A comparative SEM morphological study of biogenic and abiogenic carbonates for the search for biostructures on Mars

Next space missions will investigate the possibility of extinct or extant life on Mars. In previous laboratory works by studying the infrared spectral modifications induced by thermal processing on different carbonate samples (recent shells and fossils of different ages), we developed a method able to discriminate biogenic carbonates from their abiogenic counterparts. The method has been successfully applied to microbialites, i.e. bio-induced carbonates deposits, and particularly to stromatolites, the laminated fabric of microbialites, some of which can be ascribed among the oldest traces of biological activity known on Earth. These results are of valuable importance since such carbonates are linked to primitive living organisms which can be considered as good analogues for putative Martian life forms. Due to the fact that the microstructures of biogenic carbonate may be different from those of abiogenic origin, we have recently investigated the microscopic morphology at different scales of our samples (shells, skeletal grains, microbialites and stromatolites) using a scanning electron microscope (SEM). In this paper we present some preliminary results that can be of valuable interest in view of the high resolution imaging systems that in the near future will explore the surface of Mars in the search for biological traces of life.