Islands present both a diversity and a stability 'paradox'. They are o
ften highly species-poor but have considerable biological interest in
terms of extraordinary endemic genera and taxonomically isolated group
s. They appear to be stable, as in some cases these organisms have per
sisted for many millions of years, and having an oceanic climate, extr
eme climatic events may be comparatively rare. However, when subject t
o extrinsic (anthropogenic) disturbance they do not appear to be stabl
e, but often suffer catastrophic ecological change. These apparent par
adoxes are resolved when it is realized that all these features are co
nsequences of the same island characteristics: biotic isolation and oc
eanicity. As a result of these two characteristics, far oceanic island
s are quantitatively different from continental systems in the nature
of their ecological processes, which appear to give rise to an extreme
punctuated equilibrium model of evolutionary change. Endemics may be
ancient relict endemics displaying prolonged stasis and persistence, o
r products of adaptive radiation representing rapid punctuational even
ts. A process-based definition of a relict endemic (palaeoendemic) is
one whose founding lineage (i.e. the original continental source taxon
) has not left any descendents. A corollary of this definition is that
the time of divergence between an endemic and its continental sister-
group should predate the colonization of the island by the now endemic
lineage. An example is Dicksonia arborescens which has been on St Hel
ena for at least 9 Myrs and no longer occurs in the likely source area
of Africa. These relict endemics, frequent on islands, are important
as the last remnants of tranches of biodiversity that have vanished el
sewhere. Island conservation strategies require an integrated understa
nding of both sides of the diversity and stability paradox so that bot
h island processes and island organisms can be conserved.