A bodrogkeresztúri lösz-paleotalaj szelvény környezettörténeti és üledékföldtani vizsgálata
The loess-paleosol profile, which was deepen at Bodrogkeresztúr in 2014 was made to get better and more accurate understanding about the conditions of the paleoenvironment in the Carpathian foothills and the Gravettian culture which is found near at Henye site. Based on historical information, the s...
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| Testületi szerző: | |
| Dokumentumtípus: | Könyv része |
| Megjelent: |
2020
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| Sorozat: | Közép-európai Monográfiák
27 Magyarok a Kárpát-medencében 4. : régmúlt és jelen 27 |
| Kulcsszavak: | Környezettörténet, Paleoökológia |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/73249 |
| Tartalmi kivonat: | The loess-paleosol profile, which was deepen at Bodrogkeresztúr in 2014 was made to get better and more accurate understanding about the conditions of the paleoenvironment in the Carpathian foothills and the Gravettian culture which is found near at Henye site. Based on historical information, the section starts in late Marine Isotope Stage 3 (later MIS 3) and continues up to the recent soil sediment. This study deals with the analysis of the grains size, organic matter and carbonate content and the presentation of the age-depth models based on the comparison of Kopasz hill’s OSL and 14C and Bodrogkeresztúr I’s 14C ages and the accumulation rates derived from the modells. From sedimentological studies it was found that the profile is characterized by more significant accumulation, on average smaller particle size, and almost complete absence of sand fraction. All about these data the former investigated Bodrogkeresztúr 1, and Bodrogkeresztúr - Henye are very similar to the Kopasz hill site. In addition, the entire section is characterized by increased carbonate content due to post-sedimentation processes, recarbonization and leaching. |
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| Terjedelem/Fizikai jellemzők: | 131-140 |
| ISBN: | 9 78-963-89 724-9-1 |
| ISSN: | 2062-3712 |