Part 11 of 22 in Evolution Basics

The Cambrian Diversification and Assembling Animal Body Plans

Dennis Venema
on September 12, 2013

The Cambrian “Explosion”

In the last post in this series, we discussed the evidence for two ancient endosymbiosis events (leading to mitochondria and chloroplasts) that had a profound impact on the subsequent evolution of eukaryotic diversity. A second event that would profoundly shape the future of animal life on earth was the dramatic diversification of animal groups during the Cambrian, a period stretching from 542 million years ago until 488 million years ago.

What is especially intriguing about the Cambrian period is that it represents the first fossil record for many animal groups that bear a discernible resemblance to animals that still exist today. “Discernible” of course does not mean that what we see in the Cambrian is familiar – Cambrian fauna are markedly different from present-day organisms – but rather the first appearance of traits in the fossil record that we recognize as characteristic of groups of related organisms we observe today. In other words, certain traits we observe in the Cambrian are familiar, though the combination of traits we observe in Cambrian animals is often different from those seen in modern groups. Nonetheless, there is an interest in determining when the groups we see in the present first arose – the first “arthropods,” or “vertebrates,” for example.

If you’re wondering if this introduces something of a “present-day bias” to studying the fossil record, you’re correct – effectively, scientists are using the characteristics of present dayorganisms to attempt to place extinct organisms into groups of relatedness. Before we see how this plays out in studies of the Cambrian, however, we’ll have to explore a few deeper concepts about phylogenies than we have examined thus far.

Evolution and taxonomy

Biologists have been trying to do taxonomy – i.e. group organisms into logical categories – since the time of Linnaeus in the 1700s. Given the explanatory power of evolutionary theory and its current place as a foundational theory in biology, this practice now attempts to group organisms by their evolutionary relatedness. In this approach, the most logical classifications are said to be monophyletic – a technical term that simply means consisting of a common ancestral population and all of its descendant species. An easy way to recognize a monophyletic group is to imagine a phylogeny as a mobile – a monophyletic group can be “snipped off” the mobile with only one cut. Any other type of grouping would require two or more cuts to be made. For example, for the following phylogeny, a grouping of A, B and C is monophyletic, but a grouping of B, C, and D is not:

One cut (the blue line) removes a “monophyletic” group from a phylogeny. The science of classifying organisms (taxonomy) is an attempt to organize species into monophyletic groups.

The grouping of B, C, and D is not monophyletic, since it requires at least two “cuts” to remove it from its phylogeny. The correct taxonomic group that encompasses (B, C and D) also must include A if it is to be monophyletic.

Using monophyletic groups as the basis for taxonomy comes with challenges, however. One challenge arises when we apply the natural tendency for using combinations of traits found in present-day organisms as the basis for classifying all organisms throughout evolutionary history. Let’s work through an example to see what the issues are.

Will the first “real” arthropod please stand up?

Arthropods are a highly diverse and successful group of organisms that include present-day insects, crustaceans and arachnids (i.e. spiders and scorpions), among others. The evidence also points to arthropods being a monophyletic group. All living arthropods have a suite of defining characteristics such as a hard external skeleton (exoskeleton), specialized body segments, and specialized appendages. While these characteristics are useful for defining modern arthropods, these criteria become less useful as we travel back through the evolutionary history of arthropods. The reason is simple – from an evolutionary point of view, one would not expect these different traits to arise as a unit in one fell swoop. Rather, one would expect that these traits would arise over time in the lineage leading to modern day arthropods. If so, and if populations were diverging away from the arthropod lineage to form species as these traits were being acquired, we would expect to find species in the fossil record that do not have the full suite of “arthropod” characteristics, but only some:

For example, based on the above phylogeny we might expect to find two groups of “arthropod-like” organisms in the fossil record:  species that have only (1) of the three traits (specialized appendages only), as well as a second group (2) with specialized appendages and segments. If such species (or groups of species) existed, it would simultaneously provide information on how the characteristic suite of arthropod features was acquired over time, and blur the distinction between arthropods and other forms of life. Indeed, these species would represent “transitional forms” in the sense that they have intermediate sets of characteristic features that indicate the steps the arthropod lineage took to achieve the “modern” suite of characteristics.

In other words, the taxonomic group “arthropods” is somewhat of an arbitrary classification, since we are choosing to “cut off” a monophyletic group at a particular location on the phylogeny when it would also be just as appropriate to cut if off at a different location further back in time and include more species (or later in its history, and include less).

While understanding the evolutionary history of a monophyletic group does not lend itself to black-and-white, either/or types of taxonomic classification, it is very useful for determining how complex body plans arose in a step-by-step fashion. Next, we’ll explore this idea further by examining some Cambrian animals in more detail.

Earlier, we introduced the concept that what we define in the present day as a “body plan” or “shared suite of characteristics of a monophyletic group” in fact presents a challenge for classifying organisms from the deep past. The reason, as we discussed, is that any modern-day suite of characteristics is not expected to have arisen all at once, but rather in a step-by-step, piecemeal fashion.

Let’s return to our discussion of arthropods to see how biologists handle this challenge in the face of real data. The general approach is to start with the characteristics of a monophyletic group of species that has at least two species (or more) represented in the present day. These species, their common ancestral species, and all descendants of that common ancestral species form what is known as a “crown group” on a phylogeny (often abbreviated as a triangle to represent numerous species). Accordingly, we can define “crown group” arthropods as the last common ancestral population of all living arthropod species and all of their descendant species (living or not). Other extinct groups that have some, but not all, of the characteristics of the crown group are then classified as “stem group” species:

Velvet worms are living relatives to arthropods that live in tropical areas and temperate regions of the southern hemisphere. Although segmented, they lack the specialized appendages and segments characteristic of crown-group arthropods. (Image source)

The question then arises: is a “stem group” arthropod really an arthropod? Yes and no – such species are not a crown group arthropod, since they do not possess all of the characteristics that define modern-day arthropods (and their common ancestral population, and its descendants). However, they are more closely related to crown-group arthropods than to any other monophyletic group with living representatives, and they possess at least some of the characteristics of the crown group. As such they are arthropods in a sense, but better described as “stem group” species.

Let’s expand this example to include another crown group – velvet worms (Onychophora). Velvet worms share some features in common with arthropods (such as appendages and segmentation) but not others (for example, they lack the complex specialization of segments seen in arthropods).

Phylogenic analyses (using comparative morphology, the fossil record, and DNA sequencing) consistently place velvet worms as a close relative of arthropods. Since velvet worms have living species, we can define a crown group for them as well (as before, the last common ancestral population for all living velvet worm species, and all of its descendant species). As for arthropods, as we look back in the fossil record, we see some extinct species that have some, but not all, of the defining features of crown-group velvet worms. Accordingly, we can place these species on the “stem” of the velvet worm lineage:

What should be obvious from this phylogeny is that the distinction between a stem-group arthropod and a stem-group onychophoran will become blurred as the two lineages converge (moving from the present day backwards towards their common ancestral population). Species that we find in the fossil record can be assigned as a stem to either lineage based on their suite of characteristics, and whether they show closer relatedness to the arthropod or onychophoran lineage.

Stem-group arthropods in the Cambrian

With this understanding in hand, we can now turn to actual species that we observe in the Cambrian fossil record as examples of stem-group arthropods. One well-known, large Cambrian predator is Anomalocaris (literally, “abnormal shrimp”). Anomalocaris has a number of features that are clearly shared with crown-group arthropods, such as large compound eyes, specialized jointed appendages, specialized segmentation, and other features. What it lacks, however, is a hardened exoskeleton over its entire body (it has hardened appendages only). This suite of characteristics places it as a close relative to crown group arthropods (e.g. we would place Anomalocarisat the “X1” position in the phylogeny above), and also provides information about the state of characteristics present at the time that the lineage leading to Anomalocaris branched away from the lineage leading to crown group arthropods (i.e. that a fully hardened exoskeleton was one of the last characteristics that the ancestral population leading to crown-group arthropods acquired).

Other species in the Cambrian show even fewer characteristics of crown-group arthropods, but yet still exhibit at least some features in common. The bizarre group of species known as Hallucigenia is an example.  Features that Hallucigenia share in common with common with crown-group arthropods are specialized appendages and specialized segmentation – but other features, such as a hardened exoskeleton (on either appendages or the body as a whole), are absent. In other words, these species are stem arthropods that are more like what we would expect of stem onychophorans.

Building body plans, step by step

Taken together, we can summarize these findings as follows:

What we observe as the emergence of a new taxonomic unit (“phylum,” “family,” “genus,” and so on) is somewhat arbitrary (since it in actuality describes a continuum) and in fact is decided only in hindsight, based on the characteristics of monophyletic groups in the present day.

For better or for worse, taxonomy has been trying to shoehorn ancient species into modern categories. The fact that ancient species blur the distinctions between modern day taxonomic groups (such as arthropods and onychophorans) shows that what we recognize as large taxonomic groups (such as what we call “phyla”) are in fact best described as monophyletic groups in nested sets.

The fossil record supports the gradual acquisition of the characteristics we see in modern groups and subsequently use for classification.

The key defining features of arthropods (specialized segmentation, specialized appendages, hard exoskeletons, compound eyes, and a host of other characteristics) do not appear all at once in any one species in the fossil record. To say that “arthropods” arise and diversify in the Cambrian is not to say that fully-fledged (i.e. crown-group) arthropods appear suddenly out of nowhere. Rather, we see a range of species that demonstrate that the defining characteristics of crown-group arthropods were acquired over a long period of time. While stem-group species are not likely to be direct ancestors of crown-group species, their presence in the fossil record (and the nested hierarchy their characteristics produce) provides a means to determine the order in which the defining characteristics were assembled.

The Cambrian, though “explosive,” should not be misunderstood to be instantaneously producing crown-group species.

There is no doubt that the Cambrian “explosion”, was a spectacular diversification event – but it did not produce species with fully modern character sets instantaneously. Rather, we see a diversification of stem-group organisms, the sequential and serial addition of characteristics in some lineages over time (with the loss of other lineages), and the eventual production of character sets in successful monophyletic groups that we retrospectively recognize as taxonomic groupings.

In the next post in this series, we’ll examine the Cambrian origins of the lineage that eventually led to humans – the vertebrates.


Notes & References


Dennis Venema
About the Author

Dennis Venema

Dennis Venema is professor of biology at Trinity Western University in Langley, British Columbia. He holds a B.Sc. (with Honors) from the University of British Columbia (1996), and received his Ph.D. from the University of British Columbia in 2003. His research is focused on the genetics of pattern formation and signaling using the common fruit fly Drosophila melanogaster as a model organism. Dennis is a gifted thinker and writer on matters of science and faith, but also an award-winning biology teacher—he won the 2008 College Biology Teaching Award from the National Association of Biology Teachers. He and his family enjoy numerous outdoor activities that the Canadian Pacific coast region has to offer.

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