Allometric Growth in the Extant Coelacanth Lung During Ontogenetic Development
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Benthic Foraminifera Across the Cretaceous/Paleogene Boundary in the Southern Ocean (ODP Site 690): Diversity, Food and Carbonate Saturation
Marine Micropaleontology 105 (2013) 40–51 Contents lists available at ScienceDirect Marine Micropaleontology journal homepage: www.elsevier.com/locate/marmicro Research paper Benthic foraminifera across the Cretaceous/Paleogene boundary in the Southern Ocean (ODP Site 690): Diversity, food and carbonate saturation Laia Alegret a,⁎, Ellen Thomas b,c a Departamento de Ciencias de la Tierra & Instituto Universitario de Investigación en Ciencias Ambientales de Aragón, Universidad de Zaragoza, Spain b Department of Geology and Geophysics, Yale University, USA c Department of Earth and Environmental Sciences, Wesleyan University, USA article info abstract Article history: The impact of an asteroid at the Cretaceous/Paleogene (K/Pg) boundary triggered dramatic biotic, biogeochem- Received 20 June 2013 ical and sedimentological changes in the oceans that have been intensively studied. Paleo-biogeographical Received in revised form 21 October 2013 differences in the biotic response to the impact and its environmental consequences, however, have been less Accepted 24 October 2013 well documented. We present a high-resolution analysis of benthic foraminiferal assemblages at Southern Ocean ODP Site 690 (Maud Rise, Weddell Sea, Antarctica). Keywords: At this high latitude site, late Maastrichtian environmental variability was high, but benthic foraminiferal assem- Cretaceous/Paleogene boundary fi benthic foraminifera blages were not less diverse than at lower latitudes, in contrast to those of planktic calci ers. Also in contrast to high southern latitudes planktic calcifiers, benthic foraminifera did not suffer significant extinction at the K/Pg boundary, but show export productivity transient assemblage changes and decreased diversity. At Site 690, the extinction rate was even lower (~3%) carbonate saturation than at other sites. -
From the Crato Formation (Lower Cretaceous)
ORYCTOS.Vol. 3 : 3 - 8. Décembre2000 FIRSTRECORD OT CALAMOPLEU RUS (ACTINOPTERYGII:HALECOMORPHI: AMIIDAE) FROMTHE CRATO FORMATION (LOWER CRETACEOUS) OF NORTH-EAST BRAZTL David M. MARTILL' and Paulo M. BRITO'z 'School of Earth, Environmentaland PhysicalSciences, University of Portsmouth,Portsmouth, POl 3QL UK. 2Departmentode Biologia Animal e Vegetal,Universidade do Estadode Rio de Janeiro, rua SâoFrancisco Xavier 524. Rio de Janeiro.Brazll. Abstract : A partial skeleton representsthe first occurrenceof the amiid (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus from the Nova Olinda Member of the Crato Formation (Aptian) of north east Brazil. The new spe- cimen is further evidencethat the Crato Formation ichthyofauna is similar to that of the slightly younger Romualdo Member of the Santana Formation of the same sedimentary basin. The extended temporal range, ?Aptian to ?Cenomanian,for this genus rules out its usefulnessas a biostratigraphic indicator for the Araripe Basin. Key words: Amiidae, Calamopleurus,Early Cretaceous,Brazil Première mention de Calamopleurus (Actinopterygii: Halecomorphi: Amiidae) dans la Formation Crato (Crétacé inférieur), nord est du Brésil Résumé : la première mention dans le Membre Nova Olinda de la Formation Crato (Aptien ; nord-est du Brésil) de I'amiidé (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus est basée sur la découverted'un squelettepar- tiel. Le nouveau spécimen est un élément supplémentaireindiquant que I'ichtyofaune de la Formation Crato est similaire à celle du Membre Romualdo de la Formation Santana, située dans le même bassin sédimentaire. L'extension temporelle de ce genre (?Aptien à ?Cénomanien)ne permet pas de le considérer comme un indicateur biostratigraphiquepour le bassin de l'Araripe. Mots clés : Amiidae, Calamopleurus, Crétacé inférieu4 Brésil INTRODUCTION Araripina and at Mina Pedra Branca, near Nova Olinda where cf. -
A Framework for Post-Phylogenetic Systematics
A FRAMEWORK FOR POST-PHYLOGENETIC SYSTEMATICS Richard H. Zander Zetetic Publications, St. Louis Richard H. Zander Missouri Botanical Garden P.O. Box 299 St. Louis, MO 63166 [email protected] Zetetic Publications in St. Louis produces but does not sell this book. Any book dealer can obtain a copy for you through the usual channels. Resellers please contact CreateSpace Independent Publishing Platform of Amazon. ISBN-13: 978-1492220404 ISBN-10: 149222040X © Copyright 2013, all rights reserved. The image on the cover and title page is a stylized dendrogram of paraphyly (see Plate 1.1). This is, in macroevolutionary terms, an ancestral taxon of two (or more) species or of molecular strains of one taxon giving rise to a descendant taxon (unconnected comma) from one ancestral branch. The image on the back cover is a stylized dendrogram of two, genus-level speciational bursts or dis- silience. Here, the dissilient genus is the basic evolutionary unit (see Plate 13.1). This evolutionary model is evident in analysis of the moss Didymodon (Chapter 8) through superoptimization. A super- generative core species with a set of radiative, specialized descendant species in the stylized tree com- promises one genus. In this exemplary image; another genus of similar complexity is generated by the core supergenerative species of the first. TABLE OF CONTENTS Preface..................................................................................................................................................... 1 Acknowledgments.................................................................................................................................. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
(Early Cretaceous, Araripe Basin, Northeastern Brazil): Stratigraphic, Palaeoenvironmental and Palaeoecological Implications
Palaeogeography, Palaeoclimatology, Palaeoecology 218 (2005) 145–160 www.elsevier.com/locate/palaeo Controlled excavations in the Romualdo Member of the Santana Formation (Early Cretaceous, Araripe Basin, northeastern Brazil): stratigraphic, palaeoenvironmental and palaeoecological implications Emmanuel Faraa,*, Antoˆnio A´ .F. Saraivab, Dio´genes de Almeida Camposc, Joa˜o K.R. Moreirab, Daniele de Carvalho Siebrab, Alexander W.A. Kellnerd aLaboratoire de Ge´obiologie, Biochronologie, et Pale´ontologie humaine (UMR 6046 du CNRS), Universite´ de Poitiers, 86022 Poitiers cedex, France bDepartamento de Cieˆncias Fı´sicas e Biologicas, Universidade Regional do Cariri - URCA, Crato, Ceara´, Brazil cDepartamento Nacional de Produc¸a˜o Mineral, Rio de Janeiro, RJ, Brazil dDepartamento de Geologia e Paleontologia, Museu Nacional/UFRJ, Rio de Janeiro, RJ, Brazil Received 23 August 2004; received in revised form 10 December 2004; accepted 17 December 2004 Abstract The Romualdo Member of the Santana Formation (Araripe Basin, northeastern Brazil) is famous for the abundance and the exceptional preservation of the fossils found in its early diagenetic carbonate concretions. However, a vast majority of these Early Cretaceous fossils lack precise geographical and stratigraphic data. The absence of such contextual proxies hinders our understanding of the apparent variations in faunal composition and abundance patterns across the Araripe Basin. We conducted controlled excavations in the Romualdo Member in order to provide a detailed account of its main stratigraphic, sedimentological and palaeontological features near Santana do Cariri, Ceara´ State. We provide the first fine-scale stratigraphic sequence ever established for the Romualdo Member and we distinguish at least seven concretion-bearing horizons. Notably, a 60-cm-thick group of layers (bMatraca˜oQ), located in the middle part of the member, is virtually barren of fossiliferous concretions. -
Giant Fossil Coelacanths from the Late Cretaceous of the Eastern
^rfij^i^v^^™, - » v ' - - 4 j/ N ^P"" ,- V ^™ V- -*^ >•;:-* ' ^ * -r;' David R. Schwimmer, Geologist, Columbus State University Introduction In Autumn, 1987, a sizeable mass of fossil bone was discovered by amateur collectors in the bed of a small creek in eastern Alabama. The bone-bearing rock, some 300 kg in weight, was collected by a party led by G. Dent Williams and transferred to the paleontology laboratory at Columbus State University. Williams prepared most of the material using air percussion tools, and I further cleared some bones with acetic acid. A mandible (lower jaw bone) of 502 mm length was the first bone prepared from the material. It strangely lacked evidence of both teeth and tooth sockets, and it was covered medially with coarse denticulation resembling #40 grit sandpaper. The jawbone conformed with no recognizable North American Late Cretaceous fish or four-legged animal, and, given the large size of the mandible, my initial search for an identification ranged from ankylosaurid dinosaurs, to mosasaurs, to the larger contemporary fish, such as Xiphactinus. Nothing known in the Late Cretaceous of North America matched the mandible nor any other bone which was subsequently prepared from this matrix. J.D. Stewart of the L.A. County Museum was prior fossil record of a North American coelacanth is concurrently studying fossils of small marine Diplurus newarki, from freshwater deposits of earliest coelacanths from the Late Cretaceous of western Kansas, Jurassic age (ca. 205 Myr.: Schaeffer, 1941, 1952). USA (which were also a new discovery at the time: see Forey (1981) and Maisey (1991) recognized two sub- Stewart et al., 1991). -
I Ecomorphological Change in Lobe-Finned Fishes (Sarcopterygii
Ecomorphological change in lobe-finned fishes (Sarcopterygii): disparity and rates by Bryan H. Juarez A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science (Ecology and Evolutionary Biology) in the University of Michigan 2015 Master’s Thesis Committee: Assistant Professor Lauren C. Sallan, University of Pennsylvania, Co-Chair Assistant Professor Daniel L. Rabosky, Co-Chair Associate Research Scientist Miriam L. Zelditch i © Bryan H. Juarez 2015 ii ACKNOWLEDGEMENTS I would like to thank the Rabosky Lab, David W. Bapst, Graeme T. Lloyd and Zerina Johanson for helpful discussions on methodology, Lauren C. Sallan, Miriam L. Zelditch and Daniel L. Rabosky for their dedicated guidance on this study and the London Natural History Museum for courteously providing me with access to specimens. iii TABLE OF CONTENTS ACKNOWLEDGEMENTS ii LIST OF FIGURES iv LIST OF APPENDICES v ABSTRACT vi SECTION I. Introduction 1 II. Methods 4 III. Results 9 IV. Discussion 16 V. Conclusion 20 VI. Future Directions 21 APPENDICES 23 REFERENCES 62 iv LIST OF TABLES AND FIGURES TABLE/FIGURE II. Cranial PC-reduced data 6 II. Post-cranial PC-reduced data 6 III. PC1 and PC2 Cranial and Post-cranial Morphospaces 11-12 III. Cranial Disparity Through Time 13 III. Post-cranial Disparity Through Time 14 III. Cranial/Post-cranial Disparity Through Time 15 v LIST OF APPENDICES APPENDIX A. Aquatic and Semi-aquatic Lobe-fins 24 B. Species Used In Analysis 34 C. Cranial and Post-Cranial Landmarks 37 D. PC3 and PC4 Cranial and Post-cranial Morphospaces 38 E. PC1 PC2 Cranial Morphospaces 39 1-2. -
Giant Mesozoic Coelacanths (Osteichthyes, Actinistia) Reveal High Body Size Disparity Decoupled from Taxic Diversity
Giant Mesozoic Coelacanths (Osteichthyes, Actinistia) Reveal High Body Size Disparity Decoupled From Taxic Diversity Lionel Cavin ( [email protected] ) Natural History Museum of Geneva André Piuz Natural History Museum of Geneva Christophe Ferrante Natural History Museum of Geneva Guillaume Guinot Institut des Sciences de l'Evolution de Montpellier Research Article Keywords: morphological evolution, taxic diversication, Genomic and physiological characteristics Posted Date: March 2nd, 2021 DOI: https://doi.org/10.21203/rs.3.rs-245480/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 2 Giant Mesozoic coelacanths (Osteichthyes, Actinistia) reveal high 3 body size disparity decoupled from taxic diversity 4 5 Lionel Cavin1*, André Piuz1, Christophe Ferrante1,2 & Guillaume Guinot3 6 7 8 1 Department of Geology and Palaeontology, Natural History Museum of Geneva, Geneva, 9 Switzerland 10 2 Department of Earth Sciences, University of Geneva, Rue des Maraîchais 13, 1205 Genève, 11 Switzerland 12 3 Institut des Sciences de l’Evolution de Montpellier (Université de Montpellier, CNRS, IRD, 13 EPHE), Montpellier, France 14 15 * Corresponding author 16 Email: [email protected] 17 1 18 Abstract 19 20 The positive correlation between speciation rates and morphological evolution expressed by 21 body size is a macroevolutionary trait of vertebrates. Although taxic diversification and 22 morphological evolution are slow in coelacanths, their fossil record indicates that large and 23 small species coexisted, which calls into question the link between morphological and body 24 size disparities. Here, we describe and reassess fossils of giant coelacanths. Two genera 25 reached up to 5 meters long, placing them among the ten largest bony fish that ever lived. -
World Atlas of Biodiversity
WORLD ATLAS OF BIODIVERSITY EARTH'S LIVING RESOURCES IN THE 21st CENTURY ^ > (\ X >r BRIAN GROOMBRIDGE and MARTIN D. JENKINS UNEP WCMC World Atlas of Biodiversity addresses the remark- ible growth in concern at all levels for living things and the environment and the increased appreciation ' the links between the state of ecosystems and the state of humankind. Building on a wealth of re- search and analysis by the conservation community worldwide, this book provides a comprehensive and accessible view of key global issues in biodiver- sity. It outlines some of the broad ecological relationships between humans and the rest of the iterial world and summarizes information on the health of the planet. Opening with an outline of some fundamental aspects of material cycles and energy flow in the biosphere, the book goes on to discuss the expansion of this diversity through geo- logical time and the pattern of its distribution over the surface of the Earth, and analyzes trends in the condition of the main ecosystem types and the species integral to them. Digitized by tine Internet Arciiive in 2010 witii funding from UNEP-WCIVIC, Cambridge Iittp://www.arcliive.org/details/worldatlasofbiod02groo World Atlas of Biodiversity Published in association witli Ihe contents of this volume do not UNEP-WCMC by the University of necessarily reflect the views or policies of California Press UNEP-WCfvIC, contributory organizations, University of California Press editors or publishers. The designations Berl<eley and Los Angeles, California employed and the presentations do not imply University of California Press, Ltd. the expression of any opinion whatsoever on London, England the part of UNEP-WCIvIC or contributory organizations, editors or publishers © 2002 UNEP World Conservation concerning the legal status of any country, Monitoring Centre territory, city or area or its authority, or UNEP-WCMC concerning the delimitation of its frontiers or 219 Huntingdon Road boundaries or the designation of its name or Cambridge CB3 DDL, UK allegiances. -
New Coelacanth Material from the Middle Triassic of Eastern Switzerland, and Comments on the Taxic Diversity of Actinistans
Swiss J Geosci (2013) 106:161–177 DOI 10.1007/s00015-013-0143-7 New coelacanth material from the Middle Triassic of eastern Switzerland, and comments on the taxic diversity of actinistans Lionel Cavin • Heinz Furrer • Christian Obrist Received: 1 February 2013 / Accepted: 9 August 2013 / Published online: 16 November 2013 Ó Swiss Geological Society 2013 Abstract New coelacanth material from the Middle Tri- preserved on the holotype and allows the addition of new assic Prosanto Formation of the Ducan and Landwasser characters to a previously published data matrix of acti- area near Davos in eastern Switzerland, Canton Graubu¨n- nistians. A phylogenetic analysis is performed, which den, is described. A sub-complete individual is visible in supports that Ticinepomis is nested among the Latimeri- ventral view, and shows details of its branchial apparatus. idae. The diversity of post-Palaeozoic coelacanths is In particular, it possesses relatively large teeth on the assessed. The taxic diversity of observed occurrences ceratobranchials, and possible ossified hypobranchials. shows a peak in the Early Triassic and a peak in the Late Few diagnostic characters are observable, and most of them Jurassic, as detected in previous studies. When ghost lin- are visible on the mandibles preserved in lateral view. This eages are included in the computation, the Late Jurassic specimen shares characters with Ticinepomis peyeri,a peak is smoothened. By comparing the taxic diversity smaller form from the Middle Triassic of Monte San curves with the curve of average ghost lineage duration, we Giorgio, whose holotype is re-described in part here. A conclude that the Early Triassic peak of diversity was second specimen, a fragmentary caudal skeleton shows the probably caused by a biological radiation, whereas the Late typical supplementary lobe of coelacanths, and meristic Jurassic peak of observed diversity is probably the result of characters indicating probable close affinities with T. -
Fossils Provide Better Estimates of Ancestral Body Size Than Do Extant
Acta Zoologica (Stockholm) 90 (Suppl. 1): 357–384 (January 2009) doi: 10.1111/j.1463-6395.2008.00364.x FossilsBlackwell Publishing Ltd provide better estimates of ancestral body size than do extant taxa in fishes James S. Albert,1 Derek M. Johnson1 and Jason H. Knouft2 Abstract 1Department of Biology, University of Albert, J.S., Johnson, D.M. and Knouft, J.H. 2009. Fossils provide better Louisiana at Lafayette, Lafayette, LA estimates of ancestral body size than do extant taxa in fishes. — Acta Zoologica 2 70504-2451, USA; Department of (Stockholm) 90 (Suppl. 1): 357–384 Biology, Saint Louis University, St. Louis, MO, USA The use of fossils in studies of character evolution is an active area of research. Characters from fossils have been viewed as less informative or more subjective Keywords: than comparable information from extant taxa. However, fossils are often the continuous trait evolution, character state only known representatives of many higher taxa, including some of the earliest optimization, morphological diversification, forms, and have been important in determining character polarity and filling vertebrate taphonomy morphological gaps. Here we evaluate the influence of fossils on the interpretation of character evolution by comparing estimates of ancestral body Accepted for publication: 22 July 2008 size in fishes (non-tetrapod craniates) from two large and previously unpublished datasets; a palaeontological dataset representing all principal clades from throughout the Phanerozoic, and a macroecological dataset for all 515 families of living (Recent) fishes. Ancestral size was estimated from phylogenetically based (i.e. parsimony) optimization methods. Ancestral size estimates obtained from analysis of extant fish families are five to eight times larger than estimates using fossil members of the same higher taxa. -
THE LAZARUS AMMONOID FAMILY GONIATITIDAE, the TETRANGULARLY COILED ENTOGONITIDAE, and MISSISSIPPIAN BIOGEOGRAPHY Author(S): DIETER KORN, CHRISTIAN KLUG, ROYAL H
THE LAZARUS AMMONOID FAMILY GONIATITIDAE, THE TETRANGULARLY COILED ENTOGONITIDAE, AND MISSISSIPPIAN BIOGEOGRAPHY Author(s): DIETER KORN, CHRISTIAN KLUG, ROYAL H. MAPES Source: Journal of Paleontology, 79(2):356-365. Published By: The Paleontological Society DOI: http://dx.doi.org/10.1666/0022-3360(2005)079<0356:TLAFGT>2.0.CO;2 URL: http://www.bioone.org/doi/full/10.1666/0022-3360%282005%29079%3C0356%3ATLAFGT %3E2.0.CO%3B2 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. J. Paleont., 79(2), 2005, pp. 356±365 Copyright q 2005, The Paleontological Society 0022-3360/05/0079-356$03.00 THE LAZARUS AMMONOID FAMILY GONIATITIDAE, THE TETRANGULARLY COILED ENTOGONITIDAE, AND MISSISSIPPIAN BIOGEOGRAPHY DIETER KORN,1 CHRISTIAN KLUG,2 AND ROYAL H. MAPES3 1Museum fuÈr Naturkunde der Humboldt-UniversitaÈt zu Berlin, Invalidenstraûe 43, D-10115 Berlin, Germany, ,[email protected]., 2PalaÈontologisches Institut und Museum, UniversitaÈt ZuÈrich, Karl-Schmid-Str.