Calcareous nannofossil assemblages at core KC01B (Ionian Sea) through oxygen Marine Isotope Stages 9-13

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Published: Jan 14, 2011
DOI: https://doi.org/10.26382/
Keywords:
calcareous nannofossils, Ionian Sea, core KC01B, MIS 9-13

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Francesca Tarantino
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari “Aldo Moro”, Bari
Patrizia Maiorano
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari “Aldo Moro”, Bari
Maria Marino
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari “Aldo Moro”, Bari
Gert J. De Lange
Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University
Lucas Lourens
Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University

Abstract

Tarantino F. et al., Calcareous nannofossil assemblages at core KC01B (Ionian Sea) through oxygen Marine Isotope Stages 9-13 (IT ISSN 0394-3356, 2011).  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.

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How to Cite
Tarantino, Francesca, Patrizia Maiorano, Maria Marino, Gert J. De Lange, and Lucas Lourens , trans. 2011. “Calcareous Nannofossil Assemblages at Core KC01B (Ionian Sea) through Oxygen Marine Isotope Stages 9-13”. Alpine and Mediterranean Quaternary 24 (Extended Abstract): 219-20. https://doi.org/10.26382/.
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Vol. 24 No. Extended Abstract (2011): IL QUATERNARIO
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How to Cite

Tarantino, Francesca, Patrizia Maiorano, Maria Marino, Gert J. De Lange, and Lucas Lourens , trans. 2011. “Calcareous Nannofossil Assemblages at Core KC01B (Ionian Sea) through Oxygen Marine Isotope Stages 9-13”. Alpine and Mediterranean Quaternary 24 (Extended Abstract): 219-20. https://doi.org/10.26382/.