ГОЛОВНІ ЕТАПИ ЕВОЛЮЦІЇ КАМ‘ЯНОВУГІЛЬНИХ SPIRIFERIDA ТА SPIRIFERINIDA (BRACHIOPODS) У ПАЛЕОБАСЕЙНАХ СХІДНОЇ ЄВРОПИ

Автор(и)

DOI:

https://doi.org/10.30836/igs.1025-6814.2025.2.327915

Ключові слова:

Spiriferida, Spiriferinida, асоціація, міссісіпій, пенсильваній

Анотація

Встановлено та проаналізовано дванадцять часових інтервалів, протягом яких відбувалися зміни у родовому складі карбонових угруповань Spiriferida та Spiriferinida в межах палеобасейнів Східної Європи. Як найважливіші рівні змін виділено інтервали на границі девону і карбону, у середині турне і середині візе, поблизу границь міссісіпію і пенсильванію, башкирського і московського, низів касимовського ярусів, а також границі карбону і пермі. Вказано на зміну літологічних умов проживання як причину морфологічної еволюції системи прикріплення у представників надродин Spiriferoidea, Paeckelmanelloidea та Brachythyridoidea після Гангенберзької кризи. Підкреслено значення еволюції судинної системи представників родини Angiospiriferidae Legrand-Blain, 1985 для виникнення підродин Chorisitinae Waterhouse, 1968 та Brachythyrininae Waterhouse, 2004 наприкінці міссісіпію. Обговорюється масштаб швидкості зміни родового складу спіриферид (брахіоподи) карбону. 

 

Посилання

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