Abstract

Foraminifera are unicellular organisms which are widespread especially marine environments. They produce protective shells (called tests) around their cell bodies, and these may be hardened by either secreted CaCO3 or by the agglutination of sediment grains from the environment. Such mineralized shells readily fossilize, which makes them useful paleo/environmental and related geological applications. The morphology of foraminiferal chambers emerges from a cascade of complex genetically-controlled processes ultimately controlled through the interactions among morphogenetic components. From studies on the morphogenesis and movements of foraminiferan pseudopodia, we presume that actin meshwork, microtubules, plasma membrane and their various associated proteins all contribute to chamber formation. Here, we apply dissipative particle dynamics (DPD) simulation techniques to model interactions between the plasma membrane and actin meshwork to test their role the formation of cell body and test architecture. The present studies mark the first stage of in silico experiments aimed at developing an emergent model of foraminiferal chamber formation and shell morphogenesis.

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