Review the Ethnobotany of Ferns and Lycophytes H. A
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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. -
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. -
List of Plants for Great Sand Dunes National Park and Preserve
Great Sand Dunes National Park and Preserve Plant Checklist DRAFT as of 29 November 2005 FERNS AND FERN ALLIES Equisetaceae (Horsetail Family) Vascular Plant Equisetales Equisetaceae Equisetum arvense Present in Park Rare Native Field horsetail Vascular Plant Equisetales Equisetaceae Equisetum laevigatum Present in Park Unknown Native Scouring-rush Polypodiaceae (Fern Family) Vascular Plant Polypodiales Dryopteridaceae Cystopteris fragilis Present in Park Uncommon Native Brittle bladderfern Vascular Plant Polypodiales Dryopteridaceae Woodsia oregana Present in Park Uncommon Native Oregon woodsia Pteridaceae (Maidenhair Fern Family) Vascular Plant Polypodiales Pteridaceae Argyrochosma fendleri Present in Park Unknown Native Zigzag fern Vascular Plant Polypodiales Pteridaceae Cheilanthes feei Present in Park Uncommon Native Slender lip fern Vascular Plant Polypodiales Pteridaceae Cryptogramma acrostichoides Present in Park Unknown Native American rockbrake Selaginellaceae (Spikemoss Family) Vascular Plant Selaginellales Selaginellaceae Selaginella densa Present in Park Rare Native Lesser spikemoss Vascular Plant Selaginellales Selaginellaceae Selaginella weatherbiana Present in Park Unknown Native Weatherby's clubmoss CONIFERS Cupressaceae (Cypress family) Vascular Plant Pinales Cupressaceae Juniperus scopulorum Present in Park Unknown Native Rocky Mountain juniper Pinaceae (Pine Family) Vascular Plant Pinales Pinaceae Abies concolor var. concolor Present in Park Rare Native White fir Vascular Plant Pinales Pinaceae Abies lasiocarpa Present -
Literature Cited
Literature Cited Robert W. Kiger, Editor This is a consolidated list of all works cited in volume 9, whether as selected references, in text, or in nomenclatural contexts. In citations of articles, both here and in the taxonomic treatments, and also in nomenclatural citations, the titles of serials are rendered in the forms recommended in G. D. R. Bridson and E. R. Smith (1991), Bridson (2004), and Bridson and D. W. Brown (http://fmhibd.library.cmu.edu/fmi/iwp/cgi?-db=BPH_Online&-loadframes). When those forms are abbreviated, as most are, cross references to the corresponding full serial titles are interpolated here alphabetically by abbreviated form. In nomenclatural citations (only), book titles are rendered in the abbreviated forms recommended in F. A. Stafleu and R. S. Cowan (1976–1988) and Stafleu et al. (1992–2009). Here, those abbreviated forms are indicated parenthetically following the full citations of the corresponding works, and cross references to the full citations are interpolated in the list alphabetically by abbreviated form. Two or more works published in the same year by the same author or group of coauthors will be distinguished uniquely and consistently throughout all volumes of Flora of North America by lower-case letters (b, c, d, ...) suffixed to the date for the second and subsequent works in the set. The suffixes are assigned in order of editorial encounter and do not reflect chronological sequence of publication. The first work by any particular author or group from any given year carries the implicit date suffix “a”; thus, the sequence of explicit suffixes begins with “b”. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Palaeogeography, Palaeoclimatology, Palaeoecology 299 (2011) 110–128 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Ecology and evolution of Devonian trees in New York, USA Gregory J. Retallack a,⁎, Chengmin Huang b a Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA b Department of Environmental Science and Engineering, University of Sichuan, Chengdu, Sichuan 610065, China article info abstract Article history: The first trees in New York were Middle Devonian (earliest Givetian) cladoxyls (?Duisbergia and Wattieza), Received 16 January 2010 with shallow-rooted manoxylic trunks. Cladoxyl trees in New York thus postdate their latest Emsian evolution Received in revised form 17 September 2010 in Spitzbergen. Progymnosperm trees (?Svalbardia and Callixylon–Archaeopteris) appeared in New York later Accepted 29 October 2010 (mid-Givetian) than progymnosperm trees from Spitzbergen (early Givetian). Associated paleosols are Available online 5 November 2010 evidence that Wattieza formed intertidal to estuarine mangal and Callixylon formed dry riparian woodland. -
Devonian As a Time of Major Innovation in Plants and Their Communities
1 Back to the Beginnings: The Silurian- 2 Devonian as a Time of Major Innovation 15 3 in Plants and Their Communities 4 Patricia G. Gensel, Ian Glasspool, Robert A. Gastaldo, 5 Milan Libertin, and Jiří Kvaček 6 Abstract Silurian, with the Early Silurian Cooksonia barrandei 31 7 Massive changes in terrestrial paleoecology occurred dur- from central Europe representing the earliest vascular 32 8 ing the Devonian. This period saw the evolution of both plant known, to date. This plant had minute bifurcating 33 9 seed plants (e.g., Elkinsia and Moresnetia), fully lami- aerial axes terminating in expanded sporangia. Dispersed 34 10 nate∗ leaves and wood. Wood evolved independently in microfossils (spores and phytodebris) in continental and 35AU2 11 different plant groups during the Middle Devonian (arbo- coastal marine sediments provide the earliest evidence for 36 12 rescent lycopsids, cladoxylopsids, and progymnosperms) land plants, which are first reported from the Early 37 13 resulting in the evolution of the tree habit at this time Ordovician. 38 14 (Givetian, Gilboa forest, USA) and of various growth and 15 architectural configurations. By the end of the Devonian, 16 30-m-tall trees were distributed worldwide. Prior to the 17 appearance of a tree canopy habit, other early plant groups 15.1 Introduction 39 18 (trimerophytes) that colonized the planet’s landscapes 19 were of smaller stature attaining heights of a few meters Patricia G. Gensel and Milan Libertin 40 20 with a dense, three-dimensional array of thin lateral 21 branches functioning as “leaves”. Laminate leaves, as we We are now approaching the end of our journey to vegetated 41 AU3 22 now know them today, appeared, independently, at differ- landscapes that certainly are unfamiliar even to paleontolo- 42 23 ent times in the Devonian. -
Rutgers Home Gardeners School 2015: Workshop 32 Plant Evolution
Plant Dating Game Through Time Bruce Crawford March 21, 2015 Director, Rutgers Gardens www.rutgersgardens.rutgers.edu Oldest living organism – Bacteria, at least 3.2 Billion years old! Fungi probably colonized the land during the Cambrian (542–488.3 MYA), long before land plants Ferns Initially developed around 350 Million Years Ago (MYA), although the ferns that we know date back 250 million years or sooner. Problem: Lack flowers and seeds, but produce spores and a temporary plant form called a prothallus that produces eggs and sperm. Bar of choice: Water Bar Attraction: Malic Acid Gymnosperms Initially developed around 300 MYA and are represented today by the Pines, Cycads and the Ginkgo. Gymnosperm literally means naked (Gumnós) seed (Spérma). Problem: Lack attractive flowers, but they do produce individual male pollen baring cones and female or ovule bearing cone. Bar of choice: Windy Bar Attraction: Pure luck! Angiosperms There is a great deal of confusion as to when they initially developed but, it is between 160 and 140 MYA. The world was starting to cool down and the Ferns and Gymnosperms were having trouble with the change in ‘Management’. Angiosperm means seed (Spérma) contained within a vessel (Angeîon) Problem: Relatively few to start, it was a lonely bar with lots of ‘Lonely Eyes” – that changed! Bar of choice: Bug Bar Attraction: Make-up! Color, nectaries, high protein pollen, high water vapor, fragrance Grasses Developed about 65 Million Years Ago during periods of reduced rainfall. Problem: Flowers are a bit less colorful attractive Bar of choice: Windy Bar Attraction: Once again, back to pure luck! Devonian 419-358 MYA (Average O2 levels at 15% vs today’s 21%) First fossilized evidence of Lichens (a symbiotic relationship between fungus and photosynthetic algae) and Liverworts The early part of this period was characterized by plants that did not have roots or leaves like the plants most common today and many had no vascular tissue at all. -
Eastern Mountain Avens (Geum Peckii) Is an Herbaceous Perennial in the Rose Family
COSEWIC Assessment and Status Report on the Eastern Mountain Avens Geum peckii in Canada ENDANGERED 2010 COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC. 2010. COSEWIC assessment and status report on the Eastern Mountain Avens Geum peckii in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. x + 33 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous report(s): COSEWIC 2000. COSEWIC assessment and update status report on the Eastern Mountain Avens Geum peckii in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 11 pp. Newell, R.E. 1999. Update COSEWIC status report on the Eastern Mountain Avens Geum peckii in Canada, in COSEWIC assessment and update status report on the Eastern Mountain Avens Geum peckii in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-11 pp. Keddy, C. 1986. COSEWIC status report on the Eastern Mountain Avens Geum peckii in Canada. Committee on the Status of Endangered Wildlife in Canada. 19 pp. Production note: COSEWIC would like to acknowledge Sean Blaney for writing the status report on the Eastern Mountain Avens Geum peckii in Canada, prepared under contract with Environment Canada, overseen and edited by Erich Haber, Co-chair, COSEWIC Vascular Plants Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: 819-953-3215 Fax: 819-994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur le benoîte de Peck (Geum peckii) au Canada. -
Annual Review of Pteridological Research - 2000
Annual Review of Pteridological Research - 2000 Annual Review of Pteridological Research - 2000 Literature Citations All Citations 1. Adhya, T. K., K. Bharati, S. R. Mohanty, B. Ramakrishnan, V. R. Rao, N. Sethunathan & R. Wassmann. 2000. Methane emission from rice fields at Cuttack, India. Nutrient Cycling in Agroecosystems 58: 95-105. [Azolla] 2. Ahlenslager, K. E. 2000. Conservation of rare plants on public lands. American Journal of Botany 87 Suppl. 6: 89. [Abstract] 3. Alam, M. S., N. Chopra, M. Ali & M. Niwa. 2000. Normethyl pentacyclic and lanostane-type triterpenes from Adiantum venustum. Phytochemistry (Oxford) 54: 215-220. 4. Allam, A. F. 2000. Evaluation of different means of control of snail intermediate host of Schistosoma mansoni. Journal of the Egyptian Society of Parasitology 30: 441-450. [Azolla pinnata] 5. Allison, A. & F. Kraus. 2000. A new species of frog of the genus Xenorhina (Anura: Microhylidae) from the north coast ranges of Papua New Guinea. Herpetologica 56: 285-294. [Asplenium] 6. Alonso-Amelot, M. E., M. P. Calcagno & M. Perez-Injosa. 2000. Growth and selective defensive potential in relation to altitude in neotropical Pteridium aquilinum var. caudatum. Pp. 43-47. In J. A. Taylor & R. T. Smith (Eds.). Bracken fern: toxicity, biology and control. International Bracken Group, Aberystwyth. 7. Alonso-Amelot, M. E., U. F. Castillo, M. Avendano, B. L. Smith & D. R. Lauren. 2000. Milk as a vehicle for the transfer of ptaquiloside, a bracken carcinogen. Pp. 86-90. In J. A. Taylor & R. T. Smith (Eds.). Bracken fern: toxicity, biology and control. International Bracken Group, Aberystwyth. [Pteridium aquilinum] 8. Alonso-Amelot, M. -
The Anatomy of Arborescent Plant Life Through Time Mike Viney
The Anatomy of Arborescent Plant Life through Time Mike Viney Tree Fern Guairea carnieri Paraguay, South America Permian Introduction Collectors of petrified wood focus on permineralized plant material related to arborescent (tree-like) plant life. Fascination with fossil wood may be related to human reverence for living trees. Trees provide humans and other organisms with shelter and food. We plant trees near our homes and in our communities to enrich the environment. From crib to grave they cradle our bodies. Trees define many biomes. Trees help moderate Earth’s atmosphere sequestering carbon and releasing oxygen. Trees are one of the first plant categories a child learns. Asking a person to identify a plant as a tree may seem like “child’s play”; however, defining a tree can be difficult. The United States Forest Service defines a tree as a woody plant at least 13 feet (4 m) tall with a single trunk at least 3 inches (7.62 cm) in diameter at breast height (4.5 ft; 150 cm) (Petrides, 1993, p. 4). This definition fits well with many people’s concept of a tree being a large, columnar, woody, long-lived organism. However, many trees are not constructed from secondary growth (wood), such as palms and tree ferns. Some species, such as black willow, are multi-trunked. Size can also be problematic as an Engelmann spruce growing at tree line may be small compared to one growing at a lower elevation. Some species, such as the juniper, can grow as shrubs or trees. The Japanese art of bonsai demonstrates how environment can effect tree growth to extremes. -
Illustration Sources
APPENDIX ONE ILLUSTRATION SOURCES REF. CODE ABR Abrams, L. 1923–1960. Illustrated flora of the Pacific states. Stanford University Press, Stanford, CA. ADD Addisonia. 1916–1964. New York Botanical Garden, New York. Reprinted with permission from Addisonia, vol. 18, plate 579, Copyright © 1933, The New York Botanical Garden. ANDAnderson, E. and Woodson, R.E. 1935. The species of Tradescantia indigenous to the United States. Arnold Arboretum of Harvard University, Cambridge, MA. Reprinted with permission of the Arnold Arboretum of Harvard University. ANN Hollingworth A. 2005. Original illustrations. Published herein by the Botanical Research Institute of Texas, Fort Worth. Artist: Anne Hollingworth. ANO Anonymous. 1821. Medical botany. E. Cox and Sons, London. ARM Annual Rep. Missouri Bot. Gard. 1889–1912. Missouri Botanical Garden, St. Louis. BA1 Bailey, L.H. 1914–1917. The standard cyclopedia of horticulture. The Macmillan Company, New York. BA2 Bailey, L.H. and Bailey, E.Z. 1976. Hortus third: A concise dictionary of plants cultivated in the United States and Canada. Revised and expanded by the staff of the Liberty Hyde Bailey Hortorium. Cornell University. Macmillan Publishing Company, New York. Reprinted with permission from William Crepet and the L.H. Bailey Hortorium. Cornell University. BA3 Bailey, L.H. 1900–1902. Cyclopedia of American horticulture. Macmillan Publishing Company, New York. BB2 Britton, N.L. and Brown, A. 1913. An illustrated flora of the northern United States, Canada and the British posses- sions. Charles Scribner’s Sons, New York. BEA Beal, E.O. and Thieret, J.W. 1986. Aquatic and wetland plants of Kentucky. Kentucky Nature Preserves Commission, Frankfort. Reprinted with permission of Kentucky State Nature Preserves Commission. -
Journal of the Oklahoma Native Plant Society, Volume 9, December 2009
4 Oklahoma Native Plant Record Volume 9, December 2009 VASCULAR PLANTS OF SOUTHEASTERN OKLAHOMA FROM THE SANS BOIS TO THE KIAMICHI MOUNTAINS Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of Doctor of Philosophy May 1969 Francis Hobart Means, Jr. Midwest City, Oklahoma Current Email Address: [email protected] The author grew up in the prairie region of Kay County where he learned to appreciate proper management of the soil and the native grass flora. After graduation from college, he moved to Eastern Oklahoma State College where he took a position as Instructor in Botany and Agronomy. In the course of conducting botany field trips and working with local residents on their plant problems, the author became increasingly interested in the flora of that area and of the State of Oklahoma. This led to an extensive study of the northern portion of the Oauchita Highlands with collections currently numbering approximately 4,200. The specimens have been processed according to standard herbarium procedures. The first set has been placed in the Herbarium of Oklahoma State University with the second set going to Eastern Oklahoma State College at Wilburton. Editor’s note: The original species list included habitat characteristics and collection notes. These are omitted here but are available in the dissertation housed at the Edmon-Low Library at OSU or in digital form by request to the editor. [SS] PHYSICAL FEATURES Winding Stair Mountain ranges. A second large valley lies across the southern part of Location and Area Latimer and LeFlore counties between the The area studied is located primarily in Winding Stair and Kiamichi mountain the Ouachita Highlands of eastern ranges.