Statistical analyses of occurrence data derived from new collections throug
h scattered Caribbean sections indicate that increased speciation preceded
a pulse of extinction during regional turnover of the Caribbean reef coral
fauna in Plio-Pleistocene time. The data are based on samples that were new
ly collected and identified to species using standardized procedures. Age-d
ates were assigned using high-resolution chronostratigraphic methods. The r
esults show that coral species with a wide range of ecological traits origi
nated and were added to the species pool as much as 1-2 million years befor
e extinction peaked at the end of the turnover interval. Local assemblages
consisted of a mix of extinct and living species, which varied in compositi
on but not in richness. Extinction was selective and resulted in a faunal s
hift to the large, fast-growing species that dominate Caribbean reefs today
. The unusual relationship between origination and extinction may have been
caused by changes in oceanic circulation associated with emergence of the
Central American Isthmus, followed by the onset of Northern Hemisphere glac
iation. The pattern of origination preceding extinction may have been respo
nsible for the stability of reef ecosystems during the intense climatic flu
ctuations of the late Pleistocene, and for the composition and structure of
modern Caribbean reef ecosystems.