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Fig. 6 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 6. Phylogenetic relationships of Shri devi Turner, Montanari, and Norell, 2021, among the dromaeosaurid dinosaurs. Values of the antorbital fenestra elongation (measured as the ratio of the posterior margin height to the longitudinal length) and elongation of the maxilla (measured as the ratio of the maxilla length to its height; data after Powers et al. 2022) are mapped on the 50% majority rule consensus trees generated from the modified data matrices of Powers et al. 2022 (A), and Napoli et al. 2021 (B). White rectangles represent the missing data.

Fig. 9 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 9. Artistic post-mortem reconstruction of the Shri devi Turner, Montanari, and Norell, 2021, individual represented by a specimen ZPAL MgD-I/97 before its final burial. Artwork by Jakub Zalewski (CC BY-NC-ND-3.0).

Fig. 5 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 5. Results of the PCA for the linear measurements of maxilla (A) and pes (B) for the velociraptorines from the Upper Cretaceous of the Gobi Desert. Blue dots represent specimens from the Djadokhta strata, orange from the Baruungoyot strata, green from Ukhaa Tolgod, and black and grey from Bayan Mandahu.

Fig. 3 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 3. Dromaeosaurid dinosaur Shri devi Turner, Montanari, and Norell, 2021 (ZPAL MgD-I/97) from the Upper Cretaceous, Khulsan, Ömnögovi, Gobi Desert, Mongolia. Photographs (A1, A2, A4, A5) and 3D model (A3, A6, A7) obtained from the CT scan of the left side of the skull in dorsal (A1), medial (A2, A3), anterior (A6), and lateral (A7) views. Elements of the left palate in dorsal (A4) and ventral (A5) views. Right maxilla in the lateral (A8, A9) and anterior (A10) views, with the margin of the antorbital fenestra indicated by dashed lines, and the close up of the fifth (A11) and the second (A12) preserved tooth in labial views showing very weakly developed denticles on the mesial carina. Right mandible in the lateral (A13, A14) and medial (A15, A16) views. B. Explanatory drawings of the skull in left (B1) and right (B2) lateral views with the preserved bones (in grey).

Fig. 4 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 4. Dromaeosaurid dinosaur Shri devi Turner, Montanari, and Norell, 2021 (ZPAL MgD-I/97) from the Upper Cretaceous, Khulsan, Ömnögovi, Gobi Desert, Mongolia. A. Left metatarsus in anterior (A1, A2) and posterior (A3, A4) views, and phalanges of digit IV (A5), digit III (A6), digit II (A7), and digit I (A8) in medial views, metatarsal I in anterior view (A8). Ungual III-4 is presented as a 3D model obtained from the CT scan. B. Plot presenting the elongation of II-3 in relation to the length of metatarsal II in dromaeosaurid dinosaurs. Blue dots represent specimens from the Djadokhta strata, orange from the Baruungoyot strata, black from Bayan Mandahu, and white from North America.

Fig. 8 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 8. Reconstruction of the dromaeosaurid dinosaur Shri devi Turner, Montanari, and Norell, 2021, based on ZPAL MgD-I/97 and MPC-D 100/980. A. Skull; missing elements reconstructed on the base of Velociraptor mongoliensis Osborn, 1924 (MPC-D 100/25 and MPC-D 100/54). B. Whole body silhouette with known remains of the holotype and referred material. Silhouette based on V. mongoliensis drawn by J.A. Headden (Wikimedia Commons CC-BY-3.0).

Fig. 2 in Skull of a dromaeosaurid dinosaur Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms

Fig. 2. Dromaeosaurid dinosaur Shri devi Turner, Montanari, and Norell, 2021 (ZPAL MgD-I/97) from the Upper Cretaceous, Khulsan, Ömnögovi, Gobi Desert, Mongolia. Specimen prior to the preparation work (A1), and the 3D model of the skeleton, based on the CT and surface scanner data, with elements arranged as originally found (A2).

Fig. 2 in New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

Fig. 2. Ceratopsian dinosaur Protoceratops andrewsi Granger and Gregory, 1923 (MPC-D 100/505), from the Late Cretaceous, Zamyn Khond, Ömnögovi, Mongolia. Skull in right (A1) and left (A2) lateral views.

Fig. 7 in New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

Fig. 7. Hypothesized chronology of the Late Cretaceous Gobi Desert strata with a schematic representation of the accumulation of apomorphic Bagaceratops-phenotype features in the Protoceratops andrewsi–Bagaceratops rozhdestvenskyi lineage recorded in each of localities.

Fig. 5 in New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

Fig. 5. Ceratopsian dinosaur cf. Bagaceratops sp. (MPC-D 100/551B, field number 000719 US FJMBaga), from the Late Cretaceous, Üüden Sair, Ömnögovi, Mongolia. Skull in left lateral (A1, A2), dorsal (A3, A4), and right lateral (A5, A6) views. Slab with the skeleton in left laterodorsal view (A7). Abbreviations: l, left; r, right.

Fig. 6 in New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

Fig. 6. Distribution of the apomorphic features within the protoceratopsid material from different Late Cretaceous localities of the Gobi Desert. A. Ratio of maxillary diastema to tooth row length (after Czepiński 2019). B. Long diastema (>35% of tooth row). C. Fused nasal horn. D. No premaxillary dentition. E. Accessory antorbital fenestra. F. Sharp buccal crest of dentary. Note: A, number of specimens for each sample, with sympatric taxa separated by a comma (Bagaceratops rozhdestvenskyi, Breviceratops kozlowskii in Khulsan, and B. rozhdestvenskyi, Protoceratops hellenikorhinus in Bayan Mandahu); B–F, number of specimens showing the apomorphic features (grey-shaded area) and the total number of specimens in which the condition state can be recognized. Detailed information in SOM.

Fig. 3 in New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata

Fig. 3. Ceratopsian dinosaur Protoceratops andrewsi Granger and Gregory, 1923 (MPC-D 100/551), from the Late Cretaceous, Üüden Sair, Ömnögovi, Mongolia. Skull in left lateral (A1, A2), dorsal (A3, A4), and right lateral (A5, A6) views. Slab with the skeleton in left laterodorsal view (A7). Abbreviations:, left; r, right.

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Figure 2 in New distributional records of four amphidromous gobies (Gobioidei: Sicydiinae) in continental Vietnam

Figure 2. – Preserved specimens collected during the surveys near Da Nang, Vietnam: (A) Sicyopterus lagocephalus female (73.2 mm SL, HNUE-F00295), (B) Sicyopus zosterophorus male (39.8 mm SL, HNUE-F00296), (C) S. zosterophorus female (43.4 mm SL, HNUE-F00296), (D) Stiphodon atropurpureus male (34.5 mm SL, HNUE-F00298), (E) S. atropurpureus female (35.8 mm SL, HNUE-F00298), (F) Stiphodon percnopterygionus male (21.7 mm SL, HNUE-F00301).

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Figure 1 in Accounting for variability in life-history traits for the definition of amphidromous goby fry fisheries closure periods

Figure 1. – Ranking of the 4096 alternatives of fisheries closure periods based on the MULTIMOORA analysis on the abundance and life-history traits of Sicyopterus lagocephalus and Cotylopus acutipinnis. The best alternative is ranked 1 and the worst 4096. Fisheries closure periods are colour coded.

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Figure 2. – A in First distributional record of the goby Mangarinus waterousi (Perciformes: Gobiidae) from Vellar estuary, southeast India

Figure 2. – A: Anaesthetized male of Mangarinus waterousi collected in the Vellar estuary (CASMBAURM/2312612); B: Head; C: Dorsal fins; D: Pectoral fin; E: Anal fin; F: Caudal fin; G: Preserved holotype specimen of M. waterousi collected from Philippines (CAS-SU 36817).

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Figure 2 in DNA barcoding of two amphidromous goby postlarvae ('penja') morphotypes from Mandar River, West Sulawesi, Indonesia

Figure 2. – Neighbour-joining phylogenetic tree of amphidromous gobiid post-larvae ('penja') from the Mandar River based on Cytochrome oxydase I (COI) sequences.

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Figure 3 in DNA barcoding of two amphidromous goby postlarvae ('penja') morphotypes from Mandar River, West Sulawesi, Indonesia

Figure 3. – Penja gobiid post-larvae from the Mandar River: A. 'penja alus' (Stiphodon semoni), B. 'penja mawassar' (Sicyopterus longifilis).

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Fig. 1 in First Japanese Record of the Rare Goby Trimma panemorfum Winterbottom and Pyle, 2022 from Okinawa Island, Ryukyu Islands, Southern Japan (Teleostei, Gobiidae)

Fig. 1. Trimma panemorfum collected from Hamahiga Island, off Okinawa Island, Ryukyu Islands, Japan (OMNH-P 43986, 14.9 mm SL). A, preserved specimen, photographed by K. Fujiwara; B and C, fresh specimen, photographed by T. Suzuki.

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Fig. 6 in Comparative Analysis of Complete Mitogenomes of Two Gobies and Their Phylogenetic Implication.

Fig. 6. Termination-associated sequences (TAS), conserved sequence blocks (CSB-1, CSB-2, and CSB-3) and central conserved sequences (CSB-D) and GTGGG box in control region of two Oxyurichthys species mitogenomes.