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  • 1
    Electronic Resource
    Electronic Resource
    DNA fingerprint analysis of a free-range koala population (1993)
    Springer
    Biochemical genetics 31 (1993), S. 363-374 
    Details
    ISSN: 1573-4927
    Keywords: koala ; free-range population ; DNA fingerprint ; database
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology
    Notes: Abstract Thirty-six koalas in a free-range Queensland population were fingerprinted using an M13 probe in combination withMspI digestion. The technique was found to be highly repeatable, with estimates of 0.1–1.6% within-gel error and 0.1–2.5% between-gel error. Of the 43 different-size fingerprint bands produced in the population, only 2 bands were common to all 36 koalas. Ten bands were quite rare, occurring at a frequency of 0.2 or less. All 36 koalas had unique DNA fingerprints (probability of 1.88×10−7), which enabled them each to be uniquely identified. Despite this, there was still a high level of band sharing in the population (mean number of shared bands =0.749). This level is much higher than that reported for humans, birds, cats, dogs, and cattle but not as high as that reported previously for Victorian koalas. This lack of genetic variation may influence the ability of the population to respond to stress situations, such as lack of food, habitat destruction, and disease.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00553455
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  • 2
    Electronic Resource
    Electronic Resource
    DNA fingerprint analysis of a free-range koala population (1993)
    Springer
    Biochemical genetics 31 (1993), S. 363-374 
    Details
    ISSN: 1573-4927
    Keywords: koala ; free-range population ; DNA fingerprint ; database
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology
    Notes: Abstract Thirty-six koalas in a free-range Queensland population were fingerprinted using an M13 probe in combination withMspI digestion. The technique was found to be highly repeatable, with estimates of 0.1–1.6% within-gel error and 0.1–2.5% between-gel error. Of the 43 different-size fingerprint bands produced in the population, only 2 bands were common to all 36 koalas. Ten bands were quite rare, occurring at a frequency of 0.2 or less. All 36 koalas had unique DNA fingerprints (probability of 1.88×10−7), which enabled them each to be uniquely identified. Despite this, there was still a high level of band sharing in the population (mean number of shared bands =0.749). This level is much higher than that reported for humans, birds, cats, dogs, and cattle but not as high as that reported previously for Victorian koalas. This lack of genetic variation may influence the ability of the population to respond to stress situations, such as lack of food, habitat destruction, and disease.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02396223
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  • 3
    Electronic Resource
    Electronic Resource
    Trends of Minimum and Maximum Daily Temperatures in Italy from 1865 to 1996 (2000)
    Springer
    Theoretical and applied climatology 66 (2000), S. 49-60 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Annual and seasonal changes in maximum and minimum temperatures (Tmax and Tmin) and in daily temperature range (DTR) in Italy are investigated. Monthly average series for northern and southern Italy are analysed for evidence of trend. Tmax and Tmin show a positive trend over the period 1865–1996 which is greater in southern Italy than in northern Italy. DTR shows a positive trend, but greater in the North than in the South. There is a positive correlation between DTR and mean monthly temperature especially in spring and in summer, while there is a high significant negative correlation between DTR and monthly precipitation. Analysis of temperature, precipitation and DTR during the period 1865–1996 suggests that a general relationship between the very warm last 15–20 years and an increase in the frequency of sub-tropical anticyclones over the Central-Western Mediterranean. This relationship is based on the hypothesis that in Italy more frequent sub-tropical anticyclones could have been the most characteristic feature of the warm periods during the last 130 years.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s007040070032
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  • 4
    Electronic Resource
    Electronic Resource
    Surface Air Temperature Variations in Italy: Recent Trends and an Update to 1993 (1998)
    Springer
    Theoretical and applied climatology 61 (1998), S. 191-196 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Historical series of monthly mean temperatures from 27 Italian stations, updated to 1993, are analysed. Building on previous analysis the following new results were obtained: there is an upward trend in seasonal and annual temperatures during the last 20 years; a positive trend, stronger at southern stations compared to northern stations, is apparent from 1920 to 1950, after when temperature shows no significant trend until 1985 when it starts to increase again. Data from Northern Italy show similar characteristics to a subset of data from a global climatic database, for the period 1881–1988. This comparison, however, suggests that good station coverage is important for the construction of a more detailed picture of seasonal climate variability.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s007040050063
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  • 5
    Electronic Resource
    Electronic Resource
    Variations of Temperature and Precipitation in Italy from 1866 to 1995 (2000)
    Springer
    Theoretical and applied climatology 65 (2000), S. 165-174 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Series of annual and seasonal temperature and precipitation representing respectively northern and southern Italy are compared for trend, interannual variability and periodicity in the period 1866–1995. Temperature and precipitation trends are almost always anticorrelated except in winter in the North where an anomalous behavior is evident till about 1980. The result is that the Italian climate has become warmer and drier especially in the South since about 1930.The interannual variability does not present significant maxima, but only minima that cannot be related tothe start of a trend either for temperature or for precipitation. The power spectra of the series show broad significant peaks containing the quasi-biennial oscillation and other well known periodicities probably due to solar cycles or to the North Atlantic ocean-atmosphere oscillation (NAO).
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s007040070041
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  • 6
    Electronic Resource
    Electronic Resource
    Precipitation in Italy from 1833 to 1996 (1999)
    Springer
    Theoretical and applied climatology 63 (1999), S. 33-40 
    Details
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary  Series of annual and seasonal precipitation from 32 stations, distributed over all Italian territory and divided in two groups climatically homogeneous, were studied for the period 1833–1996. The series were checked for homogeneity and the time series analysis was performed with the Mann Kendall test and its progressive application according to Sneyers (1990). The results show considerably different trends for different seasons and zones. On a yearly basis a decreasing trend is present over all Italy, but it is statistically significant only in the Central-South. On a seasonal basis a decreasing trend is significant only for spring in Central-South, and for autumn in the North.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s007040050089
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  • 7
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    Effect of Ru substitution on atomic displacements in the layered SmFe_{1−x}Ru_{x}AsO_{0.85}F_{0.15} superconductor (2012)
    American Physical Society (APS)
    Details
    Publication Date: 2012-06-28
    Description: Author(s): A. Iadecola, B. Joseph, L. Simonelli, L. Maugeri, M. Fratini, A. Martinelli, A. Palenzona, M. Putti, and N. L. Saini The effect of Ru substitution on the local structure of layered SmFe 1− x Ru x AsO 0.85 F 0.15 superconductor has been studied by As K - and Sm L 3 -edge x-ray-absorption spectroscopy. The extended x-ray-absorption fine-structure measurements reveal distinct Fe-As and Ru-As bond lengths in the Ru substituted s... [Phys. Rev. B 85, 214530] Published Wed Jun 27, 2012
    Keywords: Superfluidity and superconductivity
    Print ISSN: 1098-0121
    Electronic ISSN: 1095-3795
    Topics: Physics
    Published by American Physical Society (APS)
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  • 8
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    DNA fingerprint analysis of a free-range koala population (1993)
    Springer
    Details
    Publication Date: 1993-10-01
    Print ISSN: 0006-2928
    Electronic ISSN: 1573-4927
    Topics: Biology , Chemistry and Pharmacology
    Published by Springer
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  • 9
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    Numerical Modelling of a Shaking Table Test for Soil-Foundation-Superstructure Interaction by Means of a Soil Constitutive Model Implemented in a FEM Code (2009)
    Springer
    Details
    Publication Date: 2009-10-25
    Print ISSN: 0960-3182
    Electronic ISSN: 1573-1529
    Topics: Geosciences
    Published by Springer
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  • 10
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    Air temperature thresholds to evaluate snow melting at the surface of Alpine glaciers by T-index models: the case study of Forni Glacier (Italy) (2014)
    Copernicus
    Details
    Publication Date: 2014-03-18
    Description: The glacier melt conditions (i.e.: null surface temperature and positive energy budget) can be assessed by analyzing meteorological and energy data acquired by a supraglacial Automatic Weather Station (AWS). In the case this latter is not present the assessment of actual melting conditions and the evaluation of the melt amount is difficult and simple methods based on T-index (or degree days) models are generally applied. These models require the choice of a correct temperature threshold. In fact, melt does not necessarily occur at daily air temperatures higher than 273.15 K. In this paper, to detect the most indicative threshold witnessing melt conditions in the April–June period, we have analyzed air temperature data recorded from 2006 to 2012 by a supraglacial AWS set up at 2631 m a.s.l. on the ablation tongue of the Forni Glacier (Italian Alps), and by a weather station located outside the studied glacier (at Bormio, a village at 1225 m a.s.l.). Moreover we have evaluated the glacier energy budget and the Snow Water Equivalent (SWE) values during this time-frame. Then the snow ablation amount was estimated both from the surface energy balance (from supraglacial AWS data) and from T-index method (from Bormio data, applying the mean tropospheric lapse rate and varying the air temperature threshold) and the results were compared. We found that the mean tropospheric lapse rate permits a good and reliable reconstruction of glacier air temperatures and the major uncertainty in the computation of snow melt is driven by the choice of an appropriate temperature threshold. From our study using a 5.0 K lower threshold value (with respect to the largely applied 273.15 K) permits the most reliable reconstruction of glacier melt.
    Print ISSN: 1994-0432
    Electronic ISSN: 1994-0440
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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