The Circulatory System of Galeaspida (Vertebrata; Stem-Gnathostomata)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
New Genus of Eugaleaspidiforms Found in China 15 February 2012
New genus of Eugaleaspidiforms found in China 15 February 2012 The new genus is most suggestive of Eugaleaspis of the Eugaleaspidae by the absence of inner corners, in addition to the diagnostic features of the family, such as only 3 pairs of lateral transverse canals from lateral dorsal canals, and the U-shaped trajectory of median dorsal canals. They differ in that the new genus possesses a pair of posteriorly extending corners, the breadth/length ratio of the shield smaller than 1.1, and the posterior end of median dorsal opening beyond the posterior margin of orbits. Dr. ZHU Min, lead author of the study, and his colleagues reexamined the type specimen of Eugaleaspis xiushanensis from the Wenlock Huixingshao Formation of Chongqing, and observed a pair of posteriorly extending lobate corners and three (instead of four in the original description) pairs of lateral transverse canals. Thus, they re-assigned it to Dunyu. The new species Fig.1: Cephalic shield of Dunyu longiforus gen. et sp. differs from Dunyu xiushanensis in its large nov. ( holotype IVPP V 17681). A. dorsal view; B. ventral cephalic shield which is longer than broad, spine- view; C. close-up view of the left corner; D. close-up shaped corners, anteriorly positioned orbits, the view to show the regional variation of polygonal length ratio between preorbital and postorbital tubercles, and minute spines on the inner surface of the portions of the shield less than 0.75, and large dermal rim encircling the median dorsal opening; E. polygonal, flat-topping tubercles exceeding 2.0 mm illustrative drawing in dorsal view. -
Flow Mechanism and Simulation Approaches for Shale Gas Reservoirs: a Review
Flow Mechanism and Simulation Approaches for Shale Gas Reservoirs: A Review Item Type Article Authors Zhang, Tao; Sun, Shuyu; Song, Hongqing Citation Zhang T, Sun S, Song H (2018) Flow Mechanism and Simulation Approaches for Shale Gas Reservoirs: A Review. Transport in Porous Media. Available: http://dx.doi.org/10.1007/ s11242-018-1148-5. Eprint version Post-print DOI 10.1007/s11242-018-1148-5 Publisher Springer Nature Journal Transport in Porous Media Rights Archived with thanks to Transport in Porous Media Download date 06/10/2021 20:33:37 Link to Item http://hdl.handle.net/10754/629903 Flow mechanism and simulation approaches for shale gas reservoirs: A review Tao Zhang1 Shuyu Sun1∗ Hongqing Song1;2∗ 1Computational Transport Phenomena Laboratory(CTPL), Division of Physical Sciences and Engineering (PSE), King Abdullah University of Science and Technology (KAUST), Thuwal 23955-6900, Kingdom of Saudi Arabia 2 School of civil and resource engineering, University of Science and Technology Beijing, 30 Xueyuan Rd, Beijing 100085, People's Republic of China Abstract The past two decades have borne remarkable progress in our understanding of flow mechanisms and numerical simulation approaches of shale gas reservoir, with much larger the number of publications in recent five years compared to that before year 2012. In this paper, a review is constructed with three parts: flow mecha- nism, reservoir models and numerical approaches. In mechanism, it is found that gas adsorption process can be concluded into different isotherm models for various reservoir basins. Multi-component adsorption mechanism are taken into account in recent years. Flow mechanism and equations vary with different Knudsen number, which could be figured out in two ways: Molecular Dynamics (MD) and Lattice Boltzmann Method (LBM). -
Fossil Jawless Fish from China Foreshadows Early Jawed Vertebrate Anatomy
LETTER doi:10.1038/nature10276 Fossil jawless fish from China foreshadows early jawed vertebrate anatomy Zhikun Gai1,2, Philip C. J. Donoghue1, Min Zhu2, Philippe Janvier3 & Marco Stampanoni4,5 Most living vertebrates are jawed vertebrates (gnathostomes), and The new genus is erected for ‘Sinogaleaspis’ zhejiangensis23,24 Pan, 1986, the living jawless vertebrates (cyclostomes), hagfishes and lampreys, from the Maoshan Formation (late Llandovery epoch to early Wenlock provide scarce information about the profound reorganization of epoch, Silurian period, ,430 million years ago) of Zhejiang, China. the vertebrate skull during the evolutionary origin of jaws1–9. The Diagnosis. Small galeaspid (Supplementary Figs 6 and 7) distinct from extinct bony jawless vertebrates, or ‘ostracoderms’, are regarded as Sinogaleaspis in its terminally positioned nostril, posterior supraorbital precursors of jawed vertebrates and provide insight into this form- sensory canals not converging posteriorly, median dorsal sensory ative episode in vertebrate evolution8–14. Here, using synchrotron canals absent, only one median transverse sensory canal and six pairs radiation X-ray tomography15,16, we describe the cranial anatomy of of lateral transverse sensory canals17,23. galeaspids, a 435–370-million-year-old ‘ostracoderm’ group from Description of cranial anatomy. To elucidate the gross cranial ana- China and Vietnam17. The paired nasal sacs of galeaspids are located tomy of galeaspids, we used synchrotron radiation X-ray tomographic anterolaterally in the braincase, -
The Pharynx of the Stem-Chondrichthyan Ptomacanthus and the Early Evolution of the Gnathostome Gill Skeleton
ARTICLE https://doi.org/10.1038/s41467-019-10032-3 OPEN The pharynx of the stem-chondrichthyan Ptomacanthus and the early evolution of the gnathostome gill skeleton Richard P. Dearden 1, Christopher Stockey1,2 & Martin D. Brazeau1,3 The gill apparatus of gnathostomes (jawed vertebrates) is fundamental to feeding and ventilation and a focal point of classic hypotheses on the origin of jaws and paired appen- 1234567890():,; dages. The gill skeletons of chondrichthyans (sharks, batoids, chimaeras) have often been assumed to reflect ancestral states. However, only a handful of early chondrichthyan gill skeletons are known and palaeontological work is increasingly challenging other pre- supposed shark-like aspects of ancestral gnathostomes. Here we use computed tomography scanning to image the three-dimensionally preserved branchial apparatus in Ptomacanthus,a 415 million year old stem-chondrichthyan. Ptomacanthus had an osteichthyan-like compact pharynx with a bony operculum helping constrain the origin of an elongate elasmobranch-like pharynx to the chondrichthyan stem-group, rather than it representing an ancestral condition of the crown-group. A mixture of chondrichthyan-like and plesiomorphic pharyngeal pat- terning in Ptomacanthus challenges the idea that the ancestral gnathostome pharynx con- formed to a morphologically complete ancestral type. 1 Department of Life Sciences, Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, UK. 2 Centre for Palaeobiology Research, School of Geography, Geology and the Environment, University of Leicester, University Road, Leicester LE1 7RH, UK. 3 Department of Earth Sciences, Natural History Museum, London SW7 5BD, UK. Correspondence and requests for materials should be addressed to M.D.B. -
LETTER Doi:10.1038/Nature13414
LETTER doi:10.1038/nature13414 A primitive fish from the Cambrian of North America Simon Conway Morris1 & Jean-Bernard Caron2,3 Knowledge of the early evolution of fish largely depends on soft- (Extended Data Fig. 4f). Incompleteness precludes a precise estimate of bodied material from the Lower (Series 2) Cambrian period of South size range, but themostcomplete specimens (Fig.1a,b) areabout 60 mm China1,2. Owing to the rarity of some of these forms and a general in length and 8–13 mm in height. Laterally the body is fusiform, widest lack of comparative material from other deposits, interpretations of near the middle, tapering to a fine point posteriorly (Fig. 1a, b and Ex- various features remain controversial3,4, as do their wider relation- tended Data Fig. 4a), whereas in dorsal view the anterior termination is ships amongst post-Cambrian early un-skeletonized jawless verte- rounded (Fig. 1d and Extended Data Fig. 4c–e). The animal was com- brates. Here we redescribe Metaspriggina5 on the basis of new material pressed laterally, as is evident from occasional folding of the body as well from the Burgess Shale and exceptionally preserved material collected as specimensindorso-ventral orientation being conspicuously narrower near Marble Canyon, British Columbia6, and three other Cambrian (Fig. 1a and Extended Data Fig. 5a). Along the anterior ventral margin Burgess Shale-type deposits from Laurentia. This primitive fish dis- there was a keel-like structure (Fig. 1b, g, i, k, l), but no fins have been plays unambiguous vertebrate features: a notochord, a pair of prom- recognized. In the much more abundant specimens of Haikouichthys1,3,4 inent camera-type eyes, paired nasal sacs, possible cranium and arcualia, fins are seldom obvious, suggesting that their absence in Metaspriggina W-shaped myomeres, and a post-anal tail. -
Table of Contents
Table of Contents 5K Fun Run/Walk . 16 Presenter Information Annual Meeting App . 16 Oral Sessions . 17 Author Index . 276 Presentation Uploading . 17 Awards & Fellows . 53 Poster Sessions . 17 Business Center . 16 Registration Center . 17 Career and Membership Center . 21 SASES . 22 CEU Approved Sessions . 34 Schedule by Date . 103 Continuing Education Credits . 16 Schedule by Section/Division . 69 Corporate Member & Exhibitor Lounge . 16 Section/Division Business Meetings . 62 Corporate Member Listing . 41 Section/Community/Division Posters . 18 Dietary Needs . 16 Social Media . 18 Early Career/Professional Development . 23 Society & Other Group Food Functions & Socials . 68 Emergency . 16 Society & Other Group Meetings . 66 Exhibit Hall . 42 Society Awards and Honors . 18 Exhibitor Descriptions & Booth Locations . 43 Society Center . 20 Featured Speakers . 5 Speaker Ready Room . 18 Field of Fun . 16 Sponsors . 14 Food Options . 16 Technical Sessions Future Annual Meeting . 51 Friday–Sunday . 121 Give Back to San Antonio . 16 Monday . 128 Graduate School Forum . 22 Tuesday . 180 Graduate Students . 23 Wednesday . 237 Internet . 17 Ticketed Functions . 15 Lost & Found . 17 Tours . 26 Maps—Session Properties . 7 Trivia Social . 18 Maps—Henry Gonzalez Convention Center (HGCC) . 9 Welcome to San Antonio . 3 Maps—Hilton Palacio del Rio . 10 Welcome Reception . 18 Movie Night . 17 Win $1,000! . 18 News Media . 17 Workshops . 30 Organizer/Moderator Index . 290 How to Use the Program Book • To Browse by Interest (Division/Section/Community) -
J32 the Importance of the Burgess Shale < Soft Bodied Fauna >
580 Chapter j PALEOCONTINENTS The Present is the Key to the Past: HUGH RANCE j32 The importance of the Burgess shale < soft bodied fauna > Only about 33 animal body plans are presently [sic] being used on this planet (Margulis and Schwartz, 1988). —Scott F. Gilbert, Developmental Biology, 1991.1 Almost all animal phyla known today were already present by 505 million years ago— the age of the Burgess shale, Middle Cambrian marine sediments, discovered at the Kicking Horse rim, British Columbia, in 1909 by Charles Doolittle Walcott, that provide a unique window on life without hard parts that had continued to exist shortly after the time of the Cambrian explosion (see Topic j34).2 Legend has it that Walcott, then secretary of the Smithsonian Institution, vacationing near Field, British Columbia, was thrown from a horse carrying him, when it tripped on, and split open a stray fallen slab of shale. Walcott, with his face literally rubbed in it, saw strange, but not hallucinational, forms crisply etched in black against the blue-black bedding surface of the shale: a bonanza of fossils of sea creatures without mineralized shells or backbones. Many are preserved whole; including those with articulated organic (biodegradable) exoskeletons. Details of even their soft body parts can be seen (best using PTM)3 as silvery films (formed of phyllosilicates on a coating of kerogenized carbon) that commonly outline even the most delicate structures on the fossilized animal.4 The Burgess shale is part of the Stephen Formation of greenish shales and thin-bedded limestones, which is a marine-offlap deposit between the thick, massive, carbonates of the overlying Eldon formation, and the underlying Cathedral formation.6 As referenced in the Geological Atlas of the Western Canada Sedimentary Basin - Chapter 8, the Stephen Formation has been “informally divided into a normal, ‘thin Stephen’ on the platform areas and a ‘thick Stephen’ west of the Cathedral Escarpment. -
The Origin of the Vertebrate Jaw: Intersection Between Developmental Biology-Based Model and Fossil Evidence
Review Progress of Projects Supported by NSFC October 2012 Vol.57 No.30: 38193828 Geology doi: 10.1007/s11434-012-5372-z The origin of the vertebrate jaw: Intersection between developmental biology-based model and fossil evidence GAI ZhiKun & ZHU Min* Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China Received May 8, 2012; accepted May 29, 2012; published online August 7, 2012 The origin of the vertebrate jaw has been reviewed based on the molecular, developmental and paleontological evidences. Ad- vances in developmental genetics have accumulated to propose the heterotopy theory of jaw evolution, i.e. the jaw evolved as a novelty through a heterotopic shift of mesenchyme-epithelial interaction. According to this theory, the disassociation of the naso- hypophyseal complex is a fundamental prerequisite for the origin of the jaw, since the median position of the nasohypophyseal placode in cyclostome head development precludes the forward growth of the neural-crest-derived craniofacial ectomesenchyme. The potential impacts of this disassociation on the origin of the diplorhiny are also discussed from the molecular perspectives. Thus far, our study on the cranial anatomy of galeaspids, a 435–370-million-year-old ‘ostracoderm’ group from China and north- ern Vietnam, has provided the earliest fossil evidence for the disassociation of nasohypophyseal complex in vertebrate phylogeny. Using Synchrotron Radiation X-ray Tomography, we further show some derivative structures of the trabeculae (e.g. orbitonasal lamina, ethmoid plate) in jawless galeaspids, which provide new insights into the reorganization of the vertebrate head before the evolutionary origin of the jaw. -
A Paleontological Perspective of Vertebrate Origin
http://www.paper.edu.cn Chinese Science Bulletin 2003 Vol. 48 No. 8 725-735 Cover: The earliest-known and most primitive vertebrates on the A paleontological perspective Earth---Myllokunmingia fengjiaoa , (upper) Zhongjianichthys rostratus of vertebrate origin ( middle ), Haikouichthys ercaicunensis (lower left and lower right). They were SHU Degan Early Life Institute & Department of Geology, Northwest products of the early Cambrian Explosion, University, Xi’an, 710069, China; School of Earth excavated from the famous Chengjiang Sciences and Resources, China University of Geosciences, Beijing, 100083, China Lagersttat, which was formed in the (e-mail:[email protected]) eastern Yunnan about 530 millions of years ago. These ancestral vertebrates not only Abstract The Early Cambrian Haikouichthys and Haikouella have been claimed to be related to contribute in an important developed primitive separate vertebral way to our understanding of vertebrate origin, but there have elements, but also possessed principal been heated debates about how exactly they are to be interpreted. New discoveries of numerous specimens of sensory organs, including a pair of large Haikouichthys not only confirm the identity of previously lateral eyes, nostril with nasal sacs, then described structures such as the dorsal and the ventral fins, and chevron-shaped myomeres, but also reveal many new had led to the transition from acraniates to important characteristics, including sensory organs of the head craniates (true vertebrates). The (e.g. large eyes), and a prominent notochord with differentiated vertebral elements. This “first fish” appears, discoveries of these “naked” agnathans however, to retain primitive reproductive features of have pushed the earliest record of acraniates, suggesting that it is a stem-group craniates. -
Synchrotron-Aided Reconstruction of the Conodont Feeding Apparatus and Implications for the Mouth of the first Vertebrates
Synchrotron-aided reconstruction of the conodont feeding apparatus and implications for the mouth of the first vertebrates Nicolas Goudemanda,1, Michael J. Orchardb, Séverine Urdya, Hugo Buchera, and Paul Tafforeauc aPalaeontological Institute and Museum, University of Zurich, CH-8006 Zürich, Switzerland; bGeological Survey of Canada, Vancouver, BC, Canada V6B 5J3; and cEuropean Synchrotron Radiation Facility, 38043 Grenoble Cedex, France Edited* by A. M. Celâl Sxengör, Istanbul Technical University, Istanbul, Turkey, and approved April 14, 2011 (received for review February 1, 2011) The origin of jaws remains largely an enigma that is best addressed siderations. Despite the absence of any preserved traces of oral by studying fossil and living jawless vertebrates. Conodonts were cartilages in the rare specimens of conodonts with partly pre- eel-shaped jawless animals, whose vertebrate affinity is still dis- served soft tissue (10), we show that partial reconstruction of the puted. The geometrical analysis of exceptional three-dimensionally conodont mouth is possible through biomechanical analysis. preserved clusters of oro-pharyngeal elements of the Early Triassic Novispathodus, imaged using propagation phase-contrast X-ray Results synchrotron microtomography, suggests the presence of a pul- We recently discovered several fused clusters (rare occurrences ley-shaped lingual cartilage similar to that of extant cyclostomes of exceptional preservation where several elements of the same within the feeding apparatus of euconodonts (“true” conodonts). animal were diagenetically cemented together) of the Early This would lend strong support to their interpretation as verte- Triassic conodont Novispathodus (11). One of these specimens brates and demonstrates that the presence of such cartilage is a (Fig. 2A), found in lowermost Spathian rocks of the Tsoteng plesiomorphic condition of crown vertebrates. -
The Nearshore Cradle of Early Vertebrate Diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Birmingham Research Portal The nearshore cradle of early vertebrate diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan DOI: 10.1126/science.aar3689 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Sallan, L, Friedman, M, Sansom, R, Bird, C & Sansom, I 2018, 'The nearshore cradle of early vertebrate diversification', Science, vol. 362, no. 6413, pp. 460-464. https://doi.org/10.1126/science.aar3689 Link to publication on Research at Birmingham portal Publisher Rights Statement: This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on 26th October 2018. DOI: 10.1126/science.aar3689 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. -
The Cambrian ''Explosion'
Perspective The Cambrian ‘‘explosion’’: Slow-fuse or megatonnage? Simon Conway Morris* Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom Clearly, the fossil record from the Cambrian period is an invaluable tool for deciphering animal evolution. Less clear, however, is how to integrate the paleontological information with molecular phylogeny and developmental biology data. Equally challenging is answering why the Cambrian period provided such a rich interval for the redeployment of genes that led to more complex bodyplans. illiam Buckland knew about it, The First Metazoans. Ediacaran assem- 1). The overall framework of early meta- WCharles Darwin characteristically blages (2, 5) are presumably integral to zoan evolution comes from molecular agonized over it, and still we do not fully understanding the roots of the Cambrian data, but they cannot provide insights into understand it. ‘‘It,’’ of course, is the seem- ‘‘explosion,’’ and this approach assumes the anatomical changes and associated ingly abrupt appearance of animals in the that the fossil record is historically valid. It changes in ecology that accompanied the Cambrian ‘‘explosion.’’ The crux of this is markedly at odds, however, with an emergence of bodyplans during the Cam- evolutionary problem can be posed as a alternative view, based on molecular data. brian explosion. The fossil record series of interrelated questions. Is it a real These posit metazoan divergences hun- provides, therefore, a unique historical event or simply an artifact of changing dreds of millions of years earlier (6, 7). As perspective. fossilization potential? If the former, how such, the origination of animals would be Only those aspects of the Ediacaran rapidly did it happen and what are its more or less coincident with the postu- record relevant to the Cambrian diversi- consequences for understanding evolu- lated ‘‘Big Bang’’ of eukaryote diversifi- fication are noted here.