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  • 1
    Keywords: Petroleum Geology ; North Sea ; Nordsee Süd ; Kohlenwasserstofflagerstätte
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (209 Seiten)
    ISBN: 1897799829
    Series Statement: Geological Society special publication 123
    DDC: 553.280916336
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 433 (2005), S. 728-731 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Silicon has a crucial role in many biogeochemical processes—for example, as a nutrient for marine and terrestrial biota, in buffering soil acidification and in the regulation of atmospheric carbon dioxide. Traditionally, silica fluxes to soil solutions and stream waters are thought to be ...
    Type of Medium: Electronic Resource
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  • 3
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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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  • 4
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    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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