132Nd Annual Academy Meeting Abstracts March 25, 2017
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IGCP 632, the Jurassic–Cretaceous Transition In
IGCP 79 IGCP 632, The Jurassic–Cretaceous transition in North Eastern China (western Liaoning and Inner Mongolia): An IGCP meeting and field excursion on the conti- nental Jurassic Jingeng Sha1, Yanhong Pan1, Enpu Gong2, and Vivi Vajda3* 1 LPS, Nanjing Institute of Geology & Paleontology, Nanjing 210008, China 2 Northeastern University, Shenyang 110004, China 3 Swedish Museum of Natural History, Frescativägen 40, 114 18 Stockholm, Sweden, *Corresponding author, E-mail: [email protected] Exposures of strata spanning the Jurassic–Cretaceous boundary been discovered. However, the correlation of the various lithostrati- occur within several basins in western Liaoning and adjacent Inner graphic units in this area is complicated due to patchy exposures and Mongolia. These continental successions host world-renowned plant the scarcity of radiometric constraints, which pose a challenge to researchers and animal fossils including feathered dinosaurs and the oldest flow- working on these deposits. ering plant, Archaeofructus. The first feathered dinosaurs from north- To understand the stratigraphy and context of the Jurassic–Creta- eastern China where found about 20 years ago and created a major ceous biota in Liaoning province, the second IGCP-632 symposium impact in science and the media. Since then, many new specimens have was organized in Liaoning, including a two-day presentation (Sep- Figure 1. (A) Sketch map over the field excursion area in north-eastern China. (B) enlargement of the field region showing the localities of the field stops. Episodes Vol. 40, no. 1 80 intracontinental orogenic system, the Yanshan Movement, and creating a new basin-range system in east Asia. Vivi Vajda presented new results (Peterffy et al., 2015; Vajda et al., 2016) where she compre- hensively analyzed the end-Triassic mass extinc- tion and aftermath and its causal mechanisms, particularly stressing the affects of Jurassic vol- canism in disrupting the major ecosystems but also its importance for fossilization. -
The Jurassic Fossil Wood Diversity from Western Liaoning, NE China
Jiang et al. Journal of Palaeogeography (2019) 8:1 https://doi.org/10.1186/s42501-018-0018-y Journal of Palaeogeography RESEARCH Open Access The Jurassic fossil wood diversity from western Liaoning, NE China Zi-Kun Jiang1,2, Yong-Dong Wang2,3*, Ning Tian4,5, Ao-Wei Xie2,6, Wu Zhang7, Li-Qin Li2 and Min Huang1 Abstract Western Liaoning is a unique region in China that bears diverse types of Jurassic plants, including leaves, fern rhizomes, and wood, providing significant proxy for vegetation and palaeoenvironment reconstruction of the well-known Yanliao Flora in East Asia. In particular, the silicified wood is very abundant in the fossil Lagerstätte of the Jurassic Tiaojishan Formation in Beipiao, western Liaoning. Previous and recent systematic investigations documented a high diversity of the Jurassic wood assemblages. These assemblages are dominated by conifers, followed by cycads and ginkgoaleans. In total, about 30 species belonging to 21 genera of fossil wood have been recorded so far, which are represented by Cycadopsida, Ginkgopsida, Coniferopsida, and Gymnospermae incertae sedis. The evolutionary implications of several distinctive fossil wood taxa as well as palaeoclimate implications are summarized based on their anatomical structures and growth ring patterns. This work approaches the vegetation development and evolutionary significances of the wood taxa and their relatives, and provides clues for the further understanding of the diversity of the Jurassic Yanliao Flora in East Asia. Keywords: Fossil wood, Diversity, Evolution, Tiaojishan Formation, Jurassic 1 Introduction 2004;Wangetal.,2009). Among these localities, western Fossil floras are a significant record for the vegetation Liaoning is a well-known fossil Lagerstätte with diverse and for the palaeoenvironment reconstructions of the and well-preserved fossil plant foliages and wood (Zhang Mesozoic. -
Plant Mobility in the Mesozoic Disseminule Dispersal Strategies Of
Palaeogeography, Palaeoclimatology, Palaeoecology 515 (2019) 47–69 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Plant mobility in the Mesozoic: Disseminule dispersal strategies of Chinese and Australian Middle Jurassic to Early Cretaceous plants T ⁎ Stephen McLoughlina, , Christian Potta,b a Palaeobiology Department, Swedish Museum of Natural History, Box 50007, 104 05 Stockholm, Sweden b LWL - Museum für Naturkunde, Westfälisches Landesmuseum mit Planetarium, Sentruper Straße 285, D-48161 Münster, Germany ARTICLE INFO ABSTRACT Keywords: Four upper Middle Jurassic to Lower Cretaceous lacustrine Lagerstätten in China and Australia (the Daohugou, Seed dispersal Talbragar, Jehol, and Koonwarra biotas) offer glimpses into the representation of plant disseminule strategies Zoochory during that phase of Earth history in which flowering plants, birds, mammals, and modern insect faunas began to Anemochory diversify. No seed or foliage species is shared between the Northern and Southern Hemisphere fossil sites and Hydrochory only a few species are shared between the Jurassic and Cretaceous assemblages in the respective regions. Free- Angiosperms sporing plants, including a broad range of bryophytes, are major components of the studied assemblages and Conifers attest to similar moist growth habitats adjacent to all four preservational sites. Both simple unadorned seeds and winged seeds constitute significant proportions of the disseminule diversity in each assemblage. Anemochory, evidenced by the development of seed wings or a pappus, remained a key seed dispersal strategy through the studied interval. Despite the rise of feathered birds and fur-covered mammals, evidence for epizoochory is minimal in the studied assemblages. Those Early Cretaceous seeds or detached reproductive structures bearing spines were probably adapted for anchoring to aquatic debris or to soft lacustrine substrates. -
The Basics of Beekeeping
The Basics of Beekeeping by M. M. Peterson on behalf of the Dunblane and Stirling Districts Beekeepers' Association 2017 edition Contents 1 Introduction 6 1.1 The beekeeper . 6 1.2 Development of methods of beekeeping . 8 1.3 Significant bee forage plants in our Association area . 10 2 Beekeeping Equipment 11 2.1 Beehives and their accessories . 11 2.1.1 Introduction . 11 2.1.2 The National hive and its accessories . 12 2.2 Protective clothing . 15 2.3 Tools for working with bees . 15 2.4 Harvesting tools . 16 2.5 Miscellaneous and specialist items . 17 2.6 Appendix | other hive designs . 17 2.6.1 Introduction . 17 2.6.2 The (Unmodified) National hive and the Wormit Commercial hive . 17 2.6.3 The Smith hive . 17 2.6.4 The WBC hive . 18 2.6.5 Some more unusual hive designs . 18 3 The basic biology of Apis mellifera, the western honeybee 19 3.1 Introduction . 19 3.2 The place of the honey bee in nature . 19 3.3 Where bees live . 21 3.4 The end of summer . 21 3.5 Stings . 21 3.6 The casting of the drones . 22 3.7 Wintering . 22 3.8 The spring build-up: brood-rearing . 22 3.9 Foraging, colony growth and bee longevity . 23 3.10 Reproduction: Dzierzon's rule, and drones . 23 3.11 Swarming and the rearing of new queens . 24 3.12 Queen production in other circumstances . 25 3.13 Autumn returns . 25 4 Handling: Spring and Summer Management 28 4.1 Beekeeping | basic handling skills . -
Instrumental Insemination
Rising Tide Seminar Enhancing Genetic Diversity in the U.S. Honey Bee Gene Pool Susan Cobey Endemic Range Apis mellifera Diversity carnica macedonica Honey bees are (1 (2 (2 6 1 4 Endemic to Europe, da d da ys ay ys Africa & Central Asia ) s) ) 28 recognized subspecies The first honey bees imported to the US were the “dark” bee of Northern Europe, Apis mellifera mellifera Colonies were established in Virginia by 1622. Dispersed and established widely in the countryside ahead of human colonial expansion. Historical Importations of Italian bees 1859 – First importation of A. m. ligustica. Sourced from Johann Dzierzon’s apiary in Germany. 1860 –A. m. ligustica imported directly from Italy to the U.S. Samual Parsons with beekeeping assistance from L. L. Langstroth. A subset of these subspecies were brought to North America And were established to form the basis for current honey bee populations in the United States 1922 Honey Bee Act Restricted further importations in attempt to keep out tracheal mites California Queen & Package Bee Industry Supplier of Queens & Bees to Re-Stock the Industry Nationwide Garvey Also Responsible for … Selection & Maintenance of Genetic Material Increasing Challenges… Loss of Diverse Forage Intensive Agricultural Practices Exposure to Chemical Residues Pests, Parasites & Pathogens Reduced Genetic Diversity Garvey Increasing Challenges… Malnutrition- Lack of Adequate and Diverse Forage Monoculture Crops Habitat Degradation Climate Change Sub-lethal Effects Of Chemical Exposure Queen Effects: Mating, Signaling Egg -
Mendel's Journey to Paris and London
1 Mendel’s journey to Paris and London: context and significance for the origin of 2 genetics. 3 4 5 Peter J. van Dijk 6 [email protected] 7 Keygene N.V., 8 Agro Business Park 90 9 6708 PW Wageningen, The Netherlands 10 11 12 T. H. Noel Ellis 13 Department of Metabolic Biology, 14 John Innes Centre, 15 Norwich Research Park 16 Norwich, 17 NR4 7UH, United Kingdom 18 19 20 21 1 22 Abstract 23 From a letter Gregor Mendel wrote to his brother-in-law, and a photograph of a large group of people in 24 Paris, it is known that Mendel visited the International Exhibition in London in August 1862. There has 25 been speculation about the status and composition of this travel group; for example, whether it was an 26 official delegation from the city of Brünn. There has also been speculation on whether Mendel visited 27 Charles Darwin on that occasion. We have now found a partial list of participants of the second 1862 28 pleasure train (Vergnügungszug) from Vienna to Paris and London, which includes Mendel’s name. The 29 names of 158 participants make a partial reconstruction of the travel group possible. Digital newspapers 30 were researched to get more insight into the status, residence, and profession of the participants. Most 31 belonged to the upper-class of the Austrian Empire, among them several citizens of Brünn. Such 32 luxurious all-inclusive pleasure trains were a new phenomenon in Vienna at the time and received much 33 attention in the newspapers. -
Late Jurassic Yanliao Biota: Chronology, Taphonomy, Paleontology and Paleoecology
Vol. 90 No. 6 pp.2229–2243 ACTA GEOLOGICA SINICA (English Edition) Dec. 2016 An Updated Review of the Middle-Late Jurassic Yanliao Biota: Chronology, Taphonomy, Paleontology and Paleoecology XU Xing1, *, ZHOU Zhonghe1, Corwin SULLIVAN1, WANG Yuan1 and REN Dong2 1 Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China 2 College of Life Sciences, Capital Normal University, Haidian District, Beijing 100048, China Abstract: The northeastern Chinese Yanliao Biota (sometimes called the Daohugou Biota) comprises numerous, frequently spectacular fossils of non-marine organisms, occurring in Middle-Upper Jurassic strata in western Liaoning, northern Hebei, and southeastern Inner Mongolia. The biota lasted for about 10 million years, divided into two phases: the Bathonian-Callovian Daohugou phase (about 168-164 million years ago) and the Oxfordian Linglongta phase (164-159 million years ago). The Yanliao fossils are often taphonomically exceptional (many vertebrate skeletons, for example, are complete and accompanied by preserved integumentary features), and not only are taxonomically diverse but also include the oldest known representatives of many groups of plants, invertebrates, and vertebrates. These fossils have provided significant new information regarding the origins and early evolution of such clades as fleas, birds, and mammals, in addition to the evolution of some major biological structures such as feathers, and have demonstrated the existence of a complex terrestrial ecosystem in northeast China around the time of the Middle-Late Jurassic boundary. Key words: Yanliao Biota, Daohugou phase, Linglongta phase, Middle-Late Jurassic, Yanliao area 1 Introduction 1983, when a rich insect assemblage was discovered from the Middle Jurassic Jiulongshan Formation in the Yanliao The Yanliao Area is a large region of northeast China, Area. -
Ron and Beth Ward Hillside Honey Easton, Kansas
A Brief History of Beekeeping Ron and Beth Ward Hillside Honey Easton, Kansas “Life is Sweet in Kansas!” Agenda • Beekeeping Overview • The Three General Historical Stages of Beekeeping • BeeHunter/Gatherers • BeeDomesticators • Beekeepers • American Beekeeping * Presentations @ www.NEKBA.org References • The World History of Beekeeping and Honey Hunting, Eva Crane • The ABC and XYZ of Bee Culture, A.I. Root • National Honey Board • Numerous Internet Resources • Boogerhill Bee Company Beekeeping Class • Bee Culture Magazine Why Beekeeping? Honey – Beeswax - Propolis • Food! Sweetener! Mead! • Status Symbol • Bartering/Legal Tender • Religious and Ceremonial • Medicinal • Science • Pollination Historical Timeline • For 150 – 100 Million Years – Flowering plants have existed and produced nectar and pollen • For 50 – 25 Million Years – Solitary bees had existed, also early primates • For 20 to 10 Million Years – Social bees have produced and stored honey • For a few Million Years – Man has existed and has eaten honey • For a few Thousand Years – Records exist of man’s exploitation of honey The Three General Historical Stages of Beekeeping • BeeHunter/Gatherers • BeeDomesticator • BeeKeepers BeeHunter/Gatherers • Survival – Seek out and rob wild bee colonies • No regard for the survival of the bees BeeHunter/Gatherers Early rock paintings on cave walls in Africa and eastern Spain show people gathering honey with beezzz a buzzin’. Man of Bicorp Discovered - early 1900's in Valencia, Spain Estimated - 8,000 years old BeeHunter/Gatherers • All -
Perspectives
Copyright 2002 by the Genetics Society of America Perspectives Anecdotal, Historical and Critical Commentaries on Genetics Edited by James F. Crow and William F. Dove The Emergence of Hymenopteran Genetics Robert E. Page, Jr.,*,1 Ju¨rgen Gadau,† and Martin Beye‡ *Department of Entomology, University of California, Davis, California 95616, †Institut fu¨r Verhaltensphysiologie und Soziobiologie, Universita¨tWu¨rzburg/Biozentrum, 97074 Wu¨rzburg, Germany and ‡Martin-Luther-Universita¨t, Molekulare O¨ kologie/Zoologie, Biozentrum, Weinberg Weg 22, 06120 Halle, Germany YMENOPTERAN geneticists converged on the demonstrating that eggs destined to be drones contained H 42nd Annual Drosophila Research Conference 16 chromosomes, whereas those of workers contained 32. held in Washington, DC, March 21–25, 2001, to partici- Gregor Mendel wanted to be a honeybee geneticist, pate in a workshop on the genetics of non-drosophilid but failed because he could not control the matings of insects and for a special satellite symposium on Hyme- queens and drones (Iltis 1924; Orel 1996). Mendel noptera. These were a result of a growing interest in wanted to breed bees belonging to different races and the genetics of Hymenoptera, recognition of the need take advantage of the effects of hybrid vigor for produc- to integrate with Drosophila geneticists, and the desire ing a better honey producer, a common theme through- to share information and methodology. It was clear from out the history of bee breeding. Apparently he also both meetings that the honeybee (Apis mellifera) and wanted to use Dzierzon’s discovery of haplodiploidy and the parasitic wasp (Nasonia vitripennis) and its closely look for segregation of color variants in the drones of related congeners are emerging as important experi- hybrid queens derived from crosses of different races. -
Crossroads Conference
Crossroads Geology Conference 2017 Sponsored by: CROSSROADS GEOLOGY CONFERENCE 2017 Welcome We would like to extend a special thank you to all of those participating in the 17th Annual Crossroads Geology Conference at Indiana University. This conference is a rich tradition for the Department of Earth and Atmospheric Sciences and we anticipate that this year’s presentations will uphold previous standards of excellence. Additionally, we are excited to present our keynote speaker, Dr. Darren Ficklin from the Indiana University Department of Geography. Finally, we want to thank our sponsors, judges, the Department of Earth and Atmospheric Sciences at Indiana University, and all of those who have volunteered their time for the preparation and execution of Crossroads 2017. Sigma Gamma Epsilon, Rho Chapter Officers Devon Colcord, President Ciara Mills, Vice President Alex Zimmerman, Treasurer Maggie Holahan, Secretary Dr. Claudia Johnson, Faculty Advisor Crossroads Committee Cameron Stewart and Andrea White..............................................................Co-Chairs Silvia Ascari.....................................................................................Program Designer Maggie Holahan, Hanah Sloan, and Chris Fitzgerald..............................Food Committee Chris Helou....................................................................................Judges Coordinator Scott David, Brigid Lynch, and Nate Mitchell................................Operations Committee 1 Crossroads Judges Joel Degenstein...................IU -
Plant Remains from the Middle–Late Jurassic Daohugou Site of the Yanliao Biota in Inner Mongolia, China
Acta Palaeobotanica 57(2): 185–222, 2017 e-ISSN 2082-0259 DOI: 10.1515/acpa-2017-0012 ISSN 0001-6594 Plant remains from the Middle–Late Jurassic Daohugou site of the Yanliao Biota in Inner Mongolia, China CHRISTIAN POTT 1,2* and BAOYU JIANG 3 1 LWL-Museum of Natural History, Westphalian State Museum and Planetarium, Sentruper Straße 285, DE-48161 Münster, Germany; e-mail: [email protected] 2 Palaeobiology Department, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 3 School of Earth Sciences and Engineering, Nanjing University, 163 Xianlin Avenue, Qixia District, Nanjing 210046, China Received 29 June 2017; accepted for publication 20 October 2017 ABSTRACT. A late Middle–early Late Jurassic fossil plant assemblage recently excavated from two Callovian– Oxfordian sites in the vicinity of the Daohugou fossil locality in eastern Inner Mongolia, China, was analysed in detail. The Daohugou fossil assemblage is part of the Callovian–Kimmeridgian Yanliao Biota of north-eastern China. Most major plant groups thriving at that time could be recognized. These include ferns, caytonialeans, bennettites, ginkgophytes, czekanowskialeans and conifers. All fossils were identified and compared with spe- cies from adjacent coeval floras. Considering additional material from three collections housed at major pal- aeontological institutions in Beijing, Nanjing and Pingyi, and a recent account in a comprehensive book on the Daohugou Biota, the diversity of the assemblage is completed by algae, mosses, lycophytes, sphenophytes and putative cycads. The assemblage is dominated by tall-growing gymnosperms such as ginkgophytes, cze- kanowskialeans and bennettites, while seed ferns, ferns and other water- or moisture-bound groups such as algae, mosses, sphenophytes and lycophytes are represented by only very few fragmentary remains. -
Establishing a Time-Scale for Plant Evolution
New Research Phytologist Establishing a time-scale for plant evolution John T. Clarke1,2, Rachel C. M. Warnock1 and Philip C. J. Donoghue1 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK; 2Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK Summary Author for correspondence: • Plants have utterly transformed the planet, but testing hypotheses of causality Philip C. J. Donoghue requires a reliable time-scale for plant evolution. While clock methods have been Tel: +44 11 7954 5440 extensively developed, less attention has been paid to the correct interpretation Email: [email protected] and appropriate implementation of fossil data. Received: 4 April 2011 • We constructed 17 calibrations, consisting of minimum constraints and soft Accepted: 16 May 2011 maximum constraints, for divergences between model representatives of the major land plant lineages. Using a data set of seven plastid genes, we performed a New Phytologist (2011) 192: 266–301 cross-validation analysis to determine the consistency of the calibrations. Six doi: 10.1111/j.1469-8137.2011.03794.x molecular clock analyses were then conducted, one with the original calibrations, and others exploring the impact on divergence estimates of changing maxima at basal nodes, and prior probability densities within calibrations. Key words: Angiosperm, calibration, chronogram, divergence time, embryophyte, • Cross-validation highlighted Tracheophyta and Euphyllophyta calibrations as fossil record, land plant, molecular clock, inconsistent, either because their soft maxima were overly conservative or because phylogeny. of undetected rate variation. Molecular clock analyses yielded estimates ranging from 568–815 million yr before present (Ma) for crown embryophytes and from 175–240 Ma for crown angiosperms.