Hiske Gesine Fink - E-LIB - Universität Bremen

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�� L.�pertusa�� De� Lange� et� al.,� 2008�� Abu�Zied� et� al.,� 2008;� Schmiedl� et� al.,� 2010�� Myers�and�Rohling,�2000�� Mangini� et� al.,� 2010�� L.�pertusa�� Davies�et�al.,�2010�� Brooke� and� Young,� 2009�� Brooke� and� Young,� 2009�� Brooke� and� Young,� 2009�� Davies�et�al.,�2010�� Figure�6.4:� Schematic� NW�SE� cross�section� across� the� Apulian� margin� showing� the� Santa� Maria� di� Leuca� cold�water�coral�province�in�the�Ionian�Sea.�A:�Phases�of�sustained�coral�growth�in�the�late�deglacial�and� Mid��to�Late�Holocene�that�were�associated�with�the�formation�of�Adriatic�Deep�Water�(AdDW)�resulting�in� enhanced�bottom�currents�and�a�well�ventilated�water�column.�B:�Temporary�demise�of�cold�water�corals� during�Early�Holocene�sapropel�S1�event�in�the�eastern�Mediterranean�Sea.�Anoxic�(>1800�m�water�depth)� to� dysoxic� (~500�1800� m� water� depth)� conditions� were� caused� by� enhanced� water�mass� stratification� associated�with�increased�freshwater�input,�enhanced�eutrophication�and�reduced�AdDW�formation.�
� � �� McCulloch� et� al.,� 2010�� 6.5.3 Recurrence�of�cold�water�corals� in�the�Late�Holocene� �� De�Lange�et�al.,�2008�� Frank�et�al.,�2011�� Freiwald� et� al.,� 2004�� Guinotte� et�al.,�2006�� Oschlies� et� al.,� 2008�� Stramma�et�al.,�2010�� M70�1� �� RV� Meteor� ��
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