The Huperzia Selago Shoot Tip Transcriptome Sheds New Light on the Evolution of Leaves
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Qrno. 1 2 3 4 5 6 7 1 CP 2903 77 100 0 Cfcl3
QRNo. General description of Type of Tariff line code(s) affected, based on Detailed Product Description WTO Justification (e.g. National legal basis and entry into Administration, modification of previously the restriction restriction HS(2012) Article XX(g) of the GATT, etc.) force (i.e. Law, regulation or notified measures, and other comments (Symbol in and Grounds for Restriction, administrative decision) Annex 2 of e.g., Other International the Decision) Commitments (e.g. Montreal Protocol, CITES, etc) 12 3 4 5 6 7 1 Prohibition to CP 2903 77 100 0 CFCl3 (CFC-11) Trichlorofluoromethane Article XX(h) GATT Board of Eurasian Economic Import/export of these ozone destroying import/export ozone CP-X Commission substances from/to the customs territory of the destroying substances 2903 77 200 0 CF2Cl2 (CFC-12) Dichlorodifluoromethane Article 46 of the EAEU Treaty DECISION on August 16, 2012 N Eurasian Economic Union is permitted only in (excluding goods in dated 29 may 2014 and paragraphs 134 the following cases: transit) (all EAEU 2903 77 300 0 C2F3Cl3 (CFC-113) 1,1,2- 4 and 37 of the Protocol on non- On legal acts in the field of non- _to be used solely as a raw material for the countries) Trichlorotrifluoroethane tariff regulation measures against tariff regulation (as last amended at 2 production of other chemicals; third countries Annex No. 7 to the June 2016) EAEU of 29 May 2014 Annex 1 to the Decision N 134 dated 16 August 2012 Unit list of goods subject to prohibitions or restrictions on import or export by countries- members of the -
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. -
Huperzine a from Huperzia Species—An Ethnopharmacolgical Review Xiaoqiang Ma A,B, Changheng Tan A, Dayuan Zhu A, David R
Huperzine A from Huperzia species—An ethnopharmacolgical review Xiaoqiang Ma a,b, Changheng Tan a, Dayuan Zhu a, David R. Gang b, Peigen Xiao c,∗ a State Key Laboratory of Drug Research, Institute of Materia Medica, Shanghai Institutes for Biological Sciences, Chinese Academy of Sciences, Shanghai 201203, PR China b Department of Plant Sciences and BIO5 Institute, The University of Arizona, 303 Forbes Building, Tucson, AZ 85721-0036, USA c Institute of Medicinal Plant Development, Peking Union Medical College and Chinese Academy of Medical Sciences, Beijing 100094, PR China Abstract Huperzine A (HupA), isolated originally from a traditional Chinese medicine Qiang Ceng Ta, whole plant of Huperzia serrata (Thunb. ex Murray) Trev., a member of the Huperziaceae family, has attracted intense attention since its marked anticholinesterase activity was discovered by Chinese scientists. Several members of the Huperziaceae (Huperzia and Phlegmariurus species) have been used as medicines in China for contusions, strains, swellings, schizophrenia, myasthenia gravis and organophosphate poisoning. HupA has been marketed in China as a new drug for Alzheimer’s disease (AD) treatment and its derivative ZT-1 is being developed as anti-AD new drug candidate both in China and in Europe. A review of the chemistry, bioactivities, toxicology, clinical trials and natural resources of HupA source plants is presented. Keywords: Huperzine A; ZT-1; Alzheimer’s disease; Huperzia serrata; Huperziaceae; Drug discovery; Bioactivities; Clinical trials; Traditional Chinese -
Bibliography of Isoetes
BIBLIOGRAPHY OF ISOETES ALLEN, B.M. 1975. A note on the distribution of Isoetes in the Cadiz Province, Spain. Fern Gaz. (U.K.) 11 (2-3): 163-164 (1975). ALONSO, PAZ, E. 1989. Notas sobre plantas nuevas o interesantes para la flora Uruguaya: 1. (Notes on new or interesting plants for the Uruguayan flora: 1.) Comun. Bot. Mus. Hist. Nat. Montevideo 5 (91): 1-4 (1989) - Isoetes pp.2-3 ALSTON, A.H.G. 1982. Isoetaceae: 1. In Steenis, C.G.G.J. van, Holttum, R. E., eds. Flora Malesiana, series 2. Pteridophytes, volume 1. The Hague, Martinus Nijhoff, Dr. W. Junk Publ. 62-64 (1982)- illus., chrom. nos., key. ANDREIS, C., RODONDI, G. 1987. Alcune stazioni di Isoetes echinospora Dur. nel Bresciano e osservazioni al SEM delle spore delle Isoetes della flora Italica. Natura Bresciana no.23: 119-130 (1986 publ. 1987) - illus., maps. 4, ANTHONY, N.C., & E.A. SCHELPE, 1985. Two new taxa and a new combination in southern African Pteridophyta. Bothalia, 15 (3 & 4): 554-555 (1985) ARREGUIN-SANCHEZ, M., 1986. Nuevos registros y taxa interesantes de pteridofitas del Valle de Mexico. (Isoetaceae, Psilotaceae y Selaginellaceae) Phytologia 59 (7): 451-453 (1986) ASH, S., & K.B. PIGG. 1991. A new Jurassic Isoetites (Isoetales) from the Wallowa Terrane in Hells Canyon Oregon and Idaho. Amer. J. Bot. 78: 1636-1642. BAJPAI, U., & H.K. MAHESHWARI,1985. EM studies on the megaspores of Isoetes coromandelina. Phytomorphology, 34 (1-4): 226-231 (1984 publ. 1985) - illus. BALDWIN, W.K.W. 1933. The organization of the young sporophyte of Isoetes engelmanni, A. -
Minnesota Biodiversity Atlas Plant List
Tettegouche State Park Plant List Herbarium Scientific Name Minnesota DNR Common Name Status Abies balsamea balsam fir Acer rubrum red maple Acer spicatum mountain maple Actaea pachypoda white baneberry Adiantum pedatum maidenhair fern Agrostis scabra rough bentgrass Allium tricoccum wild leek Alnus incana rugosa speckled alder Alnus viridis crispa green alder Alopecurus pratensis meadow foxtail Ambrosia artemisiifolia common ragweed Amelanchier bartramiana northern juneberry Amelanchier interior inland juneberry Amelanchier laevis smooth juneberry Amelanchier sanguinea sanguinea round-leaved juneberry Amelanchier spicata creeping juneberry Amelanchier wiegandii inland juneberry Arabis pycnocarpa hairy rock cress Arabis pycnocarpa pycnocarpa hairy rock cress Aralia racemosa American spikenard Arctostaphylos uva-ursi bearberry Arnica lonchophylla long-leaved arnica T Artemisia campestris caudata field sagewort Asarum canadense wild ginger Asplenium trichomanes trichomanes maidenhair spleenwort T Astragalus canadensis Canada milk-vetch Athyrium filix-femina angustum lady fern Berberis thunbergii Japanese barberry Betula cordifolia heart-leaved birch Betula papyrifera paper birch Bidens cernua nodding bur marigold Bidens frondosa leafy beggarticks Bidens tripartita tufted beggarticks Boechera grahamii spreading rock cress Botrychium matricariifolium matricary grapefern Botrychium multifidum leathery grapefern Botrychium virginianum rattlesnake fern Brachyelytrum aristosum northern shorthusk Bromus ciliatus fringed brome Calamagrostis canadensis -
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. -
Marissa Pitter, “Unearthing the Unknown: the Fossils of The
1 Unearthing the Unknown: The Fossils of the Budden Collection Marissa Pitter Fig. 1. South Gallery Room. Hinckley, Maine: L.C. Bates Museum. Photo: John Meader Photography, ©2020. In the South Gallery Room of the L.C. Bates Museum sit eight fossil display cases. In the cramped sixth case rests a significant fossil, the Pertica quadrifaria—Maine’s state fossil which comes from the rocks of the world-renowned Trout Valley Formation. Alongside the rare fossilized remains of Pertica lies “The Budden Collection,” a group of seven fossils found in northern Maine and donated to the museum in 2013. A label sits below each fossil identifying the name of the specimen (and at times, its genus and species), the geologic period and 2 formation, and the location where the fossil was found. The exact descriptions that the L.C. Bates Museum provides on the labels is given in Table 1. Table 1. The Budden Collection Fossils Fossil Geologic Period Geologic Formation Location Favositid Coral (1) Silurian Hardwood Mountain Hobbstown Township, Maine Favositid Coral (2) Silurian Hardwood Mountain Hobbstown Township, Maine Horn coral with trace Devonian Seboomook Tomhegan Township, fossils Maine Rugose Coral Ordovician/Silurian Formation Unknown Shin Pond, Maine Brachiopod Devonian Seboomook Tomhegan Township, Mucrospirifer? Maine Brachiopods likely Devonian Formation Unknown Big Moose Township, steinkerns (fossilized Maine outlines) Leptostrophia and Devonian likely Seboomook Big Moose Township, Tentaculites Maine The question mark following “Mucrospirifer,” the unknown geologic formations, and the impreciseness of the geologic age of the rugose coral indicate there are some uncertainties among the museum’s identifications. The table also points to some commonalities among the fossil collection. -
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. -
The Genus Huperzia (Lycopodiaceae) in the Azores and Madeira
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Biblioteca Digital do IPB Botanical Journal of the Linnean Society, 2008, 158, 522–533. With 15 figures The genus Huperzia (Lycopodiaceae) in the Azores and Madeira JOSÉ ANTONIO FERNÁNDEZ PRIETO1*, CARLOS AGUIAR2, EDUARDO DIAS3, MARÍA DE LOS ÁNGELES FERNÁNDEZ CASADO1 and JUAN HOMET1 1Área de Botánica, Departamento de Biología de Organismos y Sistemas, Universidad de Oviedo, 33006 Oviedo, Spain 2Área de Biologia, Escola Superior Agrária de Bragança, Campus de Santa Apolónia, Apartado 1172, 5301-855 Bragança, Portugal 3Departamento de Ciências Agrárias, Universidade dos Açores, Campus de Angra, Terra-Chã, 9701-851 Angra do Heroísmo, Açores, Portugal Received 16 February 2005; accepted for publication 15 May 2008 The taxonomy and nomenclature of the genus Huperzia Bernh. in the Azores and Madeira have been reviewed. Plants collected in the Azores and Madeira were characterized morphologically. The independence between two endemic species common to Madeira and the Azores Islands – Huperzia suberecta (Lowe) Tardieu and Huperzia dentata (Herter) Holub – is clearly shown. A clear-cut morphological separation between these taxa and Huperzia selago (L.) Bernh. ex Schrank & Mart. of continental Europe is established. © 2008 The Linnean Society of London, Botanical Journal of the Linnean Society, 2008, 158, 522–533. ADDITIONAL KEYWORDS: bulbil – Huperzia dentata – Huperzia selago – Huperzia suberecta – nomen- clature – spore – stoma – taxonomy. INTRODUCTION Most authors have accepted this systematic treat- ment of Lycopodiaceae in Europe, including the Lycopodiaceae P.Beauv. ex Mirb. sensu lato is a genera Huperzia, Lycopodium, Diphasiastrum and family with a cosmopolitan distribution, consisting of Lycopodiella (Rothmaler, 1964, 1993; Villar, 1986). -
New York Natural Heritage Program Rare Plant Status List May 2004 Edited By
New York Natural Heritage Program Rare Plant Status List May 2004 Edited by: Stephen M. Young and Troy W. Weldy This list is also published at the website: www.nynhp.org For more information, suggestions or comments about this list, please contact: Stephen M. Young, Program Botanist New York Natural Heritage Program 625 Broadway, 5th Floor Albany, NY 12233-4757 518-402-8951 Fax 518-402-8925 E-mail: [email protected] To report sightings of rare species, contact our office or fill out and mail us the Natural Heritage reporting form provided at the end of this publication. The New York Natural Heritage Program is a partnership with the New York State Department of Environmental Conservation and by The Nature Conservancy. Major support comes from the NYS Biodiversity Research Institute, the Environmental Protection Fund, and Return a Gift to Wildlife. TABLE OF CONTENTS Introduction.......................................................................................................................................... Page ii Why is the list published? What does the list contain? How is the information compiled? How does the list change? Why are plants rare? Why protect rare plants? Explanation of categories.................................................................................................................... Page iv Explanation of Heritage ranks and codes............................................................................................ Page iv Global rank State rank Taxon rank Double ranks Explanation of plant -
Inferring the Evolutionary Reduction of Corm Lobation in Isoëtes Using Bayesian Model- Averaged Ancestral State Reconstruction
UC Berkeley UC Berkeley Previously Published Works Title Inferring the evolutionary reduction of corm lobation in Isoëtes using Bayesian model- averaged ancestral state reconstruction. Permalink https://escholarship.org/uc/item/39h708p5 Journal American journal of botany, 105(2) ISSN 0002-9122 Authors Freund, Forrest D Freyman, William A Rothfels, Carl J Publication Date 2018-02-01 DOI 10.1002/ajb2.1024 Peer reviewed eScholarship.org Powered by the California Digital Library University of California RESEARCH ARTICLE BRIEF COMMUNICATION Inferring the evolutionary reduction of corm lobation in Isoëtes using Bayesian model- averaged ancestral state reconstruction Forrest D. Freund1,2, William A. Freyman1,2, and Carl J. Rothfels1 Manuscript received 26 October 2017; revision accepted 2 January PREMISE OF THE STUDY: Inferring the evolution of characters in Isoëtes has been problematic, 2018. as these plants are morphologically conservative and yet highly variable and homoplasious 1 Department of Integrative Biology, University of California, within that conserved base morphology. However, molecular phylogenies have given us a Berkeley, Berkeley, CA 94720-3140, USA valuable tool for testing hypotheses of character evolution within the genus, such as the 2 Authors for correspondence (e-mail: [email protected], hypothesis of ongoing morphological reductions. [email protected]) Citation: Freund, F. D., W. A. Freyman, and C. J. Rothfels. 2018. METHODS: We examined the reduction in lobe number on the underground trunk, or corm, by Inferring the evolutionary reduction of corm lobation in Isoëtes using combining the most recent molecular phylogeny with morphological descriptions gathered Bayesian model- averaged ancestral state reconstruction. American from the literature and observations of living specimens. -
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.