DC pole | Wartość | Język |
dc.contributor.author | Żurek, Sławomir | - |
dc.contributor.author | Nita, Małgorzata | - |
dc.contributor.author | Imioł, Katarzyna | - |
dc.date.accessioned | 2019-08-05T07:21:48Z | - |
dc.date.available | 2019-08-05T07:21:48Z | - |
dc.date.issued | 2011 | - |
dc.identifier.citation | Bulletin of Geography. Physical Geography Series, 2011, vol. 4, iss. 1, p. 89-102 | pl_PL |
dc.identifier.issn | 2080-7686 | - |
dc.identifier.issn | 2300-8490 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/10499 | - |
dc.description.abstract | Macroscopic and laboratory tests of over 4-metre-thick organic
deposits of Krzywopłoty profile (gyttjas and peat) allowed the authors
to identify the development of the peatland as having four phases, each
transition being associated with fluctuations in water level. Sediments from
a depth of 3.75–0.65 m were also included in palynological testing. Seven
local pollen assemblage zones show a continuous transformation in the plant
landscape and surroundings of the site between the end of the Vistulian
and the Holocene. Pollen data indicates a change of vegetation, from open
communities of herbaceous plants and loose pine-birch communities in the
Younger Dryas, then dense pine forests in the Preboreal chronozone, and
finally multispecies forests in the Atlantic and Subboreal chronozones. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/pl/ | * |
dc.subject | Holocene | pl_PL |
dc.subject | Mire | pl_PL |
dc.subject | Pollen analysis | pl_PL |
dc.subject | Peatland | pl_PL |
dc.subject | Krzywopłoty | pl_PL |
dc.subject | Bydlin Area | pl_PL |
dc.title | Krzywopłoty – Late Glacial and Holocene Mire in the Bydlin Area (Częstochowa Upland) | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.2478/bgeo-2011-0005 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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