Náttúrufræðingurinn

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Náttúrufræðingurinn - 1995, Qupperneq 55

Náttúrufræðingurinn - 1995, Qupperneq 55
Thamdrup, H.M. 1935. Beitriige zur Ökologie der Wattenfauna auf experimenteller Grund- lage. Meddelelser fra Kommissionen for Danmarks Fiskeri- og Havunderspgelser, Serie Fiskeri 10 (2). 125 bls. Thorson, G. 1946. Reproduction and larval de- veloptnenl of Danish marine bottom inverte- brates. Meddelelser fra Kommissionen for Danmarks Fiskeri- og HavundersOgelser, Serie Plankton 4 (1). 523 bls. Thorson G. 1968. Infaunaen, den jævne hav- bunds dyreliv. í Danmarks natur 3, Havet (rilstj. A. Nprrevang og T.J. Meyer). Politik- ens forlag, Kpbcnhavn. 82-166. van Slraaten, L.M.J.U. 1952. Biogene lextures and the formation of shell beds in the Dutch Wadden Sea. Proceedings Koninklijke Ned- erlandse Akademie van Wetenschappen, Se- ries B 55 (5). 500-516. Wells, G.P. 1945. The mode of life of Areni- cola marina L. Journal of the Marine Bio- logical Association of the U.K. 26. 170-207. Wells, G.P. 1949. The behaviour of Arenicola marina L. in sand, and the role of spontane- ous activity cycles. Journal of the Marine Biological Association of Ihe U.K. 28. 465- 478. Werner, B. 1954. Eine Beobachtung iiber die Wanderung von Arenicola marina L. (Poly- chaeta sedentaria). Helgoliinder wissen- schaftliche Meeresuntersuchungen 5. 93- 102. Werner, B. 1956. Uber die Winterwanderung von Arenicola marina L. (Polychaeta sedcnt- aria). Helgolander wissenschaftliche Meeres- untersuchungen 5. 353-378. Wesenberg-Lund. E. 1951. Polychaeta. The Zoology of lceland 2(19). 182 bls. Þorleifur Einarsson 1969. Loftslag, sjávarhiti og haffs á forsögulegum líma. í Hafísinn (ritstj. Markús Á. Einarsson). Almenna bóka- félagið, Reykjavík. 389-402. Örsted, A.S. 1843. Grönlands Annulata Dorsi- branchiata. Det Kongelige Danske Viden- skabernes Selskabs naturvidenskabelige og mathematiske Alliandlinger 10. 153-216. ■ SUMMARY Tephra-eating lugworms in SUBMERGEÐ PEAT IN SOUTHEAST ICELAND The lugworm Arenicola marina (Linné) is widely distributed in Iceland where it is a char- acteristic species for niuddy sands in tidal flats and down to about 6 m water dcpth. It seems to be equally common in the low-arctic regions of the north and east coasts and the high-boreal areas along the west and south coasts. The lugworm generally lives in a J-shaped burrow with a small depression above the oral end. The animal usually ingests muddy sand with detri- tus and microorganisms, and deposits the char- acteristic faecal heaps above the anal cnd. In the Hornatjörður region in Southeast Ice- land, lugworms were observed that had bur- rowed in subnterged peat containing lephra lay- ers. Some of thc worms were ingesting the lighl-gray tephra from the Öræfajökull eruption of 1362 and the resulting light-coloured faecal heaps were very prominent on the surface of the dark tidal llats. The tephra-eating lugworms seem to thrive well and, apparenlly, the sharp- edged glass shards do not damage the digestive organs of the animals. The peat submerged af- ter the tephra fell in 1362, due to later glacio- isostatic subsidence during the climatic deterio- ration of the „Little Ice Age“ (1600-1900). Af- ter 1900 there has been glacio-isostatic rise of land in the area, due to climatic amelioration and melting of glaciers, resulling in rising of the submerged peat to the water level, llius gradually restricting the lugwornt habitats. As sediments have been washed away from the top of the rising peat, lugworms have started to bur- row into the peat, thus adapting to the environ- mental changes. PÓSTFANG HÖFUNDA/AUTHORS' ADDRESS Leifur A. Símonarson Raunvísindastofnun Háskólans/ Science Institute Jarðfræðahúsi Háskólans IS-101 REYKJAVÍK Páll Imsland Raunvísindastofnun Háskólans/ Science Inslitute Dunhaga 3 IS-107 REYKJAVÍK 163
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