Lazăr Chirica
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摘要

黑海是一个独特的盆地,具有复杂的地质历史,其水文生物制度在时间上发生了很大的变化,并且在整个演变过程中具有显著的水平变化。是化化养细菌最重要的发育盆地,影响了硫化氢的空前发育(𝐻2S),存在厌氧过程,表现了该盆地的分生特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Starea actuală a geosistemelor din zona de litoral a mării Negre și unele tendinţe
The Black Sea is a unique basin with a complicated geological history, a hidrobiological regime that has changed much in time and has significant level variation throughout it’s evolution. Is the most important development basin of chemolitoatotrophic bacteria that influences the unprecedented development of hydrogen sulphide (𝐻2S) an anaeropic processes are present, which express the basin’s meromic character.
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