Rit Landbúnaðardeildar : B-flokkur - 01.05.1947, Síða 13

Rit Landbúnaðardeildar : B-flokkur - 01.05.1947, Síða 13
11 observed on the shores of the Azores. At the Great Lakes of America the type of C. edentula on the beach belongs to the ssp. lacustris (Fern.) Hultén, but the forms growing in West-America are named ssp. cali- fornica (Fern.) Hultén. The European species C. maritima is found at the beaches of Europe from North-Scandinavia and the Baltic Sea soutli to the Mediterranean and North-Africa. It also is observed at the Black Sea and the Persian Gulf as well as in the Faeroes and Spitzbergen. 5. Discussion. The species Cakile edentulix was originally distinguished from the Linnaean species C. maritima on the basis of its morphological character- istics. Phytogeographical observations were found to give a very good support to the taxonomical understanding of the species. The results obtained by the present writers demonstrate that a sterility barrier must be found between the both species, as the European C. maritima is diploid but the species C. edentula tetraploid. On the basis of the cytological results it is suggested that the latter species should be regarded as an autotetrapioid type. By far the most interesting' question in connection with the present investigation is the dispersion of the species to Iceland. As almost nothing has been written about the origin of the Icelandic flora some discussion on the basis of the present investigation as well as other investigations made by the present and previous writers might be of some interest. As yet, the problems of the origin of the Icelandic flora have not been studied thoroughly. Most of the older scientists seem to have taken it for granted that all the species found at present on the island had dispersed from other countries after the iast glaciation (cf. Thoroddsen> 1914; Stefánsson, 1913, 1920; Stefánsson and Steindórsson, 1937, 1946). During the last decades, however, some scholars have assuined a possible survival of at least a few species during the latest glaciation (Lindroth, 1931; Gelting, 1934; Steere, 1937; Steindórsson, 1937; Thorarinsson, 1937; Löve and Löve, 1943; Löve, 1947). Of course, these assumptions have been influenced by the studies on surviving species of Scandinavia (cf. Hansen, 1904, 1930; Fries, 1913; Nordhagen, 1932, 1933, 1935; Nannfeldt, 1935, 1940; Holmboe, 1937; Björkman, 1939; Du Rietz, 1942; Hasselrot, 1935, 1941; Samuei.sson, 1943; Arwidsson, 1943). Last summer the present writers began an investigation of the origin of the Icelandic flora elements. The present paper is the first publication

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