Subfossil
From Wikipedia, the free encyclopedia
Subfossil is attributed to bones or whole skeletons (and, in general all materials having living parts that can become fossil) whose fossilization process is not complete, either for lack of time or because the condition in which bones were buried were non optimal for fossilization.
Subfossil remains that date back into the Mesozoic are expectionally rare, usually in an advanced state of decay and consequently much disputed. The vast bulk of the material comes from Quaternary deposits.
The main importance of subfossil vs. fossil remains is that the former contain organic material, which can be used for radiocarbon dating or extraction and sequencing of DNA, protein, or other biomolecules. Additionally, isotope ratios can provide much information about the ecological conditions under which extinct animals lived.
