Abstract
Human activities have greatly reduced the amount of the earth's
area available to wild species. As the area they have left declines, so
will their rates of speciation. This loss of speciation will occur for
two reasons: species with larger geographical ranges speciate faster;
and loss of area drives up extinction rates, thus reducing the number
of species available for speciation. Theory predicts steady states in
species diversity, and fossils suggest that these have typified life
for most of the past 500 million years. Modern and fossil evidence
indicates that, at the scale of the whole earth and its major
biogeographical provinces, those steady states respond linearly, or
nearly so, to available area. Hence, a loss of x% of
area will produce a loss of about x% of species. Local
samples of habitats merely echo the diversity available in the whole
province of which they are a part. So, conservation tactics that rely
on remnant patches to preserve diversity cannot succeed for long.
Instead, diversity will decay to a depauperate steady state in two
phases. The first will involve deterministic extinctions, reflecting
the loss of all areas in which a species can ordinarily sustain its
demographics. The second will be stochastic, reflecting accidents
brought on by global warming, new diseases, and commingling the species
of the separate bio-provinces. A new kind of conservation effort,
reconciliation ecology, can avoid this decay. Reconciliation ecology
discovers how to modify and diversify anthropogenic habitats so that
they harbor a wide variety of species. It develops management
techniques that allow humans to share their geographical range with
wild species.
Publisher
Proceedings of the National Academy of Sciences
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