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

Thoresen, P. (1984). Ti nye år: Vestfold Historielag 60 år. Vestfoldminne, 1984, 3–10. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2019012581214_001 URN:NBN:no-nb_digitidsskrift_2019012581214_001

View on urn.nb.no
Vik, K. (1984). Hvorfor gikk det så greitt? Om nedleggelsen av hvalfangstnæringen i Vestfold. Vestfoldminne, 1984, 38–54. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2019012581214_001 URN:NBN:no-nb_digitidsskrift_2019012581214_001

View on urn.nb.no
Fryxell, G. A., & Hasle, G. R. (1983). The antarctic diatoms Thalassiosira dichotomica (Kozlova) comb. nov. and T. ambigua kozlova. Polar Biology, 2(1), 53–62. https://doi.org/10.1007/BF00258286

Two small antarctic diatoms, usually missed by traditional collection methods, have been studied in light and electron microscopes. Porosira dichotomica has been transferred to Thalassiosira since its valve structure and process pattern agree better with that genus. T. dichotomica is unusual in that some lines of areola walls are extended, sail-like, out from the valve, supporting Kozlova's original drawings. T. ambigua, the smaller of the two, has many similarities in structure with T. dichotomica, but has granules on the margin, lacks the sail-like structures on the valve, and has minor differences in processes and areola size. Bands stay together in T. ambigua and show more fine structure than many species in the genus.

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Kristensen, M. (1983). Iceberg calving and deterioration in Antarctica. Progress in Physical Geography: Earth and Environment, 7(3), 313–328. https://doi.org/10.1177/030913338300700301

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Kristensen, M., & Squire, V. A. (1983). Automatic collection of tilt and strain data from tabular icebergs. Annals of Glaciology, 4, 147–151. https://doi.org/10.3189/S0260305500005383
Kristensen, M., & Squire, V. A. (1983). Modelling of antarctic tabular icebergs in ocean waves. Annals of Glaciology, 4, 152–157. https://doi.org/10.3189/S0260305500005395

The prediction of the motions of a tabular iceberg in a seaway is a problem which cannot be solved with a simple approach. The main difficulty lies in the size and mass of the iceberg, which produce frequency-dependent hydrodynamical effects as it moves in the water. Specifically, any solution must take into account both the added inertia and the generation of surface waves caused by the motions of the berg. Early attempts at modelling, which did not include these terms, could not accurately predict the complicated response behaviour seen in field data. In this paper we discuss some modifications to a two-dimensional simulation of floating bodies in waves, which must be applied when the motions and the hydro-dynamical pressures beneath tabular icebergs are required.
Magnus, M. H. (1983). Norge og den sovjetiske polarforskning i nord og sør. Farmand, 6, 83–87.
Øvstedal, D. O. (1983). Some lichens from HU Sverdrup Mountains, Dronning Maud Land, Antarctis. Nova Hedwigia: Zeitschrift Fur Kryptogamenkunde, 37(4), 683–690.
Øvstedal, D. O. (1983). Some lichens from Vestfjella, Dronning Mauds Land, Antarctis. Cryptogamie. Bryologie, Lichénologie, 4(3), 217–226.
Øvstedal, D. O., & Smith, R. L. (1983). A new Pannaria species from the Antarctic. Cryptogamie, Bryologie, Lichenologie, 14(4), 337–340.

Pannaria austro-orcadensis Ovst., sp.nov., from the northern maritime Antarctic, is characterized by its purple-brown lobulate thallus, brown apothecia smooth spores and no secondary products. It grows on moist gravelly soil and bryophytes.
Sømme, L. (1983). Insekter i Antarktis. Forskningsnytt, 28(8), 3–7.
Wadhams, P., Kristensen, M., & Orheim, O. (1983). The response of Antarctic icebergs to ocean waves. Journal of Geophysical Research: Oceans, 88(C10), 6053–6065. https://doi.org/10.1029/JC088iC10p06053

The heave, tilt, and strain responses of three Antarctic tabular icebergs to ocean waves were measured during a 1980–1981 cruise of HMS Endurance to the South Atlantic. The three icebergs, located near the South Sandwich and South Orkney islands, were instrumented with accelerometers, tiltmeters, and wire strainmeters, while a Waverider buoy was used to record the ocean wave field. The thickness of the icebergs was surveyed by a helicopter-borne radio echo sounder. The heave response occurred mainly at the swell period but with outbreaks of bobbing which lasted for a few cycles at a resonant period (about 40 s), which agreed well with the predictions of a numerical finite element model. The roll response occurred mainly at a long resonant period (40–50 s), which again agreed well with the model, but there was also a significant response at ocean wave periods (5–20 s), which exceeded predictions. The strain response had a component at very long periods, which is unexplained by theory, while the surface strain at ocean wave periods agreed with the simple analytical model of Goodman et al. (1980). Using this model it is possible to predict a wave height and period that will cause breakup of the icebergs, and we conclude that swell-induced breakup is likely to occur during major storms in the open southern ocean.

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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). 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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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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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.
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.
Ingstad, H. (1982). Carsten Borchgrevink: lederen for den første overvintring i Antarktis. Polarboken, 1981/82, 44–50.

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