首页> 外文期刊>Annales Societatis Geologorum Poloniae >DINOFLAGELLATE CYSTS FROM THE PALAEOGENE OF THE ?UKOWA-4 BOREHOLE (CARPATHIAN FOREDEEP, SE POLAND): BIOSTRATIGRAPHY AND PALAEOENVIRONMENT
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DINOFLAGELLATE CYSTS FROM THE PALAEOGENE OF THE ?UKOWA-4 BOREHOLE (CARPATHIAN FOREDEEP, SE POLAND): BIOSTRATIGRAPHY AND PALAEOENVIRONMENT

机译:?UKOWA-4孔(喀尔巴阡前茅,SE波兰)的古生代中的叶小囊藻:生物体谱学和古环境

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This paper documents the presence of Eocene marine strata in the Carpathian Foredeep area in Poland. Assemblages of marine dinoflagellate cysts have been found in sands penetrated by the ?ukowa-4 borehole below the Miocene succession of the foredeep. Their age is interpreted as Late Eocene. The presence of marine strata of this age in this area sheds new light on the palaeogeography of the Carpathian foreland during the Late Eocene. The dinoflagellate cysts described are compared with coeval Carpathian and epicontinental assemblages; possible connections between these two basins are discussed. Phytogenetic deposits that occur above the marine sands of the ?ukowa-4 borehole contain freshwater palynomorphs, indicating their swamp and lacustrine origins. The overlying sand contains impoverished dinoflagellate cyst assemblages; their age is discussed.
机译:本文记录了波兰喀尔巴阡Foredeep地区的始新世海相地层。在前中新世中新统以下的Fukowa-4钻孔穿透的沙子中发现了海洋鞭毛藻囊肿的组合。他们的年龄被解释为始新世晚期。在这个地区,这个时代海相的存在为始新世晚期喀尔巴阡前陆的古地理学提供了新的思路。将所描述的鞭毛藻囊肿与同期喀尔巴阡和上陆大陆组合进行比较;讨论了这两个盆地之间可能存在的联系。发生在Fukowa-4井眼海沙上方的植物成因沉积物含有淡水古生物,表明它们是沼泽和湖泊的起源。上覆的沙子含有贫化的鞭毛藻囊体组合;他们的年龄在讨论中。

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