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Shrubs, Trees and Contingent Evolution of Wood Anatomical Diversity Using Croton (Euphorbiaceae) As a Model System
Annals of Botany 119: 563–579, 2017 doi:10.1093/aob/mcw243, available online at www.aob.oxfordjournals.org Force of habit: shrubs, trees and contingent evolution of wood anatomical diversity using Croton (Euphorbiaceae) as a model system Rafael Are´valo1,2,*, Benjamin W. van Ee3, Ricarda Riina4, Paul E. Berry5 and Alex C. Wiedenhoeft1,2 1Center for Wood Anatomy Research, USDA Forest Service, Forest Products Laboratory, Madison, WI 53726, USA, 2Department of Botany, University of Wisconsin, Madison, WI 53706, USA, 3University of Puerto Rico at Mayagu¨ez Herbarium, Department of Biology, Universidad de Puerto Rico, Call Box 9000, Mayagu¨ez, 00680, Puerto Rico, 4Real Jardın Botanico, RJB-CSIC, Plaza de Murillo 2, 28014 Madrid, Spain and 5University of Michigan, Ecology and Evolutionary Biology Department and Herbarium, Ann Arbor, MI 48108, USA *For correspondence. E-mail [email protected] Received: 7 July 2016 Returned for revision: 3 September 2016 Accepted: 5 October 2016 Published electronically: 8 January 2017 Background and Aims Wood is a major innovation of land plants, and is usually a central component of the body plan for two major plant habits: shrubs and trees. Wood anatomical syndromes vary between shrubs and trees, but no prior work has explicitly evaluated the contingent evolution of wood anatomical diversity in the context of these plant habits. Methods Phylogenetic comparative methods were used to test for contingent evolution of habit, habitat and wood anatomy in the mega-diverse genus Croton (Euphorbiaceae), across the largest and most complete molecular phy- logeny of the genus to date. Key Results Plant habit and habitat are highly correlated, but most wood anatomical features correlate more strongly with habit. -
Polskaakademianauk Instytutpaleobiologii
POLSKA AKADEMIA NAUK INSTYTUT PALEOBIOLOGII im. Romana Kozłowskiego SILURIAN AND DEVONIAN HETEROSTRACI FROM POLAND AND HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS Sylurskie i dewońskie Heterostraci z Polski oraz efektywność hydrodynamiczna psammosteidów Marek Dec Dissertation for degree of doctor of Earth and related environmental sciences, presented at the Institute of Paleobiology of Polish Academy of Sciences Rozprawa doktorska wykonana w Instytucie Paleobiologii Polskiej Akademii Nauk pod kierunkiem prof. dr hab. Magdaleny Borsuk-Białynickiej w celu uzyskania stopnia doktora w dyscyplinie Nauki o Ziemi oraz środowisku Warszawa 2020 CONTENTS ACKNOWLEDGMENTS…………………………………………………………….….... 3 STRESZCZENIE………………………………………………………………….....….. 4 SUMMARY……………………………………………………………………….…….. 8 CHAPTER I…………………………………………………………………………….. 13 TRAQUAIRASPIDIDAE AND CYATHASPIDIDAE (HETEROSTRACI) FROM LOWER DEVONIAN OF POLAND CHAPTER II……………………………………………………………………….…… 24 A NEW TOLYPELEPIDID (AGNATHA, HETEROSTRACI) FROM THE LATE SILURIAN OF POLAND CHAPTER III…………………………………………………………………………... 41 REVISION OF THE EARLY DEVONIAN PSAMMOSTEIDS FROM THE “PLACODERM SANDSTONE” - IMPLICATIONS FOR THEIR BODY SHAPE RECONSTRUCTION CHAPTER IV……………………………………………………………………….….. 82 NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID FROM HOLY CROSS MOUNTAINS (POLAND) CHAPTER V……………………………………………………………………………109 HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS: NEW INSIGHTS FROM COMPUTATIONAL FLUID DYNAMICS SIMULATIONS 2 ACKNOWLEDGMENTS First and foremost I would like to say thank you to my supervisor Magdalena -
Class Myxini Order Myxiniformes Family Myxinidae (Hagfishes)
Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) • Lacks jaws • Mouth not disk-like • barbels present • Unpaired fins as continuous fin-fold • Branchial skeleton not well developed • Eyes degenerate • 70-200 slime glands • Isoosmotic, simple kidneys, stenohayline, marine • Four rudimentary hearts • No true stomach • Unpaired gonads Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) (Northern Lampreys) • Knot-tying behavior • 8 genera, 34 species • Scavengers • Dorsal fins continuous in • Rely heavily on cutaneous respiration adults • Global, deep sea distribution • Oral disc • Commercial interest – eelskin • 7 pairs of gill openings • Single nostril • Pineal body opening • No bone • No scales • No paired fins • No jaws 1 Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae (Northern Lampreys) (Northern Lampreys) • Anadramous and freshwater • Ammocoete • Parasitic forms: – Non-parasitic forms often • Non-parasitic: freshwater – Parasitic forms often anadramous • Life history Class Conodonta, Conodonts Class Pteraspidiomorphi • Extinct, late Triassic • Extinct • First “teeth” • One of the earliest known vertebrates • No jaws • Dermal skeleton • Cranium and teeth • No jaws • Small, thought to be of paedomorphic origin • Little known, an extinct monophyletic lineage. 2 Class Anapsid Class Cephalaspidomorphi, osteostraci • Extinct, Silurian period • Extinct, early Silurian -
UNIVERSITY of CALIFORNIA Los Angeles
UNIVERSITY OF CALIFORNIA Los Angeles Evolution of the boxfish carapace: functional consequences of shape A thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Biology by Tina Ashley Marcroft 2015 ABSTRACT OF THE THESIS Evolution of the boxfish carapace: functional consequences of shape by Tina Ashley Marcroft Master of Science in Biology University of California, Los Angeles, 2015 Professor Michael Edward Alfaro, Chair Boxfishes are a group of heavily armored Tetraodontiform fishes that are highly variable in shape. Disparification of shape could be driven by a simple performance trade-off between its two hypothesized primary functions: protection from predation and maneuverability. Alternatively, disparification could be driven by many-to-one mapping of shape to performance, where a relaxation in morphological constraint where many of morphologies have the same performance. We tested this by isolating the major features of the boxfish carapace shape and tested for their correlation to performance, as well as for a negative correlation between performances. We found that some features were correlated but very weakly, and that the two performances did trade-off but also weakly. This weak correlation primarily suggests that many- to-one mapping of shape to performance is driving disparification, which was unobserved in continuous 3D shape systems until this study. ii The thesis of Tina Ashley Marcroft is approved. Blaire Van Valkenburgh David K. Jacobs Michael Edward Alfaro, Committee Chair University of California, Los Angeles 2015 iii I dedicate this thesis to Carrie Umetsu, Joseph Aprill, Mai Nguyen, Princess Gilbert, Francisca Wufu, Deb Pires, Jonathan Chang, Herbert Icasiano, and many others, without whose unwavering emotional and professional support I would not have completed this text. -
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. -
Bone Metabolism and Evolutionary Origin Of
Bone metabolism and evolutionary origin of osteocytes: Novel application of FIB-SEM tomography Yara Haridy, Markus Osenberg, André Hilger, Ingo Manke, Donald Davesne, Florian Witzmann To cite this version: Yara Haridy, Markus Osenberg, André Hilger, Ingo Manke, Donald Davesne, et al.. Bone metabolism and evolutionary origin of osteocytes: Novel application of FIB-SEM tomography. Science Ad- vances , American Association for the Advancement of Science (AAAS), 2021, 7 (14), pp.eabb9113. 10.1126/sciadv.abb9113. hal-03188775 HAL Id: hal-03188775 https://hal.sorbonne-universite.fr/hal-03188775 Submitted on 2 Apr 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. SCIENCE ADVANCES | RESEARCH ARTICLE EVOLUTIONARY BIOLOGY Copyright © 2021 The Authors, some rights reserved; Bone metabolism and evolutionary origin of osteocytes: exclusive licensee American Association Novel application of FIB-SEM tomography for the Advancement Yara Haridy1*†, Markus Osenberg2*, André Hilger2, Ingo Manke2, of Science. No claim to 3,4 1 original U.S. Government Donald Davesne , Florian Witzmann Works. Distributed under a Creative Lacunae and canaliculi spaces of osteocytes are remarkably well preserved in fossilized bone and serve as an Commons Attribution established proxy for bone cells. -
Studies in Organic Geochemistry"
A Thesis entitled "STUDIES IN ORGANIC GEOCHEMISTRY" submitted to the UNIVERSITY OF GLASGOW in part fulfilment of the requirements for admittance to the degree of DOCTOR OF PHILOSOPHY in the Faculty of Science by JAMES RANKIN MAXWELL, B.Sc. Chemistry Department April, 1967 ProQuest Number: 11011805 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11011805 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 To t:vv rorontn , v/if^ and dna^ktor, I wish to express my gratitude to Drs. G.Eglinton and J.D, Loudon for their close interest and guidance throughout the work of this thesis. My appreciation is also due to Dr. A.G, Douglas, whose assistance at all times proved to he invaluable. I would also like to thank Miss F. Greene and Miss T.Devit for technical assistance, my colleagues of the Organic Geochemistry Unit and Dr. A, McCormick for their advice and help, Mr, J.M.L. Cameron and his staff for the micro-analyses, Mrs. F. Lawrie and Miss A. -
K Urik, Pycnosteus Tuberculatus (Rohon), Ganosteus Stellatus Rohon and Psammosteus Bergi (Obr.) Are Now Presented in a Somewhat Modified Form
EESTI NSV TEADUSTE AKADEEMIA TOIMETISED. XVII KOIDE I(EEMIA • GEOLOOGIA. 1968, Nr. 3 H3BECTH51 AKAJlEMHH HAYK 3CTOHCKOH CCP. TOM XVII XI1MH5! * T'EOJ10ri15L 1968. N'o 0 D . OBRUCHEV, E. MARK-KURIK ON THE EVOLUTION OF THE PSAMMOSTEIDS (HETEROSTRACI) After our joint paper ( 1965) has been published, new materials of psammosteids have been collected in the Baltic area, and a number of new restorations have been made, and some of the older ones modified. The purpose of the present paper is to give a concise account of the evolution and ontogenetic development of this interesting group of fossil Agnatha, together with some data on their morphology. This study is based solely on the material from the Main Devonian Field (Baltic states, Leningrad, Pskov and adjacent regions), which is the chief area of deve iopment of the psammosteids in the Soviet Union, as well as in the world in general. In the Givetian and Frasnian of the Main Devonian Field the psam mosteids are represented by seven genera, comprising numerous species. Their fossil remains consist as a rule of isolated plates and scales. Only in very few cases same of the plates have been preserved in natural tonnection. Most frequently the branchial plates are met with, so that many species have been founded only on these plates. Lateral and ridge scales are rather common. Dorsal and ventral plates are twice as ·rare as the branchials. Other plates: rostrals, pineals, orbitals, postorbitals, cor nuals and the anterior plates of the ventral carapace, have been discovered only in a few occasions. Although the material of many forms is rather insufficient, attempts have been made to make restorations of a number of psammosteids (Fig. -
Chapter 2. Vegetative Morphology of Plants Vegetative Morphology of Plants
Chapter 2. Vegetative morphology of plants Vegetative morphology of plants INTRODUCTION: THE PLANT’S BASIC BODY PLAN Most plants are photosynthetic machines: they capture the energy contained in sunlight and transform solar radiation into chemical energy stored the form of bonds in chains of carbon molecules. Through the process of photosynthesis, light and atmospheric CO2 are combined in the leaves of green plants to form simple carbohydrates, which are then used to build other organic molecules such as cellulose, starch, oils, waxes, proteins, or DNA. Six molecules of CO2 (and some 72 photons of light) are needed to form one molecule of glucose: sunlight 6 CO2 + 6 H2O → C6H12O6 + 6 O2 As a byproduct of the process, six molecules of oxygen are formed and dissipated from the leaf tissue into the atmosphere. To achieve this remarkable feat of turning atmospheric carbon dioxide into living molecules while releasing oxygen into the earth’s atmosphere, plants have evolved highly specialized organs. The light-intercepting structure par excellence is the leaf. The set of leaves in the upper aerial part of the plant form the plant’s canopy, where the plant exchanges gases with the atmosphere and intercepts light from the sun. But in order to work its chemical wonder up in the leaves, the plant also needs water and mineral nutrients such as phosphorus, essential for the synthesis of DNA, or nitrogen, essential for manufacturing proteins. In order to obtain these, plants have developed the root —a complex network of underground stem-like organs— whose role is the absorption of water and mineral nutrients from the soil, and, in doing so, anchoring the plant to the ground. -
A New Middle Devonian (Givetian) Psammosteid (Vertebrata: Heterostraci) from Poland
Annales Societatis Geologorum Poloniae (2020), vol. 90: 75 – 93 doi: https://doi.org/10.14241/asgp.2020.04 A NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID (VERTEBRATA: HETEROSTRACI) FROM POLAND Marek DEC Institute of Palaeobiology, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland; e-mail: [email protected] Dec, M., 2020. A new Middle Devonian (Givetian) psammosteid (Vertebrata: Heterostraci) from Poland. Annales Societatis Geologorum Poloniae, 90: 75 – 93. Abstract: A new genus and species of psammosteid heterostracan, Psarkosteus mediocris gen. et sp. nov., is de- scribed from the Middle Devonian (Givetian) of the Skały Formation, the Holy Cross Mountains, Poland. The dor- sal plate of Psarkosteus is constricted in its anterior part and the postorbital plate is long and narrow. Both features, along with the morphology and variety of tubercles, distinguish it from other representatives of the group. Most distinctive are big, teardrop-shaped tubercles, each with a flat or slightly concave surface and with its tip directed posteriorly, and a crenulated base, located along the branchial plates. The lateral line system in Psarkosteus is similar to that of Drepanaspis gemuendenensis and confirms earlier reconstructions. Key words: Pteraspidomorphi, Heterostraci, Psammosteidae, Middle Devonian, Holy Cross Mountains. Manuscript received 19 February, 2020 accepted 1 June 2020 INTRODUCTION The fossil record of the Heterostraci is poor in Poland, 2017; Glinskiy, 2018). The main problem is concerned although fossils are known from Upper Silurian, Lower with their relationships within the Pteraspidiformes. The and Middle Devonian deposits. From a core sample of the Psammosteidae were supposed to be (1) a sister group to the Upper Silurian (Přidoli) succession in Mielnik a represen- pteraspids s.l., that is Protopteraspididae + Pteraspididae s.l. -
THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
ACTA PALAEONT OLOGICA POLONICA Vol. VII 1 9 6 2 N os. 1-2 L. BEVERLY TARLO THE CLASSIFICATION AND EVOLUTION OF THE HETEROSTRACI Abstract. - An outline classification is given of the Hetero straci, with diagnoses . of th e following orders and suborders: Astraspidiformes, Eriptychiiformes, Cya thaspidiformes (Cyathaspidida, Poraspidida, Ctenaspidida), Psammosteiformes (Tes seraspidida, Psarnmosteida) , Traquairaspidiformes, Pteraspidiformes (Pte ras pidida, Doryaspidida), Cardipeltiformes and Amphiaspidiformes (Amphiaspidida, Hiber naspidida, Eglonaspidida). It is show n that the various orders fall into four m ain evolutionary lineages ~ cyathaspid, psammosteid, pteraspid and amphiaspid, and these are traced from primitive te ssellated forms. A tentative phylogeny is pro posed and alternatives are discussed. INTRODUCTION Since 1858, when Huxley demonstrated that in the histological struc ture of their dermal bone Cephalaspis and Pteraspis were quite different from one another, it has been recognized that there were two distinct groups of ostracoderms for which Lankester (1868-70) proposed the names Osteostraci and Heterostraci respectively. Although these groups are generally considered to be related to on e another, Lankester belie ved that "the Heterostraci are at present associated with the Osteostraci because they are found in the same beds, because they have, like Cepha laspis, a large head shield, and because there is nothing else with which to associate them". In 1889, Cop e united these two groups in the Ostracodermi which, together with the modern cyclostomes, he placed in the Class Agnatha, and although this proposal was at first opposed by Traquair (1899) and Woodward (1891b), subsequent work has shown that it was correct as both the Osteostraci and the Heterostraci were agnathous. -
Proposed Black Country UNESCO Global Geopark
Great things to see and do in the Proposed Black Country UNESCO Global Geopark Black Country UNESCO Global Geopark Project The layers lying above these are grey muddy Welcome to the world-class rocks that contain seams of ironstone, fireclay heritage which is the Black and coal with lots of fossils of plants and insects. These rocks tell us of a time some 310 million Country years ago (called the Carboniferous Period, The Black Country is an amazing place with a named after the carbon in the coal) when the captivating history spanning hundreds of Black Country was covered in huge steamy millions of years. This is a geological and cultural rainforests. undiscovered treasure of the UK, located at the Sitting on top of those we find reddish sandy heart of the country. It is just 30 minutes from rocks containing ancient sand dunes and Birmingham International Airport and 10 minutes pebbly river beds. This tells us that the landscape by train from the city of Birmingham. dried out to become a scorching desolate The Black Country is where many essential desert (this happened about 250 million years aspects of the Industrial Revolution began. It ago and lasted through the Permian and Triassic was the world’s first large scale industrial time periods). landscape where anything could be made, The final chapter in the making of our landscape earning it the nick-name the ‘workshop of the is often called the’ Ice Age’. It spans the last 2.6 world’ during the Industrial Revolution. This million years of our history when vast ice sheets short guidebook introduces some of the sites scraped across the surface of the area, leaving and features that are great things to see and a landscaped sculpted by ice and carved into places to explore across many parts of The the hills and valleys we see today.