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  • 1
    Keywords: Coral reefs and islands ; Coral reef ecology ; Geology, Stratigraphic Quaternary ; Paleoecology Quaternary ; Geobiology ; Paleobiogeography ; Marine sediments ; Climatic changes ; Korallenriff ; Quartär
    Type of Medium: Book
    Pages: XVII, 532 S. , Ill., graph. Darst.
    Edition: 1. ed.
    ISBN: 9780444532473
    Series Statement: Developments in marine geology vol. 5
    DDC: 551
    Language: English
    Note: Enth. Literaturangaben S. 437 - 521 und Index , Introduction: Quaternary reefs in time and spacePalaeobiogeography: evaluation of the inheritance from the Tertiary -- Structure, zonation and dynamic patterns of coral reef communities -- Controls on the development, distribution and preservation of reefs -- Patterns of carbonate production and deposition on reefs -- Reef anatomy and stratigraphy -- Reef hydrogeology -- Reef diagenesis -- Corals and coral reefs as records of climate change -- Conclusions: coral reefs from the past to the future.
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  • 2
    Online Resource
    Online Resource
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Keywords: Freshwater ecology. ; Marine ecology. ; Bioclimatology. ; Ecology . ; Oceanography. ; Paleontology .
    Description / Table of Contents: INTRODUCTION: THE REEF PHENOMENON -- INTO THE INTIMACY OF CORALS, BUILDERS OF THE SEA -- 1 TAXONOMIC AFFILIATION -- 1.1 Systematic classification of cnidarians -- 1.2 Scleractinians -- 2 MORPHOLOGY AND ANATOMY -- 2.1 Polyp anatomy -- 2.2 Reproduction -- 2.2.1 Sexual reproduction -- 2.2.2 Asexual reproduction -- 2.3 Anatomy of calcareous skeletons -- 2.4 Coral colonies -- 2.4.1 Corallite arrangement -- 2.4.2 Colony morphology -- 3 SYMBIOSIS -- 4 BIOMINERALIZATION -- 4.1 Calicoderm and biomineralization -- 4.2 Skeletons and biomineralization -- 4.3 Interface between calicoderm and skeleton -- 4.4 Principles of calcification -- 5 NUTRITION -- 5.1 Prey capture -- 5.2 Food -- 5.3 Autotrophy -- THE MODERN TIMES -- 1 BIOZONATION -- 2 REEF MORPHOTYPES -- 2.1 Fringing reefs -- 2.2 Barrier reefs -- 2.3 Atolls -- 2.4 Bank reefs -- 2.5 High carbonate islands -- 3 GEOGRAPHICAL DISTRIBUTION -- 3.1 Ecological control -- 3.2 Tectonic control -- 3.3 Eustatic control -- 3.4 Topographic control -- 4 REEF GROWTH -- 4.1 Vertical growth strategies -- 4.1.1 Controlling factors -- 4.1.2 Give-up growth -- 4.1.3 Keep-up growth -- 4.1.4 Catch-up mode -- 4.2 Lateral growth -- 5 MORPHO-SEDIMENTARY PROCESSES -- 5.1 Bioconstruction -- 5.2 Erosion -- 5.3 Bioaccumulation -- 5.4 Cementation -- 6 INTERNAL STRUCTURE -- 6.1 Nature and distribution of facies -- 6.1.1 Framework facies -- 6.1.2 Detrital facies -- 6.1.3 Facies distribution and hydrodynamics -- 6.2 The different structural models -- 7 A BRIEF HISTORY OF REEF DEVELOPMENT -- 7.1 The climatic context -- 7.2 History of reef development since the last deglaciation -- 7.3 Reef history throughout the Pleistocene -- 8 RECORD OF ENVIRONMENTAL CHANGES -- 8.1 Record at the coral colony scale -- 8.1.1 Temperature -- 8.1.2 Salinometry -- 8.1.3 Rainfall -- 8.1.4 pH measurement -- 8.1.5 Photometry -- 8.1.6 Current measurement -- 8.2 Record at the scale of a reef edifice -- 8.2.1 Reef flats and micro-atolls -- 8.2.2 Arrangement of coral communities -- 8.2.3 Arrangement of reef edifices -- THE LONG MARCH OF CORALS -- 1 THE TIME OF THE ORIGINS -- 1.1 Early Earth and the first traces of life -- 1.2 Evolution of the atmosphere -- 1.3 Geochemical model of the early ocean -- 1.4 Emergence of biomineralization -- 1.5 The early calcifying organisms and cnidarians -- 1.6 The earliest corals -- 1.7 The appearance of scleractinian corals -- 2 THE TIME OF DIVERSIFICATION -- 2.1 Coral-algae symbiosis -- 2.1.1 Acquiring photosymbiosis -- 2.1.2 Evidence of photosymbiosis -- 2.1.3 Symbiosis and coloniality -- 2.2 A brief history of coral and reef building -- 2.2.1 Paleozoic times -- 2.2.2 Mesozoic times -- 2.2.3 Cenozoic times -- THE HIGHS AND LOWS OF THE REEF PHENOMENON -- 1 CAUSES -- 1.1 Causal relationships -- 1.2 Gas emissions and volcanic products -- 1.3 Methane emissions -- 1.4 Thermogenic gases -- 1.5 The fall of celestial bodies -- 1.6 Behaviour of organisms facing environmental disturbances -- 1.7 Disturbances induced by CO2 and ocean acidification -- 1.8 Thermal shocks -- 1.9 Disturbances induced by ocean deoxygenation -- 2 THE MAIN BIOLOGICAL CRISES -- 2.1 The Cambrian crises -- 2.2 The major crisis of the Ordovician end -- 2.3 The minor crises of the Silurian -- 2.4 The successive crises of the Devonian -- 2.5 The Permian crises -- 2.6 The Triassic crises -- 2.7 The lower Jurassic crisis -- 2.8 The Jurassic–Cretaceous transition (J–K) -- 2.9 The Cretaceous–Paleogene crisis -- 2.10 The Paleocene–Eocene crisis -- 2.11 The Eocene–Oligocene transition -- 2.12 The Oligocene end to the Plio-Quaternary -- 3 THE RESPONSE OF CORALS AND REEFS TO CRISES: FROM EXTINCTION TO RECOVERY -- 3.1 At the Ordovician end -- 3.2 During the Silurian -- 3.3 During the Devonian -- 3.4 At the Permian -- 3.5 At the Permian–Triassic boundary -- 3.6 From the middle to the end of the Triassic -- 3.7 During the Jurassic -- 3.8 From the upper Jurassic to the lower Cretaceous -- 3.9 At the Cretaceous–Paleogene (K–Pg) transition -- 3.10 From the Paleocene to the Eocene -- 3.11 From the Oligocene to the Miocene -- 3.12 During the Plio-Quaternary -- 4 CONCLUSIONS -- CORAL REEFS IN THE FACE OF THEIR FATE -- 1 DISRUPTIVE AGENTS IN ACTION -- 1.1 Carbon dioxide and rising surface water temperatures -- 1.2 Carbon dioxide and its effects on the carbonate cycle -- 1.3 Carbon dioxide and ocean acidification -- 1.4 The other disruptive agents -- 2 THE RESPONSE OF CORALS AND CORAL REEFS -- 2.1 Temperature rise of surface waters -- 2.2 To acidification -- 2.3 To other disruptive agents -- 3 THE EVOLUTION OF CORAL ISLETS -- 3.1 The modes of low-lying island formation -- 3.2 Future evolution of low-lying islands: maintenance, reduction, or destruction? -- CONCLUSIONS -- BIBLIOGRAPHY -- INDICE.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(IX, 166 p. 120 illus., 117 illus. in color.)
    Edition: 1st ed. 2023.
    ISBN: 9783031168871
    Series Statement: Coral Reefs of the World 16
    Language: English
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  • 3
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Coral reef ecology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (174 pages)
    Edition: 1st ed.
    ISBN: 9783031168871
    Series Statement: Coral Reefs of the World Series ; v.16
    DDC: 577.7890913
    Language: English
    Note: Intro -- Preface -- Contents -- 1: Introduction: The Reef Phenomenon -- References -- 2: Into the Intimacy of Corals, Builders of the Sea -- 2.1 Taxonomic Affiliation -- 2.1.1 Systematic Classification of Cnidarians -- 2.1.2 Scleractinians -- 2.2 Morphology and Anatomy -- 2.2.1 Polyp Anatomy -- 2.2.2 Reproduction -- 2.2.2.1 Sexual Reproduction -- 2.2.2.2 Asexual Reproduction -- 2.2.3 Anatomy of Calcareous Skeletons -- 2.2.4 Coral Colonies -- 2.2.4.1 Corallite Arrangement -- 2.2.4.2 Colony Morphology -- 2.3 Symbiosis -- 2.4 Biomineralisation -- 2.4.1 Calicoderm and Biomineralisation -- 2.4.2 Skeletons and Biomineralisation -- 2.4.3 Interface Between Calicoderms and Skeletons -- 2.4.4 Principles of Calcification -- 2.5 Nutrition -- 2.5.1 Prey Capture -- 2.5.2 Food -- 2.5.3 Autotrophy -- References -- 3: The Modern Times -- 3.1 Biozonation -- 3.2 Reef Morphotypes -- 3.2.1 Fringing Reefs -- 3.2.2 Barrier Reefs -- 3.2.3 Atolls -- 3.2.4 Bank Reefs -- 3.2.5 High Carbonate Islands -- 3.3 Geographical Distribution -- 3.3.1 Ecological Control -- 3.3.2 Tectonic Control -- 3.3.3 Eustatic Control -- 3.3.4 Topographic Control -- 3.4 Reef Growth -- 3.4.1 Vertical Growth Strategies -- 3.4.1.1 Controlling Factors -- 3.4.1.2 Give-Up Growth -- 3.4.1.3 Keep-Up Growth -- 3.4.1.4 Catch-Up Mode -- 3.4.2 Lateral Growth -- 3.5 Morpho-Sedimentary Processes -- 3.5.1 Bioconstruction -- 3.5.2 Erosion -- 3.5.3 Bioaccumulation -- 3.5.4 Cementation -- 3.6 Internal Structure -- 3.6.1 Nature and Distribution of Facies -- 3.6.1.1 Framework Facies -- 3.6.1.2 Detrital Facies -- Sand-Dominated Facies -- Mud-Dominated Facies -- 3.6.1.3 Facies Distribution and Hydrodynamics -- 3.6.2 The Different Structural Models -- 3.7 A Brief History of Reef Development -- 3.7.1 The Climatic Context -- 3.7.2 History of Reef Development Since the Last Deglaciation. , 3.7.3 Reef History Throughout the Pleistocene -- 3.8 Record of Environmental Changes -- 3.8.1 Record at the Coral Colony Scale -- 3.8.1.1 Temperature -- 3.8.1.2 Salinometry -- 3.8.1.3 Rainfall -- 3.8.1.4 pH Measurement -- 3.8.1.5 Photometry -- 3.8.1.6 Current Measurement -- 3.8.2 Record at the Scale of a Reef Edifice -- 3.8.2.1 Reef Flats and Micro-atolls -- 3.8.2.2 Arrangement of Coral Communities -- 3.8.2.3 Arrangement of Reef Edifices -- References -- 4: The Long March of Corals -- 4.1 The Time of the Origins -- 4.1.1 Early Earth and the First Traces of Life -- 4.1.2 Evolution of the Atmosphere -- 4.1.3 Geochemical Model of the Early Ocean -- 4.1.4 Emergence of Biomineralisation -- 4.1.5 The Early Calcifying Organisms and Cnidarians -- 4.1.6 The Earliest Corals -- 4.1.7 The Appearance of Scleractinian Corals -- 4.2 The Time of Diversification -- 4.2.1 Coral-Algae Symbiosis -- 4.2.1.1 Acquiring Photosymbiosis -- 4.2.1.2 Evidence of Photosymbiosis -- 4.2.1.3 Symbiosis and Coloniality -- 4.2.2 A Brief History of Coral and Reef Building -- 4.2.2.1 Paleozoic Times -- The Cambrian -- The Ordovician -- The Silurian -- The Devonian -- The Carboniferous -- The Permian -- 4.2.2.2 Mesozoic Times -- The Triassic -- The Jurassic -- The Cretaceous -- 4.2.2.3 Cenozoic Times -- The Paleogene -- The Neogene -- References -- 5: The Highs and Lows of the Reef Phenomenon -- 5.1 Causes -- 5.1.1 Causal Relationships -- 5.1.2 Gas Emissions and Volcanic Products -- 5.1.3 Methane Emissions -- 5.1.4 Thermogenic Gases -- 5.1.5 The Fall of Celestial Bodies -- 5.1.6 Behaviour of Organisms Facing Environmental Disturbances -- 5.1.7 Disturbances Induced by CO2 and Ocean Acidification -- 5.1.8 Thermal Shocks -- 5.1.9 Disturbances Induced by Ocean Deoxygenation -- 5.2 The Main Biological Crises -- 5.2.1 The Cambrian Crises -- 5.2.2 The Major Crisis of the Ordovician End. , 5.2.3 The Minor Crises of the Silurian -- 5.2.4 The Successive Crises of the Devonian -- 5.2.5 The Permian Crises -- 5.2.6 The Triassic Crises -- 5.2.7 The Lower Jurassic Crisis -- 5.2.8 The Jurassic-Cretaceous Transition (J-K) -- 5.2.9 The Cretaceous-Paleogene Crisis -- 5.2.10 The Paleocene-Eocene Crisis -- 5.2.11 The Eocene-Oligocene Transition -- 5.2.12 The Oligocene End to the Plio-Quaternary -- 5.3 The Response of Corals and Reefs to Crises: From Extinction to Recovery -- 5.3.1 At the Ordovician End -- 5.3.2 During the Silurian -- 5.3.3 During the Devonian -- 5.3.4 At the Permian -- 5.3.5 At the Permian-Triassic Boundary -- 5.3.6 From the Middle to the End of the Triassic -- 5.3.7 During the Jurassic -- 5.3.8 From the Upper Jurassic to the Lower Cretaceous -- 5.3.9 At the Cretaceous-Paleogene (K-Pg) Transition -- 5.3.10 From the Paleocene to the Eocene -- 5.3.11 From the Oligocene to the Miocene -- 5.3.12 During the Plio-Quaternary -- 5.4 Conclusions -- References -- 6: Coral Reefs in the Face of Their Fate -- 6.1 Disruptive Agents in Action -- 6.1.1 Carbon Dioxide and Rising Surface Water Temperatures -- 6.1.2 Carbon Dioxide and Its Effects on the Carbonate Cycle -- 6.1.3 Carbon Dioxide and Ocean Acidification -- 6.1.4 The Other Disruptive Agents -- 6.2 The Response of Corals and Coral Reefs -- 6.2.1 Temperature Rise of Surface Waters -- 6.2.2 To Acidification -- 6.2.3 To Other Disruptive Agents -- 6.3 The Evolution of Coral Islets -- 6.3.1 The Modes of Low-Lying Islet Formation -- 6.3.2 Future Evolution of Low-Lying Islet: Maintenance, Reduction or Destruction? -- References -- Conclusions -- Index.
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  • 4
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Quartear. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (550 pages)
    Edition: 1st ed.
    ISBN: 9780080932767
    Series Statement: Issn Series ; v.Volume 5
    Language: English
    Note: Front cover -- Quaternary Coral Reef Systems: History, Development Processes and Controlling Factors -- Copyright page -- Contents -- Preface -- Chapter 1. Introduction: Quaternary Reefs in Time and Space -- 1.1. The Reef Phenomenon: Definitions and History of Discovery and Research -- 1.2. Types of Coral Reefs -- 1.3. Geographical Distribution of Corals and Coral Reefs -- 1.4. Modern Tropical Climate Modes -- 1.5. Quaternary Time Scales -- 1.6. Trends in the Quaternary Climate Dynamics -- 1.7. Establishing the Chronology of Quaternary Coral Reefs -- 1.8. Methods of Obtaining Data -- Chapter 2. Palaeobiogeography: Evaluation of the Inheritance from the Tertiary -- 2.1. Introduction -- 2.2. Development Patterns of Tertiary Coral Reefs -- 2.3. Temporal and Spatial Variations in Coral and Calcareous Algal Diversity -- 2.4. Conclusions -- Chapter 3. Structure, Zonation and Dynamic Patterns of Coral Reef Communities -- 3.1. Introduction -- 3.2. Structure and Zonation of Modern Reef Communities -- 3.3. Structure and Zonation of Quaternary Reef Communities -- 3.4. Dynamic Patterns of Reef Communities -- 3.5. Conclusions -- Chapter 4. Controls on the Development, Distribution and Preservation of Reefs -- 4.1. Introduction -- 4.2. Controls on Reef Development and Distribution -- 4.3. Controls on Reef Community Preservation: The Taphonomic Approach -- 4.4. Conclusions -- Chapter 5. Patterns of Carbonate Production and Deposition on Reefs -- 5.1. Introduction -- 5.2. Patterns of Reef Carbonate Production -- 5.3. Patterns of Reef Carbonate Deposition -- 5.4. Conclusions -- Chapter 6. Reef Anatomy and Stratigraphy -- 6.1. Introduction -- 6.2. Morphology and Anatomy of Holocene Reefs -- 6.3. Structure and Pleistocene Stratigraphy of Barrier Reefs and Atolls -- 6.4. Stratigraphy of Emerged Reef Terraces -- 6.5. Stratigraphy of Submerged Reef Terraces and Banks. , 6.6. Reef Stratigraphy and Numerical Modelling -- 6.7. Conclusions -- Chapter 7. Reef Hydrogeology -- 7.1. Introduction -- 7.2. External Hydrology: Water Characteristics and Reef Responses to Waves and Currents -- 7.3. Groundwater Hydrology -- 7.4. Conclusions -- Chapter 8. Reef Diagenesis -- 8.1. Introduction -- 8.2. Mineralogy of Sediment Components -- 8.3. Cements in Quaternary Reef Limestones -- 8.4. Replacement and Dissolution -- 8.5. Hydrological Control of Flow Rates -- 8.6. Rates of Reef Diagenesis -- 8.7. Diagenetic Sequences -- 8.8. Dolomite and Reefs -- 8.9. Phosphorites -- 8.10. Conclusions -- Chapter 9. Corals and Coral Reefs as Records of Climatic Change -- 9.1. Introduction -- 9.2. Individual Coral Colonies as Records of Climate -- 9.3. Climate Reconstruction based on Individual Coral Colonies -- 9.4. Coral Reefs as Records of Sea-Level Change -- 9.5. Conclusions -- Chapter 10. Conclusions: Coral Reefs from the Past to the Future -- 10.1. The Historical Perspective -- 10.2. The Role of Controlling Factors in Reef Growth and Distribution -- 10.3. The Fossil Record as a Proxy for the Future of Reefs -- 10.4. Global Warming and the Future of Reefs -- 10.5. Prospective -- References -- Subject Index.
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 44 (1997), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The fringing reef at Pointe-au-Sable (Mauritius, Indian Ocean) was used to examine the effects of Holocene sea-level rise on coral growth. This reef is about 1000 m wide and comprises a forereef slope (30 m maximum depth), a narrow reef crest and a very shallow backreef (1·5 m maximum depth).Four major coral communities were recognized, which developed within relatively narrow depth ranges: a Pachyseris/Oulophyllia community (deeper than 20 m), an Acropora‘tabulate’Faviid community (20–6 m); a robust branching Acropora community (less than 6 m) and a Pavona community (less than 10m). Three high-recovery cores show the Holocene reef sequence is a maximum of 19·3 m thick and comprises four coral biofacies which are similar to counterparts identified in modern communities: robust branching, tabular-branching, robust branching-domal and foliaceous coral facies.A minimum sea-level curve for the past 7500 years was constructed. Using distribution patterns of coral biofacies and radiocarbon dates from corals, reconstruction of reef growth history indicates that both offshore and onshore reef zones were developing coevally, aggrading at rates of 4·3 mm year−1 from 6900 years B.P. The reef caught up with sea-level only after sea-level stabilized. Changes in coral community and reef growth rates were driven principally by increasing water agitation due to the decrease in accommodation space. Based on the composition of the successive coral assemblages, the reef appears to have grown through successive equilibrium stages.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 41 (1994), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Drill cores from Holocene reefs on Tahiti (French Polynesia) reveal a framework composed of massive branching acroporids encrusted by coralline algae associated with sessile vermetid gastropods and arborescent foraminifers. Laminated micritic crusts form coatings over coral branches or, more commonly, over related encrusting organisms throughout the cored reef sections; these crusts appear as a major structural and volumetric component of the reef framework. The microbial nature of these micritic crusts is inferred from their typical organic growth forms and geometry, the occurrence of microbial remains and stable isotope measurements. The reef communities accumulated at depths less than 5 m below mean sea level in a high energy environment throughout vertical growth from 7140 ± 170 yr bp to the present. The nature of the involved benthic communities, stable isotope data and high calcification rates of microbially encrusted corals strongly suggest that local environmental conditions have been optimal for reef development for the last 7000 years. The causes of the predominance of microbial communities over actual encrusters (red algae, foraminifers) remain problematic and could be related to short term fluctuations in ecological parameters. Microbial micritic crusts seemingly played a prominent role in protecting the coralgal colonies from bioeroders and grazers and, possibly, in strengthening the framework, due to rapid lithification. The record of similar microbial crusts in other Quaternary reef tracts suggests that microbial communities may have played a more prominent role in Quaternary reefs than presently recognized.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Barbados sea-level record8'9'17'18 suggested that the last deglaciation was characterized by two brief periods of accelerated melting superimposed on a smooth and continuous rise of sea level with no reversals. These so-called MWP-1A and MWP-1B events (14,000 and 11,300 calendar years BP, ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Coral reefs 10 (1991), S. 53-54 
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2024-01-09
    Keywords: 133-821A; Amphisteginidae; Anomalinidae; Bolivinitidae; Buliminidae; Calcarinidae; Caucasinidae; Ceratobuliminidae; Cibicididae; Coral Sea; Counting 〉125 µm fraction; Cymbaloporidae; DEPTH, sediment/rock; Discorbidae; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elphidiidae; Epistomariidae; Eponididae; Fischerinidae; Foraminifera, benthic deep water species; Foraminifera, benthic shallow water species; Glandulinidae; Joides Resolution; Leg133; Loxostomatidae; Miliolidae; Nodosariidae; Nonionidae; Nubeculariidae; Nummulitidae; Ocean Drilling Program; ODP; Rotaliidae; Sample code/label; Siphoninidae; Spirillinidae; Spritidae; Textulariidae; Turritinidae; Uvigerinidae
    Type: Dataset
    Format: text/tab-separated-values, 93 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 133-821A; Alveolinella quoyi; Ammonia beccarii; Amphistegina lessonii; Amphistegina lobifera; Amphistegina papillosa; Amphistegina radiata; Anomalina glabrata; Articulina pacifica; Asterorotalia gaimardii; Baculogypsina sphaerulata; Bifarina fimbriata; Bolivina amygdalaeformis; Bolivina compacta; Bolivina hantkeniana; Bolivina rhomboidalis; Bolivina semicostata; Bolivina subangularis; Bolivina subreticulata; Bolivinella elegans; Brizalina convallaria; Brizalina pacifica; Brizalina striatula; Buliminella latissima; Buliminella sp.; Buliminoides madagascariensis var. spicatus; Buliminoides williamsonianus; Calcarina calcar; Calcarina spengleri; Cibicides lobatulus; Cibicides mayori; Coral Sea; Cyclogyra involvens; Cymbaloporella tabellaeformis; DEPTH, sediment/rock; Discorbis mira; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elphidium advenum; Elphidium crispum; Epistomariella milletti; Fissurina marginata-perforata; Fissurina orbignyana; Fursenkoina pauciloculata; Gaudryina siphonifera; Gavelinopsis cf. lobatulus; Glabratella earlandi; Glabratella opercularis; Hauerina occidentalis; Heterolepa margaritifera; Heterolepa praecincta; Heterostegina depressa; Joides Resolution; Lagena cf. strumosa; Lamarckina scabra; Lamarckina ventricosa; Leg133; Loxostomum lobatum; Miliolinella australiana; Miliolinella baragwanathi; Monalysidium politum; Neoconorbina terquemi; Neoconorbina tuberocapitata; Neoeponides berthelotianus; Nonion subturgidum; Ocean Drilling Program; ODP; Operculina cf. ammonoides; Parrellina milletti; Patellinella carinata; Peneroplis pertusus; Planispirinella exigua; Planorbulinella larvata; Poroeponides lateralis; Pyrgo denticulata; Pyrgo oblonga; Quinqueloculina bosciana; Quinqueloculina crassicarinata; Quinqueloculina curta; Quinqueloculina distorqueata; Quinqueloculina granulocostata; Quinqueloculina lamarckiana; Quinqueloculina oblonga; Quinqueloculina poyeana carinata; Quinqueloculina pseudoreticulata; Quinqueloculina sp.; Rectobolivina raphana; Reussella simplex; Sample code/label; Sigmavirgulina tortuosa; Siphogenerina virgula; Siphonina tubulosa; Siphotextularia sp.; Siphouvigerina ampullacea; Sorites spp.; Spirillina vivipara; Spiroloculina communis; Spirosigmoilina parri; Svratkina tuberculata; Textularia agglutinans; Textularia candeina; Textularia cf. pseudogramen; Textularia conica; Textularia fistulosa; Textularia sagittula; Tretomphalus spp.; Trifarina bradyi; Triloculina eburnea; Triloculina tricarinata; Triloculina trigonula; Uvigerina porrecta; Vertebralina striata; Wiesnerella auriculata
    Type: Dataset
    Format: text/tab-separated-values, 728 data points
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