Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2022
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| _version_ | 1867171030888349696 |
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| author | Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
| author_facet | Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_939682 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna AGE; Age, dated material; Age, error; Age, radiocarbon; Bykovsky_Peninsula-1; Cape_Sabler; Chukotka, Russia; Duvanny_Yar-1; ELEVATION; Event label; Gyda_settlement; Krasnoyarsk, Russia; Kular_Settl-2; Late Pleistocene; Latitude of event; Ledovy_Obryv; Location; Longitude of event; Molotkovsky_Kamen_Section; Mongatalyangyakha_River-1; MULT; Multiple investigations; North Yakutia, Russia; organic; organic accumulation; Permafrost; Radiocarbon dating; Reference/source; Sakha Republic, Russia; Sample comment; Sample ID; Seyakha_settlement; syngenetic ice-wedges; Ust-Algan_Obryv; Yamal-Nenets, Russia; Yamal Peninsula, northwestern Siberia; Zelyony_Mys_Settl Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. |
| title | Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone |
| topic | AGE; Age, dated material; Age, error; Age, radiocarbon; Bykovsky_Peninsula-1; Cape_Sabler; Chukotka, Russia; Duvanny_Yar-1; ELEVATION; Event label; Gyda_settlement; Krasnoyarsk, Russia; Kular_Settl-2; Late Pleistocene; Latitude of event; Ledovy_Obryv; Location; Longitude of event; Molotkovsky_Kamen_Section; Mongatalyangyakha_River-1; MULT; Multiple investigations; North Yakutia, Russia; organic; organic accumulation; Permafrost; Radiocarbon dating; Reference/source; Sakha Republic, Russia; Sample comment; Sample ID; Seyakha_settlement; syngenetic ice-wedges; Ust-Algan_Obryv; Yamal-Nenets, Russia; Yamal Peninsula, northwestern Siberia; Zelyony_Mys_Settl |
| url | https://doi.org/10.1594/PANGAEA.939682 |