
this correlation does not prove causation, since there are many other things that
change between Panama and Alaska. There is no established relationship between
climatic instability and species richness.
10.4.2 Disturbance
Previously, in Section 9.4, the influence of disturbance on community structure
was examined, and it was demonstrated that when a disturbance opens up a gap,
and the community is dominance controlled (strong competitors can replace
residents), there tends in a community succession to be an initial increase in rich-
ness as a result of colonization, but a subsequent decline in richness as a result
of competitive exclusion.
If the frequency of disturbance is now superimposed on this picture, it seems
likely that very frequent disturbances will keep most patches in the early stages
of succession (where there are few species) but also that very rare disturbances
will allow most patches to become dominated by the best competitors (where
there are also few species). This suggests an intermediate disturbance hypothesis,
in which communities are expected to contain most species when the frequency
of disturbance is neither too high nor too low (Connell, 1978). The intermediate
disturbance hypothesis was originally proposed to account for patterns of rich-
ness in tropical rain forests and coral reefs. It has occupied a central place in
the development of ecological theory because all communities are subject to
disturbances that exhibit different frequencies and intensities.
Among a number of studies that have provided support for this hypothesis,
we turn first to a study of green and red algae on different-sized boulders on
the rocky shores of southern California (Sousa, 1979a, 1979b). Wave action
disturbs small boulders more frequently than larger ones; thus, small boulders
had a monthly probability of movement of 42%, intermediate-sized boulders
a probability of 9%, and large boulders a probability of only 0.1%. After a
disturbance clears space on a boulder, ephemeral green algae (Ulva spp.) are
quick to colonize, but later in the year several species of perennial red alga
feature in the succession, including Gelidium coulteri, Gigartina leptorhinchos,
Rhodoglossum affine and Gigartina canaliculata. The last of these gradually takes
over until within 2–3 years it dominates the community, tending to competitively
exclude the early and mid-successional species. G. canaliculata then persists
unless there is a further disturbance. Sousa found that algal species richness was
lowest on the frequently (F) disturbed small boulders – these were dominated
most often by Ulva. The highest levels of species richness were consistently
recorded on the intermediate boulder class (I), most of which held mixtures of
3–5 abundant species from all successional stages. Finally, species richness on the
rarely disturbed (R), largest boulders was lower than the intermediate class, with
a monoculture of G. canaliculata on some of them (Figure 10.11a).
Disturbances in small streams often take the form of bed movements during
periods of high discharge, and because of differences in flow regimes and in the
substrata of stream beds, some stream communities are disturbed more frequently
than others. This variation was assessed in 54 stream sites in the Taieri River in
New Zealand. The pattern of richness of macroinvertebrate species conformed to
the intermediate disturbance hypothesis (Figure 10.11b). Finally, in controlled
field experiments, natural phytoplankton communities in Lake Plußsee (north
Part III Individuals, Populations, Communities and Ecosystems
338
the intermediate disturbance
hypothesis...
. . . supported by studies of algae
on boulders on a rocky shore...
. . . and from studies of
invertebrates in small streams
and plankton in lakes
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