Hiske Gesine Fink - E-LIB - Universität Bremen

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�� 7.5.1 Morphology�and�development�of� coral�mounds�and�ridges�in�the� Melilla�Coral�Province� �� Comas� et� al.,�2009�� De�Mol�et�al.,�2002;�Wheeler�et�al.,�2007�� Foubert� et� al.,� 2008;� Wienberg�et�al.,�2009��Colman�et� al.,�2005��Grasmueck�et� al.,� 2006�� BR�� Ammar� et� al.,� 2007;� Martínez�García� et� al.,� 2011�� Comas�et� al.,�2009�� Kano� et� al.,� 2007�� BR�� BR�� BR� �� BR�� BR�� BR� �� BR� �� BR�� Frank�et�al.,� 2009�� BR�� Huvenne� et�al.,�2009��
� � �� Figure�7.3:�Dataset�of�multi�proxy�analyses�of�the�off�mound�sediment�core�GeoB 13731�1�from�the�Melilla� Coral�Province�(MCP)�off�northern�Morocco�compared�with�cold�water�coral�ages:�(a)�radiocarbon�ages�of� coral� fragments� collected� from� sediment� cores� (filled� diamonds)� and� surface� coral� samples� (open� diamonds);�older�corals�(e.g.�>�13.5�ka)�might�occur�beyond�the�reach�of�the�available�sediment�cores;�(b)� Ca/(Ca+Fe)�ratio;�(c)�Si/(Si+Al)�ratio;�(d)�mean�grain�size�[μm]�of�the�terrigenous�fraction;�(e)�sea�surface� temperatures�(SST)�[°C]�from�Alboran�Sea�sediment�core�MD�95�2043�[Cacho�et�al.,�1999];�(f)�stable�oxygen� isotope�of�the�NGRIP�ice�core�record�[NGRIP�Members,�2004];�(g)�stable�oxygen�isotope�record�[‰�PDB];� reverse� axis;� (h)� estimated� sedimentation�rate� [cm�ka �1 ].� Highlighted� in� gray�are� periods� of� coral�growth.� Indicated�is�the�period�of�ORL1�formation�[14.5�8.2�ka�after�Jimenez�Espejo�et�al.,�2008].� �� Huvenne� et� al.,�2009��
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