posted on 2018-02-08, 11:33authored byMark A. Purnell, Philip J. C. Donoghue, Sarah E. Gabbott, Maria McNamara, Duncan J. E. Murdock, Robert S. Sansom
Taphonomic experiments provide important insights into fossils that preserve the remains of
decay-prone soft tissues – tissues that are usually degraded and lost prior to fossilization. These
fossils are among the most scientifically valuable evidence of ancient life on Earth, giving us a view
into the past that is much less biased and incomplete than the picture provided by skeletal remains
alone. Although the value of taphonomic experiments is beyond doubt, a lack of clarity regarding
their purpose and limitations, and ambiguity in the use of terminology, are hampering progress.
Here we distinguish between processes that promote information retention and those that promote
information loss in order to clarify the distinction between fossilization and preservation.
Recognising distinct processes of decay, mineralization and maturation, the sequence in which
they act, and the potential for interactions, has important consequences for analysis of fossils, and
for the design of taphonomic experiments. The purpose of well-designed taphonomic experiments
is generally to understand decay, maturation, and preservation individually, thus limiting the
number of variables involved. Much work remains to be done, but these methodologically
reductionist foundations will allow researchers to build towards more complex taphonomic
experiments and a more holistic understanding and analysis of the interactions between decay,
maturation and preservation in the fossilization of non-biomineralized remains. Our focus must
remain on the key issue of understanding what exceptionally preserved fossils reveal about the
history of biodiversity and evolution, rather than on debating the scope and value of an
experimental approach.
Funding
MAP, SEG and DJEM funded by NERC grant
NE/K004557/1; PCJD by Royal Society Wolfson Merit Award and NERC NE/P013678/1, DJEM by
a Leverhulme Trust Early Career Fellowship, MMN by a European Research Council Starting
Grant H2020-20140-ERC-StG-637691-ANICOLEVO, RSS by NERC fellowship NE/I020253/2 and
BBSRC grant BB/N015827/1.
History
Citation
Palaeontology, 2018
Author affiliation
/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/School of Geography, Geology and the Environment
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