НОВІ ДАНІ ПРО ГЕОЛОГІЮ ТА ПАЛЕОНТОЛОГІЧНУ ХАРАКТЕРИСТИКУ ДЯКОВСЬКОЇ СЕРІЇ (КАРБОН) ЦЕНТРАЛЬНОГО ДОНБАСУ (УКРАЇНА)

Автор(и)

  • В.С. Дернов Інститут геологічних наук НАН України, Україна
  • В.І. Полєтаєв Інститут геологічних наук НАН України, Україна

DOI:

https://doi.org/10.30836/igs.1025-6814.2024.1.285644

Ключові слова:

морська фауна, наземна флора, карбон, дяковська серія, Донецький басейн

Анотація

Із частини розрізу дяковської серії, що відповідає вугленосним відкладам мандрикинської світи та нижній частині моспинської світи південної частини Луганської області, вивчено нові знахідки решток морської фауни (брахіопод, молюсків, кріноідей, артропод та риб) і наземної флори. Вперше із зазначених відкладів визначено рештки брахіопод, що представлені родами Crurithyris, Tiramnia, Alphachoristites та Lissochonetes. Крім того, вперше серед відкладів дяковської серії знайдено рештки філокарид, а також відбитки наземних рослин, що відносяться до родів Halonia, Calamites, Pinnularia, Paripteris, Eusphenopteris, Artisia та Cordaites. Бівальвії у вивченій колекції представлені представниками родів Phestia, Parallelodon, Palaeoneilo, Nuculavus, Solenomorpha, Sanguinolites, Posidoniella та ?Euchondria. Серед гастропод визначено роди Nodospira, ?Euphemites, Retispira, Glabrocingulum, Rhineoderma, Angyomphalus, ?Naticopsis; серед цефалопод – Gzheloceras, ?Pseudogzheloceras, Melvilloceras, Retites, Gastrioceras та ?Owenoceras. Крім названих груп у дяковській серії також встановлено присутність кріноідей Platyplateium, Platycrinites, ?Unilineatocrinus та Bicostulatocrinus, а також фрагментів іхтіодорулітів акантод Gyracanthidae indet. та ізольованої риб’ячої луски. Отримані дані свідчать про гарні перспективи створення палеонтологічно обґрунтованої схеми розчленування монотонної потужної товщі дяковської серії. 

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