Early Evolution of Life Cycles in Embryophytes: a Focus on the Fossil Evidence of Gametophytesporophyte Size and Morphological C
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History Department Botany
THE HISTORY OF THE DEPARTMENT OF BOTANY 1889-1989 UNIVERSITY OF MINNESOTA SHERI L. BARTLETT I - ._-------------------- THE HISTORY OF THE DEPARTMENT OF BOTANY 1889-1989 UNIVERSITY OF MINNESOTA SHERI L. BARTLETT TABLE OF CONTENTS Preface 1-11 Chapter One: 1889-1916 1-18 Chapter Two: 1917-1935 19-38 Chapter Three: 1936-1954 39-58 Chapter Four: 1955-1973 59-75 Epilogue 76-82 Appendix 83-92 Bibliography 93-94 -------------------------------------- Preface (formerly the College of Science, Literature and the Arts), the College of Agriculture, or The history that follows is the result some other area. Eventually these questions of months ofresearch into the lives and work were resolved in 1965 when the Department of the Botany Department's faculty members joined the newly established College of and administrators. The one-hundred year Biological Sciences (CBS). In 1988, The overview focuses on the Department as a Department of Botany was renamed the whole, and the decisions that Department Department of Plant Biology, and Irwin leaders made to move the field of botany at Rubenstein from the Department of Genetics the University of Minnesota forward in a and Cell Biology became Plant Biology's dynamic and purposeful manner. However, new head. The Department now has this is not an effort to prove that the administrative ties to both the College of Department's history was linear, moving Biological Sciences and the College of forward in a pre-determined, organized Agriculture. fashion at every moment. Rather I have I have tried to recognize the attempted to demonstrate the complexities of accomplishments and individuality of the the personalities and situations that shaped Botany Department's faculty while striving to the growth ofthe Department and made it the describe the Department as one entity. -
STEM Disciplines
STEM Disciplines In order to be applicable to the many types of institutions that participate in the HERI Faculty Survey, this list is intentionally broad and comprehensive in its definition of STEM disciplines. It includes disciplines in the life sciences, physical sciences, engineering, mathematics, computer science, and the health sciences. Agriculture/Natural Resources Health Professions 0101 Agriculture and related sciences 1501 Alternative/complementary medicine/sys 0102 Natural resources and conservation 1503 Clinical/medical lab science/allied 0103 Agriculture/natural resources/related, other 1504 Dental support services/allied 1505 Dentistry Biological and Biomedical Sciences 1506 Health & medical administrative services 0501 Biochem/biophysics/molecular biology 1507 Allied health and medical assisting services 0502 Botany/plant biology 1508 Allied health diagnostic, intervention, 0503 Genetics treatment professions 0504 Microbiological sciences & immunology 1509 Medicine, including psychiatry 0505 Physiology, pathology & related sciences 1511 Nursing 0506 Zoology/animal biology 1512 Optometry 0507 Biological & biomedical sciences, other 1513 Osteopathic medicine/osteopathy 1514 Pharmacy/pharmaceutical sciences/admin Computer/Info Sciences/Support Tech 1515 Podiatric medicine/podiatry 0801 Computer/info tech administration/mgmt 1516 Public health 0802 Computer programming 1518 Veterinary medicine 0803 Computer science 1519 Health/related clinical services, other 0804 Computer software and media applications 0805 Computer systems -
Phytotaxa, a Synthesis of Hornwort Diversity
Phytotaxa 9: 150–166 (2010) ISSN 1179-3155 (print edition) www.mapress.com/phytotaxa/ Article PHYTOTAXA Copyright © 2010 • Magnolia Press ISSN 1179-3163 (online edition) A synthesis of hornwort diversity: Patterns, causes and future work JUAN CARLOS VILLARREAL1 , D. CHRISTINE CARGILL2 , ANDERS HAGBORG3 , LARS SÖDERSTRÖM4 & KAREN SUE RENZAGLIA5 1Department of Ecology and Evolutionary Biology, University of Connecticut, 75 North Eagleville Road, Storrs, CT 06269; [email protected] 2Centre for Plant Biodiversity Research, Australian National Herbarium, Australian National Botanic Gardens, GPO Box 1777, Canberra. ACT 2601, Australia; [email protected] 3Department of Botany, The Field Museum, 1400 South Lake Shore Drive, Chicago, IL 60605-2496; [email protected] 4Department of Biology, Norwegian University of Science and Technology, N-7491 Trondheim, Norway; [email protected] 5Department of Plant Biology, Southern Illinois University, Carbondale, IL 62901; [email protected] Abstract Hornworts are the least species-rich bryophyte group, with around 200–250 species worldwide. Despite their low species numbers, hornworts represent a key group for understanding the evolution of plant form because the best–sampled current phylogenies place them as sister to the tracheophytes. Despite their low taxonomic diversity, the group has not been monographed worldwide. There are few well-documented hornwort floras for temperate or tropical areas. Moreover, no species level phylogenies or population studies are available for hornworts. Here we aim at filling some important gaps in hornwort biology and biodiversity. We provide estimates of hornwort species richness worldwide, identifying centers of diversity. We also present two examples of the impact of recent work in elucidating the composition and circumscription of the genera Megaceros and Nothoceros. -
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. -
Fossil Microorganisms and Land Plants: Associations and Interactions ·
SYMBIOSIS (2005) 40, 119-135 ©2005 Balaban, Philadelphia/Rehovot ISSN 0334-5114 Review article. Fossil microorganisms and land plants: Associations and interactions · Thomas N. Taylor! * and Michael K.rings2 I Department of Ecology and Evolutionary Biology, and Natural History Museum and Biodiversity Research Center, The University of Kansas, Lawrence, KS 66045-7534, USA, Tel. +1-785-864-3625, Fax. +1-785-864-5321, Email. [email protected]; 2Bayerische Staatssammlung fur Palaontologie und Geologie und GeoBio-CenterLMU, Richard-Wagner-Strasse 10, 80333 Munich, Germany, Tel. +49-89-2180-6546, Fax. +49-89-2180-6601, Email. [email protected] (Received November 30, 2005; Accepted December 25, 2005) Abstract Microorganisms are critical in the bio- and geosphere today, and certainly performed similar functions in ancient ecosystems. Bacteria, cyanobacteria, microalgae, and various fungi and fungi-like organisms constitute a substantial component of these ancient communities, and have been responsible for the evolution and sustainability of the ecosystems in functions ranging from decomposition of metabolites to catalyzation of nutrient cycles. This review provides examples of associations and interactions between microorganisms and land plants, principally from the Devonian and Carboniferous. During this time span of approximately 150 myr, most of the vascular plant lineages evolved and radiated into new terrestrial niches. Several exceptionally well-preserved fossil communities are used to demonstrate a wide range of biological interactions. Although none of the land plant partners exist today, many of the microorganisms involved appear morphologically little changed. Moreover, some interactions suggest that the genetic code and biochemical pathways necessary for the associations and interactions to be successful evolved early in the lineages of microorganisms involved, and have seemingly remained unchanged to the present. -
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) -
Attractant, Acting As a Homing Device for the Swimming Sperm. Sperm
r 62 CHAPTER 3 EVOLUTION AND DIVERSITY OF GREEN AND LAND PLANTS UN[T 11 EVOLUTION AND DIVERSITY OF PLANTS 63 gemmae propagules 2 rows of 1 row of sperm cells dorsal leaves ventral leaves (sterile “jacket” layer) neck sperm cells “ ‘fl gemmae cup I / pore dorsal (upper) ventral (lower) A B view view thalloid liverwort leafy liverwort FIGURE 3.10 A. Antheridia. B. Archegonia. Both are apomorphies of land plants. 4 (,, ••1• attractant, acting as a homing device for the swimming sperm. of the liverworts, mosses, and hornworts is relatively small, Sperm cells enter the neck of the archegonium and fertilize ephemeral, and attached to and nutritionally dependent upon the egg cell to form a diploid (2n) zygote. In addition to the gametophyte (see later discussion). effecting fertilization, the archegonium serves as a site for The relationships of the liverworts, mosses, and hornworts embryo/sporophyte development and the establishment of a to one another and to the vascular plants remain unclear. nutritional dependence of the sporophyte upon gametophytic Many different relationships among the three lineages have archegonium tissue. been proposed, one recent of which is seen in Figure 3.6. (n) The land plants share other possible apomorphies: the presence of various ultrastructural modifications of the sperm LIVERWORTS cells, fiavonoid chemical compounds, and a proliferation of Liverworts, also traditionally called the Hepaticae, are one of archegoniophore (n) archegoniophore (n) (longitudinal-section) heat shock proteins. These are not discussed here. the monophyletic groups that are descendents of some of the (longitudinal-section) first land plants. Today, liverworts are relatively minor com ponents of the land plant flora, growing mostly in moist, fertilization DIVERSITY OF NONVASCULAR LAND PLANTS shaded areas (although some are adapted to periodically dry, hot habitats). -
The Timescale of Early Land Plant Evolution PNAS PLUS
The timescale of early land plant evolution PNAS PLUS Jennifer L. Morrisa,1, Mark N. Putticka,b,1, James W. Clarka, Dianne Edwardsc, Paul Kenrickb, Silvia Presseld, Charles H. Wellmane, Ziheng Yangf,g, Harald Schneidera,d,h,2, and Philip C. J. Donoghuea,2 aSchool of Earth Sciences, University of Bristol, Bristol BS8 1TQ, United Kingdom; bDepartment of Earth Sciences, Natural History Museum, London SW7 5BD, United Kingdom; cSchool of Earth and Ocean Sciences, Cardiff University, Cardiff CF10, United Kingdom; dDepartment of Life Sciences, Natural History Museum, London SW7 5BD, United Kingdom; eDepartment of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, United Kingdom; fDepartment of Genetics, Evolution and Environment, University College London, London WC1E 6BT, United Kingdom; gRadclie Institute for Advanced Studies, Harvard University, Cambridge, MA 02138; and hCenter of Integrative Conservation, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Yunnan 666303, China Edited by Peter R. Crane, Oak Spring Garden Foundation, Upperville, VA, and approved January 17, 2018 (received for review November 10, 2017) Establishing the timescale of early land plant evolution is essential recourse but to molecular clock methodology, employing the for testing hypotheses on the coevolution of land plants and known fossil record to calibrate and constrain molecular evolu- Earth’s System. The sparseness of early land plant megafossils and tion to time. Unfortunately, the relationships among the four stratigraphic controls on their distribution make the fossil record principal lineages of land plants, namely, hornworts, liverworts, an unreliable guide, leaving only the molecular clock. However, mosses, and tracheophytes, are unresolved, with almost every the application of molecular clock methodology is challenged by possible solution currently considered viable (14). -
JUDD W.S. Et. Al. (2002) Plant Systematics: a Phylogenetic Approach. Chapter 7. an Overview of Green
UNCORRECTED PAGE PROOFS An Overview of Green Plant Phylogeny he word plant is commonly used to refer to any auto- trophic eukaryotic organism capable of converting light energy into chemical energy via the process of photosynthe- sis. More specifically, these organisms produce carbohydrates from carbon dioxide and water in the presence of chlorophyll inside of organelles called chloroplasts. Sometimes the term plant is extended to include autotrophic prokaryotic forms, especially the (eu)bacterial lineage known as the cyanobacteria (or blue- green algae). Many traditional botany textbooks even include the fungi, which differ dramatically in being heterotrophic eukaryotic organisms that enzymatically break down living or dead organic material and then absorb the simpler products. Fungi appear to be more closely related to animals, another lineage of heterotrophs characterized by eating other organisms and digesting them inter- nally. In this chapter we first briefly discuss the origin and evolution of several separately evolved plant lineages, both to acquaint you with these important branches of the tree of life and to help put the green plant lineage in broad phylogenetic perspective. We then focus attention on the evolution of green plants, emphasizing sev- eral critical transitions. Specifically, we concentrate on the origins of land plants (embryophytes), of vascular plants (tracheophytes), of 1 UNCORRECTED PAGE PROOFS 2 CHAPTER SEVEN seed plants (spermatophytes), and of flowering plants dons.” In some cases it is possible to abandon such (angiosperms). names entirely, but in others it is tempting to retain Although knowledge of fossil plants is critical to a them, either as common names for certain forms of orga- deep understanding of each of these shifts and some key nization (e.g., the “bryophytic” life cycle), or to refer to a fossils are mentioned, much of our discussion focuses on clade (e.g., applying “gymnosperms” to a hypothesized extant groups. -
Geologic Time – Part I - Practice Questions and Answers Revised October 2007
Geologic Time – Part I - Practice Questions and Answers Revised October 2007 1. The study of the spatial and temporal relationships between bodies of rock is called ____________________. 2. The geological time scale is the ____________ framework in which geologists view Earth history. 3. Both _________________ and absolute scales are included in the geological time scale. 4. Beds represent a depositional event. They are _________ 1 cm in thickness. 5. Laminations are similar to beds but are ___________ 1 cm in thickness. 6. The idea that most beds are laid down horizontally or nearly so is called the (a) Principle of Original Continuity (b) Principle of Fossil Succession (c) Principle of Cross-Cutting Relationships (d) Principle of Original Horizontality (e) Principle of Superposition 7. The idea that beds extend laterally in three dimensions until they thin to zero thickness is called the (a) Principle of Cross-Cutting Relationships (b) Principle of Original Horizontality (c) Principle of Original Continuity (d) Principle of Fossil Succession (e) Principle of Superposition 8. The idea that younger beds are deposited on top of older beds is called the (a) Principle of Original Horizontality (b) Principle of Fossil Succession (c) Principle of Cross-Cutting Relationships (d) Principle of Original Continuity (e) Principle of Superposition 9. The idea that a dike transecting bedding must be younger than the bedding it crosses is called the (a) Principle of Original Horizontality (b) Principle of Original Continuity (c) Principle of Fossil Succession (d) Principle of Cross-Cutting Relationships (e) Principle of Superposition 10. The idea that fossil content will change upward within a formation is called the (a) Principle of Cross-Cutting Relationships (b) Principle of Original Horizontality (c) Principle of Fossil Succession (d) Principle of Original Continuity (e) Principle of Superposition 11. -
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.