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Náttúrufræðingurinn - 2001, Side 32

Náttúrufræðingurinn - 2001, Side 32
Spárck, R. & Thorson, G. 1933. Marine gastro- poda prosobranchiata. The Zoology of the Faroes 3(1). 1-45. Spjeldnaes, N. & Henningsmoen, K.E. 1963. Littorina littorea: An indicator of Norse set- tlement in North America? Science 141.275- 276. Thorson, G. 1941. Marine gastropoda proso- branchiata. The Zoology of Iceland 4 (60). 1- 150. Vermeij, G.J. 1982. Environmental changes and the evolutionary history of the periwinkle (Littorina littorea) in North America. Evolu- tion 36. 561-580. Wagner, F.J.E. 1977. Recent mollusc distri- bution patterns and palaeobathymetry, southeastern Beaufort Sea. Canadian journal of Earth Sciences 14 (9). 2013-2028. West, R.G., Funnell, B.M. & Norton, P.E.P. 1980. An early Pleistocene cold Marine epi- sode in the North Sea: Pollen and faunal as- semblages at Covehite, Suffolk, England. Boreas 9 (1). 1-10. Wood, S.V. 1848. A monograph of the Crag Mollusca. 1. Univalves. The Palaeontographi- cal Society, London. 208 bls. Woodward, B.B. 1913. The life of Mollusca. Methuen, London. 158 bls. Zaslavskaya, N.I., Sergievsky, S.O. & Tatarenkov, A.N. 1992. Allozyme similarity of Atlantic and Pacific species of Littorina (Gastropoda: Littorinidae). Journal of Molluscan Studies 58. 377-384. Þorleifur Einarsson, Hopkins, D.M. & Doell, R.R. 1967. The stratigraphy of Tjörnes north- ern Iceland and the history of the Bering Land Bridge. í: The Bering Land Bridge (ritstj. D.M. Hopkins). Stanford University Press, Stanford. Bls. 312-325. Þorvaldur Thoroddsen 1892. Postglaciale marine Aflejringer, Kystterrasser og Strandlinier i Is- land. Geografisk Tidsskrift 11.209-225. ■ SUMMARY The mesogastropod Littorina littorea (Linné, 1758) in Iceland: PALAEOBIOGEOGRAPHYAND MIGRATION The periwinkle Littorina littorea (Linné, 1758) has not been found living at present in Iceland The only confirmed occurrence of the species in Iceland is in the Middle Pleistocene upper littq ral conglomerate in Búlandshöfdi, Snæfellsnes west Iceland. These layers were deposited dur- ing an interglacial, slightly older than 1.1 Ma. The species apparently evolved from the Pacific L. squalida Broderip and Sowerby, 1829, during the trans-Arctic-North Atlantic migration from the Pacific as a result of cooling. The oldest fos- sil occurrence of the species is in the British Red Crag, 2.4-2.55 Ma old, and it has not been found in the Pliocene Tjörnes deposits in north Iceland which are older than 2.6 Ma. This indicates that the species separation postdates the deposition of the uppermost Serripes Zone of Tjörnes, af- ter the tide of the migration wave passed Iceland but before it reached the North Sea area and Brit- ain. PÓSTFANG HÖFUNDA /AUTHORS'ADDRESS Ólöf E. Leifsdóttir Netfang/e-mail: oel@rhi.hi.is Leifur A. Símonarson Netfang/e-mail: leifuras@raunvis.hi.is Raunvísindastofnun Háskólans /Science Institute Jarðfræðahús Háskólans IS-101 Reykjavík 110

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