Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA 2011 (5)"

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---- du Châtelet, E.A., Gebhardt, K., Langer, M.R., 2011. [http://www.schweizerbart.de/papers/njgpa/detail/262/76273/Coastal_pollution_monitoring_Foraminifera_as_tracers_of_environmental_perturbation_in_the_port_of_Boulogne_sur_Mer_Northern_France Coastal pollution monitoring: Foraminifera as tracers of environmental perturbation in the port of Boulogne-sur-Mer (Northern France)]. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 262 (1), 91--116.
 
---- du Châtelet, E.A., Gebhardt, K., Langer, M.R., 2011. [http://www.schweizerbart.de/papers/njgpa/detail/262/76273/Coastal_pollution_monitoring_Foraminifera_as_tracers_of_environmental_perturbation_in_the_port_of_Boulogne_sur_Mer_Northern_France Coastal pollution monitoring: Foraminifera as tracers of environmental perturbation in the port of Boulogne-sur-Mer (Northern France)]. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 262 (1), 91--116.
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==FAULT-CONTROLLED STRATIGRAPHY OF THE UPPER CRETACEOUS IN NE TUNISIA==
 
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[[Image:CretaceousResearch_front.gif|left|80px| ]]<font size="2">
 
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The palaeogeographic setting of the studied Ain Medheker section represents an Early Campanian to Early Maastrichtian moderately deep carbonate shelf to distal ramp position with high rates of hemipelagic carbonate production, periodically triggered by mass-flow processes. Syndepositional extensional tectonic processes are confirmed to the Early Campanian. Planktonic foraminifera identified in thin sections and calcareous nannofossils allow the identication of the following biozones: ''Globotruncanita elevata'', ''Contusotruncana plummerae'' (replacing former ''Globotruncana ventricosa'' Zone), ''Radotruncana calcarata'', ''Globotruncana falsostuarti'', and ''Gansserina gansseri''. The following stable C-isotope events were identified: the Santonian/Campanian boundary Event, the Mid-Campanian Event, and the Late Campanian Event. Together with further four minor isotopic events, they allow for correlation between the western and eastern realms of Tunisia. Frequently occurring turbidites were studied in detail and discussed in comparison with contourites.
 
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<font size="2">([http://www.sciencedirect.com/science/article/pii/S0195667111001303 ABSTRACT])
 
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---- Bey, S., Kuss, J., Premoli Silva, I., Negra, H.M., Gardin, S., 2011. [http://www.sciencedirect.com/science/article/pii/S0195667111001303 Fault-controlled stratigraphy of the Late Cretaceous Abiod Formation at Ain Medheker(Northeast Tunisia)]. Cretaceous Research, doi:10.1016/j.cretres.2011.09.008
 
  
  

Revision as of 13:00, 24 March 2012