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04396nam a22005655i 4500 |
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978-3-540-69371-0 |
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DE-He213 |
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20151204184241.0 |
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|a 9783540693710
|9 978-3-540-69371-0
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|a 10.1007/978-3-540-69371-0
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|a QE471-471.15
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|a SCI091000
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|a 551.3
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|a Permafrost Soils
|h [electronic resource] /
|c edited by Rosa Margesin.
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|a Berlin, Heidelberg :
|b Springer Berlin Heidelberg,
|c 2009.
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|a XIV, 348 p. 78 illus., 4 illus. in color.
|b online resource.
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|a text
|b txt
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|a computer
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|a online resource
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|a text file
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|a Soil Biology,
|x 1613-3382 ;
|v 16
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|a Geological, Chemical and Physical Properties of Permafrost -- Arctic Permafrost Soils -- Antarctic Permafrost Soils -- Mountain Permafrost -- Biodiversity in Permafrost -- Very Old DNA -- Bacterial and Archaeal Diversity in Permafrost -- Viable Cyanobacteria and Green Algae from the Permafrost Darkness -- Fungi in Permafrost -- Ancient Protozoa Isolated from Permafrost -- Biological Activity in Permafrost -- Microbial Activity in Frozen Soils -- Anaerobic Ammonium Oxidation (Anammox) -- Genomic Insights into Cold Adaptation of Permafrost Bacteria -- Proteomic Insights: Cryoadaptation of Permafrost Bacteria -- Impact of Global Warming On Permafrost Properties -- Global Warming and Thermokarst -- Global Warming and Mountain Permafrost -- Global Warming and Carbon Dynamics in Permafrost Soils: Methane Production and Oxidation -- Global Warming and Dissolved Organic Carbon Release from Permafrost Soils -- Climate Change and Foundations of Buildings in Permafrost Regions -- Contaminants in Frozen Ground -- Migration of Petroleum in Permafrost-Affected Regions -- Remediation of Frozen Ground Contaminated with Petroleum Hydrocarbons: Feasibility and Limits -- Application of Reactive Barriers Operated in Frozen Ground -- Permafrost on Earth – A Model for Extraterrestrial Habitats -- Terrestrial Permafrost Models and Analogues of Martian Habitats and Inhabitants.
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|a Most of the Earth’s biosphere is characterized by low temperatures. Vast areas (>20%) of the soil ecosystem are permanently frozen or are unfrozen for only a few weeks in summer. Permafrost regions occur at high latitudes and also at high ele- tions; a significant part of the global permafrost area is represented by mountains. Permafrost soils are of global interest, since a significant increase in temperature is predicted for polar regions. Global warming will have a great impact on these soils, especially in northern regions, since they contain large amounts of organic carbon and act as carbon sinks, and a temperature increase will result in a release of carbon into the atmosphere. Additionally, the intensified release of the clima- relevant tracer gas methane represents a potential environmental harzard. Significant numbers of viable microorganisms, including bacteria, archaea, p- totrophic cyanobacteria and green algae, fungi and protozoa, are present in per- frost, and the characteristics of these microorganisms reflect the unique and extreme conditions of the permafrost environment. Remarkably, these microorg- isms have been reported to be metabolically active at subzero temperatures, even down to ?20°C.
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|a Earth sciences.
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|a Sedimentology.
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|a Biodiversity.
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|a Microbial ecology.
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|a Microbial genetics.
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|a Microbial genomics.
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|a Astrobiology.
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|a Climate change.
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|a Earth Sciences.
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|a Sedimentology.
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|a Biodiversity.
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|a Climate Change.
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|a Microbial Ecology.
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|a Microbial Genetics and Genomics.
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|a Astrobiology.
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|a Margesin, Rosa.
|e editor.
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|a SpringerLink (Online service)
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|t Springer eBooks
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776 |
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|i Printed edition:
|z 9783540693703
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|a Soil Biology,
|x 1613-3382 ;
|v 16
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|u http://dx.doi.org/10.1007/978-3-540-69371-0
|z Full Text via HEAL-Link
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|a ZDB-2-SBL
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|a Biomedical and Life Sciences (Springer-11642)
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