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- W2184177209 abstract "Both in the Modern and Ancient examples coral reefs and carbonate platforms occur frequently very close to or even directly within areas of siliciclastic sedimentation. Particularly fine grained, often suspended terrigeneous influx is mostly problematic for the reef fauna due to lowering of illumination and oxygenation, increasing nutrient values or directly settling on the organims. The modern examples show that reef growth in such settings is only possible by the existence of sheltering mechanisms such as arid climate, structural and sedimentary traps or longshore currents. If not completely effective, reefs may still prosper under reduced but noticeable siliciclastic sedimentation, but both composition and diversity of the reefs changes drastically. The Ancient examples show that temporal relations are important as well: Autocyclic switches in depositional systems and especially allocyclic events such as tectonic activation/deactivation or sea level change may open and close reef windows through time. Positive effects of siliciclastic sedimentations on reef growth include the availability of suitable substrate morphologies and, in some cases, favourable increases in nutrient concentration, an aspect which appeared to be important particularly for Mesozoic coral reef growth. The Upper Jurassic coral reefs of the siliciclastically dominated Lusitanian Basin of Portugal are a perfect example for the the intimate cooperation and juxtaposition of all these controlling factors." @default.
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- W2184177209 date "1997-01-01" @default.
- W2184177209 modified "2023-09-26" @default.
- W2184177209 title "CORAL REEFS AND CARBONATE PLATFORMS WITHIN A SILICICLASTIC SETTING. GENERAL ASPECTS AND EXAMPLES FROM THE LATE JURASSIC OF PORTUGAL." @default.
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