We investigated the variation in complexity of the lower first molar M1 of the common pine vole Microtus subterraneus. Eight different morphotypes were found. The M1 with additional structures was significantly longer than the ‘typica’ morph. This structural gain is not caused by alternating dentin triangles, as known from Microtus arvalis or M. agrestis, but by a second ‘pitymys’ field in combination with a complete anterior lobus. This morphotype is named ‘pitymys +’. Two possible routes towards increased complexity are described and depicted schematically. It depends on whether, initially, the anterior lobus narrows to the ‘maskii’ morph, and the new and complete anterior lobe will be constricted in the following step out of the remaining loop. Alternatively, additional anticlines are first formed at the anterior lobe, and the constriction of the second ‘pitymys’ rhombus takes place in the next step.
Introduction
The occlusal surfaces of the molars of rodents of the subfamily Arvicolinae show a characteristic pattern of angles and folds along the lingual and labial borders of the teeth. Their shape is of particular diagnostic importance. They are a distinctive feature used for the discrimination of genera and species, but also display considerable intraspecific variation, particularly in the first lower molar M1 (Kapischke et al. 2009, Kapischke & Kuhlisch 2016, Jentzsch & Lorenz 2019). Such forms can, in turn, occur in different species and genera in similar forms as homologous series (Ognev 1950, Angermann 1974). Minor deviations in form are neglected in classification, which leads to a ‘coarsening of the facts’ (Angermann 1974). This is evidence of evolutionary and intraspecific shape change (Guthrie 1971, Kapischke et al. 2009, Seelig et al. 2021).
The ‘pitymys’ rhombus on M1 is an important identifying feature of the common pine vole Microtus subterraneus, along with twelve other species (Kryštufek et al. 1996, Markova 2014), and is used to distinguish it from other Arvicolinae tooth patterns (Gaffrey 1961, Niethammer & Krapp 1982, Turni 1999). The nomenclature of this tooth form dates from the earlier categorisation of the short-eared mouse in the genus Pitymys (Kraft & Kapischke 2008).
Fig. 1.
Variants of the first lower molar (M1) of the common pine vole, Microtus subterraneus (a – ‘typica’, b – apical knob swaged, c – lingually additional salient angle on the anterior loop, d – almost ‘maskii’, e – buccally implied additional salient angle (red arrow), f – buccally pronounced additional salient angle and incomplete second ‘pitymys’ rhombus, g – ‘maskii’, h – ‘pitymys +’).

Based on the respective ‘typica’ morph, the variability of molar pattern, especially of M1, has been described by numerous authors (e.g. Angermann 1974, Zahreddin 1989, Kapischke et al. 2009). Additional data on aberrations of M1 in M. subterraneus populations from different German counties and some single findings from Romania and Bulgaria are presented.
Material and Methods
The skulls and lower jaws were collected at different times and locations in Germany, Bulgaria and Romania (see Table S1). Because it was not always possible to match the mandibles to each other, only the available M1 are considered below. The material was lent from different collections: Museum Mauritianum Altenburg (28 M1), Senckenberg Museum of Natural History Görlitz (17), Museum of Natural History Erfurt (2) and the private collection of Dr. Dietrich von Knorre (83), Dr. Martin Trost (16), and the first author (22). A total of 91 left and 77 right M1 were included, of which 38 M1 occurred in pairs (Table 1). Most of the material was extracted from owl pellets, and some specimens were trapped. The study refers to the total material because much of the material occurred as single skulls and mandibles or as small series per location. Summarising all the material was beneficial for the length measurements in connection with the occurrence of the various morphs to obtain the greatest possible amount of data for analysis.
The determination of species has been proven by the discriminant analyses of Kraft & Kapischke (2008). Altogether, 168 M1 were classified according to the criteria for dental morphs proposed by Grummt (1961), Angermann (1974) and Zahreddin (1989) and supplemented by intermediate stages. Only the material from Saxony, Saxony-Anhalt, and Thuringia with at least 28 analysable teeth was used for regional comparisons of the frequency of morphs.
Microsoft Excel (version 2019, Microsoft Corporation, Redmond, Washington, USA) was used for the data collection and processing and the creation of selected diagrams. The IBM SPSS Statistics program (version 23, SPSS Inc., Chicago, Illinois, USA) was used for further descriptive and inferential statistical analyses.
The length measurements of the M1 were carried out for statistical analyses using the corresponding function of the VHX-5000 digital microscope from KEYENCE. The data for the two different groups (‘typica’ and non ‘typica’) were compared. The molar lengths were normally distributed, as shown by the Kolmogorov-Smirnov test and visual analysis using Q-Q diagrams (Weiß 1999). A test for homogeneity of variance between the groups was also carried out for the molar lengths using the Levene test (Weiß 1999). Significant mean differences between the two groups were determined using an independent samples t-test (du Prel et al. 2010).
Results
Morphotypes of M1
A total of eight different morphotypes were identified (Figs. 1a-h). In general, the M1 of the common pine vole has a rounded apical knob of the anterior loop, five lingual and four buccal salient angles (5/4), three closed triangles, and the typical ‘pitymys' rhomb (forma ‘typica'; Fig. 1a). Based on this form, the anterior loop can be distinctly swaged in some molars (Fig. 1b) and shows lingually an additional salient angle (6/4; Fig. 1c) that resembles that of a knight chess piece. The anterior lobe is similar to that of Microtus oeconomus (Pallas, 1776), but otherwise, the whole molar has the typical pattern of M. subterraneus. Other patterns show almost or completely constricted anterior lobes (5/4, ‘almost maskii', Fig. 1d; 5/4 ‘maskii’, Fig. 1g). The latter presents two complete ‘pitymys' rhombuses, but only an incomplete anterior lobe. Another development towards increased molar complexity can be seen in the case of a buccally implied additional salient angle (6/(5); Fig. 1e, red arrow), followed by a buccally pronounced additional salient angle and incomplete second ‘pitymys' rhombus (6/5; Fig. 1f). The most significant increase in structure is shown by an M1 from Weiden in Thuringia, in which a second ‘pitymys' rhomb appeared and a complete anterior lobus with two salient angles was formed (Fig. 1h). To emphasise the existence of a second ‘pitymys' rhomb, we propose the term ‘pitymys +' for this morph. The two similar morphs, ‘typica’ and ‘typica’ with swaged apical knob, were the most common in our study (57.1%), followed by ‘maskii’ and almost ‘maskii’ (31%). There are differences between the regions. While the ‘typica’ morphs are also the most common in Saxony and Thuringia, those of Saxony-Anhalt revealed the ‘maskii’ morph with the highest frequency (Table 1).
Table 1.
Proportion of the respective morphs in the total number of analysed M1 per region in % (n = number).

Twenty of the 38 pairs of left and right M1 showed symmetrical structures (52.6%), five in the ‘typica’ morph (13.2% of all pairs, 25% of all symmetrical pairs). In the 18 pairs of asymmetric M1, there was no tendency in favour of one side of the body in relation to the more complex structure: eight pairs showed the more complex structure in the left M1 and ten pairs in the right. The average length of all first lower molars was 2,350 ± 106.1 µm (mean ± SD). The length of the only M1 showing the ‘pitymys‘morph was 2,419 µm and belonged to the top fifth (20.8%) of all tooth lengths.
The length of the ‘typica’ molars was 2,320.5 ± 93.5 µm, and of the non ‘typica’ molars 2,362.0 ± 108.8 µm. The distribution of molar lengths of M1 among study groups is shown in Fig. 2. There were no differences in the homogeneity of variance in molar length between the groups (P = 0.424). However, there were significant differences in molar length between the two groups (P = 0.022).
Discussion
While the different enamel types of teeth are mainly functionally determined, the taxonomic value of the enamel structures is limited primarily to the level of enamel patterns (von Koenigswald & Pfretzschner 1991). The changes in enamel patterns can be attributed to functional differences (Herrmann 2002), whereby this development is subject to morphological limits (Polly 2012). The complexity of the molars follows a linear morphogenetic gradient along the molar row (Herrmann 2002, Seelig et al. 2021) and environmental factors such as climate or the availability and composition of the diet play a distinct role in the development of such morphs, along with the lifestyle of the species (Renaud et al. 2005, Piras et al. 2012, Seelig et al. 2021). Overall, the changes in the molars are mediated by the ecology of the animals (Seelig et al. 2021). In terms of feeding ecology, this ultimately corresponds to the thesis of von Koenigswald (1982) and Guthrie (1971) that a more complex structure of the tooth surface, i.e. the development of more partial surfaces, increases chewing efficiency and favours the mechanical crushing of hard plant parts.
Fig. 2.
Violin plot illustrating the distribution of molar lengths (in µm) for the two groups examined.

While numerous identification keys refer to the typical tooth pattern of M. subterranes with the three closed dentinal triangles and the ‘pitymys’ rhombus (forma ‘typica’, e.g. Niethammer & Krapp 1982, Angermann & Hackthal 1995, Turni 1999), there are several publications dealing with different patterns and tooth morphs of this species (e.g. Zahreddin 1989, Kraft & Kapischke 2008, Barkaszi 2017). Many of these patterns are considered to be homologous series that occur in different species of Arvicolinae (Ognev 1950, Angermann 1974).
In most Arvicolinae, the structural gain of the first lower molar M1 is due to an alternating gain of dentine triangles. In M. agrestis (Linnaeus, 1762), for example, the gain is described as starting from five closed dentin triangles (‘typica’) via a sixth buccal (Jentzsch 2006) to a seventh labial triangle (Kapischke et al. 2009). In contrast, our study reveals a different tooth development in M. subterraneus. The structural gain is achieved by a second ‘pitymys’ field in combination with a complete anterior lobus (‘pitymys +’ morph). This morphotype is presented here for the first time. In the monograph of Mohr (1954), Fig. 76 comes closest to this variant, showing the anterior lobus of a ‘maskii’ morph in which the salient angles of the new lobe are already faintly indicated.
In our mandibles, the increase in the structure of M1 was accompanied by a significant increase in length. Comparable studies on M. subterraneus or other Arvicolinae were not available. Overall, the average lengths of different populations differ slightly from each other. The average value of the M1 tooth lengths given in Niethammer (1972) is 2.53 mm. The same value for our mixed samples from different locations is lower at 2.35 mm. The average value of the nine mandibles from the Pleistocene from Serbia is between the two at 2.46 mm (Bogićević et al. 2012).
Fig. 3.
Theoretically possible ways and intermediate steps of the gain in complexity in the pattern of the first lower molar of the common pine vole Microtus subterraneus towards the variant ‘pitymys +’. On the left side, the development runs through various ‘typica’ variants, and on the right, through those of ‘maskii’.

These and the cited studies represent solely morphological studies. The extent to which genetic analyses can also substantiate the described intraspecific diversity could not be clarified in the present case due to the age and condition of the material and its origin, primarily from owl pellets. Including genetic data will be an essential approach for future investigations.
Two paths and intermediate steps up to the development of the ‘pitymys +' variant are conceivable (Fig. 3). Depending on whether the anterior lobus initially narrows to the ‘maskii' morph (which already shows the second ‘pitymys’ rhombus) and the remaining loop subsequently develops to a new and complete anterior lobe, which is known from the ‘typica’ morph of this species (Fig. 3, right). In this case, the proportion of ‘maskii’ forms and transitions to ‘maskii’ usually show high values in M. subterraneus specimens (Niethammer 1972, Angermann 1974, Zahreddin 1989, this study). This scenario is in contrast to the mostly low frequency of ‘maskii’ patterns in M. agrestis and M. arvalis (Schimmelpfennig 1991, Jentzsch 2006, Kapischke et al. 2009), in which the increase in the structure is formed via alternating dentine triangles. As an alternative to the first variant, additional anticlines first form at the anterior lobe, and the constriction of the second ‘pitymys’ rhombus takes place in the next step (Fig. 3, left).
The various stages proposed here for the development of the ‘pitymys +’ variant are theoretical and based on only a small number of some morphotypes. Only ten molars with ‘maskii’ 5/4 patterns were available, and only one of the newly described ‘pitymys +’ 6/5 morph. This low frequency makes it difficult to generalise about the possible directions of development. Further investigations with a larger dataset would, therefore, be desirable. However, it is difficult to obtain a sizeable local series of the common pine vole from numerous sites, as it is rare in Europe compared to the more common M. agrestis and M. arvalis. For example, in the Red Lists of Germany, information on the species’ occurrence is currently considered inadequate, but an Endangered status can be assumed (Meinig et al. 2009, Trost et al. 2020). Nevertheless, it would be interesting to see whether the significant increase in length of the more complex morphs that we have determined in our investigation is also visible in single local populations and in what proportions the different morphotypes occur in the current series.
Acknowledgements
Our thanks go to Dr Dietrich von Knorre (Jena), Martin Trost (Halle/Saale), Kathrin Worschech (Museum of Natural History Mauritianum Altenburg), Prof. Hjalmar S. Kühl (Senckenberg Museum of Natural History Görlitz), Diana Jeschke and Konrad Kürbis (both Museum of Natural History Erfurt) for providing the collection material and to Dr Renate Angermann (Dresden) for the acquisition of literature. We would also like to thank the reviewers for their important comments on the manuscript.
This is an open access article under the terms of the Creative Commons Attribution Licence (CC BY 4.0), which permits use, distribution and reproduction in any medium provided the original work is properly cited.
Author Contributions
M. Jentzsch – conceptualisation, methodology, photo documentation, measurements, data analysis and visualisation, writing, original draft, review and editing; A.S. Mühle – photo documentation, measurements, data analysis and visualisation, writing, R. Schreiter – methodology, statistics, data analysis and visualisation, writing. All authors read and approved the final manuscript.
Literature
Appendices
Supplementary online material
Table S1. Origin and geographical coordinates of the material investigated ( https://www.ivb.cz/wp-content/uploads/JVB-vol.-74-2025-Jentzsch-M.-et-al.-Table-S1.pdf).