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

Prestvik, T., & Duncan, R. A. (1991). The geology and age of Peter I Øy, Antarctica. Polar Research, 9(1), 89–98. https://doi.org/10.3402/polar.v9i1.6781

The island Peter I Oy is located in the Bellinghausen Sea 400 km off the coast of West Antarctica. It is situated at the transition between oceanic and contintental crust close to a former transform fault, the Tharp fracture zone. The island is completely volcanic, consisting of predominantly alkali basalt and hawaiite and some more evolved rocks. Sampling done by the Aurora expedition in 1987 has made dating and detailed petrological studies possible. The island appears to be much younger (< 0.5 Ma) than previously believed. However, the volcanic activity responsible for this oceanic island may have lasted for 10-20 Ma. Volcanic activity at the island thus took place at the same time as post-subduction rift-related volcanism took place along the Antarctic Peninsula and in Marie Byrd Land. However, the petrologic data indicate that this may be coincidental and that the Peter I Oy activity is independent and related to transtensional rifting along the Tharp fracture zone.

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Ringstad, J. E. (1991). Hvalfangernes mat til hverdag og fest. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 4, 31–32. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481070_001 URN:NBN:no-nb_digitidsskrift_2018121481070_001

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Sakshaug, E., & Slagstad, D. (1991). Light and productivity of phytoplankton in polar marine ecosystems: a physiological view. Polar Research, 10(1), 69–86. https://doi.org/10.3402/polar.v10i1.6729

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Sakshaug, E., Slagstad, D., & Holm-Hansen, O. (1991). Factors controlling the development of phytoplankton blooms in the Antarctic Ocean — a mathematical model. Marine Chemistry, 35(1), 259–271. https://doi.org/https://doi.org/10.1016/S0304-4203(09)90021-4

A mathematical model describing the development of phytoplankton blooms as a function of the depth of the wind-mixed layer, spectral distribution of light, passage of atmospheric low-pressure systems, size of the initial phytoplankton stock and loss rates is presented. Model runs represent shade-adapted, large-celled, bloom-forming diatoms. Periodic deep mixing caused by strong winds may severely retard the development of blooms and frequently abort them before macronutrients are completely exhausted. Moderate depths of mixing (40-50 m) in combination with a moderately large total loss rate (about 0.01 3 h-1) can prevent blooms from developing during the brightest time of the year. Complete exhaustion of macronutrients in the upper waters is likely only if the wind-mixed layer is less than 10 m deep, i.e. in very sheltered waters, and also in the marginal ice zone when ice is melting. We do not exclude the possibility of control of phytoplankton biomass by iron in ice-free, deep-sea parts of the Antarctic Ocean, but the implied enhancement of export production through addition of iron might be restricted because of limitation by light, i.e. vertical mixing.

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Smith, R. I. L., & Øvstedal, D. O. (1991). The lichen genus Stereocaulon in Antarctica and South Georgia. Polar Biology, 11(2), 91–102. https://doi.org/10.1007/BF00234271

Six species of Stereocaulon and one unnamed taxon (close to S. glabrum) are reported from South Georgia, the maritime Antarctic islands and Antarctic Peninsula. S. caespitosum is new to the western sub-Antarctic. Variations in morphology and secondary chemistry are provided, and the ecology and geographical distribution in the sub-Antarctic and Antarctic biomes are given for each taxon.

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Sæther, B.-E. (1991). Antarktispetrellen: på grensen av det mulige. Naturen, 115(6), 249–253. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2015071381019_001

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Ursin, H., Bergan, T., Collet, J., Endresen, I. M., Lugg, D., Maki, P., Matre, R., Molvær, O. I., Müller, H. K., Olff, M., Pettersen, R. C., Sandal, G. M., Værnes, R. J., & Warncke, M. (1991). Psychobiological Studies of Individuals in Small, Isolated Groups in the Antarctic and in Space Analogues. Environment and Behavior, 23(6), 766–781. https://doi.org/10.1177/0013916591236007

Mental and physical health are both at risk under conditions of prolonged remoteness from home and removal from normal social support networks. This article examines relevant data from small groups isolated in (a) Antarctic summer stations, (b) a Transantarctic traverse expedition, and (c) a spacecraft simulator capsule.

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Wexelsen, E. (1991). Sandefjord - et naturlig polarforskningssenter. Utkikksposten (Sandefjord) : kontaktorgan for Sandefjordmuseene, 3, 30–32. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2018121481072_001 URN:NBN:no-nb_digitidsskrift_2018121481072_001

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Yen, J. (1991). Predatory feeding behavior of an Antarctic marine copepod, Euchaeta antarctica. Polar Research, 10(2), 433–442. https://doi.org/10.3402/polar.v10i2.6757

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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://hdl.handle.net/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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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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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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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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Hunt Jr, G. L. (1990). The pelagic distribution of marine birds in a heterogeneous environment. Polar Research, 8(1), 43–54. https://doi.org/10.3402/polar.v8i1.6802

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Hunt Jr, G. L. (1990). The pelagic distribution of marine birds in a heterogeneous environment. Polar Research, 8(1), 43–54. https://doi.org/10.3402/polar.v8i1.6802

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Imbert, B. C., & Hem, A. (1990). I hjertet av Antarktis; Norge i Antarktis. In Polarforskningens pionerer (Vol. 3, pp. 79–107, 129–134). Schibsted. https://doi.org/oai:nb.bibsys.no:999010468684702202 URN:NBN:no-nb_digibok_2008061004006

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Kennett, M. (1990). Radio-echo investigations in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 75–79). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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