Developmental Programmes in the Evolution of Equisetum Reproductive Morphology: a Hierarchical Modularity Hypothesis
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Variation in Sex Expression in Canada Yew (Taxus Canadensis) Author(S): Taber D
Variation in Sex Expression in Canada Yew (Taxus canadensis) Author(s): Taber D. Allison Source: American Journal of Botany, Vol. 78, No. 4 (Apr., 1991), pp. 569-578 Published by: Botanical Society of America Stable URL: http://www.jstor.org/stable/2445266 . Accessed: 23/08/2011 15:56 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Botanical Society of America is collaborating with JSTOR to digitize, preserve and extend access to American Journal of Botany. http://www.jstor.org AmericanJournal of Botany 78(4): 569-578. 1991. VARIATION IN SEX EXPRESSION IN CANADA YEW (TAXUS CANADENSIS)1 TABER D. ALLISON2 JamesFord Bell Museumof Natural History and Departmentof Ecology and BehavioralBiology, Universityof Minnesota, Minneapolis, Minnesota 55455 Sex expressionwas measuredin severalCanada yew (Taxus canadensisMarsh.) populations of theApostle Islands of Wisconsinand southeasternMinnesota to determinethe extent of variationwithin and among populations. Sex expression was recorded qualitatively (monoecious, male,or female) and quantitatively (by male to female strobilus ratios or standardized phenotypic gender).No discernibletrends in differencesin sex expressionamong populations or habitats wererecorded. Trends in sexexpression of individuals within populations were complex. Small yewstended to be maleor, if monoecious, had female-biasedstrobilus ratios. -
<I>Equisetum Giganteum</I>
Florida International University FIU Digital Commons FIU Electronic Theses and Dissertations University Graduate School 3-24-2009 Ecophysiology and Biomechanics of Equisetum Giganteum in South America Chad Eric Husby Florida International University, [email protected] DOI: 10.25148/etd.FI10022522 Follow this and additional works at: https://digitalcommons.fiu.edu/etd Recommended Citation Husby, Chad Eric, "Ecophysiology and Biomechanics of Equisetum Giganteum in South America" (2009). FIU Electronic Theses and Dissertations. 200. https://digitalcommons.fiu.edu/etd/200 This work is brought to you for free and open access by the University Graduate School at FIU Digital Commons. It has been accepted for inclusion in FIU Electronic Theses and Dissertations by an authorized administrator of FIU Digital Commons. For more information, please contact [email protected]. FLORIDA INTERNATIONAL UNIVERSITY Miami, Florida ECOPHYSIOLOGY AND BIOMECHANICS OF EQUISETUM GIGANTEUM IN SOUTH AMERICA A dissertation submitted in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in BIOLOGY by Chad Eric Husby 2009 To: Dean Kenneth Furton choose the name of dean of your college/school College of Arts and Sciences choose the name of your college/school This dissertation, written by Chad Eric Husby, and entitled Ecophysiology and Biomechanics of Equisetum Giganteum in South America, having been approved in respect to style and intellectual content, is referred to you for judgment. We have read this dissertation and recommend that it be approved. _______________________________________ Bradley C. Bennett _______________________________________ Jack B. Fisher _______________________________________ David W. Lee _______________________________________ Leonel Da Silveira Lobo O'Reilly Sternberg _______________________________________ Steven F. Oberbauer, Major Professor Date of Defense: March 24, 2009 The dissertation of Chad Eric Husby is approved. -
Earliest Record of Megaphylls and Leafy Structures, and Their Initial Diversification
Review Geology August 2013 Vol.58 No.23: 27842793 doi: 10.1007/s11434-013-5799-x Earliest record of megaphylls and leafy structures, and their initial diversification HAO ShouGang* & XUE JinZhuang Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China Received January 14, 2013; accepted February 26, 2013; published online April 10, 2013 Evolutionary changes in the structure of leaves have had far-reaching effects on the anatomy and physiology of vascular plants, resulting in morphological diversity and species expansion. People have long been interested in the question of the nature of the morphology of early leaves and how they were attained. At least five lineages of euphyllophytes can be recognized among the Early Devonian fossil plants (Pragian age, ca. 410 Ma ago) of South China. Their different leaf precursors or “branch-leaf com- plexes” are believed to foreshadow true megaphylls with different venation patterns and configurations, indicating that multiple origins of megaphylls had occurred by the Early Devonian, much earlier than has previously been recognized. In addition to megaphylls in euphyllophytes, the laminate leaf-like appendages (sporophylls or bracts) occurred independently in several dis- tantly related Early Devonian plant lineages, probably as a response to ecological factors such as high atmospheric CO2 concen- trations. This is a typical example of convergent evolution in early plants. Early Devonian, euphyllophyte, megaphyll, leaf-like appendage, branch-leaf complex Citation: Hao S G, Xue J Z. Earliest record of megaphylls and leafy structures, and their initial diversification. Chin Sci Bull, 2013, 58: 27842793, doi: 10.1007/s11434- 013-5799-x The origin and evolution of leaves in vascular plants was phology and evolutionary diversification of early leaves of one of the most important evolutionary events affecting the basal euphyllophytes remain enigmatic. -
Anatomy of the Late Devonian Sphenopsid Rotafolia Songziensis
Anatomy of the Late Devonian Sphenopsid Rotafolia songziensis , with a Discussion of Stelar Architecture of the Sphenophyllales Author(s): De‐Ming Wang, Shou‐Gang Hao, Qi Wang, and Jin‐Zhuang Xue Source: International Journal of Plant Sciences, Vol. 167, No. 2 (March 2006), pp. 373-383 Published by: The University of Chicago Press Stable URL: http://www.jstor.org/stable/10.1086/499115 . Accessed: 02/04/2015 03:18 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The University of Chicago Press is collaborating with JSTOR to digitize, preserve and extend access to International Journal of Plant Sciences. http://www.jstor.org This content downloaded from 159.226.100.224 on Thu, 2 Apr 2015 03:18:06 AM All use subject to JSTOR Terms and Conditions Int. J. Plant Sci. 167(2):373–383. 2006. Ó 2006 by The University of Chicago. All rights reserved. 1058-5893/2006/16702-0020$15.00 ANATOMY OF THE LATE DEVONIAN SPHENOPSID ROTAFOLIA SONGZIENSIS, WITH A DISCUSSION OF STELAR ARCHITECTURE OF THE SPHENOPHYLLALES De-Ming Wang,*,y Shou-Gang Hao,1,* Qi Wang,z and Jin-Zhuang Xue* *Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University, Beijing 100871, China; yInstitute for Earth Sciences, University of Graz, A-8010 Graz, Austria; and zKey Laboratory of Systematic and Evolutionary Botany, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China A previous study of the Late Devonian (Famennian) sphenopsid Rotafolia songziensis Wang, Hao, and Wang provided detailed descriptions of the morphology and a sketchy illustration of a three-ribbed primary xylem. -
Subclase Equisetidae ¿Tienes Alguna Duda, Sugerencia O Corrección Acerca De Este Taxón? Envíanosla Y Con Gusto La Atenderemos
subclase Equisetidae ¿Tienes alguna duda, sugerencia o corrección acerca de este taxón? Envíanosla y con gusto la atenderemos. Ver todas las fotos etiquetadas con Equisetidae en Banco de Imagénes » Descripción de WIKIPEDIAES Ver en Wikipedia (español) → Ver Pteridophyta para una introducción a las plantas Equisetos vasculares sin semilla Rango temporal: Devónico-Holoceno PreЄ Є O S D C P T J K Pg N Los equisetos , llamados Equisetidae en la moderna clasificación de Christenhusz et al. 2011,[1] [2] [3] o también Equisetopsida o Equisetophyta, y en paleobotánica es más común Sphenopsida, son plantas vasculares afines a los helechos que aparecieron en el Devónico, pero que actualmente sobrevive únicamente el género Equisetum, si bien hay representantes de órdenes extintos que se verán en este artículo. Este grupo es monofilético, aun con sus representantes extintos, debido a su morfología distintiva. Son plantas pequeñas, aunque en el pasado una variedad de calamitácea alcanzó los 15 metros durante el pérmico.[4] Índice 1 Filogenia 1.1 Ecología y evolución 2 Taxonomía 2.1 Sinonimia Variedades de Equisetum 2.2 Sistema de Christenhusz et al. 2011 Taxonomía 2.3 Clasificación sensu Smith et al. 2006 2.4 Otras clasificaciones Reino: Plantae 3 Caracteres Viridiplantae 4 Véase también Streptophyta 5 Referencias Streptophytina 6 Bibliografía Embryophyta (sin rango) 7 Enlaces externos Tracheophyta Euphyllophyta Monilophyta Filogenia[editar] Equisetopsida o Sphenopsida Introducción teórica en Filogenia Clase: C.Agardh 1825 / Engler 1924 Equisetidae Los análisis moleculares y genéticos de filogenia solo Subclase: se pueden hacer sobre representantes vivientes, Warm. 1883 como circunscripto según Smith et al. (2006) (ver la Órdenes ficha), al menos Equisetales es monofilético (Pryer et Equisetales (DC. -
X. the Conifers and Ginkgo
X. The Conifers and Ginkgo Now we turn our attention to the Coniferales, another great assemblage of seed plants. First let's compare the conifers with the cycads: Cycads Conifers few apical meristems per plant many apical meristems per plant leaves pinnately divided leaves undivided wood manoxylic wood pycnoxylic seeds borne on megaphylls seeds borne on stems We should also remember that these two groups have a lot in common. To begin with, they are both groups of woody seed plants. They are united by a small set of derived features: 1) the basic structure of the stele (a eustele or a sympodium, two words for the same thing) and no leaf gaps 2) the design of the apical meristem (many initials, subtended by a slowly dividing group of cells called the central mother zone) 3) the design of the tracheids (circular-bordered pits with a torus) We have three new seed plant orders to examine this week: A. Cordaitales This is yet another plant group from the coal forest. (Find it on the Peabody mural!) The best-known genus, Cordaites, is a tree with pycnoxylic wood bearing leaves up to about a foot and a half long and four inches wide. In addition, these trees bore sporangia (micro- and mega-) in strobili in the axils of these big leaves. The megasporangia were enclosed in ovules. Look at fossils of leaves and pollen-bearing shoots of Cordaites. The large, many-veined megaphylls are ancestral to modern pine needles; the shoots are ancestral to pollen-bearing strobili of modern conifers. 67 B. -
Ecological Sorting of Vascular Plant Classes During the Paleozoic Evolutionary Radiation
i1 Ecological Sorting of Vascular Plant Classes During the Paleozoic Evolutionary Radiation William A. DiMichele, William E. Stein, and Richard M. Bateman DiMichele, W.A., Stein, W.E., and Bateman, R.M. 2001. Ecological sorting of vascular plant classes during the Paleozoic evolutionary radiation. In: W.D. Allmon and D.J. Bottjer, eds. Evolutionary Paleoecology: The Ecological Context of Macroevolutionary Change. Columbia University Press, New York. pp. 285-335 THE DISTINCTIVE BODY PLANS of vascular plants (lycopsids, ferns, sphenopsids, seed plants), corresponding roughly to traditional Linnean classes, originated in a radiation that began in the late Middle Devonian and ended in the Early Carboniferous. This relatively brief radiation followed a long period in the Silurian and Early Devonian during wrhich morphological complexity accrued slowly and preceded evolutionary diversifications con- fined within major body-plan themes during the Carboniferous. During the Middle Devonian-Early Carboniferous morphological radiation, the major class-level clades also became differentiated ecologically: Lycopsids were cen- tered in wetlands, seed plants in terra firma environments, sphenopsids in aggradational habitats, and ferns in disturbed environments. The strong con- gruence of phylogenetic pattern, morphological differentiation, and clade- level ecological distributions characterizes plant ecological and evolutionary dynamics throughout much of the late Paleozoic. In this study, we explore the phylogenetic relationships and realized ecomorphospace of reconstructed whole plants (or composite whole plants), representing each of the major body-plan clades, and examine the degree of overlap of these patterns with each other and with patterns of environmental distribution. We conclude that 285 286 EVOLUTIONARY PALEOECOLOGY ecological incumbency was a major factor circumscribing and channeling the course of early diversification events: events that profoundly affected the structure and composition of modern plant communities. -
FYLOGENÉZA a SYSTÉM VYŠŠÍCH RASTLÍN Materiály Pre Študentov Odboru Systematická Biológia
Prírodovedecká fakulta Univerzity Komenského v Bratislave Katedra botaniky Mgr. Michal Hrabovský, PhD. RNDr. Jana Ščevková, PhD. Ing. Mgr. Eva Záhradníková, PhD. FYLOGENÉZA A SYSTÉM VYŠŠÍCH RASTLÍN materiály pre študentov odboru Systematická biológia (zimný semester) 2017 Bratislava 1 Obsah Systém vyšších rastlín a zoznam druhov ku skúške ...............................................................1 Hospodársky významné vyššie rastliny ...................................................................................7 Morfologická charakteristika významných čeľadí ...................................................................9 2 SYSTÉM VYŠŠÍCH RASTLÍN A ZOZNAM DRUHOV KU SKÚŠKE (zimný semester) TRACHEOPHYTA − cievnaté rastliny ODDELENIE: Lycopodiophyta − plavúňorasty VÝVOJOVÁ VETVA: Lycopodiidae − plavúne Rad: Protolepidodendrales † − prvolepidodendronotvaré Rad: Drepanophycales † − drepanofykotvaré Rad: Lycopodiales − plavúňotvaré Čeľaď: Lycopodiaceae − plavúňovité Lycopodium clavatum − plavúň obyčajný Lycopodium annotinum − plavúň pučivý Huperzia selago − chvostník jedľovitý Rad: Selaginellales − plavúnkotvaré Čeľaď: Selaginellaceae − plavúnkovité Selaginella selaginoides − plavúnka brvitá Rad: Lepidodendrales † − lepidodendronotvaré Rad: Isoëtales − šidlatkotvaré Čeľaď: Pleuromeiaceae † − pleuromeiovité Čeľaď: Nathorstianaceae † − natorstianovité Čeľaď: Isoëtaceae − šidlatkovité ODDELENIE: Monilophyta (Pteridophyta) – papraďorasty BAZÁLNE PAPRAĎORASTY – rýniové rastliny † SKUPINA VÝVOJOVÝCH VETIEV ZOSTEROPHYLLIDAE – zosterofyly -
Deep-Time Patterns of Tissue Consumption by Terrestrial Arthropod Herbivores
Naturwissenschaften DOI 10.1007/s00114-013-1035-4 ORIGINAL PAPER Deep-time patterns of tissue consumption by terrestrial arthropod herbivores Conrad C. Labandeira Received: 21 December 2012 /Revised: 26 February 2013 /Accepted: 2 March 2013 # Springer-Verlag Berlin Heidelberg (outside the USA) 2013 Abstract A survey of the fossil record of land-plant tissues from a known anatomy of the same plant taxon in better and their damage by arthropods reveals several results that preserved material, especially permineralisations. The tro- shed light on trophic trends in host-plant resource use by phic partitioning of epidermis, parenchyma, phloem and arthropods. All 14 major plant tissues were present by the xylem increases considerably to the present, probably a end of the Devonian, representing the earliest 20 % of the consequence of dietary specialization or consumption of terrestrial biota. During this interval, two types of time lags whole leaves by several herbivore functional feeding separate the point between when tissues first originated from groups. Structural tissues, meristematic tissues and repro- their earliest consumption by herbivorous arthropods. For ductive tissues minimally have been consumed throughout epidermis, parenchyma, collenchyma and xylem, live tissue the fossil record, consistent with their long lags to herbivory consumption was rapid, occurring on average 10 m.y. after during the earlier Paleozoic. Neither angiosperm dominance the earliest tissue records. By contrast, structural tissues in floras nor global environmental perturbations had any (periderm, sclerenchyma), tissues with actively dividing discernible effect on herbivore trophic partitioning of plant cells (apical, lateral, intercalary meristems), and reproduc- tissues. tive tissues (spores, megagametophytes, integuments) expe- rienced approximately a 9-fold (92 m.y.) delay in arthropod Keywords Angiosperm diversification . -
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. -
Seasonal Growth of the Female Strobilus in Pinus Radiata
No. 1 15 SEASONAL GROWTH OF THE FEMALE STROBILUS IN PINUS RADIATA G. B. SWEET and M. P. BOLLMANN Forest Research Institute, New Zealand Forest Service, Rotorua (Received for publication 12 November, 1970) ABSTRACT Growth of female strobili of Pinus radiata D. Don from central North Island of New Zealand is described and illustrated with photographs. The two-and-a-half year period from strobilus emergence until cone maturity comprises a seasonal period of growth in which pollination occurs, a second period of seasonal growth in which fertilisation occurs, and finally a period of cone maturation. The periods of rapid growth do not appear to result directly from either pollination or fertilisation, and the seasonal growth periods have some similarity to those of vegetative growth. The time taken to reach cone maturity in P. radiata (a closed-cone pine) is six months longer than that frequently described for other species of Pinus. INTRODUCTION The general pattern of female strobilus development in Pinus is well documented (e.g., Ferguson, 1904; Stanley, 1958; Sarvas, 1962). Broadly, a total period of two-and- a-half years is involved, leading through from strobilus determination one summer, to anthesis the following spring, to fertilisation late in the subsequent spring and finally to maturation the succeeding autumn. Seed production in Pinus radiata D. Don apparently follows within general limits the typical pattern for Pinus, but few details have been published either of its strobilus or its ovule development. As part of a comprehensive study of the processes leading to seed production in this species, material was collected in 1968 and 1969 to enable details of strobilus development to be determined. -
Diversity and Evolution of the Megaphyll in Euphyllophytes
G Model PALEVO-665; No. of Pages 16 ARTICLE IN PRESS C. R. Palevol xxx (2012) xxx–xxx Contents lists available at SciVerse ScienceDirect Comptes Rendus Palevol w ww.sciencedirect.com General palaeontology, systematics and evolution (Palaeobotany) Diversity and evolution of the megaphyll in Euphyllophytes: Phylogenetic hypotheses and the problem of foliar organ definition Diversité et évolution de la mégaphylle chez les Euphyllophytes : hypothèses phylogénétiques et le problème de la définition de l’organe foliaire ∗ Adèle Corvez , Véronique Barriel , Jean-Yves Dubuisson UMR 7207 CNRS-MNHN-UPMC, centre de recherches en paléobiodiversité et paléoenvironnements, 57, rue Cuvier, CP 48, 75005 Paris, France a r t i c l e i n f o a b s t r a c t Article history: Recent paleobotanical studies suggest that megaphylls evolved several times in land plant st Received 1 February 2012 evolution, implying that behind the single word “megaphyll” are hidden very differ- Accepted after revision 23 May 2012 ent notions and concepts. We therefore review current knowledge about diverse foliar Available online xxx organs and related characters observed in fossil and living plants, using one phylogenetic hypothesis to infer their origins and evolution. Four foliar organs and one lateral axis are Presented by Philippe Taquet described in detail and differ by the different combination of four main characters: lateral organ symmetry, abdaxity, planation and webbing. Phylogenetic analyses show that the Keywords: “true” megaphyll appeared at least twice in Euphyllophytes, and that the history of the Euphyllophytes Megaphyll four main characters is different in each case. The current definition of the megaphyll is questioned; we propose a clear and accurate terminology in order to remove ambiguities Bilateral symmetry Abdaxity of the current vocabulary.