Abstract
Mass extinctions have played many evolutionary roles, involving
differential survivorship or selectivity of taxa and traits, the
disruption or preservation of evolutionary trends and ecosystem
organization, and the promotion of taxonomic and morphological
diversifications—often along unexpected trajectories—after the
destruction or marginalization of once-dominant clades. The fossil
record suggests that survivorship during mass extinctions is not
strictly random, but it often fails to coincide with factors promoting
survival during times of low extinction intensity. Although of very
serious concern, present-day extinctions have not yet achieved the
intensities seen in the Big Five mass extinctions of the geologic past,
which each removed ≥50% of the subset of relatively abundant marine
invertebrate genera. The best comparisons for predictive purposes
therefore will involve factors such as differential extinction
intensities among regions, clades, and functional groups, rules
governing postextinction biotic interchanges and evolutionary dynamics,
and analyses of the factors that cause taxa and evolutionary trends to
continue unabated, to suffer setbacks but resume along the same
trajectory, to survive only to fall into a marginal role or disappear
(“dead clade walking”), or to undergo a burst of diversification.
These issues need to be addressed in a spatially explicit framework,
because the fossil record suggests regional differences in
postextinction diversification dynamics and biotic interchanges.
Postextinction diversifications lag far behind the initial taxonomic
and morphological impoverishment and homogenization; they do not simply
reoccupy vacated adaptive peaks, but explore opportunities as opened
and constrained by intrinsic biotic factors and the ecological and
evolutionary context of the radiation.
Publisher
Proceedings of the National Academy of Sciences
Cited by
185 articles.
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