: [email protected] These authors contributed equally to this article. y Received: 19 September 2020; Accepted: 17 October 2020; Published: 21 October 2020 Simple Summary: Phalacrognathus muelleri is naturally distributed in Queensland (Australia) and New Guinea, and this species can be successfully bred under artificial conditions. In this study, we compared gut bacterial community structure among different life stages. There were dramatic shifts in gut bacterial community structure between larvae and adults, which was probably shaped by their diet. The significant differences between early instar and final instars larvae suggested that certain life stages are associated with a defined gut bacterial community. Our results contribute to a better understanding of the potential role of gut microbiota in a host’s growth and development, and the data will benefit stag beetle conservation in artificial feeding conditions. Abstract: Although stag beetles are popular saprophytic insects, there are few studies about their gut bacterial community. This study focused on the gut bacterial community structure of the rainbow stag beetle (i.e., Phalacrognathus muelleri) in its larvae (three instars) and adult stages, using high throughput sequencing (Illumina Miseq). Our aim was to compare the gut bacterial community structure among different life stages. -
Middle Eocene Trees of the Clarno Petrified Forest, John Day Fossil Beds National Monument, Oregon
PaleoBios 30(3):105–114, April 28, 2014 © 2014 University of California Museum of Paleontology Middle Eocene trees of the Clarno Petrified Forest, John Day Fossil Beds National Monument, Oregon ELISABETH A. WHEELER1 and STEVEN R. MANCHESTER2 1Department of Forest Biomaterials, North Carolina State University, Raleigh, NC 27605-8005 USA; elisabeth_ [email protected]. 2Florida Museum of Natural History, University of Florida, Gainesville, FL 32611 USA; steven@ flmnh.ufl.edu One of the iconic fossils of the John Day Fossil Beds National Monument, Oregon, USA, is the Hancock Tree—a permineralized standing tree stump about 0.5 m in diameter and 2.5 m in height, embedded in a lahar of the Clarno Formation of middle Eocene age. We examined the wood anatomy of this stump, together with other permineralized woods and leaf impressions from the same stratigraphic level, to gain an understanding of the vegetation intercepted by the lahar. Wood of the Hancock Tree is characterized by narrow and numerous vessels, exclusively scalariform perforation plates, exclusively uniseriate rays, and diffuse axial parenchyma. These features and the type of vessel-ray parenchyma indicate affinities with the Hamamelidaceae, with closest similarity to the Exbucklandoideae, which is today native to Southeast and East Asia. The Hancock Tree is but one of at least 48 trees entombed in the same mudflow; 14 others have anatomy similar to the Hancock Tree; 20 have anatomy similar to Platanoxylon haydenii (Platanaceae), two resemble Scottoxylon eocenicum (probably in order Urticales). The latter two wood types occur in the nearby Clarno Nut Beds. Two others are distinct types of dicots, one with features seen in the Juglandaceae, the other of unknown affinities, and the rest are very poorly preserved and of unknown affinity.