A Fish and Tetrapod Fauna from Romer's Gap Preserved In
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Plant Macrofossil Evidence for an Early Onset of the Holocene Summer Thermal Maximum in Northernmost Europe
ARTICLE Received 19 Aug 2014 | Accepted 27 Feb 2015 | Published 10 Apr 2015 DOI: 10.1038/ncomms7809 OPEN Plant macrofossil evidence for an early onset of the Holocene summer thermal maximum in northernmost Europe M. Va¨liranta1, J.S. Salonen2, M. Heikkila¨1, L. Amon3, K. Helmens4, A. Klimaschewski5, P. Kuhry4, S. Kultti2, A. Poska3,6, S. Shala4, S. Veski3 & H.H. Birks7 Holocene summer temperature reconstructions from northern Europe based on sedimentary pollen records suggest an onset of peak summer warmth around 9,000 years ago. However, pollen-based temperature reconstructions are largely driven by changes in the proportions of tree taxa, and thus the early-Holocene warming signal may be delayed due to the geographical disequilibrium between climate and tree populations. Here we show that quantitative summer-temperature estimates in northern Europe based on macrofossils of aquatic plants are in many cases ca.2°C warmer in the early Holocene (11,700–7,500 years ago) than reconstructions based on pollen data. When the lag in potential tree establishment becomes imperceptible in the mid-Holocene (7,500 years ago), the reconstructed temperatures converge at all study sites. We demonstrate that aquatic plant macrofossil records can provide additional and informative insights into early-Holocene temperature evolution in northernmost Europe and suggest further validation of early post-glacial climate development based on multi-proxy data syntheses. 1 Department of Environmental Sciences, ECRU, University of Helsinki, P.O. Box 65, Helsinki FI-00014, Finland. 2 Department of Geosciences and Geography, University of Helsinki, P.O. Box 65, Helsinki FI-00014, Finland. -
Your Inner Fish
CHAPTER THREE HANDY GENES While my colleagues and I were digging up the first Tiktaalik in the Arctic in July 2004, Randy Dahn, a researcher in my laboratory, was sweating it out on the South Side of Chicago doing genetic experiments on the embryos of sharks and skates, cousins of stingrays. You’ve probably seen small black egg cases, known as mermaid’s purses, on the beach. Inside the purse once lay an egg with yolk, which developed into an embryonic skate or ray. Over the years, Randy has spent hundreds of hours experimenting with the embryos inside these egg cases, often working well past midnight. During the fateful summer of 2004, Randy was taking these cases and injecting a molecular version of vitamin A into the eggs. After that he would let the eggs develop for several months until they hatched. His experiments may seem to be a bizarre way to spend the better part of a year, let alone for a young scientist to launch a promising scientific career. Why sharks? Why a form of vitamin A? 61 To make sense of these experiments, we need to step back and look at what we hope they might explain. What we are really getting at in this chapter is the recipe, written in our DNA, that builds our bodies from a single egg. When sperm fertilizes an egg, that fertilized egg does not contain a tiny hand, for instance. The hand is built from the information contained in that single cell. This takes us to a very profound problem. -
Standard Procedures for the Assessment and Mitigation of Adverse Impacts to Paleontological Resources
Standard Procedures for the Assessment and Mitigation of Adverse Impacts to Paleontological Resources Society of Vertebrate Paleontology Impact Mitigation Guidelines Revision Committee Abstract Fossils are nonrenewable paleontological resources that are subject to impacts from land development. Procedures are presented for evaluating the potential for impacts of a proposed action on paleontological resources and for mitigating those impacts. Impact mitigation includes pre-project survey and salvage, monitoring and screen washing during excavation to salvage fossils, conservation and inventory, and final reports and specimen curation. The objective of these procedures is to offer standard methods for assessing potential impacts to fossils and mitigating these impacts. Introduction Fossils are nonrenewable paleontological resources that are afforded protection by federal, state, and local environmental laws and regulations. The Paleontological Resources Preservation Act (PRPA) of 2009 calls for uniform policies and standards that apply to fossils on all federal public lands. All federal land management agencies are required to develop regulations that satisfy the stipulations of the PRPA. Section 6302 of the PRPA mandates that federal agencies "shall manage and protect paleontological resources on Federal land using scientific principles and expertise." Thus, federal agencies need the help of the professional paleontological community in the formulation and implementation of these PRPA- mandated policies and regulations. The potential for destruction or degradation of paleontological resources on both public and private lands selected for development under the jurisdiction of various governmental planning agencies is recognized. The standard procedures below are intended to be applicable to both private and public lands under the jurisdiction of local, city, county, regional, state, and federal agencies. -
Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)
ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2011.01460.x IDENTIFYING HETEROGENEITY IN RATES OF MORPHOLOGICAL EVOLUTION: DISCRETE CHARACTER CHANGE IN THE EVOLUTION OF LUNGFISH (SARCOPTERYGII; DIPNOI) Graeme T. Lloyd,1,2 Steve C. Wang,3 and Stephen L. Brusatte4,5 1Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 2E-mail: [email protected] 3Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 5Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025 Received February 9, 2010 Accepted August 15, 2011 Data Archived: Dryad: doi:10.5061/dryad.pg46f Quantifying rates of morphological evolution is important in many macroevolutionary studies, and critical when assessing possible adaptive radiations and episodes of punctuated equilibrium in the fossil record. However, studies of morphological rates of change have lagged behind those on taxonomic diversification, and most authors have focused on continuous characters and quantifying patterns of morphological rates over time. Here, we provide a phylogenetic approach, using discrete characters and three statistical tests to determine points on a cladogram (branches or entire clades) that are characterized by significantly high or low rates of change. These methods include a randomization approach that identifies branches with significantly high rates and likelihood ratio tests that pinpoint either branches or clades that have significantly higher or lower rates than the pooled rate of the remainder of the tree. As a test case for these methods, we analyze a discrete character dataset of lungfish, which have long been regarded as “living fossils” due to an apparent slowdown in rates since the Devonian. -
Review and Meta-Analysis of the Environmental Biology and Potential Invasiveness of a Poorly-Studied Cyprinid, the Ide Leuciscus Idus
REVIEWS IN FISHERIES SCIENCE & AQUACULTURE https://doi.org/10.1080/23308249.2020.1822280 REVIEW Review and Meta-Analysis of the Environmental Biology and Potential Invasiveness of a Poorly-Studied Cyprinid, the Ide Leuciscus idus Mehis Rohtlaa,b, Lorenzo Vilizzic, Vladimır Kovacd, David Almeidae, Bernice Brewsterf, J. Robert Brittong, Łukasz Głowackic, Michael J. Godardh,i, Ruth Kirkf, Sarah Nienhuisj, Karin H. Olssonh,k, Jan Simonsenl, Michał E. Skora m, Saulius Stakenas_ n, Ali Serhan Tarkanc,o, Nildeniz Topo, Hugo Verreyckenp, Grzegorz ZieRbac, and Gordon H. Coppc,h,q aEstonian Marine Institute, University of Tartu, Tartu, Estonia; bInstitute of Marine Research, Austevoll Research Station, Storebø, Norway; cDepartment of Ecology and Vertebrate Zoology, Faculty of Biology and Environmental Protection, University of Lodz, Łod z, Poland; dDepartment of Ecology, Faculty of Natural Sciences, Comenius University, Bratislava, Slovakia; eDepartment of Basic Medical Sciences, USP-CEU University, Madrid, Spain; fMolecular Parasitology Laboratory, School of Life Sciences, Pharmacy and Chemistry, Kingston University, Kingston-upon-Thames, Surrey, UK; gDepartment of Life and Environmental Sciences, Bournemouth University, Dorset, UK; hCentre for Environment, Fisheries & Aquaculture Science, Lowestoft, Suffolk, UK; iAECOM, Kitchener, Ontario, Canada; jOntario Ministry of Natural Resources and Forestry, Peterborough, Ontario, Canada; kDepartment of Zoology, Tel Aviv University and Inter-University Institute for Marine Sciences in Eilat, Tel Aviv, -
Climate Instability and Tipping Points in the Late Devonian
Archived version from NCDOCKS Institutional Repository – http://libres.uncg.edu/ir/asu/ Sarah K. Carmichael, Johnny A. Waters, Cameron J. Batchelor, Drew M. Coleman, Thomas J. Suttner, Erika Kido, L.M. Moore, and Leona Chadimová, (2015) Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt, Gondwana Research The copy of record is available from Elsevier (18 March 2015), ISSN 1342-937X, http://dx.doi.org/10.1016/j.gr.2015.02.009. Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt Sarah K. Carmichael a,*, Johnny A. Waters a, Cameron J. Batchelor a, Drew M. Coleman b, Thomas J. Suttner c, Erika Kido c, L. McCain Moore a, and Leona Chadimová d Article history: a Department of Geology, Appalachian State University, Boone, NC 28608, USA Received 31 October 2014 b Department of Geological Sciences, University of North Carolina - Chapel Hill, Received in revised form 6 Feb 2015 Chapel Hill, NC 27599-3315, USA Accepted 13 February 2015 Handling Editor: W.J. Xiao c Karl-Franzens-University of Graz, Institute for Earth Sciences (Geology & Paleontology), Heinrichstrasse 26, A-8010 Graz, Austria Keywords: d Institute of Geology ASCR, v.v.i., Rozvojova 269, 165 00 Prague 6, Czech Republic Devonian–Carboniferous Chemostratigraphy Central Asian Orogenic Belt * Corresponding author at: ASU Box 32067, Appalachian State University, Boone, NC 28608, USA. West Junggar Tel.: +1 828 262 8471. E-mail address: [email protected] (S.K. -
Pterosaurs Flight in the Age of Dinosaurs Now Open 2 News at the Museum 3
Member Magazine Spring 2014 Vol. 39 No. 2 Pterosaurs Flight in the Age of Dinosaurs now open 2 News at the Museum 3 From the After an unseasonably cold, snowy winter, will work to identify items from your collection, More than 540,000 Marine Fossils the Museum is pleased to offer a number of while also displaying intriguing specimens from President springtime opportunities to awaken the inner the Museum’s own world-renowned collections. Added to Paleontology Collection naturalist in us all. This is the time of year when Of course, fieldwork and collecting have Ellen V. Futter Museum scientists prepare for the summer been hallmarks of the Museum’s work since Collections at a Glance field season as they continue to pursue new the institution’s founding. What has changed, discoveries in their fields. It’s also when Museum however, is technology. With a nod to the many Over nearly 150 years of acquisitions and Members and visitors can learn about their ways that technology is amplifying how scientific fieldwork, the Museum has amassed preeminent own discoveries during the annual Identification investigations are done, this year, ID Day visitors collections that form an irreplaceable record Day in Theodore Roosevelt Memorial Hall. can learn how scientists use digital fabrication of life on Earth. Today, 21st-century tools— Held this year on May 10, Identification Day to aid their research and have a chance to sophisticated imaging techniques, genomic invites visitors to bring their own backyard finds have their own objects scanned and printed on analyses, programs to analyze ever-growing and curios for identification by Museum scientists. -
Can Underwater Refuges Protect Fish Populations Against Cormorant
1 Can underwater refuges protect fish populations against cormorant 2 predation? Evidence from a large scale multiple pond experiment 3 Pieter Lemmens1*, Luc De Meester1 and Steven A.J. Declerck2 4 5 1 Laboratory of Aquatic Ecology, Evolution and Conservation, KU Leuven, Ch. Deberiotstraat 6 32, 3000 Leuven, Belgium; 7 2 Department of Aquatic Ecology, Netherlands Institute of Ecology (NIOO-KNAW), 8 Droevendaalsesteeg 10, 6708 PB Wageningen, The Netherlands. 9 10 * Corresponding author: [email protected] 11 12 ABSTRACT 13 Artificial structures can protect fish against predation by cormorants. However, their 14 effectiveness in larger water bodies with different fish communities in the presence of 15 natural vegetation still needs to be explored. Using a large scale field experiment with 16 twenty-four ponds stocked with differently composed fish communities, the present study 17 investigates the extent to which the effect of artificial refuges on fish is species-specific and 18 determined by the characteristics of the fish community. This study provides strong 19 experimental evidence for artificial refuges protecting fish against predation by cormorants, 20 even in the presence of submerged vegetation. The effect of the refuges was, however, 21 highly species-specific and depended on the composition of the fish community. Strong 22 positive effects of refuges on rudd and roach populations were observed, especially in ponds 23 where these species dominated from the start of the experiment. Overall, the total biomass 24 of young-of-the-year, one-year-old and adult rudd and roach was on average 500, 7 and 15 25 times lower in ponds without than in ponds with refuges, respectively. -
The Myology of the Pectoral Appendage of Three Genera of American Cuckoos
MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN, NO. 85 The Myology of the Pectoral Appendage of Three Genera of American Cuckoos BY ANDREW J. BERGER ANN ARBOR UNIVERSITY OF MICHIGAN PRESS August 20, 1954 PRICE LIST OF THE MISCELLANEOUS PUBLICATIONS OF THE MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN Address inquiries to the Director of the Museum of Zoology, Ann Arbor, Michigan Bound in Paper No. 1. Directions for Collecting and Preserving Specimens of Dragonflies for Museum Purposes. By E. B. Williamson. (1916) Pp. 15, 3 figures .................. $0.25 No. 2. An Annotated List of the Odonata of Indiana. By E. B. Williamson. (1917) Pp. 12, lmap ....................................................$0.25 No. 3. A Collecting Trip to Colombia, South America. By E. B. Williamson. (1918) Pp. 24 (Out of print) No. 4. Contributions to the Botany of Michigan. By C. K. Dodge. (1918) Pp. 14 ......... $0.25 No. 5. Contributions to the Botany of Michigan, II. By C. K. Dodge. (1918) Pp. 44, 1 map . $0.45 No. 6. A Synopsis of the Classification of the Fresh-water Mollusca of North America, North of Mexico, and a Catalogue of the More Recently Described Species, with Notes. By Bryant Walker. (1918) Pp. 213, 1 plate, 233 figures. ............. $3.00 No. 7. The Anculosae of the Alabama River Drainage. By Calvin Goodrich. (1922) Pp. 57, 3plates ...................................................$0.75 No. 8. The Amphibians and Reptiles of the Sierra Nevada de Santa Marta, Colombia. By Alexander G. Ruthven. (1922) Pp. 69, 13 plates, 2 figures, 1 map ............ $1.00 No. 9. Notes on American Species of Triacanthagyna and Gynacantha. -
Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
Jahrbuch Der Geologischen Bundesanstalt
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 2018 Band/Volume: 158 Autor(en)/Author(s): Schönlaub Hans-Peter Artikel/Article: Review of the Devonian/Carboniferous boundary in the Carnic Alps 29- 47 JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 158 Heft 1–4 S. 29–47 Wien, Dezember 2018 Review of the Devonian/Carboniferous boundary in the Carnic Alps HANS P. SCHÖNLAUB* 16 Text-Figures Österreichische Karte 1:50.000 Italy BMN / UTM Carnic Alps 197 Kötschach / NL 33-04-09 Oberdrauburg Devonian 197 Kötschach / NL 33-04-10 Kötschach-Mauthen Carboniferous Conodonts Hangenberg Crisis Contents Abstract ................................................................................................ 29 Zusammenfassung ........................................................................................ 30 Current knowledge ........................................................................................ 30 Review of sedimentary and tectonic history ..................................................................... 32 Important stratigraphic markers .............................................................................. 32 Middle and Upper Ordovician ............................................................................. 32 Silurian .............................................................................................. 32 Devonian............................................................................................ -
Fins, Limbs, and Tails: Outgrowths and Axial Patterning in Vertebrate Evolution Michael I
Review articles Fins, limbs, and tails: outgrowths and axial patterning in vertebrate evolution Michael I. Coates1* and Martin J. Cohn2 Summary Current phylogenies show that paired fins and limbs are unique to jawed verte- brates and their immediate ancestry. Such fins evolved first as a single pair extending from an anterior location, and later stabilized as two pairs at pectoral and pelvic levels. Fin number, identity, and position are therefore key issues in vertebrate developmental evolution. Localization of the AP levels at which develop- mental signals initiate outgrowth from the body wall may be determined by Hox gene expression patterns along the lateral plate mesoderm. This regionalization appears to be regulated independently of that in the paraxial mesoderm and axial skeleton. When combined with current hypotheses of Hox gene phylogenetic and functional diversity, these data suggest a new model of fin/limb developmental evolution. This coordinates body wall regions of outgrowth with primitive bound- aries established in the gut, as well as the fundamental nonequivalence of pectoral and pelvic structures. BioEssays 20:371–381, 1998. 1998 John Wiley & Sons, Inc. Introduction over and again to exemplify fundamental concepts in biological Vertebrate appendages include an amazing diversity of form, theory. The striking uniformity of teleost pectoral fin skeletons from the huge wing-like fins of manta rays or the stumpy limbs of illustrated Geoffroy Saint-Hilair’s discussion of ‘‘special analo- frogfishes, to ichthyosaur paddles, the extraordinary fingers of gies,’’1 while tetrapod limbs exemplified Owen’s2 related concept aye-ayes, and the fin-like wings of penguins. The functional of ‘‘homology’’; Darwin3 then employed precisely the same ex- diversity of these appendages is similarly vast and, in addition to ample as evidence of evolutionary descent from common ances- various modes of locomotion, fins and limbs are also used for try.