首页> 外文期刊>Annales Societatis Geologorum Poloniae >LATE TURONIAN AND EARLY CONIACIAN VENTRICULITID SPONGES (LYCHNISCOSIDA) FROM OPOLE TROUGH (SOUTHERN POLAND) AND THEIR PALAEOECOLOGICAL SIGNIFICANCE
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LATE TURONIAN AND EARLY CONIACIAN VENTRICULITID SPONGES (LYCHNISCOSIDA) FROM OPOLE TROUGH (SOUTHERN POLAND) AND THEIR PALAEOECOLOGICAL SIGNIFICANCE

机译:奥波莱·特劳(波兰南部)的晚突厥和早柯尼西亚涡虫海绵(lychniscosida)及其古生态学意义

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Eight species of ventriculitid sponges (Order Lychniscosida Schrammen, 1903) are described from the Upper Turonian marly limestones and Lower Coniacian marls of the Opole Trough (southern Poland). Among them four have not previously been noted in this area. Two species, Astropegma stellata (Roemer, 1840) and Leiostracosia robusta (Schrammen, 1902) are reported from Turonian strata for the first time. The occurrence of ventriculitid sponges in the Upper Turonian–Lower Coniacian succession of the Opole Trough indicates a soft- bottom, calm-water environment, with depths below the storm-wave base and a low rate of sedimentation.
机译:描述了八种心室海绵(订单号Lychniscosida Schrammen,1903年),它们来自Opole Trough(波兰南部)的上土伦泥灰岩和下圆锥灰泥岩。其中有四个以前在该领域没有被注意到。首次从Turonian地层中发现了两个物种,恒星天蛾(Roemer,1840年)和强壮Leiostracosia稳健(Schrammen,1902年)。 Opole槽的上Turonian–Lower Coniacian演替过程中发生了脑室海绵,表明软底部,平静的水环境,其深度低于风暴波波基且沉降率较低。

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