GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Keywords
Language
  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Stromatolites. ; Geobiology. ; Electronic books.
    Description / Table of Contents: This book contains the proceedings of the Kalkowsky Symposium 2008, held in Göttingen, Germany. It highlights new ideas and information on the formation and environmental setting of stromatolites.
    Type of Medium: Online Resource
    Pages: 1 online resource (552 pages)
    Edition: 1st ed.
    ISBN: 9783642104152
    Series Statement: Lecture Notes in Earth Sciences Series ; v.131
    DDC: 552.58
    Language: English
    Note: Intro -- Advances in Stromatolite Geobiology -- Preface -- Acknowledgments -- Contents -- Part I: General Aspects and Research History -- Founding of the Term `Stromatolite´: Ernst Louis Kalkowsky (1851-1938) and his Early Stromatolite Research -- 1 Biographical Notes -- 2 Kalkowsky´s Research on Stromatolites -- 3 Publications of E. Kalkowsky -- References -- Kalkowskys Stromatolites and Oolites (Lower Buntsandstein, Northern Germany) -- 1 Introduction -- 2 Studied Area and Stratigraphic Frame -- 3 Stromatolites -- 3.1 Macroscopic Observations -- 3.2 Microscopic Observations -- 4 Oolites -- 5 Interpretation and Discussion -- References -- The Nature of Stromatolites: 3,500 Million Years of History and a Century of Research -- 1 Introduction -- 2 Stromatolites and Spongiostromids -- 2.1 Stromatolith -- 2.2 Eozoön, Cryptozoon, Archaeozoon -- 3 Stromatolites as Lithified Microbial Mats -- 3.1 Cyanobacterial Lacustrine Tufas -- 3.2 Andros Marsh -- 3.3 Coarse-Grained Thrombolitic Stromatolites -- 3.4 Tidal Flats -- 3.5 Wrinkle Marks -- 3.6 Reef Crusts -- 4 Stromatolites as Abiogenic Structures -- 4.1 Sinters -- 4.2 Concretions -- 4.3 Folds -- 4.4 Seafloor Crusts -- 5 Stromatolite Fabrics -- 5.1 Fine-Grained Biogenic Crust -- 5.2 Sparry Crust -- 5.3 Hybrid Crust -- 6 Stromatolite Definition -- 7 Discussion -- 7.1 Abiogenic and/or Biogenic Stromatolites? -- 7.2 Microbialite -- 7.3 Seafloor Crusts -- 7.4 Biogenicity Criteria -- 7.5 Fabric Criteria Through the Geological Record -- 8 Conclusions -- References -- Part II: Stromatolite Formation and Microbial Biomineralisation -- Modern Marine Stromatolites of Little Darby Island, Exuma Archipelago, Bahamas: Environmental Setting, Accretion Mechanisms and Role of Euendoliths -- 1 Introduction -- 2 Environmental Setting of Little Darby Stromatolites -- 3 Accretional Processes in Little Darby Stromatolites. , 4 Grain Stabilization Results in a Shift in Euendolith Composition -- 5 Lithification of Bahamian Stromatolites -- 6 Post-accretional Transformations of Stromatolites -- 7 Dynamics of Stromatolite Formation -- References -- Molecular Approaches to Studying Living Stromatolites -- 1 Introduction -- 2 DNA Isolation from Stromatolites: Pros and Cons -- 3 Molecular Tools: Accessing the Genetic Diversity and Beyond -- 3.1 PCR-Based rDNA Analysis -- 3.2 Metagenomics -- 4 The Future of Stromatolite Research -- References -- Magnesium Inhibition Controls Spherical Carbonate Precipitation in Ultrabasic Springwater (Cedars, California) and Culture Experiments -- 1 Introduction -- 2 Study Area -- 3 Methods -- 3.1 Petrography and Isotopes -- 3.2 Precipitation Experiments -- 4 Results -- 4.1 Petrography and Mineralogy of Spring Carbonates -- 4.2 Carbon and Oxygen Isotopes -- 4.3 Precipitation Experiments -- 5 Discussion -- 5.1 Origin of HCO3- and Carbonate Supersaturation -- 5.2 Kinetic Effects on Crystal Structure -- 5.3 Biological Effects on Crystal Structure -- 5.4 Spherical Carbonates Through Earth´s History -- 6 Conclusions -- References -- Microbial Control on Lamina Formation in a Travertine of Crystal Geyser, Utah -- 1 Introduction -- 2 Hydrochemistry of the Crystal Geyser -- 3 Methods -- 4 Textures and Mineralogy of the Laminated Travertine -- 5 Phylogenetic Analysis -- 6 Discussion -- References -- Photosynthesis-Induced Stromatolite Formation in the Freshwater Creeks -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 4 Conclusions -- References -- The Role of Purple Sulphur Bacteria in Carbonate Precipitation of Modern and Possibly Early Precambrian Stromatolites -- 1 Introduction -- 2 Methods -- 3 Results -- 3.1 Morphology of Hypersaline Microbial Mats -- 3.2 Micro-scale Profiles of Oxygen and Sulphide. , 3.3 Artificial Anoxic Microbial Mats -- 4 Discussion -- 4.1 Photosynthesis and Carbonate Precipitation in the Archean -- 5 Conclusions -- References -- Precipitation of CaCO3 Under Sulphate-Reduction Conditions -- 1 Introduction -- 2 Methodology -- 2.1 Microorganisms -- 2.2 Media -- 2.3 Determinations -- 3 Results and Discussion -- 4 Conclusions -- References -- Myxococcus xanthus Colony Calcification: An Study to Better Understand the Processes Involved in the Formation of this Stromatolite-Like Structure -- 1 Introduction -- 2 Materials and Methods -- 2.1 Microorganism and Culture Media -- 2.2 Experimental Procedures, Analyses and Calculations -- 2.2.1 Experimental Procedure and Study of the Mineralization -- 2.2.2 Determination of the Trends of the Growth of the Bacterial Population -- 2.2.3 Study of the Chemistry of the Culture Media -- 3 Results -- 4 Discussion -- 4.1 Patterns of Colony Calcification -- 4.2 Critical Size of the Population Necessary for the Calcification of the Colony -- 4.3 Passive and Active Mechanisms of Calcium Carbonate Precipitation -- 4.4 Passive Mechanisms of Calcium Carbonate Precipitation Giving Rise to an Homogeneous Precipitation -- 4.4.1 Active Mechanism of Calcium Carbonate Precipitation -- 5 Conclusions -- References -- Are Stromatolites the Most Ancient Skeletal Organisms? -- References -- Microbial Mats and Microbialites in the Freshwater Laguna Bacalar, Yucatan Peninsula, Mexico -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Hydrology and Water Chemistry -- 3.2 Distribution and Shape of Microbialites -- 3.3 Microbial Mats -- 3.3.1 Calothrix Mat -- 3.3.2 Scytonema Mat -- 3.3.3 Leptolyngbya Mat -- 3.3.4 Internal Structures of Bacalar Microbialites -- 4 Discussion -- References -- Part III: Microbial Ecology and Fossil Record. , Geomicrobiology of Fluid Venting Structures at the Salse di Nirano Mud Volcano Area in the Northern Apennines (Italy) -- 1 Introduction -- 2 Materials and Methods -- 2.1 Study Site and Sampling -- 2.2 Gas Analysis -- 2.3 Geochemical Analyses -- 2.4 Lipid Biomarker Analyses -- 2.5 Microbiological Methods -- 3 Results and Discussion -- 3.1 Geochemistry -- 3.2 Microbiology: Enrichment Cultures -- 3.3 Lipid Biomarkers -- 4 Conclusions -- References -- Trace Element and Biomarker Signatures in Iron-Precipitating Microbial Mats from the Tunnel of Äspö (Sweden) -- 1 Introduction -- 2 Material and Methods -- 2.1 Sample Collection -- 2.2 Sample Preparation -- 2.3 Trace Element Analysis -- 2.4 Biomarker Analysis -- 2.5 Factor Analysis -- 2.6 Structure Analysis -- 3 Results -- 3.1 Structure of the Microbial Mats -- 3.2 Trace Elements -- 3.3 Biomarkers -- 4 Discussion -- 4.1 Structure of the Microbial Mats -- 4.2 Trace Elements -- 4.3 Biomarkers -- 5 Conclusion -- References -- Microbial Euendolithic Assemblages and Microborings in Intertidal and Shallow Marine Habitats: Insight in Cyanobacterial Speciation -- 1 Introduction -- 2 Materials and Methods -- 3 Morphotypic and Ecotypic Diversity and Variability of Coastal Euendolithic Cyanobacteria -- 4 The Identity of Microboring Traces -- 5 Microboring Traces in Ooid Sand Grains -- 6 Diversity of Fascichnus Traces of Coccoid Cyanobacteria in Shallow Marine Environments -- 7 Microboring Cyanobacteria and Prokaryote Speciation -- References -- On Microbiocorrosion -- 1 Introduction -- 2 Niches -- 3 Substrates -- 4 Mechanisms -- 5 Rates -- 6 Global Impact -- 7 Current Concerns -- References -- The Deep-Sea Chemoautotroph Microbial World as Experienced by the Mediterranean Metazoans Through Time -- 1 Preface -- 2 The March of Life -- 3 The Phanerozoic Record of Metazoans in Deep-Sea Chemoautotrophic Communities. , 4 The Deep Mediterranean Basin is Microbes´ Paradise -- 5 Deep Sea Chemosynthetic Environments in the Mediterranean Neogene -- 6 Postface -- References -- Gypsum Microbialite Domes Shaped by Brine Currents from the Badenian Evaporites of Western Ukraine -- 1 Introduction -- 2 Terminology -- 3 The Badenian Gypsum Deposits in Carpathian Foredeep -- 4 Geology of the Study Area -- 5 Sedimentology of Badenian Gypsum Deposits and Microbialites -- 6 The ``Dry Shore´´ Gypsum Microbialites (Unit M) -- 7 Structures Indicating the Direction of Water Flow -- 7.1 Sabre Gypsum Crystals with Concordant Orientation of Apices -- 7.2 Sub-horizontal Selenite Crystals Within Microbialites -- 7.3 Elongated Gypsum Microbialite Domes -- 7.4 Elongated Gypsum Microbialite Domes with Asymmetric Selenite Covers -- 8 Interpretation of the Oriented Badenian Selenite Crystals -- 9 Origin and Environment of the Elongated Domes and Selenite Directional Structures -- 10 Modern Analogues of the Badenian Gypsum Domes -- 11 Final Remarks -- References -- The Microbialite-Vermetid Community of the Salento Peninsula in Southern Italy: A Late Miocene Example of Automicrite Deposition -- 1 Introduction -- 2 Geological Setting -- 3 Methodology -- 4 Results and Discussion -- 4.1 Facies Observations -- 4.2 Microfacies Observations -- 4.3 FT-IR Analyses -- 5 Conclusions -- References -- The Characterisation of Sedimentary Organic Matter in Carbonates with Fourier-Transform Infrared (FTIR) Spectroscopy -- 1 Introduction -- 2 Background Data -- 2.1 Samples and Microfacies -- 2.2 Origin and Maturity of Organic Matter -- 3 Analytical Techniques -- 4 Results -- 5 Interpretation and Discussion -- 6 Conclusions -- References -- Interactions Between Microbes and Siliceous Sponges from Upper Jurassic Buildups of External Prebetic (SE Spain) -- 1 Introduction -- 2 Geological Framework. , 3 Sponge-Microbialite Buildups.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Sponges-Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (606 pages)
    Edition: 1st ed.
    ISBN: 9783642756566
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Keywords: Konferenzschrift 1988 ; Schwämme ; Schwämme
    Type of Medium: Book
    Pages: XVIII, 595 S. , Ill., graph. Darst., Kt. , 24 cm
    ISBN: 3540525092 , 0387525092
    DDC: 593.420
    Language: English
    Note: Literaturangaben
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Keywords: Evolution (Biology) ; Aufsatzsammlung ; Evolution
    Description / Table of Contents: Das Leben tritt uns in einer großartigen Vielfalt und Wandelbarkeit der Organismen entgegen, die durch eine fast vier Milliarden Jahre zurückreichende Stammesgeschichte miteinander verbunden sind. Wesentliche Gesetzmäßigkeiten dieser Evolution sind seit langem bekannt, doch viele Einzelheiten sind noch immer ungeklärt, und es wird oft gefragt, ob die naturwissenschaftlichen Theorien ausreichen, die Mannigfaltigkeit der Lebensformen zu erklären. Geistes- und Kulturwissenschaften spielen jedoch ebenfalls eine bedeutende Rolle beim Bemühen, die Entwicklungsgeschichte zu verstehen. Die Evolution beschränkt sich nicht nur auf die Optimierung von morphologischen und molekularen Merkmalen, sondern sie schließt auch die Entwicklung sozialer, politischer, kultureller, moralischer und religiöser Strukturen ein.
    Type of Medium: Book
    Pages: 461 S. , Ill., graph. Darst., Kt.
    ISBN: 9783835303010
    DDC: 576.822
    RVK:
    Language: German
    Note: Literaturangaben
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Keywords: Konferenzschrift 2010 ; Stachelhäuter ; Fossile Stachelhäuter
    Description / Table of Contents: Echinoderms are a vast group of spiny-skinned animals including starfish, brittle-stars, sea urchins, sand dollars, feather stars, sea lilies and sea cucumbers. These relatives of chordates and hemichordates have inhabited the world's oceans for more than 500 million years. Modern members of the Echinodermata are, with over 7 000 species, an integral part of marine communities from the intertidal to the deep sea. Echinoderms play a major ecological role in marine habitats and are of economic importance in fisheries, aquaculture and biomedicine. The present volume contains the abstracts of lectures and posters presented during the 7th European Conference on Echinoderms (ECE) as well as excursion guides. This year's conference was held at the northern campus of the Georg-August University in Göttingen, Germany, from October 2-9, 2010. More than 100 biologists, palaeontologists and other scientists from 25 countries participated.
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 145 S., 17,1 MB) , Ill.
    DDC: 590
    Language: English
    Note: Autorenindex S. 142 - 145 , Systemvoraussetzungen: Acrobat reader.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Keywords: Konferenzschrift
    Description / Table of Contents: The 99th Annual Meeting of the Geologische Vereinigung (GV) and International Conference on Earth Control on Planetary Life and Environment, held in October 2009 at the Geosciences Centre of the Georg-August-Universität Göttingen, brings together researchers from all fields of Earth Sciences and beyond to shape an attractive interdisciplinary program on the geological history of Planet Earth and its control over and interaction with biological evolution, development of habitats, environmental and climate change as well as history and culture of Homo sapiens. This volume contains the abstracts of invited keynote lectures as well as all oral and poster presentations.
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 165 S., 1,7 MB)
    Series Statement: Universitätsdrucke
    Language: English
    Note: Systemvoraussetzungen: Acrobat reader.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Keywords: Geologie ; Aufsatzsammlung ; Geowissenschaften ; Geowissenschaften
    Description / Table of Contents: Our planet earth is a system - scarcely understood - of geological, biological und cosmic processes of great variety, which make it an interesting object of research. The papers listed here deal with topics of a series of lectures open to the public, presented at the Academy of Sciences and at the Georg August University of Göttingen, which were organised by the publishers of this book. It is the publishers' aim to bring before the public a few important and interesting geoscientific aspects. Needless to say, there is no claim to cover all aspects of this subject area. However, the publishers would like to initiate readers to concentrate more deeply on scientific topics. The selected material should help them to find their way through the diversity of this branch of research
    Type of Medium: Online Resource
    Pages: Online-Ressource
    DDC: 550
    RVK:
    Language: German
    Note: http://creativecommons.org/licenses/by-nd/2.0/de , Literaturangaben , German
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The process of organomineralization is increasingly well understood with respect to modern carbonate sediments accumulating adjacent to tropical reef atolls and reef caves. Mineralization related to non-living organic substrates results in autochthonous micrite production (‘automicrites’). ‘Automicrites’ are the main constructive element of Lower Cretaceous (Albian) carbonate mud mounds in northern Spain. These slope mud mounds occur within transgressive and early highstand system tracts encompassing several macrobenthic ecological zones. They are clearly separated from the biocalcifying carbonate factory (Urgonian carbonate platforms), in both space and time. Within these build-ups, most ‘automicrites’ were initially indurated and accreted to form a medium-relief growth framework. ‘Automicrites’ have a uniform, presumably high-Mg-calcite precursor mineralogy. They show an inorganic stable-isotope signature (∂13C around +3·3‰) within the range of early marine cements, and skeletal compounds lacking major vital effects. Epifluorescence microscopy shows that they have facies-specific fluorescence, which is similar to skeletal compounds of Acanthochaetetes, but clearly different from allomicritic sediment and cements, which are mostly non-fluorescent. The EDTA-soluble intracrystalline organic fraction (SIOF) of Albian automicrites shows an amino acid spectrum that is similar to shallow subsurface samples from their modern counterparts. Gel electrophoresis of the SIOF demonstrates an exclusively acidic character, and a mean molecular size range between 20 and 30 kDa. Experiments in vitro (inhibition tests) indicate that the SIOF has a significant Ca2+-binding capacity. Fluorescence and chemical characteristics of SIOF point to a main substance class, such as humic and fulvic acids, compounds that form from pristine organic matter during early diagenesis. Biomarker analyses provide evidence for the crucial role of biodegradation by heterotrophic microorganisms, but no biomarker for cyanobacteria has been found. Primary sources of organic material should have been manifold, including major contributions by metazoans such as sponges. It is concluded that many carbonate mud mounds are essentially organomineralic in origin and that the resulting fabric of polygenetic muds (‘polymuds’) may represent ancestral metazoan reef ecosystems, which possibly originated during the Neoproterozoic.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2024-02-14
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉ABSTRACT〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉The Permian–Triassic and Triassic–Jurassic critical intervals are among the most significant ecological upheavals in the Phanerozoic. Both evolutionary junctures are characterized by environmental deterioration associated with a marked biodiversity decline. In this study, Permian–Triassic and Triassic–Jurassic boundary sections from South China and the Northern Calcareous Alps were investigated. In order to reconstruct the interplay between biotic and abiotic processes, a multifaceted approach that included optical microscopy, X‐ray diffraction, Raman spectroscopy, stable carbon isotopes and lipid biomarkers was employed. The lower parts of these two sections are similar as both consist of limestone with abundant fossils of eukaryotic organisms. However, the Permian–Triassic record is dominated by dasyclad green algae and fusulinid foraminifera, while the Triassic–Jurassic record is typified by corals and coralline sponges. Moving upward, both sections consist mainly of micrite and marl. Concerning the Permian–Triassic section, it transits to volcanic ash intercalated by a distinct limestone bed with abundant calcispheres (tentatively attributed to ancestors of dinoflagellates). The Triassic–Jurassic section does not provide direct evidence for volcanic activity, but also becomes rich in calcisphere‐type cysts towards the top. Additionally, the section preserves abundant 4‐methyl sterenes (diagnostic for dinoflagellates) and C〈sub〉37–39〈/sub〉 〈italic toggle="no"〉n〈/italic〉‐alkanes (indicative for haptophytes). Hence, both critical intervals were associated with marked blooms of (ancestral) dinoflagellates and haptophytes (for example, coccolithophorids). These blooms were followed by ecological lag‐phases, as indicated by low carbonate contents and scarce fossils which only increased further up the sections. For both critical intervals, it is commonly assumed that the formation of voluminous volcanic provinces (Siberian Traps and Central Atlantic Magmatic Province, respectively), as well as associated processes (for example, burning of organic‐rich sediments such as coal), resulted in ecological devastation. However, results suggest that volcanism also had a positive effect on certain planktonic primary producers such as dinoflagellates and haptophytes, perhaps by delivering essential nutrients.〈/p〉
    Description: China Council Scholarship
    Description: Teach@Tübingen Fellowship
    Keywords: ddc:560 ; Calcispheres ; dinoflagellates ; haptophytes ; lipid biomarkers ; mass extinctions ; microfacies ; stable carbon isotopes
    Language: English
    Type: doc-type:article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2017-06-27
    Description: In several fields of cell biology, correlative microscopy is applied to compare the structure of objects at high resolution under the electron microscope with low resolution light microscopy images of the same sample. It is, however, difficult to prepare samples and marker systems that are applicable for both microscopic techniques for the same specimen at the same time. In our studies, we used microbial mats from Cold Seep communities for a simple and rapid correlative microscopy method. The mats consist of bacterial and archaeal microorganisms, coupling reverse methanogenesis to the reduction of sulfate. The reverse methanogenic pathway also generates carbonates that precipitate inside the mat and may be the main reason for the formation of a microbial reef. The mat shows highly differentiated aggregates of various organisms, tightly interconnected by extracellular polysaccharides. In order to investigate the role of EPS as adhesive mucilage for the biofilm and as a precipitation matrix for carbonate minerals, samples were embedded in a hydrophilic resin (Lowicryl K4 M). Sections were suitable for light as well as electron microscopy in combination with lectins, either labeled with a fluorescent marker or with colloidal gold. This allows lectin mapping at low resolution for light microscopy in direct comparison with a highly resolved electron microscopic image.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...