Stromatolites are the most intriguing geobiological structures
of the entire earth history since the beginning of the fossil
record in the Archaean. Stromatolites and microbialites are
interpreted as biosedimentological remains of biofilms and
microbial mats. These structures are important environmental and
evolutionary archives which give us information about ancient
habitats, biodiversity, and evolution of complex benthic
ecosystems. However, many geobiological aspects of these structures
are still unknown or only poorly understood. The present
proceedings highlight the new ideas and information on the
formation and environmental setting of stromatolites presented at
the occasion of the Kalkowsky Symposium 2008, held in Gottingen,
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