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The lichen flora of Svalbard

colonization in the changing Arctic. - Science 316: 1606-1609. Alsos, I.G., Westergaard, K., Lund, L. & Sandbakk, B.F. 2004. Floraen i Colesdalen, Svalbard. - Blyttia 62: 142-150. Alstrup, A. & Elvebakk, A. 1996. Lichenicolous fungi. - Norsk Polarinst. Skr. 198: 259-270. Alstrup, A. & Hawksworth, D.L. 1990. The lichenicolous fungi of Greenland. - Medd. Grønl. Biosci. 31: 1-90. Anonymous. 2003. The place names of Svalbard. - Norsk Polarinstitutt Rapportserie 122

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The Svalbard Airport Temperature Series

References Alexandersson H., 1986, A homogeneity test applied to precipitation data, J. Climatol., 6, 661-675. Benestad R., Hanssen-bauer I., Skaugen T.E., Førland E.J., 2002, Associations between sea-ice and the local climate on Svalbard, DNMI-klima, No. 07/02. Birkeland B.J., 1930, Temperaturvariationen auf Spitzbergen, Meteorol. Zeit., 47, 234-236. Førland E.J., Hanssen-bauer I., Jónsson T., Kern-ha nsen C., Nordli P.Ø., Tveito O.E., Vaa rby Laursen E., 2002, Twentieth-century variations in

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Geographical investigations in the management of the svalbard environment

Ziaja W. , 2019 . Geographical investigations in the management of the Svalbard environment . Quaestiones Geographicae 38(3), Bogucki Wydawnictwo Naukowe , Poznań , pp. 51–57 . 4 figs. Introduction Spitsbergen or Svalbard is a unique Arctic archipelago. Being uninhabited and primeval before its discovery by the Europeans, the archipelago was then developed entirely by them, in the socio-economic sense. Varied forms of exploitation and, after the 1 st World War, protection of natural resources have determined its development. Geographical

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Frequency of Ice Days at Selected Meteorological Stations in Svalbard

References BEDNORZ E., 2011, Occurrence of winter air temperature extremes in Central Spitsbergen, Theor. Appl. Climatol., 106(3-4), 547-556. FØRLAND E.J., HANSSEN-BAUER I. and NORDLI P.Ø., 1997, Climate statistics and long term series of temperature and precipitation at Svalbard and Jan Mayen, DNMI-Rapport, 21/97. Norwegian Meteorological Institute, Oslo FØRLAND E.J. and HANSSEN-BAUER I., 2003, Past and future climate variations in the Norwegian Arctic: overview and novel analyses, Polar Res., 22

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Preservation of magmatic signals in metavolcanics from Wedel Jarlsberg Land, SW Svalbard

., Manecki, M., Rajchel, J. (1993). Geological map of the SW part of Wedel Jarlsberg Land, Spitsbergen, 1:25 000. A. Manecki (Ed.), Kraków: Institute of Geology and Mineral Deposits AGH. Czerny, J., Majka, J., Gee, D. G., Manecki, A., & Manecki, M. (2010). Torellian Orogeny: evidence of a Late Proterozoic tectonometamorphic event in southwestern Svalbard’s Caledonian basement. 29th Nordic Geological Winter Meeting, 11-13 January 2010 (pp. 35-36). Oslo, Norway. NGF Abstract and Proceedings of the Geological Society of Norway. Dallman, W. K

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Monazite Breakdown in Metapelites From Wedel Jarlsberg Land, Svalbard — Preliminary Report

indicators: an example from Wedel Jarlsberg Land, Svalbard. Geolines 20, 88-89. MAJKA J., CZERNY J., MANECKI M., 2004: Petrographical characteristics of the Isbjørnhamna Group Rocks (Wedel Jarlsberg Land, Spitsbergen). Polskie Towarzystwo Mineralogiczne — Prace Specjalne 24, 279-282. MANECKI M., HOLM D. K., CZERNY J., LUX D, 1997: Thermochronological evidence for late Proterozoic (Vendian) cooling in southwest Wedel Jarlsberg Land, Spitsbergen. Geological Magazine 135 (1), 63-69. MICHALIK M

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Svalbard reindeer (Rangifer tarandus platyrhynchus) antler characteristics reflecting the local environmental conditions

W ieren , S.E., 1979. Size and composition of the wild reindeer Rangifer tarandus platyrhynchus population in the Southeast Svalbard Nature Reserve. Holarctic Ecology , 2: 101–107. A mbro ž ová , K., L áska , K., 2017. Air temperature variability in the vertical profile over the coastal area of Petuniabukta, central Spitsbergen. Polish Polar Research , 38: 41–60. A ndersson , M.B., 1994. Sexual selection . Princeton: Princeton University Press. 624 p. C han , K.-S., M ysterud , A., Ø ritsland , N.A., S everinsen , T., S tenseth , N.C., 2005

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Morphology and surficial sediments of the Waldemar River confined outwash fan (Kaffiøyra, Svalbard)

.R., GREENBERG, H.M., 2004, Basinscale availability of salmonid spawning gravel as influenced by channel type and hydraulic roughness in mountain catchments. Canadian Journal of Fisheries and Aquatic Sciences, 61(11): 2085–2096. DALLMANN W.K, ANDRESEN A., BERGH S., MAHER H.D., JR, OHTA Y., 1993, Tertiary fold-and-thrust belt of Spitsbergen, Svalbard. Norsk Polarinstitutt, Meddelelser, 128. FERGUSON, R.I., 2003, Emergence of abrupt gravel to sand transitions along rivers through sorting processes. Geology, 31(2): 159–162. FERGUSON, R., ASHWORTH, P., 1991

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Submarine Evidence of the Late Weichselian Maximum Extent and the Little Ice Age (LIA) Glacier Limits in the St. Jonsfjorden Region (Svalbard)

References Andersen E.S., Dokken T.M., Elverhøi A., Solheim A., Fossen I., 1996, Late Quaternary sedimentation and glacial history of the western Svalbard continental margin, Marine Geol., 133, 123-156. Andersson T., Forma n S.L., Ingólfsson Ó., Manley W.F., 1999, Late Quaternary environmental history of central Prins Karls Foreland, western Svalbard, Boreas, 28, 292-307. Andersson T., Forma n S.L., Ingólfsson Ó., Manley W.F., 2000, Stratigraphic and morphologic constraints on the Weichselian glacial history of

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Effect of Specific Host Body Pigmentation on the Number and Species Composition of the Parasites of Golden Specimen of Cod Gadus Morhua L. From the Svålbard Area

of biometric characters of the "golden" cod and a sample of cod of typical pigmentation ( Gadus morhua morhua L.) captured in the Svålbard bank. EJPAU (Topic: Fisheries) 12 (2). Valtonen, E. T., Maren, M. J., Timola, O., 1983: A note on the intermediate hosts of Echinorhynchus gadi Zoega in Müller (Acanthocephala) in the Baltic Sea. Aquilo Seria Zoologica 22: 93-97. Załachowski, W., 1985: Amount and composition of food of cod ( Gadus morhua ) in the southern Baltic in 1977-1982. Acta Ichth. et Piscat. 15(2): 96

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