López-Torres and Silcox—European Paromomyidae
923
Figure 2.
1915, USGS 21712, right; (2) Paromomys depressidens Gidley, 1923, USNM 9677; (3) Edworthia lerbekmoi Fox et al., 2010, UALVP 50990, right; (4) Ignacius frugivorus Matthew and Granger, 1921, YPM-PU 20690, left; (5) Acidomomys hebeticus Bloch et al., 2002, UM 108206, left; (6) Arcius fuscus Russell et al., 1967,MU 6507, left; (7) Arcius lapparenti Russell et al., 1967, AV 5849, left; (8) Arcius zbyszewskii Estravís, 2000, SV3-47, left; (9) Arcius hookeri n. sp., BMNH.M 44945, right. The paromomyids on the top row (1–5) have an invagination at the top central area of the hypoconulid lobe; all Arcius species (6–9) lack this feature. Scale bar=1mm.
Distal view of micro-CT scan images of the M3 of various species of North American and European paromomyids. (1) Phenacolemur citatus Matthew,
(Rose, 1981; Silcox et al., 2008) and Acidomomys (Bloch et al., 2002). This might suggest that Arcius underwent a process of retention of a deciduous P4. Arcius rougieri shows a possible retention of the deciduous upper central incisor (see the following). Based on the two most complete specimens that belong to
the genus Arcius, PAT1 and PAT2, the dental formula for this genus would be 2:1:2:3
masses for all the species in the genus.
Arcius rougieri Godinot, 1984 Figures 1, 5
1981 Arcius cf. A. fuscus Godinot, 1981, p. 77. 1984 Arcius rougieri Godinot, 1984, p. 85. 1991 ?Arcius rougieri; Marandat, 1991, p. 92.
2003 Arcius rougieri; Aumont, 2003, pl. 3, fig. 5, pl. 6, fig, 5, 6. Pl. 18, fig. 1, pl. 19, 23.
Holotype.—PAT1, partial maxilla with right I1–C and left I1–M1.
Emended diagnosis (modified from Godinot, 1984).—Smaller M2 than Arcius lapparenti, A. hookeri n. sp., and A. ilerdensis n. sp., but larger M1 than A. zbyszewskii. Further differs from A. fuscus and A. lapparenti in having a more apically extended (taller) anterocone than mediocone on I1, with a significantly smaller posterocone, and laterocone proximally shifted relative to the anterocone. Further differs from all other species of Arcius in having a more buccally extended parastylar region onM1 and a stepped postvallid on M1 and M2. Further differs from A. fuscus in having a more distally expanded distolingual basin
1:0:1:3. See also Table 1 for estimated body
on M3. Further differs from A. fuscus in having two crests, instead of three, on the P4 postvallid. Paraconid of M1 is smaller than in A. fuscus and A. lapparenti but larger than in A. zbyszewskii. Mesial inflection ofM1 andM2 trigonids weaker than in A. ilerdensis n. sp. but stronger than in the other known species of Arcius. Further differs from A. zbyszewskii and A. ilerdensis n. sp. in having a cingulid on the buccal half of the distal aspect of M1 that runs up to the hypoconulid. Highest point of the alveolar ridge between P4 andM1; this has not been observed in any other species of Arcius.
Horizon and locality.—Palette (type locality, PE II, see Biostratigraphy in the following), Bouches-du-Rhône, France; Fordones (PE II, see Biostratigraphy), Aude, France; Rians (PE II; Marandat et al., 2012), Var, France.
Biostratigraphy.—There is some disagreement as to the age of Palette and
Fordones.Marandat et al. (2012) assigned Palette and Fordones to Paleocene-Eocene biozone I (PE I) and considered them intermediate in age between Silveirinha (older) and Rians/ Fournes (younger). However, there seems to be a consensus that Silveirinha is very close in age to Sotteville-sur-Mer, probably slightly younger (Smith et al., 2011; Marandat et al., 2012; Hooker, 2015), and Hooker (2015) assigned Sotteville-sur-Mer to PE II, close to the onset of the carbon isotope excursion (CIE). Rians and Fournes have been calibrated to be of similar age to the site of Meudon (Marandat et al., 2012), and Hooker (2015) suggested PE II as the age for Meudon as well. Therefore, based on the correlations suggested by Hooker (2015), Palette and Fordones would be considered to be PE II in age.
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