A succession of Miocene rodent assemblages from fissure fillings in southern France: palaeoenvironmental interpretation and comparison with Spain

A succession of Miocene rodent assemblages from fissure fillings in southern France: palaeoenvironmental interpretation and comparison with Spain
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  ELSEVIER  Palaeogeography, Palaeoclimatology, Palaeoecology 145 (1999) 215–230 A succession of Miocene rodent assemblages from fissure fillingsin southern France:palaeoenvironmental interpretation and comparison with Spain Jean-Pierre Aguilar a , Gilles Escarguel a , Jacques Michaux a,b,* a  Institut des Sciences de l’Evolution — UMR 5554 — Universite´ Montpellier II, Place Euge`ne Bataillon,C.C. 064, 34095, Montpellier Ce´dex 5, France b  Laboratoire de Pale´ontologie des Verte´bre´s, E.P.H.E., UMR 5554, Universite´ Montpellier II, Place Euge`ne Bataillon,C.C. 064, 34095, Montpellier ce´dex 5, France Received 11 March 1998; revised version received 23 June 1998; accepted 24 June 1998 Abstract An Early to Late Miocene sequence of rodent assemblages from southern France has been quantitatively studied.The resulting pattern seems very similar to a contemporary sequence from central Spain (Calatayud–Teruel Basin). Thefossil mammal-bearing localities are of different types: mainly karst infills in France and localities situated in sedimentarybasins in Spain. In order to interpret the fossil record, a comparison has been made between southern France faunas of similar age but collected in karst infills and in basin deposits. There seems to be no difference between the two kinds of faunas and thus there is no indication that karst infills systematically give a picture of drier and more open environments.Both types of localities may give a similar relative abundance of taxa and when differences exist they can be attributedto local conditions. The comparison between southern France and the Calatayud–Teruel Basin (central Spain) showsthat: (1) similar trends occurred in the two areas; (2) differences between spectra were more important during the lateEarly Miocene than during the Middle Miocene; (3) the shift between the late Early Miocene and the Middle Mioceneenvironments in southern France does not seem to be correlated with a general drop in temperatures as inferred from theanalysis of central Spain faunas.  © 1999 Elsevier Science B.V. All rights reserved. Keywords:  rodents; Miocene; France; Spain; karst; paleoenvironment 1. Introduction Chronological sequences of rodent assemblagesare good tools for reconstructing the evolution of Neogene environments. In order to estimate theirefficiency, it is useful to see how climatic changes Ł Corresponding author. Fax:  C 33 467 143610; are recorded by rodent faunas from two adjacentgeographical areas or to compare contemporary se-quences from such areas. In the present case, acomparison has been made between southern Franceand central Spain for both areas are known by theirimportant continental Neogene fossil record. In thelast 20 years, more than 100 southern France fos-sil mammal-bearing localities have been discoveredand studied, mainly in the Languedoc–Roussillon 0031-0182/99/$ – see front matter  © 1999 Elsevier Science B.V. All rights reserved.PII: S0031-0182(98)00103-5  216  J.-P. Aguilar et al./ Palaeogeography, Palaeoclimatology, Palaeoecology 145 (1999) 215–230 Fig. 1. Location map of the Miocene fossil mammal-bearing localities of southern France. Province. Most of them are karst infills and manyof them are Middle Miocene in age. They are dis-tributed over a small area of a few square kilo-metres near Baixas (Roussillon, Eastern Pyrenees).These sites document a rich Neogene small mammalfauna, especially for a late Early Miocene to MiddleMiocene time interval. Rodents but sometimes batsare especially abundant in these sites (Aguilar, 1980,1995; Aguilar et al., 1986a,b, 1991a,b, 1994, 1995,1996a; Escarguel and Aguilar, 1997; Faillat et al.,1990; Legendre, 1982; Sige´ et al., 1996). Most of thematerial has been described (Aguilar and Michaux,1990; Michaux et al., 1990). The fossil mammal-bearing localities and the list of their rodent speciesare given in Figs. 1 and 2, and in Appendix A.Apart from latitudinal or other geographical dif-ferences, several factors may affect the interpretationof data. An important one is the type of fossil mam-mal-bearing locality. On the one hand, fossiliferouskarst infills, and on the other hand sedimentary basinlocalities (fossils being preserved in swamp, lake,or stream sediments, etc.). One question usuallyraised is the possible influence of site characteris-tics on faunal compositions, which may distort theinterpretation of the relative abundance of taxa. Asassemblages are mainly collected from karst infillsin France, and from sedimentary basin localities inSpain, this question must be discussed before inter-preting the environmental evolution of the Mioceneas recorded by the rodent faunas. Another factor thatmay affect the interpretation is the precision and theaccuracy of the correlation of the two sequences.This point will be discussed further as there arestill some disagreements between authors about thecorrelations. 2. The faunal sequence in southern France 2.1. Biochronology and correlation Biochronology has been established on the ba-sis of evolutionary lineages of rodents. 24 differentbiochronological levels have been recognized fora time span of ca. 10 million years (Aguilar andMichaux, 1987). The evolutionary lineages belongto Eomyidae (Escarguel and Aguilar, 1997), Eu-cricetodontinae (Aguilar et al., 1996a), Cricetinae— mainly  Megacricetodon  (Aguilar et al., 1994;Aguilar, 1995) — and Murinae (Aguilar et al.,1991a,b, 1995; Aguilar and Michaux, 1996). Twenty levels belong to the late Early and Middle Mioceneand four to the Upper Miocene. Correlations havebeen established with important European fossil   J   .-P  .A   g u i    l    ar  e t   a l    . /   P  a l    a e o  g e o  gr  a  p h    y ,P  a l    a e o c l    i    m a t   o l    o  g  y ,P  a l    a e o e c o l    o  g  y1  4   5    (   1   9   9   9    )   2  1   5  –2   3   0   2  1   7   Fig. 2. Distribution and relative abundance of the rodent genera and = or species (left) and of rodent families (right) in Miocene faunas from karst infills from southern France.  218  J.-P. Aguilar et al./ Palaeogeography, Palaeoclimatology, Palaeoecology 145 (1999) 215–230 mammal-bearing localitiesof Miocene age. They arebased on evolutionary stages in lineages but faunalevents have also been used: the first occurrence of   Democricetodon ,  Megacricetodon  and Murinae (forthe latter, their first known occurrence in Spain andin France, respectively in Pedregueras 2c and Castel-nou 1B). The characteristic time interval named the‘cricetid vacuum’ (Daams and Freudenthal, 1990)has also been considered as isochronous in bothareas. For the Late Miocene, the French karst in-fills of Castelnou 3 and Castelnou 1 are correlated(Aguilar et al., 1991a,b, 1995) respectively with LaAlberca and Los Mansuetos — Lo Fournas 6c, andLo Fournas 7 is supposed to be slightly youngerthan Montredon (Aguilar and Michaux, 1996). Forthe Middle and the late Lower Miocene, Bouzigues2 and Serre de Verge`s (Aguilar et al., 1996a; Sige´et al., 1996) are respectively older and younger thanEstrepouy. The karst infills of Baixas 202 c and SteCatherine 9 (Escarguel and Aguilar, 1997; Aguilar etal., 1997) are respectively older and younger than thebasin locality of Beaulieu which has been recentlyradiometrically dated (Ar = Ar method): 17 : 5 š 0 : 3Ma (Aguilar et al., 1996b). Artenay is situated be-tween Ste Catherine 9 and Ste Catherine 4 and 6,and La Romieu between Ste Catherine 8 and Baixas.The karst infills of Lo Fournas 8, Sansan, and Man-chones are roughly contemporaneous, and similarlyLo Fournas 3 may be contemporaneous with LaGrive M. Castelnou 1B is slightly younger than LaGrive L3 (Aguilar, 1995; Aguilar et al., 1997). 2.2. Relative abundance of rodent taxa The relative abundance of taxa has been calcu-lated based on the total number of first and secondmolars, i.e. some 16000 teeth from 24 localities.When several localities have a similar age, the local-ity used for calculation is that with the richest faunaand the most complete list of taxa. Results are givenin Fig. 2. Five faunal phases, ranging from the oldestto the youngest, can be distinguished.Phase 1 (time interval: Bouzigues 1–Serre deVerge`s): abundance of glirids, and at a lesser degreeof eomyids, and Eucricetodontinae the abundance of which is progressively decreasing.Phase 2 (Ste Catherine 2–Ste Catherine 9): dom-inance of glirids and eomyids is characteristic. It isworth noting that  Neocometes  is present in the levelsof Ste Catherine 2 and 9 (Aguilar et al., 1997). Thistime interval corresponds to the ‘cricetid vacuum’ of Daams and Freudenthal (1990).Phase 3 (Ste Catherine 4 and 6–Ste Catherine 7):eomyids and glirids begin to decrease in number.The lower boundary of Phase 3 is determined by thefirst occurrence of the genus  Democricetodon .Phase 4 (Lo Fournas 1–Lo Fournas 3): glirids stilldecrease in number. The lower boundary of Phase4 is determined by the first occurrence of the genus  Megacricetodon .Phase 5 (from Castelnou 1B up to Castelnou 3):first occurrence of the Murinae and of the moderncricetids; glirids are few in number and the Criceti-nae disappear after Castelnou 1b.Two remarks have to be made. First, the genus Cricetodon , which is listed in the karst infill of Castelnou 1b, is only known in southern France atthe basin locality of Luc sur Orbieu which has thesame age as Lo Fournas 8. The two latter locali-ties are contemporaneous to Sansan (Aguilar, 1995).Second,  Paraethomys  is only known in France fromLa Tour and Castelnou 3: both localities are LateMiocene in age and younger than the first levelswith  Paraethomys  recognized in Spain. The fossilrecord of this genus in France is probably muchmore incomplete than it is in Spain. 2.3. Comparison between karst infills and basinlocalities It is frequently argued that a fauna collected in akarst infill gives a faunal spectrum different from thatobtained in a basin locality. The former is consid-ered (Van de Weerd and Daams, 1978) as indicatingdrier and more arid environments than the latter. Infact, it is usually observed that species related towater environments such as castorids are frequentlylacking in fissure filling faunas that are otherwiserather diverse. Both characteristics can be expectedbecause nocturnal birds of prey are generally at theorigin of bone and tooth accumulations. As bothtypes of fossil mammal-bearing localities are presentin southern France, we have tried to evaluate thepossible distortion introduced by the composition of the fissure filling faunas. However, as there are muchmore faunas from karst infills than from basin lo-   J.-P. Aguilar et al./ Palaeogeography, Palaeoclimatology, Palaeoecology 145 (1999) 215–230  219 calities, the comparisons have been conducted onlyfor two rather short time intervals. The first compar-ison involves late Early Miocene assemblages withthe localities of Baixas 202 c, Ste Catherine 9, andBeaulieu, and the second one corresponds to Mid-dle Miocene assemblages with the localities of LoFournas 8, Luc sur Orbieu, and Veyran. 2.3.1. Baixas 202 c and Ste Catherine 9 vs. Beaulieu The Beaulieu fauna has been collected frombrackish and lacustrine sediments (Aguilar, 1981;Aguilar et al., 1996b; Escarguel and Aguilar, 1997).The relative abundance of the rodent taxa are notsimilar in the three localities (Fig. 3a): eomyids andthe genus  Melissiodon  are dominant in Beaulieu, twoclear-cut differences with the spectra obtained fromkarst infill faunas of the same age. As eomyids areusually considered to be associatedwith wet environ-ments (Alvarez Sierra et al., 1990), their abundancecan be probably explained by local conditions whichare also indicated by the facies of the fossilifer-ous sediments.  Melissiodon  is usually rare in basinlocalities as well as in karst infills from southernFrance. This rodent is also rare in the basin localitiesof similar age from the Iberian Peninsula. On theother hand, it is quite frequent in central Europe inkarst infills as well as in basin localities (Hrubesch,1957; Ziegler and Fahlbusch, 1986; Fejfar, 1990) Fig. 3. Comparison between the composition of the rodent faunas from karst infills and basin localities of similar age in southern France:(a) late Early Miocene localities, and (b) Middle Miocene localities. and it may be indicative of a wet environment (Fej-far, 1990). Thus, the high number of   Melissiodon  inBeaulieu may simply indicate particular taphonomicand = or local environmental conditions. In the fau-nas of Baixas 202 c and Beaulieu, the forest gliridswhich are also dominant indicate similar environ-ments. In this case, there is no distortion caused bythe type of fossil mammal-bearing locality (Fig. 4). 2.3.2. Luc sur Orbieu, and Veyran vs. Lo Fournas 8  The fossil bearing sediments of Luc sur Orbieu(Aguilar and Magne´, 1978) correspond to brack-ish environments and those from Veyran correspondto palustrine ones (Aguilar, 1980). Both localitiesare contemporaneous with Lo Fournas 8 (Aguilar,1995). Despite the presence of   Cricetodon  in Luc surOrbieu, the three sites have similar faunal spectra.According to these two examples, it is not pos-sible to suggest that within the same area, karstinfill faunas are indicative of drier environments thanfaunas collected in basin localities. 2.4. Interpretation of the sequence of karst faunas The reconstruction of Neogene continental en-vironments in Western Europe is often based onthe analysis of sequences of small mammal assem-blages (rodents but also bats) (Van de Weerd and
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