Az ócsai láp archeomalakológiai vizsgálata - A Pomatias elegans elso{combining double acute accent} radiokarbon adatokkal korolt holocén elo{combining double acute accent}fordulása Magyarországon

Translated title of the contribution: First radiocarbon-dated holocene record of Pomatias elegans in Hungary - Results of complex archeomalacological investigations from the Marshland of Ócsa

Zsolt Veres, P. Sümegi, Tünde Törocsik

Research output: Contribution to journalArticle

Abstract

The Selyemrét of Ócsa is located on the northern part of the Duna-Tisza Interfluve at the transitional zone of two landscapes with different morphological characters. At the boundary of the Duna-Tisza Interfluve and the Dunamenti Plain in Bács-Kiskun County a marshland sequence can be found from Hajós to Ócsa. Since there have been environmental historical analysis on the southern part of the area earlier, we extended our research project to the bog of Ócsa as well. The bog of Ócsa is located in a former pool formed by the Danube River in which eolic sand and thick lake sequence deposited from the end of the Pleistocene. The initial oligotrophic lake became mesotrophic, therefore thick carbonate sediment deposited. Afterwards, as a consequence of the Neolithic human populations the natural development of the lake changed drastically and the lake filled up. The pollen and quarter malacological analysis of the area support the mentioned geological processes.

Original languageHungarian
Pages (from-to)181-196
Number of pages16
JournalArcheometriai Muhely
Volume8
Issue number2
Publication statusPublished - 2011

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Hungary
Radiocarbon
Holocene
Marshland
Historical Analysis
Danube
Sediment
Research Projects
Carbonate
Pleistocene
Pollen

ASJC Scopus subject areas

  • Archaeology

Cite this

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abstract = "The Selyemr{\'e}t of {\'O}csa is located on the northern part of the Duna-Tisza Interfluve at the transitional zone of two landscapes with different morphological characters. At the boundary of the Duna-Tisza Interfluve and the Dunamenti Plain in B{\'a}cs-Kiskun County a marshland sequence can be found from Haj{\'o}s to {\'O}csa. Since there have been environmental historical analysis on the southern part of the area earlier, we extended our research project to the bog of {\'O}csa as well. The bog of {\'O}csa is located in a former pool formed by the Danube River in which eolic sand and thick lake sequence deposited from the end of the Pleistocene. The initial oligotrophic lake became mesotrophic, therefore thick carbonate sediment deposited. Afterwards, as a consequence of the Neolithic human populations the natural development of the lake changed drastically and the lake filled up. The pollen and quarter malacological analysis of the area support the mentioned geological processes.",
keywords = "Bog, Environmental historical analysis, Selyemr{\'e}t",
author = "Zsolt Veres and P. S{\"u}megi and T{\"u}nde T{\"o}rocsik",
year = "2011",
language = "Hungarian",
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publisher = "Hungarian National Museum",
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AU - Veres, Zsolt

AU - Sümegi, P.

AU - Törocsik, Tünde

PY - 2011

Y1 - 2011

N2 - The Selyemrét of Ócsa is located on the northern part of the Duna-Tisza Interfluve at the transitional zone of two landscapes with different morphological characters. At the boundary of the Duna-Tisza Interfluve and the Dunamenti Plain in Bács-Kiskun County a marshland sequence can be found from Hajós to Ócsa. Since there have been environmental historical analysis on the southern part of the area earlier, we extended our research project to the bog of Ócsa as well. The bog of Ócsa is located in a former pool formed by the Danube River in which eolic sand and thick lake sequence deposited from the end of the Pleistocene. The initial oligotrophic lake became mesotrophic, therefore thick carbonate sediment deposited. Afterwards, as a consequence of the Neolithic human populations the natural development of the lake changed drastically and the lake filled up. The pollen and quarter malacological analysis of the area support the mentioned geological processes.

AB - The Selyemrét of Ócsa is located on the northern part of the Duna-Tisza Interfluve at the transitional zone of two landscapes with different morphological characters. At the boundary of the Duna-Tisza Interfluve and the Dunamenti Plain in Bács-Kiskun County a marshland sequence can be found from Hajós to Ócsa. Since there have been environmental historical analysis on the southern part of the area earlier, we extended our research project to the bog of Ócsa as well. The bog of Ócsa is located in a former pool formed by the Danube River in which eolic sand and thick lake sequence deposited from the end of the Pleistocene. The initial oligotrophic lake became mesotrophic, therefore thick carbonate sediment deposited. Afterwards, as a consequence of the Neolithic human populations the natural development of the lake changed drastically and the lake filled up. The pollen and quarter malacological analysis of the area support the mentioned geological processes.

KW - Bog

KW - Environmental historical analysis

KW - Selyemrét

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