Seed dispersal by water: a contribution to the interpretation of seed assemblages

Abstract

The composition of a seed flora always differs from actual vegetation. For archaeobotanists, who try to reconstruct former communities on the basis of plant macrofossils extracted from soil samples, this is a serious handicap. This difference can be explained by dispersal processes and by differences in preservation. Seeds that are incorporated into the soil may originate from both local and regional vegetation. Once incorporated, differences in preservation may result in a seed flora from a mixture of communities. The comparison may be further confounded when seeds that are transported over long distances are also of subfossil or even fossil origin. Both wind and water are effective agencies for long-distance dispersal. This study deals with the dispersal of botanical macro-remains by water. Water may be considered an important dispersal agent, especially in sites situated in the vicinity of running water, or liable to contact with water during storm surges or river floods. Therefore, the interpretation of seed assemblages from sediments that may have been in contact with running water needs special attention. In order to obtain information about the dispersal potential of plant remains by water transport, litter which had been transported by the river Rhine, and litter which had been washed ashore on the North Sea coast of the Netherlands was examined.