Problems in Cladistic Classification: Higher-Level Relationships in Land Plants Peter R
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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. -
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. -
Diversity Patterns of the Vascular Plant Group Zosterophyllopsida in Relation to Devonian Paleogeography Borja Cascales-Miñana, Brigitte Meyer-Berthaud
Diversity patterns of the vascular plant group Zosterophyllopsida in relation to Devonian paleogeography Borja Cascales-Miñana, Brigitte Meyer-Berthaud To cite this version: Borja Cascales-Miñana, Brigitte Meyer-Berthaud. Diversity patterns of the vascular plant group Zosterophyllopsida in relation to Devonian paleogeography. Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2015, 423, pp.53-61. 10.1016/j.palaeo.2015.01.024. hal-01140840 HAL Id: hal-01140840 https://hal-sde.archives-ouvertes.fr/hal-01140840 Submitted on 26 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Palaeogeography, Palaeoclimatology, Palaeoecology 423 (2015) 53–61 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Diversity patterns of the vascular plant group Zosterophyllopsida in relation to Devonian paleogeography Borja Cascales-Miñana a,b,⁎, Brigitte Meyer-Berthaud a a CNRS, Université de Montpellier, UMR Botanique et bioinformatique de l'architecture des plantes et des végétations (AMAP), F-34398 Montpellier Cedex 5, France b PPP, Département de Géologie, Université de Liège, Allée du 6 Août, B18 Sart Tilman, B-4000 Liège, Belgium article info abstract Article history: The Zosterophyllopsida originated in the Silurian and became prominent vascular components of Early Devonian Received 11 April 2014 floras worldwide. -
Fossils and Plant Phylogeny1
American Journal of Botany 91(10): 1683±1699. 2004. FOSSILS AND PLANT PHYLOGENY1 PETER R. CRANE,2,5 PATRICK HERENDEEN,3 AND ELSE MARIE FRIIS4 2Royal Botanic Gardens, Kew, Richmond, Surrey TW9 3AB, UK; 3Department of Biological Sciences, The George Washington University, Washington DC 20052 USA; 4Department of Palaeobotany, Swedish Museum of Natural History, Box 50007, S-104 05 Stockholm, Sweden Developing a detailed estimate of plant phylogeny is the key ®rst step toward a more sophisticated and particularized understanding of plant evolution. At many levels in the hierarchy of plant life, it will be impossible to develop an adequate understanding of plant phylogeny without taking into account the additional diversity provided by fossil plants. This is especially the case for relatively deep divergences among extant lineages that have a long evolutionary history and in which much of the relevant diversity has been lost by extinction. In such circumstances, attempts to integrate data and interpretations from extant and fossil plants stand the best chance of success. For this to be possible, what will be required is meticulous and thorough descriptions of fossil material, thoughtful and rigorous analysis of characters, and careful comparison of extant and fossil taxa, as a basis for determining their systematic relationships. Key words: angiosperms; fossils; paleobotany; phylogeny; spermatophytes; tracheophytes. Most biological processes, such as reproduction or growth distic context, neither fossils nor their stratigraphic position and development, can only be studied directly or manipulated have any special role in inferring phylogeny, and although experimentally using living organisms. Nevertheless, much of more complex models have been developed (see Fisher, 1994; what we have inferred about the large-scale processes of plant Huelsenbeck, 1994), these have not been widely adopted. -
A Revision of Schoenobryum (Cryphaeaceae, Bryopsida) in Africa1
Revision of Schoenobryum 147 Tropical Bryology 24: 147-159, 2003 A revision of Schoenobryum (Cryphaeaceae, Bryopsida) in Africa1 Brian J. O’Shea 141 Fawnbrake Avenue, London SE24 0BG, U.K. Abstract. The nine species and two varieties of Schoenobryum reported for Africa were investigated, and no characters were found that uniquely identified any of the taxa to be other than the pantropical Schoenobryum concavifolium. The following nine names become new synonyms of S. concavifolium: Cryphaea madagassa, C. subintegra, Acrocryphaea robusta, A. latifolia, A. subrobusta, A. tisserantii, A. latifolia var. microspora, A. plicatula and A. subintegra var. idanreense; a lectotype is selected for Acrocryphaea latifolia var. microspora P.de la Varde. INTRODUCTION as the majority have not been examined since the type description, and many have never been A recent checklist of Sub-Saharan Africa illustrated. (O’Shea, 1999) included nine species and two varieties of Schoenobryum, most of quite limited The purpose of this paper is to provide an distribution. Recent collecting in both Malawi overview of the genus worldwide, and to review (O’Shea et al., 2001) and Uganda (Wigginton et the taxonomic position of the African taxa. al., 2001) has shown the genus to be not uncommon, although there was only one CRYPHAEACEAE SCHIMP. 1856. previously published collection from the two countries (O’Shea, 1993). Apart from one Cryphaeaceae Schimp., Coroll. Bryol. Eur. 97. African taxon occurring in nine countries, the 1856 [‘1855’]. Type: Cryphaea D.Mohr in other 10 occurred in an average of 1.7 countries. F.Weber This particular profile is typical of unrevised genera in Africa, and indicative of a possible A brief review of the circumscription and need for revision (O’Shea, 1997), particularly systematics of the family, and the distinctions from related families (e.g. -
Anthocerotophyta
Glime, J. M. 2017. Anthocerotophyta. Chapt. 2-8. In: Glime, J. M. Bryophyte Ecology. Volume 1. Physiological Ecology. Ebook 2-8-1 sponsored by Michigan Technological University and the International Association of Bryologists. Last updated 5 June 2020 and available at <http://digitalcommons.mtu.edu/bryophyte-ecology/>. CHAPTER 2-8 ANTHOCEROTOPHYTA TABLE OF CONTENTS Anthocerotophyta ......................................................................................................................................... 2-8-2 Summary .................................................................................................................................................... 2-8-10 Acknowledgments ...................................................................................................................................... 2-8-10 Literature Cited .......................................................................................................................................... 2-8-10 2-8-2 Chapter 2-8: Anthocerotophyta CHAPTER 2-8 ANTHOCEROTOPHYTA Figure 1. Notothylas orbicularis thallus with involucres. Photo by Michael Lüth, with permission. Anthocerotophyta These plants, once placed among the bryophytes in the families. The second class is Leiosporocerotopsida, a Anthocerotae, now generally placed in the phylum class with one order, one family, and one genus. The genus Anthocerotophyta (hornworts, Figure 1), seem more Leiosporoceros differs from members of the class distantly related, and genetic evidence may even present -
Heterospory: the Most Iterative Key Innovation in the Evolutionary History of the Plant Kingdom
Biol. Rej\ (1994). 69, l>p. 345-417 345 Printeii in GrenI Britain HETEROSPORY: THE MOST ITERATIVE KEY INNOVATION IN THE EVOLUTIONARY HISTORY OF THE PLANT KINGDOM BY RICHARD M. BATEMAN' AND WILLIAM A. DiMlCHELE' ' Departments of Earth and Plant Sciences, Oxford University, Parks Road, Oxford OXi 3P/?, U.K. {Present addresses: Royal Botanic Garden Edinburiih, Inverleith Rojv, Edinburgh, EIIT, SLR ; Department of Geology, Royal Museum of Scotland, Chambers Street, Edinburgh EHi ijfF) '" Department of Paleohiology, National Museum of Natural History, Smithsonian Institution, Washington, DC^zo^bo, U.S.A. CONTENTS I. Introduction: the nature of hf^terospon' ......... 345 U. Generalized life history of a homosporous polysporangiophyle: the basis for evolutionary excursions into hetcrospory ............ 348 III, Detection of hcterospory in fossils. .......... 352 (1) The need to extrapolate from sporophyte to gametophyte ..... 352 (2) Spatial criteria and the physiological control of heterospory ..... 351; IV. Iterative evolution of heterospory ........... ^dj V. Inter-cladc comparison of levels of heterospory 374 (1) Zosterophyllopsida 374 (2) Lycopsida 374 (3) Sphenopsida . 377 (4) PtiTopsida 378 (5) f^rogymnospermopsida ............ 380 (6) Gymnospermopsida (including Angiospermales) . 384 (7) Summary: patterns of character acquisition ....... 386 VI. Physiological control of hetcrosporic phenomena ........ 390 VII. How the sporophyte progressively gained control over the gametophyte: a 'just-so' story 391 (1) Introduction: evolutionary antagonism between sporophyte and gametophyte 391 (2) Homosporous systems ............ 394 (3) Heterosporous systems ............ 39(1 (4) Total sporophytic control: seed habit 401 VIII. Summary .... ... 404 IX. .•Acknowledgements 407 X. References 407 I. I.NIRODUCTION: THE NATURE OF HETEROSPORY 'Heterospory' sensu lato has long been one of the most popular re\ie\v topics in organismal botany. -
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. -
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 EVOLUTION of XYLEM ANATOMY in EARLY TRACHEOPHYTES by ELISABETH ANNE BERGMAN
Conquering the terrestrial environment: the evolution of xylem anatomy in early tracheophytes Item Type text; Electronic Thesis Authors Bergman, Elisabeth Anne Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 27/09/2021 03:01:29 Item License http://rightsstatements.org/vocab/InC/1.0/ Link to Item http://hdl.handle.net/10150/626731 CONQUERING THE TERRESTRIAL ENVIRONMENT: THE EVOLUTION OF XYLEM ANATOMY IN EARLY TRACHEOPHYTES By ELISABETH ANNE BERGMAN ____________________ A Thesis Submitted to The Honors College In Partial Fulfillment of the Bachelors Degree With Honors in Biology with an Emphasis in Biomedical Sciences THE UNIVERSITY OF ARIZONA D E C E M B E R 2 0 1 7 Approved by: ____________________________ Dr. Brian Enquist Department of Ecology and Evolutionary Biology Acknowledgements Many thanks go to all of those who made contributions, big and small, to my honors thesis, and more notably, my education. Foremost, I thank Dr. Brian Enquist for accepting me into his lab and serving as my mentor for two years. I appreciate all of the time he put in to meet with me and help me to develop my honors thesis. Additional thanks go to Dr. Sean Michaletz who first introduced me to the work that would eventually become my honors thesis. From the University of Santa Cruz, California, I thank Dr. -
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. -
Giant Cladoxylopsid Trees Resolve Enigma of the Earth's Earliest Forest Stumps at Gilboa
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/6385893 Giant cladoxylopsid trees resolve enigma of the Earth's earliest forest stumps at Gilboa Article in Nature · May 2007 DOI: 10.1038/nature05705 · Source: PubMed CITATIONS READS 91 254 5 authors, including: Frank Mannolini Linda VanAller Hernick New York State Museum New York State Museum 8 PUBLICATIONS 160 CITATIONS 9 PUBLICATIONS 253 CITATIONS SEE PROFILE SEE PROFILE Ed Landing Christopher Berry New York State Museum Cardiff University 244 PUBLICATIONS 3,365 CITATIONS 48 PUBLICATIONS 862 CITATIONS SEE PROFILE SEE PROFILE All content following this page was uploaded by Ed Landing on 06 February 2017. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Vol 446 | 19 April 2007 | doi:10.1038/nature05705 LETTERS Giant cladoxylopsid trees resolve the enigma of the Earth’s earliest forest stumps at Gilboa William E. Stein1, Frank Mannolini2, Linda VanAller Hernick2, Ed Landing2 & Christopher M. Berry3 The evolution of trees of modern size growing together in forests Middle Devonian (Eifelian) into the Carboniferous, were major fundamentally changed terrestrial ecosystems1–3. The oldest trees contributors to floras worldwide14. Traditionally considered inter- are often thought to be of latest Devonian age (about 380–360 Myr mediate between Lower Devonian vascular plants and ferns or old) as indicated by the widespread occurrence of Archaeopteris sphenopsids, we do not yet understand these plants well enough to (Progymnospermopsida)4.