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41.
We studied the accumulation of polychlorinated biphenyls (PCBs), 1,1,1.trichloro-2,2-bis[p-chlorophenyl]ethane (DDT) and its metabolites, and vitamins A and E in the top levels of the Baltic Sea food web. The investigation focused on the transfer of contaminants and vitamins to the ringed seal (Phoca hispida baltica) and the grey seal (Halichoerus grypus) from their main prey species. The trophic level of the seals was investigated using stable isotopes of nitrogen and the results indicated that both species of Baltic seal feed at approximately the same level. PCBs accumulated to a greater extent in the grey seal than in the ringed seal. Biomagnification factors for DDT compounds were similar for both species of Baltic seal (85-140). Differences in observed DDT levels were due to different prey selection by the two species, while differences in PCB levels indicated a species-specific metabolic system. There was a clearly greater accumulation of DDT compounds than of PCBs in both species of seal. The supply of dietary vitamin A was normally above the recommended level in all the seal populations studied. Low levels of hepatic vitamin A in the Baltic seals could therefore indicate the toxic effects of a high level of persistent organic pollutants on vitamin A dynamics, at least in the ringed seal. In the grey seals, low hepatic vitamin A levels could also be explained by lower levels of dietary vitamin A, compared to the reference grey seals, as it is not known if seals can store unlimited amounts of vitamin A. The greater uptake of vitamin E by Baltic seals, compared to seals in the reference areas, demonstrated by elevated levels of vitamin E in the blubber, could be a response to oxidative stress caused by the high contaminant load. These results further support our previous hypothesis that the toxic effects of environmental contaminants could be causing the observed divergence in vitamin levels between the Baltic seals and the reference seal populations. 相似文献
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Reijo K. Helle 《GeoJournal》1987,14(2):211-216
In this report the author investigates the oil drilling activity after the oil crisis in 1973 when the western industrial countries made efforts to create a new balance. Efforts in oil prospecting culminated in oil drilling in order to compensate for the crude oil sources which were no longer under the control of western industrial countries. This development is studied in the frame of reference put forward by Saul Cohen in his theory of geopolitical balance concerning horizontal and vertical compensation. 相似文献
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This year is a kind of anniversary for the Norwegian Polar Institute: its establishment can be traced back to Svalbard expeditions sponsored by Prince Albert I of Monaco in 1906 and 1907. In this unreviewed biographical article, biologist Eva Fuglei, who has spent many seasons on Spitsbergen (where her research has focused on Arctic foxes), and the editor describe part of the uncommon life of botanist Hanna Marie Resvoll-Holmsen, who participated in the 1907 expedition. 相似文献
44.
The reeds of Lake Peipsi (surface area 3555 km2, mean depth 7.1 m, max. depth 15.3 m, not-regulated) have increased through the last 30 years. The most significant increase has taken place in the larger formerly mesotrophic northern part where the mean air-dry biomass of reed shoots has increased from 20 g m−2 in 1970 through 789 g m−2 in 1989 to 1563 g m−2 in 2002. The data of 34 transects for 2001–2002 along the Estonian coast and aerophotos made in 2001 showed that in places reeds reach a water depth of 1 m (mean 0.64 m) and a width of more than 200 m (mean 89.5 m). Their area of 9.3 km2 accounts for about 0.6% of the Estonian territory of the lake. The longer and thicker shoots grew in the lakeward and intermediate zones of reeds. Near villages the shoots were weaker and their biomass lower. Phosphorus content of shoots, being higher near settlements, was generally low; in some cases content of phosphorus was ≤0.001%. The monotonous reed belt occupies the growth area of shallow-water submergent and shorter emergent species and favours the accumulation of organic sediments. The frequency of several species demanding light and sandy bottom has decreased, as well has the overall diversity of the macrovegetation. The main reasons for expansion of the reed could be eutrophication, combined with low-water periods, and the decline of cattle breeding in the shore areas. Some suppressed species have reappeared on stretches cleaned from reeds. 相似文献
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From the editor: Polar Research evolves, and Norway and the IPY 总被引：2，自引：2，他引：0
Helle V. GoldmanChief Editor 《Polar research》2007,26(1):1-6
47.
Fredrik Høgaas Louise Hansen Ivar Berthling Martin Klug Oddvar Longva Helle Daling Nannestad Lars Olsen Anders Romundset 《Boreas: An International Journal of Quaternary Research》2023,52(3):295-313
This study discusses the timing and maximum flood level of the Nedre Glomsjø outburst flood, Norway, based on sediment records retrieved from 15 bog and lake basins located close to the purported maximum flooded level. The sediment records in 12 of the basins consist of a distinct light-coloured silty bed that is correlated to the outburst-flood-deposited ‘Romerike Silt Bed’ identified elsewhere in the region. The silt bed is recorded in basins up to a certain elevation and is absent above this level. The new maximum flood level inferred from the basin sediment records exceeds the established landform-induced palaeostage indicators by 5–10 m. The data indicate a higher maximum flood level and larger inundation area than previously suggested and highlight the importance of acquiring a wide range of geological data when reconstructing palaeofloods. Radiocarbon dates of terrestrial macrofossils found stratigraphically above and below the Romerike Silt Bed suggest that the glacial lake Nedre Glomsjø outburst flood occurred between 10.5 and 10.3 cal. ka BP. The new and well-constrained timing of the outburst flood is beneficial for reconstructing regional deglaciation and provides a precise age for the Romerike Silt Bed chronostratigraphical marker, which is of value for studies in SE Norway and adjacent regions. 相似文献
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Fourteen Saimaa ringed seals (Phoca hispida saimensis) were studied for PCB, DDT, chlordane and chlorophenol compounds in blubber, liver, muscle, heart and kidney in Lake Saimaa, eastern Finland, in 1977–1981. Both PCBs and total DDT increased on average from a good 5 mg kg?1 in extractable fat of blubber in a new-born to a good 65 mg kg?1 in sexually mature specimens, the maximum being 93 and 104 mg kg?1 respectively. Concentrations of PCBs and tDDT in blubber and liver were most clearly dependent on the age and weight of the seal. Chlordanes were found in all 14 specimens (mean 0.59 mg kg?1 in blubber), trichlorophenol in one, tetrachlorophenol in two and pentachlorophenol in all three specimens studied. Although some of the Saimaa seals had reached quite high levels of both PCBs and tDDT, the present results do not indicate that the steady decrease of the Saimaa seal population during the last two decades would have been caused by these toxins, at least not in isolation. 相似文献
50.
The island of Surtsey, Iceland, was formed in 1963 by a volcanic eruption. Since then, it has served as a unique natural laboratory for scientists interested in primary succession. In this study we investigated the state of the soil microfauna succession in 1995. We examined locations on the island with different vegetation types (unvegetated soil, soil with one or two plant species, and bird colony soil with a diverse vegetation). We recorded at least 16 nematode taxa and 13 flagellate taxa. Most of these were not reported in previous surveys from Surtsey. On the location with unvegetated soil, ciliates and nematodes were absent and only amoebae and heterotrophic flagellates were found. Most of the protozoan populations we examined were unable to survive salinity levels corresponding to seawater. We therefore conclude that many of soil protozoa populations on Surtsey arrived to the island as airborne cysts brought there from nearby land. However, in the bird colony soil with a high input of salts from the bird droppings, several flagellate species survived and multiplied at seawater salinity. This indicates that the bird colony soil harbours microhabitats where marine flagellate populations have been established. 相似文献