The Botany of Iceland - 01.12.1945, Page 41

The Botany of Iceland - 01.12.1945, Page 41
THE VEGETATION OF CENTRAL ICELAND 383 Molholm Hansen was the first of all botanists to make statistical analyses of the vegetation of Iceland. Among others he an- alysed the alpine flói vegetation of Arnarvatnsheiði at c. 500 m above sea-level (Molholm Hansen 1930, pp. 111-114). The results of his analyses can be compared with mine. But I think his concept of the flói too narrow, and this is also H u m 1 u m’s opinion (1936, p. 69 ff). The “plane Mýri” (level mýri) mentioned by Humlum and the Carex rariflora-mýú mentioned by Molholm Hansen I refer without reservation to the flói. My experience as to the occurrence of C. rariflora differs essentially from that of M 01 h o 1 m Hansen, as I have often met with this species in the dampest part of the flói as well as in its drier places. It is mostly assumed that the flói is only formed in depressions whence the water cannot be drained. In the highland it is often formed in inland deltas along rivers in entirely the same way as the Carex Lyngbyei mýri in the lowland. Thus the largest continuous areas of flói observed by me in the highland are found on Eyjabakkar and are formed precisely in this way. Something similar is the case with the flói in Kýlingar and in Jökuldalir. In these places the ground-water is not quite stagnant; the surface slopes, though inconsiderably, in the same direction in which the rivers flow. These areas of flói no doubt belong to the “Fétmýri” according to MolholmHansen’s defini- tion of the latter (1. c. p. 180). In another paper (Steindórsson 1936, p. 443) I have pointed out that the otherwise clear division of the mýri series made by Molholm Hansen is very difficult to maintain in practice when one examines the species composition of the different formations. Thus the character species of the Fétmýri, Carex Lyngbyei, sometimes occurs in the flói; on the other hand there are areas, at any rate in the highland, which according to their develop- ment and nature should indisputably belong to the Fétmýri as defined by Molholm Hansen, which as regards its vegetation is indis- tinguishable from the most typical flói. For these reasons I follow Stefánsson and Jónsson in distinguishing only between the two main types of the mýri series, viz. the flói and the mýri. Still it would be convenient to mention as a subdivision of the flói what in Icelandic might be called the “Flæðimýri”, which corresponds to the German “Verlandungsmoor”, on account of its special mode of formation along rivers and lakes. A brief definition of the flói formation based on the descriptions of earlier authors and on my own observations will then be as follows:
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