Short-term progressive early diagenesis in density bands of recent corals:Porites Colonies,Mauritius Island,Indian Ocean

Summary The growth history of some recentPorites colonies of Mauritius Island (Indian Ocean) was dated by sclerochronological methods. Couples of high-density and low-density bands represent the annual growth rate of the corals and allow the growth pattern of every year in the corallum to be counted. The growth and structure of the skeletons ofPorites solida andPorites lutea were investigated. Older parts of the aragonitic skeleton in these 10 to 20 year old corals show various secondary microstructures resulting from alterations and thickenings of the elements of the skeleton. The primary needle-like aragonite crystals are absent in older parts of the corallum and blocky aragonitic cements can occur. Pores and primary skeletal elements are overgrown by new microstructures. These microstructures are caused by secondary cementation and exhibit frontal zones (Stirnzonen), zigzag-like and pseudolamellar-structures. The lamellar structures can be compared with similar structures in the exoskeleton of some Rugosa. A very short early diagenesis within the recent corals is responsible for the thickening and alteration of skeletal elements. It occurs only 4 to 5 years after the formation of the skeleton and tends to increase in importance in older parts of the corallum. Nevertheless, there is no proof for any alteration of aragonite to calcite.