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rdf:type
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Description
| - Loess-palaeosol records in Central Siberia indicate establishment of periglacial steppe-tundra during OIS 4 and OIS 2, replaced by parkland steppe and boreal forest during warmer intervals within OIS 3. A gradual transition from parkland-steppe (OIS 5a) to moist tundra conditions (OIS 4) occurred ~75 ka BP. General cooling, punctuated by isolated short warm intervals, marked the period from ~75 to ~25 ka BP. OIS 2, ~25-18 ka BP, was marked by a sharp change to a dry tundra climate, followed by rapid arming ~15-8 ka BP. Mid- and latest Holocene conditions were warmer than those recorded during the OIS 5e maximum. Textural, magnetic susceptibility, and mineralogical analyses indicate that the OIS 4 and OIS 2 loess units were derived from different
- Loess-palaeosol records in Central Siberia indicate establishment of periglacial steppe-tundra during OIS 4 and OIS 2, replaced by parkland steppe and boreal forest during warmer intervals within OIS 3. A gradual transition from parkland-steppe (OIS 5a) to moist tundra conditions (OIS 4) occurred ~75 ka BP. General cooling, punctuated by isolated short warm intervals, marked the period from ~75 to ~25 ka BP. OIS 2, ~25-18 ka BP, was marked by a sharp change to a dry tundra climate, followed by rapid arming ~15-8 ka BP. Mid- and latest Holocene conditions were warmer than those recorded during the OIS 5e maximum. Textural, magnetic susceptibility, and mineralogical analyses indicate that the OIS 4 and OIS 2 loess units were derived from different (en)
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Title
| - Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia
- Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia (en)
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skos:prefLabel
| - Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia
- Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia (en)
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skos:notation
| - RIV/00025798:_____/03:00000103!RIV/2004/MZP/N03004/N
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http://linked.open.../vavai/riv/strany
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/00025798:_____/03:00000103
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Paleomagnetism, Paleoclimatology, Loess, Palaeosol, Late Quaternary, Central Siberia (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...ontrolniKodProRIV
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http://linked.open...v/mistoKonaniAkce
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http://linked.open...i/riv/mistoVydani
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http://linked.open...i/riv/nazevZdroje
| - XVI INQUA Congress Programs with Abstracts
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...ocetUcastnikuAkce
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http://linked.open...nichUcastnikuAkce
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http://linked.open...UplatneniVysledku
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http://linked.open...iv/tvurceVysledku
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http://linked.open...vavai/riv/typAkce
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http://linked.open.../riv/zahajeniAkce
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http://linked.open...n/vavai/riv/zamer
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number of pages
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http://purl.org/ne...btex#hasPublisher
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https://schema.org/isbn
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