Laganosuchus maghrebensis, Sereno & Larsson, 2009

Sereno, Paul & Larsson, Hans, 2009, Cretaceous Crocodyliforms from the Sahara, ZooKeys 28 (28), pp. 1-143 : 85-87

publication ID

https://doi.org/ 10.3897/zookeys.28.325

publication LSID

lsid:zoobank.org:pub:A979ECDE-871F-4AFC-9ABA-63A0FD6DC323

DOI

https://doi.org/10.5281/zenodo.3790381

persistent identifier

https://treatment.plazi.org/id/E5BCEEAD-DFEF-4EF6-AA62-110EF91FCD0F

taxon LSID

lsid:zoobank.org:act:E5BCEEAD-DFEF-4EF6-AA62-110EF91FCD0F

treatment provided by

Plazi

scientific name

Laganosuchus maghrebensis
status

sp. nov.

Laganosuchus maghrebensis sp. n.

urn:lsid:zoobank.org:act:E5BCEEAD-DFEF-4EF6-AA62-110EF91FCD0F

Fig. 42 View Figure 42

Table 14

Etymology. Maghreb, western (Arabic); - ensis (Latin), from. Named for the area where the holotype was discovered in the Kem Kem Beds of southeastern Morocco.

Holotype. UCRC PV2 View Materials ; anterior portion of the left dentary preserving four alveoli and one replacement tooth in the anteriormost tooth position ( Fig. 42 View Figure 42 ).

Referred material. CMN 50838, anterior left dentary fragment preserving the symphyseal end and alveoli 1–3.

Type locality. Er Rachidia District, Morocco (exact locality unknown). The referred specimen ( CMN 50838) probably was found south of Erfoud (Fig. 1A, B).

Horizon. Kem Kem Beds, upper member; Upper Cretaceous (Cenomanian), ca. 95 Mya ( Sereno et al. 1996).

Diagnosis. Metasuchian with a narrow, well defined groove on the ventral aspect of the anterior dentary immediately lateral to the splenial that arcs to the posterior aspect of the symphysis; shallow, anteriorly tapering trough on the anterior dentary just lateral to the more sharply defined groove.

Dentary. The anterior portion of the dentary is preserved in two specimens of Laganosuchus maghrebensis . Th e very rugose dentary symphysis suggests that it may have fused with maturity, and that its size, which is somewhat smaller than Laganosuchus thaumastos , may not be significant.

The more complete specimen ( Fig. 42 View Figure 42 A-D) shows a remarkable similarity to Laganosuchus thaumastos . Both have slender U-shaped lower jaws with the symphysis restricted to the dentary, festooned alveoli with enlarged first and second teeth, and a sharply incised Meckel’s canal developed as a narrow groove. Th e teeth are also spikeshaped without recurvature or marginal ornamentation.

Several differences, however, establish L. maghrebensis as a distinct species. The dentary is narrower near the symphysis ( Fig. 42C View Figure 42 ), lacking the internal crest that thickens the dentary in L. thaumastos ( Fig. 38B View Figure 38 ). Th e anterior alveoli in L. maghrebensis are not procumbent or exposed in lateral view as in L. thaumastos . Likewise, an articular scar for the splenial in L. maghrebensis shows that its anterior end tapers to a narrow tip along the ventral margin ( Fig. 42B View Figure 42 ) in contrast to the bifurcated flanges in L. thaumas- tos ( Fig. 38B View Figure 38 ). Th e incised groove representing Meckel’s canal is located on the ventral, rather than lingual, aspect of the dentary ( Fig. 42D View Figure 42 ).

Although crown size in the two species is very similar, the alveolus of the caniniform tooth (d4) is slightly larger than comparable measurements for d1 (Table 14), the reverse of the condition in Laganosuchus thaumastos (Table 13). L. maghrebensis , in addition, shows low fluting on the lingual aspect of the crown of the first dentary tooth ( Fig. 42E View Figure 42 ). A comparable crown, however is not available at the anterior end of the dentary series in L. thaumastos .

UCRC

University of California, Riverside

CMN

Canadian Museum of Nature

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