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- W248973504 abstract "The unique goniatite−rich pyritic level, 1.6 m thick, exposed at Kostomloty (Holy Cross Mountains, central Poland) represents a distinct, local biotic event in the Early Frasnian interval corresponding to the inception of a major geo− chemical (carbon cycling) perturbation in the stagnant deep−water and oxygen−deficient Kostomloty basin. The taxo− nomic and palaeoecologic characteristics of molluscan fossil associations from the Goniatite Level are presented. Most of the goniatitids and orthoconic nautiloids from the studied fossil assemblages are juvenile conchs or protoconchs, or incomplete phragmocones and represent the genera Acanthoclymenia and Linguatornoceras, the former being pre− dominant, and a single adult specimen probably of the genus Koenenites. In contrast, gastropods and bivalves are gen− erally well preserved and identifiable to species level. Two new species are described: a gastropod Palaeozygopleura (Bohemozyga) pyritica sp. nov. and a bivalve Glyptohallicardia multicostata sp. nov. These studied molluscs and also amphiporoids are allochthonous elements which must have been transported into the deeper settings during sea−level rise and flooding of fringing reefs (Timan Event) and/or storm events, and there were mixed with pelagic cephalopods. Probably, a sea−level rise even led to flooding of nearby areas, and thus to introduction of pelagic material (juvenile cephalopods) into reefal settings, and then back to the deeper water again by the quasi−estuarine circulation of water masses." @default.
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- W248973504 date "2006-01-01" @default.
- W248973504 modified "2023-09-23" @default.
- W248973504 title "Molluscs from the Early Frasnian goniatite level at Kostomloty in the Holy Cross Mountains, Poland" @default.
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