Lower Carboniferous (Mississippian) stratigraphy of northwestern Poland : conodont, miospore and ostracod zones compared

Matyja, H.; Turnau, E.; Żbikowska, B.

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Lower Carboniferous (Mississippian) stratigraphy of northwestern Poland : conodont, miospore and ostracod zones compared

Autorzy

Matyja H. , Turnau E. , Żbikowska B.

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Warianty tytułu

Stratygrafia dolnego karbonu (missisippian) Pomorza Zachodniego : porównanie zon konodontowych, miosporowych i małżoraczkowych

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Abstrakty

Detailed stratigraphy of the Tournaisian and Viséan in western Pomerania has been established on conodonts, miospores and ostracods recovered from 25 boreholes. Miospore associations from the Tournaisian and Viséan are assigned to nine biostratigraphic units (zones and subzones) erected earlier. Three successive benthic ostracod assemblages and two sub-assemblages are distinguished for the Tournaisian. The miospore zones/subzones and the ostracod assemblages/subassemblages are correlated with the Tournaisian sandbergi, Lower crenulata, isosticha-Upper crenulata, and typicus conodont zones. Stratigraphic gap has been demonstrated at the Devonian/Carboniferous boundary, using the results of both conodont and miospore studies. The Tournaisian/ Viséan boundary has been established approximately on the first appearance of the miospore species Lycospora pusilla Somers.

Przedstawiono szczegółową stratygrafię turneju i wizenu Pomorza Zachodniego w oparciu o konodonty, miospory i małżoraczki. Materiał do badań biostratygraficznych pochodził z 25 otworów wiertniczych. Zespoły miospor z badanych utworów zaliczono do dziewięciu wcześniej wyróżnionych jednostek biostratygraficznych (zon i podzon). Dla turneju wyróżniono trzy kolejne zespoły i dwa podzespoły małżoraczków bentonicznych. Zony/podzony miosporowe i zespoły/podzespoły małżoraczkowe skorelowano z turnejskimi zonami konodontowymi sandbergi, dolna crenulata, isosticha-górna crenulata i typicus. Obecność luki stratygraficznej na granicy dewon/karbon udokumentowano na podstawie konodontów i miospor. Granica turnej/wizen została ustalona jedynie w przybliżeniu, na podstawie pierwszego pojawienia się gatunku miosporowego Lycospora pusilla Somers.

Słowa kluczowe

Tournaisian Viséan biostratigraphy conodonts miospores ostracods Western Pomerania

Wydawca

Polskie Towarzystwo Geologiczne

Czasopismo

Annales Societatis Geologorum Poloniae

Rocznik

2000

Tom

Vol. 70, No. 3-4

Strony

193--217

Opis fizyczny

Bibliogr. 75 poz., fot., rys., tab.

Twórcy

autor

Matyja H.

Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland

autor

Turnau E.

Institute of Geological Sciences, Polish Academy of Sciences, Kraków Research Center, Kraków, Senacka 1, 31-002 Kraków, Poland

autor

Żbikowska B.

Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland

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