The Matuyama—Brunhes boundary in the loess-palaeosol sequence of Dolynske, southern Ukraine

• Дата: 2021
• Автори: Bakhmutov, V. G., Hlavatskyi, D. V., Veklych, Y. M., Shpyra, V. V., Yakukhno, V. I.
• Формат: Стаття
• Мова: rus
• Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2021
• Теми: магнітостратиграфія; лесово-ґрунтова формація; плейстоцен; межа Матуяма—Брюнес; Дунай; палеомагнітний метод; магнитостратиграфия; лессово-почвенная формация; граница Матуяма—Брюнес; палеомагнитный метод; magnetostratigraphy; loess-palaeosol sequence; Pleistocene; Matuyama—Brunhes boundary; Danube; palaeomagnetic method
• Онлайн доступ: https://journals.uran.ua/geofizicheskiy/article/view/244065
• Назва журналу: Geofizicheskiy Zhurnal

We present the results of a palaeomagnetic study of the Early—Middle Pleistocene deposits exposed on the left bank of the River Danube at Dolynske, southern Ukraine. A thick succession of water-lain facies is succeeded by stratigraphically complete loess-palaeosol sequence; these constitute a unique palaeoclimate archive in the southern margin of the East European loess province. The Matuyama—Brunhes boundary (MBB) has been detected at the bottom of the Lower Shyrokyne (S7S3) subunit and not in the Martonosha (S6) unit as previously thought. New data align with previous results from the Roksolany and Vyazivok sections, where the MBB was determined at the same stratigraphical level in the S7S3 soil. In contrast to terrestrial Pleistocene records in China and сentral Europe, where the MBB was regularly determined in a loess layer (representing a cold period), the MBB in the Ukrainian subaerial succession is located in the soil unit (representing a warm period). Furthermore, eight, and not seven, glacial-interglacial cycles are recorded in the Brunhes chron. This may indicate the stratigraphic completeness of the loess-soil succession of Ukraine, which can be compared with the reference global marine and terrestrial palaeoclimatic archives. Further palaeomagnetic studies of loess-palaeosol sequences of other regions of Ukraine will allow revision and correlation of still inconsistent stratigraphic and magnetostratigraphic schemes of the Pleistocene deposits.