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Aretz et al_2011.pdf - ORBi - Université de Liège

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Kölner Forum Geol. P<strong>al</strong>äont., 19 (2011)<br />

M. ARETZ, S. DELCULÉE, J. DENAYER & E. POTY (Eds.)<br />

Abstracts, 11th Symposium on Fossil Cnidaria and Sponges, <strong>Liège</strong>, August 19-29, 2011<br />

_________________________________________________________________________________________________________<br />

and recurrence rate of disturbances, such as storms or cyclones that can cause physic<strong>al</strong> damage to cor<strong>al</strong>la,<br />

but it is likely that on a given section of reef flat many nearby colonies of a given Acropora species could<br />

represent clones. Hence, disturbance events causing fragmentation and resedimentation could in some<br />

cases distribute branches of one genotype onto a colony of like genotype. Significantly, the cor<strong>al</strong> branches<br />

did not obviously appear to have been broken off of the host colony, <strong>al</strong>though that is a possibility, but they<br />

may have been transported later<strong>al</strong>ly. Regardless, they were not washed off of the colonies subsequently.<br />

Rather, they must have been held down, perhaps partly by interaction of the polyps in the un<strong>de</strong>rlying<br />

cor<strong>al</strong>lum and or the branch. That soft tissues respon<strong>de</strong>d relatively quickly to the clast is suggested by the<br />

fact that the broken end of the branches were not colonised by other benthos before they were overgrown<br />

by new cor<strong>al</strong> skel<strong>et</strong>on. Hence, soft tissues may have expan<strong>de</strong>d over the broken branch ends relatively<br />

quickly and this may help anchor the branches into place before skel<strong>et</strong><strong>al</strong> fusion occurred.<br />

Hence, we have <strong>de</strong>monstrated that live cor<strong>al</strong> branches produced during a disturbance event may come<br />

to rest on probable gen<strong>et</strong>ic clone colonies and become fused. The r<strong>et</strong>ention of branch fragments on colonies<br />

in high energy reef flat s<strong>et</strong>tings suggests an active role of cor<strong>al</strong> polyps to recognise and fuse with each<br />

other. This ability may represent an adaptation to help he<strong>al</strong> damaged colonies where branches were<br />

broken, but not removed from the host colony. Such an adaptation may be important for protecting<br />

colonies from invasion by parasites and other benthos following disturbance events.<br />

Fig. 1: A) Pebble clast of an Acropora branch encased with a cavity in another colony of Acropora sp. lined with<br />

clypeotheca (arrows). B) Photograph of fused cor<strong>al</strong> branch <strong>al</strong>ive on the reef flat of Heron Reef. C) SEM image on a<br />

polished and <strong>et</strong>ched section of large amount of thickening <strong>de</strong>posits in the broken branch.<br />

BRAGA, J.C., MARTIN, J.M. & ALCALA, B. (1990): Cor<strong>al</strong> reefs in coarse-terrigenous sedimentary environments (Upper<br />

Tortonian, Granada Basin, southern Spain). - Sedimentary Geology, 66: 135-150.<br />

HIGHSMITH, R. C. (1982): Reproduction by fragmentation in cor<strong>al</strong>s. - Marine Ecology Programm Series, 7: 207-226.<br />

HUBBARD J.A.E.B. & POCOCK Y.K. (1972): Sediment rejection by scleractinian cor<strong>al</strong>s: a key to p<strong>al</strong>eao-environment<strong>al</strong><br />

reconstruction. - Geologische Rundschau, 61: 598-626.<br />

NOTHDURFT, L.D., WEBB, G.E., LYBOLT, M.J., Price, G.J. & Jell, J. (2011): Incorporation of gravel into cor<strong>al</strong> skel<strong>et</strong>ons:<br />

Formation of clypeotheca during sediment contact. – this volume<br />

PERRY, C.T. & SMITHERS, S.G. (2009): Stabilisation of intertid<strong>al</strong> cobbles and gravels by Goniastrea aspera: an an<strong>al</strong>ogue for<br />

substrate colonisation during marine transgressions? - Cor<strong>al</strong> Reefs, 28: 805–806.<br />

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