The last 40,000 years of a floodplain area (Tisza, Hungary) comparative case study of 14C and OSL methods
Datos Bibliográficos
| ID | 6447951 |
|---|---|
| Autores | Titanilla Kertész (0000-0002-8448-1379), Katalin Hubay (0000-0002-7630-193X), Botond Búró (0000-0002-2173-1537), A J T Jull (0000-0002-4079-4947), Andrea Mindszenty (0000-0001-8927-3053), György Sipos (0000-0001-6224-2361), Tamás Bartyik (0000-0003-1608-4889), Miklós Molnár (0000-0003-4382-9508) |
| Año | 2025 |
| Volumen | 67 |
| Número | 3 |
| Páginas | 656-678 |
| Fecha de publicación | 2025-03-31 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Radiocarbon (JOURNAL) |
| Identificadores de la revista | ISSN: 0033-8222 • E-ISSN: 1945-5755 |
| Editorial | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/rdc.2024.140 |
| OpenAlex | W4408998785 |
| Idioma | EN |
| Citas recibidas | 1 |
| Referencias citadas | 72 |
To investigate the environmental history of the Tisza River (Hungary), we applied 14 C and OSL dating methods for five parallel, neighboring cores from the flood plain area (Jászság Basin). Four major sedimentary layers were identified: meadow soil on the top (S1); silty-clay (S2); clayey-silt (S3) section; and fine sand (S4). 14 C and OSL data were integrated into a synthetic age-depth model using the BACON software package. Formation of the S1 layer (depth: 0–1.0 m) falls in the Holocene, up to 10 kyrs cal BP, with moderate sedimentation rate (100 yr/cm aAR). The S2 layer (1.0–8.0 m depth) represent the entire Last Glacial to Upper Pleniglacial period (19–27 kyrs cal BP), with a much faster sedimentation (20 yr/cm aAr). The S3 section (8.0–17.0 m) represents a longer period (27–45 kyrs cal BP) with similar sedimentation rate (19 yr/cm aAr) as S2. These clayey silt layers fall into the Late Pleistocene/Middle Pleniglacial period, a period of nearly 18 kyrs of sedimentation resulting ∼9 m thick sediment. Our study delivered some new and important details about the surface evolution of the investigated Tiszasüly area. A missing part of about 10 kyrs period (between 10–19 kyrs cal BP) was revealed in the investigated synthetic cores
Absolute dating · Archaeology · Floodplain · Geography · Radiocarbon dating · Geological formations and processes · Geology and Paleoclimatology Research · Marine and environmental studies · Geology
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| Obras citantes distintas | 1 |
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| Citas por año | 1 |
| Intervalo de citas | 2026 - 2026 (1) |
| Velocidad de citación | current |
| Altamente citado | No |
| Tipos de cita | Neutras: 1 |