This study presents a synthesis of the evidence for modern archaeologi
cal, and palaeantological bioerosion of vertebrate tissue. It describe
s the first evidence for the bioerosion of modern. archaeological and
fossil bird bones. A new form of bone bioerosion, known as Hackett tun
nels, is defined. The bioerosion of vertebrate tissue by cyanobacteria
and algae in modern marine and lacustrine environments is also descri
bed. Archaeological evidence indicates that the destruction of bone by
bioerosion occurs in other terrestrial environments, such as cave dep
osits and middens. Bone from marine and lacustrine environments that a
ppears to be macroscopically well preserved can have large amounts of
microscopic fabric destruction. (C) 1997 by John Wiley & Sons, Ltd.