Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

Revision as of 09:41, 3 September 2013 (view source)

Revision as of 09:47, 3 September 2013 (view source)

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----Martínez-García, B., Pascual, A., Rodríguez-Lázato, J., Bodego, A., 2013. [http://www.sciencedirect.com/science/article/pii/S0278434313002458 Recent benthic foraminifera of the Basque continental shelf (Bay of Biscay, northern Spain: Oceanographic implication)]. Continental Shelf Research 66(1), 105-122.

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==BIOSTRATIGRAPHY OF THE UPPER ALBIAN-UPPER CENOMANIAN OF THE TATRA MASSIF, CARPATHIANS==

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[[Image:Acta Geologica Polonica front.jpg‎ ‎‎|left|80px|]]<font size="2">

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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.

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<font size="2">([http://www.degruyter.com/view/j/agp.2013.63.issue-2/agp-2013-0009/agp-2013-0009.xml ABSTRACT])

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----Bąk, K., Bąk, M., 2013. [http://www.degruyter.com/view/j/agp.2013.63.issue-2/agp-2013-0009/agp-2013-0009.xml Foraminiferal and radiolarian biostratigraphy of the youngest (Late Albian through Late Cenomanian) sediments of the Tatra massif, Central Western Carpathians]. Acta Geologica Polonica 63(2), 223-238f.

Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

Revision as of 09:47, 3 September 2013

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@@ Line 10: / Line 10: @@
 ----Martínez-García, B., Pascual, A., Rodríguez-Lázato, J., Bodego, A., 2013. [http://www.sciencedirect.com/science/article/pii/S0278434313002458 Recent benthic foraminifera of the Basque continental shelf (Bay of Biscay, northern Spain: Oceanographic implication)]. Continental Shelf Research 66(1), 105-122.
+==BIOSTRATIGRAPHY OF THE UPPER ALBIAN-UPPER CENOMANIAN OF THE TATRA MASSIF, CARPATHIANS==
+[[Image:Acta Geologica Polonica front.jpg‎ ‎‎|left|80px|]]<font size="2">
+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://www.degruyter.com/view/j/agp.2013.63.issue-2/agp-2013-0009/agp-2013-0009.xml ABSTRACT])
+----Bąk, K., Bąk, M., 2013. [http://www.degruyter.com/view/j/agp.2013.63.issue-2/agp-2013-0009/agp-2013-0009.xml Foraminiferal and radiolarian biostratigraphy of the youngest (Late Albian through Late Cenomanian) sediments of the Tatra massif, Central Western Carpathians]. Acta Geologica Polonica 63(2), 223-238f.