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During the Middle to Late Berriasian (so called “German Wealden”) a large lake system developed in the Lower Saxony Basin (LSB; in northwestern Germany) of which the eastern part is characterized by varying fluvial and lacustrine influences. The changeable situation through the earliest Cretaceous, particularly in the eastern LSB, is relatively understudied and a recently drilled well (KB-Rehburg 2; R-2) can help shedding ligh...
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