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Cirilli et al 2005

AI-generated Abstract

This research explores the stratigraphy and palynology of the Upper Triassic Nayband Formation in eastern central Iran. The Nayband Formation is significant for its geological composition, primarily consisting of alternating shales, sandstones, and carbonates, with a thickness exceeding 220 meters. Various palynological assemblages, including notable taxa such as Cycadopites, Alisporites, Equisetosporites, and others, are described to assess the paleoenvironment and age of the formation. The study highlights significant biodiversity in palynomorphs, contributing valuable insights into Upper Triassic ecosystems and their implications in geological frameworks.