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
Language
  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Anoxic zones. ; Eukaryotic cells--Evolution. ; Adaptation (Physiology). ; Extreme environments--Microbiology. ; Anaerobiosis. ; Micropaleontology. ; Eukaryota. ; Adaptation, Physiological. ; Biological Evolution. ; Paleontology. ; Electronic books.
    Description / Table of Contents: This volume presents a collection of remarkable adaptations to anoxia, observed in protists, fungi, plants and animals. The text presents case studies that provide evidence for controlled beneficial use of anoxia, like organic modification of free radicals, for example.
    Type of Medium: Online Resource
    Pages: 1 online resource (641 pages)
    Edition: 1st ed.
    ISBN: 9789400718968
    Series Statement: Cellular Origin, Life in Extreme Habitats and Astrobiology Series ; v.21
    Language: English
    Note: Intro -- Anoxia -- Table of Contents -- Introduction to Anoxia: Evidence for Eukaryotesurvival and Paleontological Strategies -- Stepping into the Book of Anoxia and Eukaryotes -- References -- List of Authors and their Addresses -- List of External Reviewers and Referees -- Acknowledgments -- Part I: General Introduction -- Anaerobic Eukaryotes -- 1. Anoxia: An Extreme Environment? -- 2. Anaerobic Multicellular Eukaryotes -- 3. Anaerobic Unicellular Eukaryotes -- 3.1. Mitochondria, Hydrogenosomes, and Mitosomes -- 3.2. Facultative Anaerobic Protists -- 3.3. Coping with Anoxia Using Endosymbiotic Phototrophs -- 4. Sensitivity to Oxygen -- 5. Sterol Synthesis -- 6. Prokaryote Symbionts -- 6.1. Methanogens -- 6.2. Ectosymbiotic Bacteria -- 6.3. Phototrophic Endosymbionts -- 7. Energy Metabolism and the Structure of Anaerobic Communities -- 8. The Origin of Anaerobic Eukaryotes -- 9. References -- Biogeochemical Reactions in Marine Sediments Underlying Anoxic Water Bodies -- 1. Introduction -- 2. Sediment Biogeochemistry in Modern Oxygenated Oceans -- 2.1. Range and Variations of Oxygen Availability in Sediments -- 3. Changes in Sedimentary Biogeochemical Reactions Under Hypoxia and Anoxia -- 3.1. Biogeochemical Processes in Naturally Occurring Oxygen Minimum Zones on Continental Margins -- 3.2. Biogeochemical Processes in Sediments Underlying Euxinic Water Bodies -- 4. Anoxia Through Time -- 4.1. Biogeochemical Processes in Sediments During Ocean Anoxic Events -- 4.2. The Initial Early Earth Anoxia and Changes During the First Rise of Oxygen -- 5. References -- Diversity of Anaerobic Prokaryotes and Eukaryotes: Breaking Long-Established Dogmas -- 1. Introduction -- 2. Novel Types of Anaerobic Metabolism in the Prokaryotic World -- 3. Anaerobic Metabolism in the Eukaryotic World: Revisited -- 4. References -- Part II: Functional Biochemistry. , The Biochemical Adaptations of Mitochondrion-Related Organelles of Parasitic and Free-Living Microbial Eukaryotes to Low Oxygen Environments -- 1. Introduction -- 1.1. Mitochondria and Mitochondrion-Related Organelles -- 2. Protein Import into Mitochondrion-Related Organelles -- 3. Organellar Substrate Exchange: The Mitochondrial Carrier Family -- 4. Iron-Sulfur Cluster Assembly -- 5. Pyruvate Metabolism -- 5.1. Malate Decarboxylation -- 6. [FeFe]-Hydrogenase -- 6.1. Evolutionary Relationships Among [FeFe]-Hydrogenases -- 7. ATP-Generation from Acetyl-CoA in Microbial Eukaryotes -- 8. Conclusions -- 10. References -- Hydrogenosomes and Mitosomes: Mitochondrial Adaptations to Life in Anaerobic Environments -- 1. Introduction -- 2. Anaerobic Protists: Diversity and Distribution of Hydrogenosomes and Related Organelles -- 3. Mitochondrial Genomes -- 4. Hydrogenosomes -- 4.1. Trichomonas -- 4.2. Trimastix pyriformis -- 4.3. Neocallimastix sp. and Piromyces E2 -- 4.4. Blastocystis sp. -- 4.5. Anaerobic Ciliates -- 4.6. Nyctotherus ovalis -- 5. Mitosomes -- 5.1 Entamoeba histolytica -- 5.2. Mastigamoeba balamuthi -- 5.3. Encephalitozoon cuniculi, Antonospora locustae, Trachipleistophora hominis -- 5.4. Cryptosporidium parvum -- 5.5. Giardia sp. -- 6. Conclusions and Discussion -- 7. References -- Adapting to Hypoxia: Lessons from Vascular Endothelial Growth Factor -- 1. Introduction -- 2. Increased Gene Transcription -- 3. Increased mRNA Stability -- 4. Translational Regulation -- 5. Summary and Future Perspectives -- 6. References -- Part III: Managing Anoxia -- Magnetotactic Protists at the Oxic-Anoxic Transition Zones of Coastal Aquatic Environments -- 1. Introduction -- 2. Discovery of Magnetotactic Protists -- 3. Magnetotactic Protists at Salt Pond -- 3.1. Types of Magnetotactic Protists -- 3.2. Behavior of Magnetotactic Protists. , 3.3. "Magnetosomes" in Magnetotactic Protists? -- 4. Origin of Magnetite in Magnetotactic Protists -- 5. Role of Magnetotactic Protists in Iron Cycling -- 6. Future Research Directions -- 8. References -- A Novel Ciliate (Ciliophora: Hypotrichida) Isolated from Bathyal Anoxic Sediments -- 1. Introduction -- 2. Materials and Methods -- 3. Results and Discussion -- 4. Conclusion -- 5. References -- The Wood-Eating Termite Hindgut: Diverse Cellular Symbioses in a Microoxic to Anoxic Environment -- 1. Introduction -- 2. Evolution of the Termite Hindgut -- 3. The Microoxic to Anoxic Gut Environment -- 4. Diversity of Organisms in the Gut -- 4.1. Protists -- 4.2. Spirochetes -- 5. Early Cell Evolution Analogs -- 6. Recent Discoveries -- 6.1. Co-evolution -- 6.2. Whole Genome of Endosymbionts -- 7. Genetic Diversity Versus Morphological Complexity -- 8. References -- Ecological and Experimental Exposure of Insects to Anoxia Reveals Surprising Tolerance -- 1. Introduction -- 1.1. Evolution of Insects and Early Terrestrial Conditions -- 1.2. Aquatic Insects and Anoxia -- 2. Insect Respiration Patterns and Hypoxia/Hyperoxia -- 2.1. Discontinuous Gas Exchange -- 3. Insects Exposed to Hypoxic/Anoxic Conditions -- 3.1. Terrestrial Insects and Flooding -- 3.2. Immersion of Economically Important Species -- 3.3. High Altitude Hypoxia and Anoxia Associated with Freezing -- 3.4. Other Severely Hypoxic Environments -- 3.5. Use of Modified Atmospheres to Manage Insect Pests -- 3.6. Insect Response to Severe Hypoxia and Anoxia -- 4. Prospectus -- 5. References -- The Unusual Response of Encysted Embryos of the Animal Extremophile, Artemia franciscana , to Prolonged Anoxia -- 1. Introduction -- 2. Encysted Embryos of Artemia franciscana -- 3. The Structure of Encysted Embryos -- 4. The Longevity and Metabolic Status of Anoxic Embryos. , 5. The Matter of the Free-Energy Requirement for Living Systems -- 6. How Are the Proteins of Anoxic Embryos Protected? -- 6.1. Control of Proteases -- 6.2. Stress Proteins/Molecular Chaperones -- 6.2.1. Artemin -- 6.2.2. The Small Heat Shock Protein p26 -- 6.3. Late Embryogenesis Abundant (Lea) Proteins -- 6.4. Trehalose -- 7. Concluding Comments -- 9. References -- Survival of Tardigrades in Extreme Environments: A Model Animal for Astrobiology -- 1. Introduction -- 2. Anhydrobiosis in Tardigrades -- 3. Radiation Tolerance -- 4. Tolerance to Low and High Temperatures -- 5. Tolerance to Low and High Pressures -- 6. Exposure to Actual and Simulated Extraterrestrial Environments -- 7. Conclusion -- 9. References -- Long-Term Anoxia Tolerance in Flowering Plants -- 1. Prevalence of Anoxia in Flowering Plants -- 1.1. Anoxia in the Arctic -- 1.2. Anoxia and the American Cranberry -- 1.3. Natural Anoxia in Seeds -- 2. Evolution of Flooding Tolerance -- 3. Survival Strategies for Anoxia Avoidance -- 3.1. Short-Term Anoxia Tolerance -- 3.2. Long-Term Anoxia Tolerance -- 3.2.1. Foliar Tolerance of Anoxia -- 3.2.2. Adaptations for Winter Survival Under Anoxia -- 3.2.3. End Products of Glycolysis and the Accumulation of the Oxygen Debt -- 4. Post-anoxic Injury and the Dangers of Un-flooding -- 5. Anoxia Sensing in Plants -- 6. Ecological Advantages of Anoxia Tolerance -- 8. References -- Part IV: Foraminifera -- Benthic Foraminifera: Inhabitants of Low-Oxygen Environments -- 1. Introduction -- 2. Spatial Distribution: Foraminiferal Communities Living in Low-Oxygen Settings -- 2.1. Seasonally Low-Oxygen Environments -- 2.2. Permanent Low-Oxygen Environments -- 3. Foraminiferal Depth Zonation in Sediment: Oxic, Hypoxic, and Anoxic Microhabitats -- 3.1. Foraminiferal Species Living in Hypoxic and Anoxic Microhabitats -- 3.1.1. Intermediate Infauna. , 3.1.2. Deep Infauna -- 3.1.3 Infauna with Variable Microhabitat -- 3.2. Test Chemistry: Relation to Foraminiferal Microhabitat -- 4. Experimental Evidence -- 5. Survival Strategies in Low-Oxygen Environments -- 5.1. Internal Nitrate Pool and Denitrification -- 5.2. Foraminiferal Cell Ultrastructure, Including Chloroplast Sequestration -- 5.3. Bacterial Symbionts -- 6. Outlook into Future Research Directions -- 8. References -- Ecological and Biological Response of Benthic Foraminifera Under Oxygen-Depleted Conditions: Evidence from Laboratory Approaches -- 1. Introduction -- 2. Laboratory Methodologies -- 3. Survival Experiments -- 4. Orientation in the Sediment: Foraminiferal Aerotaxis? -- 5. Sediment Oxidation and the Influence of Bioturbation -- 6. Foraminiferal Metabolism Under Oxic and Anoxic Conditions -- 7. References -- The Response of Benthic Foraminifera to Low-Oxygen Conditions of the Peruvian Oxygen Minimum Zone -- 1. Introduction -- 2. Study Area -- 3. Materials and Methods -- 3.1. Sample Processing -- 3.2. Environmental Data -- 4. Species Distribution Patterns of Benthic Foraminifera in the OMZ Off Peru -- 5. Discussion -- 5.1. Species Patterns -- 5.2. A New Proxy for Estimation of Bottom Water Oxygen Concentrations -- Appendix 1: Faunal Reference List -- Appendix 2: Supplementary Data -- 7. References -- Benthic Foraminiferal Communities and Microhabitat Selection on the Continental Shelf Off Central Peru -- 1. Introduction -- 2. Material and Methods -- 3. Results -- 3.1. Oceanographic Setting and Sediment Properties -- 3.2. Benthic Foraminiferal Assemblages and Vertical Distribution -- 4. Discussion -- 4.1. Benthic Foraminiferal Assemblages and Biogeochemical Conditions -- 4.2. Vertical Distribution and Microhabitat Selection -- 4.3. Virgulinella fragilis and H 2 S Concentration -- 5. Conclusions -- 7. References. , Part V: Zones and Regions.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Type of Medium: Book
    Pages: 249 S , graph. Darst., Kt
    Series Statement: Berichte aus dem Sonderforschungsbereich 313 28
    Language: German
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Type of Medium: Book
    Pages: 155 S , Ill., graph. Darst., Tab , 30 cm
    Series Statement: Berichte aus dem Sonderforschungsbereich 313, Sedimentation im Europäischen Nordmeer Nr. 19
    Language: German
    Note: Literaturangaben
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Keywords: Dissertation ; Meteor ; Foraminiferen ; Nordatlantik ; Hochschulschrift
    Type of Medium: Book
    Pages: 167 S , graph. Darst., Kt , 21 cm
    Language: German
    Note: Literaturverz. S 121 - 132 , Kiel, Univ., Diss., 1985
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Book
    Book
    Kiel : Sonderforschungsbereich 313, Univ.
    Type of Medium: Book
    Pages: 87 S. , Ill., graph. Darst.
    Series Statement: Berichte aus dem Sonderforschungsbereich 313 "Sedimentation im Europäischen Nordmeer" 6
    Language: German
    Note: Beitr. teilw. dt., teilw. engl , Intermediärsprache: Englisch
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Keywords: Aufsatzsammlung ; Festschrift ; Biografie ; Norddeutschland ; Mikropaläontologie ; Mikropaläontologie
    Type of Medium: Book
    Pages: 265 S. , Ill., graphische Darst., Kt.
    Series Statement: Geologisches Jahrbuch 128
    Language: German
    Note: Bibliographie H. Hiltermann S. 9 - 16
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    In: Journal of foraminiferal research, Alexandria, Va. : GeoScienceWorld, 1971, 39(2009), 4, Seite 361-363, 0096-1191
    In: volume:39
    In: year:2009
    In: number:4
    In: pages:361-363
    Type of Medium: Online Resource
    Pages: Ill
    ISSN: 0096-1191
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: 95, XV S , graph. Darst., Kt , 30 cm
    Language: German
    Note: Kiel, Univ., Habil.-Schr. : 1993
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lutze, Gerhard F; Altenbach, Alexander V (1988): Rupertina stabilis (WALLICH), a highly adapted, suspension feeding foraminifer. Meyniana, 40, 55-69, https://doi.org/10.2312/meyniana.1988.40.55
    Publication Date: 2024-02-02
    Description: Rupertina stabilis occupies a depth restricted biotope of suspension feeding animals situated at the Norwegian continental margin. It extends from the Voring plateau northwards for at least 200 - 300 km, in depths between 600 and 800 m. This slope position is known for relatively strong bottom currents and shifting watermass boundaries. - The species is attached to hard substrates, mainly stones or hydroid stalks and obviously prefers an elevated position. It is building a permanent cyst of sponge spicules and debris at the apertural region. The spicules are used to support a pseudopodial network similar to that described from Halyphysema (LIPPS 1983). It is believed to serve as a filter apparatus. - A review of known occurences in the Atlantic is given, suggesting a temperature adaption of the species ranging from 0°C to a maximum of 8°C. Specimens were successfully cultured for about 2-3 weeks.
    Keywords: Date/Time of event; Elevation of event; Event label; Foraminifera, benthic, biomass as carbon; Foraminifera, benthic, standing stock; Giant box corer; GIK23000-2; GIK23014-1; GIK23015-1; GIK23016-1; GIK23022-1; GIK23023-1; GIK23027-1; GIK23076-1; GIK23222; GIK23237; GKG; Latitude of event; Longitude of event; M2/2; Meteor (1986); Norwegian Sea; P284-2; P309-1; P317; P318; POS119; Poseidon; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 2 mm, gravel; Size fraction 2.000-0.063 mm, sand; Voring Plateau
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 84 (1995), S. 89-107 
    ISSN: 1437-3262
    Keywords: Paleo-oceanography ; Abrupt climatic change ; Deep-sea micropaleontology ; Late Quaternary ; North Atlantic ; Atlantic Salinity Conveyor Belt
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Quantitative and semiquantitative proxy data based on more than 200 core-top samples and 100 deep-sea cores lead to important new insights about late Quaternary changes in paleo-oceanography, climate and microfaunal habitats in the north-eastern North Atlantic and Nordic Seas, insights resulting from a detailed investigation by the Kiel research project SFB 313/132 summarized in this paper. Planktonic foraminifera species provide reliable tracers of past sea surface temperatures and currents. The genus Beella in particular was found to trace subtropical water masses up to the far north. Benthic foraminifera species served as sensors of bottom currents and local flux rates of organic matter. New orders of time resolution are reached via stable isotope stratigraphy and accelerator mass spectrometry carbon-14 dating, allowing the identification of meltwater events lasting a few hundred years and shorter, a time range where, however, the yet unquantified role of bioturbation presents a growing problem. Based on this high-resolution stratigraphy a number of ‘time slices’ (synoptic time intervals) are defined to reconstruct the incursion of Atlantic water masses, to map paleocurrent patterns within the Nordic Seas and the north-eastern North Atlantic and to test alternative circulation models — for example, for the last glacial maximum (LGM) and various meltwater episodes. These are clearly coeval with Dansgaard-Oeschger events found in Greenland ice cores, with the actual cause of the flickering climate as yet unknown. Likewise, there is ongoing controversy about the extent of past sea-ice cover and about possible changes from the present anti-estuarine to estuarine mode of deep water exchange between the North Atlantic and the Nordic Seas during the LGM. South of Iceland, however, the history of deep water renewal over the last glacial cycle covering the last 30000 years was largely deciphered.
    Type of Medium: Electronic Resource
    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...