TRILOBITES AS ARTHROPODS: THE IMPLICATIONS OF THE ARTHRODIAL MEMBRANE FOR TRILOBITE TAPHONOMY
There are several implications of this. First, the discrete trilobite sclerites we observe in the fossil record were actually linked by the unmineralized bit of exoskeleton called the arthrodial membrane in life. Disarticulation of the mineralized exoskeletal sclerites, after death or molting, necessarily requires degradation of the chitinous arthrodial membrane first. Second, as observed by Seilacher (2007), the ventral chitinous membrane of trilobites would have also required molting in order to grow. How that would have been accomplished in light of proposed trilobite ‘molt configurations’ is not completely clear, though it may have involved a biphasic molting process.
Articulated trilobite remains are used as indicators of calm sedimentary environments. However, the chitinous exoskeleton of freshly dead/molted remains is surprisingly resistant to transport. As such, they should be interpreted in light of other sedimentological evidence.