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

Fevolden, S. E., & Schneppenheim, R. (1989). Genetic homogeneity of krill (Euphausia superba Dana) in the Southern Ocean. Polar Biology, 9(8), 533–539. https://doi.org/10.1007/BF00261038

Development of a comprehensive picture of the genetic population structure of the Antarctic krill (Euphausia superba) has been hampered by a lack of genetic data from two major areas of the species' distribution, the Bellingshausen Sea and the Ross Sea. Evidence from earlier studies of a discrete “Bellingshausen Sea” population was based on anomalous allele frequencies in two sample sets that were collected near the west coast of the Antarctic Peninsula rather than in the Bellingshausen Sea proper. In this paper we describe the first biochemical genetic data obtained on krill from the central Bellingshausen Sea and from the Ross Sea. Analyses of eight polymorphic loci in samples from these two areas have failed to provide any evidence of population structuring within the Pacific sector of the Southern Ocean, and have indicated that Pacific sector krill cannot be genetically discriminated from Atlantic sector krill or Indian Ocean sector krill. These findings further support the hypothesis of a single circumpolar breeding population of Antarctic krill.

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Gjessing, Y. (1989). Excess and deficit of sulfate in polar snow. Atmospheric Environment (1967), 23(1), 155–160. https://doi.org/https://doi.org/10.1016/0004-6981(89)90108-X

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Gjessing, Y., & Øvstedal, D. O. (1989). Microclimates and water budget of algae, lichens and a moss on some nunataks in Queen Maud Land. International Journal of Biometeorology, 33(4), 272–281. https://doi.org/10.1007/BF01051089

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Holm-Hansen, O., Mitchell, B. G., Hewes, C. D., & Karl, D. M. (1989). Phytoplankton blooms in the vicinity of palmer station, Antarctica. Polar Biology, 10(1), 49–57. https://doi.org/10.1007/BF00238290

Fifteen oceanographic stations were occupied in the vicinity of Anvers Island, Antarctica, in January of 1985 and 1987. All stations showed high phytoplankton biomass (4.0 to 30 μg chl-a/liter) which was either uniformly distributed in the upper mixed layer or showed a pronounced sub-surface maximum at 4–5 m depth. As phosphate was less than 0.02 μm and nitrate about 2.0 μm in surface waters, it appears that nutrient limitation of phytoplankton growth may be of importance during such blooms. This view is supported by chemical measurements of the particulate material which showed high chl-a/ATP ratios (about 7.7), as well as high POC/ATP ratios (about 700). Microscopical analysis revealed a dominance of large-celled diatoms and the near absence of heterotrophic protozoans. Size fractionation studies showed that the nanoplankton accounted for only 28% of the total phytoplankton biomass. When phytoplankton biomass reaches the levels found at these stations, it appears that the cells are light-limited and hence dark-adapted, which results in the high chl-a/ATP ratios and the low assimilation values (0.49–1.64) obtained in our studies. Under such conditions greater than 50% of the total phytoplankton biomass is found below the 1% light level.

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Indreeide, T. V. (1989). The relationship between science and politics in international management of marine living resources: the case of CCAMLR. International Challenges, 9(3), 27–32.
Lien, R., Solheim, A., Elverhøi, A., & Rokoengen, K. (1989). Iceberg scouring and sea bed morphology on the eastern Weddell Sea shelf, Antarctica. Polar Research, 7(1), 43–57. https://doi.org/10.3402/polar.v7i1.6829

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Løvlie, R., & Mitchell, J. (1989). Anomalous palaeomagnetic directions in a Mesozoic basaltic dyke; arguments for fault-induced remagnetization. Physics of the Earth and Planetary Interiors, 58(2), 239–248. https://doi.org/https://doi.org/10.1016/0031-9201(89)90057-5

Anomalously steep palaeomagnetic directions from the central part of an ∼ 5 m wide basaltic dyke from Fossilryggen, East Antarctica, suggest a Recent to late Tertiary age for its remanent magnetization, in conflict with KAr isotope ages of 162 ± 4 and 217 ± 3 Ma obtained from the central and slickenside margins respectively. Three neighbouring basaltic intrusions carry stable magnetizations whose directions (mean D, 23°; mean I, −40° and pole position, 38°N, 40°E) accord with previously obtained Mesozoic results from lava flows in the Vestfjella basalt province, East Antarctica. Rock magnetic properties do not discriminate between the different dykes, and it is proposed that the anomalous directions represent spot-readings of the geomagnetic field which arise from complete remagnetization during a period of faulting in Recent to late Tertiary times.

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Lundqvist, J. (1989). Former extension of the East Antarctic Ice Sheet. Polar Research, 7(2), 109–117. https://doi.org/10.3402/polar.v7i2.6835

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Nilsen, T. L., & Thowsen, A. (1989). Hjelpekrysser kaprer norske hvalfangere. Sjøfartshistorisk årbok : Norwegian yearbook of maritime history, 1989, 147. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2020042181736_001 URN:NBN:no-nb_digitidsskrift_2020042181736_001

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Orheim, O. (1989). A hundred years of Norwegian exploration of the polar regions. Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 43(3), 123–127. https://doi.org/10.1080/00291958908552229

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Sakshaug, E., & Skjoldal, H. R. (1989). Life at the Ice Edge. Ambio, 18(1), 60–67. http://www.jstor.org/stable/4313526

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Barnes, P. W., & Lien, R. (1988). Icebergs rework shelf sediments to 500 m off Antarctica. Geology, 16(12), 1130–1133. https://doi.org/10.1130/0091-7613(1988)016<1130:IRSSTM>2.3.CO;2

Icebergs and sea ice rework the sediments of high-latitude shelves, producing modern diamicts (ice-keel turbates) unrelated to glacial proximity. Off Antarctica, sidescan sonar data indicate the presence of ice-gouge features formed by the physical interaction between ice keels and the sea bed. These are recognized as incisions a few metres deep and tens of metres wide, in water depths up to 500 m. On the submarine bank tops and slopes off Wilkes Land and in the Weddell Sea, subcircular depressions 30 to 150 m in diameter, a washboard pattern, and hummocky bed features also represent iceberg-resting sites. The freshness of sea-bed morphology, nearby Holocene sediment ponding, and active hydraulic sedimentary processes indicate that the sea floor is being reworked by iceberg keels. Tabular iceberg drafts in excess of 330 m have been measured, and modeling studies suggest that nontabular iceberg drafts of 500 m are possible. We conclude that a modern ice-keel turbate deposit in the form of a poorly stratified diamicton is probably widespread on that part (54%) of the Antarctic shelf less than 500 m deep.

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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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Danning, P. (1988). I fotsporene til Robert Falcon Scott. Været: populærvitenskapelig tidsskrift, 12(2), 59–61.
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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Haftorn, S., Mehlum, F., & Bech, C. (1988). Size variation in the snow petrel Pagodroma nivea. Notornis, 35(2), 109–116.
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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