Pteridophytes, Gymnosperms and Paleobotany)
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A Comparative Study of the Primary Vascular System Of
Amer. J. Bot. 55(4): 464-472. 1!16'>. A COMPARATIVE STUDY OF THE PRIMARY VASCULAR SYSTE~1 OF CONIFERS. III. STELAR EVOLUTION IN GYMNOSPERMS 1 KADAMBARI K. NAMBOODIRI2 AND CHARLES B. BECK Department of Botany, University of Michigan, Ann Arbor ABST RAe T This paper includes a survey of the nature of the primary vascular system in a large number of extinct gymnosperms and progymnosperms. The vascular system of a majority of these plants resembles closely that of living conifers, being characterized, except in the most primitive forms which are protostelic, by a eustele consisting of axial sympodial bundles from which leaf traces diverge. The vascular supply to a leaf originates as a single trace with very few exceptions. It is proposed that the eustele in the gyrr.nosperms has evolved directly from the protostele by gradual medullation and concurrent separation of the peripheral conducting tissue into longitudinal sympodial bundles from which traces diverge radially. A subsequent modification results in divergence of traces in a tangential plane, The closed vascular system of conifers with opposite and whorled phyllotaxis, in which the vascular supply to a leaf originates as two traces which subsequently fuse, is considered to be derived from the open sympodial system characteristic of most gymnosperms. This hypothesis of stelar evolution is at variance with that of Jeffrey which suggests that the eustele of seed plants is derived by the lengthening and overlapping of leaf gaps in a siphonostele followed by further reduction in the resultant vascular bundles. This study suggests strongly that the "leaf gap" of conifers and other extant gymnosperms is not homologous with that of siphonostelic ferns and strengthens the validity of the view that Pterop sida is an unnatural group. -
Origin and Evolution of Lycopods ""'"'Ill{
Origin and evolution of lycopods C. G. K. Ramanujam Ramanujam CGK 1992. Origin and evolution of lycopods. Palaeobotanist 41 51·57. The lycopods are known from as early as Sieginean Stage of the Lower Devonian. Lower and Middle Devonian lycopods were all herbaceous. Arborescent taxa appeared by Upper Devonian (e.g., Cyclostigma and Lepidosigillaria). The microphyllous foliage of lycopods seem to have originated from enations as well as telomic trusses. The lycopods auained peak of their evolution during the Upper Carboniferous. Towards the close of the Carboniferous and dawn of the Permian, with gradual dWindling and disappearance of swamps, the lepidodendrids suffered drastic decline numerically and phytogeographically. General aridity of the Triassic resulted in acute dwarfing as evidenced by Pleuromeia. This trend continued funher resulting in the highly telescoped Nathorstiana during the Cretaceous. The earlier lycopods were homosporous; heterospory appeared by Upper Devonian. Heterospory ran rampant in the Lepidodendrales. The ultimate in heterospory and the approach to seed habit could be witnessed in Lepidocarporz. Four discrete types of strobilus organization could be recognized by the Lower Carboniferous, viz., 1. Lepidostrobus type, 2. Mazocarpon type, 3. Achlamydocarpon type, and 4. Lepidocarpon type. Recent studies point towards the origin of lycopods along rwo different pathways, with both Zosterophyllopsida and Rhyniopsida representing the progenirors All available evidence show that Lycopsida constitutes a "Blind Alley" -
Prepared in Cooperation with the Lllinois State Museum, Springfield
Prepared in cooperation with the lllinois State Museum, Springfield Richard 1. Leary' and Hermann W. Pfefferkorn2 ABSTRACT The Spencer Farm Flora is a compression-impression flora of early Pennsylvanian age (Namurian B, or possibly Namurian C) from Brown County, west-central Illinois. The plant fossils occur in argillaceous siltstones and sand- stones of the Caseyville Formation that were deposited in a ravine eroded in Mississippian carbonate rocks. The plant-bearing beds are the oldest deposits of Pennsylva- nian age yet discovered in Illinois. They were formed be- fore extensive Pennsylvanian coal swamps developed. The flora consists of 29 species and a few prob- lematical forms. It represents an unusual biofacies, in which the generally rare genera Megalopteris, Lesleya, Palaeopteridium, and Lacoea are quite common. Noegger- athiales, which are seldom present in roof-shale floras, make up over 20 percent of the specimens. The Spencer Farm Flora is an extrabasinal (= "upland1') flora that was grow- ing on the calcareous soils in the vicinity of the ravine in which they were deposited. It is suggested here that the Noeggerathiales may belong to the Progymnosperms and that Noeggerathialian cones might be derived from Archaeopteris-like fructifica- tions. The cone genus Lacoea is intermediate between Noeggerathiostrobus and Discini tes in its morphology. Two new species, Lesleya cheimarosa and Rhodeop- teridi urn phillipsii , are described, and Gulpenia limbur- gensis is reported from North America for the first time. INTRODUCTION The Spencer Farm Flora (table 1) differs from other Pennsylvanian floras of the Illinois Basin. Many genera and species in the Spencer Farm Flora either have not been found elsewhere in the basin or are very l~uratorof Geology, Illinois State Museum, Springfield. -
New Paleobotanical Data on the Portuguese Pennsylvanian (Douro Carboniferous Basin, NW Portugal)
Versão online: http://www.lneg.pt/iedt/unidades/16/paginas/26/30/185 Comunicações Geológicas (2014) 101, Especial I, 409-414 IX CNG/2º CoGePLiP, Porto 2014 ISSN: 0873-948X; e-ISSN: 1647-581X New paleobotanical data on the Portuguese Pennsylvanian (Douro Carboniferous Basin, NW Portugal) Novos dados paleobotânicos do Pensilvaniano português (Bacia Carbonífera do Douro, NW Portugal) P. Correia1*, Z. Šimůnek2, J. Pšenička3, A. A. Sá4,5, R. Domingos6, A. Carneiro7, D. Flores1,7 Artigo Curto Short Article © 2014 LNEG – Laboratório Nacional de Geologia e Energia IP Abstract: This paper describes nine new macrofloral taxa from 1. Introduction Douro Carboniferous Basin (lower Gzhelian) of Portugal. The plant assemblage is mainly composed by pteridophylls (Sphenopteriss The fossil flora of Carboniferous of Portugal is still little arberi Kidston, Sphenopteris fayoli Zeiller, Sphenopteris tenuis known. The new megafloral occurrences recently found in Schenk, Odontopteris schlotheimii Brongniart), sphenopsids the Upper Pennsylvanian strata of Douro Carboniferous (Annularia spicata Gutbier, Stellotheca robusta (Feistmantel) Basin (DCB) provide new and important data about Surange and Prakash, Calamostachys grandis Zeiller (Jongmans) and Calamostachys calathifera Sterzel) besides the gymnosperm paleobotanical richness and diversity of the Paleozoic Cordaites foliolatus Grand`Eury. The new data provide a better floras of Portugal offering more information to previous understating of the knowledge of Late Carboniferous floras of researches reported from diverse localities and by different Portugal, showing the high plant diversity of Gzhelian floras, when authors (e.g. Wenceslau de Lima, Bernardino António considerable changes in paleogeography and climate dynamics are Gomes, Carlos Ribeiro, Carríngton da Costa, Carlos evidenced in Euramerican floristic assemblages. -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
<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. -
Tansley Review Evolution of Development of Vascular Cambia and Secondary Growth
New Phytologist Review Tansley review Evolution of development of vascular cambia and secondary growth Author for correspondence: Rachel Spicer1 and Andrew Groover2 Andrew Groover 1The Rowland Institute at Harvard, Cambridge, MA, USA; 2Institute of Forest Genetics, Pacific Tel: +1 530 759 1738 Email: [email protected] Southwest Research Station, USDA Forest Service, Davis, CA, USA Received: 29 December 2009 Accepted: 14 February 2010 Contents Summary 577 V. Evolution of development approaches for the study 587 of secondary vascular growth I. Introduction 577 VI. Conclusions 589 II. Generalized function of vascular cambia and their 578 developmental and evolutionary origins Acknowledgements 589 III. Variation in secondary vascular growth in angiosperms 581 References 589 IV. Genes and mechanisms regulating secondary vascular 584 growth and their evolutionary origins Summary New Phytologist (2010) 186: 577–592 Secondary growth from vascular cambia results in radial, woody growth of stems. doi: 10.1111/j.1469-8137.2010.03236.x The innovation of secondary vascular development during plant evolution allowed the production of novel plant forms ranging from massive forest trees to flexible, Key words: forest trees, genomics, Populus, woody lianas. We present examples of the extensive phylogenetic variation in sec- wood anatomy, wood formation. ondary vascular growth and discuss current knowledge of genes that regulate the development of vascular cambia and woody tissues. From these foundations, we propose strategies for genomics-based research in the evolution of development, which is a next logical step in the study of secondary growth. I. Introduction this pattern characterizes most extant forest trees, significant variation exists among taxa, ranging from extinct woody Secondary vascular growth provides a means of radially lycopods and horsetails with unifacial cambia (Cichan & thickening and strengthening plant axes initiated during Taylor, 1990; Willis & McElwain, 2002), to angiosperms primary, or apical growth. -
Further Interpretation of Wodehouseia Spinata Stanley from the Late Maastrichtian of the Far East (China) M
ISSN 0031-0301, Paleontological Journal, 2019, Vol. 53, No. 2, pp. 203–213. © Pleiades Publishing, Ltd., 2019. Russian Text © M.V. Tekleva, S.V. Polevova, E.V. Bugdaeva, V.S. Markevich, Sun Ge, 2019, published in Paleontologicheskii Zhurnal, 2019, No. 2, pp. 94–105. Further Interpretation of Wodehouseia spinata Stanley from the Late Maastrichtian of the Far East (China) M. V. Teklevaa, *, S. V. Polevovab, E. V. Bugdaevac, V. S. Markevichc, and Sun Ged aBorissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647 Russia bMoscow State University, Moscow, 119991 Russia cFederal Scientific Center of the East Asia Terrestrial Biodiversity, Vladivostok, 690022 Russia dCollege of Paleontology, Shenyang Normal University, Shenyang, Liaoning Province, China *e-mail: [email protected] Received May 25, 2018; revised September 30, 2018; accepted October 15, 2018 Abstract—Dispersed pollen grains Wodehouseia spinata Stanley of unknown botanical affinity from the Maastrichtian of the Amur River Region, Far East are studied using transmitted light, scanning and trans- mission electron microscopy. The pollen was probably produced by wetland or aquatic plants, adapted to a sudden change in the water regime during the vegetation season. The pattern of the exine sculpture and spo- roderm ultrastructure suggests that insects contributed to pollination. The flange and unevenly thickened endexine could facilitate harmomegathy. A tetragonal or rhomboidal tetrad type seems to be most logical for Wodehouseia pollen. The infratectum structure suggests that Wodehouseia should be placed within an advanced group of eudicots. Keywords: Wodehouseia, exine morphology, sporoderm ultrastructure, “oculata” group, Maastrichtian DOI: 10.1134/S0031030119020126 INTRODUCTION that has lost its flange (see a review Wiggins, 1976). -
Embryophytic Sporophytes in the Rhynie and Windyfield Cherts
Transactions of the Royal Society of Edinburgh: Earth Sciences http://journals.cambridge.org/TRE Additional services for Transactions of the Royal Society of Edinburgh: Earth Sciences: Email alerts: Click here Subscriptions: Click here Commercial reprints: Click here Terms of use : Click here Embryophytic sporophytes in the Rhynie and Windyeld cherts Dianne Edwards Transactions of the Royal Society of Edinburgh: Earth Sciences / Volume 94 / Issue 04 / December 2003, pp 397 - 410 DOI: 10.1017/S0263593300000778, Published online: 26 July 2007 Link to this article: http://journals.cambridge.org/abstract_S0263593300000778 How to cite this article: Dianne Edwards (2003). Embryophytic sporophytes in the Rhynie and Windyeld cherts. Transactions of the Royal Society of Edinburgh: Earth Sciences, 94, pp 397-410 doi:10.1017/S0263593300000778 Request Permissions : Click here Downloaded from http://journals.cambridge.org/TRE, IP address: 131.251.254.13 on 25 Feb 2014 Transactions of the Royal Society of Edinburgh: Earth Sciences, 94, 397–410, 2004 (for 2003) Embryophytic sporophytes in the Rhynie and Windyfield cherts Dianne Edwards ABSTRACT: Brief descriptions and comments on relationships are given for the seven embryo- phytic sporophytes in the cherts at Rhynie, Aberdeenshire, Scotland. They are Rhynia gwynne- vaughanii Kidston & Lang, Aglaophyton major D. S. Edwards, Horneophyton lignieri Barghoorn & Darrah, Asteroxylon mackiei Kidston & Lang, Nothia aphylla Lyon ex Høeg, Trichopherophyton teuchansii Lyon & Edwards and Ventarura lyonii Powell, Edwards & Trewin. The superb preserva- tion of the silica permineralisations produced in the hot spring environment provides remarkable insights into the anatomy of early land plants which are not available from compression fossils and other modes of permineralisation. -
Ordovician Land Plants and Fungi from Douglas Dam, Tennessee
PROOF The Palaeobotanist 68(2019): 1–33 The Palaeobotanist 68(2019): xxx–xxx 0031–0174/2019 0031–0174/2019 Ordovician land plants and fungi from Douglas Dam, Tennessee GREGORY J. RETALLACK Department of Earth Sciences, University of Oregon, Eugene, OR 97403, USA. *Email: gregr@uoregon. edu (Received 09 September, 2019; revised version accepted 15 December, 2019) ABSTRACT The Palaeobotanist 68(1–2): Retallack GJ 2019. Ordovician land plants and fungi from Douglas Dam, Tennessee. The Palaeobotanist 68(1–2): xxx–xxx. 1–33. Ordovician land plants have long been suspected from indirect evidence of fossil spores, plant fragments, carbon isotopic studies, and paleosols, but now can be visualized from plant compressions in a Middle Ordovician (Darriwilian or 460 Ma) sinkhole at Douglas Dam, Tennessee, U. S. A. Five bryophyte clades and two fungal clades are represented: hornwort (Casterlorum crispum, new form genus and species), liverwort (Cestites mirabilis Caster & Brooks), balloonwort (Janegraya sibylla, new form genus and species), peat moss (Dollyphyton boucotii, new form genus and species), harsh moss (Edwardsiphyton ovatum, new form genus and species), endomycorrhiza (Palaeoglomus strotheri, new species) and lichen (Prototaxites honeggeri, new species). The Douglas Dam Lagerstätte is a benchmark assemblage of early plants and fungi on land. Ordovician plant diversity now supports the idea that life on land had increased terrestrial weathering to induce the Great Ordovician Biodiversification Event in the sea and latest Ordovician (Hirnantian) -
The Fossil Flora and Age of the Wamsutta Red Beds (Middle
Document generated on 10/01/2021 10:12 p.m. Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique The fossil flora and age of the Wamsutta red beds (Middle Pennsylvanian), Narragansett Basin, southeastern Massachusetts, USA and correlation with the Cumberland Group of the Maritime Provinces of Canada Paul C. Lyons and Robert G. Sproule Volume 54, 2018 Article abstract New collections of plant macrofossils provide a precise Middle Pennsylvanian URI: https://id.erudit.org/iderudit/1055420ar age for the lower Wamsutta Formation red beds of the Narragansett Basin, DOI: https://doi.org/10.4138/atlgeol.2018.011 southeastern Massachusetts, USA. The Wamsutta assemblage indicates strong correlation with the Cumberland Group of the Maritimes Provinces of Canada, See table of contents which was earlier considered to be of late Langsettian to early Duckmantian age. This correlation is supported by the presence in the Wamsutta Formation of the following plant-fossil species: Neuralethopteris schlehanii, Neuropteris Publisher(s) obliqua, Senftenbergia plumosa, Calamites suckowii, Annularia asteris, Annularia cf. microphylla,Asterophyllites charaeformis, Asterophyllites Atlantic Geoscience Society grandis, Asterophyllites lindleyanus, Sphenophyllum cuneifolium, and Sphenopteris valida. Moreover, the new fossil flora resembles the Middle ISSN Pennsylvanian florules of western Europe, such as the Laveineopteris loshii Subzone. The new flora is especially similar to those of the Iberian Peninsula, 0843-5561 (print) where there is a complete succession of Carboniferous macrofloral zones, and 1718-7885 (digital) this similarity confirms a late Langsettian or early Duckmantian age for the lower Wamsutta macroflora. The new collections of Wamsutta Formation Explore this journal plant fossils, along with a smaller existing collection, represent the oldest known macroflora in the Narragansett Basin. -
Scouring-Rush Horsetail Scientific Name: Equisetum Hyemale Order
Common Name: Scouring-rush Horsetail Scientific Name: Equisetum hyemale Order: Equisetales Family: Equisetaceae Wetland Plant Status: Facultative Ecology & Description Scouring-rush horsetail is an evergreen, perennial plant that completes a growing season in two years. At maturity, scouring-rush horsetail usually averages 3 feet in height but can be range anywhere from 2 to 5 feet. It can survive in a variety of environments. One single plant can spread 6 feet in diameter. It has cylindrical stems that averages a third of an inch in diameter. Noticeably spotted are the jointed unions that are located down the plant. The stems are hollow and don’t branch off into additional stems. Also, scouring- rush horsetail has rough ridges that run longitudinal along the stem. Although not covered in leaves, tiny leaves are joined together around the stem which then forms a black or green band, or sheath at each individual joint on the stem. This plant has an enormous root system that can reach 6 feet deep and propagates in two ways: rhizomes and spores. Incredibly, due to the fact that this plant is not full of leaves, it is forced to photosynthesize through the stem rather than leaves. Habitat Scouring-rush horsetail is highly tolerant of tough conditions. It can survive and thrive in full sun or part shade and can successfully grow in a variety of soil types. It can also grow in moderate to wet soils, and can survive in up to 4 inches of water. Distribution Scouring-rush horsetail can be found throughout the United States, Eurasia, and Canada.