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The Pannonian Sea was a shallow ancient sea located where the Pannonian Basin in Central Europe is now. The Pannonian Sea existed during the Miocene and Pliocene epochs, when a three to four kilometre depth of marine sediments were deposited in the Pannonian Basin. ==History== The Pannonian Sea, for most of its history, was part of the Paratethys Sea. A Miocene uplift of the Carpathian Mountains isolated the sea from the rest of Paratethys (about 10 million years ago). During its first historical phase, the Pannonian Sea had a western connection with the Mediterranean Sea through the territories of the modern Ligurian Sea, Bavaria, and Vienna Basin. Through the Đerdap Strait, the Pannonian Sea was linked to the Paratethys in the Wallachian-Pontic Basin. The Pannonian Sea was also attached to the Aegean Sea through the modern Preševo Valley. Due to its diverse history the salinity of the sea often shifted. The decrease of salinity resulted an endemic fauna. The Pannonian Sea existed for about 9 million years. Eventually, the sea lost its connection to the Paratethys and became a lake permanently (''Pannonian Lake''). Its last remnant, the Slavonian Lake, disappeared in the Pleistocene era. The remnants of the former islands of the Pannonian Sea are the modern Pannonian island mountains (Mecsek, Papuk, Psunj, Krndija, Dilj, Fruška Gora, and Vršac Mountains). 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Pannonian Sea」の詳細全文を読む スポンサード リンク
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