| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2025 |
| Язык | английский |
|
Елисеев Николай Алексеевич, автор
Жаринова Вероника Владимировна, автор
Куликова Анна Викторовна, автор
Мифтахутдинова Динара Надировна, автор
Нургалиева Нурия Гавазовна, автор
Силантьев Владимир Владимирович, автор
Уразаева Миляуша Назимовна, автор
|
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Тихомирова Марион , автор
|
| Библиографическое описание на языке оригинала |
1. Silantiev, V. V., Gutak, Y. M., Tichomirowa, M., Käßner, A., Kulikova, A. V., Arbuzov, S. I., Nourgalieva, N. G., Karasev, E. V., Felker, A. S., Naumcheva, M. A., Bakaev, A. S., Porokhovnichenko, L. G., Eliseev, N. A., Zharinova, V. V., Miftakhutdinova, D. N., & Urazaeva, M. N. (2025). Revisiting the Permian Stratigraphy of the Kuznetsk Coal Basin (Siberia, Russia) Using Radioisotopic Data: Sedimentology, Biotic Events, and Palaeoclimate. Minerals, 15(6), 643. |
| Аннотация |
Radioisotopic dating of five stratigraphic levels within the Permian succession of the Kuznetsk Coal Basin refines the ages of the corresponding stratigraphic units and, for the first time, enables their direct correlation with the International Chronostratigraphic Chart (2024). The analysis reveals significant discrepancies between the updated ages and the previously accepted regional scheme (1982–1996). A comparison of regional stratigraphic units' durations with estimated coal and siliciclastic sediment accumulation rates indicates that the early Permian contains the most prolonged stratigraphic hiatuses. The updated stratigraphic framework enables re-evaluating the temporal sequence of regional sedimentological, volcano-tectonic and biotic events, allowing for more accurate comparison with the global record. Palaeoclimate reconstructions indicate that during the early Permian, the Kuznetsk Basin was characterised by a relatively warm, humid, and aseasonal climate, consistent with its mid-latitude position during the Late Palaeozoic Ice Age. In contrast, the middle to late Permian shows a transition to a temperate, moderately humid climate with pronounced seasonality, differing from the warmhouse conditions of low-latitude palaeoequatorial regions. The latest Lopingian reveals a distinct trend toward increasing dryness, consistent with global palaeoclimate signals associated with the end-Permian crisis. |
| Ключевые слова |
Permian, Kuznetsk Basin, regional stratigraphy, U?Pb geochronology, sedimentary hiatus, coal-bearing succession, biotic events, palaeoclimate reconstruction |
| Название журнала |
Minerals
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https://repository.kpfu.ru/?p_id=321718 |
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Язык |
| dc.contributor.author |
Елисеев Николай Алексеевич |
ru_RU |
| dc.contributor.author |
Жаринова Вероника Владимировна |
ru_RU |
| dc.contributor.author |
Куликова Анна Викторовна |
ru_RU |
| dc.contributor.author |
Мифтахутдинова Динара Надировна |
ru_RU |
| dc.contributor.author |
Нургалиева Нурия Гавазовна |
ru_RU |
| dc.contributor.author |
Силантьев Владимир Владимирович |
ru_RU |
| dc.contributor.author |
Уразаева Миляуша Назимовна |
ru_RU |
| dc.contributor.author |
Тихомирова Марион |
ru_RU |
| dc.date.accessioned |
2025-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2025-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2025 |
ru_RU |
| dc.identifier.citation |
1. Silantiev, V. V., Gutak, Y. M., Tichomirowa, M., Käßner, A., Kulikova, A. V., Arbuzov, S. I., Nourgalieva, N. G., Karasev, E. V., Felker, A. S., Naumcheva, M. A., Bakaev, A. S., Porokhovnichenko, L. G., Eliseev, N. A., Zharinova, V. V., Miftakhutdinova, D. N., & Urazaeva, M. N. (2025). Revisiting the Permian Stratigraphy of the Kuznetsk Coal Basin (Siberia, Russia) Using Radioisotopic Data: Sedimentology, Biotic Events, and Palaeoclimate. Minerals, 15(6), 643. |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=321718 |
ru_RU |
| dc.description.abstract |
Minerals |
ru_RU |
| dc.description.abstract |
Radioisotopic dating of five stratigraphic levels within the Permian succession of the Kuznetsk Coal Basin refines the ages of the corresponding stratigraphic units and, for the first time, enables their direct correlation with the International Chronostratigraphic Chart (2024). The analysis reveals significant discrepancies between the updated ages and the previously accepted regional scheme (1982–1996). A comparison of regional stratigraphic units' durations with estimated coal and siliciclastic sediment accumulation rates indicates that the early Permian contains the most prolonged stratigraphic hiatuses. The updated stratigraphic framework enables re-evaluating the temporal sequence of regional sedimentological, volcano-tectonic and biotic events, allowing for more accurate comparison with the global record. Palaeoclimate reconstructions indicate that during the early Permian, the Kuznetsk Basin was characterised by a relatively warm, humid, and aseasonal climate, consistent with its mid-latitude position during the Late Palaeozoic Ice Age. In contrast, the middle to late Permian shows a transition to a temperate, moderately humid climate with pronounced seasonality, differing from the warmhouse conditions of low-latitude palaeoequatorial regions. The latest Lopingian reveals a distinct trend toward increasing dryness, consistent with global palaeoclimate signals associated with the end-Permian crisis. |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
Permian |
ru_RU |
| dc.subject |
Kuznetsk Basin |
ru_RU |
| dc.subject |
regional stratigraphy |
ru_RU |
| dc.subject |
U?Pb geochronology |
ru_RU |
| dc.subject |
sedimentary hiatus |
ru_RU |
| dc.subject |
coal-bearing succession |
ru_RU |
| dc.subject |
biotic events |
ru_RU |
| dc.subject |
palaeoclimate reconstruction |
ru_RU |
| dc.title |
Revisiting the Permian Stratigraphy of the Kuznetsk Coal Basin (Siberia, Russia) Using Radioisotopic Data: Sedimentology, Biotic Events, and Palaeoclimate |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
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