In the present study we have investigated the activity concentrations of (210)Pb, (210)Po as well as (7)Be in surface air of the North and South Atlantic (1988-1989), the Arctic Ocean (1991), and along the coastline of Siberia (1994) during succeeding expeditions in the Swedish Polar Research program. During the cruises in the Arctic Ocean during 1991-07-28 to 1991-10-04 the average air concentrations of (7)Be was 0.6 ± 0.4 mBq/m(3), (210)Pb 40 ± 4 µBq/m(3) and (210)Po-38 ± 10 µBq/m(3). During the Swedish-Russian Tundra Ecology-94 expedition along the Siberian coastline the average air concentrations of (7)Be and (210)Pb measured during May-July were 11 ± 3, and 2.4 ± 0.4 mBq/m(3), and during July-September they were 7.2 ± 2 and 2.7 ± 1.1 mBq/m(3) respectively. The results from measurements of the activity concentration of (210)Pb in the air over the Arctic Ocean vary between 75 and 176 µBq/m(3). In the air close to land masses, however, the activity concentration of (210)Pb in the air increases to 269-2712 µBq/m(3). The activity concentration of (7)Be in the South Atlantic during the cruise down to Antarctica varied between 1.3 and 1.7 with an average of 1.5 ± 0.8 mBq/m(3). The activity concentration of (210)Pb in the South Atlantic down to Antarctica varied between 6 and 14 µBq/m(3). At the Equator the activity concentration recorded in November 1988 was 630 µBq/m(3) and in April 1989 it was 260 µBq/m(3). The average activity concentration of (210)Pb during the route Gothenburg-Montevideo in 1988 was 290 and on the return Montevideo-Gothenburg it was 230 µBq/m(3). The activity concentration of (210)Po in the South Atlantic down to Antarctica varied between 15 and 58 µBq/m(3). At the Equator the activity concentration in November 1988 was 170 and in April 1989 it was 70 µBq/m(3). The average activity concentration of (210)Po during the route Gothenburg-Montevideo in 1988 was 63 and on the return Montevideo-Gothenburg it was 60 µBq/m(3). The average of the activity concentrations in the Antarctic air of (210)Pb was 27 ± 10 µBq/m(3) and of (210)Po it was 12 ± 7 µBq/m(3). All our results were compiled together with other published data, and the global latitudinal distribution of (210)Pb was converted to total annual deposition (Bq/m(2)/a) and fitted to a 4th degree polynomial. By using the global latitudinal distribution of (210)Po/(210)Pb-activity ratio from our own results the global latitudinal distribution of (210)Po annual deposition was derived.
The preservation of human health in polar and circumpolar regions depends mainly on the strategy for future development of these regions. The consequences of human intervention into northern ecology are irreversible, as in the case of greenhouse effect, industrial and atomic pollutions of polar nature, tundra devastation, destruction of northern flora and fauna, etc. The ongoing creation of large-scale industrial population centers in the North due to newcomers is to be stopped. Polar regions are to be used for biospheric reservation and tourist sanitary zones, to preserve specific flora and fauna, to provide the rhythms and customs necessary to survive in extreme climatic and geophysical conditions of high latitudes. The programme for securing man's survival in circumpolar regions should comprise several stages of practical measures to provide necessary resources and to combine international efforts. The preservation of human health should be based on the understanding of the relationship between the health status and biospheric processes and the assessment of the role of human intervention into polar ecology. A programme facilitating the preservation of human health and survival in the North and in the Antarctic should be launched.
The examinations were carried out during the 27th Soviet Antarctic expedition. Baseline data were collected before the departure of the test subjects to the Antarctic Region. Prior to their ascent to the high mountain area they were divided into two groups with a high and a low level of hypoxic tolerance in terms of the work capacity index calculated on the basis of standard bicycle ergometry tests. Heart rate, body temperature and salivary content of sodium and potassium were measured 6 times a day at 4-hour intervals. The results obtained were treated by nonparametric tests. It was found that on adaptation day 30 the subjects with low hypoxic tolerance and nonspecific resistance developed changes in biorhythm amplitudes and phases and showed ultradian components with a 12-hour period. By contrast, the subjects with high hypoxic tolerance retained the ability to maintain circadian patterns. By the middle of the wintering time the circadian rhythms shifted towards ultradian components regardless of individual hypoxic tolerance.
In the Antarctic, fishes of dominant suborder Notothenioidei have evolved in a unique thermal scenario. Phylogenetically related taxa of the suborder live in a wide range of latitudes, in Antarctic, sub-Antarctic and temperate oceans. Consequently, they offer a remarkable opportunity to study the physiological and biochemical characters gained and, conversely, lost during their evolutionary history. The evolutionary perspective has also been pursued by comparative studies of some features of the heme protein devoted to O(2) transport in fish living in the other polar region, the Arctic. The two polar regions differ by age and isolation. Fish living in each habitat have undergone regional constraints and fit into different evolutionary histories. The aim of this contribution is to survey the current knowledge of molecular structure, functional features, phylogeny and adaptations of the haemoglobins of fish thriving in the Antarctic, sub-Antarctic and Arctic regions (with some excursions in the temperate latitudes), in search of insights into the convergent processes evolved in response to cooling. Current climate change may disturb adaptation, calling for strategies aimed at neutralising threats to biodiversity.
Department of Plant Protection, Division of Plant Pathology and Mycology, Wroclaw University of Environmental and Life Sciences, Grunwaldzki Sq. 24a, 50-363, Wroclaw, Poland. email@example.com.
Studies on the presence of atmospheric fungi in both Arctic and Antarctic polar areas are rare, and many of them were carried out briefly. Currently, when climate change is a fact, polar areas may be subject to various changes and fluctuations, negatively affecting sensitive polar ecosystems. The paper presents the results of tests on presence of fungi in the air over 30 years after the last investigations at the Svalbard Archipelago. A total of fifteen taxa of fungi were isolated in area of Longyearbyen, the majority of which were saprotrophic fungi of the genus Cladosporium that are associated with dead organic matter. Therefore, the presence of this taxon may be a good bioindicator of changes occurring in the Arctic environment, indirectly indicating the melting of glaciers and exposing increasingly larger areas inhabited by microorganisms, including fungi, which increase in number in the air. Additionally, the number of tourists visiting Longyearbyen is increasing, which may significantly affect the number and type of fungi in the air.
The Alfred Wegener Institute carries out research in the Arctic and Antarctic as well as in the high and mid latitude oceans. The institute coordinates German polar research and makes available to national and international science important infrastructure, e.g. the research ice breaker &quot;Polarstern&quot; and research stations in the Arctic and Antarctic.
The pH of polar ice is important for the stability and mobility of impurities in ice cores and can be strongly influenced by volcanic eruptions or anthropogenic emissions. We present a simple optical method for continuous determination of acidity in ice cores based on spectroscopically determined color changes of two common pH-indicator dyes, bromophenol blue, and chlorophenol red. The sealed-system method described here is not equilibrated with CO2, making it simpler than existing methods for pH determination in ice cores and offering a 10-90% peak response time of 45 s and a combined uncertainty of 9%. The method is applied to Holocene ice core sections from Greenland and Antarctica and compared to standard techniques such as electrical conductivity measurement (ECM) conducted on the solid ice, and electrolytic meltwater conductivity, EMWC. Acidity measured in the Greenland NGRIP ice core shows good agreement with acidity calculated from ion chromatography. Conductivity and dye-based acidity Hdye(+) are found to be highly correlated in the Greenland NEGIS firn core (75.38? N, 35.56? W), with all signals greater than 3s variability coinciding with either volcanic eruptions or possible wild fire activity. In contrast, the Antarctic Roosevelt Island ice core (79.36? S, 161.71? W) features an anticorrelation between conductivity and Hdye(+), likely due to strong influence of marine salts.
An historical review is made of Antarctic medical practice, which is unique because of the absence of an indigenous population. This review begins with the primitive shipboard practice of doctors accompanying Captain James Cook around 1775 and concludes with the modern era of permanent stations and vast scientific endeavour. The heroic era of Scott, Shackleton, Amundsen and Mawson and the highly mechanized transition period are contrasted with the present day. Medical practice on modern expeditions has reached a high standard, but there is still much to be learned concerning human adaptation. Comment is made on the possible utilization of Antarctica's natural resources bringing increases in polar populations and facilitating the expansion of medical research in the future era of polar medicine.