Beyond memorization: an intermediate-level paleontology activity that integrates anatomy, ecology, and macroevolutionary theory using trilobites
© Casey and Lieberman; licensee Springer 2014
Received: 9 April 2014
Accepted: 4 August 2014
Published: 22 August 2014
Here we present a stand-alone, upper level undergraduate laboratory exercise that integrates organismal ecology and evolutionary concepts and minimizes the need for student memorization. This laboratory seeks to integrate both anatomical and conceptual content into paleontology lab pedagogy by demonstrating how taxon-specific anatomical information are the fundamental data by which scientists evaluate big picture questions related to the study of macroevolution and ecology. Real specimen photos are provided to familiarize students with a relatively limited suite of anatomical terms and taxonomic detail while allowing schools lacking large paleontology collections to participate in specimen-based inquiry. A matching exercise requires students to assign various trilobite morphologies to their interpreted ecological niches, thus reinforcing the students’ new anatomical knowledge and helping students to distinguish between primary and secondary interpretation of scientific evidence. The use of trilobites as a macroevolutionary case study introduces students to questions still being actively investigated by scientists and provides an effective refutation of creationist arguments. By deemphasizing systematics and highlighting intriguing patterns from the recent published literature, this laboratory hopes to promote paleontology as a vibrant and relevant field, and avoid the misconception that paleontologists are simply stamp collectors, intent on naming and categorizing fossils. We hope that the broad implementation of this laboratory exercise will generate the data necessary to evaluate the validity of this approach and its ease of use in the classroom.
Learning goals and pedagogy
We have developed a trilobite laboratory for college students; here we describe aspects and elaborate on the background and pedagogical philosophy behind the formulation of this lab. The complete version of the lab itself and the key are available as a pdf downloadz at the end of this article (Additional files 1 and 2). However, since the pedagogical and background elements pertaining to the development of the lab are not provided therein, we felt it important to present this information in the context of a broader discussion about the best way to teach paleontology and evolution to undergraduates. The trilobite lab we developed is intended for an upper level undergraduate paleontology course enrolling mainly sophomores and juniors who have already taken historical geology or its equivalent but may also be appropriate for introductory college biology or advanced high school biology courses provided that concepts such as geologic time, phylogeny, and trace fossils are familiar to students. It aims to comprise an exercise for one week in what would be a multi-week lab, though it can also serve as a standalone exercise as well. This lab will be particularly helpful to those institutions that lack a large teaching collection by providing color photographs of museum specimens. Students may find previous exposure to phylogenetic methods and terminology helpful in completing this laboratory exercise. The learning goals for this lab are: 1) to familiarize students with the anatomy and terminology relating to trilobites; 2) to give students experience identifying morphologic structures on real fossil specimens, not just diagrammatic representations; 3) to highlight at the grand scale the evolutionary history and ecology of Trilobita; 4) to outline scientific reasoning and present paleontology as an exciting, modern discipline; and 5) to introduce students to the study of macroevolution in the fossil record using trilobites as a case study.
The Teaching Paleontology in the 21st century website (On the Cutting Edge - Professional Development for Geoscience Faculty ) compares and contrasts two organizational schemes for the teaching of paleontology. The taxon approach covers phyla sequentially. The benefit of this approach is that it provides in-depth coverage of all taxa, so that students learn the same types of information about all of the disparate groups. This is also the way that many textbooks and sources are organized. The drawbacks of such an approach are that they can potentially be dry, they emphasize memorization, and fail to teach or develop problem solving or critical thinking skills. A secondary byproduct of this teaching approach is that students may fail to see paleontology as a relevant and important discipline. By contrast, the conceptual model organizes the course around a series of big picture concepts within paleontology which tends to generate greater student interest and enthusiasm. However, by the same token, coverage of the taxonomy and morphology of individual groups may be too cursory for students to gain a true appreciation of each fossil clade. Given that each of these two approaches has strengths and weaknesses we have tried to combine them in the present laboratory exercise by mixing the traditional taxon approach and the conceptual framework approach. We accomplish this by covering information on the anatomy and ecology of the group while also delving into macroevolutionary concepts the group elucidates. In particular, this lab teaches the basic anatomy and ecology of Trilobita and then requires the students to apply that new knowledge to an exercise on macroevolution. We aim by reinforcement to inculcate anatomical terminology via the lab, as retention and understanding of anatomy is still critical for tackling modern problems in paleontology. Ultimately, it is critical to integrate both anatomical and conceptual content into paleontology lab pedagogy. One mode to attain this, and the tack followed in the present lab, involves demonstrating how taxon-specific anatomical information are the fundamental data by which scientists evaluate big picture questions related to the study of macroevolution.
Proper undergraduate paleontology education is crucial in an age where debates over the teaching of evolution continue to make headlines (Weissert ). Padian () argued that teaching macroevolution is an effective way to counter creationist arguments that are typically more focused on microevolution. In particular, Padian () suggested that by increasing the coverage of macroevolutionary concepts at the college level not only is greater student interest generated but a greater understanding of the fallacy of creationism is attained. Padian () also demonstrated that an emphasis on macroevolution is often lacking in upper level biology, evolution, and paleontology textbooks. By combining a discussion of macroevolutionary theory with the latest published research on trilobite pattern and process, this lab aims to follow Padian’s (, ) precepts.
Trilobite morphology and specimen photographs
These discussions of form and function give students a sense of what trilobites were like as living animals rather than treating them as inert objects. By replacing the lengthy descriptions of each trilobite order (a more traditional approach) with this morphological variety approach, we are deemphasizing the role of memorization. Reducing an exercise’s reliance on memorization as a means of assessment is important because a student’s negative perception of a course as memorization-based can decrease a student’s interest in and perceived value of the course material (Vermunt and Vermetten ). These changes in student affect can lead to decreased learning, persistence, and effort on the part of the student (McConnell and van der Hoeven Kraft ). DeHaan () summarizes the recommendations of numerous reports on science education reform by stating that science education should focus, “less on vocabulary and facts that students memorize, and more on students’ understanding of scientific concepts and how those concepts fit together in a framework of knowledge about a subject”. In addition to the benefits of decreased memorization listed above, it behooves us as paleontologists to present our discipline to future generations of potential scientists in the best possible light. An over-reliance on systematics and taxonomic memorization gives students the false impression that paleontologists are stamp collectors only interested in naming and classifying organisms and squanders the opportunity to paint a vivid picture of past life.
The combination of learning anatomical vocabulary and developing observational skills will allow students to use published taxonomic descriptions to make identifications on their own if necessary. This ability will negate the need to memorize systematic groups and help students hone a skill that they can transfer to other labs within a paleontology course or other courses in the natural and biological sciences. The simple fill-in-the-blank assessment used for this section allows for immediate feedback on students’ grasp of the morphological terminology covered, so that professors can clarify points before moving on. Immediate application of the anatomical terminology reinforces the students’ newly acquired knowledge and justifies why some terminology must be learned in order to discuss scientific questions, namely that differences in morphology are the evidence on which we base much of our scientific inquiry.
Inferring organismal ecology using scientific reasoning
Ecological niches of trilobites based on morphological or sedimentary evidence
Inferred lifestyle or behavior
Reduced thorax and pygidium; smoothed cephalon; downward projecting spines; facies independence
Light, streamlined body allows fast swimming. Spines prohibit effective movement on the sediment surface. Distribution controlled by water column characteristics rather than sediment characteristics.
Smooth exterior, broad & flat axial lobe
Larger muscle attachments
Stronger limb motions to move sediments
Eyes reduced or absent
Darker conditions, less need/no need for keen eyesight
Living in deep water
Wide bodies, genal spines
Added support for soupy substrate
Well-developed limbs, flexible hypostome, Cruziana feeding traces
Food passed anteriorly towards the mouth during the course of movement, flexible hypostome used as a scoop.
Unusual occipital angle, pitted fringe
Pits allow water to flow through cephalon from leg-generated currents
Rigid, strongly braced hypostome; forked hypostome projections
Ability to process relatively large food particles
Predatory, feeding on soft bodied worms
The study of ecological niches speaks to students’ natural curiosity about how long extinct animals lived. This approach informs students about trilobite ecology from a knowledge acquisition perspective rather than rote memorization of details. Further, this set of examples aims to illustrate the relevance paleontology has when it comes to reconstructing past worlds and answering questions about ancient life using anatomy as evidence. In addition, this emphasis on how morphology can be used to make ecological inferences helps demonstrate to students why the small amount of anatomical information included in the laboratory is necessary to develop a common language with which scientists can approach larger scientific questions.
The matching portion of the exercise (Figure 4) provides another opportunity for students to apply their anatomical knowledge by critically examining specimen photos to recognize diagnostic features listed in the evidence column. The matching exercise allows professors to assess students’ understanding of numerous anatomical concepts without overwhelming students with multiple in-depth questions. For instance, the professor may assess whether or not students understand what the phrase ‘pitted fringe’ means and if they can recognize one. Students will also be required to distinguish between dorsal and ventral views of specimens and recognize the hypostome. Matching rewards students for thinking critically as it allows them to eliminate possibilities. For example, students should be able to eliminate the possibility that the trilobites pictured in Figure 4B and E were burrowers, given their long spines.
Trends/events in the evolutionary history of trilobites
Students, especially those with a background in biology, have frequently requested more information summarizing the evolutionary history of the fossil groups they were studying. This can be quite challenging when teaching students about taxonomic groups with which you are only marginally familiar. This lab utilizes recent scientific publications on intriguing trends in trilobite evolution to provide this information to both teachers and students who may not be particularly familiar with the Trilobita. The following example is an excerpt from the Spatial and Temporal Distribution section summarizing the biogeographic history of the clade.
The earliest trilobites appear suddenly in rocks of Early Cambrian age (522–530 Ma) from present day Scandinavia and eastern Europe. Soon afterwards trilobites also appeared in China, North America, Antarctica, and Australia and within the Early Cambrian are found throughout the world. The early history of trilobite evolution shows a pattern of biogeographic differentiation which taken with other evidence suggests that there may have been some significant period of trilobite evolution before they actually appeared in the fossil record. Current estimates suggest that although the earliest trilobites appeared in the fossil record around 525 Ma they may have originated 550–600 Ma (Lieberman and Karim ). Paleontologists continue to investigate this trend looking for evidence of older trilobites and working to better constrain the timing of their origins. The reasons why the earliest relatives may have been absent from the fossil record remain unclear but may include the fact that they were small, lacked a hard shell, or they were very rare and restricted to environments where they were unlikely to fossilize.
Another example is the following excerpt from the same section that summarizes the history of trilobite diversification.
The trilobites continued to diversify into the Ordovician, but were hit particularly hard by the end Ordovician mass extinction. Trilobites were able to partially recover after the end Ordovician mass extinction, only to be hit again by the Late Devonian mass extinction. Trilobite diversity failed to rebound after the Late Devonian event and the group was eventually wiped out during the largest mass extinction of all time at the end of the Permian. Indeed, as we will discuss in more detail below, scientists are exploring the possibility that part of the reason trilobites are no longer with us today has to do with the fact that they fared particularly poorly during times of mass extinction (Lieberman and Melott ).
These passages introduce fossil patterns scientists are still actively studying and trying to explain. By highlighting areas of ongoing research, we hope to avoid the all-too-common impression among undergraduates that everything we wish to know about a certain group has already been discovered.
Macroevolution: a case study
Macroevolution is the study of the patterns and processes that affect the birth, death, and persistence of species. For instance, scientists who study macroevolution might wonder when and why new species arise or why some groups speciate rapidly while others give rise to new species very slowly. Ultimately, macroevolution is the study of evolution at the grand scale and this is an area studied by paleontologists, evolutionary biologists, and systematists. Examples of macroevolutionary patterns include: similar changes in trait evolution across multiple groups within a given lineage and pulses of evolution in response to climate change (Vrba ; Congreve ).
The Macroevolution of the Trilobites section goes on to describe a specific trend in trilobite evolution based on the recent literature. “For example, the trilobites appear to be harder hit by mass extinctions than their contemporaries (Lieberman and Karim ). In spite of their high levels of diversity, trilobites suffered major losses during the end Ordovician (Melott et al., ) and Late Devonian mass extinctions (McGhee ). After the Late Devonian biodiversity crisis, trilobite diversity failed to fully recover (Brezinski ) and the group was wiped out completely during the largest mass extinction of all time at the end of the Permian (Fortey and Owens )”. The description of this trend leads naturally to the question, “Why do the trilobites thrive in normal background conditions yet remain more susceptible to mass extinctions than other types of organisms?”
To help students explore this question, the laboratory introduces and defines the concepts of extinction, origination, background extinction, mass extinction, and volatility. Volatility is defined in the exercise as a measure of a group’s stability through time and, therefore, as a function of background rates of origination and extinction. The laboratory goes on to discuss the concept of volatility as it relates to trilobites and the question posed above.
High volatility clades have high rates of background extinction and origination, which can lead to the frequent turnover of species within the group. Low volatility groups have low rates of origination and extinction, leading to a stable clade made up of the same species over long periods of time. Volatility has been decreasing across all taxa throughout the Phanerozoic because high volatility groups have an increased probability of their diversity falling to zero, a value from which they can never recover (Lieberman and Melott ). Lieberman and Melott () describe this increased risk of clade-wide extinction as resulting in a “survival of the blandest” pattern as high volatility clades are weeded out over time while low volatility clades persist. The impacts of volatility seem to be particularly important during times of mass extinction, with high volatility clades, like ammonites and trilobites, suffering greater losses than their low-volatility contemporaries (Lieberman and Karim ). Interestingly, the reason trilobites, and also ammonites are no longer with us today, is likely because they evolved rapidly. It was the same factors that made them evolve rapidly, however, that made them prone to extinction.
Next the laboratory describes an analogy between volatility as it applies to paleontology and volatility in the stock market. This analogy will aid student understanding and retention by connecting the new information to the student’s existing framework of knowledge (DeHaan ) and relating abstract principles to something students are familiar with in their daily lives. “In this analogy, stock market volatility is a measure of how a stock changes price relative to changes in the market as a whole. High volatility stocks are those that experience dramatic increases or decreases in price unpredicted by the greater market trend, while low volatility stocks are more likely to change their price congruently with the overall market trend. Research has shown that low volatility stocks yield the best returns for long-term investors; adjusting for inflation, an initial $1 investment in 1968 yields $10.28 in 2008 if invested in low volatility stocks and only $0.64 if invested in high volatility stocks (from Baker et al. )”.
Finally, macroevolutionary inquiries combine many different types of paleontological evidence and could therefore be used to great advantage as a linking concept or larger framework (DeHaan ) in a paleontology course. This particular exercise draws on tree thinking or tree reading skills that students would have already developed as well as the concepts of background extinction versus mass extinctions. Additional themes that could be investigated under the umbrella of their relevance to the study of macroevolution include: stratigraphic correlation and dating, phylogentics and systematics, biogeography, data gaps or biases (temporal or spatial), ecological roles or niches, environmental reconstruction, or climate reconstruction and cyclicity. A macroevolutionary framework could be incorporated into a class formally by introducing a new macroevolutionary question each week, and then exploring the new source(s) of data necessary to evaluate that week’s line of inquiry. Use of macroevolution as a framework could also be introduced into the course less formally if so desired by linking concepts back to their relevance for addressing macroevolutionary questions in the course discussion of each specific topic. Regardless, this laboratory exercise will prove useful both in the context of a larger macroevolutionary framework or as a stand-alone exercise in a more traditionally structured paleontology course.
As this laboratory exercise hopefully becomes broadly utilized at various colleges we hope to gather data on its ease of use and efficacy. This publication (and distribution of the lab through the SERC educational website http://serc.carleton.edu/NAGTWorkshops/paleo/activities/79291.html, the PaleoNet listserv, the Trilogenetics website, and the new University of Kansas Invertebrate Paleontology Division’s website) will provide the needed exposure to alert professors to its availability. We are especially interested in testing the validity of the approach that emphasizes a combination of macroevolutionary concepts in conjunction with the presentation of a relatively limited suite of anatomical terms and taxonomic detail (yet still enough of the two latter to make the exercise specimen based). Ultimately, we and others (e.g., Padian, ) feel that a macroevolutionary discussion provides the best pedagogical approach for students and professors. However, like any hypothesis, validation will come from data derived from the users, both professors and students. Initial student response to the lab has been positive, with students noting in most cases that they particularly liked the pictures and illustrations. Many people were struck by the morphological variety attained by trilobites and their range in body size. One student noted, “There were trilobites as big as umbrellas (!!!!)”. Students also remembered the volatility and mass extinction discussion and at least one student’s survey response indicated that “the stock market and extinctions” portion was his/her favorite part of the lab. We suspect that in the long-term the use of such on line laboratory exercises will grow, as many college students have a strong interest in paleontology, yet few universities actually have the physical specimens in their collections to facilitate development of a lab exercise in paleontology. Further, we are currently working to modify this lab for middle school and high school audiences with the help of a junior high Earth Science teacher. In the future we hope to develop additional university-level labs on other key invertebrate fossil taxa such as brachiopods, mollusks, echinoderms, etc., using the same specimen-based approach focusing on ecology and evolutionary trends rather than memorization.
We would like to thank Una Farrell, Bruce Scherting, and Greg Ornay for help with KU exhibit specimens and two anonymous reviewers for thoughtful comments and suggestions. Financial support for making this lab was provided by NSF DEB 1256993 and EF 1206757.
- Abe FR, Lieberman BS: Quantifying morphological change during and evolutionary radiation of Devonian trilobites. Paleobiology 2012, 38: 292–307. 10.1666/10047.1View ArticleGoogle Scholar
- Anderson LI, Selden PA: Opisthosomal fusion and phylogeny of Palaeozoic Xiphosura. Lethaia 1997, 30: 19–31. 10.1111/j.1502-3931.1997.tb00440.xView ArticleGoogle Scholar
- Baker M, Bradley B, Wurgler J: Benchmarks as limits to arbitrage: understanding the low-volatility anomaly. Financial Analysts Journal 2011, 67: 40–54. 10.2469/faj.v67.n1.4View ArticleGoogle Scholar
- Brezinski DK: The rise and fall of late Paleozoic trilobites of the United States. Journal of Paleontology 1999, 73: 164–175.Google Scholar
- Congreve CR: Cladal turnover: the end Ordovician as a large-scale analogue of species turnover. Palaeontology 2013, 56: 1285–1296. 10.1111/pala.12077View ArticleGoogle Scholar
- Cross R, Price R: Towards teaching science for social responsibility: an examination of flaws in science, technology and society. Research in Science Education 1991, 21(1):47–54. (2013). doi:10.1007/BF02360456 (2013).View ArticleGoogle Scholar
- DeHaan RL: The impending revolution in undergraduate science education. Journal of Science Education and Technology 2005, 14: 253–269. 10.1007/s10956-005-4425-3View ArticleGoogle Scholar
- Driver R, Newton P, Osborne J: Establishing the norms of scientific argumentation in classrooms. Science education 2000, 84(3):287–312. 10.1002/(SICI)1098-237X(200005)84:3<287::AID-SCE1>3.0.CO;2-AView ArticleGoogle Scholar
- Fortey RA, Owens RM: Evolutionary history. In Treatise on Invertebrate Paleontology, O (Arthropoda 1, Trilobita, Revised). Edited by: Kaesler RL. Geological Society of America and University of Kansas Press, Lawrence, KS; 1997:249–287.Google Scholar
- Lieberman BS: Systematic revision of the Olenelloidea (Trilobita, Cambrian). Bulletin of the Peabody Museum of Natural History 1999, 45: 1–150.Google Scholar
- Lieberman BS, Karim TS: Tracing the trilobite tree from the root to the tips: a model marriage of fossils and phylogeny. Arthropod Structure and Development 2010, 39: 111–123. 10.1016/j.asd.2009.10.004View ArticlePubMedGoogle Scholar
- Lieberman BS, Melott AL: Declining volatility, a general property of disparate systems: From fossils, to stocks, to the stars. Palaeontology 2013, 56: 1297–1304. 10.1111/pala.12017View ArticleGoogle Scholar
- McConnell DA, van Der Hoeven Kraft KJ: Affective domain and student learning in the geosciences. Journal of Geoscience Education 2011, 59: 106–110. 10.5408/1.3604828View ArticleGoogle Scholar
- McGhee GR: The Late Devonian Mass Extinction: The Frasnian/Famennian Crisis. Columbia University Press, New York, NY; 1996.Google Scholar
- Melott AL, Lieberman BS, Laird CM, Martin LD, Medvedev MV, Thomas BC, Cannizo JK, Gehrels N, Jackman CH: Did a gamma-ray burst initiate the late Ordovician mass extinction? International Journal of Astrobiology 2004, 3: 55–61. 10.1017/S1473550404001910View ArticleGoogle Scholar
- On the Cutting Edge - Professional Development for Geoscience Faculty. (2013). Teaching Paleontology In The 21st Century. http://serc.carleton.edu/NAGTWorkshops/paleo/index.html#coursedesign. Accessed 18 December 2013.
- Osborne J: Arguing to learn in science: the role of collaborative, critical discourse. Science 2010, 328(5977):463–466. (2010). doi:10.1126/science.1183944 (2010). doi:10.1126/science.1183944 10.1126/science.1183944View ArticlePubMedGoogle Scholar
- Padian K: Trickle-down evolution: an approach to getting major evolutionary adaptive changes into textbooks and curricula. Integrative and Comparative Biology 2008, 48(2):175–188. 10.1093/icb/icn023View ArticlePubMedGoogle Scholar
- Padian K: How to win the evolution war: teach macroevolution! Evolution: Education and Outreach 2010, 3(2):206–214.Google Scholar
- Vermunt JD, Vermetten YJ: Patterns in student learning: relationships between learning strategies, conceptions of learning and learning orientations. Educational Psychology Review 2004, 16: 359–384. 10.1007/s10648-004-0005-yView ArticleGoogle Scholar
- Vrba ES: The Fossil Record Of African Antelopes (Mammalia, Bovidae) In Relation To Human Evolution And Paleoclimate (pp. 385–424). In Paleoclimate and Evolution with Emphasis on Human Origins. Edited by: Vrba ES, Denton GH, Partridge TC, Burckle LH. Yale University Press, New Haven, CT; 1995.Google Scholar
- Weissert W: Evolution Debate Again Engulfs Texas Board of Ed. AP. 2013. http://bigstory.ap.org/article/evolution-debate-again-engulfs-texas-board-ed. Accessed 10 January 2013.Google Scholar
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