Structural Fingerprints of Development at the Intersection of Evo-Devo and the Fossil Record
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Plant Life MagillS Encyclopedia of Science
MAGILLS ENCYCLOPEDIA OF SCIENCE PLANT LIFE MAGILLS ENCYCLOPEDIA OF SCIENCE PLANT LIFE Volume 4 Sustainable Forestry–Zygomycetes Indexes Editor Bryan D. Ness, Ph.D. Pacific Union College, Department of Biology Project Editor Christina J. Moose Salem Press, Inc. Pasadena, California Hackensack, New Jersey Editor in Chief: Dawn P. Dawson Managing Editor: Christina J. Moose Photograph Editor: Philip Bader Manuscript Editor: Elizabeth Ferry Slocum Production Editor: Joyce I. Buchea Assistant Editor: Andrea E. Miller Page Design and Graphics: James Hutson Research Supervisor: Jeffry Jensen Layout: William Zimmerman Acquisitions Editor: Mark Rehn Illustrator: Kimberly L. Dawson Kurnizki Copyright © 2003, by Salem Press, Inc. All rights in this book are reserved. No part of this work may be used or reproduced in any manner what- soever or transmitted in any form or by any means, electronic or mechanical, including photocopy,recording, or any information storage and retrieval system, without written permission from the copyright owner except in the case of brief quotations embodied in critical articles and reviews. For information address the publisher, Salem Press, Inc., P.O. Box 50062, Pasadena, California 91115. Some of the updated and revised essays in this work originally appeared in Magill’s Survey of Science: Life Science (1991), Magill’s Survey of Science: Life Science, Supplement (1998), Natural Resources (1998), Encyclopedia of Genetics (1999), Encyclopedia of Environmental Issues (2000), World Geography (2001), and Earth Science (2001). ∞ The paper used in these volumes conforms to the American National Standard for Permanence of Paper for Printed Library Materials, Z39.48-1992 (R1997). Library of Congress Cataloging-in-Publication Data Magill’s encyclopedia of science : plant life / edited by Bryan D. -
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. -
Chapter 23: the Early Tracheophytes
Chapter 23 The Early Tracheophytes THE LYCOPHYTES Lycopodium Has a Homosporous Life Cycle Selaginella Has a Heterosporous Life Cycle Heterospory Allows for Greater Parental Investment Isoetes May Be the Only Living Member of the Lepidodendrid Group THE MONILOPHYTES Whisk Ferns Ophioglossalean Ferns Horsetails Marattialean Ferns True Ferns True Fern Sporophytes Typically Have Underground Stems Sexual Reproduction Usually Is Homosporous Fern Have a Variety of Alternative Means of Reproduction Ferns Have Ecological and Economic Importance SUMMARY PLANTS, PEOPLE, AND THE ENVIRONMENT: Sporophyte Prominence and Survival on Land PLANTS, PEOPLE, AND THE ENVIRONMENT: Coal, Smog, and Forest Decline THE OCCUPATION OF THE LAND PLANTS, PEOPLE, AND THE The First Tracheophytes Were ENVIRONMENT: Diversity Among the Ferns Rhyniophytes Tracheophytes Became Increasingly Better PLANTS, PEOPLE, AND THE Adapted to the Terrestrial Environment ENVIRONMENT: Fern Spores Relationships among Early Tracheophytes 1 KEY CONCEPTS 1. Tracheophytes, also called vascular plants, possess lignified water-conducting tissue (xylem). Approximately 14,000 species of tracheophytes reproduce by releasing spores and do not make seeds. These are sometimes called seedless vascular plants. Tracheophytes differ from bryophytes in possessing branched sporophytes that are dominant in the life cycle. These sporophytes are more tolerant of life on dry land than those of bryophytes because water movement is controlled by strongly lignified vascular tissue, stomata, and an extensive cuticle. The gametophytes, however still require a seasonally wet habitat, and water outside the plant is essential for the movement of sperm from antheridia to archegonia. 2. The rhyniophytes were the first tracheophytes. They consisted of dichotomously branching axes, lacking roots and leaves. They are all extinct. -
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. -
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. -
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. -
Acaulosporoid Glomeromycotan Spores with a Germination Shield from the 400-Million-Year-Old Rhynie Chert
KU ScholarWorks | http://kuscholarworks.ku.edu Please share your stories about how Open Access to this article benefits you. Acaulosporoid glomeromycotan spores with a germination shield from the 400-million- year-old Rhynie chert by Nora Dotzler, Christopher Walker, Michael Krings, Hagen Hass, Hans Kerp, Thomas N. Taylor, Reinhard Agerer 2009 This is the published version of the article, made available with the permission of the publisher. The original published version can be found at the link below. Dotzler, N., Walker, C., Krings, M., Hass, H., Kerp, H., Taylor, T., Agerer, R. 2009. Acaulosporoid glomeromycotan spores with a ger- mination shield from the 400-million-year-old Rhynie chert. Mycol Progress 8:9-18. Published version: http://dx.doi.org/10.1007/s11557-008-0573-1 Terms of Use: http://www2.ku.edu/~scholar/docs/license.shtml This work has been made available by the University of Kansas Libraries’ Office of Scholarly Communication and Copyright. Mycol Progress (2009) 8:9–18 DOI 10.1007/s11557-008-0573-1 ORIGINAL ARTICLE Acaulosporoid glomeromycotan spores with a germination shield from the 400-million-year-old Rhynie chert Nora Dotzler & Christopher Walker & Michael Krings & Hagen Hass & Hans Kerp & Thomas N. Taylor & Reinhard Agerer Received: 4 June 2008 /Revised: 16 September 2008 /Accepted: 30 September 2008 / Published online: 15 October 2008 # German Mycological Society and Springer-Verlag 2008 Abstract Scutellosporites devonicus from the Early Devo- single or double lobes to tongue-shaped structures usually nian Rhynie chert is the only fossil glomeromycotan spore with infolded margins that are distally fringed or palmate. taxon known to produce a germination shield. -
The Impacts of Land Plant Evolution on Earth's Climate and Oxygenation State – an Interdisciplinary Review
The impacts of land plant evolution on Earth's climate and oxygenation state – An interdisciplinary review Dahl, Tais W.; Arens, Susanne K.M. Published in: Chemical Geology DOI: 10.1016/j.chemgeo.2020.119665 Publication date: 2020 Document version Publisher's PDF, also known as Version of record Document license: CC BY-NC-ND Citation for published version (APA): Dahl, T. W., & Arens, S. K. M. (2020). The impacts of land plant evolution on Earth's climate and oxygenation state – An interdisciplinary review. Chemical Geology, 547, [119665]. https://doi.org/10.1016/j.chemgeo.2020.119665 Download date: 10. Sep. 2020 Chemical Geology 547 (2020) 119665 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Invited research article The impacts of land plant evolution on Earth's climate and oxygenation state T – An interdisciplinary review ⁎ Tais W. Dahl , Susanne K.M. Arens GLOBE Institute, University of Copenhagen, 1350 Copenhagen K, Denmark ARTICLE INFO ABSTRACT Keywords: The Paleozoic emergence of terrestrial plants has been linked to a stepwise increase in Earth's O2 levels and a Early land plants cooling of Earth's climate by drawdown of atmospheric CO2. Vegetation affects the Earth's2 O and CO2 levels in Terrestrialization multiple ways, including preferential organic carbon preservation by decay-resistant biopolymers (e.g. lignin) Climate and changing the continental weathering regime that governs oceanic nutrient supply and marine biological Oxygenation production. Over shorter time scales (≤1 Myr), land plant evolution is hypothesized to have occasionally en- Soils hanced P weathering and fertilized the oceans, expanding marine anoxia and causing marine extinctions. -
CPY Document
CHAPTER 1 Plant diversity has evolved and is evolving on the earth today according to the processes of natural selection. All basic "body plans" of vascular plants were in existence by the Early Carboniferous, approximately 340 million years ago, and each major radiation occupied a particular habitat type, for example, wetland versus terra firma, pristine versus disturbed environments. Today the great spe- cies diversity we see on theplanetis dominated by just a few of these hasicplant types. This chapter sets the stage to understanding the origin and radiation of plant diversity on the earth before the significant influence of humans. The im- plication is that plants may become more diverse in the number of species level over time, but less diverse in overall form. The history of life tells us that plants that are dominant and diverse today will certainly be inconspicuous or even ex--' tinct in the distant future. EVOLUTION OF LAND PLANT DIVERSITY MAJOR INNOVATIONS AND LINEAGES THROUGH TIME William A. DiMichele and Richard M. Bateman PLANT DIVERSITY VIEWED through the lens of deep time takes on a con- siderably different aspect than when examined in the present. Although the fossil record captures only fragments of the terrestrial world of the past 450 million years, it does indicate clearly that the world of today is simply a passing phase, the latest permutation in a string of spasmodic changes in the ecological organization of the terrestrial biosphere. The pace of change in species diversity and that of ecosystem structure and composition have followed broadly parallel paths, unquestionably related but not always changing in unison.