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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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Dur<strong>in</strong>g four stages <strong>in</strong> the development of red p<strong>in</strong>e plantations, spider and<br />

harvestmen (Phalangida) made up about one third of the arthropod fauna dur<strong>in</strong>g the<br />

first two stages-establ ishment and transitional . However, <strong>in</strong> the latter two<br />

stages--macrocul ture and young forest--of community development, spiders made up<br />

50 percent of the total arthropod fauna (Mart<strong>in</strong> 1965).<br />

Forest Soi 1 Mesofauna<br />

Many studies, pr<strong>in</strong>cipally <strong>in</strong> North America and Europe, have dealt with the<br />

effect of harvest<strong>in</strong>g, and residue management, and fire management on forest soil<br />

biota. Most of the research has <strong>in</strong>volved the effect of fire, both prescribed and<br />

wildfire, on soil mesofauna, but some <strong>in</strong>vestigators have studied the response of<br />

mesofauna to silvicul tural practices. There is a general feel <strong>in</strong>g that harvest<strong>in</strong>g<br />

stimulates the development of soil organisms, while prescribed fire substantially<br />

reduces opulations, at least temporarily. Recovery is usually fairly rapid,<br />

especial ! y <strong>in</strong> the upper layers of soil (Bell and others 19741.. I will review the<br />

studies of harvest<strong>in</strong>g, residue management and fire as related to soil mesofauna by<br />

geographic regions, and conclude the section by discuss<strong>in</strong>g soil and surface temperature<br />

dur<strong>in</strong>g fires and its effect on mesofauna.<br />

RESEARCH IN WESTERN UNITED STATES<br />

In the northern Rockies, Fell <strong>in</strong> and Kennedy (1972) studied the relative abundance<br />

of forest soil fauna 1, 2, and 3 years after western white p<strong>in</strong>e forests were clearcut<br />

and prescribed burned. Consider<strong>in</strong>g a1 1 taxa, the total number of <strong>in</strong>dividual s<br />

collected <strong>in</strong> samples from the 1962 burn was nearly half aga<strong>in</strong> as great as samples<br />

from either the 1961 or 196Q burn. Exclud<strong>in</strong>g the mites (Acar<strong>in</strong>a), arthropods <strong>in</strong><br />

samples from the 1960 burn outnumbered those from the 1961 burn by more than five<br />

times and were nearly four times more abundant than those from the 1962 burn. The<br />

Acar<strong>in</strong>a--which comprised 77 percent of the total fauna--were most abundant oe the<br />

1962 burn, more than twice as numerous as on the 1960 burn, and 25 percent more<br />

abundant than on the 1961 burn.<br />

A recent study <strong>in</strong>vestigated the effects of harvest<strong>in</strong>g and residue management<br />

practices, <strong>in</strong>clud<strong>in</strong>g prescribed fire, on forest soi 1 mesofauna <strong>in</strong> northwestern<br />

Montana, Partial results of that study are presented elsewhere <strong>in</strong> this proceed<strong>in</strong>gs<br />

ell<strong>in</strong> <strong>in</strong> 1980~).<br />

Vlug and Borden (1973) studied soil Acari qnd Callembola populations for<br />

1 year <strong>in</strong> clearcut areas that were burned and not burned, and <strong>in</strong> adjacent unlogged<br />

areas, <strong>in</strong> a coastal British Columbia western hemlock and western redcedar forest.<br />

They found the density of mites, Collembola, and other arthropods was reduced by<br />

logg<strong>in</strong>g, and was even further reduced by slash burn<strong>in</strong>g. P~pulation levels and<br />

diversity <strong>in</strong> the logged and burned areas was relatively high, however, <strong>in</strong>dicat<strong>in</strong>g<br />

that neither treatment <strong>in</strong>duced total mortal i ty. Moreover, there was a rapid re<strong>in</strong>vasion<br />

of treated areas. The density of some mites and of Qne family of Callembola<br />

<strong>in</strong> the litter and upper two layers of soil was progressiyely reduced by logg<strong>in</strong>g and<br />

slash burn<strong>in</strong>g, but papul ation densities <strong>in</strong>creased <strong>in</strong> the third and fourth soil<br />

levels. This <strong>in</strong>dicated that either migration to deeper levels or adaptation to<br />

conditions further be1 ow the surface had occurred.

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