Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy
Results of archaeological studies from the territory of Poland show that prehistorical settlements were often founded on the banks of lakes and mires. Botanical composition of organic deposits allows reconstructing historical plant communities and palaeohydrological conditions of the settlement, the...
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Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie
2008-12-01
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| Series: | Studia Ecologiae et Bioethicae |
| Online Access: | https://czasopisma.uksw.edu.pl/index.php/seb/article/view/7571 |
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| author | Krzysztof J. Wójcicki Marek Kloss |
| author_facet | Krzysztof J. Wójcicki Marek Kloss |
| author_sort | Krzysztof J. Wójcicki |
| collection | DOAJ |
| description | Results of archaeological studies from the territory of Poland show that prehistorical settlements were often founded on the banks of lakes and mires. Botanical composition of organic deposits allows reconstructing historical plant communities and palaeohydrological conditions of the settlement, the subject of research was a peatland situated in the neighborhood of the archaeological site at Łany Małe. The latter is located on hillslopes of the Kłodnica valley (Upper Silesia, southern Poland). Peat formation at the Łany Małe site took place in the Pre-Boreal Period as an effect of the valley floor paludification. In the Mesolithic and Neolithic Periods as well as the Early Bronze Age, swampy alder forests occupied the entire area of the peatland. At that time, the fen surface was relatively easily accessible for humans, especially for people of the Funnel Beaker Culture in the Middle Neolithic Period. It was then when, probably, the ground water level dropped down and peat decay processes took over those of peat production. In the Hallstatt Period, during the presence of the Lusatian Culture settlement, there was subsequent increase in biotope moisture. Forest communities became more open and trees were gradually displaced by grasslike plants, especially of sedge (Carex) genus. In the Fate Roman Period (the Przeworsk Culture settlement) and in the early Middle Ages, the peatland was subject to inundation due to frequent flooding, the peat accumulation was then halted by the delivery of fine-grained products of soil erosion. |
| format | Article |
| id | doaj-art-8e666f94a17a4fb3a7663b7208ba5221 |
| institution | Kabale University |
| issn | 1733-1218 |
| language | English |
| publishDate | 2008-12-01 |
| publisher | Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie |
| record_format | Article |
| series | Studia Ecologiae et Bioethicae |
| spelling | doaj-art-8e666f94a17a4fb3a7663b7208ba52212025-02-02T23:29:48ZengUniwersytet Kardynała Stefana Wyszyńskiego w WarszawieStudia Ecologiae et Bioethicae1733-12182008-12-016110.21697/seb.2008.6.1.31Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie KłodnicyKrzysztof J. Wójcicki0Marek Kloss1Wydział Nauk o Ziemi, Uniwersytet Śląski w Katowicach,Instytut Ekologii i Bioetyki, Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie,Results of archaeological studies from the territory of Poland show that prehistorical settlements were often founded on the banks of lakes and mires. Botanical composition of organic deposits allows reconstructing historical plant communities and palaeohydrological conditions of the settlement, the subject of research was a peatland situated in the neighborhood of the archaeological site at Łany Małe. The latter is located on hillslopes of the Kłodnica valley (Upper Silesia, southern Poland). Peat formation at the Łany Małe site took place in the Pre-Boreal Period as an effect of the valley floor paludification. In the Mesolithic and Neolithic Periods as well as the Early Bronze Age, swampy alder forests occupied the entire area of the peatland. At that time, the fen surface was relatively easily accessible for humans, especially for people of the Funnel Beaker Culture in the Middle Neolithic Period. It was then when, probably, the ground water level dropped down and peat decay processes took over those of peat production. In the Hallstatt Period, during the presence of the Lusatian Culture settlement, there was subsequent increase in biotope moisture. Forest communities became more open and trees were gradually displaced by grasslike plants, especially of sedge (Carex) genus. In the Fate Roman Period (the Przeworsk Culture settlement) and in the early Middle Ages, the peatland was subject to inundation due to frequent flooding, the peat accumulation was then halted by the delivery of fine-grained products of soil erosion.https://czasopisma.uksw.edu.pl/index.php/seb/article/view/7571 |
| spellingShingle | Krzysztof J. Wójcicki Marek Kloss Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy Studia Ecologiae et Bioethicae |
| title | Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy |
| title_full | Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy |
| title_fullStr | Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy |
| title_full_unstemmed | Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy |
| title_short | Makroszczątki roślinne w torfie w analizie paleośrodowiskowych uwarunkowań osadnictwa na przykładzie stanowiska Łane Małe w dolinie Kłodnicy |
| title_sort | makroszczatki roslinne w torfie w analizie paleosrodowiskowych uwarunkowan osadnictwa na przykladzie stanowiska lane male w dolinie klodnicy |
| url | https://czasopisma.uksw.edu.pl/index.php/seb/article/view/7571 |
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