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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Publication year

Between 1900 and 1999
- Between 1990 and 1999
  - 1990

Results 63 resources

Abstracts

Amundsen, R., & Nakada, O. (1990). Nankyoku ten. Dorufin Press.
Andersen, R. T. (1990). Negtiationg a new regime: how CRAMRA came into existence. International Challenges, 10(1), 21–23.
Barnes, J. N. (1990). Protection of the environment in Antarctica: are present regimes sufficient? International Challenges, 10(1), 52–55.
Barr, S. (1990). Antarctica’s cultural heritage: can ICOMOS help? Icomos Information, 1990(2), 30–35.
Beck, P. J. (1990). The resource conventions implemented: the consequences for the sovereignty issue. International Challenges, 10(1), 56–60.
Beddington, J. R., Basson, M., & Gulland, J. A. (1990). The practical implications of the eco-system approach in CCAMLR. International Challenges, 10(1), 17–20.
Bos, A. (1990). Consultative status under the Antarctic Treaty: redefining the criteria? International Challenges, 10(1), 73–77.
Brown, A. D. (1990). The design of CRAMRA: how appropriate for the protection of the environment? International Challenges, 10(1), 24–26.
Bucher-Nurminen, K., Ohta, Y., Austrheim, H., & Dallmann, W. K. (1990). Geological observations in Gjelsvikfjella and Mühling-Hofmannfjella. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 91–100). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Dallmann, W. K., Austrheim, H., Bucher-Nurminen, K., & Ohta, Y. (1990). Geology around the Norwegian Antarctic station “Troll”, Jutulsessen, Dronning Maud Land (Vol. 111). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173018

During the Norwegian Antarctic Research Expedition 1989/90, a pennanent, unmanned research station was raised in Jutulsessen, Gjelsvikfjella, western Dronning Maud Land. The present report is a description of the geology of the area accessable from the station. Exposures of rocks in this part of Dronning Maud Land are restricted to a coastal mountain chain at c. 200-250 km distance from the ice shelf edge at elevations between 1000 and 3000 m. Quaternary deposits are particularly restricted to the inner parts of the Jutulsessen glaeier cirques. Deposits are till and talus which locally are admixing at slope angles of c. 25°. Moraines are poorly developed. Patterned ground ('stone pits') are common at slope angles below c. 15°. Recently active phenomena of special interest are ice-margin meltwater lakes with pingo-like 'blisters " the deep frost-shattering all over the mountain walls and hoIes in rock surfaces as a result of wind activity with grinding particles. The bedrock belongs to the East Antarctic craton. The area under consideration (western Miihlig-Hofmannfjella and Gjelsvikfjella) consists of high-grade metamorphic rocks and fonns one of the world's best exposed granulite terranes. Orthogneisses and minor metasediments have been intruded by a series of charnockites, partly altered to granulites (the 'Svarthamaren charnockite complex'), and a sequence of dyke rocks. Migmatization has affected large parts of the gneisses. Both gneisses and granulites/charnockites show abundant evidence of transition from granulite to amphibolite facies and vice versa, and the important role of fluid-rock interactions leading to these processes can be studied. The gneisses at Jutulsessen show a complex defonnation history. They are thought to be derived from granitic intrusions, though minor amounts of high-grade metamorphic, metapelitic gneisses may represent their original host rocks. Early tectonism (c. 1000-1200 m.y.) produced gneissosity, compositional banding and a leucosome phase under high-grade metamorphic conditions. This was followed by multiple and complex intrusive activity, partial migmatization and a tectonic overprint with abundant shear defonnation under amphibolite-facies conditions (c. 450-500 m.y.).

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Dumas, R. (1990). The Antarctic in world politics. International Challenges, 10(1), 4–8.
Eiken, T., Luktvasslimo, B. Å., & Lytskjold, B. (1990). Geodetic measurements in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 101–112). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Falk, R. (1990). Antarctica Treaty System: are there viable alternatives? International Challenges, 10(1), 91–93.
Foldvik, A., Gammelsrød, T., Nordlund, N., & Nytun, K. (1990). Observations of ice shelf water at the southern Weddel sea shelf break. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 125–130). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Foldvik, A., Middleton, J. H., & Foster, T. D. (1990). The tides of the southern Weddell Sea. Deep Sea Research Part A. Oceanographic Research Papers, 37(8), 1345–1362. https://doi.org/https://doi.org/10.1016/0198-0149(90)90047-Y

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Gulliksen, B., Lønne, O. J., & Hellum, C. (1990). Marine biological studies in the Weddel sea and north of Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 131–138). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Haron, M. (1990). The ability of the Antarctic Treaty System to adapt to external challenges. International Challenges, 10(1), 64–67.
Harris, S. (1990). The influence of the United Nations on the Antarctic system: a source of erosion or cohesion? International Challenges, 10(1), 68–72.
Heap, J. A. (1990). Has CCAMLR worked? management policies and ecological needs. International Challenges, 10(1), 13–16.
Hewes, C. D., Sakshaug, E., Reid, F. M. H., & Holm-Hansen, O. (1990). Microbial autotrophic and heterotrophic eucaryotes in Antarctic waters: relationships between biomass and chlorophyll, adenosine triphosphate and particulate organic carbon. Marine Ecology Progress Series, 63(1), 27–35. http://www.jstor.org/stable/24842265

Microscopical examination of near-surface eucaryotic microbial populations in circumcontinental waters of Antarctica indicated that nanoplankton (<20 μm diameter) dominated in regions with low chlorophyll concentrations (< 1 μg l⁻¹). About 30 % of the mean nanoplankton carbon consisted of heterotrophic flagellates. Heterotrophic microplankton carbon (> 20 μm diameter) was generally less significant. The variation in phytoplankton biomass was the result primarily of changes in cell density of pennate diatoms in the East Wind Drift, and of centric diatoms in the Weddell Sea and the Scotia Ridge region. Autotrophic and heterotrophic carbon as determined by microscopical analysis were compared with data for total particulate carbon, chlorophyll a, and adenosine triphosphate. Estimates for the C:chl ratio of autotrophs increased with decreasing concentrations of chlorophyll a, with mean values of 46 in bloom waters and 144 in 'blue water'. A C:ATP ratio for heterotrophic nanoplankton was estimated to be about 100, while that for heterotrophic microplankton may be lower. Algorithms, incorporating concentrations of chlorophyll a and ATP, are described which allow estimates of autotrophic and heterotrophic microbial biomass.

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Last update from database: 3/1/25, 3:17 AM (UTC)