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| Pathways
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Lessons on the Pathways of Evolution General Lessons on Systematics Distinguishing Classification from Phylogenetic Systematics |
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Backgound Information
The
diversity of life on earth is overwhelming. So overwhelming that for
centuries humans have attempted to organize, or classify, organisms
into categories that make sense. The most famous system of classification,
developed by Linnaeus in the 1700’s and still used today, is the
binomial nomenclature system. There are two important features of this
system. First, each species has a two-part name: genus and
species. Second, the system classifies species into hierarchical
groupings, in which groups are nested within larger groups. Similar
species are grouped into a genus. Similar genera are grouped into a
family, and so on. In short, organisms are classified together because
they are similar. There has only been one history of life on earth. The goal of modern systematics is to discover what this history has been. In other words, how are living and extinct organisms related to one another? What is the genealogy of life? As in all fields of science, systematists develop hypotheses. The hypotheses of systematics are phylogenetic trees, or phylogenies. A phylogeny is the hypothesized evolutionary relationship among a group of taxa. Constructing
phylogenetic hypotheses is in principle a simple thing, but in practice
can be quite difficult. Indeed, much of the work in modern systematics
is to determine the most appropriate methods for reconstructing evolutionary
history.
The
first two are homologies (similarity due to shared ancestry), while
the third is analogy (similarity due to adaptation to similar environments).
Only homologies are useful in phylogenies, as homologies reflect a shared
history. Of the two types of homologies, only shared derived characters
are useful for inferring the true evolutionary relationship among taxa.
Shared derived characters define a group with a shared history: they
evolved in an
Because
of the historical nature of systematics, phylogenetic hypotheses cannot
be tested with experiments. However, this does not mean they cannot
be tested. Phylogenetic history is reconstructed in a way that is similar
to how a criminal investigator reconstructs a crime scene. Investigators
are never present when the crime actually happened, but they are very
good at determining what most likely occurred. The reason is that clues
to past events are always left, and the job of the investigator is to
piece together this evidence into a story about what most likely happened.
If more clues are found that do not fit the story, then something about
the story is wrong, and needs to be modified. Well-supported
phylogenies are extremely useful in many different fields within biology.
Their primary uses are to better understand the history of change in
a particular character, and to test hypotheses about the evolution of
a particular character or characters. The
study of macroevolution involves the investigation of patterns and processes
that are important in evolution above the level of the species. For
example, one question is what is the pattern of character
evolution? Does character evolution proceed
at a continuous, gradual rate (as Darwin envisioned), or do characters
change relatively little over long periods of time, with this period
of stasis “punctuated” with very rapid change? Punctuated
equilibrium is a model that describes this second pattern, as well as
proposing a hypothesis to help explain it (see below).
Another major question about process is what is the genetic mechanism responsible for the pattern of large phenotypic differences between taxa? There are two hypotheses that have been put forward to explain the pattern of phenotypic gaps found between extant taxa. These hypotheses deal with the genetic causes of the phenotypic differences found in higher taxa: 1)
saltation—these gaps exist because there were never any intermediates:
gaps are explained by single events of macromutations (single mutations
of very large phenotypic effects). Contrary
to popular belief, punctuated equilibrium is a gradualistic model (i.e.
evolution occurs through the accumulation of mutations of small effects).
In this model, intermediates do not appear in the fossil record because
the change in morphology occurred so rapidly that the fossil record
appears discontinuous. The more rapid the change, the less likely it
will have been preserved by fossilization.
Lessons
on the Pathways of Evolution
The University of California’s Museum of Paleontology has a “Phylogeny Wing Exhibit,” which includes a tutorial on phylogenetic systematics. The ENSI website has two general read-and-discuss lessons on systematics: “Why Cladistics?”, and “What, If Anything, is a Zebra?”
There
are several lessons that help introduce the concept of phylogenetic
systematics and help students make the jump from the nested hierarchy
of classification, to the evolutionary relationships among organisms.
They use the concepts of distinguishing characteristics to get across
the idea that groups have a common ancestor. In other words, organisms
are classed together because they are similar and they are similar because
they share a common ancestry. The following two lessons are from
the ENSI website: “Primate
Classification” and “Cladistics
is a Zip…Baggie.” The first uses primates,
with the nested hierarchy represented as boxes within boxes, and the
second uses vertebrates, with nesting within various sized Ziploc baggies.
ENSI also has a whole class activity, “Classroom
Cladogram,” in which the class as a whole builds
a large tree of vertebrates. There
are several rather simple exercises on tree building at the Access Excellence
web site: “From Restriction Maps to Cladograms,”
“Molecular Biology and Primate Phylogenetics,”
and “Using Amino Acid Sequences to Show Evolutionary Relationships.”
These can all be found at their Activities
Exchange’s Evolution Program. You can also find “Constructing
a Phylogenetic Tree Using DNA Sequence Data” there. In
this lesson the students simulate the historical process to produce
the sequences, so they know that the tree they make is accurate. They
then trade data with another student, and work “backwards”
with the data to infer the evolutionary relationship of an “unknown”
phylogeny. ENSI has two lessons on the pattern in the fossil record: “Macroevolution: Patterns and Trends, and Rates of Change,” and “A Peek at the Past: Fossil Patterns,” which uses caminalcules. They also have a lesson on extinction: “’Theory’ Choices: What Happened to the Dinosaurs?” |
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