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June 1 - 3 , 1978 - University of Hawaii at Manoa

June 1 - 3 , 1978 - University of Hawaii at Manoa

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level were analysed against altitude distributions <strong>of</strong> the sample<br />

st<strong>at</strong>ion plotsites via correl<strong>at</strong>ion coefficients gener<strong>at</strong>ed by:<br />

= S x ~ where 2xy (covariance). = 1 (Cxiyi - 1 XxiCyi)<br />

SxS y n-l n<br />

and 2, = hi2 - (CX?) '/n j .-I<br />

- sy = jiyi2 - (~yi)~/n<br />

n - 1<br />

where 2, and sy are standard devi<strong>at</strong>ions, x and y being values <strong>of</strong><br />

two discrete and changing factors: alfitude and the number <strong>of</strong><br />

insect families encountered.<br />

RESULTS<br />

There was a general linear increase in the number <strong>of</strong><br />

families collected with decreasing altitude (Table 1). Correl<strong>at</strong>ion<br />

coefficients calcul<strong>at</strong>ed using the mean number<br />

collected <strong>at</strong> isoaltitudinal plots substanti<strong>at</strong>ed<br />

<strong>of</strong> families<br />

this linear<br />

rel<strong>at</strong>ionship (r<br />

n = 5).<br />

- = -0.72, -<br />

With decreasing altitude, gre<strong>at</strong>er numbers <strong>of</strong> families appeared<br />

during the first half <strong>of</strong> the collection periods. At the<br />

1690 m st<strong>at</strong>ion, 50% <strong>of</strong> families encountered were collected by the<br />

midpoint <strong>of</strong> the collection period. At 1150 m, this figure had<br />

increased to 70%. while <strong>at</strong> 875 m it was 79% and <strong>at</strong> 585 m, the<br />

insects collected by the first half <strong>of</strong> the collecting period<br />

amounted to 84% <strong>of</strong> the total yield. The rise in this temporal<br />

packing correl<strong>at</strong>ed with altitude (r - = -0.74, - n = 12).<br />

An interesting exception to the linear rel<strong>at</strong>ionship <strong>of</strong> both<br />

family diversity and temporal packing trends ocurred <strong>at</strong> the<br />

1440 m elev<strong>at</strong>ion, where both diversity and packing exceeded figures<br />

characteristic <strong>of</strong> the 1150 m plots, and were only slightly<br />

lower than values <strong>at</strong> the 875 m level. This "hump" is easily seen<br />

in Figure 2. If the d<strong>at</strong>a from the 1440 m plots are deleted, and<br />

correl<strong>at</strong>ion coefficients are again calcul<strong>at</strong>ed, the linear fit<br />

against altitude is far more precise (family diversity/altitude<br />

- r = -0.82, - n = 9; temporal packing/altitude - r = -0.91, - n = 9).<br />

The distribution <strong>of</strong> entomology sites, veget<strong>at</strong>ion ecology<br />

relevi st<strong>at</strong>ions, habit<strong>at</strong> descriptions, and clim<strong>at</strong>ic observ<strong>at</strong>ions<br />

along the altitudinal gradient are presented in Figure 3. The<br />

number <strong>of</strong> vascular plant species and insect families encountered<br />

<strong>at</strong> identical sites are compared in Figure 4. The d<strong>at</strong>a is uti-<br />

lized in the discussion to assess veget<strong>at</strong>ional correl<strong>at</strong>ions and<br />

to incorpor<strong>at</strong>e several situ<strong>at</strong>ions to interpret both general<br />

trends and the "hump" phenomenon.

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