Hiske Gesine Fink - E-LIB - Universität Bremen

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�� Malinverno�et�al.,�2010;� McCulloch�et�al.,�2010�� 6.5.2 Impact�of�decreasing�bottom� water�oxygenation� �� Freiwald�et�al.,�2009�� Lophelia� �� Davies� et� al.,� 2008�� Figure�6.2:� Sediment� cores� GeoB� 11186�1� (A) and� GeoB� 11185�1� (B�E). Both� cores� reveal� two� intervals� containing�cold�water�corals�(growth�period�(gp)�a�and�b;�coral�symbols,�diagonal�hatched)�interrupted�by�a� coral�barren�layer�(cb).�Numbers�give�ages�of�corals�and�planktonic�foraminifera�(indicated�by�diamonds)� [cal�kyr�BP].�Sediments�deposited�during�sapropel�S1�event�are�shaded�in�grey.�A�and�B:�Mean�grain�sizes.�C:� Bottom�water�oxygen�concentration�estimated�from�the�abundance�of�deep�infaunal�benthic�foraminifera� after� Jorissen� et� al.[2007].� D:� Oxygen�Index� calculated� after� Schmiedl� et� al.� [2003]� E:� Content� of� organic� carbon.��
� � �� Figure�6.3:�Holocene�cold�water�coral�development�in�the�eastern�Mediterranean�Sea.�Coral�ages�of�cores� GeoB� 11185�1� (triangles)� and� GeoB� 11186�1� (diamonds)� (Table�6.1).� Additional� coral� ages� (L.�pertusa,� M.�oculata)�reported�for�the�eastern�Mediterranean�Sea�(crosses:�McCulloch�et�al.[2010];�dots:�Malinverno� et�al.�[2010]).�Indicated�are�the�cold�water�coral�growth�periods�(gp)�a�and�b�(diagonal�hatched)�and�the� period�of�sapropel�S1�formation�[shade�in�grey;�after�De�Lange�et�al.,�2008].�� L.�pertusa�� Dodds� et� al.,� 2007�� De�Lange�et�al.,�2008�� Rohling,� 1994;� Kallel� et� al.,� 2000;� De� Lange� et� al.,� 2008�� Abu�Zied� et� al.,� 2008;� Schmiedl� et� al.,� 2010�� Rohling,� 1994;� De� Lange� et� al.,�2008;�Geraga�et�al.,�2008�� De�Lange�et�al.,�2008�� Emeis�et�al.,�2000;�Giunta�et�al.,�2003�� Budillon� et� al.,� 2010�� Brayshaw�et�al.,�2011�� L.�pertusa�� Freiwald�et�al.,�2009;�Budillon�et�al.,�2010�� L.�pertusa��
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Hiske Gesine Fink - E-LIB - Universität Bremen

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