The Stele – a Developmental Perspective on the Diversity and Evolution of Primary Vascular 2 Architecture 3 4 Alexandru M.F
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History and Philosophy of Systematic Biology
History and Philosophy of Systematic Biology Bock, W. J. (1973) Philosophical foundations of classical evolutionary classification Systematic Zoology 22: 375-392 Part of a general symposium on "Contemporary Systematic Philosophies," there are some other interesting papers here. Brower, A. V. Z. (2000) Evolution Is Not a Necessary Assumption of Cladistics Cladistics 16: 143- 154 Dayrat, Benoit (2005) Ancestor-descendant relationships and the reconstruction of the Tree of Lif Paleobiology 31: 347-353 Donoghue, M.J. and J.W. Kadereit (1992) Walter Zimmermann and the growth of phylogenetic theory Systematic Biology 41: 74-84 Faith, D. P. and J. W. H. Trueman (2001) Towards an inclusive philosophy for phylogenetic inference Systematic Biology 50: 331-350 Gaffney, E. S. (1979) An introduction to the logic of phylogeny reconstruction, pp. 79-111 in Cracraft, J. and N. Eldredge (eds.) Phylogenetic Analysis and Paleontology Columbia University Press, New York. Gilmour, J. S. L. (1940) Taxonomy and philosophy, pp. 461-474 in J. Huxley (ed.) The New Systematics Oxford Hull, D. L. (1978) A matter of individuality Phil. of Science 45: 335-360 Hull, D. L. (1978) The principles of biological classification: the use and abuse of philosophy Hull, D. L. (1984) Cladistic theory: hypotheses that blur and grow, pp. 5-23 in T. Duncan and T. F. Stuessy (eds.) Cladistics: Perspectives on the Reconstruction of Evolutionary History Columbia University Press, New York * Hull, D. L. (1988) Science as a process: an evolutionary account of the social and conceptual development of science University of Chicago Press. An already classic work on the recent, violent history of systematics; used as data for Hull's general theories about scientific change. -
PLANT ANATOMY Lecture 15 - Stele and Bundle Types
Jim Bidlack - BIO 5354/4354 PLANT ANATOMY Lecture 15 - Stele and Bundle Types I. Types of steles (stellar types); stele refers to the central vascular network if the shoot and the root (includes outermost phloem and everything to the inside of it) A. Protostele 1. No pith and usually no separate vascular bundles 2. First pattern (phylogenetically) that appeared in vascular plants 3. Predominant pattern found in roots of almost all plants and shoots of lower vascular plants 4. Types of protostele a) Haplostele - xylem is a circular mass b) Actinostele - xylem margin is not smooth; it "undulates" c) Plectostele - xylem not one mass; series of plates B. Siphonostele 1. Has a pith and can have separate vascular bundles (primary growth) 2. More advanced plants 3. Found in shoots of seed plants and in roots having a broad stele (monocots) 4. Types of siphonostele a) Amphiphloic - phloem found on both sides of the xylem 1) Solenostele - very few or little leaf gaps widely separated (continuous cylinder) 2) Dictyostele - leaf gaps are abundant b) Ectophloic - phloem found only to outside of the xylem 1) Eustele (dicots) - one ring of vascular bundles surround a pith 2) Atactostele (monocots) - scattered bundle arrangement II. Stellar patterns at the node (Nodal pattern) A. Different because this is where leaves and buds are attached B. Area above & behind the leaf or bud is the leaf gap C. Area showing where the leaf (bundle(s)) attaches to stem is called leaf trace D. Examples of patterns: 1. Unilacunar, 1 trace; unilacunar, 3 trace; trilacunar, 3 trace III. -
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. -
The Lower Cretaceous Flora of the Gates Formation from Western Canada
The Lower Cretaceous Flora of the Gates Formation from Western Canada A Shesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Department of Geological Sciences Univ. of Saska., Saskatoon?SI(, Canada S7N 3E2 b~ Zhihui Wan @ Copyright Zhihui Mian, 1996. Al1 rights reserved. National Library Bibliothèque nationale 1*1 of Canada du Canada Acquisitions and Acquisitions et Bibliographic Services services bibliographiques 395 Wellington Street 395. rue Wellington Ottawa ON KlA ON4 Ottawa ON K1A ON4 Canada Canada The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant à la National Libraxy of Canada to Bibliothèque nationale du Canada de reproduce, loan, distribute or sell reproduire, prêter, distribuer ou copies of this thesis in microfom, vendre des copies de cette thèse sous paper or electronic formats. la fome de microfiche/nlm, de reproduction sur papier ou sur foxmat électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des extraits substantiels may be printed or otherwise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation. College of Graduate Studies and Research SUMMARY OF DISSERTATION Submitted in partial fulfillment of the requirernents for the DEGREE OF DOCTOR OF PHILOSOPHY ZHIRUI WAN Depart ment of Geological Sciences University of Saskatchewan Examining Commit tee: Dr. -
Additional Observations on Zosterophyllum Yunnanicum Hsü from the Lower Devonian of Yunnan, China
This is an Open Access document downloaded from ORCA, Cardiff University's institutional repository: http://orca.cf.ac.uk/77818/ This is the author’s version of a work that was submitted to / accepted for publication. Citation for final published version: Edwards, Dianne, Yang, Nan, Hueber, Francis M. and Li, Cheng-Sen 2015. Additional observations on Zosterophyllum yunnanicum Hsü from the Lower Devonian of Yunnan, China. Review of Palaeobotany and Palynology 221 , pp. 220-229. 10.1016/j.revpalbo.2015.03.007 file Publishers page: http://dx.doi.org/10.1016/j.revpalbo.2015.03.007 <http://dx.doi.org/10.1016/j.revpalbo.2015.03.007> Please note: Changes made as a result of publishing processes such as copy-editing, formatting and page numbers may not be reflected in this version. For the definitive version of this publication, please refer to the published source. You are advised to consult the publisher’s version if you wish to cite this paper. This version is being made available in accordance with publisher policies. See http://orca.cf.ac.uk/policies.html for usage policies. Copyright and moral rights for publications made available in ORCA are retained by the copyright holders. @’ Additional observations on Zosterophyllum yunnanicum Hsü from the Lower Devonian of Yunnan, China Dianne Edwardsa, Nan Yangb, Francis M. Hueberc, Cheng-Sen Lib a*School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff CF10 3AT, UK b Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China cNational Museum of Natural History, Smithsonian Institution, Washington D.C. 20560-0121, USA * Corresponding author, Tel.: +44 29208742564, Fax.: +44 2920874326 E-mail address: [email protected] ABSTRACT Investigation of unfigured specimens in the original collection of Zosterophyllum yunnanicum Hsü 1966 from the Lower Devonian (upper Pragian to basal Emsian) Xujiachong Formation, Qujing District, Yunnan, China has provided further data on both sporangial and stem anatomy. -
The Taxonomic Position of the Psilotales in the Light of Our Knowledge of Devonian Plant Life*
THE TAXONOMIC POSITION OF THE PSILOTALES IN THE LIGHT OF OUR KNOWLEDGE OF DEVONIAN PLANT LIFE* F. P. JONKER Laboratory of Palaeobotany and Palynology, Utrecht, The Netherlands ABSTRACT exclusively Devonian Psilophytales and of the latter the Rhyniaceae are regarded The order Psilotales, containing the two recent genera Psilatum and Tnzesiptel'is only, is usually usually as the closest relatives. Among classified by taxonomists and palaeo botanists those who take this st?nd I mention G. M. in the phylum Psiiophyta. This concept is, Smith (1955), Magdefra.u in Strasburger in spite of the synangia, based on the primitive (1971) and Lcmoigne (1968c). The concept general appearance reminding one of that of the of the last mentioned author will be dis• Devonian Rhyniaceae. Numerous attempts have been made to derive both genera, including their cussed further on. Darrah (1960) states synangia, from either the Rhvniaceae or from other that the status of the putative primitive Psilophyta. These attempts' sometimes led to the nature of the plant body in the Psilotaceae acceptance of a series of missing Jinks but this concept is, however, not supported bv palaeo· is controversial although there is a strong botanical data. tendency to accept the family as a pel'sis• In the opinion of the present reporter the order tent remnant of the Psilopsida. Andrews has kept a primitive general appearance of its (1961) states that Psilatum has been reaarded Devonian ancestors but in its synangia and in its monolete spores it is more advanced. by some botanists as a very simpl~ land In its anatomy, its microphyllous leaves, and in its plant, possibly a very ancient type that gametophyte perhaps, it shows more affiinity to the has managed to survive for several hundreds phylum Lycopodiophyta. -
Effect of Stele Type in the Growth Rotation of Dalbergia Melanoxylon
International Journal of Plant and Forestry Sciences Vol. 2, No. 3, May 2015, pp. 1 -10 Available online at http://ijpfs.com/ Research article Effect of Stele type in the growth rotation of Dalbergia melanoxylon. Dr. Washa B. Washa Mkwawa University College of Education Private Bag, MUCE Iringa Tanzania. E-mail: [email protected], +255 752 356 709 This work is licensed under a Creative Commons Attribution 4.0 International License. _____________________________________________________________________________________________ Abstract Examination of the effect of stele type in Dalbergia melanoxylon growth was conducted. Examination of stems to observe stele type and tissue water potential of Barreveld Faux, Cupressus sempervirens and Dalbergia melanoxylon was carried between 2nd – 23rd April 2015 at Mkwawa University Laboratories. About 120 stained stem sections were examined for stele type while other 120 stem pieces were incubated in Nacl solution for water potential. Forty (40) stained sections indicated ectophloic siphonostele in Barreveld Faux and C. sempervirens while 40 sections of D. melanoxylon indicated atactostele. Calculated water potential of Barreveld Faux was -0.01158597 bars and that of C. sempervirens was -0.01257201 bars while that of D. melanoxylon was -0.00320463 bars. Results found that, low water potential in D. melanoxylon is a factor for its slow growth rotation and this is due to the atactostele type existing in D. melanoxylon. A hard Blackwood and valued wood in D. melanoxylon is brought by this stele type. In order to initiate rapid growth rotation in D. melanoxylon is recommended to conduct genetic recombination of the D. melanoxylon with other species which have an easily growing wood although this can lower the hardwood quality and value of the D. -
Stelar Evolution
Stelar System of Plant: Definition and Types Definition of Stelar System: According to the older botanists, the vascular bundle is the fundamental unit in the vascular system of pteridophytes and higher plants. Van Tieghem and Douliot (1886) interpreted the plant body of vascular plant in the different way. According to them, the fundamental parts of a shoot are the cortex and a central cylinder, is known as stele. Thus the stele is defined as a central vascular cylinder, with or without pith and delimited the cortex by endodermis. The term stele has been derived from a Greek word meaning pillar. Van Tieghem and Douliot (1886) recognized only three types of steles. They also thought that the monostelic shoot were rare in comparison of polystelic shoots. It is an established fact that all shoots are monostelic and polystelic condition rarely occurs. The stele of the stem remains connected with that of leaf by a vascular connection known as the leaf supply. Types of Steles: 1. Protostele: Jeffrey (1898), for the first time pointed out the stelar theory from the point of view of the phylogeny. According to him, the primitive type of stele is protostele. In protostele, the vascular tissue is a solid mass and the central core of the xylem is completely surrounded by the strand of phloem. This is the most primitive and simplest type of stele. There are several forms of protostele: (a) Haplostele: This is the most primitive type of protostele. Here the central solid smooth core of xylem remains surrounded by phloem (e.g., in Selaginella spp.). -
Pterido Classes General Characters
1. Class: Psilotopsida: The members of the class Psilotopsida show close resemblance in fundamental characteristics to the Silurian and Devonian members of Rhyniopsida (e.g., Rhynia, Cooksonia), Zostero- phyllopsida (e.g., Zosterophyllum) and Trimero- phytopsida (e.g., Trimerophyton, Psilophyton). Psilotopsida includes only two living genera viz., Psilotum and Tmesipteris. Characteristic Features of Class Psilotopsida: 1. The plant body is a rootless sporophyte that differentiates into a subterranean rhizome and an aerial erect shoot. 2. Branching is dichotomous in both subterranean rhizome and aerial shoot. 3. The large rhizoids borne on the rhizome absorb water and nutrients from the soil. 4. On the aerial shoots, spirally arranged scale-like (e.g., Psilotum) or leaf-like appendages (e.g., Tmesipteris) are borne. 5. Stele is protostelic or siphonostelic with sclerenchymatous pith. 6. Secondary growth is absent. 7. Bi- or trilocular sporangia are borne in the axils of leaf-like appendages. 8. Mode of sporangial development is of eusporangiate type. 9. Spores are of equal sizes and shapes i.e., homosporous. 10. The gametophytes are non-green, cylindrical, branched and subterranean. They grow as saprophytes with an associated endophytic fungus. 11.Antherozoids are spirally coiled and multi- flagellated. 2. Class. Lycopsida: This class has a long evolutionary history and is represented both by extant and extinct genera. This group first originated during the Lower Devonian period of Palaeozoic Era (ca 390 my). This class is represented by five living genera — Lycopodium, Selaginella, Phylloglossum, Styhtes, and Isoetes, and fourteen extinct genera — Asteroxylon, Baragwanathia, Protolepido- dendron, Lepidodendron, Sigillaria etc. Salient Features of the Class Lycopsida: (a) The sporophyte plant body is differentiated into definite root, stem and leaves. -
The Classification of Early Land Plants-Revisited*
The classification of early land plants-revisited* Harlan P. Banks Banks HP 1992. The c1assificalion of early land plams-revisiled. Palaeohotanist 41 36·50 Three suprageneric calegories applied 10 early land plams-Rhyniophylina, Zoslerophyllophytina, Trimerophytina-proposed by Banks in 1968 are reviewed and found 10 have slill some usefulness. Addilions 10 each are noted, some delelions are made, and some early planls lhal display fealures of more lhan one calegory are Sel aside as Aberram Genera. Key-words-Early land-plams, Rhyniophytina, Zoslerophyllophytina, Trimerophytina, Evolulion. of Plant Biology, Cornell University, Ithaca, New York-5908, U.S.A. 14853. Harlan P Banks, Section ~ ~ ~ <ltm ~ ~-~unR ~ qro ~ ~ ~ f~ 4~1~"llc"'111 ~-'J~f.f3il,!"~, 'i\'1f~()~~<1I'f'I~tl'1l ~ ~1~il~lqo;l~tl'1l, 1968 if ~ -mr lfim;j; <fr'f ~<nftm~~Fmr~%1 ~~ifmm~~-.mtl ~if-.t~m~fuit ciit'!'f.<nftmciit~%1 ~ ~ ~ -.m t ,P1T ~ ~~ lfiu ~ ~ -.t 3!ftrq; ~ ;j; <mol ~ <Rir t ;j; w -.m tl FIRST, may I express my gratitude to the Sahni, to survey briefly the fate of that Palaeobotanical Sociery for the honour it has done reclassification. Several caveats are necessary. I recall me in awarding its International Medal for 1988-89. discussing an intractable problem with the late great May I offer the Sociery sincere thanks for their James M. Schopf. His advice could help many consideration. aspiring young workers-"Survey what you have and Secondly, may I join in celebrating the work and write up that which you understand. The rest will the influence of Professor Birbal Sahni. The one time gradually fall into line." That is precisely what I did I met him was at a meeting where he was displaying in 1968. -
Download This Article As
Int.J.Curr.Res.Aca.Rev.2017; 5(6): 86-92 International Journal of Current Research and Academic Review ISSN: 2347-3215 (Online) ҉҉ Volume 5 ҉҉ Number 6 (June-2017) Journal homepage: http://www.ijcrar.com doi: https://doi.org/10.20546/ijcrar.2017.506.012 Fossil Pteridophytes-A Review Teena Agrawal* and Priyanka Danai Banasthali University, Niwai, India *Corresponding author Abstract Article Info Evolution of the plants is the very important aspects of the life on the planet. Since Accepted: 05 June 2017 early plant life was typically aquatic in nature. It was the assemblage of many kinds of Available Online: 20 June 2017 the aquatic algae and the other taxa of the aquatic importance. Among them the bryophytes are the plants which were amphibious in nature. However the pteridophytes Keywords are typically land plants having well developed vascular bundles as well as other features of the and adaptations. Pteridophytes have the long fossils history and plants Fossils pteridophytes, were well developed in the whole Palaeozoic era. They were flourished well in the late Evolution, Devonian and the carboniferous period. In that era one can find a number of the Adaptations, examples of the fossils plants which were intimidate in evolution of the many kinds of Land plants. the organs. Lepidocarpales was the assemblage of the organs like structure which have the pioneer symptoms of the evolution of the ovules. This review presents the assemblage of the fossil pteridophytes. Introduction beautiful tree ferns can be seen with good physiognomy, similarly epiphytic ferns and the other hanging club The pteridophytes formed the dominant part of the mosses can be seen in the Nilgiri hills. -
Jurassic Flora of Cape 1,Isburne Alaska
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR THE JURASSIC FLORA OF CAPE 1,ISBURNE ALASKA F. H. KNOWLTON Publishecl January 28, 1914 PART D OF PROFESSIONAL PAPER 85, "CONTRIBUTIONS TO GENERAL GEOLOGY 1913" WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page . Introduction ............................................................................................ 39 The Corwin formation ..................................................................................... 39 Plant collections ......................................................................................... 40 Age of the plant-bearing beds ............................................................................. 41 Distribution of Jurassic floras ............................................................................. 43 Geographicrange .................................................................................... 43 Means of dispersal ................................................................................... 45 Avenues of dispersal ................................................................................. 45 Probable climatic conditions .......................................................................... 46 .The flora ................................................................................................ 46 ILLUSTRATIONS. Page . PLATESV-VIII . Jurassic flora of Cape Lisburne, Alaska .................................................... 57-64 THE' JUR,ASSIC FLORA OF CAPE