Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

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==SANTONIAN-CAMPANIAN PLANKTONIC FORAMINIFERA SPECIES DEPTH ECOLOGY AND PALEOCEANOGRAPHIC INFERENCES==
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[[Image:Marine_Micropaleontology_Front.gif|left|80px|]]<font size="2">
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The Santonian–Campanian interval is of particular interest as it encompasses a cooling trend after the Late Cretaceous greenhouse maximum warmth of the Turonian as well as a possibly related major faunal turnover among planktonic foraminifera. The recovery of pristinely preserved planktonic foraminifera from Santonian–Campanian sequences in southeastern Tanzania allows examination of faunal changes and documentation of species-specific stable isotope (δ<sup>13</sup>C and δ<sup>18</sup>O) signatures. These isotopic data are ideal for inferring species paleoecological preferences and for tracing major paleoceanographic changes. This study reports the first δ<sup>18</sup>O and δ<sup>13</sup>C data generated on “glassy” specimens of ''Marginotruncana coronata'', ''M. undulata'', ''M. marginata'', and ''M. pseudolinneiana'' and ''Sigalia carpatica''. Additional results from Shatsky Rise (Ocean Drilling Program Leg 198, Hole 1210B) and Exmouth Plateau (ODP Leg 122, Hole 762C) provide geographic control on species habitat preferences and paleoceanographic context. ......
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<font size="2">([http://www.sciencedirect.com/science/article/pii/S0377839813000777# ABSTRACT])
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----Falzoni, F., Petrizzo, M.R., MacLeod, K.G., Huber, B., 2013. [http://www.sciencedirect.com/science/article/pii/S0377839813000777# Santonian–Campanian planktonic foraminifera from Tanzania, Shatsky Rise and Exmouth Plateau: Species depth ecology and paleoceanographic inferences]. Marine Micropaleontology 103, 15-29.
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==DO FORAMINIFERA MIRROR DIVERSITY AND DISTRIBUTION PATTERNS OF MACROBENTHIC FAUNA IN AN ARCTIC FJORD?==
 
==DO FORAMINIFERA MIRROR DIVERSITY AND DISTRIBUTION PATTERNS OF MACROBENTHIC FAUNA IN AN ARCTIC FJORD?==

Revision as of 10:06, 5 September 2013