Biomarkery jako wskaźniki facji organicznych w utworach dolomitu głównego

• Autorzy: Grotek I.

Warianty tytułu

EN

Biomarkers as an organic facies indicators in main dolomite sediments

• Języki publikacji: PL

Abstrakty

PL

W opracowaniu podano zawartość dwóch grup cyklicznych węglowodorów nasyconych, triterpanów i steranów, w osadach dolomitu głównego z obszarów: pomorskiego, Polski centralnej oraz NW obrzeżenia Gór Świętokrzyskich w celu określenia materiału źródłowego i paleośrodowiska badanych biomarkerów (33 próbki rdzeni z 17 otworów wiertniczych). Wyniki analizy chromatograficznej (gc-ms) wykazały, iż zarówno całkowita jak i względna ilość triterpanów i steranów zmienia się znacznie w poszczególnych próbkach. Ich dystrybucja pozwala przypuszczać, że badane poziomy dolomitu głównego zawierają materię organiczną pochodzenia bakteryjnego i algowego ze znacznym udziałem materiału terygenicznego. Źródłowy materiał organiczny deponowany był w osadach ewaporacyjnych i węglanowych facji salinarnej i hipersalinarnej. Wyraźnie wyższy potencjał redox (warunki słabo utleniające) wykazują osady południowo-wschodniej części basenu cechsztyńskiego, w strefie Korabiewice-Nieświn-Opoczno.

EN

This report focusing on the 2 groups of saturated cyclic compounds (triterpanes and steranes) from the Main Dolomite sediments from Pomerania, central Poland and NW surrounding of Świętokrzyskie Mts. areas (33 samples of core material from 17 wells). The main aim of this work was determined organic source and palaeoenvironmental condition of examined biomarker. Data obtained from chromatogram analysis (gc-ms) indicate that both absolute and relative amounts of triterpanes and steranes vary greatly in particular samples. Theirs distributions suggest that investigated Main Dolomite horizons contain organic matter of bacterial and algae origin with strong terrestrial contribution. Organic source material was deposited in evaporatic and carbonate sequences in saline and hypersaline facies. Significantly higher redox potential characterized sediments from SE part of the Zechstein basin within Korabiewice-Nieświn-Opoczno area.

Słowa kluczowe

PL

paleośrodowisko; facje organiczne; prekursor; triterpany; sterany; biomarkery; dolomit główny; Pomorze; Polska centralna; Góry Świętokrzyskie

EN

palaeoenvironment; organic facies; precursor; triterpanes; steranes; biomarker; Main Dolomite; Pomerania; Central Poland; NW Świętokrzyskie Mts.

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Biuletyn Państwowego Instytutu Geologicznego
• Rocznik: 2002
• Tom: nr 402
• Strony: 51--74
• Opis fizyczny: Bibliogr. 41 poz., rys., tab., wykr.

Twórcy

autor

Grotek I.

• Państwowy Instytut Geologiczny, ul. Rakowiecka 4, 00-975 Warszawa

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