Lord Howe Island (31 degrees 33'S,159 degrees 05'E) is surrounded by t
he southern-most coral reefs in the Pacific Ocean, The status of the b
enthic communities at Lord Howe Island was quantified in 1992-93 using
replicated video-transects at 20 sites in the shallow reefal area (<2
0 m depth). The cover of hard coral was comparable with coral cover on
some tropical reefs, ranging from less than 10% at some reef flat sit
es to greater than 40% cover at two seaward beach sites. The process o
f reef formation is apparently slow, and accretion of limestone is loc
alized. A total of 59 scleractinian coral species were recorded during
this study (including 19 new records), bringing the total number reco
rded at Lord Howe Island to 83. The coral communities contain a unique
association of tropical species at their southern limits of distribut
ion, and subtropical species which are rare or absent from the Great B
arrier Reef. Many of the species that have been recorded from Lord How
e Island are rare, and may have resulted from chance recruitment of on
ly a few larvae. There have been few major changes in the coral commun
ities at Lord Howe Island in the past 16 years. At two inshore sites t
here was an apparent reduction in hard coral cover in the 1980s.