“海岸带湖泊生态系统的地质档案”:巴法湖(地中海)

Özlem Bulkan, Bilgehan Toksoy Ediş, M. N. Çağatay
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引用次数: 1

摘要

一本假想的小说,旨在总结地中海沿岸地区的整个地质历史,可能包含一系列密集而令人印象深刻的主题,如海啸、风暴、地震、火山活动、人与自然的相互作用及其产物。这些突发性地质事件变化(例如,水化学波动)反映了这一独特沿海地区的动态性质。对沿海湖泊档案(即土耳其巴法湖)的古湖泊学研究,结合在邻近地质环境(即沼泽、三角洲、泻湖、海洋)中积累的同生沉积物,使我们能够重建当地的地质历史。在此基础上,对八发湖及周边沿海地区的古环境建设进行了研究。湖泊(BAF37:4.2 m)岩心和周围沼泽(BS:12 m)沉积物的岩性和地球化学调查为我们提供了一个优秀的地质档案,在过去的4.5 ky中不断积累。主要沉积阶段有:最近的沼泽-湖泊分离阶段(S-I:最后0.8 ky),泻湖阶段(S-II)。: 0.8 - 1.75 ky BP)、海洋-河流相互作用阶段(S-III: 1.75 - 2.7 ky BP)和海洋主导阶段(S-IV: 2.7 - 4.5 ky BP)。研究表明,盆地的生态系统特征主要受水文气候和大地构造过程的控制。
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“Geo-archives of a Coastal Lacustrine Eco-system”: Lake Bafa (Mediterranean Sea)
A hypothetical novel, which aims to summarize the whole geological history of the coastal area surrounding the Mediterranean Sea, probably contains a sum of intensive and impressive topics, such as tsunamis, storms, earthquakes, volcanic activities, human-nature interactions, and their products. These abrupt geo-event changes (e.g., water chemistry fluctuations) remark a dynamic nature of this unique coastal area. Paleolimnological studies of a coastal lacustrine archive (i.e., Lake Bafa, Turkey), associated with syngenetic deposits accumulated in neighboring geological settings (i.e., swamp, deltaic, lagoon, marine), has allowed us to reconstruct the local geological history. Following this hypothesis, we aimed at investigating the paleoenvironmental establishment of the Lake Bafa and surrounding coastal area. Lithologic and geochemical investigations of the lacustrine ( “ BAF37:4.2 m) core and surrounding swamp ( “ BS ” :12 m) sediments supplied us an excellent geo-archive, continuously accumulated during the last 4.5 ky. Following conclusions are provided concerning the main depositional stages: Recent swamp-lacustrine separated stage (S-I: last 0.8 ky), lagoon stage (S-II.: 0.8 – 1.75 ky BP), marine-river interaction stage (S-III: 1.75 – 2.7 ky BP), and marine-dominated stage (S-IV: 2.7 – 4.5 ky BP). Our observations indicate that ecosystem characteristics of the basin have been mainly controlled by the hydroclimate and geotectonic processes.
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