Articles | Volume 11, issue 3
https://doi.org/10.5194/cp-11-509-2015
https://doi.org/10.5194/cp-11-509-2015
Research article
 | 
24 Mar 2015
Research article |  | 24 Mar 2015

A high-resolution δ18O record and Mediterranean climate variability

C. Taricco, G. Vivaldo, S. Alessio, S. Rubinetti, and S. Mancuso

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Carla Taricco on behalf of the Authors (27 Jan 2015)  Author's response 
ED: Publish as is (13 Feb 2015) by Nerilie Abram
AR by Carla Taricco on behalf of the Authors (18 Feb 2015)
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Short summary
The key to gaining information on climate over the last millennia is the study of proxy records in ice and sediment cores, trees, etc. We measured the oxygen isotopic ratio in planktonic foraminifera of a high-resolution, well-dated central Mediterranean core. The comparison between the variability detected in this core and that characterizing the Northern Hemisphere allows for local and global (hemispheric) climate variations to be distinguished.