ВИВЧЕННЯ ПАЛЕОЗОЙСЬКИХ КОНОДОНТІВ В УКРАЇНІ
DOI:
https://doi.org/10.30836/igs.2522-9753.2017.142182Ключові слова:
конодонти, силур, карбон, стратиграфія, зональна схема, кореляціяАнотація
В Україні вивчення палеозойських конодонтів бере початок із середини 1960-х років. Першим дослідником конодон- тів із розрізів ордовику, силуру та девону Подолії і Волині був Д.М. Дригант (Державний Природознавчий музей НАНУ, м. Львів). Кам’яновугільні конодонти Донецького басейну, Дніпровсько-Донецької западини та Львівсько- Волинського басейну України почали вивчати на початку 70-х років минулого століття чотири аспіранти проф..Д.Є. Айзенверга: Олег Є.Котляр, Олег М. Ліпнягов, Раіса Й. Козицька та Тамара І.Немировська (Інститут геологічних наук НАНУ, Київ). Конодонти московського яруса карбону Донбасу із керна свердловин, пробурених у південно-західній частині Донбасу, вивчала Зоя А. Косенко (“Артемгеологія”, м. Артемівськ, нині – м. Бахмут).
В результаті проведених досліджень були детально вивчені та монографічно описані силурійські та девонські коно- донти Волино-Подолії та кам’яновугільні конодонти Донбасу та Дніпровсько-Донецької западини, установлено ряд нових таксонів. Складені перші зональні схеми за конодонтами карбону Донбасу. Вивчалися конодонти карбону різ- них регіонів Європи та Азії, що дозволило провести надійну кореляцію карбону Донбасу з кам’яновугільними басей- нами інших регіонів світу. Результати досліджень опубліковані в великій кількості статей і монографій з конодонтів. Декілька видів конодонтів, установлених у карбоні Донбасу, запропоновано в якості видів-індексів для встановлення GSSPs на границях башкирського і московського та московського і касимовського ярусів Глобальної Шкали карбону. Вперше для Східної Європи було виявлено значну подію вимирання ранньокам’яновугільних конодонтів на межі міс- сісіпської та пенсильванської підсистем у Кальміуському розрізі Донбасу. Цей розріз Донбасу був запропонований як один із перших кандидатів на стратотип серединної границі карбону.
Посилання
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