Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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| + | ==BIOSTRATIGRAPHY OF THE YOUNGEST SEDIMENTS OF THE TATRA MASSIF, CENTRAL WESTERN CARPATHIANS== | ||
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| + | The foraminiferal and radiolarian biostratigraphy of selected sections of the Zabijak Formation, the youngest sediments of the Tatra massif (Central Western Carpathians), have been studied. Benthic foraminifers, mainly agglutinated species, occur abundantly and continuously throughout the studied succession, while planktic foraminifers are generally sparse. Five planktic and two benthic foraminiferal zones have been recognized. The marly part of the Zabijak Formation comprises the ''Pseudothalmanninella ticinensis'' (Upper Albian) through the ''Rotalipora cushmani'' (Upper Cenomanian) planktic foraminiferal zones, and the ''Haplophragmoides nonioninoides'' and ''Bulbobaculites problematicus'' benthic foraminiferal zones. The radiolarians were recognized exclusively in the Lower Cenomanian part of the formation. | ||
| + | <font size="2">([http://agp.org.pl/table/abstracts/63-2.htm ABSTRACT]) | ||
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| + | ----Bąk, K. and Bąk, M., 2013. [http://agp.org.pl/table/abstracts/63-2.htm Foraminiferal and radiolarian biostratigraphy of the youngest (Late Albian through Late Cenomanian) sediments of the Tatra massif, Central Western Carpathians]. Acta Geologica Polonica 63, 223–237. | ||
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==NEW SUPRAORDINAL CLASSIFICATION OF FORAMINIFERA: MOLECULES MEET MORPHOLOGY== | ==NEW SUPRAORDINAL CLASSIFICATION OF FORAMINIFERA: MOLECULES MEET MORPHOLOGY== | ||
