PRINCIPLES OF PHYLOGENY
Phylogeny, the ancestral tree
of species, is often difficult to determine when a species has no closely
related species. Molecular phylogeny was
thought to be a source of superior answers to the questions of relationships. That would be true if all genetic material
evolved at the same rate. But different
portions of the genome can have different rates of mutation, so can different
species, and the rate can be affected by the longevity of individuals. So other factors have to be considered to
improve accuracy of phylogeny.
The path is determined by
natural selection. Selection may maintain a stable species
composition for long times when it is well-adapted to stable environmental
conditions. In a variable environment
changes may be relatively rapid over a comparable time period.
Features can be lost more
rapidly than they are gained. The formation of a new structure or a biochemical
substance is usually due to accumulation of many mutations. Many accumulated factors must interact in
proper sequence to produce the feature.
But one change may disrupt the entire process. The change may be fatal if it is an essential
feature. An example, albino organisms
may result from one of many possible disruptions leading to a failure to
produce the melanin pigment.
Complex features are
present in some way in ancestral species. The eye is an excellent example of this principle. Some one-celled animals had pigment spots
near a light sensitive swelling of the basal part of a flagellum. The flagellum is a thread-like structure that
can undulate; it has internal fibrils in a unique pattern common to cilia. Variations of the fibril pattern occur in the photo-receptors of eyes of all groups of higher animals with eyes. The eye structure itself shows variation
distinguishing major groups.
Genotypic selection is
accomplished through phenotypic selection. Because genes interacting with
environmental factors determine the phenotype (the physical expression
resulting from that interaction) many seem to think natural selection acts
directly on the genotype. But survival
of the individual is dependent on the success of the phenotype. Consequently, anatomy and other phenotypic
expressions are better guides than genes are to evolutionary pathways in many
cases.
Factors causing natural
selection can be variable or constant. They can be characteristics of (a) the physical
environment, (b) the biotic environment, or (c) the interaction of those
factors. Ice ages come and go. Solar radiation is relatively constant, but
varies greatly by latitude, time of day, and cloud cover. Microhabitats vary, such as the side of a tree
favorable for moss growth.
Extinction events are typically
followed by accelerated evolutionary changes among survivors in the
post-extinction period. The early Cambrian expansion of major phyla
is the most remarkable example.
Rapidly evolving species
may have greater genetic similarity to descendants of slowly evolving ancestral stock
species than to more recently evolved sister groups. The most dramatic
example is the pogonophorans that show up in an intermediate position among
other more recent deuterostome clusters.
This aspect of evolution can probably not be found in the scientific
literature, since I appear to be the only one that knows about the extreme age
of pogonophorans and their connecting link position between annelids and
deuterostomes. Some such suggestion may
have been made in a 1978 Copenhagen symposium on the Pogonophora before my 1983*
presentation to the Am. Soc. of Zoologists.
Geographic factors are
immensely important in affecting the course of evolution. Continents
can act as barriers to marine species dispersal and highways for terrestrial
species. Isolation of groups allows
separate evolutionary paths for related forms.
Isolation of marsupials in
Australia enabled them to evolve into forms comparable to many of the placental
mammals that were so successful on other continents. The variations in each location are examples
of adaptive radiation into new species, while those of opposite groups
radiating into forms similar to those in other locations are examples of convergent
evolution.
An interesting example of
geographic barriers and highways is shown by some terrestrial species found at
many different latitudes found at higher locations in the tropics and progressively
closer to sea-level as latitudes closer to the poles are reached. Conversely, some marine invertebrates of
shallow coastal seas of high latitude regions are found in progressively deeper
waters as they transition to tropical locations. Temperature is presumably the major factor
determining such distribution.
*Engemann, J. G. 1983.
Coelomate animals are monophyletic.
American Zoologist,
23(4):1008. Abstract # 753. A submission
of the complete paper was rejected by an editor of Nature because he considered it to not be of enough general interest.
Joseph G. Engemann
June 17, 2013
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