Модель магнітного запису лесів півдня України  на прикладі розрізу середнього плейстоцену Долинське

Д.В. Главацький

doi:10.24028/gj.v47i3.323058

Автор(и)

Д.В. Главацький Інститут геофізики ім. С.І. Субботіна НАН України, Київ, Україна, Україна

DOI:

https://doi.org/10.24028/gj.v47i3.323058

Ключові слова:

Дунайський басейн, лесово-ґрунтові відклади, магнітна сприйнятливість, петромагнетизм, педогенна модель, перехід середнього Брюнеса

Анотація

Значну роль у дослідженнях клімату плейстоцену відіграють магнітні параметри лесово-ґрунтових відкладів, насамперед магнітна сприйнятливість і коефіцієнт її частотної залежності. Зазвичай інтерпретація поведінки магнетизму в лесах ґрунтується на двох загальноприйнятих моделях: педогенній («китайській») моделі магнітного підсилення та «аляскинській» (англ. «reducing-pedogenic») моделі. Проте зростає кількість випадків, коли жодна модель не може бути застосована окремо (так звана перехідна модель), зокрема на північному заході України. У цьому дослідженні наведено петромагнітні дані з лесового розрізу середнього плейстоцену Долинське на півдні України. Результати, у поєднанні з отриманими раніше даними з розрізу Роксолани та інших розрізів регіону, свідчать про збільшення у похованих ґрунтах концентрації феримагнітних мінералів, зокрема суперпарамагнітного магнетиту. Це вказує на переважання типової педогенної моделі магнітного запису (англ. «magnetic enhancement») для півдня України, як і для більшості території України. За петромагнітними маркерами в інтервалі середнього плейстоцену у лесово-ґрунтовій серії півдня України ідентифіковано сім інтергляціалів, що відповідають морським ізотопним стадіям MIS 19, MIS 17, MIS 15, MIS 13, MIS 11, MIS 9, MIS 7. Також встановлено ритми окремих кліматичних оптимумів — інтерстадіалів — зокрема MIS 15e, MIS 15a, MIS 13c, MIS 13a, MIS 9e, MIS 9a, MIS 7e, MIS 7a—c, які чітко виявляються магнітними методами. Розглянуто декілька (хроно-)стратиграфічних проблем в інтерпретації формування середньоплейстоценових лесів півдня України, а також здійснено спробу порівняти палеогеографічні етапи української кліматостратиграфічної системи з основними глобальними та регіональними палеокліматичними трендами

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