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Strefy faunistyczne westfalu A i B w Lubelskim Zagłębiu Węglowym

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3. C a I v er· M. A. - Westfalian of Britain.

se

Intern. Congr. Stratigr. Geol. Carbo Sheffield, 11967.

4. Dembowski Z. - Utwory westfalu w Lu-belskim Zagl~biu W~lowym. Kwart. geol., 1968, nr 2.

5.

Ii

e m bow ski Z., P 0 r z y c k i J. - Wyniki prac geologicrLr.lo-poszukiwawczych prowadzonych w nowo odkrytym Lubelskim Zagl~biu W~g1o­

wym. Prz. geol., 1967, nr 1.

6. Ko r e j wo K. - Wyniki wiercenia w Chelmie - karbon. Biu!. IG, nr 165.

7. K 0 r e j w 0 K., Tell er L. - Stratygrafia kar-bonu zachodniej . cz~~ci niecki lubelskiej. Acta geol. pol., 1968, vol. 18, nr 1.

SUMMARY

Fauna from 19 bore holes made in the Lublin Coal Basin (Fig. 1), worked out by the present aut-hors, allowed the deposits of Westphalian A and B to be distinguished within the Carboniferous forma-tions examined. These deposits reveal some correla-tive horizons, bearing both freshwater and marine fauna representatives (Table I). Characteristic assem-blages of freshwater pelecypods were a basis to dis-tinguish the following faunistic zones:

Lenisulcata zone - Lowel Westphalian A. Within this 'ZOne two main horizons occur - a marine hori-zon at the bottom of the Westphalian A deposits and an overlying -freshwater. horizon with Carbonicola exporrecta;

Communis zone - middle part of the Westpha-lian A. The zone is characterized by the occurrence of three horizons with freshwa.ter fauna and by a marine horizon. The lowermost freshwater ·horizon has been called by the presenlt authors the Carbo-nicola pseudorobusta h{)rizon;

Mediolaris zone - the uppermost Westphalian A and B. In this zone a boundary marine horizon with DunbareUa papyracea occurs, distinguished

al-so as the uppermost horizon of the Westphalian A. Just below this horizon and above it are found· ho-rizons with freshwater fauna. The species assembla-ge of the wreshwater pelecypods· found to .overlie the horizon with Dunbarella. papyracea is cha,racte-ristic of the Westfalian B(Table II). .

8. K 0 r e j w 0 K. - Stratigraphy and palaeogeo-graphy of the Namurien in the Polish Lowland. Ibidem, 1969, vo!. 119, nr 4.

9. Mu

s

i all... - Opracowanie rodzaju Pterinopec-!ten z karbonu lubelskiego. Arch. Oddz. G6rno~1.

IG, 1968.

10. Tab 0 r M. - Fauna karbonikolowa z karbonu lubelskiego. Arch. IG, 1969 ..

11. Tab 0 r M. - Opracowanie Naiadites z karbonu lubelskiego. Ibidem, 1970.

12. Trueman A. E., Weir J. - A monograph of British Carboniferous non marine lamelli-branchs. Palaeont. Soc., London, 1946-1956.

PE310ME

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npe-~eJIax 9TOA 3{)HbI SaJIeraIOT ~Ba OCHOBHbIX ropHSOHTa - MOpcKoli: oopJ!lSOHT B IIO~OJlllBe BecT<l>aJIJI A, a TaKlKe

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30Ha Modiolaris - CaMbIfi BbIClIIHA BecTcPam. A H BecTcPam. B. B 9TOH 30He SaJIeraeT CaMbIfi BepXHHA B BecTcPaJIe A, H O~HOBPeMeHHO norpa~, MOP-CKOjj; roPHSOHT c Dunbarella papyracea, HeIIOCpep;-CTBeHHO :IIO~ HHM, a TalOKe H8~ HHM SaJIeraIOT ropJI-SOHTbI c npecHOBOP;Holi: cPaYBoli:. BH,n;!JB1UI rp~a

npecHOBO;I{HbIX neJIHQHDO~, SaJ.IeraIOI.QHX ~ ropJ:lSOH-TOM c· Dunbarella papyracea JlBJIHeTCJI xapamepHojj;

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