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  • 1
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    PANGAEA
    In:  Supplement to: Kouchinsky, Artem; Bengtson, Stefan; Gallet, Y; Korovnikov, I; Pavlov, Vladimir; Runnegar, Bruce; Shields, Graham; Veizer, Jan; Young, Edward; Ziegler, Karen (2008): The SPICE carbon isotope excursion in Siberia: a combined study of the upper Middle Cambrian–lowermost Ordovician Kulyumbe River section, northwestern Siberian Platform. Geological Magazine, 145(5), 609-622, https://doi.org/10.1017/S0016756808004913
    Publication Date: 2023-05-12
    Description: An integrated, high-resolution chemostratigraphic (C, O and Sr isotopes) and magnetostratigraphic study through the upper Middle Cambrian – lowermost Ordovician shallow-marine carbonates of the northwestern margin of the Siberian Platform is reported. The interval was analysed at the Kulyumbe section, which is exposed along the Kulyumbe River: an eastern tributary of the Enisej River. It comprises the upper Ust'-Brus, Labaz, Orakta, Kulyumbe, Ujgur, and lower Iltyk formations and includes the Steptoean positive carbon isotopic excursion (SPICE) studied here in detail from upper Cambrian carbonates of the Siberian Platform for the first time. The peak of the excursion, showing d13C positive values as high as +4.6‰ and least-altered 87Sr/86Sr ratios of 0.70909, is reported herein from the Yurakhian Horizon of the Kulyumbe Formation. The stratigraphic position of the SPICE excursion does not support traditional correlation of the boundary between the Orakta and Labaz formations at Kulyumbe River with its supposedly equivalent level in Australia, Laurentia, South China, and Kazakhstan, where the Glyptagnostus stolidotus and G. reticulatus biozones are known to immediately precede the SPICE excursion and span the Middle-Upper Cambrian boundary. The Cambrian-Ordovician boundary is probably situated in the middle Nyajan Horizon of the Iltyk Formation, in which carbon isotope values show a local maximum below a decrease in the upper part of the Nyajan Horizon, attributed herein to the Tremadocian. A refined magnetic polarity sequence shows that the geomagnetic reversal frequency was very high during the Middle Cambrian at 5-10 reversals per Ma, assuming a total duration of ~10 Ma and up to 100 magnetic intervals in the Middle Cambrian. By contrast, the sequence attributed herein to the Upper Cambrian on chemostratigraphic grounds contains only 10-11 magnetic intervals. Preprint in Open Access hdl:10013/epic.30209.d001
    Keywords: Geological profile sampling; GEOPRO; Kulyumbe river, Siberia, Russia; Kulyumbe-section
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Kouchinsky, Artem; Bengtson, Stefan; Pavlov, Vladimir; Runnegar, Bruce; Val'kov, Anatolij K; Young, Edward (2005): Pre-Tommotian age of the lower Pestrotsvet Formation in the Selinde section on the Siberian platform: carbon isotopic evidence. Geological Magazine, 142(4), 319-325, https://doi.org/10.1017/S0016756805000865
    Publication Date: 2023-05-12
    Description: Carbon isotopic data from the Selinde section in the southeastern part of the Siberian platform area are correlated with the reference isotopic profile from the Lower Cambrian stratotype sections of the Lena Aldan region, but also show additional d13C excursions unrecognized there. The chemostratigraphic correlation suggests that the geological and fossil record of the lower Pestrotsvet Formation in the Selinde section has a deeper history than the stratotype region. This conclusion is important for both constraining the age of the earliest Cambrian marine transgression on the Siberian platform and providing a clearer understanding of the pace and order of early Cambrian geochemical and biological events.
    Keywords: Isotope ratio mass spectrometry; OUTCROP; Outcrop sample; POINT DISTANCE from start; Sample code/label; Selinde; Siberia, Russia; δ13C, carbonate; δ18O, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 795 data points
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Kouchinsky, Artem; Bengtson, Stefan; Pavlov, Vladimir; Runnegar, Bruce; Torssander, Peter; Young, Edward; Ziegler, Karen (2007): Carbon isotope stratigraphy of the Precambrian-Cambrian Sukharikha River section, northwestern Siberian platform. Geological Magazine, 144(3), 1-10, https://doi.org/10.1017/S0016756807003354
    Publication Date: 2023-05-12
    Description: A high-resolution carbon isotope profile through the uppermost Neoproterozoic–Lower Cambrian part of the Sukharikha section at the northwestern margin of the Siberian platform shows prominent secular oscillations of d13C with peak-to-peak range of 6-10 ‰. There are six minima, 1n-6n, and seven maxima 1p-7p, in the Sukharikha Formation and a rising trend of d13C from the minimum 1n of -8.6 ‰ to maximum 6p of +6.4 ‰. The trough 1n probably coincides with the isotopic minimum at the Precambrian-Cambrian boundary worldwide. Highly positive d13C values of peaks 5p and 6p are typical of the upper portion of the Precambrian-Cambrian transitional beds just beneath the Tommotian Stage in Siberia. A second rising trend of d13C is observed through the Krasnoporog and lower Shumny formations. It consists of four excursions with four major maxima that can be cor related with Tommotian-Botomian peaks II, IV, V, and VII of the reference profile from the southeastern Siberian platform. According to the chemostratigraphic cor relation, the first appearances of the index forms of archaeocyaths are earlier in the Sukharikha section than in the Lena-Aldan region.
    Keywords: Aluminium; Barium; Boron; Calcium; Cerium; Chromium; Cobalt; Comment; Copper; ELEVATION; Formation; Iron; Lanthanum; Lead; Lithium; Magnesium; Magnesium/Calcium ratio; Manganese; Manganese/Strontium ratio; Neodymium; Nickel; Niobium; OUTCROP; Outcrop sample; Phosphorus; Potassium; Samarium; Sample code/label; Siberia, Russia; Silicon; Sodium; Strontium; Sukharikha; Sulfur, total; Titanium; Tungsten; Vanadium; Yttrium; Zinc; δ13C, carbonate; δ18O, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 3924 data points
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 20 (2001), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: One of the parameters useful for monitoring large-scale climate variability in the Arctic Ocean is sea level. It integrates virtually all static and dynamic processes in the hydrosphere and atmosphere of the Arctic. Previously unavailable mean monthly sea level data at 44 coastal and island stations in the Kara, Laptev, East Siberian and Chukchi seas covering years from 1950 to 1990 were used to analyse seasonal and inter-annual variability. Sea level has a significant annual cycle with an average seasonal amplitude (from peak to peak) in the coastal zone of the Arctic seas on the order of 20 - 30 cm. The analysis of inter-annual and inter-decadal changes has shown that at nearly all stations in the Kara, Laptev, East Siberian and Chukchi seas from the beginning of the 1950s through the end of 1980s there is a positive trend in sea level variability. The main contribution to the sea level rise was in the 1980s; on average for the coastal zone of Siberian shelf the sea level in the 1980s was 5-6 cm higher than in the previous decades. A reasonable agreement between observed decadal mean sea level values and the results of diagnostic model simulations suggests that this rise in the Arctic seas is connected with the reorganization of large-scale circulation of the Arctic Ocean, rather than the regional lowering of the coasts, as has been suggested previously.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 125 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We present the magnetostratigraphy of the early Palaeozoic Moyero river section in north-western Siberia. the section investigated, which consists mainly of reddish limestones, marls and greyish limestones, extends from the upper Cambrian to the lower Silurian. Palaeomagnetic analyses reveal two magnetic components. One is interpreted as a remagnetization acquired during Siberian trap emplacement; the other is believed to be early diagenetic, consistent with the established lower Palaeozoic apparent polar wander path for Siberia. Reversed polarity dominates from the upper Cambrian to the middle Ordovician, while normal polarity dominates from the upper Ordovician to the lower Silurian. Only a few reversals, which are poorly defined, are observed through the section, in particular during the Llandeilo. These data are in agreement with previous magnetostratigraphic data from the Baltic platform and Siberia and indicate that magnetic reversal frequency was low during the Ordovician. Because of the time-delayed process of acquisition of the magnetization carried by haematite, we cannot clearly ascertain if a reversed superchron occurred during the lower to middle Ordovician. However, our results suggest that a 15 Myr-long reversed interval existed during the Arenig.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1573-1421
    Keywords: acid pulse ; Barents Region ; baseflow ; snow melt ; springtime flood ; time-series
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Stream water composition, measured weekly for 8–9 months in 1994 in three arctic catchments on and around the Kola Peninsula (Russia, Finland and Norway), is presented in the form of time-series. In all three catchments, snowmelt causes a major dilution of the stream water, as reflected by marked dips in electrical conductance. In the most polluted catchment (C2), the snowmelt flood (the major hydrological event at these latitudes) is reflected in the stream water by a pH dip and a pulse in technogenic heavy metals (Cu, Ni, etc.), Al and S. This results from melting of the snow laden with heavy metals and sulphate, and from leaching of the topsoil layer. In the most pristine catchment (C8), snowmelt causes no heavy metal pulse (remote location) but yields an increase in stream water Al (acidic lithology/overburden). In the intermediate catchment (C5), very subdued heavy metal and S increases are noticeable in the stream water, whilst its pH increases steadily until summer (basic lithology). Some elements (Cl, S) may be mobilised out of the snowpack before its complete thawing and reach the stream 1–2 weeks ahead of the heavy metals. The substrate (soil, overburden and bedrock) of a catchment controls to a large extent its ability to buffer acid inputs.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1573-1421
    Keywords: anthropogenic ; Barents region ; contamination ; geogenic ; sea spray ; trace metal
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The pH, electrical conductance and concentration of six anions and 33 cations were determined in stream waters sampled in 1994 from eight arctic catchments on and adjacent to the Kola Peninsula (Russia, Finland and Norway). The catchments are located at various distances (5–300 km) from the major industrial emissions centres of Monchegorsk, Nikel and Zapoljarniy in Russia. The source of the elements can be (1) natural, marine (sea spray), (2) natural, geogenic (blowing soil/dust, till, bedrock), and/or (3) anthropogenic, industrial (emissions from smelters, dust from mining, etc.), each source showing a distinct signature. The median concentration of many contaminants can vary by up to three orders of magnitude from polluted to remote locations, and the concentration ranges observed in different catchments often do not overlap. This implies that contamination falls sharply with distance from source, but is quite profound and lasting close to the emission centres. Elevated trace metal contents in the most polluted streams indicates that deposited contaminants are transferred to the aquatic ecosystem, and eventually can reach the ocean.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1573-2932
    Keywords: airborne pollution ; copper ; humus ; Hylocomium splendens ; nickel ; nickel smelter ; Pleurozium schreberi ; sulphur ; terrestrial moss
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Terrestrial moss and humus (the O-horizon) are often used separately for determining and monitoring airborne heavy metal pollution. Here, we directly compare the results of analyses of moss and humus samples taken at a density of one site per 300 km2 in a 12 000 km2 area (45 samples) around the nickel smelter in Nikel, the nickel ore roasting plant in Zapoljarnij, both in Russia, and the iron ore mine and mill near Kirkenes in Norway. The samples were air dried, digested in conc. HNO3 and analysed for more than 30 elements by ICP-MS and ICP-AES at the laboratory of the Geological Survey of Finland (GTK). For most elements, observed levels and variations are considerably greater in soil than in moss. The main contaminants, Ni and Cu, reach equally high median levels in the moss and soil, but maximum values are far higher in soil. Both media show comparable regional distribution patterns for the heavy metals, but not for sulphur. Cu and Ni can be used to delineate the limits of contamination in the survey area. Both media show the same picture, with a generally very steep gradient from east to west and background levels being reached 30–50 km from the nickel smelter. When moss is used, Cu/Ni, Cu/S and Ni/S ratios can be used to separate input from the smelting and roasting processes in Russia. Both media are well suited to use separately to detect airborne pollution in this heavily contaminated area. The moss data are generally easier to interpret, but moss is not available at the most polluted sites. Levels for many elements other than Cu and Ni are close to the detection levels in moss samples, but not in humus samples. Information gathered from both media thus complement each other in a regional multi-element survey.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-2932
    Keywords: airborne pollution ; copper ; humus ; Hylocomium splendens ; nickel ; nickel smelter ; Pleurozium schreberi ; sulphur ; terrestrial moss
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Terrestrial moss and humus (the O-horizon) are often used separately for determining and monitoring airborne heavy metal pollution. Here, we directly compare the results of analyses of moss and humus samples taken at a density of one site per 300 km2 in a 12 000 km2 area (45 samples) around the nickel smelter in Nikel, the nickel ore roasting plant in Zapoljarnij, both in Russia, and the iron ore mine and mill near Kirkenes in Norway. The samples were air dried, digested in conc. HNO3 and analysed for more than 30 elements by ICP-MS and ICP-AES at the laboratory of the Geological Survey of Finland (GTK). For most elements, observed levels and variations are considerably greater in soil than in moss. The main contaminants, Ni and Cu, reach equally high median levels in the moss and soil, but maximum values are far higher in soil. Both media show comparable regional distribution patterns for the heavy metals, but not for sulphur. Cu and Ni can be used to delineate the limits of contamination in the survey area. Both media show the same picture, with a generally very steep gradient from east to west and background levels being reached 30–50 km from the nickel smelter. When moss is used, Cu/Ni, Cu/S and Ni/S ratios can be used to separate input from the smelting and roasting proccesses in Russia. Both media are well suited to use separately to detect airborne pollution in this heavily contaminated area. The moss data are generally easier to interpret, but moss is not available at the most polluted sites. Levels for many elements other than Cu and Ni are close to the detection levels in moss samples, but not in humus samples. Information gathered from both media thus complement each other in a regional multi-element survey.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2002-09-01
    Print ISSN: 0047-2425
    Electronic ISSN: 1537-2537
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Wiley
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