Record details

Title
    Influence of acid volcanism and CO2 production on sedimentation and distribution of organic matter (Variscan Central Europe)
Statement of responsibility
    Jaroslav Dvořák
Other titles
    Influence du volcanisme acide et de la production de CO2 sur la sédimentation et la distribution de matiere organique (Europe centrale varisque)
    Stratigraphie du Paléozoique - Hommage a Maurice Streel (Variant.)
Author
    Dvořák, Jaroslav
Language
    anglicky
Source title - serial
    Annales de la Société géologique de Belgique
Vol./nr.
    Vol. 117, no. 1
Pages
    p. 69-73
Year
    1994
Notes
    Francouzské resumé
    il.
    Obsahuje bibliografické odkazy
    Zkr. název ser.: Ann. Soc. géol. Belg.
Subject group
    devon
    flyš
    karbon-spodní
    moravskoslezský devon a spodní karbon
    oxid uhličitý
    paleoklimatologie
    sedimentace útesová
    sedimentologie
    vrásnění variské
    vulkanismus
Geographical name
    ČR-Morava
Keyword
    Acid
    Central
    CO2
    Distribution
    Europe
    Influence
    Matter
    Organic
    Production
    Sedimentation
    Variscan
    Volcanism
Abstract (in english)
   From Silurian to Permian times we can document the existence of a single supercontinent - Pangea. The mobile zones within variscan Europe, which developed on unstable continental crust, were flooded by epicontinental seas. Northward continental drift of the Pangea was documented. There is a considerable contrast between Middle Devonian time of reef-limestone sedimentation (fixation of CO2 from the water and atmosphere in limestones) and the later Carboniferous sedimentation and contemporaneous acid volcanism with a high rate of production of CO2 and probably short-lived greenhouse effects
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    19. 6. 2009
Import date
    8. 8. 2012