Náttúrufræðingurinn

Ukioqatigiit

Náttúrufræðingurinn - 1988, Qupperneq 32

Náttúrufræðingurinn - 1988, Qupperneq 32
þvermál og eru því um það bil helmingi minni en stærstu rauðviðartrén, sem verða yfir 110 m á hæð, og eru með stærstu lífverum jarðarinnar. En hvað sem segja má um stærðina þá virðist kínarauðviðurinn ætla að þrauka og er nú talinn úr útrýmingarhættu. HEIMILDIR Chaney, R.W. 1951. A revision of fossil Sequoia and Taxodium in western North America based upon recent discoveries. — Trans. Amer. Phil. Soc. New Ser. 40: 171-263. Freysteinn Sigurðsson & Kristján Sæmunds- son. 1984. Surtarbrandur á Vestfjörðum. - Orkustofnum OS-84039/OBD-02, 43 bls. Gothan, W. & H. Weyland. 1964. Lehrbuch der Paláobotanik, 2. útg. - Akademie Verlag, Berlín: 594 bls. Guðmundur G. Bárðarson. 1918. Um surtar- brand. - Andvari 43: 1-71. Hewes, J. 1981. Redwoods. - Hamlyn, Lond- on: 192 bls. Jóhannes Áskelsson. 1942. Surtarbrands- náman í Botni. - Náttúrufr. 12: 144-148. McDougall, I., Leó Kristjánsson & Kristján Sæmundsson. 1984. Magnetostratigraphy and geochronology of Northwest Iceland. - J. Geoph. Res. 89 (88): 7029-7060. Miki, S. 1941. On the change of flora in east- ern Asia since the Tertiary period. - Jap- an J. Bot. 11: 237-303. Rasmussen, J. & E.B. Koch. 1963. Fossil Metasequoia from Mikines, Faroe Is- lands. - Fróðskaparrit 12: 83-96. SUMMARY Fossil Metasequoia from Súgandafjörður, Northwest Iceland by Leifur A. Símonarson Raunvísindastofnun Háskólans Dunhaga 3 107 Reykjavík, Iceland Fragmentary shoots of Metasequoia with several decussate, linear leaves are described from Tertiary interbasaltic sediments in Súg- andafjörður, Northwest Iceland. The shoots probably belong to Metasequoia occidentalis Chaney which occurs in the entire Tertiary system. However, here Metasequoia is descri- bed for the first time in Icelandic deposits. The sediments in Súgandafjörður are of Upp- er Miocene age and 13-14 m.y. old. They belong to the oldest plant-bearing horizon in Iceland, which comprises the Selárdalur- Botn flora consisting of mixed warm-temp- erate forest of deciduous trees and conifers where angiosperms dominate over conifers and Taxodiaceae over Pinaceae. 26
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