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Wednesday, April 28th, 2021
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1:28a |
[Herpetology • 2021] Pedioplanis branchi & P. mayeri • Lizards of A Different Stripe: Phylogenetics of the Pedioplanis undata Species Complex (Squamata, Lacertidae), with the Description of Two New Species
 | Pedioplanis branchi & Pedioplanis mayeri
Childers, Kirchhof & Bauer, 2021
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Abstract The lacertid genus Pedioplanis is a moderately speciose group of small-bodied, cryptically-colored lizards found in arid habitats throughout southern Africa. Previous phylogenetic work on Pedioplanis has determined its placement within the broader context of the Lacertidae, but interspecific relations within the genus remain unsettled, particularly within the P. undata species complex, a group largely endemic to Namibia. We greatly expanded taxon sampling for members of the P. undata complex and other Pedioplanis, and generated molecular sequence data from 1,937 bp of mtDNA (ND2 and cyt b) and 2,015 bp of nDNA (KIF24, PRLR, RAG-1) which were combined with sequences from GenBank resulting in a final dataset of 455 individuals. Both maximum likelihood and Bayesian analyses recover similar phylogenetic results and reveal the polyphyly of P. undata and P. inornata as presently construed. We confirm that P. husabensis is sister to the group comprising the P. undata complex plus the Angolan sister species P. huntleyi + P. haackei and demonstrate that P. benguelensis lies outside of this clade in its entirety. The complex itself comprises six species including P. undata, P. inornata, P. rubens, P. gaerdesi and two previously undescribed entities. Based on divergence date estimates, the P. undata species complex began diversifying in the late Miocene (5.3 ± 1.6 MYA) with the most recent cladogenetic events dating to the Pliocene (2.6 ± 1.0 MYA), making this assemblage relatively young compared to the genus Pedioplanis as a whole, the origin of which dates back to the mid-Miocene (13.5 ± 1.8 MYA). Using an integrative approach, we here describe Pedioplanis branchi sp. nov. and Pedioplanis mayeri sp. nov. representing northern populations previously assigned to P. inornata and P. undata, respectively. These entities were first flagged as possible new species by Berger-Dell’mour and Mayer over thirty years ago but were never formally described. The new species are supported chiefly by differences in coloration and by unique amino acid substitutions. We provide comprehensive maps depicting historical records based on museum specimens plus new records from this study for all members of the P. undata complex and P. husabensis. We suggest that climatic oscillations of the Upper Miocene and Pliocene-Pleistocene era in concert with the formation of biogeographic barriers have led to population isolation, gene flow restrictions and ultimately cladogenesis in the P. undata complex.
Key Words: Biogeography, molecular phylogeny, phylogenetics, southern Africa, species description, taxonomy
 | Figure 8. Life photographs of representative individuals of Pedioplanis branchi sp. nov. highlighting color pattern variation within the species. (a.) Lateral and (b.) dorsal whole body images of an adult specimen from the Chuos Mountains (Chuosberg) (SK376.2014; not included in study), note the dense, dark speckling on the dorsum, and bold dark lateral markings. (c.) Dorsal and (d.) lateral whole body images of an adult specimen (SK402.2014; not included in study) from the northward extension of the Swakop River Canyon, note the more uniformly gray and red dorsum lacking speckling and fainter yellow spots along the flanks. Lateral (e.) head and (f.) whole body images of an adult specimen from the northward extension of the Swakop River Canyon; note the black, vertical bar beneath the lower eyelid, the bold, dark lateral markings on the body, and the distinct longitudinal row of yellow spots along the flanks. |
Pedioplanis inornata “South”/P. inornata “Central” The type series of Eremias inornata Roux, 1907 comprises eight specimens collected from “Oranje-Fluß, Kl.-Namaqualand” [the Orange River, Little Namaqualand, Northern Cape, Province, South Africa]. Syntype ZMA11049 (Zoological Museum Amsterdam) was subsequently designated as the lectotype (Daan and Hillenius 1966). The ZMA collections have subsequently been incorporated into those of the Naturalis Biodiversity Center in Leiden (RMNH). The geographic origin of the specimens and the relatively detailed description and accompanying plate, clearly tie the name-bearing lectotype of Pedioplanis inornata to the P. inornata “South” clade. No other nomina are currently within the synonymy of Pedioplanis inornata and none are available for application to the P. inornata “Central” clade, which is here described as:
Pedioplanis branchi sp. nov.
Etymology: The specific epithet is a patronym formed in the genitive singular honoring our friend and colleague, the British-born South African herpetologist, William Roy Branch (1946–2018), in recognition of his many contributions to African herpetology and in remembrance of many happy trips in the field together.
Distribution: Pedioplanis branchi sp. nov. is endemic to the Erongo Region in Namibia. Its range stretches from just south of the Swakop River in the South, where it occurs in parapatry with P. husabensis, through the pro-Namib, to the Ugab River and the Brandberg in the north and Mount Erongo and Otjimbingwe in the east, probably occurring in parapatry with P. mayeri all along its northeastern border (see Fig. 6 for map of locality records).
 | Figure 9. Habitat of Pedioplanis branchi sp. nov. (a.) Collection site for ZMB 89310 (Farm Friedhelm Sack, Erongo Region, Namibia) from the extended Swakop River Canyon on a marble/calc silicate slope with sparse grass cover and isolated shrubs. (b.) Collection site for ZMB 89612 (not included in study) from a small hill slope in the Tsiseb conservancy in the Pro-Namib, 20 km south of the Brandberg (visible in the background) depicting a sparsely vegetated scree slope with a Commiphora shrub. |
 | Figure 4. Life photographs of representative individuals of Pedioplanis mayeri sp. nov. highlighting color pattern variation within the species. (a.) Dorsal and (b.) lateral whole body images of an adult possessing bold dorsal stripes collected at the type locality (Farm Omandumba, Erongo Region, Namibia), note the row of yellow spots along the flanks; (c.) Dorsal image of an adult from the Kamanjab area depicting fainter, medium-brown dorsal stripes; (d.) An adult female collected from Gobabis (ZMB 80391; see also Fig. 5a) with dorsal striping of varying boldness and a more grayish-brown hindbody compared to the more reddish hindbody observed in other individuals. |
Pedioplanis undata “South”/P. undata “North” Mayer and Böhme (2000) examined the type material of Lacerta undata Smith, 1838 and noted that the rediscovered syntype specimens in the National Museums of Scotland collection were, in fact, representatives of the taxon long associated with the name Pedioplanis lineoocellata pulchella (Gray, 1845) and now, based on the findings of Edwards (2013), considered as P. lineoocellata (Duméril & Bibron, 1839). They proposed to conserve the current usage of names within Pedioplanis by calling on the ICZN in Case 3085 to set aside the original type designation and recognize the designation of a neotype for L. undata. Opinion 1992 of the ICZN (Anonymous 2002) accepted this solution and thus the neotype was fixed as Naturhistorisches Museum Wien (NMW) 31886 from “near Windhoek, Namibia.” This links the name P. undata to the P. undata “South” clade. The assignment of the name Pedioplanis undata to the more restricted, southern clade is notable in that the predominant concept of the species based on previous studies of P. undata is largely affiliated with populations and representative specimens from the more broadly distributed northern clade (Branch 1998; Makokha et al. 2007; Conradie et al. 2012). In these cases the presence of bold dorsal stripes was considered diagnostic for the species, however based on our results this character is now largely applicable to the unnamed northern clade, and is exhibited inconsistently and with variation among true P. undata. No other nomina are currently within the synonymy of Pedioplanis undata and none are available for application to the P. undata “North” clade, which we describe as:
Pedioplanis mayeri sp. nov.
Etymology: The specific epithet is a patronym formed in the genitive singular honoring our friend and colleague, the Austrian lacertid specialist Werner Mayer (1943–2015), who first recognized the distinctiveness of his namesake species and whose contributions to the study of Pedioplanis have been seminal.
Distribution: Pedioplanis mayeri sp. nov. is endemic to northern Namibia and occurs from south of the Kunene River and east of the Namib Desert along the eastern side of the escarpment, thence throughout the eastern Kunene Region, entering the northeastern parts of the Erongo Region and east through the Otjozondjupa Region, reaching at least as far east as Oshikango (TM17028) in the north, Gobabis (Omaheke Region) in the south-east, and Nauchas in the south. It does not enter the Kalahari dune fields, and is possibly absent from the Khomas Hochland, where it is replaced by P. undata (see Fig. 6 for map of locality records).
 | Figure 5. Habitat of Pedioplanis mayeri sp. nov. (a.) Collection site near Gobabis for ZMB 80389–80392 in open savannah woodland, with tall, dense grasses and introduced Opuntia. (b.) Collection site for ZMB 89350 (29 km N of Palmwag, Kunene Region, Namibia) in stony Pro-Namib habitat with sparse vegetation dominated by Euphorbia damarana (center). |

Jackie L. Childers, Sebastian Kirchhof and Aaron M. Bauer. 2021. Lizards of A Different Stripe: Phylogenetics of the Pedioplanis undata Species Complex (Squamata, Lacertidae), with the Description of Two New Species. Zoosystematics and Evolution. 97(1): 249-272. DOI: 10.3897/zse.97.61351
| 1:33a |
[Paleontology • 2021] Yamatosaurus izanagii • A New Basal Hadrosaurid (Dinosauria: Ornithischia) from the latest Cretaceous Kita-ama Formation in Japan implies the Origin of Hadrosaurids
 | (Silhouette & left) Yamatosaurus izanagii & Kamuysaurus japonicus (right)
Kobayashi, Takasaki, Kubota & Fiorillo, 2021 Life reconstruction by Masato Hattori |
Abstract Here we describe a partial hadrosaurid skeleton from the marine Maastrichtian Kita-ama Formation in Japan as a new taxon, Yamatosaurus izanagii gen. et sp. nov., based on unique characters in the dentition. Our phylogenetic analysis demonstrates Yamatosaurus izanagii belongs to Hadrosauridae, composed of Hadrosaurus foulkii + (Yamatosaurus izanagii + (Saurolophinae + Lambeosaurinae)). The coracoid lacks a biceps tubercle as in non-hadrosaurid hadrosauroids, suggesting its presence is a key feature for the clade of Saurolophinae and Lambeosaurinae. The evolutionary rates analysis further supports that shoulder and forelimb features, which are likely to have been involved in locomotion, were important for the early evolution of Hadrosauridae. Our biogeographic analyses show that basal hadrosaurids were widely distributed in Asia and Appalachia, that the clade of Saurolophinae and Lambeosaurinae originated in Asia, and that eastern Asia may have served as a refugium of relict hadrosauroid taxa such as Plesiohadros djadokhtaensis, Tanius sinensis, and Yamatosaurus izanagii during the Late Cretaceous. The contemporaneous occurrence of basal (Yamatosaurus izanagii) and derived (Kamuysaurus japonicus) hadrosaurids during the Maastrichtian in Japan is the first record in Asia. Because of the long geographical distance between these localities, they likely did not co-exist, but instead demonstrate some level of provinciality.
 | Map of Japan, showing the localities of Yamatosaurus izanagii gen. et sp. nov. on Awaji Island (green star), Kamuysaurus japonicus in Mukawa Town (blue star), and other Late Cretaceous hadrosauroids (red circles) (a) and the location of Locality Aw on Awaji Island (b). Ammonite biostratigraphy, showing the position of the Nostoceras hetonaiense Zone (c). Stratigraphic sections of the Kita-ama and Hakobuchi formations (d) and depositional environments of Yamatosaurus izanagii (green star) and Kamuysaurus japonicus (blue star) (e).
Note that (d) differs from Fig. 1 of Tanaka et al.27 because we corrected errors, including the scale and the stratigraphic boundaries between the Kita-ama and Noda formations and between the Campanian and Maastrichtian. Silhouette of Yamatosaurus izanagii, showing recovered skeletal elements (f) (Courtesy of Genya Masukawa). Life reconstruction of Yamatosaurus izanagii (left) and Kamuysaurus japonicus (right) (g) (Courtesy of Masato Hattori).
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 | Right dentary of Yamatosaurus izanagii gen. et sp. nov. in lateral (a), medial (b), dorsal (c), ventral (d), and anterior (e) views. Numbers in white in (b) indicate the positions of nutrient foramina. |
 | An isolated dentary tooth of Yamatosaurus izanagii gen. et sp. nov. from left side in lingual (a) and mesial (b) views and its denticles (c). Isolated dentary teeth of Yamatosaurus izanagii gen. et sp. nov. from left side in distal (d,f) and occlusal (e,g) views. Dentary teeth of Yamatosaurus izanagii gen. et sp. nov. in place on the right dentary in lingual (h) and occlusal (i) view. Numbers in (h), (i), and (j) are tooth positions. Occlusal surfaces of the eleventh and fourteenth teeth are highlighted in light gray in (i). Scales for (a), (b), and (d) to (i) are 1 cm. Scales for (c) and (j) are 0.5 mm and 3 cm, respectively. |
Systematic paleontology Dinosauria Owen, 1842 Ornithischia Seeley, 1888
Ornithopoda Marsh, 1881 Hadrosauridae Cope, 1869
Yamatosaurus izanagii gen. et sp. nov.
Holotype: MNHAH D1-033516, a right dentary, a right surangular, twelve isolated dentary teeth, four cervical vertebrae, a distal caudal vertebra, three cervical ribs, and a coracoid. This specimen is stored in the Museum of Nature and Human Activities, Hyogo, Sanda City, Hyogo Prefecture, Japan.
Diagnosis: A hadrosaurid with unique characters in having only a single tooth as a minimum number of functional teeth per tooth position in the middle of the dentary dental battery (9th, 11th, 14th, 16th, 19th, 21st, and 23rd tooth positions) and the complete absence of the “branched ridges” on the dentary tooth occlusal surfaces. It is also unique in the combination of the additional following characters: the low angle between the dentary symphysis and lateral surface of the dentary and ventrally facing ventral surface of the surangular. Etymology: “Yamato” refers to the ancient name for a region of the Japanese archipelago, including the western half of the main island (Honshu Island), Shikoku Island, and the northern half of Kyushu Island, ruled by the Yamato Kingdom from the third to the seventh century. “Sauros” means reptiles. The specific name, “izanagi”, refers to a deity in Japanese mythology, which created eight countries of Yamato with another deity, Izanami, based on the oldest history book in Japan called “Kojiki (Records of Ancient Matters)”, published in 712 CE (Common Era). The first country created was the Awaji Island, followed by the Shikoku, Oki, Kyushu, Iki, Tsushima, Sado, and Honshu islands.
Locality and horizon: Locality Aw (Morozumi) of Yura Town, Sumoto City of the Awaji Island, Hyogo Prefecture, Japan; the early Maastrichtian (71.94–71.69 Ma) Kita-ama Formation of the Izumi Group.
  Yoshitsugu Kobayashi, Ryuji Takasaki, Katsuhiro Kubota and Anthony R. Fiorillo. 2021. A New Basal Hadrosaurid (Dinosauria: Ornithischia) from the latest Cretaceous Kita-ama Formation in Japan implies the Origin of Hadrosaurids. Scientific Reports. 11: 8547. DOI: 10.1038/s41598-021-87719-5
| 3:32a |
[Ichthyology • 2021] Etelis boweni • A New Cryptic Deepwater Eteline Snapper (Perciformes: Lutjanidae) from the Indo‐Pacific  | Etelis boweni Andrews, Fernandez‐Silva, Randall & Ho, 2021
Photo: NOAA Fisheries |
Abstract A new species of Etelis is described based on 16 specimens collected from the Red Sea and Western Australia, with confirmed genetic records throughout the Indo‐West Pacific. It is similar to and was often misidentified as Etelis carbunculus Cuvier, with both species sharing the diagnostic character of low number of developed gill rakers. Nonetheless, the two species are genetically divergent and differ morphologically in adult body length; proportions of eye, snout, cheek and caudal fin; shape of head, opercular spine and sagittal otolith; and coloration of the tip of the upper caudal fin. Etelis boweni has a wide Indo‐west Pacific distribution that largely overlaps with E. carbunculus, and the two species are often caught on the same fishing line.
Keywords: Actinopterygii, cryptic species, ichthyology, Pisces, snappers, taxonomy
Etelis boweni sp. nov. Bowen's Red Snapper, Giant Ruby Snapper
Etymology: The authors are grateful to name this fish after Dr. Brian W. Bowen of the Hawaiʻi Institute of Marine Biology, University of Hawaiʻi, in recognition of his contributions to the field of Ichthyology, and in particular for his use of molecular genetic techniques in support of the taxonomy of fishes.
 | A fresh caught specimen of Etelis boweni sp. nov. from East Bank, American Sāmoa in 2016, weight 31 kg, estimated >1 m total length.
Photo: NOAA Fisheries |
Kimberly R. Andrews, Iria Fernandez‐Silva, John E. Randall and Hsuan‐Ching Ho. 2021. Etelis boweni sp. nov., A New Cryptic Deepwater Eteline Snapper from the Indo‐Pacific (Perciformes: Lutjanidae). Journal of Fish Biology. DOI: 10.1111/jfb.14720
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