New information on the presence and relative abundances of 41 reef-building
(zooxanthellate) coral species at 11 eastern Pacific and 3 central Pacific
localities is examined in a biogeographic analysis and review of the easte
rn Pacific coral reef region. The composition and origin of the coral fauna
and other reef-associated taxa are assessed in the context of dispersal an
d vicariance hypotheses. A minimum variance cluster analysis using coral sp
ecies presence-absence classification data at the 14 localities revealed th
ree eastern Pacific reef-coral provinces: (1) equatorial - mainland Ecuador
to Costa Rica, including the Galapagos and Cocos Islands; (2) northern - m
ainland Mexico and the Revillagigedo Islands; (3) island group - eastern Pa
cific Malpelo Island and Clipperton Atoll, and central Pacific Hawaiian, Jo
hnston and Fanning Islands. Coral species richness is relatively high in th
e equatorial (17-26 species per locality) and northern (18-24 species) prov
inces, and low at two small offshore island localities (7-10 species). A hi
gh proportion (36.6%, 15 species) of eastern Pacific coral species occurs a
t only one or two localities; of these, three disappeared following the 198
2-83 ENSO event, three occur as death assemblages at several localities, an
d five are endangered with known populations of ten or fewer colonies. Prin
cipal component analysis using ordinal relative density data for the 41 spe
cies at the 14 localities indicated three main species groupings, i.e., tho
se with high, mid, and narrow spatial distributions. These groupings correl
ated with species population-dynamic characteristics. These results were co
mpared with data for riverine discharges, ocean circulation patterns, shore
line habitat characteristics, and regional sea surface temperature data to
help clarify the analyses as these measures of environmental variability af
fect coral community composition. Local richness was highest at localities
with the highest environmental variability. Recent information regarding th
e strong affinity between eastern and central Pacific coral faunas, abundan
ce of teleplanic larvae in oceanic currents, high genetic similarity of num
erous reef-associated species, and appearances of numerous Indo-west Pacifi
c species in the east Pacific following ENSO activity, suggest the bridging
of the east Pacific filter bridge (formerly east Pacific barrier).