首页 | 本学科首页   官方微博 | 高级检索  
   检索      


Temporal variations of macroborers in massive Porites lobata on Moorea,French Polynesia
Authors:M Peyrot-Clausade  P Hutchings  G Richard
Institution:(1) UA 41, Centre d'Oceanologie de Marseille, F-13007 Marseille, France;(2) Centre de l'Environnement de Moorea, Museum National d'Histoire Naturelle et Ecole Pratique des Hautes Etudes, Moorea, French Polynesia;(3) The Australian Museum, P.O. Box A285, 2000 Sydney, NSW, Australia;(4) UA 1453, Ecole Pratique des Hautes Etudes, 55 Rue de Buffon, F-75005 Paris, France
Abstract:Massive colonies of Porites lobata on the barrier reef of Tiahura, Moorea, can be divided into four categories: living colonies, colonies consisting of 50% live coral and 50% dead skeleton, 100% dead coral and colonies which have been reduced to a basal plate. Replicate samples of each of these colony types were collected in the same vicinity of the barrier reef during October 1987. The macroborers were extracted, identified, counted and their volumes determined by displacement. Kruskal-Wallis tests showed that three different boring communities occur within these four categories of Porites colonies. Live colonies are characterised by only 3 species, the bivalve, Lithophaga laevigata; the vermetid Dendropoma maximun; and the non boring serpulid polychaete Spirobranchus. The completely dead colonies contain up to 17 boring species, with five to six individuals per 100 cm. Sipunculans are the dominant bioeroders with the most abundant species being Aspidosiphon elegans, sp A and sp B. Colonies of Porites which have been reduced to basal plates contain up to 18 boring species of which the bivalve Lithophaga hanleyana and the sipunculan Aspidosiphon sp. B are the most abundant.The cumulative volume of CaCO3 lost by boring activity increases from 0.1 cm3 per 100 cm3 in a completely dead Porites colony to 1.4 cm3 per 100 cm3 in the residual basal plates of Porites. These can be extrapolated to minimum losses of 14.2 kg m-3. We suggest that rates of boring increase with the time which has elapsed since the death of the colony and the dominant agents of boring also change with increasing age of the coral structure. There are significant additional losses of 5.25 kg m-3 CaCO3 caused by grazing echinoids and scarids.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号