The study of recent echinoids from the Red Sea has shown that actuopalaeontological investigations have importantimplications for at least two major aspects of palaeonenvironmental interpretations: 1) taphonomic processes and 2) the distribution of sea urchins with respect to environmental parameters. An important aspect of actuopalaeontological studies based on experimental as well as field observations, concerns taphonomic processes. It can be shown that a number of agents including predation, transport, encrustation etc. differentially affect the fossilization potential of echinoid species. The extent of these processes are both facies dependent as well being influenced by the inherent skeletal properties of the echinoid skeleton. The distribution of echinoids is controlled by a number of environmental factors including substrate characteristics, nutrient supply, and exposure to differential current conditions. Actuopalaeontological studies can elucidate these dependencies especially in conjunction with detailed facies and sediment analyses. The distributions of irregular echinoids are shown to be tightly constrained by grain size characteristics of the sediment. Cryptic habitats and patchy distributions lead to difficulties in quantifying living echinoids over large areas. The instability of the echinoid test complicates the comparison of echinoid biocoenosis and taphocoenosis. These problems are seen to constitute the main limits of actuopalaeontological investigations.
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