Paleoclimate of the Southern Adriatic Sea region during the ‘Medieval Climate Anomaly’ reflected by organic walled dinoflagellate cysts
To obtain insight into the character and forcing of southern Italian climate change during the ‘Medieval Climate Anomaly’ (c. ad 900–1200), marine sediments deposited between ad 990 and 1200 from the Gulf of Taranto have been analyzed for their dinoflagellate cyst content with a 3.5 yr resolution. T...
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Veröffentlicht in: | Holocene (Sevenoaks) 2013-05, Vol.23 (5), p.645-655 |
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