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Plant Mobility in the Mesozoic Disseminule Dispersal Strategies Of
Palaeogeography, Palaeoclimatology, Palaeoecology 515 (2019) 47–69 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Plant mobility in the Mesozoic: Disseminule dispersal strategies of Chinese and Australian Middle Jurassic to Early Cretaceous plants T ⁎ Stephen McLoughlina, , Christian Potta,b a Palaeobiology Department, Swedish Museum of Natural History, Box 50007, 104 05 Stockholm, Sweden b LWL - Museum für Naturkunde, Westfälisches Landesmuseum mit Planetarium, Sentruper Straße 285, D-48161 Münster, Germany ARTICLE INFO ABSTRACT Keywords: Four upper Middle Jurassic to Lower Cretaceous lacustrine Lagerstätten in China and Australia (the Daohugou, Seed dispersal Talbragar, Jehol, and Koonwarra biotas) offer glimpses into the representation of plant disseminule strategies Zoochory during that phase of Earth history in which flowering plants, birds, mammals, and modern insect faunas began to Anemochory diversify. No seed or foliage species is shared between the Northern and Southern Hemisphere fossil sites and Hydrochory only a few species are shared between the Jurassic and Cretaceous assemblages in the respective regions. Free- Angiosperms sporing plants, including a broad range of bryophytes, are major components of the studied assemblages and Conifers attest to similar moist growth habitats adjacent to all four preservational sites. Both simple unadorned seeds and winged seeds constitute significant proportions of the disseminule diversity in each assemblage. Anemochory, evidenced by the development of seed wings or a pappus, remained a key seed dispersal strategy through the studied interval. Despite the rise of feathered birds and fur-covered mammals, evidence for epizoochory is minimal in the studied assemblages. Those Early Cretaceous seeds or detached reproductive structures bearing spines were probably adapted for anchoring to aquatic debris or to soft lacustrine substrates. -
Triassic) in Barreal Depocenter, San Juan Province, Argentina
Andean Geology ISSN: 0718-7092 ISSN: 0718-7106 [email protected] Servicio Nacional de Geología y Minería Chile Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Bodnar, Josefina; Iglesias, Ari; Colombi, Carina E.; Drovandi, Juan Martín Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Andean Geology, vol. 46, no. 3, 2019 Servicio Nacional de Geología y Minería, Chile Available in: https://www.redalyc.org/articulo.oa?id=173961656006 This work is licensed under Creative Commons Attribution 3.0 International. PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative Josefina Bodnar, et al. Stratigraphical, sedimentological and palaeofloristic characterization of ... Research article Stratigraphical, sedimentological and palaeofloristic characterization of the Sorocayense Group (Triassic) in Barreal depocenter, San Juan Province, Argentina Caracterización estratigráfica, sedimentológica y paleoflorística del Grupo Sorocayense (Triásico) en el área de Barreal, provincia de San Juan, Argentina Josefina Bodnar *12 Redalyc: https://www.redalyc.org/articulo.oa? Universidad Nacional de La Plata, Argentina id=173961656006 [email protected] Ari Iglesias 23 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Carina E. Colombi 24 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Juan Martín Drovandi 24 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina [email protected] Received: 30 November 2017 Accepted: 30 October 2018 Published: 04 February 2019 Abstract: e northern area of Cuyo Basin (west-central Argentina) corresponds to the Rincón Blanco half-graben, whose filling is arranged into the Rincón Blanco and Sorocayense groups. -
The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/Telemachus (Voltziales) from Antarctica
KU ScholarWorks | http://kuscholarworks.ku.edu Please share your stories about how Open Access to this article benefits you. The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/ Telemachus (Voltziales) From Antarctica by Benjamin Bomfleur, Rudolph Serbet, Edith L. Taylor, and Thomas N. Taylor 2011 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. Bomfleur, B., Serbet, R., Taylor, E., and Taylor, N. 2011. The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/Telemachus (Voltziales) From Antarctica. Antarctic Science 23(4): 379-385. Published version: http://dx.doi.org/10.1017/S0954102011000241 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. Antarctic Science 23(4), 379–385 (2011) & Antarctic Science Ltd 2011 doi:10.1017/S0954102011000241 The possible pollen cone of the Late Triassic conifer Heidiphyllum/Telemachus (Voltziales) from Antarctica BENJAMIN BOMFLEUR, RUDOLPH SERBET, EDITH L. TAYLOR and THOMAS N. TAYLOR Division of Paleobotany at the Department of Ecology and Evolutionary Biology, and Natural History Museum and Biodiversity Institute, University of Kansas, Lawrence, KS 66045, USA bbomfl[email protected] Abstract: Fossil leaves of the Voltziales, an ancestral group of conifers, rank among the most common plant fossils in the Triassic of Gondwana. Even though the foliage taxon Heidiphyllum has been known for more than 150 years, our knowledge of the reproductive organs of these conifers still remains very incomplete. Seed cones assigned to Telemachus have become increasingly well understood in recent decades, but the pollen cones belonging to these Mesozoic conifers are rare. -
Araucaria Indica and Two Other Conifers from the Jurassic-Cretaceous Rocks of Madhya Pradesh, India
ARAUCARIA INDICA AND TWO OTHER CONIFERS FROM THE JURASSIC-CRETACEOUS ROCKS OF MADHYA PRADESH, INDIA SUKH-DEV & ZEBA-BANO Birbal Sahni Institute of Palaeobotany, Lucknow-226007, India ABSTRACT This paper reports the occurrence of the living genus Araucaria in the Juras• sic-Lower Cretaceous flora of the Jabalpur Formation, Madhya Pradesh. The species of this genus, Araucaria indica (Sahni) n. comb., is based on leaves and seed-scales. Also, a new genus Satpuria is instituted to accommodate linear conifer leaves, the affinities of which are yet uncertain. Under this genus, S. sehoraensis n. sp. and Satpuria sp. are described from the same formation. INTRODUCTION whose affinities are yet uncertain. These leaves are described here under a new genus Satpuria. Presently two species, S. sehora• INdesh,the UpperdetachedGondwanaslinear leavesof Madhyaof Desmio•Pra• ensis n. sp. and Satpuria sp. are dis• phyllum indicum Sahni (1928) are found tinguished. near jhirnapur, jatarnao, Parsapani, Hasna• pur, Hard River, lmjhiri, Sehora, jabalpur, Bansa and Chandia; near Sehora, Bansa and DESCRIPTION Chandia they are in abundance. Till now Family - ARAUCARIACEAE their affinities were not fully certain. Asso• ciated with Desmiophyllum indicum, in the Genus - Araucaria Jussieu beds of Sehora, jabalpur, Bansa and Chandia detached seed-scales Araucaria Araucaria indica (Sahni) n. comb. pantiana Bose & Maheshwari (1973) are PI. 1, figs. 1-10; Text-fig. lA-J found which were first referred to the lA. Leaves: living genus Araucaria by Pant and Srivastava (1968) on the basis of their 1877 Podozamite9 lanceolatus Schimp. close similarity with seed-scales of Araucaria (Lind!. & Hutt. sp.): Feistmantel, columnaris (Forster) Hooker. -
Foliage of a Broad Leaved Conifer Dammarophyllum from the Cenomanian of Bohemia
Časopis Národního muzea, Řada přírodovědná (J. Nat. Mus., Nat. Hist. Ser.) Vol. 172 (1–4):13–20, 2003 Palaeobotany FOLIAGE OF A BROAD LEAVED CONIFER DAMMAROPHYLLUM FROM THE CENOMANIAN OF BOHEMIA Jiří Kvaček Department of Palaentology, National Museum, 115 79 Praha 1, Czech Republic Received May 6, 2003 Accepted May 30, 2003 Abstract. The morphogenus Dammarophyllum VELENOVSKÝ is validated and emended to accommodate broad-leaved coniferous foliage with an affinity to Araucariaceae or Podocarpaceae. It shows character- istic parallel venation consisting of simple veins, arising from the base and gradually converging to the apex. Cuticle of hypostomatic leaves shows haplocheilic stomata without dorsal lamelae arranged irregu- larly or longitudinally in short rows. The genus Dammarophyllum is sofar monospecific. It is compared to other genera of similar leaf morphology Dammarites PRESL, Lindleycladus HARRIS, Nageiopsis FONTAINE, and Podozamites C.F.W. BRAUN. I Araucariaceae, Podocarpaceae, conifers, Cenomanian, Cretaceous. INTORODUCTION Broad-leaved conifers are rare elements of mid-European Cretaceous floras. Their fossil remains have been traditionally associated with the family Araucariaceae, although similar foliage is known e. g. in the family Podocarpaceae. Unequivocal remains of the Araucariaceae showing a cone scale with one centrally arranged inverted seed were recorded in the Upper Cretaceous of the Czech Republic in the Březno Formation by Bayer (in Frič 1893). Other fossils found in the Bohemian Cretaceous Basin and inter- preted as araucariaceous, e.g. Dammara borealis HEER and Brachyphyllum squamosum (VELENOVSKÝ) PALIBIN, are considered here as doubtful. Dammara borealis is probably related to the recently described family Doliostrobaceae (Z. Kvaček 2002). Although the Araucariaceae, in contrast to the Podocarpaceae, has been recorded in the European Cretaceous the morphogenus Dammarophyllum is suggested to include foliage of the both families. -
Exceptionally Well-Preserved Early Cretaceous Leaves of Nilssoniopteris from Central Mongolia
Acta Palaeobotanica 58(2): 135–157, 2018 e-ISSN 2082-0259 DOI: 10.2478/acpa-2018-0016 ISSN 0001-6594 Exceptionally well-preserved Early Cretaceous leaves of Nilssoniopteris from central Mongolia FABIANY HERRERA1,5,*, GONGLE SHI2, GOMBOSUREN TSOLMON3, NIIDEN ICHINNOROV 3, MASAMICHI TAKAHASHI4, PETER R. CRANE5,6 and PATRICK S. HERENDEEN1 1 Chicago Botanic Garden, Glencoe, Illinois 60022 USA; e-mails: [email protected]; [email protected] 2 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008 People’s Republic of China; e-mail: [email protected] 3 Institute of Paleontology and Geology, Mongolian Academy of Sciences, Ulaanbaatar-51, Mongolia; e-mails: [email protected]; [email protected] 4 Department of Environmental Sciences, Niigata University, Ikarashi, Nishi-ku, Niigata 950-2181 Japan; e-mail: [email protected] 5 Oak Spring Garden Foundation, Upperville, Virginia 20184 USA 6 School of Forestry and Environmental Studies, Yale University, New Haven, Connecticut 06511 USA; e-mail: [email protected] Received 20 June 2018; accepted for publication 25 October 2018 ABSTRACT. Two new Early Cretaceous (Aptian-Albian) species of fossil bennettitalean leaves are described from central Mongolia and assigned to the genus Nilssoniopteris. Nilssoniopteris tomentosa F.Herrera, G.Shi, Tsolmon, Ichinnorov, Takahashi, P.R.Crane, et Herend. sp. nov., isolated from bulk sediment samples collected for mesofossils in the Tevshiingovi Formation at the Tevshiin Govi opencast coal mine, is distinctive in having a dense, well-developed indumentum composed of branched, fattened multicellular trichomes on the abaxial leaf surface. -
Diversity and Homologies of Corystosperm Seed-Bearing Structures from the Early Cretaceous of Mongolia Aã B,C D E F Gongle Shi , Peter R
Journal of Systematic Palaeontology ISSN: 1477-2019 (Print) 1478-0941 (Online) Journal homepage: https://www.tandfonline.com/loi/tjsp20 Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera To cite this article: Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera (2019) Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia, Journal of Systematic Palaeontology, 17:12, 997-1029, DOI: 10.1080/14772019.2018.1493547 To link to this article: https://doi.org/10.1080/14772019.2018.1493547 Published online: 14 Jan 2019. Submit your article to this journal Article views: 142 View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tjsp20 Journal of Systematic Palaeontology, 2019 Vol. 17, No. 12, 997–1029, http://dx.doi.org/10.1080/14772019.2018.1493547 Diversity and homologies of corystosperm seed-bearing structures from the Early Cretaceous of Mongolia aà b,c d e f Gongle Shi , Peter R. Crane , Patrick S. Herendeen , Niiden Ichinnorov , Masamichi Takahashi and Fabiany Herrerad aState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China; bOak Spring Garden -
Jurassic Flora of Cape 1,Isburne Alaska
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR THE JURASSIC FLORA OF CAPE 1,ISBURNE ALASKA F. H. KNOWLTON Publishecl January 28, 1914 PART D OF PROFESSIONAL PAPER 85, "CONTRIBUTIONS TO GENERAL GEOLOGY 1913" WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page . Introduction ............................................................................................ 39 The Corwin formation ..................................................................................... 39 Plant collections ......................................................................................... 40 Age of the plant-bearing beds ............................................................................. 41 Distribution of Jurassic floras ............................................................................. 43 Geographicrange .................................................................................... 43 Means of dispersal ................................................................................... 45 Avenues of dispersal ................................................................................. 45 Probable climatic conditions .......................................................................... 46 .The flora ................................................................................................ 46 ILLUSTRATIONS. Page . PLATESV-VIII . Jurassic flora of Cape Lisburne, Alaska .................................................... 57-64 THE' JUR,ASSIC FLORA OF CAPE -
Revision of the Talbragar Fish Bed Flor (Jurassic)
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS White, Mary E., 1981. Revision of the Talbragar Fish Bed Flora (Jurassic) of New South Wales. Records of the Australian Museum 33(15): 695–721. [31 July 1981]. doi:10.3853/j.0067-1975.33.1981.269 ISSN 0067-1975 Published by the Australian Museum, Sydney naturenature cultureculture discover discover AustralianAustralian Museum Museum science science is is freely freely accessible accessible online online at at www.australianmuseum.net.au/publications/www.australianmuseum.net.au/publications/ 66 CollegeCollege Street,Street, SydneySydney NSWNSW 2010,2010, AustraliaAustralia REVISION OF THE TALBRAGAR FISH BED FLORA (jURASSiC) OF NEW SOUTH WALES MARY E. WH ITE The Australian Museum, Sydney. SUMMARY The three well known form-species of the Talbragar Fish Bed Flora-Podozamites lanceolatus, Elatocladus planus and Taeniopteris spa tu lata - are redescribed as Agathis jurassica sp. nov., Rissikia talbragarensis sp. novo and Pentoxylon australica sp. novo respectively. The minor components of the assemblage are described and illustrated, and in some cases, reclassified. Additions are made to the list of plants recorded from the horizon. INTRODUCTION The Talbragar Fish Beds are characterised by their beautifully preserved fish and plant remains which occur in great profusion throughout the shale lens which comprises the Beds. The ochre-coloured shale is ferruginous, with impressions of plants and fish, white in colour, standing out dramatically. The weathering of the outer layers of blocks of the shale has resulted in contrasting bands of iron-rich stain framing many of the specimens and enhancing their appearance. Specimens are much prized by collectors. The fossil locality is the valley ofthe Talbragar River, about twenty miles due North of Home Rule Mine in the Cassilis District, "on the southern boundary of Boyce's selection" (Anderson 1889). -
The Jurassic Plants from Shitaka (The Maizuru Coal-Field), Prov
Title The Jurassic Plants from Shitaka (the Maizuru Coal-field), Prov. Tango (Kyôto Prefecture), Japan Author(s) Ôishi, Saburô Citation Journal of the Faculty of Science, Hokkaido Imperial University. Ser. 4, Geology and mineralogy, 2(1), 1-14 Issue Date 1932-11 Doc URL http://hdl.handle.net/2115/35750 Type bulletin (article) File Information 2(1)_1-14.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP THE YURASSXC PLAN arS FROM SwnllTAKA (THE MAXZURU'COALpFXELD), PROV. TANGO (KYOTO A PREFEC'ffrURE), JAPAN By Sabur6 AOIsm valth 3 Plates ancl 1 Text-PiguTe. The geology of the so-ca]Ied Maizuru eoal-field, about 8 km. SWW ' of ]YIaizuru, and the surrounding area was first mentioned by D. YAMA- smTA in 1895 in the IExpianatory Text to the Geological Map in 11200,OeO; Sheet Hieizan. But he did not announce the occurrence of any Mesozoic fossil plants there, and only correlated the coal seams to those of the Cretaceous age developed in the Islands of Amakusa. In l897, Dr. [[7. 0GAwA(') also touched upon the geology of the ]Mresozoic area in his study on the basie eruptive rocks of northern Tamba and ealled the coal-bearing series, in which he found some fossil plants, the Shitaka Series. He enumerated the following fossil plants col- lected from Shital<a where the main anthraeite searns are being worked now and mentioned that they indicate the Mesozoic age of the plant-beds; they are: Zamiophyllum sp. Podozamites lanceolatus Aspleniu7n ToesseTti ? Taeniopteris Of these Zamiophyllum sp. may be a fragment of Cfr. -
Emese Réka Bodor
Növényi reproduktív képletek a Mecseki Kőszén Formációból DOKTORI ÉRTEKEZÉS 2015 BODOR EMESE RÉKA ELTE TTK, Őslénytani Tanszék MFGI, Földtani és Geofizikai Gyűjteményi Főosztály Témavezetők: Dr. BARBACKA MARIA (Főmuzeológus, MTM, Növénytár) Dr. KÁZMÉR MIKLÓS (Tanszékvezető egyetemi tanár, ELTE, TTK, Őslénytani Tanszék) ELTE, TTK, Földtudományi Doktori Iskola Doktori iskola vezetője: Dr. NEMES- NAGY JÓZSEF Földtan Geofizika Programvezetője: Dr. MINDSZENTY ANDREA Bodor Emese Réka Növényi reproduktív képletek a Mecseki Kőszén Formációból Tartalomjegyzék A KUTATÁSI TÉMA ELŐZMÉNYEI ÉS CÉLKITŰZÉSEI .......................................................................... 3 FÖLDTANI HÁTTÉR .......................................................................................................................................... 5 ANYAG ÉS MÓDSZEREK ................................................................................................................................. 9 VIZSGÁLT ANYAG ............................................................................................................................................... 9 ANYAGVIZSGÁLATI MÓDSZEREK ......................................................................................................................... 9 Kutikula vizsgálati eljárások ......................................................................................................................... 9 SZEDIMENTOLÓGIAI VIZSGÁLATI MÓDSZEREK ................................................................................................. -
An Advanced Peltasperm Permoxylocarpus Trojanus Naug
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Wulfenia Jahr/Year: 2010 Band/Volume: 17 Autor(en)/Author(s): Naugolnykh Serge V., Oskolski Alexei A. Artikel/Article: An advanced peltasperm Permoxylocarpus trojanus Naug. from the Lower Permian of the Urals (Russia): an ancient case of entomophily in gymnosperms? 29-43 © Landesmuseum für Kärnten; download www.landesmuseum.ktn.gv.at/wulfenia; www.biologiezentrum.at Wulfenia 17 (2010): 29 – 43 Mitteilungen des Kärntner Botanikzentrums Klagenfurt An advanced peltasperm Permoxylocarpus trojanus Naug. from the Lower Permian of the Urals (Russia): an ancient case of entomophily in gymnosperms? Serge V. Naugolnykh & Alexei A. Oskolski Summary: The evolutionarily advanced gymnosperm of peltaspermalean affi nity Permoxylocarpus trojanus Naug. from the Lower Permian deposits of the Urals (Russia) is described. Female reproductive organs of P. trojanus are spherical, semi-closed, peltate capsules with 15 –16 enclosed seeds. Both macromorphology and microstructure, including epidermal-cuticular characters and the anatomical structure of conducting tissues, are characterized. Sterile leaves of Praephylladoderma leptoderma Naug., provisionally belonging to the same parent plant, are also described. Some aspects of peltasperm evolution during the Late Palaeozoic – Early Mesozoic are briefl y summarized. The occurrence of enclosed ovuliferous organs (capsules) in some peltasperms, the structure of their pollen grains as well as some palaeoentomological evidences suggest the gradual shift from anemophily to entomophily in evolution of these gymnosperms. Keywords: peltasperms, evolution, Permian, seed-bearing organs, preangiosperms, fossil records, entomophily Pteridosperms sensu lato were widely distributed seed plants during the Late Palaeozoic. This very diverse group is commonly regarded as a grade rather than a well-supported clade.