skip to main content
Idioma:
Primo Advanced Search
Primo Advanced Search Query Term
Primo Advanced Search Query Term
Primo Advanced Search Query Term
Primo Advanced Search prefilters
Busca Simples

Paleoclimate changes in the late precambrian: Evidence from the upper precambrian section of the South Urals

Maslov, A. V. ; Podkovyrov, V. N. ; Gareev, E. Z. ; Graunov, O. V.

Lithology and Mineral Resources, 2016-03, Vol.51 (2), p.117-135 [Periódico revisado por pares]

Moscow: Pleiades Publishing

Texto completo disponível

Citações Citado por
  • Título:
    Paleoclimate changes in the late precambrian: Evidence from the upper precambrian section of the South Urals
  • Autor: Maslov, A. V. ; Podkovyrov, V. N. ; Gareev, E. Z. ; Graunov, O. V.
  • Assuntos: Brackish ; Earth and Environmental Science ; Earth Sciences ; Environmental impact ; Marine ; Mineral Resources ; Mineralogy ; Paleoclimate science ; Sedimentary geology ; Sedimentology
  • É parte de: Lithology and Mineral Resources, 2016-03, Vol.51 (2), p.117-135
  • Notas: ObjectType-Article-1
    SourceType-Scholarly Journals-1
    ObjectType-Feature-2
    content type line 23
  • Descrição: The climatic impact on the formation of fine-grained rocks from the Riphean stratotype and Vendian Asha Group on the western slope of the South Urals during the time interval lasting approximately 1200 Ma is considered. It is shown that these rocks are largely represented by “tectonosilicate-dominated” shales. This feature combined with changes in the average K 2 O/Al 2 O 3 values disavows the hypothesis in (Kennedy et al., 2006), according to which the growth of free oxygen concentration in the Late Riphean and Vendian atmosphere was determined by gradual intensification of the organic carbon extraction from the biosphere by clays. The average values of the hydrolyzate module, chemical index of alteration (CIA), and several lithogeochemical parameters calculated for the Riphean and Vendian clayey rocks provide grounds for the conclusion that intensity of weathering in paleodrainage areas during the accumulation of the Upper Precambrian sedimentary successions was low. The curve reflecting changes of the average CIA values in the Upper Precambrian fine-grained siliciclastic rocks of the South Urals is similar to some extent with the “standard” CIA correct . curve (GonzalezAlvarez and Kerrich, 2012). It is assumed that changes in microand macrobiotic communities during the Late Precambrian were controlled to a variable extent by climate fluctuations as well. At the same time, these fluctuations most likely left the chemical composition of water in the ocean virtually unchanged, which is evident from analysis of the redox conditions in the ocean and the distribution of primary producers with the average CIA correct . and CIA values.
  • Editor: Moscow: Pleiades Publishing
  • Idioma: Inglês
Voltar para lista de resultados
Ir para página anteriorAnterior Resultado  7 AvançarIr para próxima página

  • Realização: ABCD-USP USP   Logos de Redes Sociais: Freepik

Buscando em bases de dados remotas. Favor aguardar.