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.

Your search

Publication year

Between 1900 and 1999
- Between 1970 and 1979

Online resource

yes

Results 79 resources

Abstracts

Fevolden, S. E. (1979). Investigations on krill (Euphausiacea) sampled during the Norwegian Antarctic Research Expedition 1976–1977. Sarsia, 64(3), 189–198. https://doi.org/10.1080/00364827.1979.10411381

Krill was sampled in the Weddell Sea, farther south than ever before, and off Bouvet-öya. Five species were found: Euphausia superba, E. crystallorophias, E. frigida, E. triacantha, and Thysanoessa macrura. E. superba and E. crystallorophias were the most abundant species north and south of 74° S respectively. Length frequency analyses suggest that E. superba from the inner Weddell Sea takes three years to reach maturity. This population differed in several aspects from the populations farther north. E. crystallorophias and T. macrura were registered south to 77°45′ S, the southernmost localisation investigated. The material gives no clear evidence whether these species take one or two years to reach maturity. Their spawning activity seems to start earlier in the season than for E. superba. E. frigida and E. triacantha were only-found off Bouvetöya. Continuous echosounder recordings revealed that the total abundance of krill in the southern parts of the Weddell Sea was low, as was also the abundance on the route between the South Orkney Islands and Dronning Maud Land.

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Fryxell, G. A., & Hasle, G. R. (1979). The genus Thalassiosira: species with internal extensions of the strutted processes. Phycologia, 18(4), 378–393. https://doi.org/10.2216/i0031-8884-18-4-378.1

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Løvlie, R. (1979). Mesozoic palaeomagnetism in Vestfjella, Dronning Maud Land, East Antarctica. Geophysical Journal of the Royal Astronomical Society, 59(3), 529–537. https://doi.org/https://doi.org/10.1111/j.1365-246X.1979.tb02571.x

Thermal and alternating field demagnetization of oriented samples of Mesozoic lava flows (200–230 Myr) and dykes (154–172 Myr) collected from seven nunataks within the Vestfjella region, Dronning Maud Land, revealed stable directions of magnetization of normal and reverse polarity. Directional distributions of both polarities define tight groups along the same palaeomagnetic axis. Depending on whether the regional westward dip of the lava flows originated prior to, or after the intrusive igneous phase, two or one, respectively, palaeomagnetic pole(s) can be estimated. Both poles, however, are in general accord with previous Mesozoic poles from East Antarctica.

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Block, W., Young, S. R., Conradi-Larsen, E.-M., & Sømme, L. (1978). Cold tolerance of two Antarctic terrestrial arthropods. Experientia, 34(9), 1166–1167. https://doi.org/10.1007/BF01922934

Two Antarctic arthropods,Alaskozetes antarcticus (Acari) andCryptopygus antarcticus (Collembola) possess the ability to supercool to −30°C, but the realisation of this potential is dependent on starvation. The mite contains glycerol in a concentration of about 1% fresh weight.

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Børde, H., & Johansen, K. H. (1978). Eventyret Antarktis. Gyldendal. https://doi.org/oai:nb.bibsys.no:997810920784702202 URN:NBN:no-nb_digibok_2007062801052

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Furnes, H., & Løvlie, R. (1978). An eruptional model for recent lava flow on Bouvetøya, South Atlantic Ocean. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 103–108, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Furnes, H., & Mitchell, J. G. (1978). Age relationships of Mesozoic basalt lava and dykes in Vestfjella, Dronning Maud Land, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 45–68, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Gade, H. G. (1978). Melting of ice in sea water: a primitive model with application to the Antarctic ice shelf and ice bergs. Universitetet i Bergen. https://urn.nb.no/URN:NBN:no-nb_digibok_2017041048074

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Hjelle, A., Ohta, Y., & Winsnes, T. S. (1978). Stratigraphy and igneous petrology of Southern Heritage Range, Ellsworth Mountains, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 5–43, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

Sedimentary and magmatic rocks of Late Proterozoic to Late Paleozoic age, from the southern half of Ellsworth Mountains are described. Basic volcanic rocks, mainly agglomeratic, occur abundantly in the lower part of the succession, in the Minaret Group, and in the lower part of the Heritage Group, but are not recorded in the upper part of the Heritage Group. Due to this lithostratigraphic contrast a new classification is proposed: the Heritage Group including the Middle Horseshoe Formation and the Edson Hills Formation. A stratigraphic gap is evident above the Edson Hills Formation and a separate unit--the Dunbar Ridge Formation--is proposed. This formation is of Middle-Upper Cambrian age, with trilobite-bearing limestones. The structure is governed by a major anticline with a NW plunge in the north but almost horizontal in the south. Contrast of fold intensity and fold style below the youngest exposed unit, the Whiteout Conglomerate and a weathered surface above the Crashite Quartzite suggests a late Paleozoic deformation phase. Two phases of magmatism are distinguished. The pre-Middle Cambrian magmatism is dominantly K-alkalic and suggests the beginning of block subsidence at the early stage of a rift tectonics on a continental crust. The presumptive Late Paleozoic magmatism is N-alkalic and tholeiitic, and occurred after the main deformation; however the rocks were regionally metamorphosed in the actinolite-greenschist facies probably in late Paleozoic time. This magmatism is considered to represent an advanced stage of block tectonics. (Auth. mod.)

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Løvlie, R., & Furnes, H. (1978). Palaeomagnetism and morphology of lava(s) at Cape Meteor, Bouvetøya. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 93–101, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Orheim, O. (1978). Den norske Antarktis-ekspedisjonen 1976/77. Naturen, 102(6), 256. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2015071381095_001

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Orheim, O. (1978). Glaciological studies by Landsat imaginery of perimeter of Dronning Maud Land, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 69–80, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Polarinstitutt, N. (1978). Results from Norwegian Antarctic research 1974-1977 (Vol. 169). https://brage.npolar.no/npolar-xmlui/handle/11250/173570

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Repp, K. (1978). Snow accumulation and snow stratigraphy on Riiser-Larsenisen, Dronning Maud Land, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 81–92, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Sannes, T. B. (1978). Sel- og hvalfangstskuter. Sydpolskipet som aldri ble bygget. Med “Southern Cross” til det sjette kontinent. In Colin Archer skipene (pp. 62–67, 111–121). Bokhandlerforlaget. https://doi.org/oai:nb.bibsys.no:998121389294702202 URN:NBN:no-nb_digibok_2007061901017

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Sømme, L. (1978). Cold-Hardiness of Cryptopygus antarcticus (Collembola) from Bouvetøya. Oikos, 31(1), 94–97. https://doi.org/10.2307/3543388

Cryptopygus antarcticus Willem were extracted from samples of mosses collected at Bouvetøya during the Norwegian Antarctic Expedition in February 1977. The body length of the collembolans from these samples ranged from 225 to 1125 μm. The collembolans had average supercooling points between -24° and -26°C. Acclimation at -5°, 0° and 12°C for various time intervals had no significant effect on their ability to supercool. Glycerol was not found in specimens acclimated at -5° and 0°C. All specimens were killed by freezing at temperatures in the range of their supercooling points. Chill-coma temperatures of the collembolans were between -2° and -7°C.

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Vinje, T. E. (1978). Meteorological observations from Bouvetøya. In Bouvetøya, South Atlantic Ocean : results from the Norwegian Antarctic Research Expeditions 1976/77 and 1978/79 (Vol. 175, pp. 85–103, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Vinje, T. E. (1978). Weather and tide observations at Bouvetøya. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 109–117, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Børde, H. (1977). Norge i Antarktis. Samtiden: tidsskrift for politikk, litteratur og samfunnsspørsmål, 86(10), 577–593. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2014071481072_001 URN:NBN:no-nb_digitidsskrift_2014071481072_001

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Fevolden, S. E., & Sømme, L. (1977). Observations on birds and seals at Bouvetøya. In Norsk Polarinstitutt. Årbok 1976 (pp. 367–371). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172821

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