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Eustatic cycles around the Devonian-Carboniferous Boundary and the sedimentary and fossil record in Sauerland (Federal Republic of Germany)
Bless, M.J.M.; Becker, R. T.; Higgs, K.; Paproth, E.; Streel, M. (1992). Eustatic cycles around the Devonian-Carboniferous Boundary and the sedimentary and fossil record in Sauerland (Federal Republic of Germany). Ann. Soc. géol. Belg. (1968) 115(2): 475-481
In: Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège. ISSN 0037-9395
Peer reviewed article  
Available in  Authors 
Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Carboniferous
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian
    Germany
    Spores
    Cephalopoda [WoRMS]; Conodonta; Ostracoda [WoRMS]; Trilobita † [WoRMS]
    Germany [Marine Regions]
    Marine/Coastal
Authors  Top 
  • Bless, M.J.M.
  • Becker, R. T.
  • Higgs, K.
  • Paproth, E.
  • Streel, M.
Abstract
    A review of the sedimentary and fossil record around the Devonian/Carboniferous (D/C) boundary in Sauerland at the northern border of the Rhenish Slate Mountains (Rheinisches Schiefergebirge; Germany) forms the basis for the recognition of a succession of relative sea level changes in that area. This transgression/regression (T-R) curve shows a remarkable similarity with the one constructed for the La Serre D/C boundary stratotype (Montagne Noire, France). It is therefore suggested that these T-R curves are closely related to global (eustatic) sea level changes.
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