THE CLIMATE VARIABILITY DURING MARINE ISOTOPE STAGE 19: EVIDENCES FROM A WEST-EAST MEDITERRANEAN TRANSECT

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Published: 2018-05-17
Keywords:
MIS 19, calcareous plankton, SST, pollen, stable oxygen and carbon isotopes, Mediterranean

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Maria Marino
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy
Franck Bassinot
Laboratoire des Sciences du Climat et de l’Environnement, Gif-sur-Yvette, France
Adele Bertini
Dipartimento di Scienze della Terra, Università degli Studi di Firenze, Firenze, Italy
Salvatore Gallicchio
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy
Angela Girone
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy
Timothy Herbert
4 Department of Earth, Environmental & Planetary Sciences, Brown University, Providence, USA
Patrizia Maiorano
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy
Sebastien Nomade
Laboratoire des Sciences du Climat et de l’Environnement, Gif-sur-Yvette, France
Paola Petrosino
Dipartimento di Scienze della Terra dell'Ambiente e delle Risorse, Università degli Studi di Napoli Federico II, Napoli, Italy
Ornella Quivelli
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy
Teresa Rodrigues
Instituto Portugues do Mar e da Atmosfera, Lisboa, Portugal
Francesco Toti
Dipartimento di Scienze della Terra, Università degli Studi di Firenze, Firenze, Italy
Neri Ciaranfi
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Bari, Italy

Abstract

New high temporal resolution data on calcareous nannofossil and planktonic foraminifera assemblages, alkenone-derived sea surface temperature and stable oxygen and carbon isotopes are acquired on the Montalbano Ideale section (southern Italy) and at the Ocean Drilling Program (ODP) sites 975 and 976 through Marine Isotope Stages (MIS) 20-18. Results describe accurate climate pattern and distinct orbital-suborbital up to millennia-scale oscillations across the investigated interval. MIS 19

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Vol. 31 (2018): "Quaternary: Past, Present, Future - AIQUA Conference 2018"

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How to Cite

THE CLIMATE VARIABILITY DURING MARINE ISOTOPE STAGE 19: EVIDENCES FROM A WEST-EAST MEDITERRANEAN TRANSECT (M. Marino, F. Bassinot, A. Bertini, S. Gallicchio, A. Girone, T. Herbert, P. Maiorano, S. Nomade, P. Petrosino, O. Quivelli, T. Rodrigues, F. Toti, & N. Ciaranfi , Trans.). (2018). Alpine and Mediterranean Quaternary, 31, 151-154. https://amq.aiqua.it/index.php/amq/article/view/206