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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 434 (2005), S. 749-752 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Grain size reduction and gouge formation are found to be ubiquitous in brittle faults at all scales, and most slip along mature faults is observed to have been localized within gouge zones. This fine-grain gouge is thought to control earthquake instability, and thus understanding its ...
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Wilson, Brent (2012): Percentage carrying capacity in fossil successions: A new ecostratigraphic tool with potential for detecting palaeoenvironmental change illustrated using bathyal benthic foraminifera in the Late Quaternary of ODP Hole 1006A, Santaren Channel. Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 143-150, https://doi.org/10.1016/j.palaeo.2012.04.008
    Publication Date: 2024-02-03
    Description: The percent carrying capacity Kp is the equilibrium population in percentage terms of a species that an area can support while adequately meeting the needs of every individual. It is readily determined from a time series of percentage abundances for a species, in which pit is the percentage abundance of the ith species at time t. The percentage point change in abundance of a species Dpi between two samples is given by Dpi = pit + 1 − pit, where pit + 1 is the percentage abundance at a subsequent time t + 1. The rate of population change in percentage points for each percent at a given time or point t, here termed rt, is given by rt = Dpi/pit. Linear regression of rt against pit gives rt = rm–s · pit, in which the constant rm is the rate of increase in rt where pit approaches zero, and the negative slope s represents the combined strength of intraspecific, interspecific and abiotic interactions for the species investigated. Setting rt = 0, so that pit = Kp and rm–s · Kp = 0, gives Kp = rm/s. The Upper Quaternary of ODP 1006A contains two subsections with rich bathyal benthic foraminiferal assemblages separated by samples yielding few specimens. Values of rm, s and Kp were calculated for five species (Globocassidulina subglobosa, Planulina ariminensis, Cibicidoides pachyderma, Cassidulina laevigata, Uvigerina laevis) within these subsections and 95% confidence intervals were computed for rm and s. The rate of change of the percentage abundance for each percent rt, as indicated by the slope s, differs between species (P. ariminensis and C. pachyderma vs. C. laevigata) and can also vary within a single species over time (G. subglobosa). Likewise, values of rm differ between species (P. ariminensis vs. C. pachyderma) and can also change within a single species over time (G. subglobosa). Points of change from one value of Kp to another in a stratigraphic section mark regime shifts and have potential for ecostratigraphic correlation. Within the Upper Quaternary of ODP Hole 1006A they apparently reflect an increase in the organic matter flux in the uppermost part of the section. The method described here can be applied to any species in any taxon for which percentage data are available. For those in the hydrocarbon industry it should prove especially useful for detailed studies of intervals of economic interest.
    Keywords: 166-1006A; Cassidulina laevigata; Cibicidoides pachyderma; Counting 〉105 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Foraminifera, benthic bathyal; Globocassidulina subglobosa; Joides Resolution; Leg166; Ocean Drilling Program; ODP; Planulina ariminensis; Sample code/label; Sample position; South Atlantic Ocean; Uvigerina laevis
    Type: Dataset
    Format: text/tab-separated-values, 580 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Haynert, Kristin; Schönfeld, Joachim; Schiebel, Ralf; Wilson, Brent; Thomsen, Jörn (2014): Response of benthic foraminifera to ocean acidification in their natural sediment environment: a long-term culturing experiment. Biogeosciences, 11(6), 1581-1597, https://doi.org/10.5194/bg-11-1581-2014
    Publication Date: 2024-03-15
    Description: Calcifying foraminifera are expected to be endangered by ocean acidification; however, the response of a complete community kept in natural sediment and over multiple generations under controlled laboratory conditions has not been constrained to date. During 6 months of incubation, foraminiferal assemblages were kept and treated in natural sediment with pCO2-enriched seawater of 430, 907, 1865 and 3247 µatm pCO2. The fauna was dominated by Ammonia aomoriensis and Elphidium species, whereas agglutinated species were rare. After 6 months of incubation, pore water alkalinity was much higher in comparison to the overlying seawater. Consequently, the saturation state of Omega calc was much higher in the sediment than in the water column in nearly all pCO2 treatments and remained close to saturation. As a result, the life cycle (population density, growth and reproduction) of living assemblages varied markedly during the experimental period, but was largely unaffected by the pCO2 treatments applied. According to the size-frequency distribution, we conclude that foraminifera start reproduction at a diameter of 250 µm. Mortality of living Ammonia aomoriensis was unaffected, whereas size of large and dead tests decreased with elevated pCO2 from 285 µm (pCO2 from 430 to 1865 µatm) to 258 µm (pCO2 3247 µatm). The total organic content of living Ammonia aomoriensis has been determined to be 4.3% of CaCO3 weight. Living individuals had a calcium carbonate production rate of 0.47 g/m**2/a, whereas dead empty tests accumulated a rate of 0.27 g /m**2/a. Although Omega calc was close to 1, approximately 30% of the empty tests of Ammonia aomoriensis showed dissolution features at high pCO2 of 3247 µatm during the last 2 months of incubation. In contrast, tests of the subdominant species, Elphidium incertum, stayed intact. Our results emphasize that the sensitivity to ocean acidification of the endobenthic foraminifera Ammonia aomoriensis in their natural sediment habitat is much lower compared to the experimental response of specimens isolated from the sediment.
    Keywords: Abundance; Abundance, standard deviation; Alkalinity, total; Ammonia aomoriensis; Ammotium cassis; Aragonite saturation state; Armorella sphaerica; Baltic Sea; Benthos; Bicarbonate ion; Calcite saturation state; Calcium carbonate, mass; Calcium carbonate, mass per individual; Calcium carbonate, mass per individual, standard deviation; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Colorimetric; Comment; Community composition and diversity; Coulometric titration; Diameter; Diameter, standard deviation; Elphidium excavatum clavatum; Elphidium excavatum excavatum; Elphidium gerthi; Elphidium incertum; Entire community; EXP; Experiment; Field observation; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Incubation duration; Individuals; Kiel_fjord; Mass; Mass, standard deviation; Number of specimens; Number of specimens, standard deviation; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Percentage; Percentage, standard deviation; pH; pH, standard deviation; Phosphate; Phosphate, standard deviation; Potentiometric; Reophax dentaliniformis; Replicate; Replicates; Salinity; Salinity, standard deviation; Silicate; Silicate, standard deviation; Size; Soft-bottom community; Species; Table; Temperate; Temperature, water; Temperature, water, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 30268 data points
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  • 4
    Publication Date: 2020-06-16
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 5
    Publication Date: 2007-03-01
    Print ISSN: 0021-9584
    Electronic ISSN: 1938-1328
    Topics: Chemistry and Pharmacology , Education
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  • 6
    Publication Date: 2020-03-03
    Description: The perceived replication crisis and the reforms designed to address it are grounded in the notion that science is a binary signal detection problem. However, contrary to null hypothesis significance testing (NHST) logic, the magnitude of the underlying effect size for a given experiment is best conceptualized as a random draw from a continuous distribution, not as a random draw from a dichotomous distribution (null vs. alternative). Moreover, because continuously distributed effects selected using aP〈 0.05 filter must be inflated, the fact that they are smaller when replicated (reflecting regression to the mean) is no reason to sound the alarm. Considered from this perspective, recent replication efforts suggest that most publishedP〈 0.05 scientific findings are “true” (i.e., in the correct direction), with observed effect sizes that are inflated to varying degrees. We propose that original science is a screening process, one that adopts NHST logic as a useful fiction for selecting true effects that are potentially large enough to be of interest to other scientists. Unlike original science, replication science seeks to precisely measure the underlying effect size associated with an experimental protocol via large-Ndirect replication, without regard for statistical significance. Registered reports are well suited to (often resource-intensive) direct replications, which should focus on influential findings and be published regardless of outcome. Conceptual replications play an important but separate role in validating theories. However, because they are part of NHST-based original science, conceptual replications cannot serve as the field’s self-correction mechanism. Only direct replications can do that.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Publication Date: 2011-01-01
    Description: The 3.85 m-long piston core En20-10, from the NE Caribbean Sea (17{degrees}02.2'N, 63{degrees}03.3'W, 885 m water depth) comprises hemipelagic sediment interrupted by calcareous turbidites at ~160-200 cm. SHE Analysis for Biozone Identification (SHEBI) revealed four abundance biozones (ABs), one of which (AB2) was coincident with the turbidites. The AB3/AB4 boundary may be coincident with the Pleistocene/Holocene boundary. The {alpha} diversities ranged 22.6-36.0 effective species, being lowest in AB2 and highest in the succeeding AB3. The {beta} diversities were 0.728-1.593. However, only the {beta} diversity across the AB2/AB3 boundary was significant. This indicates that the major control of {alpha} diversity was sedimentological, low {alpha} being associated with the turbidites. The {beta} diversity across the AB3/AB4 boundary was not significant, which implies that the environmental change at the end of the Pleistocene that impacted the composition of the bathyal fauna did not influence {alpha} diversity.
    Print ISSN: 0096-1191
    Topics: Geosciences
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  • 8
    Publication Date: 2012-07-01
    Print ISSN: 0078-0421
    Electronic ISSN: 0078-0421
    Topics: Geosciences
    Published by Schweizerbart
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  • 9
    Publication Date: 2011-10-01
    Description: Deep Sea Drilling Project Hole 148 was drilled on the Aves Ridge, eastern Caribbean Sea at a lower-bathyal depth (1232 m) beneath the eastern edge of the Orinoco plume. The drillhole penetrated ~124 m of Pleistocene sediment, but core recovery was poor (66%). From 62 samples taken at ~2-m intervals, 17,259 〉105-m benthonic foraminifera were picked and 212 species were identified. Only four species accounted for 〉5% of the total recovery: Sigmoilopsis schlumbergeri, Uvigerina peregrina, U. auberiana, and Bulimina aculeata. Species of Uvigerina and Bulimina, indicative of organic loading and low dissolved-oxygen content, respectively formed 22.6% and 14.3% of total recovery. Cibicidoides bradyi formed 4.4% of total recovery and Globocassidulina subglobosa 3.3%. This indicates that, although the Caribbean Sea is bordered to the north, east, and west by oligotrophic waters, the Pleistocene in DSDP Hole 148 was deposited under organic-rich, low-oxygen conditions. The organic material was derived from high surface productivity within the nutrient-rich Orinoco plume. Uvigerina and Bulimina show a long-term ecostratigraphic signal, beginning with U. hispida and B. alazanensis being common in the lower part of the section, then U. peregrina and B. aculeata in the middle and U. peregrina and U. dirupta in the upper part. This succession may reflect temporal changes in surface productivity, possibly resulting from plate tectonic movement of DSDP Hole 148 relative to the Orinoco plume, as surface productivity generally decreases from the center to the margins of the plume. The Stilostomella Extinction, in which uniserial foraminifera decreased through the section, occurred through a gradual loss of specimens.
    Print ISSN: 0096-1191
    Topics: Geosciences
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  • 10
    Publication Date: 2011-03-01
    Description: There is not yet a precise classification of or terminology for ecostratigraphic boundaries. SHE analysis for biozone identification (SHEBI) objectively places boundaries between abundance biozones (ABs). Alpha diversity ( = SE = eH, where H is the information function) measures the community diversity within an AB in units of effective species, whereas the dimensionless {beta} diversity ( = SE2/SE1, where SE1 and SE2 are the [α] diversities of successive ABs) quantifies the difference in [α] diversity between successive ABs. Three categories of AB boundary are recognized depending on the value of {beta}. In Type -1{beta}, the [α] diversity of the younger AB is significantly less than that of the older. In Type 0{beta}, SE2 {approx} SE1, while in Type +1{beta}, the [α] diversity of the younger AB is significantly greater than in the older. Benthonic foraminifera were sampled from the [~]124-m-thick Pleistocene strata of DSDP Hole 148 (eastern Caribbean Sea). SHEBI indicated 18 ABs; of the 17 AB boundaries, seven were Type -1{beta}, two were Type 0{beta}, and eight, Type +1{beta}. The direction of inflection of the graph of lnE versus lnN did not indicate AB boundary type. Although the Pleistocene was characterized by repeated alternations between glacial and interglacial conditions, there was no regular alternation of Type -1{beta} and +1{beta} AB boundaries. Complementarity (i.e., species level distinctiveness of successive ABs) was measured using a percentage similarity index, CP. Differing complimentarities show that boundaries between ABs varied with respect to permeability to species, while beta diversities and CP were uncorrelated.
    Print ISSN: 0883-1351
    Electronic ISSN: 0883-1351
    Topics: Geosciences
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