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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Full bibliography 2,884 resources

Page 76 of 145

Abstracts

Ursin, H., Collet, J., & Etienne, J. L. (1990). An Antarctic crossing as an analogue for long-term manned spaceflight. ESA Bulletin, 64, 44–49.

The long-duration space missions planned for the end of this century will involve both physiological and psychological problems for the crew who will fly them. If Europe is to achieve autonomy in space, it must increase its expertise in these associated disciplines. One means of acquiring relevant experience is to study human behaviour in environments that are similar from a psychological viewpoint. A planned crossing of the Antarctic by a six-man international team therefore offered ESA a unique opportunity to observe the psychological problems that can occur during an international expedition involving prolonged isolation in a hostile environment.
Wexelsen, E. (1990). På hvalfangst med blyant og farvestifter. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 2, 20–21. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481060_001 URN:NBN:no-nb_digitidsskrift_2018121481060_001

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Wexelsen, E. (1990). Pierce’s kastebørse - et “Reodor Felgen” -patent med lang levetid. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 2, 10–11. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481060_001 URN:NBN:no-nb_digitidsskrift_2018121481060_001

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Winther, J.-G. (1990). Glaciological and meteorological measurements in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 81–86). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Wolfrum, R. (1990). The unfinished task: CRAMRA and the question of liability. International Challenges, 10(1), 27–31.
Aarset, A. V., & Torres, J. J. (1989). Cold resistance and metabolic responses to salinity variations in the amphipod Eusirus antarcticus and the krill Euphausia superba. Polar Biology, 9(8), 491–497. https://doi.org/10.1007/BF00261032

The krill Euphausia superba, unlike the amphipod, Eusirus antarcticus, tolerates being frozen into solid sea-ice at temperatures down to about-4°C. Cooled in air, the amphipod and the krill freeze and will die at temperatures of-11° and-9°C respectively, representing the supercooling points of the animals. The krill is an osmoconformer in the salinity range of 25 to 45 ppt, while the amphipod conforms in the salinity range of 26 to 40 ppt. The animals thereby lower the melting point of their body fluids in the vicinity of the freezing sea ice, preventing internal ice formation at low temperatures. The mean oxygen consumption rates, at raised and lowered salinities, were not significantly different from rates obtained in normal (35 ppt.) seawater, indicating that salinity has little effect on the metabolism of either species.

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Albregtsen, F. (1989). Fractal Texture Signature estimated by Multiscale LIT-SNN and MAX-MIN Operators on LANDSAT-5 MSS Images of the Antarctic. In M. Pietikainen & J. Röning (Eds.), Proceedings of the 6th Scandinavian Conference on Image Analysis: Oulu, June 19-22, 1989 (Vol. 2, pp. 995–1002). Pattern Recognition Society of Finland.
Amlien, J. (1989). Satellittkartlegging ved Norsk Polarinstitutt. Kart og plan, 49(6), 519–522. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2013061382042_001 URN:NBN:no-nb_digitidsskrift_2013061382042_001

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Barr, S. (1989). Kulturminnevern i Antarktis: noe for ICOMOS? Icomos nytt, 1989(3), 5–10.
Denton, G. H., Bockheim, J. G., Wilson, S. C., Leide, J. E., & Andersen, B. G. (1989). Late Quaternary ice-surface fluctuations of Beardmore Glacier, Transantarctic Mountains. Quaternary Research, 31(2), 183–209. https://doi.org/https://doi.org/10.1016/0033-5894(89)90005-7

Former longitudinal profiles of Beardmore Glacier, an outlet through the Transantarctic Mountains, constrain polar plateau elevations near the center of Antarctica and ice-shelf grouding in the southern Ross Embayment. Three gravel drift sheets of late Quaternary age occur alongside Beardmore Glacier. Plunket drift, the youngest, is parallel to and 7–30 m above the present ice surface. The upper limit of Beardmore drift, intermediate in age, is within 35–40 m of the present ice surface near the polar plateau but about 1100 m above the present ice surface near the glacier mouth. The upper limit of Meyer drift, the oldest, is parallel to and 30–50 m above Beardmore drift. From correlation with numerically dated drifts farther north, we assign an early Holocene age to Plunket drift, a late Wisconsin age to Beardmore drift, and an age of marine isotope Stage 6 to Meyer drift. By our age model, Beardmore Glacier was close to current elevations in its upper reaches and thickened considerably in its middle and lower reaches during the last two global glaciations represented by Beardmore and Meyer drifts. Most likely, grounded ice in the southern Ross Embayment caused such thickening of Beardmore Glacier almost to the polar plateau. A concomitant decline in precipitation is implied by ice-cap retreat on the nearby Dominion Range and is consistent with little change of upper Beardmore Glacier. Ice-shelf grounding most likely resulted from lowered sea level and/or basal melting. Lower than present precipitation was probably caused by colder air temperatures and more-distant open water. The Plunket profile records Holocene ice-surface lowering from increased surface ablation, decreased ice flow, or grounding-line recession.

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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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Gjelsvik, T. (1989). Place-names of Heimefrontfjella and Lingetoppane, Dronning Maud Land, Antarctica (Vol. 54). http://hdl.handle.net/11250/173326

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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). Forholdet mellom vitenskap og politikk i internasjonal ressursforvaltning: det internasjonale samarbeid om forvaltning av de levende marine ressurser i Antarktis (p. 196). Fridtjof Nansens institutt.
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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