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主要研究安纳托利亚中部昌克勒-乔鲁姆盆地(Cankiri-Corum Basin)始新世含褐煤层中的孢粉与环境。在采尔特克组(Celtek Fm.)30块样品中共发现至少100种孢粉类型,包括部分具地层意义的分子,从而确定孢粉组合的时代为中-?晚始新世。孢粉反映本组褐煤层形成于近湖沼泽环境或具茂密低地植被的泛滥平原。在乔鲁姆-阿马西亚地区的阿姆特鲁组(Armutlu Fm.)中共发现59属、133种孢粉,包括部分现代分布在大西洋和印度-太平洋地区的典型红树林分子,为土耳其红树林化石花粉的首次记录,说明沉积时期受到海陆的共同作用,可能为潮间带沼泽环境。奥斯曼诺格鲁组(Osmanoqlu Fm.)的褐煤层中也含有丰富的孢粉,指示地层时代为早渐新世。
It mainly studies the sporopollen and environment in the Eocene lignite in the Cankiri-Corum Basin in Central Anatolia. At least 100 types of sporo-pollen, including some stratigraphic molecules, were found in 30 samples of Celtek Fm. It was confirmed that the age of sporopollen assemblages was Meso-Late Eocene. Pollen reflects the formation of lignite in this group of swamps in the lake environment or dense lowland vegetation flood plain. A total of 59 genera and 133 species of sporopollen were discovered in the Armutlu Fm. Region of the Qorum-Amasya region, including some typical mangrove species distributed in the Atlantic and Indo-Pacific regions, The first record of the fossil forest fossils shows that the sedimentation period was affected by the combined action of land and sea, which may be intertidal marsh environment. The lignite in the Osmanoqlu Fm. Group is also abundant in sporopollen, indicating that the stratigraphic age was Early Oligocene.