Eocyzicus, Daday, 1913

Schwentner, Martin, Rabet, Nicolas, Richter, Stefan, Giribet, Gonzalo, Padhye, Sameer, Cart, Jean- François, Bonillo, Céline & Rogers, D. Christopher, 2020, Pseudosesarma crassimanum, Zoological Studies (Zool. Stud.) 59 (44), pp. 1-23 : 9-13

publication ID

https://doi.org/ 10.6620/ZS.2020.59-44

persistent identifier

https://treatment.plazi.org/id/03D987B7-FB7E-1844-EB3F-F99DFD881BCE

treatment provided by

Felipe

scientific name

Eocyzicus
status

 

Eocyzicus View in CoL

The phylogenetic relationships within Eocyzicus were not consistently resolved ( Figs. 2 View Fig , 3A View Fig , Figs. S7– S 9). In particular, with regards to the positions of the North American E. digueti (Richard, 1895) and the South African Eocyzicus species. While the analyses with Matrices 1 and 2 mainly suggested the latter to be sister group to all other Eocyzicus species (potentially together with Asian, North African and Middle Eastern species) ( Fig. 2 View Fig , Figs. S1–S View Fig 3 View Fig ), analyses based on Matrices 5 and 6 mainly placed E. digueti as sister group to all other Eocyzicus species ( Fig. 3A View Fig , Fig. S7– S 9). Below, we focus on analyses of Matrices 5 and 6 as these were tailored specifically to improve the resolution within this taxon. All Australian Eocyzicus species constitute a well supported monophyletic group (pp = 1.0; bs = 94%) with an inferred age of 52.8 mya (39.2– 67.2 mya 95% HPD) ( Fig. 4 View Fig ). This Australian clade is sister group to a clade comprising the African, Asian and Middle Eastern species (pp = 0.96–0.97; bs = 50%; RAxML analysis of Matrix 6 had suggested diverging relationships but with extremely low support). In the latter clade, E. mongolianus Uéno, 1927 ( Mongolia) and E. orientalis Daday, 1913 ( China) are nested within a group of Middle Eastern and South African species (pp = 1.0; bs = 89–91%). The Taiwanese species is either sister group to all of the other species of this clade or closer to the Australian clade, but with low support. More taxa are needed to better resolve this clade. The oldest divergence within Eocyzicus was dated to 95.6 mya (71.1–119.3 mya 95% HPD) but the molecular clock analyses did not include the North American E. digueti and inferred slightly different relationships among species ( Fig. 4 View Fig ).

Leptestheriidae

The phylogenetic relationships within Leptestheriidae were not consistently recovered among analyses ( Figs. 2–4 View Fig View Fig View Fig , Figs. S1–S View Fig 3 View Fig , S 7–S 9, S 12–S 14). The obtained topologies of the analyses with both Leptestheriidae-specific matrices (Matrices 5 and 6) are rather similar (apart from the taxa not included in Matrix 5), with distinct differences between maximum likelihood and Bayesian analyses. The topologies obtained with the spinicaudatan-wide matrices (Matrices 1 and 2) or in the molecular clock analyses with BEAST differed markedly from these and from each other and had relatively low support for many recovered groups. Also the RAxML analyses had relatively low support values among clades. Below, we focus on analyses of Matrices 5 and 6 as these were tailored specifically to improve the resolution within this taxon. The age of extant Leptestheriidae was estimated at 126 mya (103.3–148.6 mya 95% HPD) ( Fig. 4 View Fig ).

The most important difference between Matrices 5 and 6 is the presence of a European representative of Eoleptestheria ticinensis (Balsamo-Crivelli, 1859) in Matrix 5. This specimen clustered with Maghrebestheria maroccana Thiery, 1988 , though it should be kept in mind that only the relatively conserved 28S rRNA was available for the European E. ticinensis . This clade (or only M. maroccana in the analysis of Matrix 6) was sister group to all other Leptestheriidae in the Bayesian analyses (pp = 1.0; Fig. 3A View Fig , Fig. S9) or most other Leptestheriidae except for L. kawachiensis and an Indian species (specimen M089) in the maximum likelihood analyses ( Figs. S7, S 8). The Australian specimen of E. ticinensis ( Fig. 1J View Fig ) does not cluster with the European representative, but is nested deep within Leptestheria . The uncorrected p -distance for the conservative 28S rRNA is 3.9% between these two specimens of Eoleptestheria . Leptestheria nobilis , which was formerly assigned to the now synonymized genus Leptestheriella , is also nested within a group of Leptestheria species.

The leptestherid species do not group according to their geographic origin ( Figs. 2 View Fig , 3A View Fig ). Notably, there are several clusters of species from continents that once formed Gondwana, for example L. brevirostris Barnard, 1924 ( Botswana), one specimen identified as L. rubridgei ( Baird, 1862) ( South Africa), Leptestheria sp. ( Madagascar; specimen M124) and Leptestheria nobilis ( India) or L. venezuelica Daday, 1913 (South America), Leptestheria sp. from Brazil (South America), Leptestheria sp. ( India; specimen M128) and Leptestheria sp. ( Madagascar; specimen M052) (age estimated at 94 mya excluding the Madagascan species) or E. ticinensis ( Australia), L. rubidgei ( South Africa) and L. cortieri ( Mauritania) with the European L. dahalacensis nested well within this last cluster (each cluster with pp = 1; Fig. 3A View Fig , Fig. S3 View Fig ).

There were some instances of putatively cryptic or unrecognized species diversity within Leptestheriidae , in addition to Eoleptestheria (see above). Specimens identified as L. rubidgei were divided into two strongly separated groups (uncorrected p -distance for 16S rRNA: 4.7–5.0%) that clustered at very different positions within Leptestheriidae ( Figs. 2 View Fig , 3A View Fig ). The Algerian and Tunisian specimens of L. mayeti (Simon, 1885) differed by 12.9% uncorrected p -distance in COI from each other. In North America, L. compleximanus ( Packard, 1877) is currently the only recognized species. Within this species uncorrected p -distances of up to 4.8% for COI, 3.1% for 16S rRNA and 1.1% for EF1α were observed; these increased to 14.5% (COI) and 2.4% (EF1α) if the unidentified North American Leptestheria specimens are included as well.

Limnadiidae

There are two well (pp = 1.0; bs = 96–99%) and consistently supported main clades within Limnadiidae : a clade of Australian endemic genera ( Limnadopsis , Paralimnadia and Australimnadia ), in which Paralimnadia is sister group to Limnadopsis and a clade of species from South America ( Metalimnadia and a putative new genus), Africa ( Gondwanalimnadia and Calalimnadia ) as well as the globally distributed genus Eulimnadia ( Figs. 2 View Fig , 4 View Fig , Figs. S1–S View Fig 3 View Fig , S 12– S 14). The relationships of the Holarctic Imnadia and Limnadia species, Imnadia yeyetta Hertzog, 1935 (Europe), Limnadia lenticularis ( Linnaeus, 1761) (Europe), L. nipponica Ishikawa, 1895 ( Japan) and L. americana Morse, 1868 ( USA), are not consistently resolved ( Figs. 2 View Fig , 4 View Fig , Figs. S1–S View Fig 3 View Fig , S 12–S 14). Either Imnadia and Limnadia constituted a monophyletic clade that was sister group to the Australian clade, all other Limnadiidae , or Limnadia was the sole sister taxon to the Australian clade. However, the support values for these alternative relationships were low and nonsignificant.

The divergence between the two main clades was dated to 154 mya in the PhyloBayes analyses ( Figs. S4 View Fig , S 5; unfortunately, no representative of Imnadia or Limnadia was available for this molecular clock analyses) and to 205.5 mya (172.2–240.2 mya 95% HPD) in the BEAST analyses ( Fig. 4 View Fig ). The age of the Australian clade was estimated to 130.3 mya (101.6–159.4 mya 95% HPD), the divergence between Paralimnadia and Limnadopsis to 105.6 mya (83.4–129.1 mya 95% HPD) (59 mya in the PhyloBayes analyses) and the oldest divergence within Limnadopsis to 65.5 mya (47.7–87 mya 95% HPD) (24 mya in the PhyloBayes analyses) ( Fig. 4 View Fig ). The split between the new South American limnadiid genus and Eulimnadia was dated to about 109.4 mya (73–145.5 mya 95% HPD) while the split between the North American Eulimnadia texana Packard, 1871 and the other Eulimnadia species studied herein was dated to 52.2 mya (36.7–70.3 mya 95% HPD).

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