Antarktis-bibliografi er en database over den norske Antarktis-litteraturen.

Hensikten med bibliografien er å synliggjøre norsk antarktisforskning og annen virksomhet/historie i det ekstreme sør. Bibliografien er ikke komplett, spesielt ikke for nyere forskning, men den blir oppdatert.

Norsk er her definert som minst én norsk forfatter, publikasjonssted Norge eller publikasjon som har utspring i norsk forskningsprosjekt.

Antarktis er her definert som alt sør for 60 grader. I tillegg har vi tatt med Bouvetøya.

Det er ingen avgrensing på språk (men det meste av innholdet er på norsk eller engelsk). Eldre norske antarktispublikasjoner (den eldste er fra 1894) er dominert av kvalfangst og ekspedisjoner. I nyere tid er det den internasjonale polarforskninga som dominerer. Bibliografien er tverrfaglig; den dekker både naturvitenskapene, politikk, historie osv. Skjønnlitteratur er også inkludert, men ikke avisartikler eller upublisert materiale.

Til høyre finner du en «HELP-knapp» for informasjon om søkemulighetene i databasen. Mange referanser har lett synlige lenker til fulltekstversjon av det aktuelle dokumentet. For de fleste tidsskriftartiklene er det også lagt inn sammendrag.

Bibliografien er produsert ved Norsk Polarinstitutts bibliotek.

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Abstracts

Botnen, A., & Øvstedal, D. O. (1988). Muscicolous Lepraria species and other leprarioid lichens in the Antarctic. Polar Research, 6(1), 129–133. https://doi.org/10.3402/polar.v6i1.6853

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Fevolden, S. E. (1988). Biochemical genetics and population structure of Euphausia superba. Comparative Biochemistry and Physiology Part B: Comparative Biochemistry, 90(3), 507–513. https://doi.org/https://doi.org/10.1016/0305-0491(88)90289-1

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Fevolden, S. E., & Schneppenheim, R. (1988). Genetic population structure of Euphausia superba DANA in the Atlantic Sector of the Southern Ocean as demonstrated by different electrophoretic techniques. Polar Biology, 9(1), 1–8. https://doi.org/10.1007/BF00441759

Electrophoretic analyses of allele distributions at nine polymorphic gene loci were conducted in samples of Euphausia superba from the Bransfield Strait, off the South Orkney Islands, and from the south-eastern part of the Weddell Sea. The aim was to determine whether reported phenotypic differences between krill stocks from these areas could be linked to genotypic differences. Despite minor deviations of genotype distributions from Hardy-Weinberg expectations, the data gave no evidence of genetic heterogeneity over the sampled area, and the hypothesis of a single genetically homogeneous krill population could not be rejected. Genetic data for four selected loci were verified by using two different electrophoretic methods. Results from these two techniques yielded no discrepancies in interpretation of the data.

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Foldvik, A., & Gammelsrød, T. (1988). Notes on Southern Ocean hydrography, sea-ice and bottom water formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 67(1), 3–17. https://doi.org/https://doi.org/10.1016/0031-0182(88)90119-8

The Southern Ocean circulation and sea-ice distribution is briefly described. The formation of extremely cold bottom water in the Weddell Sea and its relation to the floating Ronne-Filchner Ice Shelves is discussed. It is shown that a concentrated swift eroding bottom current with anomalous low ratio transports the cold and dense ice Shelf Water from the shelf towards large depths. Comments are made on possible implications of this process for the large-scale deep-water circulation and for the interpretation of sediment cores.

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Haftorn, S., Mehlum, F., & Bech, C. (1988). Navigation to nest site in the snow petrel (Pagodroma nivea). The Condor, 90(2), 484–486. https://doi.org/10.2307/1368578

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Horner, R. A., Syvertsen, E. E., Thomas, D. P., & Lange, C. (1988). Proposed terminology and reporting units for sea ice algal assemblages. Polar Biology, 8(4), 249–253. https://doi.org/10.1007/BF00263173

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Huntford, R., & Hoff, T. (1988). Sydpolen 1910-1912. In Roald Amundsens oppdagelsesreiser i bilder (pp. 39–142, ill.). Grøndahl. https://doi.org/oai:nb.bibsys.no:998830791604702202 URN:NBN:no-nb_digibok_2013091638079

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Jakobsen, Ø., & Fiskeridirektoratet. (1988). Skjellressurser i Sydishavet: litteraturstudie (p. 29). Norges fiskerihøyskole. http://hdl.handle.net/11250/131092

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Koren, J. (1988). Journal over den Belgiske Sydhavs-Expedition 97-99. https://media.digitalarkivet.no/view/77494/59

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Kristoffersen, Y., & Aalerud, J. (1988). Aeromagnetic reconnaissance over the Riiser-Larsen Ice Shelf, east Antarctica. Polar Research, 6(1), 123–128. https://doi.org/10.3402/polar.v6i1.6852

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Mehlum, F., Gjessing, Y., Haftorn, S., & Bech, C. (1988). Census of breeding Antarctic petrels Thalassoica antarctica and physical features of the breeding colony at Svarthamaren, Dronning Maud Land, with notes on breeding snow petrels Pagodroma nivea and south polar skuas Catharacta maccormicki. Polar Research, 6(1), 1–9. https://doi.org/10.3402/polar.v6i1.6841

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Orheim, O. (1988). Antarctic icebergs: production, distribution and disintegration (abstract). Annals of Glaciology, 11, 205. https://doi.org/10.3189/S0260305500006649

A programme of systematic iceberg observations was initiated in 1981 by Norsk Polarinstitutt through the SCAR Working Group on Glaciology. Icebergs are recorded every 6 h and in five length groups: 10-50, 50-200, 200-500 and 500-1000 m, and those over 1000 m, which are described individually. Data on more than 100 000 icebergs are now on file at Norsk Polarinstitutt, and practically all ships travelling to and from Antarctica participate in the collection of data. This paper presents the first comprehensive analysis of the iceberg data. The quality of the data set is discussed, with consideration of potential errors in and limitations of the data, and various statistical evaluations. Representative distribution data are presented, and used to determine iceberg production, disintegration and mean residence times, and regional and total Antarctic calving rates. The incidence of large-scale calving in particular is evaluated, including the remarkably large break-offs in recent years. These exceed both the total annual accumulation on the Antarctic continent and the mean annual calving rate as determined from ship observations. The results show further: (1) that there are more than 200 000 icebergs south of the Antarctic Convergence, (2) that there are large regional differences in iceberg calving rates and iceberg sizes, and (3) that the calving rate from Antarctica is higher than that given in most previous estimates, which implies (4) that the mass balance of the Antarctic ice sheet is not positive as suggested by most recent estimates.

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Orheim, O., & Lucchitta, B. K. (1988). Numerical Analysis of Landsat Thematic Mapper Images of Antarctica: Surface Temperatures and Physical Properties. Annals of Glaciology, 11, 109–120. https://doi.org/10.3189/S026030550000642X

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[Smedvig, N. (1988). Belgica : den første overvintringen i Antarktis 1897-1899. [Nordsjøselskapet]. https://doi.org/oai:nb.bibsys.no:990702483464702202 URN:NBN:no-nb_digibok_2009103004042

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Zinsmeister, W. J. (1988). Early geological exploration of Seymour Island, Antarctica. In Geology and Paleontology of Seymour Island, Antarctic Peninsula (Vol. 169, pp. 1–16). Geological Society of America. https://doi.org/10.1130/MEM169-p1

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Barr, S. (1987). Norway’s polar territories. Aschehoug. https://doi.org/oai:nb.bibsys.no:998830116624702202 URN:NBN:no-nb_digibok_2014061805034

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Ciesielski, P., & Kristoffersen, Y. (1987). Palaeoceanography of the subantarctic South Atlantic. Nature, 328(6132), 671–672. https://doi.org/10.1038/328671a0

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Ellingsen, T. E., & Mohr, V. (1987). Biochemistry of the autolytic processes in Antarctic krill post mortem. Autoproteolysis. Biochemical Journal, 246(2), 295–305. https://doi.org/10.1042/bj2460295

1. Autoproteolysis post mortem was examined at 0 degree C by following the changes in the major classes of krill (Euphausia superba and Euphausia crystallorophias) proteins and by liberation of peptides and free amino acids, and was based on experiments conducted on board expedition vessels in the Antarctic. 2. Primarily salt-soluble proteins were broken down during the first week of incubation, whereas water-soluble and insoluble proteins were degraded to a much smaller extent. The enzymes responsible for the hydrolysis presumably originate primarily from the digestive apparatus of the krill. 3. In general, the individual amino acids were released at rates corresponding to their relative occurrence in the bulk protein of the krill. Alanine was liberated in larger amounts than would be expected from the composition of the krill protein, and was evidently formed also by reactions other than proteolysis. Glutamic acid, and certain amino acids which presumably occur with high frequency adjacent to glumatic acid residues in the krill protein, were liberated only to a limited extent, and accumulated in smaller peptides. 4. During proteolysis, arginine seemed to be converted to some degree into ornithine, and on prolonged incubation conversion of arginine and lysine into their corresponding decarboxylation products, agmatine and cadaverine, appeared to take place.

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Engelskjøn, T. (1987). Botany of Bouvetøya, South Atlantic Ocean. II. The terrestrial vegetation of Bouvetøya. Polar Research, 5(2), 129–163. https://doi.org/10.3402/polar.v5i2.6872

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Fridtjof, M., Claus, B., & Svein, H. (1987). Breeding ecology of the Antarctic petrel Thalassoica Antarctica in Mühlig-Hofmannfjella, Dronning Maud Land. Proceedings of the NIPR Symposium on Polar Biology, 1, 161–165. http://id.nii.ac.jp/1291/00005025

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