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NORSK ENTOMOLOGISK TIDSSKRIFT - Norsk entomologisk forening

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The Tana often floods as early as mid-May,<br />

and the inundations are usually over before<br />

mid-June.<br />

Flooding is seldom accompanied by ice­<br />

drifting on the Gaula, the Namsen, Saltdals­<br />

elva, and Malselva. This only happened on the<br />

Namsen on 3 March 1948 and 9 February<br />

1960, and on the Gaula on 1 May 1966 (water<br />

level at Gaulfoss 6.7 m). Along these rivers the<br />

thaw in the lowland is usually complete<br />

before is has commenced in the mountains.<br />

On the Tana in Finnmark, drifting of ice<br />

usually occurs at the same time as the spring<br />

floods, because of simultaneous thawing over<br />

a wide range within the watercourse.<br />

The temperature in the Gaula during the<br />

spring flood in 1965 was 7-8°C, in Mfilselva<br />

in June 1966 8·9°C, and on 2 June 1967 it<br />

was 6°C. These temperatures were measured<br />

in the rivers. In backwaters the temperature<br />

at Rundhaug, 2 June 1967, was higher, up to<br />

12°C, but as the river rapidly rose the<br />

temperature decreased, and finally the tem­<br />

perature differences were negligible.<br />

THE EFFECT OF INUNDATION<br />

THE EFFECT OF INUNDATIONS<br />

119<br />

Investigation of fauna during and after inunda­<br />

tions<br />

I. Investigations during rising water level<br />

on MiUselva (Rundhaug) 2-3 June and<br />

22-23 June 1967<br />

On both occasions, the river rose rapidly<br />

from a moderate to a high level during the<br />

night. The surface layer of the zones up to<br />

1 m above the water's edge was investigated.<br />

Sample 1-1 (Table II), 2 June 1967: Sandy<br />

places without vegetation. Lower lying sandy<br />

places submerged.<br />

Samples 1-2 (Table II), 2 June (1-2, A) and<br />

22 June 1967 (1-2, B and C): Gravelly slopes<br />

without vegetation, mostly elevated.<br />

Samples 1-3 (Table 1I), 2 June (1-3, A) and<br />

22 June 1967 (1-3, B): Strongly sloping, gravel­<br />

ly declivity, ending above in a dense grassy<br />

mat. Most of the lower lying gravelly sites<br />

submerged. None of the species listed in the<br />

table were taken from the same sites at low<br />

water level.<br />

Table 11. Coleoptera collected in Samples / /-3 by time-catch. The figures give the number o[specimens;<br />

ifestimated, the abundance per m 2 is given in brackets<br />

Sample I-I 1-2, A 1-2, B 1-2, C 1-3, A 1-3, B<br />

Collecting time (mins.) 15 26 20 14 40 20<br />

Dyschirius septentrionum Munst. 1 (0.3)<br />

Bembidion dlffici/e Mtsch. 1 (0.2)<br />

B. /apponicum Zett. 2 2 (0.6) 1 (0.4) 1 (0.5) 2 (0.4) 1 (0.4)<br />

B. petrosum Geb\. I 25 (7.2) 21 (7.9) 10 (5.4) 83 (15.6) 18 (6.8)<br />

B. prasinum Dft. 1 (0.3) 2 (1.2) 3 (0.6) 2 (0.8)<br />

B. schueppe/i Dej. 5 (1.5) 1 (0.4)<br />

B. virens Gyl\. I (0.2)<br />

Agonum [u/iginosum Panz. 1 (0.4)<br />

Geodromicus p/agiatus F. 2 (0.8)<br />

Stenus [uscipes Gr. 1 (0.4)<br />

S. strandi Bck. 2 (0.4)<br />

Oxypoda proceru/a Mnh. 1 (0.2)<br />

Hypnoidus pu/che//us L. 2<br />

H. rivu/arius Gyl\. 2 (0.4)

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