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By Riding J.B., Fedorova V.A., Ilyina V.I.

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Additional resources for Jurassic and Lowermost Cretaceous Dinflagellate Cyst Biostratigraphy of the Russian Platform and Northern Siberia, Russia

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G. ) were observed rarely. 11). The most prominent dinoflageuatecyst species include Chytroeisphaeridia chytroeides, Endoscrinium galeriturn, Gonyaullrcysta jzrrassica subsp. adecta var. Furthermore,Ambonosphaera? staffwensis, Chytroeisphaeridia cerastes, Clafhroclenocystis asapha, Crussolia deflandrei, Gonyaulacysta eisenackii, Nannoceratopsis pellucida, Rhynchodiniopsis cladophora, Xigaudella aemula, Sirmiodinitrrn grossii and Stephanelytron spp. 11). 3). The range bases of several characteristic taxa confirmthat samples RP 6 and RP 5 are no older than latest Callovian.

A . • I I O .. . I BED NUMBER SAMPLE POINTS & NUMBERS {RP) VI q"pm W • • Sentusidlnium sp. (verrucate) Batiacasuhaera SDD. •• • 0 . 1 • Dinoflagellate cysts - indeterminate . . .. Chorate dinoflagellate cysts - indet. I. • m I Chlamydophorellaspp. Ste~hanelvtronscarburqhense 1 Tubotuberella rhombifonis Fromea arnphom Pareodinia SPP. - * e m • / I • 1 . 1 I Leptodinium rnirabile 1 12 21 1 Gonyaulacysta sp. (small) Gonyaulacysta spp. Sentusidiniurn creberbarbatum Stephaneiytron caytonense I • l A o Pareodinia ceratophom Aoteodinium sorr.

This genus typifies the early Oxfordian in western Europe (Riding and Thomas, 1997),and appears to be a typically Boreal genus. The stratigraphc ranges and relative proportions of dinoflagellate cysts, however, are closely comparable to coeval counterparts from western Europe; major biotic provincialism did not operate at this time (Smelror, 1993). adecta var. 13). The range top of Gonyaulacysta centriconnata was observed in sample RP 29; this datum is consistent with western Europe (Riding, 1983b; Riding and Thomas, 1992).

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Jurassic and Lowermost Cretaceous Dinflagellate Cyst Biostratigraphy of the Russian Platform and Northern Siberia, Russia by Riding J.B., Fedorova V.A., Ilyina V.I.


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