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 67 of 145

Abstracts

Østerhus, S., & Orheim, O. (1994). Oceanographic and glaciologic investigations through Jutulgryta, Fimbulisen in the 1991/92 season. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 21–28). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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Palm, H., Andersen, K., Klöser, H., & Plötz, J. (1994). Occurrence of Pseudoterranova decipiens (Nematoda) in fish from the Southeastern Weddell Sea (Antarctic). Polar Biology, 14(8), 539–544. https://doi.org/10.1007/BF00238223

Eleven fish species from the Weddell Sea (Antarctic) were examined for infestation with anisakid nematodes. Two species of the genus Contracaecum and the sealworm Pseudoterranova decipiens were isolated from the liver and the body cavity of fish affected. Only two specimens of P. decipiens (1.4%) partly invaded the belly flaps. The following fish species were infested by P. decipiens at the given prevalences: Cygnodraco mawsoni (74.4%), Trematomus scotti (23.2%), Pagetopsis maculatus (10.0%), Cryodraco antarcticus (7.1%), Trematomus lepidorhinus (3.0%), and Dolloidraco longedorsalis (2.7%). All of these, except Trematomus scotti, are new host records. Chaenodraco wilsoni, Chionodraco myersi, Gerlachea australis, Racovitzia glacialis and T. eulepidotus were not infested. The reasons for low prevalence and intensity of infestation are seen in the difficulties of P. decipiens in completing its benthic life cycle in the Weddell Sea environment, in the absence of shallow coastal waters due to the floating shelf-ice. Cygnodraco mawsoni is a crucial intermediate host, without which completion of the parasite life cycle might not be possible. In order to clarify the taxonomical position of Antarctic Pseudoterranova, morphological comparisons with specimens of P. decipiens from the German and Norwegian coast were made using scanning electron microscopy. Results revealed no differences; hence, all specimens studied belong to the same species P. decipiens.

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Røv, N., Lorentsen, S.-H., & Bangjord, G. (1994). Seabird studies at Svarthamaren, Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 9–20). Norsk Polarinstitutt.
Salvini, F., Della Maggiore, R., Fortunati, L., & Mazzarini, F. (1994). Rock mapping of glaciated areas by satellite image processing. Polar Research, 13(1), 23–33. https://doi.org/10.3402/polar.v13i1.6678

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Smith, R. I. L., & Øvstedal, D. O. (1994). Solorina Spongiosa in Antarctica: An Extremely Disjunct Bipolar Lichen. The Lichenologist, 26(2), 209–213. Cambridge Core. https://doi.org/10.1006/lich.1994.1017

The bipolar foliose lichen Solorina spongiosa (Sm.) Anzi is reported from James Ross Island, Antarctica, where it grows on moss. This is only the third known occurrence of this lichen from the Southern Hemisphere, the other localities being in Tierra del Fuego and New Zealand. Its morphology resembles that of the New Zealand population and arctic-alpine populations from the Northern Hemisphere, although there are some differences in apothecial and spore size. As elsewhere, it occupies base-rich habitats colonized by predominantly calcicolous mosses and lichens.

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Solheim, A. (1994). Proximal sub ice-shelf sedimentation Jutulgryta, East Antarctica. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 29–33). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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Tollefsen, I. (1994). Dronning Maud Land (V. Sand, Ed.). Mortensen. https://doi.org/oai:nb.bibsys.no:999429985614702202 URN:NBN:no-nb_digibok_2009042804042

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Vidas, D. (1994). The Antarctic Treaty system and Antarctic tourism: towards a legal regime? International Challenges, 14(2), 22–31.
Winther, J.-G. (1994). Spectral bi-directional reflectance of snow and glacier ice measured in Dronning Maud Land, Antarctica. Annals of Glaciology, 20, 1–5. https://doi.org/10.3189/1994AoG20-1-1-5

Visible and near-infrared spectral reflectances of snow and superimposed ice were measured in Dronning Maud Land, Antarctica, during the 1992-93 austral summer. Spectral-reflectance curves of both snow and superimposed ice remain high ( > 80%) in the visible region. A pronounced decrease in reflectance appears in the near-infrared, especially for superimposed ice. Superimposed ice with a 1 cm thick surface layer of ice-bound snow crystals had a considerably higher reflectance than superimposed ice containing only a few snow crystals. Furthermore, these data prove that snow and superimposed ice reflect solar radiation specularly and suggest that the anisotropy strengthens with increasing wavelengths. Integrated in-situ reflectances corresponding to Landsat TM bands 1-4 show that TM band 1 is least affected, whereas TM band 4 is most affected by anisotropy. Furthermore, the anisotropy increases with increasing off-nadir viewing angles up to an angle corresponding to 90°-θs (θs = solar elevation). For a 15° off-nadir sensor-observation angle, the average snow reflectance for TM bands 1--4 is about 10% higher than at nadir. Similarly, the apparent reflectance can be more than 50% higher than the nadir reflectance for larger observation angles. Consequently, if satellite-derived reflectances are going to be considered as absolute values, a topographic-correction model is needed to correct for the effects of anisotropy.

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Executive summary: International Antarctic Regime Project publication series 1993 (p. 10). (1993). Fridtjof Nansens institutt.
Amundsen, R., & Thylwe, H. (1993). Moje życie polarnika. Iskry.
Andersen, R., Sæther, B.-E., & Pedersen, H. C. (1993). Resource limitation in a long-lived seabird, the Antarctic petrel Thalassoica antarctica: a twining experiment. Fauna Norvegica. Serie C. Cinclus, Norwegian Journal of Ornithology, 16(1), 15–18.
Barr, S. (1993). Norwegian Antarctic whaling seen through the eye of the camera. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 177–189). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Barthelmess, K. (1993). A century of German interests in modern whaling, 1860s-1960s. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 121–138). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Basberg, B. L. (1993). Survival against all odds? Shore station whaling at South Georgia in the Pelagic. Era, 1925-1960. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 157–167). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Brekke, A. (1993). Norway in the Antarctic. Ministry of Foreign Affairs.
Bucher-Nurminen, K., & Ohta, Y. (1993). Granulites and garnet–cordierite gneisses from Dronning Maud Land, Antarctica. Journal of Metamorphic Geology, 11(5), 691–703. https://doi.org/https://doi.org/10.1111/j.1525-1314.1993.tb00181.x

The central sector of Mühlig-Hofmannfjellet (3°E/71°S) in western Dronning Maud Land (East Antarctic shield) is dominated by large intrusive bodies of predominantly orthopyroxene-bearing quartz syenites (charnockites). Metasedimentary rocks are rare; however, two distinct areas with banded gneiss–marble–quartzite sequences of sedimentary origin were found during the Norwegian Antarctic Research Expedition NARE 1989/90. Cordierite-bearing metapelitic gneisses from two different localities contain the characteristic mineral assemblage: cordierite + garnet + biotite + K-feldspar + plagioclase + quartz ± sillimanite ± spinel. Thermobarometry indicates equilibration conditions of about 650°C and 4 kbar. Associated orthopyroxene–garnet granulites, on the other hand, revealed pressures of about 8 kbar and temperatures of 750°C. The earlier granulite facies metamorphism is not well preserved in the cordierite gneisses as a result of excess K-feldspar combined with interaction with an H2O-rich fluid phase, probably released by the cooling intrusives. These two features allowed the original high-grade K-feldspar + garnet assemblages to recrystallize as cordierite–biotite–sillimanite gneisses, completely re-equilibrating them. Phase relationships indicate that the younger metamorphic event occurred in the presence of a fluid phase that varied in composition between the lithologies.

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Davis, B. W., & Herr, R. A. (1993). The legitimacy of the Convention on the Conservation of Antarctic Marine Living Resources (p. 20). Fridtjof Nansens institutt.
Ekra, S. I. S. (1993). Den farlige isen i Antarktis. Norges teknisk-naturvitenskapelige universitet SINTEF. https://gemini.no/2011/03/den-farlige-isen-i-antarktis/

All is i antarktiske havområder er flerårig under den antarktiske sommeren. Slik is er særlig sterk og hard og smelter ikke. I store bølger får de farlige stykkene stor fart. Treffer de en båt, skjer det med stor kraft.

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Headland, R. K. (1993). Geographical discoveries in Antarctica by the whaling industry. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 191–202). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Last update from database: 11/1/24, 3:10 AM (UTC)

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