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Principles of terrestrial ecosystem ecology.pdf

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<strong>ecosystem</strong>s and current climate. Similarly, the<br />

legacies <strong>of</strong> the current environment will exert<br />

large effects on the future structure and functioning<br />

<strong>of</strong> <strong>ecosystem</strong>s.<br />

Disturbance<br />

Conceptual Framework<br />

Disturbance is a major cause <strong>of</strong> long-term fluctuations<br />

in the structure and functioning <strong>of</strong><br />

<strong>ecosystem</strong>s. We define disturbance as a relatively<br />

discrete event in time and space that<br />

alters the structure <strong>of</strong> populations, communities,<br />

and <strong>ecosystem</strong>s and causes changes in<br />

resource availability or the physical environment<br />

(Pickett and White 1985, Pickett et al.<br />

1999). Many natural disturbances, such as<br />

herbivore outbreaks, treefalls, fires, hurricanes,<br />

floods, glacial advances, and volcanic eruptions,<br />

exert these effects through reductions in live<br />

plant biomass or sudden changes in the pool <strong>of</strong><br />

actively cycling soil organic matter. Disturbance<br />

is difficult to define unambiguously.<br />

Events such as intensive grazing and subzero<br />

temperatures that are normal features <strong>of</strong> some<br />

<strong>ecosystem</strong>s seriously disrupt the functioning <strong>of</strong><br />

others. Disturbance must therefore be defined<br />

in the context <strong>of</strong> the normal range <strong>of</strong> environmental<br />

variation that an <strong>ecosystem</strong> experiences.<br />

The dividing line between disturbance<br />

and normal function is somewhat arbitrary.<br />

Herbivory, for example, is <strong>of</strong>ten treated as part<br />

<strong>of</strong> the steady-state functioning <strong>of</strong> <strong>ecosystem</strong>s,<br />

whereas stand-killing insect outbreaks are<br />

treated as disturbances. The processes are<br />

similar, however, and there is a continuum in<br />

size, severity, and frequency between these two<br />

extremes. Disturbance is clearly not an external<br />

event that “happens” to an <strong>ecosystem</strong>. Like<br />

other interactive controls, disturbance is an<br />

integral part <strong>of</strong> the functioning <strong>of</strong> all <strong>ecosystem</strong>s<br />

that responds to and affects most<br />

<strong>ecosystem</strong> processes. Naturally occurring disturbances<br />

such as fires and hurricanes are<br />

therefore not “bad”; they are normal properties<br />

<strong>of</strong> <strong>ecosystem</strong>s.<br />

Human activities have altered the frequency<br />

and size <strong>of</strong> many natural disturbances, such as<br />

Disturbance 285<br />

fires and floods, and have produced new types<br />

<strong>of</strong> disturbance, such as large-scale logging,<br />

mining, and wars. Many human disturbances<br />

have ecological effects that are similar to those<br />

<strong>of</strong> natural disturbances, so the study <strong>of</strong> either<br />

natural or human disturbances provides<br />

insights into the regulation <strong>of</strong> <strong>ecosystem</strong><br />

processes and human impacts on these processes.<br />

Natural and anthropogenic disturbances<br />

interact with environmental gradients to create<br />

much <strong>of</strong> the spatial patterning in landscapes<br />

(see Chapter 14).<br />

After disturbance, <strong>ecosystem</strong>s undergo<br />

succession, a directional change in <strong>ecosystem</strong><br />

structure and functioning resulting from biotically<br />

driven changes in resource supply. Disturbances<br />

that remove live or dead organic matter,<br />

for example, are colonized by plants that gradually<br />

reduce the availability <strong>of</strong> light at the soil<br />

surface and alter the availability <strong>of</strong> water and<br />

nutrients (Tilman 1985). If there were no<br />

further disturbance, succession would proceed<br />

toward a climax, the end point <strong>of</strong> succession<br />

(Clements 1916). At this point, the structure<br />

and rates <strong>of</strong> <strong>ecosystem</strong> processes approach<br />

a steady state in which resource demand by<br />

vegetation would be balanced by the rate <strong>of</strong><br />

resource supply. In practice, however, new disturbances<br />

usually occur before succession<br />

reaches a climax, so individual stands <strong>of</strong> an<br />

<strong>ecosystem</strong> are seldom in steady state. Nonetheless,<br />

the concept <strong>of</strong> directional changes in<br />

vegetation after disturbance provides a useful<br />

framework for analyzing the role <strong>of</strong> disturbance<br />

in <strong>ecosystem</strong> processes.<br />

Succession occurs in response to biotically<br />

driven changes in resource supply, which<br />

typically occur over time scales <strong>of</strong> years to<br />

centuries. Succession does not therefore<br />

include the seasonal fluctuations in <strong>ecosystem</strong><br />

processes from summer to winter, which are<br />

driven more directly by climate than by the<br />

internal dynamics <strong>of</strong> <strong>ecosystem</strong>s.<br />

Disturbance Properties<br />

The impact <strong>of</strong> disturbance on <strong>ecosystem</strong> processes<br />

depends on its severity, frequency, type,<br />

size, timing, and intensity. Together these attributes<br />

<strong>of</strong> disturbance constitute the disturbance

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