НЕМОРСЬКІ ПЕЛЕЦИПОДИ МОСПИНСЬКОЇ СВІТИ (ВЕРХНІЙ БАШКИР) ДОНЕЦЬКОГО БАСЕЙНУ: СИСТЕМАТИЧНИЙ СКЛАД, ПАЛЕОЕКОЛОГІЯ ТА СТРАТИГРАФІЧНЕ ЗНАЧЕННЯ

Автор(и)

  • В.С. ДЕРНОВ Інститут геологічних наук НАН України, Київ, Ukraine

DOI:

https://doi.org/10.30836/igs.1025-6814.2022.3.255491

Ключові слова:

неморські пелециподи, карбон, верхній башкир, Донецький басейн, Україна

Анотація

В кам’яновугільних вугленосних відкладах Донбасу значно поширені рештки неморських пелеципод. Їхнє вивчення має велике стратиграфічне, палеоекологічне та палеобіогеографічне значення. На кількох стратиграфічних рівнях в розрізі моспинської світи Центрального Донбасу виявлено рештки неморських пелеципод. Зі сланців покрівлі вугільного шару g2 ідентифіковано Carbonicola obtusa (Hind) і Naiadites sp.; зі сланців покрівлі вугільного шару g12 визначено Curvirimula trapeziforma (Dewar) та C. tesselata (Jones), а у алевролітах нижче вапняку G12 знайдено Carbonicola rectilinearis Trueman et Weir та C. limax Wright. Дані пелециподи відомі переважно у вестфалі А (Langsettian) Західної Європи. Верхню частину нижньої половини моспинської світи в даній статті віднесено до верств з Carbonicola rectilinearis, які відповідають верхній частині зони lenisulcata Західної Європи. Нижньою межею цих верств умовно є підошва потужної пачки пісковиків в 43 м нижче вапняку G12; верхньою, також умовною, є вугільний шар g12. Зона Carbonicola pseudorobusta, що встановлена М.Т. Сергєєвою, виділяється в інтервалі «покрівля вугільного шару g12—шар h61». Вона відповідає зоні communis Західної Європи. Пелециподи з покрівлі вугільних шарів g12 і g2 мешкали в мілководних евтрофних прісних або солонуватих озерах, розташованих на приморській акумулятивній низовині. Для цих водойм був характерним істотно збіднений склад гідробіонтів і зараженість сірководнем мулів і, можливо, придонного шару водної товщі. В осадах цих озер знайдено представників родів Curvirimula та Naiadites, які, ймовірно, вели псевдопланктонний спосіб життя. Пелециподи з алевролітів нижче вапняку G12 (Carbonicola) мешкали в мілководній опрісненій лагуні, яка глибоко врізалась в дельтову рівнину. 

 

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