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266 tocGeographic and temporal variability in Pleistocene lion-like felids: Implications for their evolution and taxonomy

Martin Sabol, Adam Tomašových, and Juraj Gullár

Article number: 25.2.a26
https://doi.org/10.26879/1175
Copyright Society for Vertebrate Paleontology, August 2022

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Submission: 2 July 2021. Acceptance: 28 July 2022.

ABSTRACT

Several taxa of lions occurred in the Pleistocene of the Northern Hemisphere. Although crania of these large cats are relatively rare in the fossil record, they allow us to assess size and shape differences among Pleistocene lions from Europe, Asia, and North America (Panthera fossilis, P. spelaea, P. atrox) and to compare them with the extant P. leo. We use basic 14 morphometric data (cranial length/width dimensions, auditory bulla diameters, cranial profile) including data on sex and ontogenetic age in 44 fossil and eight recent specimens, along with their geological age and altitude. We show that: first, crania of the P. fossilis (including P. “intermedia”) differs from crania of the Last Glacial P. spelaea and the extant P. leo. Second, P. spelaea shows a high morphologic variation in cranial morphology across its geographic range, with partial morphological segregation between the Western European and Eastern European assemblages. However, the main axis of morphological variation between geographic forms of P. spelaea and P. fossilis-“intermedia” correlates with size (in contrast to major differences relative to P. atrox), and cranial data thus do not consistently differentiate between these geographically and temporally-separated forms. These forms probably represent ecologically-differing geographic populations of the same chronospecies rather than distinct species. Geographic differences are driven by allometry, although other traits such as the teeth may allow their separation in the future analyses. However, the relationships in cranial morphospace still reveal geographic relatedness among subspecies: P. spelaea assemblage from the Western Europe is very similar to P. fossilis-“intermedia”, and contrasts with P. spelaea from the Eastern Europe and Asia. On one hand, such patterns suggest that the western P. spelaea is more related to P. fossilis-“intermedia” lineage and the eastern P. spelaea is related to individuals from Siberia. On the other hand, the similarity between the West-European specimens of P. spelaea (as immigrants from the East) and specimens of P. fossilis-“intermedia” can reflect functional convergence to similar environmental and climatic conditions prevailing in Western Europe.

Martin Sabol. Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Ilkovičova Str. 6, SK - 842 15, Bratislava, Slovak Republic,
Adam Tomašových. Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, SK - 840 05, Bratislava, Slovak Republic,
Juraj Gullár. Reconum - Gullár, Muškátová 32, SK - 821 01, Bratislava, Slovak Republic,

Keywords: Panthera fossilis; Panthera spelaea; Panthera atrox; Panthera leo; Pleistocene; cranial morphology

Final citation: Sabol, Martin, Tomašových, Adam, and Gullár, Juraj. 2022. Geographic and temporal variability in Pleistocene lion-like felids: Implications for their evolution and taxonomy. Palaeontologia Electronica, 25(2):a26. https://doi.org/10.26879/1175
palaeo-electronica.org/content/2022/3681-lion-cranial-variability

Copyright: August 2022 Society of Vertebrate Paleontology.
This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
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INTRODUCTION

Lions (or lion-like felids) form a group of large pantherine cats comprising the extant species (Panthera leo) and its Pleistocene close relatives from the Northern Hemisphere, such as cave lion or American lion. The phylogenetic relationships of these felids and their taxonomic ranking are, however, still controversial and not well resolved. Morphological studies supplemented by molecular data in the past decades have provided support for both the species model (Terzea, 1965; Vereshchagin, 1971; Wiszniowska, 1978; Baryshnikov and Boeskorov, 2001; Sotnikova and Nikolskiy, 2006; Ovodov and Zaika, 2008; Barnett et al., 2009, 2014, 2016; Christiansen and Harris, 2009; Mazák, 2010; Stuart and Lister, 2011; Ersmark et al., 2015; Chernova et al., 2020; Stanton et al., 2020) and the subspecies model (Boule, 1906; Kurtén, 1968, 1985; Hemmer, 1967, 1974; Schütt, 1969; Schütt and Hemmer, 1978; Turner, 1984; Gross, 1992; Burger et al., 2004; Bona, 2006; Diedrich, 2008, 2009, 2011a, 2011b, 2011c; Schouwenburg et al., 2009; Baryshnikov and Tsoukala, 2010; Diedrich and Rathgeber, 2012; de Manuel et al., 2020). In addition, lions with their enormous Pleistocene geographic distribution from Africa through Eurasia up to America show relatively great morphological differences between regions. This is also reflected in certain morphological variations, which may not only be intraspecific variability, but may also be a manifestation of interspecies differentiation. These variations are observed in both dental and cranial morphology (Hemmer, 1974; Yamaguchi et al., 2004; Sotnikova and Nikolskiy, 2006; Barycka, 2008; Mazák, 2010).

Although crania of lion-like felids are relatively rare in the fossil record, some specimens are relatively well-preserved. This enables allometric and multivariate analyses that can be used to assess morphological differences between groups from different regions and stratigraphic units. In our analyses, using basic morphometric data, such as cranial length/width dimensions, auditory bulla diameters, and cranial profile, we assess: 1) whether taxa identified to species level and assigned to P. fossilis (steppe lion), P. spelaea (cave lion), P. atrox, (American lion) and P. leo (extant lion) on the basis of non-cranial morphological characters can be discriminated on the basis of cranial characters, and 2) whether some morphological differences among these extinct and extant lion-like felids from Europe, Asia, Africa, and North America can be rather explained by differences in ontogenic stage, sex, altitude, or stratigraphic age of specimens. Specifically, to assess whether the morphological variability in the cranium of lions can resolve their evolutionary and biogeographic history in response to environmental and climate changes, we evaluate whether craniometric variation in lion crania can discriminate between: 1) the steppe lion and the cave lion; 2) the Western and Eastern European forms of the cave lion; 3) the cave lion and the modern lion, and 4) whether the American lion overlaps with European and Asian extinct lions. Our analyses are based on traditional morphometric measurements and estimate bivariate allometric coefficients of several variables regressed on the log-transformed cranial length, multivariate (principal coordinate) analyses, and analyses of cranial profile angles.

STATE OF ART

s figure1Based on craniometric (and partly also dental) characters, three to four distinct species of lions are traditionally distinguished, which is partly consistent with the results of some more recent molecular and paleogenetic analyses (Ersmark et al., 2015; Stanton et al., 2020) (Figure 1). In this model, the extant lion species represents a lineage that diverged from lineage(-s) of extinct lions during the early Pleistocene, while the cave lion and the American lion evolved from P. fossilis probably around the middle/late Pleistocene transition (Sabol, 2011). However, Hankó and Korsós (2007) inferred from the cladistic analysis that P. spelaea is not a direct descendant of P. fossilis but represents a separate, more advanced lineage. According to molecular and paleogenetic data, the split between extant lion and extinct lion clades could occur approximately 1.85 m.y.a. (Stanton et al., 2020) or 1.89 m.y.a. (Barnett et al., 2016), although younger ages (ca. 500-600 k.y.a.) were also published (Burger et al., 2004; de Manuel et al., 2020). These latest ages, based only on the molecular estimates or the whole genome data, are too low and do not correspond with the fossil record (Sala, 1990; Lewis et al., 2010).

In P. leo, the northern (P. leo leo) and southern (P. leo melanochaita) lineages are distinguished on the basis of craniometric data (Mazák, 2010), although their morphological diagnoses are so far unknown (Kitchener et al., 2017). Based on the simulation of population history, de Manuel et al. (2020) estimated the divergence between both these leo lineages at ca. 70 k.y.a. However, Bertola et al. (2016) put the split of extant lion lineages at 244.8 k.y.a., which better corresponds with the fossil record. In any case, this divergence of the extant lion lineages took place later than in the case of the lineage(-s) of extinct lions, although lion-like felids had existed in Africa for more than 3 m.y.a. (see Sabol, 2011: p. 229-230, and references therein).

The oldest non-African representative of extinct lions is P. fossilis occurred in the European fossil record for the first time during MIS 17 (~ 680 k.y.a.) at Pakefield (Lewis et al., 2010) and Kozi Grzbiet (Marciszak et al., 2021), or during MIS 15 (~ 610 k.y.a.) at Isernia la Pineta (Sala, 1990; Hemmer, 2011), respectively. Its first appearance is, however, probably much earlier as evidenced by finds from late early Pleistocene sediments in Western Siberia, correlated with the Jaramillo Subchron (Sotnikova and Foronova, 2014). This lion form persisted at least until MIS 6 period mainly in Europe (Wurm, 1912; Thenius, 1972; Kurtén and Poulianos, 1977; Argant, 1988, 2010; Marciszak et al., 2014, 2019; Sabol, 2014; Argant and Brugal, 2017), from where it is originally mentioned in two chronosubspecies, as P. spelaea fossilis (>MIS 17-MIS 10/9) and P. spelaea intermedia (~ MIS 10/9-MIS 6) (Argant and Brugal, 2017; Marciszak et al., 2019). These taxa significantly differ, inter alia, in the shape of the nasofrontal cranial profile from late Pleistocene cave lions. The fossilis-lineage diverged from other extinct lion lineages certainly more than 1.0 m.y.a., since the first split of cave lion clades is assumed after this period (Stanton et al., 2020). However, this oldest cave lion split (Clade A, 0.97 m.y.a.) should be treated with the caution (Stanton et al., 2020), because it is based only on one site record in Bilibino (Russia) with different radiocarbon data (Kirillova et al., 2015). In addition, the molecular tip dating estimates its age only at 643 k.y.a. (Stanton et al., 2020), which better corresponds to the assumed divergence period from the ancestral lineage.

According to Stanton et al. (2020), the better documented split of spelaea-lineage (Clades B and C) took place around 578 k.y.a. Clade B can be identified with P. spelaea vereshchagini that inhabited Beringia probably in the time span between 419 k.y.a. and 28.0 k.y.a., whereas Clade C contained Eurasian specimens dated between 311 k.y.a. to 12.4 k.y.a. (or 11.2 k.y.a.; see Argant, 2010) and can be identified as P. spelaea spelaea. Both subspecies differ significantly in size (Baryshnikov and Boeskorov, 2001) and perhaps also in prey preferences (Guthrie, 1990; Matheus et al., 2003; Bocherens et al., 2011; Diedrich, 2012; Kirillova et al., 2015), although this is conditioned by number of factors. The genetic diversity of cave lions has already been noted by Ersmark et al. (2015) and the division of these extinct felids into at least two groups was also reported in earlier morphometric studies (Hemmer, 1974; Yamaguchi et al., 2004).

American lion, formerly assumed to be a descendant of Asian populations of Panthera fossilis (e.g., Sabol, 2011 or Sotnikova and Foronova, 2014) or placed inside the basal diversity of spelaea-form with the estimated genetic (reproductive) isolation at around 337 k.y.a. (Barnett et al., 2009), is today rather considered to represent an extinct lineage that diverged from a Beringian population approximately before 165 k.y.a. (Salis et al., 2021). However, these latest paleogenetic data are not supported by morphological analyses (Merriam and Stock, 1932; Simpson, 1941; Kurtén, 1965; Thenius, 1972; Christiansen and Harris, 2009; Benoit, 2010), which suggest that the American lion has retained more primitive characters than the coeval Eurasian cave lion (Sotnikova and Foronova, 2014). In addition, the analyses of mtDNA from American and cave lions are consistent with a degree of reproductive isolation, suggesting some degree of competition between these sister taxa (Barnett et al., 2009). On the other hand, certain dispersal scenarios could also lead to a late divergence date of P. atrox with more primitive characters.

The second, subspecies model is based primarily on molecular tip-dating methods (Burger et al., 2004; de Manuel et al., 2020) and supports the subspecies status of all lion forms, belonging to the single species P. leo (P. leo fossilis, P. leo spelaea, P. leo atrox). Within the scope of this paper, we follow the species model for the taxonomic determination of analyzed crania of single lion forms.

MATERIAL AND METHODS

The cranial analyses here were based on original morphometric data collected from paleontological and zoological collections of the Slovak National Museum-Natural History Museum in Bratislava (SNM-PM), Slovak Museum of Nature Protection and Speleology in Liptovský Mikuláš (SMOPaJ), National Museum in Prague (NMP), Moravian Land Museum-Anthropos in Brno (MZMA), and Natural History Museum in Vienna (NHMW) as well as on morphometric data and photographs published in the scientific literature. All analyzed specimens are listed in Appendix 1. The morphometric dataset consisted of 14 main linear cranial measurements, a categorical variable referring to the shape of the cranial profile, and three angle measurements, stratigraphic age, and site altitude of 52 lion-like felid crania (34 adult males and 18 adult females). Among eight crania of the extant lion (from Cameroon, Chad, Senegal, Tanzania, Zambezi, two unknown African sites, and western India) only two specimens belong to animals that originally did not live in the wild (specimens from SNM-PM). The rest of the material is represented by nine crania of P. atrox (Ichetucknee, Natural Trap Cave, and Rancho la Brea), two crania of P. fossilis (Mauer and Azé I-3), 27 crania of P. spelaea (Bottrop, Huttenheim, Perickhöhlen, Siegsdorf, Zoolithenhöhle, Zandobbio, Brno, Sloup, Srbsko-Chlum, Výpustek 1 and 3, Igrita, Ursilor, Binagady, Desna, Isa, Kondakovka, Mokhokho, Uzhur, and Medvedia Cave in the Western Tatras), and six crania of P. “intermedia” (Romain-la-Roche, Vence, Edingen, Niedźwiedzia, San, and Petralona; all originally attributed to “fossilis-spelaea” or “primitive spelaea” forms). The latter taxon is, according to Argant and Brugal (2017), an intermediate form between steppe and cave lion, and the crania of P. fossilis and P. “intermedia” are thus assigned to one taxonomic group (P. fossilis below). In our analyses, we primarily assessed differences in the size and shape of crania among these four groups (P. fossilis, P. spelaea, P. atrox, and P. leo). In some analyses, we also assessed differences between the Western European P. spelaea and the Eastern European-Asian P. spelaea. As the sexual dimorphism in pantherine cats is relatively high (Mazák, 1980; Mazák, 2004, 2010), we account for the effects of sex by assigning each cranium to male or female on the basis of morphometric data. The assignment of specimen to species is primarily based on non-cranial characters or on other criteria not based on cranial morphology.

s figure2The 12 linear cranial characters (Figure 2) are as follows: the greatest cranial length (L), the palatal length (LP), the medial length of nasals (LMN), the lateral length of nasals (LLN), the greatest nasal width (BN), the snout width (BS), the interorbital width (IOB), the width across zygomatic arches (BZ), the postorbital width or constriction (POC), the greatest neurocranial width (BNC), the mastoid width (BM), and the greatest diameter of the auditory bullae (LAB). In addition to these variables, we have measured two profile depths on crania (the profile depth and the profile depth of assumed straight cranial profile) and three angles (the cranial profile angle-angle A, the angle between narial aperture and nasofrontal profile-angle B, the angle between alveolar margin and postorbital process-angle C) to quantify the shape of the nasofrontal region (Figure 3). s figure3The profile depth and the cranial profile angle are related to the shape of the profile of the nasofrontal cranial area. In relation to that, three basic types of crania are distinguished (Figure 4)-with straight nasofrontal profile (0), with concave nasofrontal profile (2), and a profile that is intermediate between the two end-member types (1). The measurement methods of lion crania follow Argant (1991) and Christiansen and Harris (2009). The measurements were taken to the nearest 0.1 mm using engineering vernier calipers with 0.3 mm standard deviation, 0.1 mm dispersion, and 4.2% random error. Except for angles, all measured data are given in millimeters (see Appendix 1).

s figure4Although the total number of specimens is limited, this cranial morphometric dataset allows us to test whether crania of these apriori-defined species differ with univariate, bivariate, and multivariate methods. Some analyzed crania are, however, incomplete and thus not all cranial characters were measured on these specimens. First, we compared median differences in three angle dimensions among the four groups in univariate analyses (visualized in boxplots and tested with the Wilcoxon rank-sum test). Second, we measured bivariate allometric coefficients between cranial length and other morphological log-transformed dimensions based on the subsets of crania with the available measurements, using the reduced major axis regressions. Third, to explore multivariate variation in cranial morphology among all specimens, we used the principal coordinate analysis that allows for missing measurements (using Euclidean distances), based on log-transformed dimensions of 14 cranial characters. We use the permutational multivariate analysis of variance (PERMANOVA) to test whether between-group variation on the basis of 14 variables is larger than within-group variation. To summarize, we assessed univariate, bivariate, and multivariate differences in cranial morphology: 1) between P. fossilis (incorporating specimens assigned to P. “intermedia” to this group) on one hand and P. spelaea on the other hand; 2) between nine specimens of P. spelaea from Western Europe (Germany and Italy) differ from 18 specimens of P. spelaea from Eastern Europe and Asia (Siberia); 3) between P. atrox and other groups, and 4) between P. spelaea and P. leo.

RESULTS

Cranial Lengths

s figure5The crania of Panthera species differ distinctly in size (Miththapala, 1992; Mazák, 2004, 2010) in comparison to crania of lion-like felids, where considerable size overlaps are recorded among species (Turner, 1984; Mazák, 2010; Sabol et al., 2018). Cranial lengths of P. atrox and P. fossilis tend to be larger than cranial lengths of P. spelaea, which are in turn tend to exceed cranial lengths of P. leo (Figure 5). However, some differences can be observed when the interorbital width (IOB) and the postorbital constriction (POC) are plotted (Figure 5). The logged POC/IOB ratio of all species observed here generally overlaps with the total range of variability documented by Mazák (2010) for P. leo. However, the median POC/IOB ratio is higher in the Recent P. leo (median =-0.02) than in all extinct Panthera species (between-0.05 and-0.06; Figure 5). Mazák (2010) also documented that this ratio is sex-dependent, but median per-region POC/IOB ratio is between-0.05 and 0 for African P. leo, whereas it is smaller in Asian P. leo and in the Pleistocene P. spelaea.

Analyses of Profiles and Angles

s figure6Other differences are evident in the analysis of the nasofrontal profile. From three defined morphological types, the straight nasofrontal profile (0) prevails in the analyzed lion crania. It was observed predominantly in Last Glacial cave lions from Central and Eastern Europe, but also in Siberian and American lions, as well as in extant P. leo. Lions with such nasofrontal profile have also been depicted by Paleolithic artists on the cave walls of Chauvet, La Marche, or Aldène (Figure 6). The concave nasofrontal profile (2) occurs in lion-like felids from the mid-middle Pleistocene (Holsteinian) to the early late Pleistocene (Eemian), mainly of Western Europe and Poland (Niedźwiedzia and San), but sporadically also in crania from the Last Glacial of Moravia (Sloup Cave) or even from Siberia (Kondakovka). This type of profile was probably present also in lion cranium from Mauer (P. fossilis) and is clearly visible on some manifestations of the Paleolithic art, such as lion head sculpture from Kostenki (Figure 6). A “link” between above mentioned cranial profiles (1) is rarely observed in lion crania from Edingen, Petralona, Zoolithen, and also in extant lions (SNM-PM C 1521 and SNM-PM 1701). Based on the figured giant lion cranium from Kenyan site of Natodomeri (Manthi et al., 2017, figure 3), it seems that this individual could also belong to this group.

s figure7Boxplots in Figure 7 show that cranial variables related to the shape of their nasofrontal profile discriminate between crania assigned to P. fossilis and P. “intermedia” on one hand and those assigned to P. spelaea on the other hand. The profile angle (angle A) is significantly less concave (Wilcoxon test, p<0.001) and the premaxillary-nasofrontal angularity (angle B) is significantly larger, i.e., less sharp (Wilcoxon test, p<0.001) in P. spelaea (median profile angle = 174-175°, median of angle B = 141-144°) than in P. fossilis (median profile angle = 164°, median of angle B = 138°). The profile angle is also less concave in P. atrox (median profile angle = 177°, median of angle B = 143°) than in P. fossilis. The median of angle B is also significantly higher in P. leo (149°) relative to P. spelaea (Wilcoxon test, p =0.02) and in other species. Therefore, these groups of lions can be discriminated on the basis of the profile of the nasofrontal region. The two geographic subgroups of P. spelaea do not differ in the three angle characters (Wilcoxon test, p<0.001).

Bivariate Allometric Coefficients

s figure8Bivariate relationships between the cranial length and other morphological variables document some consistent between-group differences in allometric coefficients (Figure 8-Figure 9). First, although 95% confidence intervals tend to be broad, these coefficients demonstrate more positive allometry for mastoid width, snout width, medial nasal length, and lateral nasal length in P. fossilis relative to other three species. Second, the postorbital width (POC) increases slowly with increasing cranial length (negative allometry) in P. leo and in P. atrox whereas it increases at higher rate in P. spelaea and P. fossilis. Third, zygomatic width, snout width, and medial nasal length increases at slower rate relative to the cranial length in P. atrox (negative allometry) relative to other species where these traits show positive allometry (Figure 9). It can be seen in Figure 8G that the palatal length shows an isometric relation relative to overall size in all species, but the difference in intercepts between P. atrox and the other groups effectively contributes to the second PCO axis that separates the American lion from other species. The postorbital constriction width shows positive allometry in P. fossilis and P. spelaea, but negative allometry in P. leo and P. atrox (Figure 8I).

Multivariate Analyses

s figure9The first two axes of principal coordinate analysis (PCO) explain 92% of among-specimen variation in cranial morphology (Figure 10A). First, multivariate analysis of variance shows that on the basis of 14 cranial characters, P. atrox is clearly segregated from other Panthera species along the PCO axis 2 (PERMANOVA F=5.05, p=0.01). Second, crania of P. fossilis (including P. “intermedia”) differ weakly from P. spelaea ones, with borderline significance (PERMANOVA F=3.5, p=0.04), being primarily separated along the PCO axis 2. Third, P. spelaea crania are characterized by high variability that overlaps to some degree with P. leo and with P. fossilis. However, despite this overlap, the distance between multivariate means of P. spelaea crania from Eastern Europe and Western Europe is higher than within-group distances between the means and crania of constituent individualss figure10 (PERMANOVA, F=6.02, p=0.004), and are partly separated along the PCO axis 1. However, P. fossilis and P. “intermedia” do not differ from the Western European assemblage of P. spelaea alone, and the overall difference between P. spelaea (across its whole geographic range) and P. fossilis is driven by the Eastern European assemblage of P. spelaea. In turn, pooling the crania of P. spelaea from western regions with P. fossilis and P. “intermedia” into one group forms a set that significantly differs from crania of P. spelaea from Eastern Europe and Asia (PERMANOVA F=5.1, p=0.003). Morphological differences between geographic variants of P. spelaea and among P. spelaea and other forms remain in the PCO analysis when P. atrox is excluded (Figure 10B). Figure 11 s figure11shows that all variables strongly correlate with the PCO axis 1 (with weaker correlations related to braincase width and auditory bulla), similarly as in the exhaustive analysis based on all species, and the nasale width, palatal length, auditory bulla, and the full profile depth correlate with the PCO axis 2. The morphological separation among P. fossilis and P. spelaea still occurs along the PCO axis 1, with a marked overlap between the Western forms of P. spelaea and P. fossilis. However, P. fossilis is also slightly offset along the PCO axis 2, indicating that a shift in morphospace is unrelated to size-related shift in morphology along the PCO axis 1.

We note that the effects of sexual differences and altitudinal effects are small and insignificant, although the detection of such effects is limited by the small sample size (i.e., small number of crania).

DISCUSSION

Relationships Between Extinct and Extant Lions

The morphological differences in the dentition and skulls between extinct (Hemmer, 1974; Baryshnikov and Boeskorov, 2001; Yamaguchi et al., 2004; Sotnikova and Nikolskiy, 2006; Barycka, 2008; Christiansen and Harris, 2009; Benoit, 2010; Marciszak et al., 2014, 2019) and extant lions (Mazák, 2010) in former analyses indicated a certain variability, what was also reflected in taxonomic studies still before the more demonstrable results of molecular and paleogenetic analyses. One of the most conspicuous different features in the cranial morphology is a shape of the cranial profile in the nasofrontal region, known also from the Paleolithic art. Our analyses confirm the existence of differences in cranial morphology between extinct and extant lions. These analyses also show some geographic differences between the Pleistocene forms themselves, although the overall within-group variability exceeds differences among groups (e.g., between Western European P. spelaea and P. fossilis), and the cranial morphology rather supports the chronospecies model.

The crania of P. leo are generally smaller, showing the higher median POC/IOB ratio and the higher median of angle B compared to crania of extinct lions. On the other hand, Hemmer (1974) mentioned certain similarities of modern North African-Asian lions with the middle Pleistocene lions in cranial morphology. But the “fossilis-intermedia” lions are clearly different from other lions in the distinct concave nasofrontal profile and demonstrate also more positive allometry for the mastoid width, snout width, medial nasale length, and lateral nasale length. When results of multivariate analyses are considered, their crania show some resemblance to those of Western European cave lions, which are separated from crania of cave lions from the Eastern European-Asian region. However, both these geographical subgroups of cave lions do not differ in their angle characters. The division of European cave lions into at least two groups (west and east ones) based on cranial morphology was first pointed out by Hemmer (1974), and later also by Yamaguchi et al. (2004) or by Barycka (2008). This variability observed was considered either as a consequence of the invasion of Siberian lions (Hemmer, 1974) or as a result of the penetration of modern lions from SW Asia already during the Pleistocene (Yamaguchi et al., 2004).

Relationships Between P. atrox and Other Lions

Unlike to above mentioned lion taxa, the American lions form a separate, clearly different group in our multivariate analysis. This separation supports the results of some previous morphological observations (Merriam and Stock, 1932; Thenius, 1972; Martin and Gilbert, 1978; Baryshnikov and Boeskorov, 2001; Christiansen and Harris, 2009; Benoit, 2010; Sakamoto and Ruta, 2012). On the other hand, their crania are also characterized by the straight nasofrontal profile, which is predominantly present in most crania of cave and modern lions.

Relationships Between P. spelaea and P. fossilis–Chronospecies Model

Based on the differences in the cranial morphology observed among individual lion forms, these could constitute separate taxonomic units, as assumed by the species model. However, the originally estimated age of the split of extinct lion lineage(s) from the extant one (Burger et al., 2004) based on molecular tip-dating (ca. 0.6 m.y.a.) did not support their taxonomic status as separate species since the entire extinct lion clade(-s) was considered too young (at least according to the criteria of Kitchener et al., 2017). On the other hand, if dating using the fossil record and some recent molecular data (Stanton et al., 2020) are correct, this split between extant and extinct lion lineages must have already occurred during the early Pleistocene (ca 1.8-1.9 m.y.a.). In this case, extinct lions would be acceptable as a Holarctic clade distinct from the P. leo clade, forming at least one separate species (P. spelaea) with some subspecies. Its division into several separate species is also not excluded, but their taxonomic position may not be stable in terms of the value of observed morphological characters, which may be related to various factors influenced by local climate and environmental conditions. A similar situation can also be observed in the study of cave hyenas, where it is still discussed whether European and Asian populations are different species, even though they were separated for at least 2.0 million years ago (Westbury et al., 2020).

However, multivariate analyze show, first, that the major axis of variation among specimens of P. spelaea and P. fossilis-P. “intermedia” occurs along the first PCO axis, but this axis also correlates with the size of all variables (with the exception of palatal length). As in many other similar morphometric analyses, this axis thus largely captures size variability. Therefore, morphological differences between the western and eastern forms of P. spelaea as well as between the cave lions and P. fossilis-P. “intermedia” can be largely accounted for by size variation. Second, high variability of P. spelaea is probably accentuated by long temporal coverage of specimens of this species (middle-late Pleistocene, up to the Last Glacial Maximum) relative to the snapshot nature of P. leo specimens collected just in the twentieth century. Longer temporal span of morphometric variability assessed over long temporal duration (covered specimens of P. fossilis and P. spelaea) can be coupled with the temporally-shifting adaptive landscape, leading to presence of transient traits related to temporally-unique climatic conditions or to the development of transient geographic barriers.

In fact, the species defined in the fossil record often represent only the chronospecies of a continually-evolving biospecies. P. fossilis and P. spelaea can represent such an example of a chronospecies (as also inferred for hyenas; Rohland et al., 2005). Although these lions are considered to be a separate species based on their morphological characters and, of course, stratigraphic position, our analyses indicate high overlap between these two temporally-separated forms, suggesting that they rather grade into each other. The American lion can retain a separate species status, because it distinctly differs from other lions in morphology and paleobiogeographical distribution. Its separate position in our analyses can result from its rapid divergence after dispersal to the southern part of North America. From this point of view, a higher number of well-preserved and stratified cranial material, analytically also integrated with non-cranial data, will be needed to future confirm the subspecies model in lions.

Multivariate analysis of all forms that potentially belong to one chronospecies indicates that one source of variation relates to geographic partitioning of populations. On one hand, the morphometric patterns that show the gradation between Eastern and Western European P. spelaea and their relation to P. fossilis can suggest that the West-European P. spelaea is more related to P. fossilis and P. “intermedia” lineage and the East-European P. spelaea is related to immigrants from Siberia. On the other hand, the similarity between the West-European specimens (as immigrants from the East) and specimens of P. fossilis-“intermedia” can reflect a functional convergence to similar environmental and climatic conditions prevailing in Western Europe. More complex scenarios due to secondary mixing or hybridization among populations of different (sub-)species are also possible.

One of the last unresolved questions, although beyond the scope of this paper, is related to the causes of the transition from concave to straight nasofrontal profile during the evolution of lions. The influence of sexual differences and altitudinal effects in this process was negligible, and the formerly assumed influence of the individual age on the cranial profile shape (Schütt and Hemmer, 1978) was also shown as insignificant. A similar transition is observed between the crania of brown bear (Ursus arctos), with a more concave nasofrontal profile, and polar bear (Ursus maritimus), with a straighter nasofrontal profile. This transition is probably caused by adaptation to life in colder climatic conditions and/or by different dietary requirements. Did similar processes also play a role in the “straightening” of the nasofrontal profile on lion crania? Although the role of cold climate and diet preferences cannot be completely ruled out, other factors have probably played a role here, as straight nasofrontal profiles also occur in modern lions inhabiting subtropical to tropical climate zones. It seems that this transition could be related to the adaptation to hunting of large, metabolically valuable prey (Carbone et al., 1999). According to Sakamoto and Ruta (2012), however, the shape of cranium may not have been a result of direct selection forces, and its evolution was rather a result of selection based on the influence of latent factors such as function, ecology/environment, or development.

CONCLUSION

The craniometric dissimilarities documented in our study visualize certain variations among extinct and extant lions, which can relate to phenotypic variances or can also indicate a more distinct differentiation among separate lion forms what can relate to a different range of their temporal and spatial distribution. The results of our analyses show that, with the exception of American lion, the overall differences between fossilis and spelaea groups (1) are rather minor and reflect differences in size and allometric consequences, but (2) are also affected by high size and shape variation that is geographically structured, with the partial difference between the Western and Eastern European forms of P. spelaea and with a similarity between the Western European P. spelaea and P. fossilis. These lions can, therefore, be considered as chronospecies within one common clade (P. spelaea). However, this chronospecies model should be supported with further research, as the similarity in some cranial characters between middle Pleistocene steppe lions (fossilis-“intermedia”) and Western European cave lions from the late Pleistocene may not only indicate phylogenetic affinity but may also reflect a functional convergence based on similar environmental and climatic conditions prevailing in Western Europe. The cranial variability observed between Western European and Eastern European-Asian cave lions could be related to various migration events. The American lion clearly differs from other lion forms and could be considered a separate taxon (P. atrox). The observed different characters in the cranial morphology of the extant lions also support their independent species status (P. leo) with respect to extinct lion forms. The future research should include not only the higher geographic coverage of the cranial material but also non-cranial material, and a better understanding of lion evolution can only be obtained by integrating diverse analytical procedures. In this context, the trend towards the straightening of the nasofrontal profile of lion crania during the Pleistocene can also be resolved.

ACKNOWLEDGMENTS

The research for this paper was carried out with financial support from the Slovak Research and Development Agency (project APVV-20-0079 [M.S.]) and from the Slovak Scientific Grant Agency (project VEGA 0169/19 [A.T.]). The authors also gratefully acknowledge the helpful comments and suggestions of anonymous reviewers for improvement of the manuscript. Their gratitude goes also to Editor M. Stewart for handling the manuscript.

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