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

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Maria Marino
Franck Bassinot
Adele Bertini
Salvatore Gallicchio
Angela Girone
Timothy Herbert
Patrizia Maiorano
Sebastien Nomade
Paola Petrosino
Ornella Quivelli
Teresa Rodrigues
Francesco Toti
Neri Ciaranfi

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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How to Cite
Marino, Maria, Franck Bassinot, Adele Bertini, Salvatore Gallicchio, Angela Girone, Timothy Herbert, Patrizia Maiorano, et al. , trans. 2018. “THE CLIMATE VARIABILITY DURING MARINE ISOTOPE STAGE 19: EVIDENCES FROM A WEST-EAST MEDITERRANEAN TRANSECT”. Alpine and Mediterranean Quaternary 31 (May): 151-54. https://amq.aiqua.it/index.php/amq/article/view/206.
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How to Cite

Marino, Maria, Franck Bassinot, Adele Bertini, Salvatore Gallicchio, Angela Girone, Timothy Herbert, Patrizia Maiorano, et al. , trans. 2018. “THE CLIMATE VARIABILITY DURING MARINE ISOTOPE STAGE 19: EVIDENCES FROM A WEST-EAST MEDITERRANEAN TRANSECT”. Alpine and Mediterranean Quaternary 31 (May): 151-54. https://amq.aiqua.it/index.php/amq/article/view/206.