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[Botany • 2019] Dendrobium nagataksaka (Orchidaceae: Epidendroideae) • A New Species of Dendrobium Section Spatulata from Papua, Indonesia

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Dendrobium nagataksaka Metusala

in Metusala, 2019. 
Photo: Anton Tri Raharjo

Abstract
Dendrobium nagataksaka, a new species of Dendrobium section Spatulata (Orchidaceae: Epidendroideae) from Papua, Indonesian New Guinea, is described and illustrated. The flower of this new species is morphologically close to Dendrobium gouldii, but differs in having longer midlobe relative to the sidelobes which it is as long as the sidelobes, a different shape midlobe, and a different shape keels on lip.

Keywords: DendrobiumSpatulata, Papua, Monocots


Dendrobium nagataksaka Metusala, sp. nov.  

Etymology:— The specific epithet “naga” (Bahasa Indonesia) means dragon and “taksaka” is the name of the ancient Indian, Javanese and Balinese mythical dragon. It refers to the shape of the flower which has erect petals and long protruding lip resembling the dragon’s head with long horns and long lip.


Destario Metusala. 2019. Dendrobium nagataksaka (Orchidaceae: Epidendroideae), A New Species of Section Spatulata from Papua, Indonesia. Zootaxa. 415(5); 271–278. DOI: 10.11646/phytotaxa.415.5.3

Spesies baru dari anggrek telah ditemukan di Kabupaten Asmat, Papua, Indonesia. Secara morfologi, anggrek baru ini mirip Dendrobium gouldii, namun terdapat perbedaan pada bagian midlobe-nya.
Pemberian nama spesies "nagatatsaka" secara etimologi berasal dari kata "naga" dan "tatsaka", mitologi naga dari Jawa dan Bali.
Penggunaan nama naga karena bentuk bunga anggrek tersebut memiliki petal berdiri yang mirip seperti tanduk naga.

 


[Entomology • 2019] Colacus rubrofemoratus • A New Species of Colacus Ohaus, 1910 (Coleoptera: Scarabaeidae: Dynastinae) from the Mata Seca Biotope of Brazil, and Notes on Colacus morio Ohaus, 1910

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Colacus rubrofemoratus 
Sobral, Morais, & Grossi, 2019


Abstract
In this contribution, Colacus rubrofemoratus Sobral, Morais, & Grossi new species (Coleoptera: Scarabaeidae: Dynastinae: Agaocephalini) is described and illustrated based on male specimens found in a transitional area of Caatinga, Atlantic Forest, and Cerrado in Brazil. In addition, the female of Colacus morio Ohaus, 1910 is redescribed, a distribution map for the genus is provided, and a new key to the species of Colacus is presented.

Keywords: Coleoptera, Agaocephalini, rhinoceros beetles, Scarabaeoidea, taxonomy




Rafael Sobral, José W. De Morais and Paschoal C. Grossi. 2019. A New Species of Colacus Ohaus, 1910 (Coleoptera: Scarabaeidae: Dynastinae) from the Mata Seca Biotope of Brazil, and Notes on Colacus morio Ohaus, 1910. Zootaxa. 4695(2); 159–167.  DOI: 10.11646/zootaxa.4695.2.5

[Paleontology • 2019] Ferrisaurus sustutensis • A New Leptoceratopsid Dinosaur from Maastrichtian-aged Deposits of the Sustut Basin, northern British Columbia, Canada

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Ferrisaurus sustutensis
 Arbour & Evans, 2019


Abstract 
A partial dinosaur skeleton from the Sustut Basin of northern British Columbia, Canada, previously described as an indeterminate neornithischian, is here reinterpreted as a leptoceratopsid ceratopsian, Ferrisaurussustutensis, gen. et. sp. nov. The skeleton includes parts of the pectoral girdles, left forelimb, left hindlimb, and right pes. It can be distinguished from other named leptoceratopsids based on the proportions of the ulna and pedal phalanges. This is the first unique dinosaur species reported from British Columbia, and can be placed within a reasonably resolved phylogenetic context, with Ferrisaurus recovered as more closely related to Leptoceratops than Montanoceratops. At 68.2–67.2 Ma in age, Ferrisaurus falls between, and slightly overlaps with, both Montanoceratops and Leptoceratops, and represents a western range extension for Laramidian leptoceratopsids.


Systematic palaeontology
DINOSAURIA Owen, 1842
ORNITHISCHIA Seeley, 1888
NEORNITHSICHIA Cooper, 1985
MARGINOCEPHALIA Sereno, 1986

CERATOPSIA Marsh, 1890
NEOCERATOPSIA Sereno, 1986
CORONOSAURIA Sereno, 1986

LEPTOCERATOPSIDAE Nopcsa, 1923

FERRISAURUS SUSTUTENSIS gen. et sp. nov.  

Diagnosis: Ferrisaurus can be differentiated from other known leptoceratopsids based on the following unique combination of characters: penultimate pedal phalanges in digits III and IV are equal or subequal in proximodistal length compared to the length of the preceding phalanx, rather than shorter as in all other leptoceratopsids for which these elements are preserved except possibly USNM 13863 (Cerasinops); astragalus and tibia coossified, unlike all other leptoceratopsids except for AMNH 5464 (Montanoceratops); distal end of ulna broader relative to radius length than in Leptoceratops; distal end of ulna medially bowed, unlike the straight ulna of the penecontemporaneous Maastrichtian taxa Leptoceratops and Montanoceratops, but similar to Cerasinops and Prenoceratops from the Campanian.

Etymology:Iron lizard,” from Latin ferrum (=iron) and Greek sauros (=lizard), in reference to the specimen’s discovery along a railway line, and sustutensis in reference to its provenance near the Sustut River and within the Sustut Basin.

Holotype: RBCM P900, a partial skeleton consisting of a partial right coracoid, fragmentary left scapula, complete left radius, distal portion of the left ulna, associated distal two thirds of the left tibia and fibula and coossified astraglus and ?calcaneum, partial articulated digits III and IV of the right pes, and an unprepared block removed from the posterior surface of the tibia that appears to contain four metatarsals, presumably from the left pes. Previously catalogued as RBCM.EH2006.019.0001 to RBCM.EH2006.019.010 and published under RBCM.EH2006.019 by Arbour & Graves (2008).

Locality: RBCM P900 was discovered near the confluence of Birdflat Creek and the Sustut River in the Sustut Basin (Fig. 1); the bones were found loose in the rubble during construction along the BC Rail line, which has since been abandoned. Fieldwork in the Sustut Basin in 2017 provided strong support for the relocation of the original collection site a few hundred meters from the confluence of the Sustut River and Birdflat Creek (Arbour et al. (in press)); exact GPS coordinates are on file at the Royal BC Museum.

Formation and Age: Tatlatui Member, Tango Creek Formation, Sustut Group. Palynomorphs recovered from the presumed holotype locality included the Maastrichtian marker taxon Pseudoaquilapollenites bertillonites, indicating an age of approximately 68.2–67.2 Ma for the site (Arbour et al. (in press)).

  
Victoria M. Arbour and David C. Evans. 2019.  A New Leptoceratopsid Dinosaur from Maastrichtian-aged Deposits of the Sustut Basin, northern British Columbia, Canada. PeerJ. 7:e7926. DOI:  10.7717/peerj.7926

[Paleontology • 2019] Rare Evidence of A Giant Pliosaurid-like Plesiosaur from the Middle Jurassic (lower Bajocian) of Switzerland

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Pliosaurid-like plesiosaur mandible section (PIMUZ A/III0521) recovered from the Passwang Formation near Arisdorf (Switzerland).

in Sachs, Klug & Kear, 2019.

Abstract
Here, we describe part of a large-bodied macrophagous plesiosaur jaw from the lower Bajocian (Middle Jurassic) Passwang Formation near Arisdorf in the Basel-Land canton of Switzerland. The specimen preserves the posterior glenoid extremity of the right mandibular ramus comprising the surangular, angular, articular, and probably the prearticular. Notable character states include a transversely expanded surangular that incorporates a prominent medial ridge adjacent to the glenoid and a shallow dorsal fossa, together with a conspicuous trough extending across the lateral surfaces of both the surangular and angular; there is also a basally broad and medially deflected retroarticular process. Collectively, these features suggest affinities with Middle–Late Jurassic pliosaurids, as well as some coeval rhomaleosaurids. Based on such comparisons, we estimate that the Passwang Formation mandible was approximately 1.5 m long when complete, and thus approaches the size range of the largest-known pliosaurids. This discovery supplements the sparse record of diagnostic pliosaurid-like remains from Switzerland and contributes to the currently incomplete knowledge of pre-Callovian Middle Jurassic plesiosaurs globally.

Keywords: Plesiosauria, Pliosauromorph, Pliosauridae, Rhomaleosauridae, Bajocian, Apex predator 

Systematic palaeontology
Sauropterygia Owen 1860
Plesiosauria de Blainville 1835

?Pliosauridae indet.

Pliosaurid-like plesiosaur mandible section (PIMUZ A/III0521) recovered from the Passwang Formation near Arisdorf (Switzerland).  




Material: PIMUZ A/III0521, the glenoid extremity of a right mandibular ramus.


Stratigraphic and geographic provenance: Emileia sauzei Zone (early Bajocian) of the upper Passwang Formation exposed on the north-western slope of the Eileten, southeast of Arisdorf, Canton of Basel-Land, north-western Switzerland.


Conclusions: 
Our documentation of the incomplete plesiosaur mandible, PIMUZ A/III0521, from the lower Bajocian upper Passwang Formation near Arisdorf in Basel-Land is significant because it provides a new addition to the hitherto sparse record of plesiosaur fossils from Switzerland (e.g. Geister 1998; Peyer 1940; von Meyer 1856; Wild 1968). It is also one of only a handful of pre-Callovian Middle Jurassic plesiosaur occurrences currently reported from Europe, and indeed, worldwide (e.g. Buchy 2004; Gasparini 1997; Gasparini and Fernández 2006; Godefroit 1994; Kear 2012; Sachs and Hornung 2016; Vincent et al. 2007, Vincent et al. 2013b). PIMUZ A/III0521 displays key traits that suggest affinity with Pliosauridae (Benson and Druckenmiller 2014), as well as morphological compatibility with coeval taxa, especially Simolestes keileni (Godefroit 1994), and the rhomaleosaurids Maresaurus coccai (Gasparini 1997) and Borealonectes russelli (Sato and Wu 2008). However, PIMUZ A/III0521 is proportionately larger, with an estimated complete mandible length of around 1.5 m; this not only hints at possible taxonomic distinction, but also implies that pliosaurid-like plesiosaurs had achieved giant body sizes and radiated ecologically as dominant marine apex predators by at least the early Middle Jurassic.


Sven Sachs, Christian Klug and Benjamin P. Kear. 2019. Rare Evidence of A Giant Pliosaurid-like Plesiosaur from the Middle Jurassic (lower Bajocian) of Switzerland. Swiss Journal of Palaeontology. DOI: 10.1007/s13358-019-00200-9
Rare evidence of a giant Jurassic pliosaur from Switzerland  uu.se/en/news-media/news/article/?id=13528 

  

[Botany • 2019] Coccoloba gigantifolia (Polygonaceae) • A New Species of Coccoloba P. Browne from the Brazilian Amazon with Exceptionally Large Leaves

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Coccoloba gigantifolia E. Melo, C.A. Cid Ferreira & R. Gribel

in Melo, Cid Ferreira & Gribel, 2019. 

ABSTRACT
We describe and illustrate a new species of Coccoloba (Polygonaceae), named Coccoloba gigantifolia, from the Brazilian Amazon. It resembles Coccoloba mollis Casar, but differs from the latter species by its much larger leaves in the fertile branches. The species has only been recorded in the Madeira River basin, in the states of Amazonas and Rondônia, in the central and southwestern Brazilian Amazon. The description was based on herbarium material, cultivated plants, and individual trees in their natural habitat. We provide illustrations, photographs, and an identification key with morphological characteristics that distinguish the new taxon from the other two related taxa of the Coccoloba sect. Paniculatae, as well as comments on the geographic distribution and conservation status of the species.

KEYWORDS: taxonomic botany; Amazon rainforest; geographic plant distribution; Paniculatae

Figure 2 A. Individual of Coccoloba gigantifolia about 15 m high in its natural environment, reaching the sub-canopy of a secondary forest in the Jamarí National Forest (Rondônia state, Brazil); B. Individual in the collection process; C. Trunk of a cultivated adult plant; D. Details of the trunk showing two transverse rings; E. Leaf of a young cultivated plant; F. Leaf sample collected in the Jamarí National Forest (Rondônia state, Brazil), 2.15 m long and 1.38 m wide (abaxial view); G. Adaxial view of the same leaf; H. View of the petiole articulation at ochrea base in a young branch; I. Inflorescence; J-K. Mature fruits 
(photos: A-G and I-K: C.A. Cid Ferreira and R. Gribel, H: E. Melo). 


Coccoloba gigantifolia E. Melo, C.A. Cid Ferreira & R. Gribel sp. nov. (Figures 1-3)


Type material: Brazil. Rondônia. Floresta Nacional do Jamari, Serra da Onça, 2 km from the residential village, .... 05.ix.2008 (fr.), C.A. Cid Ferreira et al. 11211 (Holotype: INPA 258.437).

Trees 10-15 m high, polygamous-dioecious, with a straight, segmented trunk that occasionally sprouts at the base with transverse rings distanced about 10 cm, with thin branches of whitish bark restricted to the apex. The trees also have young, pubescent branches and ferruginous trichomes (Figures 2a-d). Leaves are alternate, spiral, and petiolate. Leaf blades measure 0.6 - 2.5 × 0.5 - 1.4 m and are elliptic, with acute or acuminate apex, base obtuse, subcordate, subtruncate, entire margin, wavy, coriaceous or subcoriaceous, discolor, pubescent glabrescent, pubescent adaxial face with ferruginous trichomes concentrated in the veins when young, pubescent abaxial face with ferruginous trichomes, brochidodromous venation, 16-45 pairs of lateral veins, flat on the adaxial side and prominent on the abaxial face (Figure 2e); petiole is 5-10 cm long, inserted at the base of the ochrea and articulated to it (Figure 2f), older leaves are completely glabrous or puberule; ochrea is 5-10 cm long, persistent at base, coriaceous, pubescent ferruginous, apex with acuminate edge, scariose and deciduous. Inflorescence a branched thyrse, paniculate, 40-80 cm in length (Figure 2g), rachis pubescent or puberulent, glabrescent, triangular bracts, 0.2-0.3 mm, coriaceous, puberulent or pubescent; ochreola campanulate, 0.5-10 mm, membranaceous, puberulent or pubescent with bilobed edge, persistent and lacerated after fruit maturation (Figure 3a). Flowers 1-2 mm in length, greenish-white; staminate flowers with campanulate hypanthium and vestigial pistil, stamens excluded, filaments fused at the base to form a bulbous, nectariferous tissue, covered with whitish papillae (Figure 3b), pistillate flowers with campanulate hypanthium, reduced stamens, reduced and sterile anthers, ovary ovoid, three glabrous styles, stigmas capitate papillose. Anthocarps 5-8 mm long, globose (Figure 3c-d), pubescent or puberulent, red, vinaceous or purple when mature (Figure 2h-i); globose nucules, smooth, slightly grooved, apex acute or pyramidal (Figure 3e), seeds with ruminate endosperm (Figure 3f); fruit pedicels 2-5 mm long, not thickened.

Geographic distribution and habitat: Coccoloba gigantifolia is endemic to the Madeira River basin. So far, individuals have been recorded in the states of Amazonas and Rondônia (Figure 1). At present, individuals have been collected in the wild only in the middle (Jamari and Samuel) and lower (Autazes and Borba) stretches of the Madeira River basin. The distance between the sampled populations of the middle and low Madeira River is of approximately 600 km, which may indicate a disjunct distribution restricted to the Madeira River basin. The scarcity of botanical collections in the region, however, does not allow to draw reliable conclusions about the distribution of the species. Coccoloba gigantifolia grows in open, ombrophylous forests, secondary forests, and in early successional stages (capoeira, in Portuguese), in altitudes of 20-100 m a.s.l., in areas of flat relief, on sandy or clayey, humid soils. Cultivated trees in Manaus bloomed from March to June and exhibited mature fruits in September.

Etymology: The specific epithet of C. gigantifolia is given in reference to its leaves presenting unusual proportions.



CONCLUSIONS: 
We describe a new species of Coccoloba (Polygonaceae), named Coccoloba gigantifolia from the Madeira River basin, in the Brazilian Amazon region. The species is very distinct, mainly due to the large size of the leaf blade, and is further differentiated by the petiole inserted at the base of the ochrea and articulated to it, inflorescence in panicles, campanulate ochreola with bilobate border, globose anthocarps and globose nucules, slightly grooved with an acute or pyramidal apex.


Efigenia de MELO, Carlos Alberto CID FERREIRA and Rogério GRIBEL. 2019. A New Species of Coccoloba P. Browne (Polygonaceae) from the Brazilian Amazon with Exceptionally Large Leaves [Uma nova espécie de Coccoloba P. Browne (Polygonaceae) da Amazônia brasileira com folhas excepcionalmente grandes]Acta Amazonica. 49(4); Epub Nov 04, 2019. DOI: 10.1590/1809-4392201804771

RESUMO: Uma nova espécie de Coccoloba (Polygonaceae) da Amazônia brasileira, denominada Coccoloba gigantifolia, é descrita e ilustrada. É semelhante a Coccoloba mollis Casar. mas difere desta espécie por ter folhas muito maiores nos ramos férteis. A espécie foi registrada apenas na bacia do Rio Madeira, nos estados do Amazonas e Rondônia, no centro e sudoeste da Amazônia Brasileira. A descrição foi feita a partir de material de herbário, plantas cultivadas e observações de campo de indivíduos em seu habitat natural. São apresentadas pranchas ilustrativas, fotografias e uma chave de identificação com caracteres morfológicos que distinguem o novo táxon de outras duas espécies de Coccoloba sect. Paniculatae, bem como, comentários sobre a distribuição geográfica e conservação da espécie.
PALAVRAS-CHAVE: botânica taxonômica; floresta amazônica; distribuição geográfica de plantas; Paniculatae

[Mammalogy • 2019] Camera-trap Evidence that the Silver-backed Chevrotain Tragulus versicolor remains in the wild in Vietnam

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Tragulus versicolor (Thomas, 1910)

in Nguyen, Tran, Hoang,et al., 2019.

Abstract
In an age of mass extinctions, confirming the survival of lost species provides rare second chances for biodiversity conservation. The silver-backed chevrotain Tragulusversicolor, a diminutive species of ungulate known only from Vietnam, has been lost to science for almost three decades. Here, we provide evidence that the silver-backed chevrotain still exists and the first photographs of the species in the wild, and urge immediate conservation actions to ensure its survival.








An Nguyen, Van Bang Tran, Duc Minh Hoang, Thi Anh Minh Nguyen, Dinh Thang Nguyen, Van Tiep Tran, Barney Long, Erik Meijaard, Jeff Holland, Andreas Wilting and Andrew Tilker. 2019. Camera-trap Evidence that the Silver-backed Chevrotain Tragulus versicolor remains in the wild in Vietnam. Nature Ecology & Evolution.   nature.com/articles/s41559-019-1027-7  NatureEcoEvoCommunity.nature.com/u
FOUND: Miniature Fanged ‘Deer’ Rediscovered Tiptoeing Through Vietnam’s Coastal Forests
First-ever Photos and Footage of Silver-backed Chevrotain Confirm First Rediscovery of Lost Mammal on Global Wildlife Conservation’s ‘Most Wanted’ ListGlobalWildlife.org/press/found-chevrotain-miniature-fanged-deer-rediscovered-tiptoeing-through-vietnams-coastal-forests/


Silver-Backed Chevrotain, With Fangs And Hooves, Photographed In Wild For First Time  tinyurl.com/yx86b4wo

  

[PaleoEntomology • 2019] Angimordella burmitina • Pollination of Cretaceous Flowers

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Angimordella burmitina 
Bao, Wang, Li & Dilcher, 2019

The color and morphology of flowers are artistic only. Illustration: Ding-hau Yang. 

Significance: 
Since Darwin, insect pollination was thought to be a key contributor to the Cretaceous radiation of angiosperms. Both insects and angiosperms were common during the mid-Cretaceous, but direct evidence for a Cretaceous insect-angiosperm pollination mode was until now absent. Here, we report a specialized beetle-angiosperm pollination mode preserved in Burmese amber where a tumbling flower beetle is carrying tricolpate pollen grains that belongs to the eudicots that comprise the majority of extant angiosperm species. Our study provides direct evidence of insect pollination of Cretaceous flowers, which is further supported by the flower-visiting body shape, specialized pollen-feeding mouthparts, and zoophilous pollen grains. These findings demonstrate that insect pollination of flowering plants was well established 99 million years ago.

Abstract
Insect pollination of flowering plants (angiosperms) is responsible for the majority of the world’s flowering plant diversity and is key to the Cretaceous radiation of angiosperms. Although both insects and angiosperms were common by the mid-Cretaceous, direct fossil evidence of insect pollination is lacking. Direct evidence of Cretaceous insect pollination is associated with insect-gymnosperm pollination. Here, we report a specialized beetle-angiosperm pollination mode from mid-Cretaceous Burmese amber (99 mega-annum [Ma]) in which a tumbling flower beetle (Mordellidae), Angimordellaburmitina gen. et sp. nov., has many tricolpate pollen grains attached. A. burmitina exhibits several specialized body structures for flower-visiting behavior including its body shape and pollen-feeding mouthparts revealed by X-ray microcomputed tomography (micro-CT). The tricolpate pollen in the amber belongs to the eudicots that comprise the majority of extant angiosperm species. These pollen grains exhibit zoophilous pollination attributes including their ornamentation, size, and clumping characteristics. Tricolpate pollen grains attached to the beetle’s hairs are revealed by confocal laser scanning microscopy, which is a powerful tool for investigating pollen in amber. Our findings provide direct evidence of insect pollination of Cretaceous angiosperms, extending the range insect-angiosperm pollination association by at least 50 million years. Our results support the hypothesis that specialized insect pollination modes were present in eudicots 99 million years ago.

Keywords: amber, insect, angiosperm, pollen, paleoecology


  Fig. 2. Angimordella burmitina and tricolpate pollen grains.
 (A) Habitus. Pollen grains attached to the body are indicated by red dots, unattached are indicated by yellow dots, clumped pollen are indicated by blue squares. (B−H) Locations are highlighted in A. (B and C) Pollen grains near the body. Yellow arrows point to colpi. (D and E) Pollen grains on the body. (F−H) Clumped pollen grains. (G and H) Locations are highlighted in F and G, respectively. Blue arrows point to colpi.

Family Mordellidae Latreille, 1802.
Subfamily Mordellinae Latreille, 1802.

Angimordella burmitina gen. et sp. nov.

Etymology: The generic name is derived from the Latin prefix “angi” (referring to angiosperm) and the genus Mordella Linnaeus. The specific name is derived from Latin “Burmitina,” referring to the mineralogical name of Burmese amber.

Holotype :NIGP171315 (Fig. 1), a complete beetle with left side visible but its right side covered by abundant microbubbles. A thrip is near the maxillary palpi of the beetle on the left side.

Horizon and Locality: Mid-Cretaceous (∼99 Ma); Burmese amber, from the Hukawng Valley, Kachin State, Myanmar.

Diagnosis: Body small, with pronotum and elytra with wrinkles or ridges dorsally; antennae serrate; mesotibiae and metatibiae without any kind of ridge including subapical one; pygidium not well developed, shorter than 1/2 of last abdominal sternite.

 Fig. 3. Ecological reconstruction of Angimordella burmitina. These tumbling flower beetles are feeding on eudicot flowers.
The color and morphology of flowers are artistic only. 
Illustration: Ding-hau Yang. 


Tong Bao, Bo Wang, Jianguo Li, and David Dilcher. 2019. Pollination of Cretaceous Flowers. PNAS. DOI: 10.1073/pnas.1916186116

New fossil pushes back physical evidence of insect pollination to 99 million years ago  phys.org/news/2019-11-fossil-physical-evidence-insect-pollination.html via @physorg_com
A Specialized Beetle-Angiosperm Pollination Mode from mid-Cretaceous Burmese Amber

[Paleontology • 2019] A Polar Dinosaur Feather Assemblage from Australia

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Australian feathered polar dinosaur.

in Kundrát, Rich, Lindgren, et al., 2019. 
 Illustration: Peter Trusler 

Highlights: 
• Fossil feathers from the Koonwarra Fossil Bed in southeastern Australia record the first demonstrable dinosaur (including birds) integumentary structures described from the Mesozoic polar regions.
• This diverse range of non-avian theropod (paravian) and bird feathers more than doubles the number of Mesozoic fossil feather specimens and morphologies recovered from the Gondwanan landmasses to date.
• Possible traces of eumelanosomes imply original dark colouration and patterning. Some of the geologically oldest barbicel-like structures also evince advanced avian-grade flight feather morphologies in the Early Cretaceous.

ABSTRACT
Exceptionally preserved Mesozoic feathered dinosaur fossils (including birds) are famous, but recognized from only very few localities worldwide, and are especially rare in the Southern Hemisphere. Here we report an assemblage of non-avian and avian dinosaur feathers from an Early Cretaceous polar (around 70°S) environment in what is now southeastern Australia. The recovered remains incorporate small (10–30 mm long) basal paravian-like tufted body feathers, open-vaned contour feathers, and asymmetrical bird-like wing feathers that possess high-angled barbs with possible remnants of barbicels — amongst the geologically oldest observed to date. Such morphological diversity augments scant skeletal evidence for a range of insulated non-avian theropods and birds inhabiting extreme southern high-latitude settings during the Mesozoic. Although some of these fossil feathers exhibit what may be residual patterning, most are uniformly toned and preserve rod-shaped microbodies, as well as densely-packed microbody imprints on the barbules that are structurally consistent with eumelanosomes. Geochemical analysis detected no identifiable residual biomolecules, which we suspect were lost via hydrolysis and oxidization during diagenesis and weathering. Nevertheless, an originally dark pigmentation can be reasonably inferred from these melanic traces, which like the coloured feathers of modern birds, might have facilitated crypsis, visual communication and/or thermoregulation in a cold polar habitat.

Keywords: Mesozoic birds, Aves, Paravesmelanosomes, Early Cretaceous







 Martin Kundrát, Thomas H. Rich, Johan Lindgren, Peter Sjövall, Patricia Vickers-Rich, Luis M. Chiappe and Benjamin P. Kear. 2019. A Polar Dinosaur Feather Assemblage from Australia. Gondwana Research. In Press. DOI: 10.1016/j.gr.2019.10.004 

First evidence of feathered polar dinosaurs found in Australia - Uppsala University  mynewsdesk.com/uk/uu/pressreleases/first-evidence-of-feathered-polar-dinosaurs-found-in-australia-2942524 


[Botany • 2019] Amomum spathilabium (Zingiberaceae: Alpinieae) • A New Species from northern Thailand

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Amomum spathilabium W.Kaewsri

in Kaewsri & Kanjanawattanawong, 2019. 


ABSTRACT
Amomum spathilabium, a new species from Nan Province in northern Thailand, is described and illustrated. It is closely related to A. subcapitatum but differs in the labellum shape, anther crest shape and longer ligule. Details on distribution, ecology, etymology, and a preliminary conservation assessment are provided.

KEYWORDS: Amomum subcapitatum, Doi Phukha, native plant, spathulate labellum, taxonomy

Figure 1. Amomum spathilabium W.Kaewsri:
A–B. Habit; C. Detail of ligules; D. Leaves; E. Inflorescences; F. Stamen; G. Detail of flower including a calyx, pistil and corolla (from left):  H. Detail of labellum (from left): front and back views; I. Infructescence with mature fruits. 

Amomum spathilabium W.Kaewsri, sp. nov. 
Type: Thailand, northern: Nan, Doi Phu Kha, ..., 20 June 2010, Kaewsri-254 (holotype BKF!; isotypes BK!). 

Similar to Amomum subcapitatum Y.M.Xia by its winged fruits and and leaf blade, but differs in its ligule being longer, bilobed, 5–7 cm long, papery, apex dry at maturity, glabrous; and the glabrous petiole, 7–17 cm long; a comparison of the characters of these two species is given in Table 1.


Etymology.— The specific epithet of this new species refers to its main distinguishing character, the spathulate labellum shape.

Distribution.— Endemic to Thailand

Ecology.— Growing in montane evergreen forest, on the slope of mountain, in light gaps, 1,326 m above sea level.


Wittaya Kaewsri and Supanath Kanjanawattanawong. 2019. Amomum spathilabium (Zingiberaceae: Alpinieae), A New Species from northern Thailand.  Thai Forest Bulletin (Botany). 47(2); 193-195. DOI: 10.20531/tfb.2019.47.2.11


[Herpetology • 2019] Hyalinobatrachium adespinosai • A New Glassfrog (Centrolenidae: Hyalinobatrachium) from the Topo River Basin, Amazonian Slopes of the Andes of Ecuador

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Hyalinobatrachium adespinosai
Guayasamin, Vieira, Glor & Hutter, 2019


Abstract
A new species of glassfrog (Centrolenidae) is described from the San Jacinto River, an affuent of the Topo River, on the Amazonian slopes of the Ecuadorian Andes. The new species, Hyalinobatrachium adespinosai sp. nov., can be differentiated from all other centrolenids by the combination of its coloration (transparent peritoneum and pericardium) and vocalization (call duration = 0.38–0.44 s, with 9–13 pulses per call; dominant frequency = 4,645–5,001 Hz). However, H. adespinosai sp. nov. is morphologically cryptic with H. anachoretus, H. esmeralda,and H. pellucidum, from which it differs by call traits (in H. anachoretus: call duration = 0.32–0.37 s, with 5 or 6 pulses per call, dominant frequency = 4,670–4,800 Hz; in H. esmeralda: call duration = 0.218–0.257 s, tonal call, dominant frequency = 4,739–5,580 Hz; in H. pellucidum: call duration = 0.112– 0.140 s, tonal, dominant frequency = 5,000–5,710 Hz). Biogeographically, the new species is separated from H. anachoretus by a considerable distance and, also, the Marañon valley. Finally, following IUCN conservation criteria, the status of the new species is considered as Data Defcient. 

Keywords: Amphibia, Anura, Ecuador, Pastaza basin, phylogeny, Tungurahua Province 


Fig. 2. Hyalinobatrachium adespinosai sp. nov. in life, holotype.

    

 Hyalinobatrachium adespinosai new species
Suggested English name: Adela’s Glassfrog
 Suggested Spanish name: Rana de Cristal de Adela 

Holotype. ZSFQ 1648 (JMG 583, Fig. 2), adult male from riverine vegetation along the San Jacinto River (1.3447°S, 78.1814°W; 1,795 m asl), Tungurahua Province, Ecuador, collected by CRH, REG, and KC on 4 August 2017. Paratypes. ZSFQ 1650–52, 1647, adult males with same data as holotype. 


Generic placement. The new species is placed in the genus Hyalinobatrachium (Ruiz-Carranza and Lynch, 1991, as modifed by Guayasamin et al. 2009) on the basis of morphological and molecular data. The main diagnostic phenotypic traits of Hyalinobatrachium are: (1) ventral parietal peritoneum completely transparent; (2) digestive tract and bulbous liver covered by iridophores; (3) humeral spines absent; (4) white bones in life; (5) males call from the underside of leaves; (6) females place the eggs on the underside of leaves; and (7) males provide extended parental care. All the aforementioned characteristics are shared by the new species. Additionally, analyses of the mitochondrial 16S gene place the new species as a close relative of other Hyalinobatrachium species (Fig. 1); thus, generic placement in Hyalinobatrachium is unambiguous.

 Diagnosis. Within the genus Hyalinobatrachium, the new species is diagnosable mainly by having a transparent pericardium. However, the new species is morphologically cryptic with three closely related taxa (H. anachoretus, H. pellucidum, H. esmeralda). Based on comparisons with specimens examined (see Appendix 1), all these species display a similar size and color pattern (pale green dorsum with yellow dots and a transparent venter and pericardium; red heart visible ventrally). However, calls between species diverge noticeably; the major difference is the structure of the call, with two species (H. adespinosai sp. nov. and H. anachoretus) having pulsed calls and the others having tonal vocalizations (Fig. 3; Table 1). The call of H. adespinosai sp. nov. is further differentiated from that of H. anachoretus by being longer, having more pulses per note, and being produced at a higher rate (Table 1). Toe webbing (Toe IV) is less extensive in the new species (21/3 IV 2+) than in H. anachoretus (1+ IV 1+; Twomey et al. 2014). Additionally, the new species and H. anachoretus are separated by considerable distance (airline distance = 473 km), including one of the most important biogeographic barriers in South America, the Marañon valley (see Duellman 1999; Winger and Bater 2015 and references therein). Uncorrected p genetic distances for the mitochondrial gene 16S between H. adespinosai sp. nov. and its closest relatives are summarized in Table 2.

Fig. 5. Distribution of Hyalinobatrachium adespinosai sp. nov. in Ecuador.

Fig. 4. Natural history and in-situ photographs of the new species. (A) Adult male of Hyalinobatrachium adespinosai near his egg clutch; other males were observed on the same leaf as the egg clutch. (B) Close-up of the egg clutch. (C) Spider predation on an unattended egg clutch.

Ecology. All individuals of the new species were found on the underside of leaves of riverine vegetation along the San Jacinto River. The section of river was fast-fowing and had visible rapids. Although the population is locally abundant (as heard from numerous advertisement calls), individuals are very diffcult to observe because they are usually found at the canopy level (4–16 m above ground level). The type series consists of males exclusively; they were calling in the months of July and August. One male (ZSFQ 1648) was apparently guarding an egg clutch containing 22 embryos; both the adult male and the egg clutch were on the same leaf most of the time, but the male also moved to nearby leaves (Fig. 4). 

Distribution. Hyalinobatrachium adespinosai sp. nov. is only known from the type locality: San Jacinto River (...; 1,795 m asl), Tungurahua Province, Ecuador (Fig. 5). 

Evolutionary relationships. The phylogenetic analyses recover Hyalinobatrachium adespinosai sp. nov. haplotypes as sister to haplotypes sampled from H. anachoretus and nested within other members of a monophyletic clade comprised of all other sampled species of Hyalinobatrachium (Fig. 1). The most closely related species to H. adespinosai sp. nov. share several morphological traits, including a red heart exposed ventrally (H. adespinosai + H. anachoretus + H. pellucidum + H. yaku). 


Etymology. The specifc epithet adespinosai honors Adela Espinosa, an Ecuadorian conservationist and board member of the Jocotoco Foundation (http:// www.jocotoco.org). Adela’s work has focused on the conservation of species and ecosystems. The new glassfrog described here is found only within the limits of a natural reserve owned by Adela and her husband, Antonio Páez. We are delighted to recognize Adela’s devotion to nature with this marvelous species.


Juan M. Guayasamin, José Vieira, Richard E. Glor and Carl R. Hutter. 2019. A New Glassfrog (Centrolenidae: Hyalinobatrachium) from the Topo River Basin, Amazonian Slopes of the Andes of Ecuador. Amphibian & Reptile Conservation. 13(2) [General Section]: 133–144 (e194). amphibian-reptile-conservation.org/



Resumen.— Describimos una nueva especie de rana de cristal (Centrolenidae) del río San Jacinto, afuente del río Topo, en la vertiente amazónica de los Andes del Ecuador. La especie nueva, Hyalinobatrachium adespinosai sp. nov., se diferencia de todos los centrolénidos por la combinación de su coloración ventral (peritoneo y pericardio transparentes) y las características de su canto (duración del canto = 0.382–0.430 s, con 9–13 pulsos por canto; frecuencia dominante = 4,645–5,001 Hz). Sin embargo, es morfológicamente críptica con H. anachoretus, H. esmeralda y H. pellucidum, especies de las cuales difere por su canto (en H. anachoretus: duración del canto = 0.32–0.37 s, con 5 or 6 pulsos por canto, frecuencia dominante = 4,670–4,800 Hz; en H. esmeralda: duración del canto = 0.218–0.257 s, tonal, frecuencia dominante = 4,739–5,580 Hz; en H. pellucidum: duración del canto = 0.112–0.140 s, tonal, frecuencia dominante = 5,000–5,710 Hz). Finalmente, siguiendo los criterios de la UICN, sugerimos que Hyalinobatrachium adespinosai sp. nov. sea ubicada en la categoría de Datos Insufcientes. 
Palabras clave. Amphibia, Anura, Cuenca del Pastaza, Ecuador, flogenia, Tungurahua Province 

[Herpetology • 2019] A Revised Dichotomous Key to the Snakes of Italy (Squamata, Serpentes), According to Recent Systematic Updates

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the Snakes of Italy (Reptilia, Squamata, Serpentes)

in Di Nicola, 2019. 

The diffusion of “citizen science” brings considerable benefits to ecological research (Bonney et al. 2009; Dickinson et al. 2012) and involves an increasing use of data provided by “non-professionals” for the establishment of distribution atlases (for instance, through online platforms such as “iNaturalist”). Therefore, it is important that the presented data are sufficiently reliable and, for this reason, photographic documentation of what has been observed is always encouraged. In many cases, however, the circumstances or the conditions of the observed organism do not allow a photographic identification. Dichotomous keys are tools that, in addition to the use by technicians, researchers and students, can be useful to “non-professional” observers to improve the accuracy in the determination of observations to be submitted to the scientific community. This also applies to the herpetological field, and thus to this work, which offers an updated dichotomous key for the determination of Italian snakes (the first since the one published in Corti et al. (2011)) in light of the various systematic updates that affected this taxon.



Matteo Riccardo Di Nicola. 2019. A Revised Dichotomous Key to the Snakes of Italy (Reptilia, Squamata, Serpentes), According to Recent Systematic Updates. Zootaxa. 4686(2); DOI: 10.11646/zootaxa.4686.2.10


[Entomology • 2019] Diversity and Distribution of Pleioplectron Cave Wētā (Orthoptera: Rhaphidophoridae: Macropathinae), with the Synonymy of Weta and the Description of Seven New Species

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A. Pleioplectron auratum sp. nov., adult ♂, Whites Beach, Rarangi. 
B. P. gubernator  sp. nov., two adult ♂♂, Three Pointer, Gouland Downs, Heaphy Track. 

C. P. caudatum sp. nov., adult ♂, Blowfly Hut, Moeraki River, South Westland. 
D. P. flavicorne sp. nov., sub-adult ♀, Blowfly Hut, Moeraki River, South Westland.
 E–F. P. crystallae sp. nov. E. Adult ♂, Cave Brook, Gouland Downs, Kahurangi NP. F. Adult ♀ feeding on Racomitrium Brid. moss, Salisbury Lodge, Mt Arthur, Kahurangi NP.

Hegg, Morgan-Richards & Trewick, 2019

Abstract
The genus Pleioplectron was first described by Hutton (1896) and included six New Zealand species. This genus has since had three species moved, one each to the genera Pachyrhamma Brunner von Wattenwyl, 1888, Miotopus Hutton, 1898 and Novoplectron Richards, 1958. Here we clarify the status and appearance of Pleioplectron simplex Hutton, 1896 (incl. P. pectinatum Hutton, 1896 syn. nov.) and P. hudsoni Hutton, 1896, as well as P. thomsoni(Chopard, 1923) comb. nov., which is transferred from the genus Weta Chopard, 1923. The genus Weta is newly synonymised with Pleioplectron. We also describe seven new species of Pleioplectron from South Island, New Zealand: P. auratum sp. nov., P. caudatum sp. nov, P. crystallae sp. nov., P. flavicorne sp. nov., P. gubernator sp. nov., P. rodmorrisi sp. nov and P. triquetrum sp. nov. We base these descriptions on morphology using fresh specimens of both male and female adults, and provide support for each with DNA sequence variation (mtDNA, partial COI).

Keywords: Cave wētā; Pleioplectron; Rhaphidophoridae; systematics; New Zealand


Fig. 14. Live Pleioplectron Hutton, 1896 in their natural environments.
A–B. P. simplex Hutton, 1896, Hinewai Reserve, Banks Peninsula. A. Adult ♀ feeding on a small native snail Flammulina zebra (Le Guillou, 1842). B. Adult ♂. The different colouration is due to individual variation, not sexual dimorphism.
C–D. P. thomsoni (Chopard, 1923) comb. nov. C. Adult ♂ in natural cave, Trotters Gorge, Otago. D. Adult ♀ in mining tunnel in Bannockburn, Central Otago, where a population of nearly white colour exists.
E. P. hudsoni Hutton, 1896, adult ♀, Otaki Forks, Tararua Forest. F. P. triquetrum sp. nov., ♂, Hinau Track, Kaikōura.

Fig. 15. Live Pleioplectron Hutton, 1896 in their natural environments.
A.P. auratum sp. nov., adult ♂, Whites Beach, Rarangi. B.P. gubernator sp. nov., two adult ♂♂, Three Pointer, Gouland Downs, Heaphy Track.
C. P. caudatum sp. nov., adult ♂, Blowfly Hut, Moeraki River, South Westland. D. P. flavicorne sp. nov., sub-adult ♀, Blowfly Hut, Moeraki River, South Westland.
E–F. P. crystallaesp. nov. E. Adult ♂, Cave Brook, Gouland Downs, Kahurangi NP. F. Adult ♀ feeding on Racomitrium Brid. moss, Salisbury Lodge, Mt Arthur, Kahurangi NP.

Fig. 18. Known distribution of cave wētā in the genus Pleioplectron Hutton, 1896.
A. North Island, New Zealand, showing the distribution of P. hudsoni. B–J. South Island, New Zealand, showing the distribution of the remaining nine species.


Danilo Hegg, Mary Morgan-Richards and Steven A. Trewick. 2019. Diversity and Distribution of Pleioplectron Hutton Cave Wētā (Orthoptera: Rhaphidophoridae: Macropathinae), with the Synonymy of Weta Chopard and the Description of Seven New Species. European Journal of Taxonomy.  577;1–46.  DOI: 10.5852/ejt.2019.577

[Ichthyology • 2019] Netuma patriciae • A New Sea Catfish (Siluriformes: Ariidae) from the Philippines

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Netuma patriciae  
Takahashi, Kimura & Motomrua, 2019


Abstract
A new sea catfish (Ariidae), Netuma patriciae, is described based on the holotype and nine paratypes, 127.3–303.4 mm in standard length, collected from Panay and Luzon islands, Philippines. The new species most resembles N. thalassina (Rüppell 1837), in sharing counts of anal-fin rays (17–19 in N. patriciae, 15–17 in N. thalassina) and a distinct dorsomedian head groove (longitudinal length of the groove, 33.7–40.1% of head length, 22.3–31.0%). However, the new species can be easily distinguished from the latter in having fused vomerine tooth patches, and more numerous free vertebrae (43–44 vs. 41–42 in N. thalassina). Although N. bilineata (Valenciennes in Cuvier and Valenciennes 1840a) has also fused vomerine tooth patches, the new species is distinguished by having fewer free vertebrae (43–44 vs. 47–51 in N. bilineata) and longer dorsomedian head groove (33.7–40.1% of head length vs. 0–9.7%). The new species can also be easily distinguished from both N. thalassina and N. bilineata by having a filamentous dorsal-fin ray (longest dorsal-fin ray 26.9–35.9% of standard length vs 20.3–23.3% in N. thalassina, 20.9–25.3% in N. bilineata, standard length > 127 mm) and a U-shaped junction of dorsomedian head ridge (vs. V-shaped in both species).

Keywords: Teleostei, Fork-tailed catfish, Netuma thalassina, Netuma bilineata, Taxonomy 


Netuma patriciae sp. nov. KAUM–I. 98403, holotype, 200.1 mm SL, Iloilo, Panay Island, Philippines, fresh condition;

Netuma patriciae sp. nov.
(New English name: Whipfin Sea Catfish)

Etymology. The specific name patriciae is in honor of Patricia J. Kailola, the University of the South Pacific and Pacific Dialogue Ltd, in recognition of her research on the catfish family Ariidae.

Distribution. Known only from Panay Island and Manila Bay, Philippines. Type locality Iloilo, Panay Island, Philippines.


Yumeka Takahashi, Seishi Kimura and Hiroyuki Motomrua. 2019. A New Sea Catfish, Netuma patriciae (Siluriformes: Ariidae), from the Philippines. Ichthyological Research.  DOI: 10.1007/s10228-019-00719-4 


[Herpetology • 2019] Acanthosaura tongbiguanensis • A New Species of the Genus Acanthosaura (Squamata, Agamidae) from Yunnan, China

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Acanthosaura tongbiguanensis
 Liu & Rao, 2019


Abstract
A new species of Acanthosaura from Yunnan, China is described based on unique morphometric and meristic external characters and a very distinctive color pattern. The fourteenth species recorded of this genus, Acanthosaura tongbiguanensis sp. nov., was previously considered A. lepidogaster although it more closely resembles A. crucigera. It can be separated from all other species of the genus by having different numbers of subdigital lamellae on the fourth finger and toe, and a different shape of the black eye patch. The new species differs genetically from investigated congeners by percentage distance of 14.46% to 23.27% (cytochrome b gene).

Keywords: Acanthosaura crucigera, Dehong, Acanthosaura lepidogaster, Tongbiguan


Figure 3. Adult male holotype (KIZL201804) of  Acanthosaura tongbiguanensis sp. nov. in life
 A lateral view of the head B dorsal view of the body C dorsal view of the head D lateral view of the body E ventral view of the head F ventral view of the body.


Figure 4. Adult female paratype (KIZL201805) of  Acanthosaura tongbiguanensis sp. nov. in life
 A lateral view of the head B dorsal view of the body C dorsal view of the head D lateral view of the body E ventral view of the head F ventral view of the body.  


Figure 7. Comparison of three different types of eye patch A  Acanthosaura tongbiguanensis sp. nov. B A. lepidogaster C A. nataliae.  


 Acanthosaura tongbiguanensis sp. nov. 
Acanthosaura lepidogaster: Zhao et al. 1999: 82–85.
Acanthosaura lepidogaster: Yang and Rao 2008: 186–187.

Diagnosis: 
A medium-sized (maximum SVL 115.6 mm) agamid lizard with two pairs of spines: postorbital (supraciliary) spines and spines on occiput between tympanum and nuchal crest; tympanum naked; moderately developed gular pouch; scales on flanks randomly intermixed with medium and large scales; nuchal crest present and strongly developed; diastema between the nuchal and dorsal crests present; dorsal crest slightly developed, composed of enlarged, pointed scales beginning at shoulder region and decreasing regularly in size; tail 1.56–1.85 times SVL; black nuchal collar present; black eye patch present; black oblique folds anterior to the fore limb insertions present.

The new species can be separated from all congeners by having different numbers of subdigital lamellae on the fourth finger (19–21) and toe (25–28), and a different shape of the black eye patch, that extends from posterior margin of nostrils through orbit posteriorly and downwards beyond the posterior end of the tympanum but neither meeting the diamond shaped black nuchal collar on nape nor black oblique humeral fold.
....

Etymology: The name refers to Tongbiguan Nature Reserve, the locality where the new species was found.

Figure 10.  Acanthosaura tongbiguanensis sp. nov. A live adult male on the ground B live adult female on a leaf C live adult female asleep on a branch D live juvenile asleep on branches and leaves.


Figure 9. Habitat at the type locality of  Acanthosaura tongbiguanensis sp. nov., Tongbiguan Township, Yingjiang County, Dehong Autonomous Prefecture, Yunnan, China
A distant view B close view.

Distribution: Acanthosaura tongbiguanensis sp. nov. is only recorded in Tongbiguan Nature Reserve including Yingjiang County, Longchuan County and Ruili City, the border region with northern Myanmar in western Yunnan, China, so it probably occurs in northern Myanmar.

Natural history: The type series of Acanthosaura tongbiguanensis sp. nov. was collected at night while they were asleep on small trees in a primordial forest. However, we suppose that they forage for food on the ground during the day. At the type locality we found four other species of reptiles, namely Cyrtodactylus khasiensis (Jerdon, 1870), Pseudocalotes kakhienensis (Anderson, 1879); P. microlepis (Boulenger, 1887); Trimeresurus yingjiangensis Chen et al., 2019; and seven species of amphibians, Leptobrachella yingjiangensis (Yang et al., 2018); Limnonectes longchuanensis Suwannapoom et al., 2016; Megophrys feii Yang et al., 2018; M. glandulosa Fei et al., 1990; Raorchestes longchuanensis (Yang & Li, 1978); Theloderma moloch (Annandale, 1912); Zhangixalus smaragdinus (Blyth, 1852).



 Shuo Liu and Dingqi Rao. 2019. A New Species of the Genus Acanthosaura from Yunnan, China (Squamata, Agamidae).  ZooKeys. 888: 105-132. DOI: 10.3897/zookeys.888.38491

[Crustacea • 2019] Paguroids (Decapoda: Anomura: Diogenidae and Paguridae) of the Remote Oceanic Archipelago Trindade and Martin Vaz, off southeast Brazil, with New Records, Description of Three New Species and Zoogeographical Notes

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Iridopagurus martinvaz 
 Lima, Tavares & de Mendonça, 2019


Abstract
Trindade and Martin Vaz (TMV) is a highly isolated, oceanic volcanic archipelago located some 1200 km off the Brazilian coast and about 4200 km away from the nearest African coast. For almost 100 years Calcinus tibicen (Herbst, 1791) was the only hermit crab species known from TMV. From 2012 to 2018, 263 daytime SCUBA diving and intertidal samplings conducted at TMV yielded 1075 paguroid specimens in 10 species, three of which are established herein as new species: Iridopagurus martinvaz sp. nov., Nematopagurus micheleae sp. nov., and Pagurus carmineus sp. nov. Iridopagurus margaritensis García-Gómez, 1983, and Phimochirus leurocarpus McLaughlin, 1981, both only known from the northern hemisphere, are recorded for the first time from the southwestern Atlantic. Opportunity was taken herein to include hitherto unreported or little known specimens from along the Vitória-Trindade Seamount Chain, namely, Dardanus venosus H. Milne Edwards, 1848, Nematopaguroides pusillus Forest & de Saint Laurent, 1968, Pagurus provenzanoi Forest & de Saint Laurent, 1968, and Phimochirus holthuisi (Provenzano, 1961). The lectotype of Pagurus venosus H. Milne Edwards, 1848 is designated as the neotype for the obscure Pagurus arrosor divergens Moreira, 1905, which thus becomes an objective junior synonym of the former. A list of all paguroid species known from the tropical southern-central Atlantic oceanic archipelagoes and islands (Ascension, Cape Verde, Fernando de Noronha, Gulf of Guinea, Rocas Atoll, Saint Helena, Trindade and Martin Vaz) with their gross distribution in the Atlantic Ocean is provided. Investigation on the existence of patterns of geographic distribution for the paguroid fauna of the tropical southern-central Atlantic oceanic islands showed that 70% percent of the paguroids from TMV are western Atlantic in origin and 30% endemic. No amphi-Atlantic paguroid species are known from TMV. Conversely, the affinity of Ascension’s (33%) and Saint Helena’s (50%) paguroids is with the eastern Atlantic; no western Atlantic paguroids have been reported from these two islands so far. Exploration on the existence of trends of correlation between islands area and species richness through the Spearman’s coefficient of correlation showed that the patterns in the number of paguroid species cannot be explained by variation in island area alone (rs = 0.4728; p = 0.28571).

Keywords: Crustacea, Vitória-Trindade Seamount Chain, species-area relationships, hermit crabs, Crustacea, Paguroidea


 Trindade and Martin Vaz Archipelago (TMV):
A—Position of the TMV relative to the Brazilian continental coastline and Vitória-Trindade Seamount Chain, and isobath curves around TMV; B—Trindade Island viewed from distance; C—Martin Vaz Islands viewed from distance; D–G—Trindade Island; D—rocky-sandy beach near Parcel das Tartarugas, partly exposed at low tide; E—artificial reef substrate (ARS) being deployed on hard bottom composed of large boulders among patches of sand and calcareous algae; F—mixed hard bottom characterised by numerous nodules of calcareous algae; G—irregular hard limestone bottom. A, adapted from Perreira-Filho et al. (2011); photographs by J.B. Mendonça

Daniel Lima, Marcos Tavares and Joel Braga Jr. de Mendonça. 2019.  Paguroids (Decapoda: Anomura: Diogenidae and Paguridae) of the Remote Oceanic Archipelago Trindade and Martin Vaz, off southeast Brazil, with New Records, Description of Three New Species and Zoogeographical Notes. Zootaxa. 4694(1); 1–63. DOI: 10.11646/zootaxa.4694.1.1


[Botany • 2019] Ombrophytum chilensis (Balanophoraceae) • A New Species of Ombrophytum from Chile, with Notes on Subterranean Organs and Vegetative Reproduction in The Family

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Ombrophytum chilensis Kuijt & Delprete

in Kuijt & Delprete, 2019

Abstract
The Chilean desert specimens of Ombrophytum (Balanophoraceae) reported in the literature as O. subterraneum (Asplund) Hansen differ structurally in several respects from that species, which was described from moist tropical forest in Bolivia. Therefore the Chilean specimens are treated as a narrowly endemic, separate species, Ombrophytum chilensis Kuijt & Delprete, on the basis of the type specimen and published photographs. Discussions on morphology, distribution and conservation status are provided for this species. Critical comments on the underground organs and reproduction in Neotropical Balanophoraceae are also presented.

Keywords: Corynaea, Helosis, Langsdorffia, Thonningia, parasitic plants, underground structures, Eudicots

FIGURE 2. Ombrophytum chilensis, details from holotype specimen (Martin 468 (SI [Sheet A]).
 A, Specimen from upper envelope (see Fig. 1), view from external side; B, Same specimen, view from dissected side. Courtesy M. Belgrano. 

FIGURE 3. Inflorescences of Ombrophytum chilensis, from Murata (1997).
Photograph by J.D. Mauseth (near Chiu Chiu, Chile).

Ombrophytum chilensis Kuijt & Delprete, sp. nov. 

Diagnosis:— Ombrophytum chilensis differs from the other species of the genus in the translucent scales on the young peduncle (Fig. 3), while the other species apparently have naked peduncles, except for O. subterraneum having some scattered scales. Equally distinctive are the large, mostly tridentate fertile bracts (i.e., subtending inflorescence branches) that intergrade with the scales below (i.e., on the peduncle), while in other species of the genus they have a truncate-obconical stalk and a hemi-ellipsoid head in O. guayanensis Delprete (2014: 264, figs. 1D, F)), or they are clavate in O. violaceum B. Hansen (1977: 231; Hansen 1980: 58), or with a filiform stalk and distally obtriangular in O. microlepis B. Hansen (1980: 60, figs. 24F, G), or with a flat stalk and a “subulate to bifurcate or irregularly incised dent protruding upward from its lower part” (Hansen 1980: 64) in O. subterraneum.
...

 Distribution and Ecology:— At this time it appears that the above cited Antofagasta site represents the only Chilean one, not just for the genus, but for Balanophoraceae generally. Ecologically, the present species is unusual in existing in one of the most arid regions worldwide, while other species of the genus are mostly found in moist tropical forests, with the possible exception of the Galapagos population that has previously been assigned to O. subterraneum.

 Vernacular name:— Siicha (H.C. Martin 486).

Job Kuijt and Piero G. Delprete. 2019. A New Species of Ombrophytum (Balanophoraceae) from Chile, with Notes on Subterranean Organs and Vegetative Reproduction in The Family. Phytotaxa. 420(4); 264–272. DOI: 10.11646/phytotaxa.420.4.2

[Chilopoda • 2019] Revision of the Neotropical Species of Aphilodontinae (Geophilomorpha, Geophilidae), with Eight New Species and A First Phylogenetic Analysis of the Subfamily

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Mairata itatiaiensis 
Calvanese, Brescovit & Bonato, 2019


Abstract 
Aphilodontinae are a well distinct but poorly known group of soil centipedes (Chilopoda: Geophilomorpha: Geophilidae) inhabiting two disjunct areas in South America and South Africa respectively. A comprehensive revision of the Neotropical species is presented based on the examination of >150 specimens, the phylogenetic analysis of the entire subfamily based on 47 morphological characters, and the description of eight new species from Southeastern Brazil. The Aphilodontinae were confirmed a monophyletic clade within Geophilidae and closely related to Geoperingueyia, with which they share synapomorphic characters in the labrum, second maxillae and forcipules. Particular groups of clypeal setae, inconspicuous lateral parts of labrum and coalescent forcipular throchanteroprefemur and femur were recovered as synapomorphies of the Aphilodontinae. Four monophyletic genera are recognized within the subfamily Aphilodontinae Silvestri, 1909 (1908) (= Brasilophilidae Verhoeff, 1908; = Mecistaucheninae Verhoeff, 1925 n. syn.), three exclusively Neotropical and one exclusively South African. The Neotropical genera are: Aphilodon Silvestri, 1898 (= Mecistauchenus Brölemann, 1907 n. syn.; = Brasilophilus Verhoeff, 1908 n. syn.), with ten species (including A. caboclos n. sp., A. indespectus n. sp., A. meganae n. sp., A. pereirai n. sp. and A. silvestrii n. sp.), characterized by a small terminal spine on the ultimate legs, in both males and females; Mecophilus Silvestri, 1909, with two species (includingM. tupiniquim n. sp.), characterized by elongated forcipular segment and first leg-bearing segment; Mairata n. gen., with two species (M. butantan n. sp. and M. itatiaiensis n. sp.), characterized by the partial reduction of the distal article of the second maxillary telopodite and a particular shape of ultimate legs, in both males and females. The South African genus, Philacroterium Attems, 1926, comprises eleven known species (including P. weberi (Silvestri, 1909) n. comb., P. caffrarium (Verhoeff, 1937) n. comb., P. porosum (Verhoeff, 1937) n. comb., P. brevipes (Verhoeff, 1938) n. comb., P. bidentatum (Lawrence, 1955) n. comb., P. longipes (Lawrence, 1955) n. comb., P. macronyx (Lawrence, 1955) n. comb., P. maritimum (Lawrence, 1963) n. comb., P. pauciporum (Lawrence, 1963) n. comb. and P. transvaalicum (Lawrence, 1963) n. comb.) and is characterized by vestigial lateral parts of the labrum and the complete suppression of the distal article of the telopodites of the second maxillae. Identification keys are provided for the Aphilodontinae genera and for the species of Aphilodon, Mecophilus and Mairata n. gen. The known occurrence of Aphilodon in Brazil is extended from the states of São Paulo and Mato Grosso to the states of Minas Gerais and Rio de Janeiro, that of Mecophilus from the state of Paraná to the state of São Paulo.

Keywords: Myriapoda, centipedes, taxonomy, morphology, phylogeny, biodiversity



Victor C. Calvanese, Antonio D. Brescovit and Lucio Bonato. 2019. Revision of the Neotropical Species of Aphilodontinae (Geophilomorpha, Geophilidae), with Eight New Species and A First Phylogenetic Analysis of the Subfamily. Zootaxa. 4698(1); 1–72. DOI: 10.11646/zootaxa.4698.1.1


[Paleontology • 2019] Fukuipteryx prima • An Unusual Bird (Theropoda, Avialae) from the Early Cretaceous of Japan suggests Complex Evolutionary History of Basal Birds

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Fukuipteryx prima
Imai, Azuma, Kawabe, Shibata, Miyata, Wang & Zhou, 2019

(artwork by M. Yoshida)

Abstract
The Early Cretaceous basal birds were known largely from just two-dimensionally preserved specimens from north-eastern China (Jehol Biota), which has hindered our understanding of the early evolution of birds. Here, we present a three-dimensionally-preserved skeleton (FPDM-V-9769) of a basal bird from the Early Cretaceous of Fukui, central Japan. Unique features in the pygostyle and humerus allow the assignment of FPDM-V-9769 to a new taxon, Fukuipteryx prima. FPDM-V-9769 exhibits a set of features comparable to that of other basalmost birds including Archaeopteryx. Osteohistological analyses indicate that FPDM-V-9769 is subadult. Phylogenetic analyses resolve F. prima as a non-ornithothoracine avialan basal to Jeholornis and outgroup of the Pygostylia. This phylogenetic result may imply a complex evolutionary history of basal birds. To our knowledge, FPDM-V-9769 represents the first record of the Early Cretaceous non-ornithothoracine avialan outside of the Jehol Biota and increases our understanding of their diversity and distribution during the time.


Figure 1: FPDM-V-9769. a Photograph. A box indicates where a sample was taken for osteohistological analyses. b Schematic line drawing of the skeletons. Abbreviations: cev cervical vertebra, co coracoid, dv dorsal vertebra, fe femur, fu furcula, hu humerus, il ilium, mc metacarpal, md manual digit, py pygostyle, ra radius, sv sacral vertebra, ti tibia, ul ulna. Scale bars equal 3 cm in a and b

Figure 2: Reconstructions and restoration. a–c Skeletal reconstructions of FPDM-V-9769 in cranial (a), dorsal (b), and left-lateral (c) views. d Life restoration of Fukuipteryx prima (artwork by M. Yoshida). One side of a cube in each image equals 1 cm

Systematic palaeontology
Theropoda Marsh, 1881
Maniraptora Gauthier, 1986
Avialae Gauthier, 1986

Fukuipteryx prima gen. et sp. nov.


Etymology: Fukui refers to Fukui Prefecture in central Japan, where the specimen was collected, and pteryx (Latin) for wingprima (Latin) for primitive, as the species exhibits several primitive morphological features among fossil birds.

Diagnosis: A pigeon-sized non-ornithothoracine avialan with the following autapomorphies: semicircular depression on the craniodorsal corner of the humeral head, dorsally bowed humeral shaft, and robust pygostyle with incipient spinal processes and paddle-like structure at the distal end.

Holotype: FPDM-V-9769 (FPDM: Fukui Prefectural Dinosaur Museum, Fig. 1), a disarticulated but closely associated skeleton, including right surangular; two cervicals; four dorsals including two nearly complete ones, an isolated centrum, and incomplete vertebral arch; incomplete synsacrum composed of two sacrals; five caudals; pygostyle; several dorsal ribs; incomplete furcula; incomplete left and right coracoids; incomplete right ilium; forelimbs including left humerus, incomplete left and complete right ulna, complete left and incomplete right radius, right major metacarpal, left minor metacarpal, left alular digit 1, left major digits 2 and 3, minor digits 3 and 4; and hindlimbs including left and right femur; left and right incomplete tibia; and variably preserved metatarsals II (left), III (incomplete left), and IV (complete left and incomplete right).

Type locality and horizon: Kitadani Dinosaur Quarry in the northern part of the city of Katsuyama, Fukui, Japan (Supplementary Fig. 1); the Lower Cretaceous Kitadani Formation (Aptian)23 (see Supplementary Notes for further details).



Takuya Imai, Yoichi Azuma, Soichiro Kawabe, Masateru Shibata, Kazunori Miyata, Min Wang and Zhonghe Zhou. 2019. An Unusual Bird (Theropoda, Avialae) from the Early Cretaceous of Japan suggests Complex Evolutionary History of Basal Birds. Communications Biology. 2: 399.  nature.com/articles/s42003-019-0639-4



[PaleoIchthyology • 2019] Cretodus houghtonorum • A New Large Late Cretaceous Lamniform Shark from North America, with Comments on the Taxonomy, Paleoecology, and Evolution of the Genus Cretodus

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  Cretodus houghtonorum
Shimada & Everhart, 2019


ABSTRACT
We describe a partial skeleton of the Late Cretaceous shark, Cretodus, collected from the Blue Hill Shale (middle Turonian) in north-central Kansas, U.S.A. It consists of 134 disarticulated teeth, 61 vertebrae, 23 placoid scales, and fragments of calcified cartilage. The scale morphology suggests that Cretodus was a rather sluggish shark, and the vertebral morphology affirms its placement into Lamniformes. With a strong tendency towards monognathic heterodonty, the dental morphology indicates that the specimen belongs to a new species, Cretodus houghtonorum, sp. nov., increasing the total known species of Cretodus to five. The five species can be divided into three distinct groups: the longiplicatus/semiplicatus-grade, gigantea/houghtonorum-grade, and crassidens-grade. Cretodus, that successively evolved by broadening the tooth crown. The individual of C. houghtonorum, sp. nov., is estimated to be about 515 cm in total length (TL). Our vertebra-based growth analysis suggests that the shark was about 118 cm TL at birth and that the species had an estimated maximum growth length of 684 cm TL. The large size at birth indicates that the intrauterine cannibalism behavior of embryos seen in extant lamniforms had already evolved by the Late Cretaceous. Where C. houghtonorum, sp. nov., preferred nearshore environments, the specimen co-occurred with isolated teeth of Squalicorax and fragments of two dorsal fin spines of a hybodont shark, circumstantially indicating that the individual of Cretodus fed on the much smaller hybodont and was scavenged by Squalicorax.


SYSTEMATIC PALEONTOLOGY

Class CHONDRICHTHYES Huxley, 1880
Subclass ELASMOBRANCHII Bonaparte, 1838

Cohort EUSELACHII Hay, 1902
Subcohort NEOSELACHII Compagno, 1977

Order LAMNIFORMES Berg, 1958

Family PSEUDOSCAPANORHYNCHIDAE Herman, 1979

Included Genera— Cretodus Sokolov, 1965; Eoptolamna, Kriwet, Klug, Canudo, and Cuenca-Bescos, 2008a; Leptostyrax Williston, 1900; Protolamna Cappetta, 1980; Pseudoscapanorhynchus Herman, 1977.

Genus CRETODUS Sokolov, 1965

Included Species— Cretodus crassidens (Dixon, 1850); C. gigantea (Case, 2001); C. houghtonorum, sp. nov. (this study); C. longiplicatus Werner, 1989; C. semiplicatus (Agassiz, 1843).


CRETODUS HOUGHTONORUM, sp. nov.

    Lamna semiplicata Agassiz, 1843: Cappetta, 1973:506, figs. 3.7, 3.7’.
    Odontaspis macrota Agassiz, 1843: Edward, 1976:67, fig. 1d–h.
    Cretodus semiplicatus (Agassiz, 1843): Wolberg, 1985a:10, figs. 3.10–3.21; Wolberg, 1985b:4, fig. 3f, g, j.
    Cretodus crassidens (Dixon, 1850): Welton and Farish, 1993:98, 1a, b, 2, two leftmost teeth on row ‘a’ and third tooth from the left on row ‘b’ on p. 99 (others on pp. 98–99 questionable).
    Cretodus semiplicatus (Agassiz, 1843): Williamson et al., 1993:figs. 5.6–5.8.
    Cretodus crassidens (Dixon, 1850): Cappetta and Case, 1999:21, fig. 2a–h; Cicimurri, 2004a:9–10, fig. 5e; Shimada, 2006b:166, figs. 3b, 4d; Becker et al., 2010:255, 257, figs. 5.6–5.9, 6.1?
    Cretodus sp.: Shimada et al., 2010a:fig. 4c.
    Cretodus crassidens: Bice and Shimada, 2016:177, fig. 3h (not 3g); Ouroumova et al., 2016: fig. 2l.

Diagnosis— Cretodus differing from all other known species of the genus by having teeth with moderately wide principal cusp, small lateral cusplets relative to principal cusp in tall, erect teeth, ‘V’-shaped crown base, relatively narrow tooth neck on lingual face, ‘V’-shaped basal root concavity, and short root lobes.

Etymology— The species name, houghtonorum, is in honor of Keith and Deborah Houghton, the owners of the land where the Cretodus specimen was found and who kindly donated the specimen to FHSM for the purpose of this present study.



Kenshu Shimada and Michael J. Everhart. 2019. A New Large Late Cretaceous Lamniform Shark from North America, with Comments on the Taxonomy, Paleoecology, and Evolution of the Genus CretodusJournal of Vertebrate Paleontology. e1673399. DOI: 10.1080/02724634.2019.1673399

Dinosaur-era shark fossil discovered in Kansas; researchers name it Cretodus houghtonorum
Fossil dig leads to unexpected discovery of 91-million-year-old shark new to science  phys.org/news/2019-11-fossil-unexpected-discovery-million-year-old-shark.html 

[Herpetology • 2019] Leptobrachella namdongensis • A New Species of Leptobrachella Smith 1925 (Anura: Megophryidae) from Thanh Hoa Province, Vietnam

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Leptobrachella namdongensis 
Chung, Nguyen, Luu, Nguyen & Jiang, 2019

RAFFLES BULLETIN OF ZOOLOGY. 67

Abstract
 Based on the results of molecular and morphological systematics analyses, a new species, Leptobrachella namdongensis, is recognised from Nam Dong Conservation Area in Thanh Hoa Province, Vietnam. Genetic divergences in the16S rRNA gene between the new form and other species in the genus range from 4.7 to 21.0% and average at approximately 24%. The new species is most similar to L. petrops and L. puhoatensis, but can be distinguished from them and other congeners by a combination of the following morphological characters: size medium (30.9 mm in the adult male and 32.1–35.3 mm in adult females); head wider than long; tympanum distinct; throat immaculate white, chest and belly with dark specking on outer margins; toes with basal webbing; supratympanic fold edged by a distinct black line; inter-orbital region with distinct black blotches; iris bicoloured, upper half copper, fading to golden in its lower half; head without dorsolateral markings. 

Key words: Nam Dong Conservation Area, phylogenetics, Vietnam, taxonomy


Fig. 3. Dorsolateral view (A) and ventral view (B) of the holotype (VNUF A.2017.37, male) of Leptobrachella namdongensis, new species in life. 
Photos by Vinh Q. Luu.

Fig. 6. Paratypes of Leptobrachella namdongensis, new species in life.
 A, female VNUF A.2017.95 (SVL 32.1mm); B, female VNMN2019.04 (SLV 33.0mm); C, female IEBR 4512 (SVL 32.2mm).
 Photos by Vinh Q. Luu.

Leptobrachella namdongensis, new species

Diagnosis. Leptobrachella namdongensis, new species is distinguished from its congeners by a combination of the following morphological characters: size medium (30.9 mm in the adult male and 32.1–35.3 mm in adult females); head wider than long; tympanum distinct; throat immaculate white, chest and belly with dark specking on outer margins; toes with basal webbing and without lateral fringe; supratympanic fold edged by a distinct black line; inter-orbital region with distinct black blotches; iris bicoloured, upper half copper, fading to golden in its lower half; head without dorsolateral markings.

Etymology. Specific epithet is in reference to the type locality of the Nam Dong Conservation Area. We recommend “Nam Dong litter frog” as the common English name and “Cóc mày nam động” as the Vietnamese name.

Distribution and ecological notes. Leptobrachella namdongensis, new species is currently known from Nam Dong Conservation Area and Pu Hu Nature Reserve (NR), Thanh Hoa Province, Vietnam. All specimens of the new species were found on rocks in small streams or near cascade streams in evergreen forest at elevations between 500 and 740 m a.s.l. (Fig. 7). Leptobrachella namdongensis, new species occurs sympatrically with Leptobrachella ventripunctata.

Fig. 7. Habitat of Leptobrachella namdongensis, new species in Nam Dong Conservation Area, Thanh Hoa Province, Vietnam.



Hoang Van Chung, Nguyen Thien Tao, Luu Quang Vinh, Nguyen Quang Truong and Jiang Jianping. 2019. A New Species of Leptobrachella Smith 1925 (Anura: Megophryidae) from Thanh Hoa Province, Vietnam. RAFFLES BULLETIN OF ZOOLOGY67;  536–556.  

     


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