Traces of the action of mechanical and chemical boring, scraping
or crushing organisms on hard substrates appear in fossil
carbonates as old as the Precambrian, providing valuable
palaeoenvironmental indicators. Bioerosion has been extensively
studied in tropical seas, but data from cold-temperate to polar
settings remain sparse. This book presents an experimental study
into the pace of carbonate degradation and the chronology of boring
community development along a bathymetric gradient in high-latitude
settings.
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