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Filozofia przyrody jako podstawa dla sozologii

Lemańska A.

Problemy Ekologii

2009

R. 13, nr 6

297-299

W artykule uzasadnia się, że filozofia przyrody stanowi jeden z filarów, na których można się oprzeć, poszukując podstaw aksjologicznych dla działań podejmowanych w celu ochrony środowiska. Takich fundamentów nie mogą dostarczyć same nauki przyrodnicze, gdyż metoda eksperymentalna nie dopuszcza możliwości dokonywania wartościowań. W ramach filozofii przyrody można też próbować poszukiwać rozwiązań unikających skrajności zarówno antropocentryzmu, jak i biocentryzmu.

The article presents a justification that the philosophy of nature is one of the pillars which can be used as a support while seeking the axiological foundations for the actions undertaken for environmental protection. These foundations cannot be solely provided by the natural sciences as the experimental method does not allow making valuations. The framework of the philosophy of nature enables making attempts to find solutions which avoid extremes of both anthropocentrism and biocentrism.

Comparison of deep-water agglutinated foraminifera from the hemipelagic variegated shales (Lower Turonian-Lower Santonian) and turbiditic Godula beds (Upper Santonian-Campanian) in the Lanckorona-Wadowice area (Silesian Unit, Outer Carpathians, Poland)

Lemańska A.

Studia Geologica Polonica

2005

Vol. 124

259-272

Deep-water agglutinated foraminifera (DWAF) have been studied from variegated shales and Godula beds exposed in the vicinity of Kalwaria Zebrzydowska (Silesian Nappe, Outer Carpa- thians, Poland). Following the standard foraminiferal zonation scheme of Geroch & Nowak (1984), the studied variegated shales can be correlated with the Uvigerinammina jankoi Zone (Lower Turonian-Lower Santonian). The Godula beds can be correlated to the Caudammina gigantea Zone (Upper Santonian-Campanian). Foraminiferal assemblages from the variegated shales are dominated by infaunal and semi-infaunal forms. Their occurrence suggests aerobic bottom water conditions associated with low organic matter availability during the deposition of this unit. Such conditions are presumably related to slow sedimentation rate in low energy, well-oxygenated and oligotrophic bottom environment. In contrast, foraminiferal assemblages from the Godula beds are dominated by epifaunal forms, which collected food from the sediment/water interface. It may suggest that sedimentation took place under relatively higher energy conditions with a higher organic matter flux.