Data from: Experimental analysis of organ decay and pH gradients within a carcass and the implications for phosphatization of soft tissues

Replacement of soft-tissues by calcium phosphate yields spectacular
fossils. Decay experiments have shown that pH is a major control on the
precipitation of calcium phosphate and tissue replication: for this to
occur pH must fall below the carbonic acid dissociation constant (pH
6.38). However, in the fossil record, phosphatisation is highly selective
- some internal organs, such as muscles, stomachs, and intestines, appear
to preferentially phosphatise while other organs seldomly phosphatise. The
reasons for this are unclear but one hypothesis is that, during decay,
organs create distinct chemical microenvironments and only some fall below
the critical pH threshold for mineralization to occur. Here, we present a
novel investigation using microelectrodes that records fluctuating dynamic
spatial and temporal pH gradients inside of organs within a carcass in
real time. Our experiments demonstrate that within a decaying carcass,
organ-specific microenvironments are not generated. Rather, a pervasive pH
environment forms within the body cavity (i.e. the coelom) which persists
until integumentary failure. With no evidence to support the development
of organ-specific microenvironments during decay other factors must
control organ phosphatisation. We propose it is tissue histology that
plays an important role in selective phosphatisation. Tissues with high
phosphate content (and those rich in collagen) are most likely to
phosphatise. Internal organs that have low tissue-bound phosphate,
including the integuments of the stomach and intestine, only phosphatise
when associated with ingested phosphate-rich organic matter. Identifying
the driver behind selective phosphatisation may provide insights into
other highly selective modes of soft-tissue preservation i.e.
pyritization.