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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Between 1900 and 1999
- Between 1980 and 1989
  - 1982

Results 36 resources

Abstracts

Basberg, B. L. (1982). Technological change in the Norwegian whaling industry: A case-study in the use of patent-statistics as a technology indicator. Research Policy, 11(3), 163–171. https://doi.org/https://doi.org/10.1016/0048-7333(82)90017-8

This paper presents an example of the use of patent statistics as a technology indicator in one industry. The first part deals with the problem of interpretation. Through examination of several other partial technology indicators, it is concluded that at least in this industry, patent statistics provide a reliable indicator, not only for the timing of inventions, but for the timing of innovations and diffusion as well. The reason is that the intervals between the stages in the innovation process are very short. This contradicts evidence from many other industries, and it is therefore emphasized that generalizations are unwarranted. The second part of this paper deals with the possible causes of technological change in Norwegian whaling. The methodology is inspired by J. Schmookler's work. Thus, the patents are correlated with other indicators of economic development in the industry. But while Schmookler's view is that the patent activity is determined by social demand and economic growth, the conclusions for the Norwegian whaling industry point in the opposite direction: the technological transformation that took place during the 1920s and early 1930s was forced upon the firms in their efforts to cut costs, which was achieved by rationalizing production and catching methods in line with a downward price trend for whale oil.

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Block, W., & Sømme, L. (1982). Cold Hardiness of Terrestrial Mites at Signy Island, Maritime Antarctic. Oikos, 38(2), 157–167. https://doi.org/10.2307/3544015

The cold hardiness of four species was studied in respect of supercooling ability, cryoprotective substances, chill-coma temperatures and survival under anaerobiosis. The effects of low temperature acclimation and starvation on cold hardiness were examined experimentally. (2) Mean supercooling points of field animals ranged from -6.1° to -28.8°C during Jan-Mar 1980. In Nanorchestes antarcticus (Strandtmann) and Alaskozetes antarcticus (Michael), a bimodal distribution of individual supercooling points occurred with the low group (LG) consisting of animals without gut nucleators. In Stereotydeus villosus (Trouessart) and Gamasellus racovitzai (Trouessart) only a high group (HG) was present in the supercooling-point distributions. (3) In all species, except the predatory G. racovitzai, starvation combined with low temperature exposure for various time periods lowered the mean supercooling point. This was associated with increased concentrations of glycerol in the body fluid. Glucose, ribitol and mannitol together with straight chain hydrocarbons were also detected in the extracts by GLC techniques. (4) Chill-coma temperatures varied from -4.5° to -8.0°C. (5) Under anoxia at 0°C, survival of A. antarcticus was greater than that of G. racovitzai, with the later nymphal stages being slightly more resistant than adults.

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Devig, T. N. (1982). Fagbevegelsen og hvalfangerne 1920-1935. Universitetet i Oslo.
Devig, T. N. (1982). Hvalbåten gjennom 100 år. Vestfoldminne, 1982, 42–51. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2019012581218_001 URN:NBN:no-nb_digitidsskrift_2019012581218_001

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Egeland, K. (1982). Norge i polarområdene. Leif Holtedahls forl. https://doi.org/oai:nb.bibsys.no:998421032284702202 URN:NBN:no-nb_digibok_2012052505083

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Ellingsen, T. E., & Mohr, V. (1982). Lipids in Antarctic krill : composition and post mortem changes (Vol. 57).
Ellingsen, T. E., & Norges tekniske høgskole Institutt for teknisk, biokjemi. (1982). Biokjemiske studier over antarktisk krill [Institutt for teknisk biokjemi]. https://www.nb.no/items/URN:NBN:no-nb_digibok_2015062508118

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Fossum, B. A., Maisey, G. H., & Torsen, H. O. (1982). Marine geophysical research in the Weddell Sea during the Norwegian Antarctic research expedition of 1976-77. In Craddock, Campbell (Ed.), Antarctic geoscience : Symposium on Antarctic Geology and Geophysics, Madison, Wisconsin, U.S.A., August 22-27, 1977: Vol. Series B-Number 4 (pp. 397–405). The University of Wisconsin Press Madison.
Furnes, H., Neumann, E.-R., & Sundvoll, B. (1982). Petrology and geochemistry of Jurassic basalt dykes from Vestfjella, Dronning Maud Land, Antarctica. Lithos, 15(4), 295–304. https://doi.org/https://doi.org/10.1016/0024-4937(82)90020-2

Mineral and whole rocks analyses of 12 Jurassic basalt dykes from Vestfjella, Dronning Maud Land, Antarctica, are presented, and their genesis discussed. On the basis of major oxides and norms the basalts may be classified as olivine and quartz tholeiites. Plotted in the Plag Cpx (Opx + 4Q) and Ol Plag Q projections, the compositions are most compatible with fractional crystallization of olivine, clinopyroxene and plagioclase from a basalt liquid at very low pressure. The ratios between strongly incompatible elements such as Rb, Cs, Zr, Hf, Ta and Th vary considerably, and petrographic mixing calculations give poor fits with respect to Rb, Cs, Ta, Th and light REE. Initial 87Sr/86 Sr ratios range between 0.70347 and 0.70687, and show no correlation with Rb/Sr or any other SIE ratios. The trace element and Sr isotope data thus do not suggest any simple cogenetic petrogenetic model. It is concluded that the basalt melts most plausibly have been contaminated by, or mixed with anatectic melts of crustal material, rather than reflecting mantle heterogeneity.

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Greve, T. (1982). Antarktis. In Australia, Oceania og Antarktis (pp. 445–497). Cappelen. https://doi.org/oai:nb.bibsys.no:998320273914702202 URN:NBN:no-nb_digibok_2008060904047

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Haftorn, S., & Voisin, J.-F. (1982). The Southern giant petrel Macronectes giganteus (Gmelin) on Bouvet Island. Fauna Norvegica. Serie C. Cinclus, Norwegian Journal of Ornithology, 5([1]), 47–48.
Haugland, K. (1982). Seismic reconnaissance survey in the Weddell Sea. In Craddock, Campbell (Ed.), Antarctic geoscience: Vol. Series B-Number 4 (pp. 405–413). The University of Wisconsin Press Madison.
Heintz, N. (1982). Nye fossile virveldyr fra Antarktis. Naturen, 106(5/6), 166. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2015071381014_001

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Hinz, K., & Krause, W. (1982). The Continental Margin of Queen Maud Land/Antarctica: Seismic Sequences, Structural Elements and Geological Development. Geologisches Jahrbuch. Reihe E, Geophysik, 23, 14–41.
Hjelle, Audun, Ohta, Yoshihide, & Winsnes, Thore S. (1982). Geology and petrology of the Southern Heritage Range, Ellsworth Mountains. In Craddock, Campbell (Ed.), Antarctic geoscience: Vol. Series B-Number 4 (pp. 599–608). The University of Wisconsin Press.
Ingstad, H. (1982). Carsten Borchgrevink: lederen for den første overvintring i Antarktis. Polarboken, 1981/82, 44–50.
Jacobsen, A. R. (1982). Eventyret Anders Jahre. Oktober. https://doi.org/oai:nb.bibsys.no:998320987794702202 URN:NBN:no-nb_digibok_2013092407005

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Kristensen, M., Squire, V. A., & Moore, S. C. (1982). Tabular icebergs in ocean waves. Nature, 297(5868), 669–671. https://doi.org/10.1038/297669a0

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Kristoffersen, Y., & Bungum, H. (1982). A microearthquake survey of Bouvet Island, South Atlantic. Tectonophysics, 81(1), T1–T5. https://doi.org/https://doi.org/10.1016/0040-1951(82)90111-1

A microearthquake survey carried out during the 1978–1979 Norwegian Antarctic Research Expedition indicates that only minor seismic activity is associated with the Bouvet volcano.

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Norheim, G., Sømme, L., & Holt, G. (1982). Mercury and persistent chlorinated hydrocarbons in antarctic birds from bouvetøya and dronning maud land. Environmental Pollution Series A, Ecological and Biological, 28(3), 233–240. https://doi.org/https://doi.org/10.1016/0143-1471(82)90079-4

The concentrations of DDE, PCB, hexachlorobenzene (HCB) and mercury were determined in samples from chinstrap penguin Pygoscelis antarctica, macaroni penguin Eudyptes chrysolophus, snow petrel Pagodroma nivea, Cape pigeon Daption capense, southern fulmar Fulmarus glacialoides, south polar skua Catharacta maccormicki and brown skua Catharacta lonnbergi. The birds were taken in central parts of Vestjella in Dronning Maud Land in February 1977 and at Bouvetøya in the South Atlantic in February 1977 and January 1979. Low levels of DDE, PCB and HCB were found in the two species of penguins, snow petrel, Cape pigeon and southern fulmar, while significantly higher levels were found in south polar and brown skua. The lowest mercury levels were found in the two penguin species and snow petrel. Cape pigeon, southern fulmar and south polar skua form an intermediate group, while the highest mercury levels were found in brown skua. It is assumed that there is a connection between the present findings and the migration pattern of the different birds. The results seem to be in agreement with previous investigations.

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