РЕКОНСТРУКЦІЯ КЛІМАТУ ДОНБАСУ У ПІЗНЬОМУ ЕОЦЕНІ–РАННЬОМУ МІОЦЕНІ ЗА МЕТОДОМ COEXISTENCE APPROACH НА ПІДСТАВІ ДАНИХ СПОРОВО-ПИЛКОВИХ ДОСЛІДЖЕНЬ
DOI:
https://doi.org/10.30836/igs.2522-9753.2025.330439Ключові слова:
спори та пилок, палеоклімат, Донбас, Сoexistence Approach, пізній еоцен, олігоцен, ранній міоценАнотація
Методом Coexistence approach виконано реконструкцію клімату регіону Донецької складчастої споруди впродовж пізнього еоцену–раннього міоцену на підставі результатів спорово-пилкових досліджень. Проведено порівняння отриманих результатів із такими попередніх досліджень палеоклімату олігоценового часу цього регіону за даними вивчення відповідних комплексів спор та пилку, плодів і насіння, відбитків рослин. Отримано значення сімох параметрів клімату для пізньоеоценового часу (приабон), двох проміжків ранньоолігоценового часу (ранній рюпель, середній рюпель) та пізньоолігоценового часу (хат), а також початку ранньоміоценового часу (початок аквітану). Зареєстровано поступове але нелінійне зниження середньорічної температури впродовж усього дослідженого інтервалу часу з мінімумом у пізньому еоцені, максимумом у середньорюпельський час (ранній олігоцен) і мінімумом на початку раннього міоцену. Встановлено впродовж пізнього еоцену–раннього міоцену тенденцію до зміщення максимуму опадів із теплого на холодний сезон року. Виконано порівняльний аналіз отриманих результатів із такими, що отримані автором раніше для олігоценового часу Українського щита, Дніпровсько-Донецької западини, Північного Причорноморʼя та Рівнинного Криму. Визначено, що реконструйований клімат належить до теплопомірного, помірно вологого, із сухим спекотним літо м, типу Csa за Кьоппеном.
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