The Kačák event (Czech pronunciation: [ˈkatʃaːk]), also known as the Kačák-otomari event, is a widely recognised bioevent or series of events that occurred close to the end of the Eifelian age of the Middle Devonian period. It involved a global eustatic rise in sea level and ecological turnover.
The Kačák event (Czech pronunciation: [ˈkatʃaːk]), also known as the Kačák-otomari event, is a widely recognised bioevent or series of events that occurred close to the end of the Eifelian age of the Middle Devonian period. It involved a global eustatic rise in sea level and ecological turnover.
Source: Wikipedia "Kačák event" · CC BY-SA 4.0
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