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Communication

A Brief Note on the Presence of the Common Hamster during the Late Glacial Period in Southwestern France

1
Biogéosciences, UMR 6282 CNRS, Université Bourgogne Franche-Comté, 21000 Dijon, France
2
UMR 5199 CNRS, PACEA Université Bordeaux, 33615 Pessac CEDEX, France
*
Author to whom correspondence should be addressed.
Quaternary 2018, 1(1), 8; https://doi.org/10.3390/quat1010008
Submission received: 18 May 2018 / Revised: 4 June 2018 / Accepted: 5 June 2018 / Published: 7 June 2018

Abstract

:
The Late Glacial period is characterized by slow warming, punctuated by short, cold episodes, such as the Younger Dryas (i.e., GS1). The impact of this climatic event on the mammal community is still poorly documented in southwestern France. Here, a new radiocarbon date obtained directly on fossil remains of common hamster, Cricetus cricetus, confirms its presence in southwestern France during the Younger Dryas (GS1). This observation currently suggests that C. cricetus could be an accurate chronological indicator of this event in southwestern France. In this particular case, it also demonstrates an attritional death, polluting the deposit, these remains having been found in the Combe-Cullier layer, attributed to an earlier period.

The common hamster, Cricetus cricetus, is a medium-sized fossorial rodent with a weight varying between 150 g and 550 g. The current distribution of this rodent in Eurasia is limited between 42° and 55° North and 5° and 95° East, constrained by the July and January isotherms (+17 °C and +2 °C, respectively) and soft soils in which to dig their galleries [1,2]. Thus, the common hamster is mainly found in the steppes and grasslands of Western Asia and Eastern Europe, whereas its range is fragmented in the west. One such population, in Alsace, exploded during the first part of the twentieth century [3]. However, over the last 30 years, partly due to urbanization and change in agricultural practice, the status of the common hamster passed from that of an invasive species to that of a protected one [4]. The common hamster is thus currently classed as “strictly protected”, with a population in Alsace of fewer than 1000 individuals.
Fossil remains appear regularly in many localities in Eastern and Central Europe [5], but are still rare in the fossil record in comparison with the remains of voles. Therefore, the past distributions of cricetids and their evolution are not well known (e.g., [6]), particularly in regions such as southwestern France, where the eastern plains terminate with mountains and oceanic barriers. Nevetheless, over the last 130,000 years, three species of Cricetinae were observed in southwestern France: Allocricetulus bursae, which disappeared during the last interglacial period [7]; the migratory hamster, Cricetulus migratorius, which has been observed at Mousterian sites in Charente, dated to Marine Isotope Stage 3 (e.g., [7,8]); and the common hamster, C. cricetus.
Remains of this latter larger cricetid are almost entirely limited to the eastern part of France [7,9,10,11], except for three sites in southwestern France, where hamster fossil remains have been observed: Artenac (Charente) in levels attributed to Marine Isotope Stage 5/4 [12]; Taillis-des-Coteaux (Vienne), where five post-cranial remains have been found in levels dated between 17.4 and 21.1 cal ky BP [13]; and Peyrazet (Lot) where three dental remains have been found in recent Laborian levels dated to ca 11.2 cal ky BP [14,15]. However, the remains from this last site were located in the upper part of the stratigraphy, not very far from the soil surface, at the limit between the two first layers. Being mainly associated with temperate and mountain species, it has been suggested that these remains could most likely be attributed to the Younger Dryas (i.e., GS1 [16]).
The scarcity of remains associated with this rodent in this region led us to question the chronology of its presence as well as the continuity of its distribution at the end of the Late Pleistocene, despite the sizeable climatic variations. This paper describes a recent discovery of C. cricetus remains found at Combe-Cullier (Lot, France), a site that offers us the opportunity to better understand their palaeobiogeography.
The site of Combe-Cullier is located in the Lot region, in the area of Lacave, near Rocamadour. The site, which was discovered in the early twentieth century, was notably excavated discontinuously by A. Viré between 1906 and 1935 [17,18,19]. Between 1964 and 1974, J.F. Flies then carried out excavations on the mound in front of the cave, the findings of which are still largely unpublished. The material and stratigraphy of this excavation are currently being reevaluated [20,21,22] in order to propose a new archaeo-stratigraphy. Initial results showed a chronological succession of lithic industry and fauna from the Lower to Upper Magdalenian, without any stratigraphic inversion (e.g., [22,23]).
A few small mammal remains were collected by Flies during his excavations [24]. This material allowed us to identify 70 different bone remains, not mentioned previously by Delpech [24], which we believe come from one common hamster individual (C. cricetus). Indeed, these remains were grouped in the same small box, leading us to suppose that they came from a single collection removed during the excavations. All the bones show a similar patina. All the post-cranial elements are present, including the humerus, femur, pelvis, vertebra, costal, metapodial and phalange remains. The two mandibular and hemi-maxillary remains showed similar dental wear. No elements showed any signs suggesting the presence of an additional individual. Moreover, no breakage or digestion marks were observed. These remains come from level C4’2, which according to the new archaeo-stratigraphy is attributed to the Upper Magdalenian [23].
The site of Combe-Cullier (Lot) is situated less than 15 km from the site in Peyrazet. These two sites present complementary stratigraphies, with that of Combe-Cullier preceding that of Peyrazet. The two sites document the only two fossil occurrences of the common hamster at such low latitude, potentially suggesting the (semi-)continuous presence of this taxon in this region during the latter part of the Late Pleistocene.
This is based, however, on the working hypothesis of a strict association between the rodent remains and the archaeostratigraphy, and thus of a good archaeological integrity between the two sites. In the case of the remains from Peyrazet, two difficulties in interpretation are encountered: (1) the remains were discovered in the upper levels, close to the soil surface. Due to this delicate archaeological context, preventing clear association with any specific period, they could just as well be modern as medieval (presence of Rattus rattus and Glis glis [14]) or Laborian, which seems most likely; (2) they were poorly preserved, precluding any radiocarbon dates. Nonetheless, by considering both the European context and the archaeological one, the most likely hypothesis is that the distribution of this common hamster could have extended into southwestern France during the Younger Dryas, the last cold period before the Holocene warming [15]. In the case of Combe-Cullier, no taphonomic analysis can be performed, because there are no further small mammal remains, preventing us from evaluating the integrity of the site and the remains. It is worth noting that the common hamster is a burrowing species. Finding a complete individual, as during this excavation, could suggest death in its gallery, even if such cases are rare, as was demonstrated with regard to rabbit warrens [25].
A radiocarbon date was obtained directly from several of the hamster bones together weighing around 120 mg. The sample was dated at the Oxford Radiocarbon Accelerator Unit (University of Oxford, Oxford, UK) and was treated according to the Oxford Radiocarbon Accelerator Unit standard procedures for bones. The radiocarbon date obtained on the hamster remains (OxA-34939) is 10,295 ± 50 uncalibrated years BP. Using the IntCal13 calibration curve [26], a time interval was obtained at 2σ of between 12,384 and 11,833 cal yr BP (Figure 1), indicating the latter part of the Younger Dryas (GS1). The radiocarbon date of the hamster remains from Combe-Cullier thus confirms the hypothesis proposed for the Peyrazet remains, with the presence of the hamster extending into southwestern France, thanks to the opportunity afforded by the climatic conditions of the Younger Dryas. If C. cricetus thus seems a good biochronological taxa for the Younger-Dryas event in southwestern France, the lack of further data does not, however, allow us to presently evaluate the exact chronology of the presence of this taxon in this region.
In addition, this study also illustrates the caution needed with burrowing species. If such cases are carefully considered (e.g., [28,29]), they are always particularly difficult to demonstrate, especially when burrows were dug in the past. The advent of radiocarbon dating performed directly on large or medium-sized mammals offers a unique opportunity for us to ensure the integrity of faunal assemblages, and to identify intrusive burrowers (e.g., [30,31]). The recent improvement of methods allowing the extraction of smaller sample sizes [32,33] now offers new applications for smaller-sized mammals, and thus, the opportunity to explore the integrity of small mammal assemblages within the surrounding archaeological material and sites.

Author Contributions

The authors all contributed to the determinations, to the analysis of the results and to the writing of the manuscript. M.L. contributes to funding acquisition.

Funding

This research was funded by MAGDAQUI project (Nouvelle Aquitaine region; Langlais coord.).

Acknowledgments

The authors are grateful to V. Laroulandie, J.B. Mallye, and M. Pavard for their help in Flies collection treatments. Finally, we would like to thank reviewers for their corrections that improved the earlier version of our manuscript.

Conflicts of Interest

The authors declare no conflicts of interest.

References

  1. Nechay, G.; Hamar, M.; Grulich, I. The common hamster (Cricetus cricetus [L.]); a review. EPPO Bull. 1977, 7, 255–276. [Google Scholar] [CrossRef]
  2. Nechay, G. Status of Hamsters Cricetus cricetus, Cricetus migratorius, Mesocricetus newtoni, and Other Hamster Species in Europe; Council of Europe: Strasbourg, France, 2000; Volume 106. [Google Scholar]
  3. O’Brien, J. Saving the common hamster (Cricetus cricetus) from extinction in Alsace (France): Potential flagship conservation or an exercise in futility? Hystrix 2015, 26. [Google Scholar] [CrossRef]
  4. Quéré, J.P.; Le Louarn, H. Les Rongeurs de France: Faunistique et Biologie—3e Édition Revue et Augmentée; Editions Quae: Paris, France, 2011. [Google Scholar]
  5. Kowalski, K. Pleistocene rodents of Europe. Folia Quat. 2001, 72, 3–389. [Google Scholar]
  6. Feoktistova, N.Y.; Meschersky, I.G.; Bogomolov, P.L.; Sayan, A.S.; Poplavskaya, N.S.; Surov, A.V. Phylogeographic structure of the Common hamster (Cricetus cricetus L.): Late Pleistocene connections between Caucasus and Western European populations. PLoS ONE 2017, 12, e0187527. [Google Scholar] [CrossRef] [PubMed]
  7. Marquet, J.-C. Paléoenvironnement et chronologie des sites du domaine Atlantique français d’âge Pléistocène moyen et supérieur d’après l’étude des rongeurs. Les Cahiers de la Claise 1993, 346, 297–316. [Google Scholar]
  8. Royer, A.; Lécuyer, C.; Montuire, S.; Escarguel, G.; Fourel, F.; Mann, A.; Maureille, B. Late Pleistocene (MIS 3–4) climate inferred from micromammal communities and δ18O of rodents from Les Pradelles, France. Quat. Res. 2013, 80, 113–124. [Google Scholar] [CrossRef]
  9. Chaline, J. Les Rongeurs du Pléistocène Moyen et Supérieur de France; Cahiers de Paléontologie, CNRS: Paris, France, 1972. [Google Scholar]
  10. Jeannet, M. Les Cricétidés (Mammalia, Rodentia) des gisements moustériens de Soyons (Ardèche, France). Bulletin Mensuel de la Société Linnéenne de Lyon 1995, 64, 41–48. [Google Scholar] [CrossRef] [Green Version]
  11. Jeannet, M. L’environnement tardiglaciaire préalpin: Essai de restitution basée sur le potentiel climatique et écologique des microvertébrés. Revue Archéologique de l’Est 2009, 58, 5–56. [Google Scholar]
  12. Delagnes, A.; Tournepiche, J.F.; Armand, D.; Desclaux, E.; Diot, M.F.; Ferrier, C.; Le Fillâtre, V.; Vandermeersch, B. Le gisement Pléistocène moyen et supérieur d’Artenac (Saint-Mary, Charente): Premier bilan interdisciplinaire. Bulletin de la Société Préhistorique Française 1999, 96, 469–496. [Google Scholar] [CrossRef]
  13. Jeannet, M. La grotte du Taillis des Coteaux à Antigny (Vienne). Taphonomie et paléo-environnement selon les microvertébrés. Bilan Scientifique 2011, 2001, 304–313. [Google Scholar]
  14. Langlais, M.; Laroulandie, V.; Jacquier, J.; Costamagno, S.; Chalard, P.; Mallye, J.B.; Pétillon, J.M.; Rigaud, S.; Royer, A.; Sitzia, L.; et al. Le Laborien récent de la grotte-abri de Peyrazet (Creysse, Lot). Nouvelles données pour la fin du Tardiglaciaire en Quercy. Paléo Revue D'archéologie Préhistorique 2015, 26, 79–115. [Google Scholar]
  15. Royer, A. How complex is the evolution of small mammal communities during the Late Glacial in southwest France? Quat. Int. 2016, 414, 23–33. [Google Scholar] [CrossRef]
  16. Rasmussen, S.O.; Bigler, M.; Blockley, S.P.; Blunier, T.; Buchardt, S.L.; Clausen, H.B.; Cvijanovic, I.; Dahl-Jensen, D.; Johnsen, S.J.; Fischer, H.; et al. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: Refining and extending the INTIMATE event stratigraphy. Quat. Sci. Rev. 2014, 106, 14–28. [Google Scholar] [CrossRef] [Green Version]
  17. Viré, A. La Crozo de Gentillo. L’Anthropologie 1908, 19, 409–424. [Google Scholar]
  18. Viré, A.; Niederlander, A. Nouvelles fouilles à la Crozo de Gentillo, commune de Lacave (Lot). Bulletin de la Société Préhistorique Française 1921, 18, 269–270. [Google Scholar] [CrossRef]
  19. Lorblanchet, M. (1972)–Aperçu sur le Magdalénien moyen et supérieur du Haut-Quercy. In Congrès Préhistorique de France, XIXe Session, Auvergne; Société Préhistorique Française: Paris, France, 1969; pp. 256–283. [Google Scholar]
  20. Adachi, T. Étude des Industries Magdaléniennes de Combe-Cullier (Lot), une Approche Typologique, Lithologique et Technologique, Mémoire de DEA. Bachelor’s Thesis, Université Bordeaux 1, Talence, France, 2000. [Google Scholar]
  21. Pavard, M. Stratégies de Chasse et Exploitation des Carcasses Animales au Magdalénien Moyen: L’exemple de la Couche 13a de Combe Cullier (Lot). Master’s Thesis, Université de Bordeaux, Talence, France, 2016. [Google Scholar]
  22. Sécher, A. Traditions, Techniques et Paléogéographie du Magdalénien Moyen Ancien dans le Sud-Ouest de la France (19,000–17,500 cal. BP). Des Groupes Humains à Plusieurs Visages? Ph.D. Thesis, Université de Bordeaux, Talence, France, 2017. [Google Scholar]
  23. Langlais, M.; Sécher, A.; Laroulandie, V.; Mallye, J.-B.; Pétillon, J.-M.; Royer, A. Combe-Cullier (Lacave, Lot): Une séquence oubliée du Magdalénien. Apport des Nouvelles Dates 14C, Bulletin de la Société Préhistorique Française 2018, 115, 9–13. [Google Scholar]
  24. Delpech, F. Les Faunes du Paléolithique Supérieur Dans le Sud-Ouest de la France; du CNRS (Cahiers du Quaternaire, 6): Paris, France, 1983. [Google Scholar]
  25. Pelletier, M.; Brugal, J.P.; Cochard, D.; Lenoble, A.; Mallye, J.B.; Royer, A. Identifying fossil rabbit warrens: Insights from a taphonomical analysis of a modern warren. J. Archaeol. Sci. Rep. 2016, 10, 331–344. [Google Scholar] [CrossRef]
  26. Reimer, P.; Bard, E.; Bayliss, A.; Beck, J.; Blackwell, P.; Bronk Ramsey, C.; Buck, C.; Cheng, H.; Edwards, R.; Friedrich, M.; et al. IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP. Radiocarbon 2013, 55, 1869–1887. [Google Scholar] [CrossRef] [Green Version]
  27. Bronk Ramsey, C. OxCal Program, version 4.3; University of Oxford, Radiocarbon Accelerator Unit: Oxford, UK, 2017. [Google Scholar]
  28. Andrews, P. Owls, Caves and Fossils: Predation, Preservation and Accumulation of Small Mammal Bones in Caves, with an Analysis of the Pleistocene cave Faunas from Westbury-Sub-Mendip, Somerset, UK; University of Chicago Press: Chicago, IL, USA, 1990. [Google Scholar]
  29. Stahl, P.W. The recovery and interpretation of microvertebrate bone assemblages from archaeological contexts. J. Archaeol. Method Theory 1996, 3, 31–75. [Google Scholar] [CrossRef]
  30. Costamagno, S.; Barshay-Szmidt, C.; Kuntz, D.; Laroulandie, V.; Pétillon, J.M.; Boudadi-Maligne, M.; Pétillon, J.-M.; Chevallier, A. Reexamining the timing of reindeer disappearance in southwestern France in the larger context of late glacial faunal turnover. Quat. Int. 2016, 414, 43–61. [Google Scholar] [CrossRef]
  31. Pelletier, M.; Royer, A.; Holliday, T.W.; Discamps, E.; Madelaine, S.; Maureille, B. Rabbits in the grave! Consequences of bioturbation on the Neandertal “burial” at Regourdou (Montignac-sur-Vézère, Dordogne). J. Hum. Evol. 2017, 110, 1–17. [Google Scholar] [CrossRef] [PubMed]
  32. Cersoy, S.; Zazzo, A.; Lebon, M.; Rofes, J.; Zirah, S. Collagen extraction and stable isotope analysis of small vertebrate bones: A comparative approach. Radiocarbon 2017, 59, 679–694. [Google Scholar] [CrossRef]
  33. Cersoy, S.; Zazzo, A.; Rofes, J.; Tresset, A.; Zirah, S.; Gauthier, C.; Kaltnecker, E.; Thil, F. Tisnerat-Laborde, N. Radiocarbon dating minute amounts of bone (3–60 mg) with ECHoMICADAS. Sci. Rep. 2017, 7, 7141. [Google Scholar] [CrossRef] [PubMed]
Figure 1. Photograph of the common hamster mandible from Combe Cullier (Lot) with the radiocarbon date obtained from bone remains calibrated with OxCal v4.3.2 [27] and IntCal13 [26]. The radiocarbon date was reported along the oxygen isotope compositions from the Greenland ice core record (GICC05). Scale = 1 cm.
Figure 1. Photograph of the common hamster mandible from Combe Cullier (Lot) with the radiocarbon date obtained from bone remains calibrated with OxCal v4.3.2 [27] and IntCal13 [26]. The radiocarbon date was reported along the oxygen isotope compositions from the Greenland ice core record (GICC05). Scale = 1 cm.
Quaternary 01 00008 g001

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Royer, A.; Sécher, A.; Langlais, M. A Brief Note on the Presence of the Common Hamster during the Late Glacial Period in Southwestern France. Quaternary 2018, 1, 8. https://doi.org/10.3390/quat1010008

AMA Style

Royer A, Sécher A, Langlais M. A Brief Note on the Presence of the Common Hamster during the Late Glacial Period in Southwestern France. Quaternary. 2018; 1(1):8. https://doi.org/10.3390/quat1010008

Chicago/Turabian Style

Royer, Aurélien, Anthony Sécher, and Mathieu Langlais. 2018. "A Brief Note on the Presence of the Common Hamster during the Late Glacial Period in Southwestern France" Quaternary 1, no. 1: 8. https://doi.org/10.3390/quat1010008

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