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  • 1
    Online Resource
    Online Resource
    Amsterdam ; : Elsevier Academic
    Keywords: Geology Encyclopedias ; Wörterbuch ; Geowissenschaften ; Geologie
    Description / Table of Contents: Covers earth history, earth materials, surface processes, regional geology, economic geology, engineering geology, petroleum geology, geochemical and mineral exploration, the history of geology, and more.
    Type of Medium: Online Resource
    Pages: 1 online resource (5 volumes)
    ISBN: 9781601193674 , 160119367X , 9780123693969 , 0123693969 , 9780126363807 , 0080547915
    RVK:
    Language: English
    Note: Includes bibliographical references and index. - Print version record
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  • 2
    Online Resource
    Online Resource
    Boca Raton :Taylor & Francis Group,
    Keywords: Brachiopoda-Congresses. ; Brachiopoda, Fossil-Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (456 pages)
    Edition: 1st ed.
    ISBN: 9781135731458
    Series Statement: Systematics Association Special Volumes
    DDC: 594.68
    Language: English
    Note: Book Cover -- Title -- Copyright -- Contents -- Contributors -- Editors' Foreword -- Chapter 1 Introduction -- Part I Living brachiopods and palaeobiology -- Chapter 2 Apatite varieties in Recent and fossil linguloid brachiopod shells -- Chapter 3 Chemico-structural differentiation of the organocalcitic shells of rhynchonellate brachiopods -- Chapter 4 A TEM investigation of modulated microstructure in Recent and fossil articulate brachiopod shells from New Zealand -- Chapter 5 The acrosome reaction of the spermatozoa of the inarticulate brachiopod Lingula anatina -- Chapter 6 Brachiopod larval setae-a key to the phylum's ancestral life cycle? -- Chapter 7 Variation in the loops of two Recent species of Liothyrella (Brachiopoda -- Terebratuloidea) from New Zealand and… -- Chapter 8 Shell morphology and geographical distribution of Neocrania (Brachiopoda, Recent) in the eastern North Atlantic and -- Chapter 9 Developmental and settlement characteristics of the Antarctic brachiopod Liothyrella uva (Broderip 1833) -- Chapter 10 Embryonic shells of Devonian linguloid brachiopods -- Chapter 11 Global surface-water circulation and the main features of brachiopod biogeography -- Chapter 12 Fundamental differences in external spine growth in brachiopods -- Part II Advances in molecular studies -- Chapter 13 Brachiopod molecular phylogeny advances -- Chapter 14 Molecular phylogenetics and evolution of long-looped brachiopods -- Chapter 15 Phylogenetic relationships of brachiopods within the Metazoa based on mitochondrial amino acid sequence analyses -- Chapter 16 The phylogenetic position of brachiopods inferred from mitochondrial gene orders -- Chapter 17 Genetic differentiation of Terebratella sanguinea in the New Zealand fiords: a dispersal barrier in the marine… -- Part III Evolution and phylogeny. , Chapter 18 Functional morphology of articulatory structures and implications for patterns of musculature in Cambrian… -- Chapter 19 Early Silurian stricklandiid brachiopod evolution in eastern North America -- Chapter 20 Post-Palaeozoic Rhynchonellida (Brachiopoda): classification and evolutionary background -- Chapter 21 Radiations and extinctions of atrypide brachiopods: Ordovician-Devonian -- Chapter 22 Trends in athyridide diversity dynamics -- Chapter 23 The systematic position of some Upper Permian terebratulide genera -- Chapter 24 Ancestry and heterochronic origin of brachiopods of the Superfamily Megathyridoidea (Order Terebratulida): … -- Chapter 25 Thecideide phylogeny, heterochrony, and the gradual acquisition of characters -- Chapter 26 Incorporating stratigraphic data in the phylogenetic analysis of the Rhynchonelliformea -- Part IV Palaeoecology and ecology -- Chapter 27 Brachiopods of the Isca submarine cave: observations during ten years -- Chapter 28 Brachiopod/crinoid associations in the late Cenozoic of the Antillean region -- Chapter 29 Pragian-Emsian brachiopod communities of the Faou Formation (Massif Armoricain, France) -- Chapter 30 Palaeoecological interpretation of the brachiopod faunas of the Bardahessiagh Formation (middle Caradoc), Pomeroy, -- Part V Palaeobiogeography and biostratigraphy -- Chapter 31 Palaeolatitudinal distribution patterns of higher rhynchonelliform brachiopods in the early Ordovician -- Chapter 32 Distribution and diversity of Ordovician articulated brachiopods in the East Baltic -- Chapter 33 The orthide Platystrophia in the Ordovician and Early Silurian of the East Baltic -- Chapter 34 Silurian-Devonian biogeography -- Chapter 35 Extinction of some lingulate brachiopod families: new stratigraphical data from the Silurian and Devonian of…. , Chapter 36 Lower and Middle Permian brachiopods from Oman and Peri-Gondwanan palaeogeographical reconstructions -- Chapter 37 Permian Productida of Australasia: palaeobiogeographical and palaeoclimatological implications -- Chapter 38 A Permian Boreal brachiopod fauna from Okutadami, central Japan, and its tectonic implication -- Chapter 39 Brachiopod biostratigraphy of the Middle Triassic in Bulgaria and comparison with elsewhere in Europe -- Chapter 40 Mesozoic articulated brachiopods from the Western Cordillera of North America: their significance for… -- Chapter 41 Diversification of Mediterranean Early Jurassic brachiopods after the end-Triassic mass extinction-new results… -- Chapter 42 Stratigraphic distribution of brachiopods - a new method of storing and querying loosely-structured biodiversity… -- Index -- Systematics Association Publications.
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  • 3
    Online Resource
    Online Resource
    Cambridge : Cambridge University Press
    Keywords: Geology ; Paleogeography / Paleozoic
    Description / Table of Contents: Using full-colour palaeogeographical maps from the Cambrian to the present, this interdisciplinary volume explains how plate motions and surface volcanism are linked to processes in the Earth's mantle, and to climate change and the evolution of the Earth's biota. These new and very detailed maps provide a complete and integrated Phanerozoic story of palaeogeography. They illustrate the development of all the major mountain-building orogenies. Old lands, seas, ice caps, volcanic regions, reefs, and coal beds are highlighted on the maps, as well as faunal and floral provinces. Many other original diagrams show sections from the Earth's core, through the mantle, and up to the lithosphere, and how Large Igneous Provinces are generated, helping to understand how plates have appeared, moved, and vanished through time. Supplementary resources are available online, making this an invaluable reference for researchers, graduate students, professional geoscientists and anyone interested in the geological history of the Earth
    Type of Medium: Online Resource
    Pages: 1 online resource (317 pages) , digital, PDF file(s)
    ISBN: 9781107105324 , 9781316225523
    Language: English
    Note: Title from publisher's bibliographic system (viewed on 02 Dec 2016)
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  • 4
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Brachiopoda, Fossil. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (240 pages)
    Edition: 1st ed.
    ISBN: 9781119782360
    Series Statement: Fossils and Strata Monograph Series ; v.66
    DDC: 564.6809585
    Language: English
    Note: Intro -- Table of Contents -- Title Page -- A mid-Ordovician brachiopod evolutionary hotspot in southern Kazakhstan -- Introduction -- Geological setting and key sections -- Brachiopod associations -- Implications for biodiversity -- Localities -- Systematic palaeontology -- Acknowledgements -- References -- PLATES 1 - 21 -- Appendix -- End User License Agreement.
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 263 (1976), S. 304-306 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 The times at which faunas became common to both sides of the Lower Palaeozoic lapetus Ocean, 0, Closure of ocean (Norway); 6, freshwater fish; c, benthic ostracods; d, trilobite and brachiopod species; e, trilobite and brachiopod genera (? island hopping);/, Didymograptus bifidus; g, ...
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 39 (1995), S. 269-275 
    ISSN: 1573-1626
    Keywords: Cambrian ; Ordovician ; Silurian ; Devonian ; palaeomagnetism ; Gondwana ; Laurentia ; Avalonia
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Fresenius' Zeitschrift für analytische Chemie 102 (1935), S. 54-54 
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 9
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    Elsevier
    In:  Gondwana Research, 48 . pp. 257-284.
    Publication Date: 2020-04-08
    Description: Geological evidence, supported by biogeographical data and in accord with palaeomagnetic constraints, indicates that “one ocean” models for the Variscides should be discarded, and confirms, instead, the existence of three Gondwana-derived microcontinents which were involved in the Variscan collision: Avalonia, North Armorica (Franconia and Thuringia subdivided by a failed Vesser Rift), and South Armorica (Central Iberia/Armorica/Bohemia), all divided by small oceans. In addition, parts of south-eastern Europe, including Adria and Apulia, are combined here under the new name of Palaeo-Adria, which was also Peri-Gondwanan in the Early Palaeozoic. Oceanic separations were formed by the break-up of the northern Gondwana margin from the Late Cambrian onwards. Most of the oceans or seaways remained narrow, but – much like the Alpine Cenozoic oceans – gave birth to orogenic belts with HP-UHP metamorphism and extensive allochthons: the Saxo-Thuringian Ocean between North and South Armorica and the Galicia-Moldanubian Ocean between South Armorica and Palaeo-Adria. Only the Rheic Ocean between Avalonia and peri-Gondwana was wide enough to be unambiguously recorded by biogeography and palaeomagnetism, and its north-western arm closed before or during the Emsian in Europe. Ridge subduction under the northernmost part of Armorica in the Emsian created the narrow and short-lived Rheno-Hercynian Ocean. It is that ocean (and not the Rheic) whose opening and closure controlled the evolution of the Rheno-Hercynian foldbelt in south-west Iberia, south-west England, Germany, and Moravia (Czech Republic). Devonian magmatism and sedimentation set within belts of Early Variscan deformation and metamorphism are probably strike-slip-related. The first arrival of flysch on the forelands and/or the age of deformation of foreland sequences constrains the sequential closure of the Variscan seaways (Galicia-Moldanubian in the Givetian; Saxo-Thuringian in the Early Famennian; Rheno-Hercynian in the Tournaisian). Additional Mid- to Late Devonian and (partly) Early Carboniferous magmatism and extension in the Rheno-Hercynian, Saxo-Thuringian and Galicia-Moldanubian basins overlapped with Variscan geodynamics as strictly defined. The Early Carboniferous episode was the start of episodic anorogenic heating which lasted until the Permian and probably relates to Tethys rifting.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2013-01-30
    Description: The Late Ordovician equatorial zone, like the zone today, had few hurricane-grade storms within 10° of the equator, as emphasized by the preservation of massive-bedded Thalassinoides ichnofacies in a trans-Laurentian belt more than 6000 km long, from the southwestern United States to North Greenland. That belt also includes nonamalgamated shell beds dominated by the brachiopod Proconchidium , which would not have been preserved after hurricane-grade storms. The belt lacks such storm-related sedimentary features as rip-up clasts, hummocky cross-stratification, or large channels. In contrast, other contemporaneous Laurentian Thalassinoides facies and shell beds on either side of the belt have been disturbed by severe storms below fair-weather wave base. The position of the biofacies-defined equatorial belt coincides with the Late Ordovician equator deduced from paleomagnetic data from Laurentia, thus providing both a high-precision equatorial location and an independent test of the geocentric axial dipole hypothesis for that time.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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