4th Symposium IGCP-506, University of Bristol, 4-8 July by Wimbledon W.A.P. (coord.) PDF

By Wimbledon W.A.P. (coord.)

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During the Subcrassum Chron multidirectional migrations of the little intensity occur. Eosphinctoceras and Subdichotomoceras are penetrated westwards until East Greenland and Britain and southwards until South-West Germany, simultaneously with eastward Pectinatites migration. Pectinatus Chron has been marked by the vast sea level rise and practically the same ammonite assemblages inhabited Boreal seas from England until Northern Siberia. Eudemic Eosphinctoceras-Subdichotomoceras lineage of Subpolar Dral became extinct near to Subcrassum/Pectinatum boundary.

Stupachenkoi, G. russiensis Ch. buckmani, Koenigi ? gr. e C. tschemyschewi, C. suevicum, G. sp. juv. ~ 32 Elatmae Herveyi ? Elatmae Subzone Keppleri Subzone Elatmae K. keppleri, K. traillensis, C. sp. Keppleri Subzone 30 C. frearsi, K. keppleri C. nordenskjoeldi, C. bodylevskyi, K. traillensis Nordenskjoeldi 29 28 ? Discus no data Apertum Apertum C. ==tl: K. vardekloeftensis, K. aff. dietli K. svalbardensis, K. aff. peramplus, P. , C. calyx e== ~ ~ Orbis =-=;:J Keuppi Hodsoni P. keuppi, K. aigii, K.

Of Milan, Milan, Italy 2 - Institut fur Geophysik & Geologie, Universitat Leipzig, Germany 3 - Dep. of Geological Sciences, University of Florida, Gainesville, USA 4 - Dep. of Earth Sciences, Univ. , 1989). , 2003) have also been documented. Integrated magneto- and calcareous nannofossil biostratigraphy across the Jurassic/Cretaceous (JIK) boundary have been independently investigated in Tethyan land sections (Torre de Busi and Foza, Southern Alps) and at Atlantic Ocean DSDP sites (534A, Blake Bahama Basin and 105, Hatteras Basin).

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4th Symposium IGCP-506, University of Bristol, 4-8 July 2007, Abstracts by Wimbledon W.A.P. (coord.)


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