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The signatures of microbial organisms that can be preserved in rocks are related to the morphological, organic, and metabolic characteristics of the organisms.
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There are three types of traces to be considered: morphological, organic biomarkers (fossil lipids) and isotopic.
Biosignature identification needs to take into account a broad variety of morphological, geochemical, and organic characteristics.
The physical-chemical, morphological and dimensional determinations of the complex mixture of organic and inorganic particulates are one of the major aspects for their characterization and for identification of emission sources that contribute to particulate air concentrations [4].
The results from morphological, spectral and gravimetric experiments show that the cast films are bicontinuous, indicating a strong compatibility of the organic and inorganic phases.
"It's organic and dry-farmed.
The food is mostly organic and local.
Everything was both organic and unpredictable.
Coals contain both organic and inorganic phases.
It is organic and miraculously harmonious.
The result is simultaneously organic and mechanical.
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