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Permafrost Soils
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 permafro...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor Corporativo: | |
| Otros Autores: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Berlin, Heidelberg :
Springer Berlin Heidelberg : Imprint: Springer,
2009.
|
| Edición: | 1st ed. 2009. |
| Colección: | Soil Biology,
16 |
| Temas: | |
| Acceso en línea: | Texto Completo |
MARC
| LEADER | 00000nam a22000005i 4500 | ||
|---|---|---|---|
| 001 | 978-3-540-69371-0 | ||
| 003 | DE-He213 | ||
| 005 | 20220113153022.0 | ||
| 007 | cr nn 008mamaa | ||
| 008 | 100301s2009 gw | s |||| 0|eng d | ||
| 020 | |a 9783540693710 |9 978-3-540-69371-0 | ||
| 024 | 7 | |a 10.1007/978-3-540-69371-0 |2 doi | |
| 050 | 4 | |a QE471-471.15 | |
| 072 | 7 | |a RBGB |2 bicssc | |
| 072 | 7 | |a SCI091000 |2 bisacsh | |
| 072 | 7 | |a RBGB |2 thema | |
| 082 | 0 | 4 | |a 551.3 |2 23 |
| 245 | 1 | 0 | |a Permafrost Soils |h [electronic resource] / |c edited by Rosa Margesin. |
| 250 | |a 1st ed. 2009. | ||
| 264 | 1 | |a Berlin, Heidelberg : |b Springer Berlin Heidelberg : |b Imprint: Springer, |c 2009. | |
| 300 | |a XIV, 348 p. 78 illus., 4 illus. in color. |b online resource. | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 347 | |a text file |b PDF |2 rda | ||
| 490 | 1 | |a Soil Biology, |x 2196-4831 ; |v 16 | |
| 505 | 0 | |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. | |
| 520 | |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. | ||
| 650 | 0 | |a Sedimentology. | |
| 650 | 0 | |a Biodiversity. | |
| 650 | 0 | |a Environment. | |
| 650 | 0 | |a Microbial ecology. | |
| 650 | 0 | |a Microbial genetics. | |
| 650 | 0 | |a Astrobiology. | |
| 650 | 1 | 4 | |a Sedimentology. |
| 650 | 2 | 4 | |a Biodiversity. |
| 650 | 2 | 4 | |a Environmental Sciences. |
| 650 | 2 | 4 | |a Microbial Ecology. |
| 650 | 2 | 4 | |a Microbial Genetics. |
| 650 | 2 | 4 | |a Astrobiology. |
| 700 | 1 | |a Margesin, Rosa. |e editor. |4 edt |4 http://id.loc.gov/vocabulary/relators/edt | |
| 710 | 2 | |a SpringerLink (Online service) | |
| 773 | 0 | |t Springer Nature eBook | |
| 776 | 0 | 8 | |i Printed edition: |z 9783540865438 |
| 776 | 0 | 8 | |i Printed edition: |z 9783642088872 |
| 776 | 0 | 8 | |i Printed edition: |z 9783540693703 |
| 830 | 0 | |a Soil Biology, |x 2196-4831 ; |v 16 | |
| 856 | 4 | 0 | |u https://doi.uam.elogim.com/10.1007/978-3-540-69371-0 |z Texto Completo |
| 912 | |a ZDB-2-SBL | ||
| 912 | |a ZDB-2-SXB | ||
| 950 | |a Biomedical and Life Sciences (SpringerNature-11642) | ||
| 950 | |a Biomedical and Life Sciences (R0) (SpringerNature-43708) | ||