DC pole | Wartość | Język |
dc.contributor.author | Hrynowiecka, Anna | - |
dc.contributor.author | Szymczyk, Artur | - |
dc.date.accessioned | 2019-08-05T07:21:00Z | - |
dc.date.available | 2019-08-05T07:21:00Z | - |
dc.date.issued | 2011 | - |
dc.identifier.citation | Bulletin of Geography. Physical Geography Series, 2011, vol. 4, iss. 1, p. 21-45b | pl_PL |
dc.identifier.issn | 2080-7686 | - |
dc.identifier.issn | 2300-8490 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/10497 | - |
dc.description.abstract | The environmental variability during the Mazovian/Holsteinian
interglacial is better understood thanks to the results of multidisciplinary
palaeobotanical studies. The perfectly preserved and abundant material
from Nowiny Żukowskie in SE Poland has been the subject of numerous
palaeobotanical analyses. The results both of initial pollen analysis and of the
examination of plant macroremains provide a detailed view of changes in the
palaeoenvironment of this area during the Mazovian/Holsteinian interglacial.
Originally, the water basin was mostly the habitat of plants indicative
of low trophy. The frequent occurence of swamp plants evidences a change
in hydrological and climatic conditions consistent with the intra-interglacial
climatic oscillation. In the subsequent part of the optimum, an expansion
of swamps with Aracites interglacialis and Dulichium arundinaceum was
recorded. The development of a peat bog overgrown by i.a. Sphagnum
sp., Eriophorum vaginatum, and Andromeda polifolia was also observed.
The growth of swamp and peat vegetation resulted in the nearly complete
disappearance of aquatic vegetation, apart from species typical of the climatic
optimum of the Mazovian/Holsteinian interglacial: Brasenia borysthenica
and Aldrovanda dokturovskyi. The close of the interglacial was marked by the intensive development of peat bog and swamp communities with Carex
rostrata, Menyanthes trifoliata, and A. interglacialis. The intensive increase
in the number of A. interglacialis during the period described as the “birch
oscillation” supports the hypothesis of noticeable changes in hydrological
conditions at that time. The end of the described period is typified by
a deterioration of climatic conditions, indicated by the increase in values
for Betula humilis, B. nana, and Juniperus communis. | 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 | Mazovian/Holsteinian interglacial | pl_PL |
dc.subject | Pollen analysis | pl_PL |
dc.subject | Macroremains | pl_PL |
dc.subject | Palaeoenvironment | pl_PL |
dc.subject | SE Poland | pl_PL |
dc.title | Comprehensive Palaeobotanical Studies of Lacustrine-Peat Bog Sediments from the Mazovian/ Holsteinian Interglacial at the Site of Nowiny Żukowskie (Se Poland) – Preliminary Study | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.2478/bgeo-2011-0002 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
|