Abstract
Calcareous nannofossil assemblages from deep sea core KC01B in Ionian Sea have been analysed in high sample resolution (0.6-0.8 kyr) through the Pleistocene Marine Isotope Stages (MIS) 9-13 interval, which includes significant climate changes during the known Mid-Brunhes Event. Collected data show complex relationships between coccolithophores modification and environmental parameters.
Original language | English |
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Pages (from-to) | 219-220 |
Number of pages | 2 |
Journal | Alpine and Mediterranean Quaternary |
Volume | 24 |
Publication status | Published - 2011 |
Keywords
- Calcareous nannofossils
- Core KC01B
- Ionian Sea
- MIS 9-13