@article {1183,
	title = {Late Glacial-Holocene ecostratigraphy of the south-eastern Aegean Sea, based on plankton and pollen assemblages},
	journal = {Geo-Marine Letters},
	volume = {29},
	year = {2009},
	note = {Cited By (since 1996):23Export Date: 22 October 2014},
	month = {2009},
	pages = {249 - 267},
	abstract = {<p>Quantitative analyses of coccolithophores, planktonic\&nbsp;foraminifers, dinoflagellate cysts and pollen assemblages\&nbsp;were carried out on shallow (NS-14) and deeper (NS-40)\&nbsp;sediment cores from the south-eastern Aegean Sea. Nine\&nbsp;coccolithophore (ACE 1{\textendash}9) and nine planktonic foraminifer\&nbsp;(APFE 1{\textendash}9) ecozones, correlated with dinoflagellate cyst\&nbsp;evidence, have been defined for the last ~14.5 cal. ka.\&nbsp;Additionally, eight pollen assemblage zones (PAZ 1{\textendash}8) have\&nbsp;been recognised and correlated with the plankton ecozones.\&nbsp;Although generally consistent with existing schemes for the\&nbsp;central and eastern Mediterranean, the established high resolution\&nbsp;ecostratigraphy has led to an expanded palaeoecological\&nbsp;reconstruction of the Late Glacial{\textendash}Holocene\&nbsp;archive in the south-eastern Aegean Sea, defining two warm\&nbsp;and humid phases at 9.3{\textendash}8.6 and 7.6{\textendash}6.4 cal. ka B.P.,\&nbsp;associated with the deposition of the early Holocene sapropel\&nbsp;S1, and a third one between 5.2 and 4.2 cal. ka B.P. The high\&nbsp;sedimentation rates which characterise the study area enabled\&nbsp;the detection of even minor and brief climatic events in the\&nbsp;Aegean Sea during S1 deposition times.\&nbsp;</p>},
	url = {http://link.springer.com/article/10.1007\%2Fs00367-009-0139-5$\#$page-1},
	author = {Triantaphyllou, M.V. and Antonarakou, A. and Kouli, K. and Dimiza, M. and Kontakiotis, G. and Papanikolaou, M.D. and Ziveri, P. and Mortyn, P.G. and Lianou, V. and Lykousis, V. and Dermitzakis, M.D.}
}
