The Botany of Iceland - 01.12.1914, Qupperneq 136

The Botany of Iceland - 01.12.1914, Qupperneq 136
320 THORODDSEN lowing mosses are found on stones in rivulets and brooks: Fonti- nalis antipyretica verv frequently, also F. gracilis and F. thulensis, Ambtystegium Kneiffii, A. ochraceum, Hypnum rusciforme var. attantica, and others1. The vegetation of lakes and pools is much richer and differs considerably according to the depth of the water and the nature of the bottom, etc. The plankton of the Icelandic lakes has as yet been very little investigated; there are only a few notes to hand from Myvatn and Thingvallavatn. In Myvatn zooplankton only was found; Thingvallavatn contained phytoplankton in which diatoms were dominant2. In deep lakes tliere is usually very little or no vegetation at greater depths, only in places where it is shal- lower does plant-life occur. In Thingvallavatn, however, there are large areas covered with Chara and Nitelta, especially at a depth of 13—30 metres, and they extend even down to 38 metres3. Where the lakes are shallower various species of Potamogeton and Myrio- phyllum and also Batrachium paucistamineum are common. Near the margin and in smaller pools the most common, and usually dominant, species are the following: Heleocharis palustris, Equisetum timosum, Carex rostrata, Menyanthes trifoliata, and in the southern lowlands Glyceria ftuitans is common; to these should be added Hippuris vulgaris, Eriophorum angustifolium, Sparganinm minimum, S. submuticum, Ranunculus hyperboreus aud R. reptans, Subularia aquatica, Callitriche hamulata and C. verna, Limosella aquatica and several others, the occurrence of which varies somewhat according to the quantity of the water, the conditions at the bottom, elc. Where Equisetum limosum occurs in abundance it is cut annually and used for fodder for milch cows. In Myvatn and in other lakes in Thingeyjarsysla NostocAumps are found in abundance, often thrown up on the shore in very great quantities. Sometimes in warm sum- mers large areas of Myvatn become turbid; this phenomenon is known by the inhabitants as “leirlos” — it is said to be very injurious to salmon-trout, their gills becoming filled with the fine parlicles — when this occurs they retreat in great numbers to the eastern shore of the lake, where the water is purer and clearer owing to the numer- ous springs which here issue from the lava4. 1 H.Jónsson, 1900, p. 17, 1905, p. 7. 2 C. H. Ostenfeld and C. Wesenberg-Lund: A Regular Fortnightly Explor- ation of the Plankton of the two Icelandic Lakes, Thingvallavatn and Myvatn. (Proc. R. Society Edinburgh, Vol. 25, Part 12, 1906, pp. 1092—1167). 8 B. Sæmundsson in Andvari, 1904, p. 89. 4 Dr. H. Jónsson informs me that the so-called "leirlos" is probably due to Blue-green Algæ perhaps Aphanizomenon ftos aquœ.
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The Botany of Iceland

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