Based on genetic information scientists can group
living organisms
into biospecies, groups of
organisms separated by genetic differences. Being unable to
sample the DNA of organisms that lived millions of years ago,
paleontologists identify species of fossilized organisms
on the basis of quantifiable morphological characteristics, hence the term morphospecies.
Biospecies:
The
evolution of Modern dogs as observed by quantified changes in DNA over
the last 12,000
years
Morphospecies:
The
evolution of rilobites as observed in the fossil record over the last
500 million years
Breaking fossil organisms up in to morphospecies is an
effective tool to study evolution, however it
requires the researcher to quantitatively separate changes that come
about
due to evolution from those that may be a result of "environmental
plasticity", or the potential that most organisms have to vary
their
morphology as a response to environmental change. Examples of
this behavior can be observed in some tropical corals, for example Porites spp.
which are able to
adapt their colony shape to environmental stress, such as sedimentation
rate. However, if the stressor is removed, colony shape will
revert. This raises the question, "how do scientists
delineate between morphological change
associated environmental plasticity and
evolutionary change?" Paleontologists need to examine
environmental factors recorded in the rocks, and compare these to how
morphology changes over time. Environmental stressors such as
sedimentation rate are short lived, and often are cyclic, whereas
morphological change due to evolution is ongoing and unidirectional.
Photographs courtesy of the University of
California Museum of
Paleontology:
(http://evolution.berkeley.edu/)