Published October 1, 2014 | Version v1
Taxonomic treatment Open

Pontophoca Mc Laren 1960

Description

Genus Pontophoca Mc Laren, 1960

1860 (atlas 1858) Phoca — von Nordmann: 317, 356–357, pl. 23, fig. 3, 7; pl. 24, fig. 1; 1922 Phoca — Kellogg: 120 (part); 1924 Phoca — Alekseev: 203, fig. 4–7; 1925 Phoca — Simionescu: 180, 188, 190–191, fig. 5P; pl. 1, fig. 2; 1941 Phoca — Macarovici, Oescu: 351–352, 363–367, 378–379, fig. 7, 8; pl. 2, fig. 13, 19; 1941 Pontophoca — Kretzoi: 354, fig. 3.2 (nom. nud.); 1942 Phoca — Macarovici: 262–263, 267, pl. 2, fig. 18.1; 1947 Phoca — Friant: 12; 1947 Monachus — Friant: 6, 16, 47–50, pl. 1, fig. 1a–c; 1956 Phoca — Pidoplichko: 142; 1960 Phoca — McLaren: 51, 52; *1960 Pontophoca — McLaren: 47, 52, fig. 1g, h, I; 1961 Phoca — Kirpichnikov: 29, 32, 34, 36; 1964 Pontophoca — King: 131; 1965 Phoca — Aslanova: 52; 1977 Phoca — Grigorescu: 407, 411, 413–418, fig. 5D; 1979 Phoca — Dubrovo, Kapelist: 36; 1985 Phoca — Trelea, Simionescu: 19; 1992 Phoca — Muizon: 35; 2002 Pontophoca — Koretsky, Grigorescu: 149–162, fig. 1–3.

T y p e s p e c i e s: Phoca sarmatica Alekseev, 1924 (pl. 1, 1А, 1B). Holotype from Kishinev, Moldova, Eastern Europe (Alekseev, 1924), Middle Miocene, middle Sarmatian.

S t r a t i g r a p h i c a l r a n g e. Aside from the type locality the genus is also known from the late Miocene (early-middle Tortonian, 8.0–11.5 ma) of Denmark, northern Europe.

I n c l u d e d s p e c i e s. Until now, only the type species was included in this genus. Here, we introduce a second species, Pontophoca jutlandica Koretsky et al., sp. n.

R e f e r r e d m a t e r i a l. Mandible, scapula, tibiae and fibulae, femora, humeri, innominates (Koretsky, Grigorescu, 2002).

E m e n d e d d i a g n o s i s. Lower premolars p1 and p2 double-rooted, placed parallel to tooth row axis; protoconid on p2 triangular; diastemata present; metaconid and basal cingulum weakly developed. Deltoid crest of humerus terminates in middle of diaphysis, its proximal part averted in dorsal direction; distal epiphysis considerably inflated compared to proximal epiphysis; lesser tubercle located higher than proximal end of deltoid crest and head; index of head’s height (ratio of head width/head height) near 100 %; supracondylar crest strongly developed. Height of femoral greater trochanter slightly exceeds that of head; its distal end narrower than its proximal end; head very small compared with the otherwise massive bone and seated on narrow neck; minimal width of diaphysis located in proximal part of bone between neck and distal part of greater trochanter; distal end of femur 1.4– 1.5 times broader than proximal end; condyles widely separated; maximal distance between epicondyles about or more than 70 % of bone’s length.

Notes

Published as part of Koretsky, I., Rahmat, S. & Peters, N., 2014, Rare Late Miocene Seal Taxa (Carnivora, Phocidae) From The North Sea Basin, pp. 419-432 in Vestnik Zoologii 48 (5) on page 421, DOI: 10.2478/vzoo-2014-0050, http://zenodo.org/record/6449169

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Linked records

Additional details

Related works

Biodiversity

Family
Phocidae
Genus
Pontophoca
Kingdom
Animalia
Order
Carnivora
Phylum
Chordata
Scientific name authorship
Mc Laren
Taxon rank
genus
Type status
holotype
Taxonomic concept label
Pontophoca Laren, 1960 sec. Koretsky, Rahmat & Peters, 2014

References

  • Alekseev, A. K. Seals in the Sarmatian deposits of the south of Russia // Journal Nauchno-Issledovatelskich kafedr v Odesse. - 1924. - 1, N 5. - P. 26 - 34. - Russian: Aлikсiiv A. K. Tюлiнi v сaрмatсkik otлoziнiik юga Рoссii.
  • Koretsky, I. A., Grigorescu, D. The fossil monk seal Pontophoca sarmatica (Alekseev) (Mammalia: Phocidae: Monachinae) from the Miocene of eastern Europe // Smithsonian Contributions to Paleobiology. - 2002. - 93. - P. 149 - 162.