Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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{{Recent Publications on Foraminifera Navigation}}<font size="2"> | {{Recent Publications on Foraminifera Navigation}}<font size="2"> | ||
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| + | ==MULTIDISCIPLINARY STUDY OF RARELY RECOVERED PARTS OF DEEP-SEA SANTONIAN-CAMPANIAN TRANSITION== | ||
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| + | The Cretaceous deep-sea record of the Santonian–Campanian transition is commonly interrupted by an extensive unconformity (representing <10 Myr of hiatus). The resultant palaeoceanographic gap can now be partly bridged by a recent short core of pelagic ooze from Shatsky Rise (Integrated Ocean Drilling Program (IODP) Site U1348), with precise multidisciplinary age constraints developed herein. New oxygen isotope data from very well-preserved benthic foraminifera, together with accurately compiled comparable benthic data from previous Pacific deep-sea sections, exhibit a large (c. +1‰) early Campanian shift. We propose the Santonian–Campanian climatic transition was not gradual but was the first major cooling step after sustained mid-Cretaceous hothouse conditions. | ||
| + | <font size="2">([http://jgs.lyellcollection.org/content/170/3/381.abstract ABSTRACT]) | ||
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| + | ----Ando, A., Woodard, S.C., Evans, H.F., Littler, K., Herrmann, S., Macleod, K.G., Kim, S., Khim, B.-K., Robinson, S.A. and Huber, B.T., 2013. [http://jgs.lyellcollection.org/content/170/3/381.abstract An emerging palaeoceanographic ‘missing link’: multidisciplinary study of rarely recovered parts of deep-sea Santonian–Campanian transition from Shatsky Rise]. Journal of the Geological Society 170 (5), 381-384. | ||
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==BIOSTRATIGRAPHY OF THE YOUNGEST SEDIMENTS OF THE TATRA MASSIF, CENTRAL WESTERN CARPATHIANS== | ==BIOSTRATIGRAPHY OF THE YOUNGEST SEDIMENTS OF THE TATRA MASSIF, CENTRAL WESTERN CARPATHIANS== | ||
