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首页> 外文期刊>Quaternary International >Fauna and flora of drilling and core data from the iznik Lake: The Marmara and the Black Sea connection
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Fauna and flora of drilling and core data from the iznik Lake: The Marmara and the Black Sea connection

机译:伊兹尼克湖的动物和动植物群以及核心数据:马尔马拉与黑海的联系

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摘要

The study deals with on the Quaternary connection of the Iznik Lake between the Gemlik Gulf and the Black Sea located in the Marmara Region. The core and drilling data were evaluated. They were collected at two locations and depths from drilling cores and at the three deepest locations of the lake. A total of 510 samples were examined from the lake-bottom cores. Ostracod, mollusc, nannoplankton, ascidian spicule, and diatom assemblages observed at different levels of the drillings were studied. No foraminiferal data were recorded. Molluscan association such as Dreissena bugensis, D. caspia, Monodacna pontica, Clathrocaspia makarovi, Euxinipyrgula milachevitchi, Euxinipyrgula lincta indicate Neoeuxinian age. Amnicythere olivia, A. stepanaitysae, A. striatocostata, Tyrrhenocythere amnicola and Loxoconcha immodulata of the ostracod assemblage, exhibiting Ponto-Caspian origin, were found. In addition, fossil ascidian spicules comprising various species of Bonetia, Micrascidites, Monniotia, and Rigaudia genera were encountered, probably representing Late Pleistocene to Holocene ages. Campylodiscus echeneis, Cocconeis placentula var. lineata Epithemia turgida var. granulata, Epithemia adnata, Nitzschia commutate and N. vermicularis, from the diatom assemblage are genera and species also found in the Iznik Lake and in the Black Sea. Mollusc and ostracod fauna, the Ponto-Caspian origin indicates that the Iznik Lake was connected with the Black Sea and the Marmara Sea in the recent period. Thus, the Ponto-Caspian assemblages indicate the early Neoeuxinian (Surozhian) brackish water inundated the study area.
机译:这项研究涉及的是伊兹尼克湖的第四纪联系,该海湾位于马尔马拉地区的吉姆利克湾和黑海之间。评估了岩心和钻井数据。它们是在两个位置和深度处从钻芯收集的,并且是在湖中三个最深的位置收集的。从湖底岩心总共检查了510个样品。研究了在不同水平的钻探中观察到的Ost类,软体动物,浮游生物,海鞘针和硅藻组合。没有记录有孔虫的数据。软体动物协会,如Dreissena bugensis,D。caspia,pondacna pontica,Clathrocaspia makarovi,Euxinipyrgula milachevitchi,Euxinipyrgula lincta都表明了新苏木时代。发现了显示出蓬图里海起源的羊角纲组合的羊栖小球藻,步长曲霉,条状曲霉,痢疾棘突羊膜和Loxoconcha immodulata。此外,还遇到了由Bonetia,Micrascidites,Monniotia和Rigaudia属组成的各种海生化石针刺,可能代表了晚更新世至全新世时代。弯弯曲菌,球菌胎盘变种。 Lineata上皮血型变种在伊兹尼克湖和黑海中也发现了硅藻组合中的粒状体,上皮性腺炎,尼兹菌换向和蠕虫N. vermicularis。蓬图-里海起源的软体动物和兽类动物表明,伊兹尼克湖在最近时期与黑海和马尔马拉海相连。因此,蓬-里海组合表明早期的新新世(Surozhian)微咸水淹没了研究区域。

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