caa a22 4500 475827554 CHVBK 20180406123832.0 cr unu---uuuuu 170329e20000901xx s 000 0 eng 10.1007/s005310000078 doi (NATIONALLICENCE)springer-10.1007/s005310000078 Origins and development of Holocene coral reefs: a revisited model based on reef boreholes in the Seychelles, Indian Ocean [Elektronische Daten] [C. J. R. Braithwaite, L. F. Montaggioni, G. F. Camoin, H. Dalmasso, W. C. Dullo, A. Mangini]  Until recently, concepts of coral reef growth and accumulation have been predominantly based on a Darwinian model. In this, the upwards and outwards growth of a reef core (a coral framework) takes place over a foreslope consisting of reef talus, with the simultaneous filling of the back-reef lagoon by reef-derived debris. The principal adaptations of this pattern relate to the influence of relative changes in sea level and commonly ignore oceanographic factors such as storm frequency and severity. Boreholes through the outer edge of a fringing reef in the Seychelles, western Indian Ocean, reveal a record of Holocene sediment accumulation first established approximately 8 ka ago. Faunal and floral associations show that growth of this body began in relatively deep water but that this shallowed to <5 m within 1 ka. Subsequent accumulation was of "keep-up” style but, as the rate of sea-level rise slowed, shoaling became more frequent and aggradation was limited by reducing accommodation space. Constructional facies are characterised either by massive corals, including Leptastrea, Porites and faviids, or by branching corals, typically Acropora of the danai-robusta group. Coral surfaces may be encrusted by red algae, foraminifera and vermetids, and are commonly bored by filamentous algae, clionids and molluscs. However, detrital facies are volumetrically dominant, and the paucity of a constructional framework requires a re-evaluation of models of reef accretion. New models relate the geometry of accretion to the interplay between extreme storm events and fairweather hydrodynamic conditions. These suggest that a contiguous framework forms in areas of moderate fairweather energy without extreme storm events. Severe storms destroy the continuity of reef structures and generate increasing volumes of coarse detritus. Low storm severity, coupled with low fairweather hydrodynamic energy, may promote the accumulation of fine-grained reef-derived sediments that inhibit framework growth. While ecology reflects year-by-year sea conditions, lithology and structure are controlled by exceptional storms, with the effects of changing sea level superimposed. Springer-Verlag Berlin Heidelberg, 2000 Key words Reef structure nationallicence Reef models nationallicence Reef boreholes nationallicence Influence of storms nationallicence Seychelles nationallicence Braithwaite C. J. R. Division of Earth Sciences, Gregory Building, The University of Glasgow, Lilybank Gardens, Glasgow G12 8QQ, UK e-mail: c.braithwaite@earthsci.gla.ac.uk Tel.: +44-141-3305449 Fax: +44-141-3304817, GB aut Montaggioni L. F. Université de Provence, Centre de Sédimentologie-Paleontologie, URA 1208 CNRS, Place Victor Hugo, F-13331 Marseille cédex 3, France, FR aut Camoin G. F. Centre Européen d'Enseignement et de Recherche en Géosciences de l'Environnement, Europôle de l'Arbois, B. P. 80, F-13545 Aix-en-Provence cédex 4, France, FR aut Dalmasso H. Université de Provence, Centre de Sédimentologie-Paleontologie, URA 1208 CNRS, Place Victor Hugo, F-13331 Marseille cédex 3, France, FR aut Dullo W. C. GEOMAR, Research Center for Geosciences, Wischhofstrasse 1-3, D-24148 Kiel, Germany, DE aut Mangini A. Heidelberger Akademie der Wissenschaften, Radiometrische Altersbestimmung von Wasser und Sedimenten, Im Neuenheimer Feld 366, D-69120 Heidelberg, Germany, DE aut https://doi.org/10.1007/s005310000078 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/s005310000078 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Braithwaite C. J. R. Division of Earth Sciences, Gregory Building, The University of Glasgow, Lilybank Gardens, Glasgow G12 8QQ, UK e-mail: c.braithwaite@earthsci.gla.ac.uk Tel.: +44-141-3305449 Fax: +44-141-3304817, GB aut NATIONALLICENCE 700 1- Montaggioni L. F. Université de Provence, Centre de Sédimentologie-Paleontologie, URA 1208 CNRS, Place Victor Hugo, F-13331 Marseille cédex 3, France, FR aut NATIONALLICENCE 700 1- Camoin G. F. Centre Européen d'Enseignement et de Recherche en Géosciences de l'Environnement, Europôle de l'Arbois, B. P. 80, F-13545 Aix-en-Provence cédex 4, France, FR aut NATIONALLICENCE 700 1- Dalmasso H. Université de Provence, Centre de Sédimentologie-Paleontologie, URA 1208 CNRS, Place Victor Hugo, F-13331 Marseille cédex 3, France, FR aut NATIONALLICENCE 700 1- Dullo W. C. GEOMAR, Research Center for Geosciences, Wischhofstrasse 1-3, D-24148 Kiel, Germany, DE aut NATIONALLICENCE 700 1- Mangini A. Heidelberger Akademie der Wissenschaften, Radiometrische Altersbestimmung von Wasser und Sedimenten, Im Neuenheimer Feld 366, D-69120 Heidelberg, Germany, DE aut Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer