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Full-text - Norsk entomologisk forening

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Norwegian stoneflies II 215<br />

of Finnmark, northern Norway and can in<br />

this sense be compared with the inner areas<br />

of Rogaland (area 1). The main differences<br />

are in latitude, vegetation belts and in the<br />

fact that the oceanity factor is much lower.<br />

Area description<br />

Ten streams and 2 lakes were investigated<br />

in the area. The central parts consist largely<br />

of sandstone and greenstone, while the peripheral<br />

parts consist of little altered Eocambrian<br />

sediments. Drift material is present,<br />

especially in the stream valleys.<br />

The climate has a pronounced continental<br />

character. Precipitation generally lies between<br />

400 and 600 mm a year, although the<br />

southern parts can have below 400 mm. The<br />

June isotherm is similar to the inner fjords<br />

of area 1 (western Norway). The July temperature<br />

is lower and can be compared to<br />

the western coastal areas or the mountain<br />

areas of southern Norway.<br />

In the Alta area there are deep valleys<br />

which converge on the fjord at Alta. In the<br />

southern and eastern parts of the area, mountains<br />

between 800 and 700 m a.s.l. are common,<br />

while in the western parts the landscape<br />

is generally higher, with mountains of 1100<br />

m a.s.l. and above. Around the village of<br />

Alta and the lower parts of the valleys there<br />

are pine woods, mixed with willow, alder<br />

and other deciduous trees. Above this, in the<br />

Sub-Alpine belt, there is largely birch and<br />

willow.<br />

Stream descriptions<br />

The main river in this area is the River<br />

Alta. In addition, there are numerous small<br />

and large streams. In places there is a dense<br />

fringe of deciduous trees along the streams<br />

which consists mainly of willow, alder and<br />

birch. In the Sub-Alpine belt willow dominates<br />

alongside the streams and may be very<br />

dense and high in the lower sections. Higher<br />

up the bushes are lower, but growth may still<br />

be dense. In the Alpine belts the willow<br />

gradually disappears (Figs. 9, 10).<br />

Calcium hardness was measured both<br />

during 1968 and 1972 in several places, and<br />

values varied between 0.9 and 2.7 mg<br />

Ca++/l. Values of pH lay generally between<br />

Fig. 9. Stream by Leirbotnvann in the Sub-Alpine<br />

belt.<br />

Fig. 10. Stream in Stokkedalen in the Low-Alpine<br />

belt.<br />

6.0 and 6.8, although somewhat lower in the<br />

higher areas.<br />

Stonefly fauna<br />

In this area 18 species of stoneflies were<br />

taken (Table VIII). Of the five species which<br />

are restricted to northern Norway, only two<br />

were represented, N emoura arctica and Nemoura<br />

sahlbergi.<br />

The dominant carnivore was Arcynopteryx<br />

compacta, which occurred in lakes, lake outlets,<br />

and in streams. Diura bicaudata was<br />

also common and was taken in streams, lakes<br />

and lake outlets. Diura nanseni was taken in<br />

streams and lake outlets and all three species<br />

were taken together in the outlet of a lake<br />

(Fig. 10). The most common herbivores were<br />

Capnia atra, Leuctra hippopus, and Nemoura<br />

cinerea. In this area 16 species were taken in<br />

streams, 7 in lake outlets, and 5 in lakes.

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