Yapay Zeka Hızlı Bakış & Çıkarımlar
AI InsightTheconodont assemblages are representative of the palmatolepid-bispathodid biofacies, which indicate deposition on an outer shelf to slopeenvironment.
📌 3 Maddede Bu Makale
Abstract
The Palaeozoic sequence in the İstanbul region is made up of a continuous transgressive sedimentary series extending fromOrdovician continental clastic rocks to Lower Carboniferous turbidites. The middle part of this sequence consists predominantly ofcarbonates ranging from shallow marine Upper Silurian limestones to latest Devonian to earliest Carboniferous deep marine limestonesand shales. Here, we describe a new Upper Devonian deep marine limestone-siltstone section from the Sarıyer region in the Europeanpart of İstanbul. The 37-m thick section located in the campus of the İstanbul Technical University consists at the base of darkmicritic limestones interbedded with carbonate-rich siltstones, which pass up into siltstones with rare micritic limestone lenses andbeds. Conodonts indicate a late Famennian (latest Devonian) age for the İTÜ campus section; 5 conodont biozones are documented;Pseudopolygnathus granulosus, Polygnathus styriacus, Palmatolepis gracilis manca, Palmatolepis gracilis expansa, and Bispathodusaculeatus aculeatus. The Late Devonian fauna from the İTÜ Campus section are dominated by the important marker species ofPalmatolepis, Bispathodus and Polygnathus. There are also some Branmehla, Mehlina, and Icriodus elements within the succession. Theconodont assemblages are representative of the palmatolepid-bispathodid biofacies, which indicate deposition on an outer shelf to slopeenvironment.