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OPEN ACCESS JCTS Report SERIES B

Baraminological Analysis of the (Synapsida: Pelycosauria) M. Aaron

Cedarville University, Cedarville, OH

Abstract

Previous creationist research has indicated that the level of the created kind is at or near the level in living organisms. However, little research has been done to expand this concept to organisms. In this study, Caseidae, a family of , was analyzed using statistical baraminology. Pelycosauria is a grouping of or “-like reptiles” considered paraphyletic by conventional researchers. Since are thought to share ancestry with by the mainstream scientific community, it is imperative that creationists analyze their relationships using baraminological techniques. If the family rank can approximate the holobaramin among fossil taxa, then one should expect to find discontinuity around the caseids. A cladistic study by Maddin et al. (2008) was reanalyzed using baraminic distance correlation analysis (BDC) and classical multidimensional scaling (MDS). Shared positive correlation was found between all caseids analyzed in this study and is interpreted as continuity. The results from the BDC and MDS suggest discontinuity between caseids and all other taxa analyzed. In light of this analysis, I propose that the family Caseidae is a holobaramin.

Editor: T.C. Wood Received February 28, 2012; Accepted January 30, 2014; Published July 7, 2014

Introduction Caseidae is a family of fossil pelycosaur synapsids known exclusively from beds (Kemp 1982, p. 40; Huttenlocker Hybridization is one of the primary ways that baraminological and Rega 2012, p. 93). Synapsida is a that includes status has been determined for extant organisms (Wood and pelycosaurs, , and modern mammals (Reisz and Laurin Murray 2003, p. 98). Unfortunately, the hybridization test is 2001). The major synapomorphy uniting Synapsida is the unavailable to researchers studying fossil groups. With , presence of the lower temporal fenestrae in the “bounded only morphological and stratigraphic data are available for use above by the postorbital region and squamosal bones, and in determining taxonomic relationships. In addition, fossils are below by the jugal” (Kemp 1982, p. 18). The two major often found incomplete, and there are still gaping holes in our of modern , Diapsida and Synapsida, appear suddenly knowledge of many taxa. Nevertheless, several researchers have in the fossil record simultaneously (Kemp 2012, p. 3). The approached the baraminology of fossil groups with some success, clade is thought to be the sister mainly with a focus on Cenozoic mammal groups including equids group to all amniotes (Kissel 2010, 2011). The (Cavanaugh et al. 2003), archaeocetes (Mace and Wood 2005) Pelycosauria is now considered paraphyletic because it includes and hominids (Wood 2010). The vast majority of fossil groups basal synapsids but excludes their descendants (Botha- have not been studied. This may be due to a lack of creationist Brink and Modesto 2007; Modesto et al. 2011; Kemp 2012, p. 3). paleontologists, or a lack of easily attainable datasets for ancient Caseids are distinguished among the basal synapsids by a stout organisms. However, with the increased use of the internet by body with robust fore and hind limbs, and a “disproportionately paleontologists and other researchers, many new datasets have small cranium with a procumbent snout that overhangs the become available. row” (Maddin et al. 2008). A cast of the skull of

©2014 The author. This article is open access and distributed under a Creative Commons Attribution License, which allows unrestricted use, distribution, and in any medium as long as the original author and medium are credited. Citation: Aaron. 2014. Baraminological Analysis of the Caseidae (Synapsida: Pelycosauria). Journal of Creation Theology and Science Series B: Life Sciences 4:19-22. 33 postcranial characters. Twelve taxa were analyzed in their study: six caseid taxa (Cotylorhynchus; broilii; Casea rutena, now Euromycter rutenus [Reisz et al. 2011]; Angelosaurus; Oromycter; and Ennatosaurus), three other pelycosaur taxa (Eothyris, , and ), the taxon Reptilia, and two diadectomorph taxa (Limonscelis and ). When conducting the baraminological analyses, I removed the taxa Angelosaurus and Oromycter because they did not meet the taxic relevance cutoff of 0.60. The composite taxon Reptilia was also excluded because it holds a taxonomic rank far above the generic level possessed by all other taxa in this analysis. The remaining nine taxa were included in a baraminic distance correlation analysis using BDISTMDS version 2.0 (Wood 2005, 2008; Robinson and Cavanaugh 1998). The character relevance cutoff of 0.75 excluded 23 characters, leaving 83 characters for the analysis. The baraminic distances were then analyzed using Figure 1. Photograph taken by the author of a cast of classical multidimensional scaling (MDS) in order to visualize a the skull and neck of Cotylorhynchus from the Smith- three-dimensional graph of the character space. For comparison to these tests, I conducted another baraminic distance correlation sonian Museum of Natural History in Washington, analysis including the four caseid taxa, Eothyris, and the two D.C. diadectomorph taxa. This analysis had a character relevance cutoff of 0.75 and a taxic relevance cutoff of 0.60, allowing for 71 characters to be utilized. is shown in Figure 1. There is little morphological variation within the family Caseidae, and all appear to have been Results and Discussion judging from their marginal leaf-like teeth and palatal dentition (Maddin et al. 2008; Kemp 2012, p. 4-5). The family Caseidae The baraminic distance correlation graph shows positive was hypothesized to be monophyletic by Maddin et al. (2008). correlation between the four caseid taxa (Figure 2). Positive They identified five synapomorphies as uniting the Caseidae: correlation can also be seen between the two diadectomorph (non- synapsid) taxa, Diadectes and . The two eupelycosaur 1. Medial projection of the lacrimal contributes to narial taxa, Mycterosaurus and Varanops, share significant positive emargination. correlation, but they show negative correlation with the caseid 2. Absence of an anterior tapering of the lower jaw. taxa (Figure 2). This implies continuity within the members 3. First premaxillary tooth is the largest in the tooth row. of Caseidae and discontinuity between the Caseidae and the 4. Shape of the lingual surface of the marginal dentition is eupelycosaur outgroup. The caseids show neither positive nor spatulate. negative correlation to the other taxa. 5. Marginal dentition with lingual shoulder and lingual curvature. The 3D MDS graph likewise supports the caseid monobaramin with large gaps in character space between the caseid cluster Here, I report the results of a baraminological analysis of (circled cluster on the far left of Figure 3), the diadectomorph a published cladistic dataset of caseids using BDISTMDS, a outgroup (cluster on the upper right corner), and the eupelycosaur software program that 1) calculates baraminic distance and outgroup (cluster on the lower right corner). This graph implies estimates the statistical significance of the similarity between that there is continuity within the family Caseidae, and that the two organisms, and 2) plots taxa in 3-dimensional space via family Caseidae constitutes a monobaramin. This combined with multidimensional scaling. Significant positive correlation implies the large area of empty character space between the caseid taxa continuity between organisms and probable inclusion in the same and all other taxa used in this analysis seems to indicate that the monobaramin, whereas significant negative correlation implies family Caseidae constitutes a holobaramin. discontinuity between the organisms. A 3-dimensional graph Because the BDC did not show negative correlation between with clustered data points is obtained through multidimensional Caseidae and the diadectomorphs, I conducted another BDC scaling. Each point represents a taxon existing in multidimensional analysis including the four caseids, Eothyris, and the two character space. Points that cluster close together in character diadectomorph taxa. The negative correlation between Caseidae space imply continuity, whereas large gaps between clusters and the diadectomorph outgroup in Figure 4 substantiates the imply discontinuity. idea that there is discontinuity between the Caseidae and the diadectomorphs. Materials and Methods In Figure 2, it can be seen that the taxon Eothyris shows neither positive nor negative correlation with any of the other Maddin et al. (2008) published a morphological dataset from taxa. In phylogenetic studies, Eothyris and the Oedaleops caseid and several outgroup taxa. A total of 106 characters were form the clade Eothyrididae (Langston Jr. 1965; Reisz et al. used in their study including 73 cranial and dental characters and 2009; Kemp 2012, p. 4). Eothyrididae and Caseidae form the

JCTS B: Life Sciences www.coresci.org/jcts Volume 4:20 clade (Reisz and Dilkes 2003; Maddin et al. 2008; Huttenlocker and Rega 2012, p. 93), which is the sister clade of (Reisz et al. 2009). This baraminological analysis does not confirm or deny this close relationship, although the 3D MDS shows a gap in character space between Eothyris and the caseids. Because Eothyris is only known from a single skull, it is lacking many of the characters used in this baraminological study.

Conclusion

After reviewing the results from the baraminic distance graphs and from the MDS graph, it is apparent that the four caseid taxa Figure 2. Baraminic Distance Correlation graph from this study (Cotylorhynchus, Casea broilii, Euromycter, and of the nine taxa analyzed. Black squares represent Ennatosaurus) share continuity. In addition, the family Caseidae significant, positive correlation, whereas white circles appears to be discontinuous from the outgroup taxa. Based on represent significant, negative correlation. the results of this study, I conclude that the family Caseidae is a holobaramin. However, it must be remembered that this conclusion is based solely on current skeletal morphological data (a very limited subset of the data available from extant organisms), and it may be subject to change as more fossils are discovered. Currently, Eothyris is excluded from the caseid holobaramin; however, it is possible that future fossil discoveries and baraminological analyses may overturn this exclusion. As this is another example of a holobaramin at the family level, this gives further support to the idea that the created kind is approximately equivalent with the taxonomic rank of family in both extant and extinct organisms.

Acknowledgements

I would like to thank Dr. Todd Wood for his assistance in using the BDISTMDS software and in interpreting the obtained Figure 3. Multidimensional scaling results. The four results. As well, I would like to thank Dr. Kurt Wise and Dr. caseid taxa (in blue) cluster together on the left side John Whitmore for assistance in research and interpretation of the of the image and are circled. The two eupelycosaur baraminic status of these organisms. I would also like to thank taxa group in the upper right corner (in red), and the two anonymous reviewers, as their comments and critiques the diadectomorph taxa group in the lower right hand significantly improved this paper. corner (in orange). The genus Eothyris is shown in References green. Cavanaugh, D.P., T.C. Wood, and K.P. Wise. 2003. Fossil equidae: a monobaraminic, stratomorphic series. In: Ivey, R.L., ed. Proceedings of the Fifth International Conference on Creationism. Creation Science Fellowship, Pittsburgh, pp. 143-153. Botha-Brink, J. and S.P. Modesto. 2007. A mixed-age classed ‘pelycosaur’ aggregation from South Africa: earliest evidence of parental care in amniotes? Proceedings of the Royal Society of Biology 274:2829-2834. Huttenlocker, A.K. and E. Rega. 2012. The paleobiology and bone microstructure of pelycosaurian-grade synapsids. In: Chinsamy-Turan, A., ed. Forerunners of Mammals. Indiana University Press, Bloomington, IN, pp. 91-119. Figure 4. BDC graph comparing the caseid taxa to Kemp, T.S. 1982. Mammal-like Reptiles and the Origin of Eothyris and the diadectomorph outgroup. Black Mammals. Academic Press Inc., New York, NY. squares represent positive correlation, whereas white Kemp, T.S. 2012. The origin and early radiation of therapsids. In: Chinsamy-Turan, A., ed. Forerunners of Mammals. Indiana circles indicate negative correlation. University Press, Bloomington, IN, pp. 3-28.

JCTS B: Life Sciences www.coresci.org/jcts Volume 4:21 Kissel, R.A. 2010. Morphology, phylogeny, and evolution of Oedaleops: Do these Early Permian synapsids from New (Cotylosauria: Diadectomorpha). Doctor of Mexico form a clade? Journal of Philosophy Thesis, University of Toronto, Canada, pp. 1-200. 29(1):39-47. Kissel, R.A. 2011. From meat to beet: Phylogeny and evolution Reisz, R.R., H.C. Maddin, J. Fröbisch, and J. Falconnet. 2011. of Diadectomorpha (Tetrapoda: Cotylosauria). Geological A new large caseid (Synapsida, Caseasauria) from the Permian Society of America Abstracts with Programs 43(1):98. of Rodez (France), including a reappraisal of “Casea” rutena Langston, W., Jr. 1965. Oedaleops campi (Reptilia: Pelycosauria) Sigogneau-Russell & Russell, 1974. Geodiversitas 33(2):227- new genus and from the Lower Permian of New Mexico, 246. and the family Eothyrididae. Bulletin of the Memorial Richardson, D. and J. Richardson. 3D Analysis: Mage Display Museum 9:5-47. Software. http://kinemage.biochem.duke.edu/software/mage. Mace, S.R. and T.C. Wood. 2005. Statistical evidence for five php. whale holobaramins (Mammalia: Cetacea). Occasional Papers Robinson, D.A. and D.P. Cavanaugh. 1998. A quantitative of the Baraminology Study Group 5:15. approach to baraminology with examples from the primates. Maddin, H.C., C.A. Sidor, and R. R. Reisz. 2008. Cranial anatomy CRSQ 34:196-208. of Ennatosaurus tecton (Synapsida: Caseidae) from the Middle Wood, T.C. 2005. Visualizing baraminic distances using classical Permian of Russia and the evolutionary relationships of multidimensional scaling. Origins 57:9-29. Caseidae. Journal of 28(1):160-180. Wood, T.C. 2007. The Current status of baraminology. CRSQ Modesto, S.P., R.M.H. Smith, N.E. Campione, and R.R. Reisz. 43:149-158. 2011. The last “pelycosaur”: a varanopid synapsid from the Wood, T.C. 2008. BDISTMDS software, v. 2.0. Core Academy Pristerognathus Assemblage Zone, Middle Permian of South of Science. Distributed by the author. Africa. Naturwissenschaften 98:1027-1034. Wood, T.C. 2010. Baraminological analysis places Homo habilis, Reisz, R.R. and M. Laurin. 2001. The Macroleter: Homo rudolfensis, and Australopithecus sebida in the human First vertebrate evidence for correlation of Upper Permian holobaramin. Answers Research Journal 3:71-90. continental strata of and Russia. Geological Wood, T.C. and M.J. Murray. 2003. Understanding the Pattern Society of America Bulletin 113(9):1229-1233. of Life: Origins and Organization of the Species. Broadman & Reisz, R.R., S.J. Godfrey, and D. Scott. 2009. Eothyris and Holman Publishers, Nashville, Tennessee.

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