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  • 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.
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 403 (2000), S. 77-80 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] It is generally agreed that the origin and initial diversification of Eucarya occurred in the late Archaean or Proterozoic Eons when atmospheric oxygen levels were low and the risk of DNA damage due to ultraviolet radiation was high. Because deep water provides refuge against ultraviolet ...
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 42 (1995), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: . Epifluorescence microscopy and spectrofluorimetry were investigated as possible non-terminal methods to distinguish live from dead foraminifera. Seven fluorogenic probes (diacetates of fluorescein [FDA], carboxyfluorescein, dichlorofluorescein, and carboxyeosin; AM-esters of biscarboxyethylcarboxyfluorescein [BCECF-AM], calcein, and calcein blue) were tested on Allogromia laticollaris. The probes that consistently produced the brightest fluorescence signals (BCECF-AM and FDA) were judged non-toxic to Allogromia, on the basis of short-term pseudopodial deployment and long-term reproduction assays. Once protocols were established, these two probes were tested on 13 additional benthic foraminiferal species. We found that BCECF-AM is the most suitable probe for direct epifluorescence microscopy of metabolically active foraminifera, especially tectinous and transparent calcareous species. Using spectrofluorimetry, FDA showed promise for opaque species because fluorescence is detected in the incubation media after its release from the cell. However, both approaches could only be used with confidence in light of appropriate controls established for each species examined.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 40 (1993), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: . The fine structure, elastic properties, and distribution of the fibrous, meshlike cement (bioadhesive) were studied for the test of the antarctic agglutinated foraminiferan Astrammina rara. Grain-size analysis of particles incorporated into the test compared with adjacent sediment indicates that A. rara is grain-size selective. Fractured tests curl inward, suggesting that the test is under tension—an impression substantiated by micromanipulation observations. Changes in test appearance were examined by scanning electron microscopy after sequential chemical treatments combined with ultrasonication. Organic fibrils securing fine-grained particulates on the test exterior were removed during initial sonication. A veil of fibrous organic material lining the test interior (i.e. inner organic lining) was removed by treatment with a nonionic detergent, revealing ligamentous cables of bioadhesive securely joining large grains. These cables are partially disrupted by treatment with sodium dodecyl sulfate, and further disrupted by disulfide reducing agents, suggesting that protein is an integral adhesive component. The large detrital grains incorporated into the test are arranged in an interlocked, optimally packed fashion. Together, these observations indicate that the seemingly simple spherical architecture of A. rara's test is in fact quite complex, consisting of large grains compressed by tensile cables of a proteinaceous bioadhesive, with additional rigidity supplied by fine particulate “mortar” deposited externally.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Inc
    The @journal of eukaryotic microbiology 52 (2005), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Eukaryote origin and earliest diversification occurred in the Proterozoic when Earth's atmosphere was undoubtedly different from that of today. Atmospheric oxygen levels were increasing from the primordial anoxic atmosphere due, for example, to cyanobacterial oxygenic photosynthesis. Late Proterozoic (∼0.6–0.9 Gya) deep-ocean oxygen concentrations are less certain, but geochemical evidence suggests anoxia and hydrogen-sulfide enrichment. It can, therefore, be postulated that initial eukaryotic diversification occurred in oxygen-depleted, sulfide-enriched environments. Foraminifera are aerobes and, thus, not expected in anoxic settings. Recently, however, we found a saccamminid allogromian in a deep-water anoxic, sulfidic setting. Samples were collected from Santa Barbara Basin (California) when bottom-water oxygen was undetectable and sediments smelled strongly of hydrogen sulfide. Foraminiferal SSU rDNA sequences recovered from sediments included one from a previously uncharacterized saccamminid. Ultrastructural analysis indicated the presence of intact Golgi, mitochondria, and prokaryotic endobionts. Saccamminid occurrence in environmental conditions known to exist during the Proterozoic supports the possibility of their origin early in eukaryotic evolution. Extant saccamminids could have competed well in the prokaryote-dominated Proterozoic benthic ecosystem given their diet includes bacteria, bacterial biofilms and unicellular algae. Thus, Proterozoic foraminifers may have been top carnivores.Funded by NASA NRA-01-01-EXB-057, the Geological Society of America's W. Storrs Cole Memorial Research Award, and NSF OPP0003639.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 15 (1991), S. 127-149 
    ISSN: 1573-515X
    Keywords: anoxia ; ATP ; foraminifera ; geochemistry ; organic-rich sediments ; ultrastructure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The pore-water geochemistry and benthic foraminiferal assemblages of sediments from two slope sites and within the central portion of the Santa Barbara Basin were characterized between February 1988 and July 1989. The highest foraminiferal numerical densities (1197 cm−3 as determined by an ATP assay) occurred at a slope site in June 1988 (550 m) in partially laminated sediments. In continuously laminated sediments from the central basin, foraminifera were found living (as determined by ATP assay) in October 1988 to depths of 4 cm, and specimens prepared for transmission electron microscopy were found with intact organelles to 3 cm, indicating their inhabitation of anoxic pore waters. Ultrastructural data from Nonionella stella is consistent with the hypothesis that this species can survive by anaerobic respiration. However, the benthic foraminifera appear unable to survive prolonged anoxia. The benthic foraminiferal population was completely dead in July 1989 when bottom water O2 was undetectable.
    Type of Medium: Electronic Resource
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: van Geen, Alexander; Zheng, Y; Bernhard, Joan M; Cannariato, Kevin G; Carriquiry, José D; Dean, Walter E; Eakins, B W; Ortiz, Joseph D; Pike, Jennifer (2003): On the preservation of laminated sediments along the western margin of North America. Paleoceanography, 18(4), 1098, https://doi.org/10.1029/2003PA000911
    Publication Date: 2023-05-12
    Description: Piston, gravity, and multicores as well as hydrographic data were collected along the Pacific margin of Baja California to reconstruct past variations in the intensity of the oxygen-minimum zone (OMZ). Gravity cores collected from within the OMZ north of 24°N did not contain laminated surface sediments even though bottom water oxygen (BWO) concentrations were close to 5 µmol/kg. However, many of the cores collected south of 24°N did contain millimeter- to centimeter-scale, brown to black laminations in Holocene and older sediments but not in sediments deposited during the Last Glacial Maximum. In addition to the dark laminations, Holocene sediments in Soledad Basin, silled at 290 m, also contain white coccolith laminae that probably represent individual blooms. Two open margin cores from 430 and 700 m depth that were selected for detailed radiocarbon dating show distinct transitions from bioturbated glacial sediment to laminated Holocene sediment occurring at 12.9 and 11.5 ka, respectively. The transition is delayed and more gradual (11.3-10.0 ka) in another dated core from Soledad Basin. The observations indicate that bottom-water oxygen concentrations dropped below a threshold for the preservation of laminations at different times or that a synchronous hydrographic change left an asynchronous sedimentary imprint due to local factors. With the caveat that laminated sections should therefore not be correlated without independent age control, the pattern of older sequences of laminations along the North American western margin reported by this and previous studies suggests that multiple patterns of regional productivity and ventilation prevailed over the past 60 kyr.
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, comment; Age, dated; Age, dated standard error; Calendar age; Calendar age, standard error; Depth, relative; DEPTH, sediment/rock; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Melville; MUC; MultiCorer; North Pacific/Gulf of California; OXMZ01MV; OXMZ01MV-GC31; OXMZ01MV-GC32; OXMZ01MV-GC38; OXMZ01MV-GC41; OXMZ01MV-MC17; OXMZ01MV-MC19; OXMZ01MV-PC08; OXMZ01MV-PC09; OXMZ01MV-PC10; OXMZ01MV-PC14; PC; Piston corer; Reservoir age; Reservoir age, standard error; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 438 data points
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  • 8
    Publication Date: 2024-03-15
    Description: Ocean chemistry is changing as a result of human activities. Atmospheric carbon dioxide (CO2) concentrations are increasing, causing an increase in oceanic pCO2 that drives a decrease in oceanic pH, a process called ocean acidification (OA). Higher CO2 concentrations are also linked to rising global temperatures that can result in more stratified surface waters, reducing the exchange between surface and deep waters; this stronger stratification, along with nutrient pollution, contributes to an expansion of oxygen-depleted zones (so called hypoxia or deoxygenation). Determining the response of marine organisms to environmental changes is important for assessments of future ecosystem functioning. While many studies have assessed the impact of individual or paired stressors, fewer studies have assessed the combined impact of pCO2, O2, and temperature. A long-term experiment (10 months) with different treatments of these three stressors was conducted to determine their sole or combined impact on the abundance and survival of a benthic foraminiferal community collected from a continental-shelf site. Foraminifera are well suited to such study because of their small size, relatively rapid growth, varied mineralogies and physiologies. Inoculation materials were collected from a 77-m deep site south of Woods Hole, MA. Very fine sediments (〈53 μm) were used as inoculum, to allow the entire community to respond. Thirty-eight morphologically identified taxa grew during the experiment. Multivariate statistical analysis indicates that hypoxia was the major driving factor distinguishing the yields, while warming was secondary. Species responses were not consistent, with different species being most abundant in different treatments. Some taxa grew in all of the triple-stressor samples. Results from the experiment suggest that foraminiferal species' responses will vary considerably, with some being negatively impacted by predicted environmental changes, while other taxa will tolerate, and perhaps even benefit, from deoxygenation, warming and OA.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calcite saturation state, standard deviation; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; Entire community; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Manometric; New_England_continental_shelf; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Oxygen; Oxygen, dissolved; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Potentiometric titration; Replicate; Salinity; Sample ID; Shannon Diversity Index; Soft-bottom community; Species; Species richness; Specimen count; Temperate; Temperature; Temperature, water; Treatment; Type
    Type: Dataset
    Format: text/tab-separated-values, 50320 data points
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: McIntyre-Wressnig, Anna; Bernhard, Joan M; Wit, Johannes C; McCorkle, Daniel C (2014): Ocean acidification not likely to affect the survival and fitness of two temperate benthic foraminiferal species: results from culture experiments. Journal of Foraminiferal Research, 44(4), 341-351, https://doi.org/10.2113/gsjfr.44.4.341
    Publication Date: 2024-03-15
    Description: Specimens of Bolivina argentea and Bulimina marginata, two widely distributed temperate benthic foraminiferal species, were cultured at constant temperature and controlled pCO2 (ambient, 1000 ppmv, and 2000 ppmv) for six weeks to assess the effect of elevated atmospheric CO2 concentrations on survival and fitness using Adenosine Triphosphate (ATP) analyses and on shell microfabric using high-resolution SEM and image analysis. To characterize the carbonate chemistry of the incubation seawater, total alkalinity and dissolved inorganic carbon were measured approximately every two weeks. Survival and fitness were not directly affected by elevated pCO2 and the concomitant decrease in seawater pH and calcite saturation states (Omega c), even when seawater was undersaturated with respect to calcite. These results differ from some previous observations that ocean acidification can cause a variety of effects on benthic foraminifera, including test dissolution, decreased growth, and mottling (loss of symbiont color in symbiont-bearing species), suggesting that the benthic foraminiferal response to ocean acidification may be species specific. If so, this implies that ocean acidification may lead to ecological winners and losers even within the same taxonomic group.
    Keywords: Adenosine 5-Triphosphate; Alkalinity, total; Aragonite saturation state; Benthos; Bicarbonate ion; Bolivina argentea; Bottles or small containers/Aquaria (〈20 L); Bulimina marginata; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Coast and continental shelf; Coulometric titration; Date; EXP; Experiment; Foraminifera; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Heterotrophic prokaryotes; Incubation duration; Laboratory experiment; Mortality/Survival; Mud_Patch; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Potentiometric titration; Salinity; Single species; Species; Survival; Temperate; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 783 data points
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  • 10
    Publication Date: 2024-03-15
    Description: Agglutinated foraminifera create a shell by assembling particles from the sediment and comprise a significant part of the foraminiferal fauna. Despite their high abundance and diversity, their response to environmental perturbations and climate change is relatively poorly studied. Here we present results from a culture experiment with four different species of agglutinating foraminifera incubated in artificial substrate and exposed to different pCO2 conditions, in either dysoxic or oxic settings. We observed species-specific reactions (i.e., reduced or increased chamber formation rates) to dysoxia and/or acidification. While chamber addition and/or survival rates of Miliammina fusca and Trochammina inflata were negatively impacted by either dysoxia or acidification, respectively, Textularia tenuissima and Spiroplectammina biformis had the highest survivorship and chamber addition rates with combined high pCO2 (2000 ppm) and low O2 (0.7 ml/l) conditions. The differential response of these species indicates that not all agglutinating foraminifera are well-adapted to conditions induced by predicted climate change, which may result in a shift in foraminiferal community composition.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calcite saturation state, standard deviation; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Calculated using seacarb after Orr et al. (2018); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, standard deviation; Chamber number; Chromista; Coast and continental shelf; EXP; Experiment; Foraminifera; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Fugacity of carbon dioxide in seawater, standard deviation; Growth/Morphology; Heterotrophic prokaryotes; Laboratory experiment; Miliammina fusca; Mortality/Survival; Mudpatch; North Pacific; Number of specimens; OA-ICC; Ocean Acidification International Coordination Centre; Oxygen; Oxygen, dissolved; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Percentage; pH; pH, standard deviation; Potentiometric titration; Registration number of species; Salinity; Single species; Species; Species interaction; Spiroplectammina biformis; Survival; Temperate; Temperature, water; Temperature, water, standard deviation; Textularia tenuissima; Treatment; Trochammina inflata; Type; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 586 data points
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