THE study of biomineralization is inspiring new approaches to the cont
rolled fabrication of synthetic materials such as nanoparticles, polym
er-mineral composites and templated crystals(1-3). Although this biomi
metic approach is gaining momentum, the biological mechanisms involved
in biomineralization remain relatively unexplored. One major reason f
or this is the difficulty of analysing biomineralization processes in
their native dynamic state. Here we demonstrate that a highly organize
d composite material-a 'flat pearl'-can be biofabricated on disks of g
lass, mica and MoS2 inserted between the mantle and shell of Haliotis
rufescens (red abalone). We shove that the construction of this materi
al is spatially and temporally regulated and proceeds through a develo
pmental sequence that closely resembles that at the growth front of th
e natural shell. Recognition of the implanted inorganic surfaces by ma
ntle cells apparently governs a switch, perhaps genetically controlled
, from aragonite to calcite biomineralization. Once a partially orient
ed calcite-protein primer layer has been deposited, there is a switch
back to the nucleation and assembly of columnar stacks of highly order
ed aragonitic nacre. Thus the presence of an inorganic surface between
the mantle and shell of the organism triggers a change in the nature
of the mineral phase deposited.