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

Konvensjon om bevaring av marine levende ressurser i Antarktis = Convention on the Conservation of Antarctic Marine Living Resources. (1980). Lovdata. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2017101781154_001

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Borchgrevink, C. E. (1980). First on the Antarctic Continent: being an account of the British Antarctic Expedition 1898-1900. C. Hurst & Company; Australian National University Press. https://doi.org/oai:nb.bibsys.no:998222507724702202 URN:NBN:no-nb_digibok_2009020402003

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Fevolden, S. E. (1980). Krill off Bouvetøya and in the southern Weddell Sea with a description of larval stages of Euphausia crystallorophias. Sarsia, 65(2), 149–162. https://doi.org/10.1080/00364827.1980.10431481

In the austral summer 1978/79 samples of krill were taken off Bouvetøya and in the southern Weddell Sea. Off Bouvetøya Euphausia superba Dana was the dominant species, but the population pattern indicates that the individuals found there were expatriates from other areas. For the first time larvae of E. superba were found in significant amounts in the southern Weddell Sea. Except from shallow water and the most southern position, they were equal in abundance to the larvae of E. crystallorophias Holt & Tattersall. Larval stages of the latter are described as is the successive spawning that takes place among the three species of krill found in the southern Weddell Sea.

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Foldvik, A., Gammelsrød, T., & Gjessing, Y. (1980). Flow Around Icebergs. Annals of Glaciology, 1, 67–70. https://doi.org/10.3189/S0260305500016992

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Huntford, R., & Christensen, J. (1980). Scott og Amundsen. Aschehoug. https://doi.org/oai:nb.bibsys.no:998011517164702202 URN:NBN:no-nb_digibok_2013052908070

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Morris, E. (Ed.). (1980). Bestemt på å lykkes: Amundsen på Sydpolen. In De Fryktløse : oppdagelsesferdene som endret vår verden (pp. 288–297). Det Beste. https://doi.org/oai:nb.bibsys.no:998221640864702202 URN:NBN:no-nb_digibok_2012091238005

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Pedersen, A. F. (1980). Hvalfangst i Sørishavet. In Kampen på havet : en krigsseilers beretning (pp. 7–29). Aschehoug. https://doi.org/oai:nb.bibsys.no:998011677284702202 URN:NBN:no-nb_digibok_2007062701077

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Sømme, L. (1980). Terrestrial arthropods from Vestfjella, Dronning Maud Land (Acari, Collembola), with notes on their taxonomy. Insect Systematics & Evolution, 11(1), 61–64. https://doi.org/https://doi.org/10.1163/187631280X00374

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Vinje, T. E. (1980). Some satellite tracked iceberg drifts in the Antarctic. Annals of Glaciology, 1, 83–87. https://doi.org/10.3189/S026030550001702X

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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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