Published December 31, 2002
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Fig. 7. Trace element environmental proxies for the F–F in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records
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Fig. 7. Trace element environmental proxies for the F–F transition in the Syv'yu River section. Bio−productivity tracers* are normalized according to Schmitzetal.(1997).DownwardarrowedtrendsarebasedonthesinglesampleCB99−222,located2.15mbelow;recognizedMo/Alenrichment,indicative of anoxic−sulfidic deposition, is shown as well. For explanations see Fig. 4.
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Published as part of Yudina, Alexandra B., Racki, Grzegorz, Savage, Norman M., Racka, Maria & Małkowski, Krzysztof, 2002, The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records, pp. 355-372 in Acta Palaeontologica Polonica 47 (2) on page 365, DOI: 10.5281/zenodo.13304843
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- Journal article: 10.5281/zenodo.13304843 (DOI)
- Journal article: urn:lsid:plazi.org:pub:514EF72BFFECC56A896A7908FFAADA4F (LSID)