The Egg and the Nest: Obtaining Information About the Reproductive Biology of Apteryx Spp
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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. -
Jurassic Algae of the Perachora-Peninsula: Biostratigraphical and Paleoecological Implications
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 1994 Band/Volume: 19 Autor(en)/Author(s): Dragastan Ovidiu, Gielisch Hartwig, Richter Detlef K., Grewer Till, Kaziur Thomas, Kube Bärbel, Radusch Christoph Artikel/Article: Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications 49-81 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 19:49-81, Wien 1994 Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications Jurassische Algen der Perachora Halbinsel: Biostratigraphische und paläoökologische Folgerungen by DRAGASTAN, Ovidiu,* GIELISCH, Hartwig**, RICHTER, Detlev K.**, GREWER, TiU**, KAZIUR, Thomas**, KUBE, Bärbel **& RADUSCH, Christoph** DRAGASTAN, O., GIELISCH, H„ RICHTER, D.K., GREWER, T„ KAZIUR, T„ KUBE, B. & RADUSCH, C., 1994. Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications. — Beitr. Palaont., 19:49-81, 9 Figures, 6 Plates, Wien. ceae), Rivularia (Rivulariaceae), Alpinelia graeca n.sp. Contents (Scytonemataceae), Girvanella, Hedstroemia (Porostro- Abstract, Zusammenfassung.................................................. 49 mata) and Microproblematicae. 1. Introduction..............................................................................50 Biostratigraphically, a succession of algae and foramini- 2. Geological setting................................................................. -
Late Jurassic) Near Gulgong, New South Wales
DOI: 10.18195/issn.0312-3162.23(1).2006.043-076 Records of the Western Australian Museum 23: 43-76 (2006). The leptolepid fish Cavenderichthys talbragarensis (Woodward, 1895) from the Talbragar Fish Bed (Late Jurassic) near Gulgong, New South Wales 1. B. Bean Dept of Earth and Marine Sciences, The Australian National University, Canberra, ACT 0200, Australia e-mail: [email protected] Abstract - "Leptolepis" talbragarensis Woodward, 1895, is the most common fish species in the Talbragar Fish Bed near Gulgong, New South Wales. The genus Cavenderichthys Arratia, 1997, has this species as its type. The three species originally proposed by Woodward (1895) for "Leptolepis" are a single species. A detailed comparison of Cavenderichthys talbragarensis with members of the genus Leptolepis, and also with the Late Jurassic forms Tharsis dubius and Leptolepides sprattiformis, indicates that Cavenderichthys talbragarensis is most closely related to Late Jurassic members of the Family Leptolepididae. Analysis of zircons for geochronology showed that the sediment just below the richest fish layer has a youngest component of 151.55 ± 4.27 Ma, corresponding to the Kimmeridgian Stage of the Late Jurassic. Thin sections of the upper prolific fish layer show preservation in tuffaceous sediments, indicating that the fish population was killed by ash falls of felsic tuff that filled the pond they inhabited. INTRODUCTION partly on his own observations, but also on the Fossil fishes were first discovered at Talbragar work of Cavender (1970) who compared about 30 km northeast of Gulgong by Arthur Lowe coregonines and other salmonids with some of the of Wilbertree, NSW in 1889 (Woodward 1895). -
Wollemia Nobilis Wollemi Pine
MULCH Much Useful Learning Concerning Horticulture VOL.22 No.1, January, 2016 Castlemaine & District Garden Club Inc. Wollemia nobilis Wollemi pine Castlemaine & District Garden Club P.O. Box 758, Castlemaine 3450 [email protected] http://castlemainegardenclub.wordpress.com COMMITTEE Wollemia nobilis President Judy Uren 5470 6462 Vice-president Judy Eastwood 0417 149 251 Secretary Sally Leversha 0437 683 469 [email protected] Treasurer Alan Isaacs 5473 3143 Committee Members Marion Cooke Jan Gower Heather Spicer Sue Spacey Wollemi Pine: Kew Gardens Newsletter Editor Tom Comerford 5470 6230 Wollemia nobilis is a conifer in the [email protected] plant family Araucariaceae. The Webmaster discovery of the Wollemi Pine in Judy Hopley 5472 1156 1994 created great excitement in the [email protected] botanical community due to its resemblance to conifer fossils like Dillwynites and Agathis jurassica. Wollemi Pines are restricted to approximately 40 adult and 200 juvenile Wollemi Pines growing in the Wollemi National Park of New South Wales, 200 km north-west of Sydney. The rare nature of the I really look forward to Monday Wollemi Pine has seen it listed as morning—it gets me back to work endangered. The Wollemi Pine is a tree, which about striking the Wollemi Pine is can grow up to 40 m in the wild with that cuttings taken from the top of a trunk diameter reaching up to one the tree will produce a vertical metre. The bark of the tree is bubbly growing plant, whilst cuttings taken in appearance, chocolate brown from the bottom of the tree will colour in colour. -
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). -
Geology of the Petroleum and Coal Deposits in the Junggar (Zhungaer) Basin, Xinjiang Uygur Zizhiqu, Northwest China by K. Y
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology of the petroleum and coal deposits in the Junggar (Zhungaer) basin, Xinjiang Uygur Zizhiqu, northwest China By K. Y. Lee Open-File Report 85-230 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature, 1985 CONTENTS Page ADS tract ~~ ~~ 1 T.__introduction 4_ ~» ~^ J _ _ -^ 4_ ^ *-* * _ ~~ _ _ __ jO General statement ~ 3 Regional setting ~~ 3 Purpose, scope, and method of the report 6 ot ra t ig rapriy Pre-Carboniferous 6 Lower Paleozoic _______ ^ Devonian o Upper Paleozoic Carboniferous and Permian 8 Carboniferous 8 c"D cA Ly» II1J--y. 3 allf~ _. ~~ "~ "~ ______ ____ ^1 ^1 Me so zoic ~~ 1 j T*^»iLiaysxc -I f* ft ft £ -» ^__ ____ _._ _ __ _ __ _ ^ _^ _ _ _ _ ^1 -jC JurassicT_.___J_ ±o1Q f"tjic1 'r»x.k denozoi c n^A w» ±cJ. Quaternary 2.1 Geotectonics and evolution of the basin 27 .tectonics and sedimentation 2.1 OQ "I"L. **iiI. Ut- r* -f"uUUJL v»£k C _ __ _ "~ "~ JO ^O iNOLLncrnVT -» ~» ^- l_ --. ^» _ iriaLrorm"O 1 « *- f y-k «*rn ~ oz*5 O Northern Tian Shan Foredeep 33 Jretroieum and coal deposits IT~D C£^ -I"L *V*JL (JXcULllf\ 1 A11TYI __ ~~ _________________________________________ j^O /l Source rocks 35 Reservoir rocks ~ 37 LT3f\t- \J LCllLlet Qi->4- -i n -L1 ~~ ~~ ~~ . i+/ i.1 ____________________ _ ______________________________________ /, Q uccurrence ^ ^ ^y T?jxci rt -p Crt T»^Y>JL C11L.CO /^ £1 O t-J./ » "1 t"^k^1Led K>^«*«.^«.^«. -
Eggs and Eggshells of Crocodylomorpha from the Upper Jurassic of Portugal
João Paulo Vasconcelos Mendes Russo Licenciado em Geologia Eggs and eggshells of Crocodylomorpha from the Upper Jurassic of Portugal Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Octávio Mateus, Professor Auxiliar, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientadora: Ausenda Balbino, Professora Catedrática, Universidade de Évora Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha Arguente: Prof. Doutor José Carlos Alcobia Rogado de Brito Vogal: Prof. Doutor Octávio João Madeira Mateus Janeiro 2016 João Paulo Vasconcelos Mendes Russo Licenciado em Geologia Eggs and eggshells of Crocodylomorpha from the Upper Jurassic of Portugal Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Octávio Mateus, Professor Auxiliar, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientadora: Ausenda Balbino, Professora Catedrática, Universidade de Évora Janeiro 2016 J. Russo Eggs and eggshells of Crocodylomorpha from the Upper Jurassic of Portugal Acknowledgments As such an important step of my still short academic journey comes to a close, it comes the time to remember that I would never be able to have done this on my own, without the unwavering support and invaluable input of so many people, too many to name them all here. First and foremost, my deepest appreciation and thanks to my supervisor Professor Octávio Mateus, for granting me the possibility to study the material on this thesis and giving me the opportunity to be a part of such an important research project and become something I’ve aspired since I can remember. I appreciate the many eye opening discussions we had on Paleontology in general, and on Paleoology in particular, his counseling, and for making sure I was on the right track! None of this would be possible of course without the invaluable help of my co-supervisor, Professor Ausenda Balbino, who always made sure that I had every resource and support I needed to achieve the goals during this Master’s and this research. -
Review of Historical and Current Research on the Late Cretaceous
第55卷 第2期 古 脊 椎 动 物 学 报 pp. 187-200 2017年4月 VERTEBRATA PALASIATICA figs. 1-5 Review of historical and current research on the Late Cretaceous dinosaurs and dinosaur eggs from Laiyang, Shandong ZHANG Jia-Liang1,2 WANG Qiang1 JIANG Shun-Xing1 CHENG Xin1 LI Ning1 QIU Rui1,2 ZHANG Xin-Jun1,2 WANG Xiao-Lin1,2* (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 * Corresponding author: [email protected]) (2 University of Chinese Academy of Sciences Beijing 100049) Abstract Here we briefly review the history of research on the Laiyang dinosaur and dinosaur egg faunas, summarize the contributions of C. C. Young and other elder paleontologists to the discoveries of the Late Cretaceous dinosaurs and dinosaur eggs from Laiyang, and introduce the new discoveries and the advances in the research on the Laiyang faunas. The new investigations in Laiyang from 2008 have found a series of valley developed in plain and more than ten new dinosaur or dinosaur egg fossil beds. In 2010, we began the massive excavations at two localities in Jingangkou and collected abundant dinosaurs and other vertebrate fossils, such as a new saurolophine, some theropod material and a new taxon of turtle egg. The bone beds in Locality 2 with the typical sedimentary and burial patterns of mudflow, and these fossil deposits are interpreted as having been carried and deposited by mudflow. The re-observation and the CT scanning data of the crest of Tsintaosaurus spinorhinus (IVPP V 725) show that the crest is fractured and solid. -
Stage De Second Semestre : Mission De Mediation Scientifique Et De Presentation De Squelettes De Reptiles Marins Des Falaises Des Vaches Noires
Maxence LAMAURY Paléospace L’Odyssée Université de Rennes 1 – M2 PPP BP 6 Avenue Jean-Moulin 01 Mars – 31 Juillet 2017 14 640 Villers-sur-Mer STAGE DE SECOND SEMESTRE : MISSION DE MEDIATION SCIENTIFIQUE ET DE PRESENTATION DE SQUELETTES DE REPTILES MARINS DES FALAISES DES VACHES NOIRES Musée Paléospace L’Odyssée, Villers-sur-Mer Maître de stage : Laurent PICOT Tuteur universitaire : Didier NERAUDEAU STAGE DE SECOND SEMESTRE : MISSION DE MEDIATION SCIENTIFIQUE ET DE PRESENTATION DE SQUELETTES DE REPTILES MARINS DES FALAISES DES VACHES NOIRES Musée Paléospace L’Odyssée, Villers-sur-Mer SOMMAIRE : ▪ RESUME……………………………………………………………………………...p3 ▪ ABSTRACT…………………………………………………………………………..p3 1) INTRODUCTION……………………………………………………………………p4 • PALEOSPACE L’ODYSSEE…………………………………………………..p4 2) MATERIEL & METHODES…………………………………………………….....p5 a. LES FALAISES DES VACHES NOIRES……………………………………..p5 b. METHODES……………………………………………………………………..p8 I LES REPTILES MARINS………………………………………………………....p8 A. ICHTHYOSAURES………………………………………………………………...p9 B. PLESIOSAURES………………………………………………………………….p10 C. PLIOSAURES……………………………………………………………………..p11 D. CROCODILES MARINS………………………………………………………….p12 II PRESENTATION DE L’AFFICHE CREEE………………………………….p13 A. QUESTIONNAIRE………………………………………………………………..p13 B. RESULTATS………………………………………………………………………p14 C. AFFICHE…………………………………………………………………………..p16 3) CONCLUSION……………………………………………………………………..p18 4) REMERCIEMENTS……………………………………………………………….p18 5) BIBLIOGRAPHIE………………………………………………………………….p18 ▪ ANNEXE 1 – Photos des reptiles marins suspendus…………………………I ▪ ANNEXE 2 – Cartels de présentation -
Chinaxiv:201711.01905V1
ChinaXiv合作期刊 第55卷 第2期 古 脊 椎 动 物 学 报 pp. 187-200 2017年4月 VERTEBRATA PALASIATICA figs. 1-5 Review of historical and current research on the Late Cretaceous dinosaurs and dinosaur eggs from Laiyang, Shandong ZHANG Jia-Liang1,2 WANG Qiang1 JIANG Shun-Xing1 CHENG Xin1 LI Ning1 QIU Rui1,2 ZHANG Xin-Jun1,2 WANG Xiao-Lin1,2* (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 * Corresponding author: [email protected]) (2 University of Chinese Academy of Sciences Beijing 100049) Abstract Here we briefly review the history of research on the Laiyang dinosaur and dinosaur egg faunas, summarize the contributions of C. C. Young and other elder paleontologists to the discoveries of the Late Cretaceous dinosaurs and dinosaur eggs from Laiyang, and introduce the new discoveries and the advances in the research on the Laiyang faunas. The new investigations in Laiyang from 2008 have found a series of valley developed in plain and more than ten new dinosaur or dinosaur egg fossil beds. In 2010, we began the massive excavations at two localities in Jingangkou and collected abundant dinosaurs and other vertebrate fossils, such as a new saurolophine, some theropod material and a new taxon of turtle egg. The bone beds in Locality 2 with the typical sedimentary and burial patterns of mudflow, and these fossil deposits are interpreted as having been carried and deposited by mudflow. The re-observation and the CT scanning data of the crest of Tsintaosaurus spinorhinus (IVPP V 725) show that the crest is fractured and solid. -
New Ootype Prismatoolithids from the Late Cretaceous, Laiyang Basin
第56卷 第3期 古 脊 椎 动 物 学 报 pp. 264–272 2018年7月 VERTEBRATA PALASIATICA figs. 1–3 DOI: 10.19615/j.cnki.1000-3118.180708 New ootype prismatoolithids from the Late Cretaceous, Laiyang Basin and its significance WANG Qiang1,2 LI Yu-Guang3 ZHU Xu-Feng1,2,4 FANG Kai-Yong1,5 WANG Xiao-Lin1,2,4 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044) (2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044 [email protected]) (3 Capital Normal University Beijing 100048) (4 University of Chinese Academy of Sciences Beijing 100049) (5 School of Earth Sciences and Resources, China University of Geosciences, Beijing Beijing 100083) Abstract Here we discribe a new ootypes of prismatoolithids found from the Late Cretaceous Jiangjunding Formation in the Laiyang Basin, Shandong Province. On the basis of characters such as elongate ovoids, smooth eggshell surface, relatively thinner eggshell thickness, prismatic eggshell units, slender pores in radial section of eggshell and little pores with round or irregular shapes in tangeital section of eggshell, we erect one new oogenus and one new oospecies: Laiyangoolithus lixiangensis oogen. et oosp. nov. The discovery of L. lixiangensis not only enriches the diversity and composition of the Laiyang Dinosaur Egg Fauna, but the paleogeographic distribution of primatoolithids as well. In addition, it provides more paleontological materials for the study of the diversity and paleogeographic distribution of troodontids in China. Key words Laiyang, Shandong; Late Cretaceous; Jiangjunding Formation; dinosaur eggs, Prismatoolithidae Citation Wang Q, Li Y G, Zhu X F et al., 2018. -
Vanuata Vegetation
Plant Formations in the Vanuatu BioProvince Peter Martin Rhind Vanuatu Mixed Lowland Rain Forest Up to about 600 m altitude lowland rain forest is the natural vegetation on the southeastern, windward sides of all Vanuatu islands. Important trees are Antiaris toxicaria, Castanospermum australe, Intsia bijuga and Kleinhovia hospitat. Endemic species include Alangium vitense (Cornaceae). On old volcanic ash, rich in plant nutrients, trees can reach more than 30 m in height with large crowns. Typical sub canopy trees include Diospyros acris, Garcinia pancheri and Syzygium species, while endemic small trees include various Veitchia palms, Calophyllum inophyllum (Clusiaceae) and Trilocularia pedicellata (Balanopsidaceae). These forests are best developed on the northern islands of Malakula and Espiritu Santo, and are structurally similar to forests on the Solomon Islands. However, many are in various stages of recovery following disturbance from hurricanes. Vines and epiphytes are numerous and certain areas are covered with lianas. The undergrowth includes various shrubs, and typically there is an herbaceous ground layer comprising genera such as Geophila and Homalomena and ferns like Asplenium, Microsorium and Pteris, but tree ferns are usually absent. Of endemic species, however, many seem to be specific to certain islands or island groups. On Aneityum, for example, there are endemic trees such as Boehmeria anisoneura (Urticaceae), Canarium aneityensis (Burseraceae), Couthovia neo-ebudica (Loganiaceae), Cryptocarya wilsonii (Lauraceae), Cupaniopsis