Verlandete Altwässer auf der Niederterrasse bei Köln?: Die Entstehung des Linder Bruchs aufgrund einer Pollen- und Großrestanalyse

Ilse Peters
A pollen-analysis was made of the Linder Bruch, which is located on the Lower Rhine Terrace south of Wahn. Additionally, an examination was made of the macro-floral remains. The results show that the organic sediments were deposited at the beginning of pollenzone X/XI (Overbeck & Schneider). They are not old river deposits, but the product of secondary mooring of a dried-up river arm, which apparently belongs to the Rhine system. The overflow-water was run-off from...