This study investigates the nature and components of annual luminescent ban
ding in massive Porites coral skeletons, with a view to refining the techni
que for using this banding to reconstruct past environmental conditions. Th
ree-dimensional excitation-emission-matrix spectroscopy and optical fibre b
eam delivery have been used to investigate the luminescence properties of t
he bright and dull bands of solid coral. Six characteristic excitation/emis
sion peaks have been identified: 280/450-600, 340/450, 370/470, 390/485, 42
0/505 and 450/530 nm. The first peak corresponds to protein-type fluorescen
ce. The others are characteristic of humic acid luminescence. The differenc
e in luminescence intensity between bright and dull bands has been quantifi
ed and characterised spectroscopically. The luminescence of the bright band
s is up to 25% more intense than their neighbouring dull bands with the gre
atest increase in relative intensity in the long wavelength emission region
, between 500 and 600 nm. The contribution of long-lived phosphorescence to
the total luminescence intensity has been determined by time-resolved meas
urements on the 100 ms timescale, Both bright and dull bands show long-live
d phosphorescence with decay times up to 1.5 s, This phosphorescence accoun
ts for about 10% of the total luminescence intensity of bright bands. The d
ifference in phosphorescence intensity between bright and dull bands is sub
stantially greater than the difference in total luminescence intensity: the
phosphorescence of bright bands is up to twice as intense as that of dull
bands. This suggests that phosphorescence plays an important role in defini
ng luminescent banding ill coral. Furthermore, the large observable differe
nce in phosphorescence between bright and dull bands indicates that measure
ment of phosphorescence profiles across growth bands in corals may prove to
be a moro sensitive indicator of past environmental conditions than measur
ements of total luminescence.