26.10.2012 Views

Hiske Gesine Fink - E-LIB - Universität Bremen

Hiske Gesine Fink - E-LIB - Universität Bremen

Hiske Gesine Fink - E-LIB - Universität Bremen

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

��������������������������������������������������������� �<br />

Figure�8.3:�Schematic�W�E�cross�section�across�the Mediterranean�Sea�(see�(a) for�profile)�showing�phases�<br />

of�cold�water�coral�growth�and�the�prevailing�environmental�settings�during�the�last�15�ka.�Coloured�bars�<br />

indicate�cold�water�coral�growth�and�the�sampling�depth�of�the�dated�cold�water�corals�(based�on�the�coral�<br />

age� compilation� shown� in� Fig.� 8.2).� Dashed� bars� indicate� especially� wide� depth� ranges� resulting� from�<br />

dredged�samples�hindering�the�assignment�of�a�certain�sampling�depth�to�individual�corals.�Colour�code�is�<br />

the�same�as�in�Figures�8.1�and�8.2�and�indicates�the�sampling�region.�Schematic�foraminifers�indicate�the�<br />

degree�of�marine�productivity�in�the�surface�waters.�Displayed�are�the�main�water�masses:�Blue�arrows:�<br />

Surface�water�circulation�(Modified�Atlantic�Water�(MAW)�and�fresh�water).�Dashed�dotted�black�arrows:�<br />

Intermediate� water� circulation� (Levantine� Intermediate� Water� (LIW)� and� Winter� Intermediate� Water�<br />

(WIW)).� Grey�arrows:� Deep�water� circulation� (Eastern� Mediterranean� Deep�Water�(EMDW)� and� Western�<br />

Mediterranean� Deep� Water� (WMDW).� Dotted� black� arrows:� Mediterranean� Outflow� Water� (MOW);�<br />

continued�on�next�page�<br />

���

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!