@article {3777,
	title = {Preliminary results of high resolution paleoceanography during sapropel S1 deposition: benthic foraminiferal assemblages (South Limnos basin, North Aegean Sea)},
	journal = {Bulletin of the Geological Society of Greece},
	volume = {XLVII},
	year = {2013},
	pages = {194-203},
	abstract = {<p>The paleoenviromental conditions during the depositional interval of sapropel S1 in\&nbsp;the northeastern Aegean (gravity core M-4, length 2.53 m; south Limnos basin) are\&nbsp;studied based on quantitative micropaleontological (benthic and planktonic foraminifera)\&nbsp;and geochemical (OC, δ13Corg) analyses. Special feature of core M-4 is\&nbsp;the thickness of S1 layer (96 cm). Our study points that sapropelic layer S1a has\&nbsp;been deposited in more dysoxic and warmer conditions in respect to S1b. Both primary\&nbsp;productivity and preservation of organic material are more intense during the\&nbsp;lower part of S1. An interruption of the sapropelic conditions at 8.0 Ka BP which is\&nbsp;mainly characterized by the increase of agglutinated foraminiferal forms confirms\&nbsp;both higher oxygen bottom conditions and freshwater input.</p>},
	url = {http://www.geosociety.gr/index.php/publications-gr/2000/197-xlvii-13o-5-8-2013$\#$V1},
	author = {Kostopoulou, S., and Triantaphyllou, M., and Dimiza, M., and Gogou, A., and Bouloubassi, I., and Roussakis, G., and Parinos, C., and Diamantopoulou, An., and Geraga, M., and Lykousis, V.,}
}
