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Foraminifers and stable isotope record of the Dubivtsi chalk (upper Turonian, Western Ukraine): palaeoenvironmental implications

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EN
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EN
A combined micropalaeontological and stable isotope study of the Dubivtsi chalk in the Western Ukraine indicates its middle late Turonian age. One long-term and clearly distinguishable positive excursion of the isotope curve (d1318
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199--214
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Bibliogr. 78 poz., rys., wykr.
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Bibliografia
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bwmeta1.element.baztech-article-BUS6-0036-0009
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