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Figure 2 from: Topalović O, Moore JF, Janssen T, Bert W, Karssen G (2017) An early record of Meloidogyne fallax from Ireland. ZooKeys 643: 33-52. https://doi.org/10.3897/zookeys.643.11266
Figure 2 - The comparison of tail and hyaline tail terminus shape in second-stage juveniles, lateral position. A an unknown Irish species B type material of Meloidogyne fallax C type material of Meloidogyne chitwoodi D type material of Meloidogyne minor E reference material of Meloidogyne hapla; F reference material of Meloidogyne incognita. Scale bar = 20 µm.
Figure 3 from: Topalović O, Moore JF, Janssen T, Bert W, Karssen G (2017) An early record of Meloidogyne fallax from Ireland. ZooKeys 643: 33-52. https://doi.org/10.3897/zookeys.643.11266
Figure 3 - The comparison of anterior region in males of populations of observed Meloidogyne species. A an unknown Irish species (ventral position) B type material of Meloidogyne fallax (lateral position); C: type material of Meloidogyne chitwoodi (ventral position) D reference material of Meloidogyne hapla (lateral position) E reference material of Meloidogyne incognita (lateral position) F type material of Meloidogyne minor (lateral position). Scale bar = 20 µm.
Figure 1 from: Topalović O, Moore JF, Janssen T, Bert W, Karssen G (2017) An early record of Meloidogyne fallax from Ireland. ZooKeys 643: 33-52. https://doi.org/10.3897/zookeys.643.11266
Figure 1 - Comparison of perineal patterns in females. A Irish unknown Meloidogyne sp. B type material of Meloidogyne fallax; C type material of Meloidogyne chitwoodi D type material of Meloidogyne minor. Scale bar = 20 µm.
FIGURE 2 in First record and a new species of the fossil dragonfly genus Proinogomphus (Odonata: Liassogomphidae) from the Early Jurassic of Bascharage in the Grand Duchy of Luxembourg
FIGURE 2. Photograph of holotype SMNS 67854 of Proinogomphus kreuzerorum sp. nov. Scale bar = 5 mm.
Fig. 5 in Early evolution of Coriariaceae (Cucurbitales) in light of a new early Campanian (ca. 82 Mya) pollen record from Antarctica
Fig. 5. Fossil and extant representatives of Coriariaceae observed with light microscopy. A, B, D, E, G & H, Pollen of Coriaripites goodii sp. nov. from the late Cretaceous of Antarctica (blue frames). A & B, Pollen on slide BA-Pal. ex CIRGEO Palin 611b: C54-1; D & E, Pollen on slide BA-Pal. ex CIRGEO Palin 963b: R31-1; G & H, Pollen on slide BA-Pal. ex CIRGEO Palin 698b: E30-2. All grains in polar view. A & B, Note the well-defined fastigium and short colpi with pointed ends (arrowheads); D & E, Note stratified thin exine and short colpi (arrowheads); G & H, Pollen with four apertures; note clearly defined fastigium and very short colpi (arrowheads). C, F & I, Pollen of extant species for comparison (magenta frames). C, Extant Coriaria plumosa; F, Extant Coriaria ruscifolia; I, Extant Coriaria myrtifolia, pollen with four apertures and clearly defined fastigium (arrowhead). — Scale bars = 5 μm.
Fig. 3 in Early evolution of Coriariaceae (Cucurbitales) in light of a new early Campanian (ca. 82 Mya) pollen record from Antarctica
Fig. 3. Chronogram for Coriariaceae inferred from the concatenated ML alignment. The stars indicate a constraint based on the early Campanian (82 Mya) pollen described in this study and another based on the Oligocene flowering branch shown in Fig. 2B, which has been dated to 23 to 33.9 Mya. We here set this constraint to 33 Mya An alternative chronogram in which we set the same fossil to 23 Mya is shown in suppl. Fig. S2. We used a relaxed clock model; the permitted age ranges around the two fossil constraints are described in Materials and Methods and symbolized by the curves above the asterisks. Accessions in blue are from Australasia, in red from America, in purple from Eurasia, and in yellow from Eastern Asia. NI stands for North Island and SI for South Island. Error bars around age estimates are shown in suppl. Fig. S1.
Text-fig. 16. Carnivorans from Gaverdovsky and Volchaya Balka, Late Miocene, North Caucasus. a–c – Promephitis maeotica, p4, dex, GIN-1144-302, a – labial, b – lingual, c – occlusal view; d–e –?Procyonidae gen., occlusal view; d – dP3, sin, GIN-1143-401, e – dP4, sin, GIN-1144-301. in Late Miocene (Early Turolian) Vertebrate Faunas And Associated Biotic Record Of The Northern Caucasus: Geology, Taxonomy, Palaeoenvironment, Biochronology
Text-fig. 16. Carnivorans from Gaverdovsky and Volchaya Balka, Late Miocene, North Caucasus. a–c – Promephitis maeotica, p4, dex, GIN-1144-302, a – labial, b – lingual, c – occlusal view; d–e –?Procyonidae gen., occlusal view; d – dP3, sin, GIN-1143-401, e – dP4, sin, GIN-1144-301.
Fig. 1 in New Early Records from the Intendant's Palace Site (Québec City) for the Introduction of some Adventive Coleoptera in Eastern Canada
Fig. 1. Taxa identified from the Intendant's Palace archaeological site in Québec City.
Figure 5 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 5 - Detail of Zophotermes ashoki Engel and Singh, sp. n. (Tad-42), dorsal view of thorax and anterior portion of forewings (slightly reconstructed).
Figure 6 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 6 - Wing venation of Cambay amber species of Zophotermes Engel, gen. n. A Hind wing of Zophotermes ashoki Engel & Singh, sp. n. (Tad-42) B Forewing of Zophotermes? sp. (Tad-95) C Hind wing of Zophotermes? sp. (Tad-278). Scale bar applies to all figures.
Figure 3 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 3 - Details of Parastylotermes krishnai Engel & Grimaldi, sp. n., holotype (Tad-277). A Forewing venation B Clypeus (from Tad-96) C Pretarsus, tarsus, and extreme apex of tibia D Detail of spur.
Figure 2 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 2 - Photomicrographs of dealate male and female of Prostylotermes kamboja Engel & Grimaldi, gen. et sp. n. (Stylotermitidae: Tad-321C). A Dorsal view of female B Ventral view of female C Ventral view of male. Not to the same scale.
Figure 4 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 4 - Detail of Prostylotermes kamboja Engel & Grimaldi, gen. et sp. n. (Tad-321C). A Head in lateral aspect B Tip of lacinia C Dorsal view of wing scales (female specimen) D Meso-pretarsus, mesotarsus, and extreme apex of mesotibia (female specimen) E Apex of female abdomen, ventral view, with detail of eggs preserved at abdominal apex F Apex of male abdomen, ventral view. Scale bars are identical and apply to all figures except the detail enlargements of B and D.
Figure 7 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 7 - Details of Nanotermes isaacae Engel & Grimaldi, gen. et sp. n. (Tad-262). A Head (as preserved, showing preservational distortion), pronotum, and base of right forewing B Protarsus, pro-pretarsus, and extreme apex of protibia C Metatarsus, meta-pretarsus, and extreme apex of metatibia D Forewing (reconstructed from both wings). Detail enlargements in B and C not to same scale.
Figure 1 from: Engel M, Grimaldi D, Nascimbene P, Singh H (2011) The termites of Early Eocene Cambay amber, with the earliest record of the Termitidae (Isoptera). ZooKeys 148: 105-123. https://doi.org/10.3897/zookeys.148.1797
Figure 1 - Photomicrographs of Cambay amber (Early Eocene) termites. A Nanotermes isaacae Engel & Grimaldi, gen. et sp. n., holotype (Termitidae: Tad-262) B Parastylotermes krishnai Engel & Grimaldi, sp. n., holotype (Stylotermitidae: Tad-277) C Zophotermes ashoki Engel & Singh, sp. n., holotype (Rhinotermitidae: Tad–42). Not to the same scale.
Figure 9 from: Williamson TE, Brusatte SL, Wilson GP (2014) The origin and early evolution of metatherian mammals: the Cretaceous record. ZooKeys 465: 1-76. https://doi.org/10.3897/zookeys.465.8178
Figure 9 - Right petrosal Type A (Protolambda) after Wible (1990) showing reconstruction of vasculature. Abbreviations: ac aqueductus cochleae; adm arteria diploetica magna; cev capsuloparietal emissary vein; cp crista parotica; ctpp caudal tympanic process of petrosal; er epitympanic recess; fc fenestra cochleae; fi fossa incudis; fs facial sulcus; fv fenestra vestibuli; hF, hiatus Fallopii; If, lateral flange of petrosal; lhv lateral head vein; It, lateral trough of petrosal; me mastoid exposure; mp mastoid process; pc prootic canal; pcv vein ofprootic canal; pff primary facial foramen; pp paroccipital process; pr promontorium; ri ramus inferior of stapedial artery; rs ramus superior of stapedial artery; rtpp rostral tympanic process of petrosal; sa stapedial artery; sev sphenoparietal emissary vein; sf stapedius fossa; sff secondary facial foramen; sips sulcus for inferior petrosal sinus; spd sulcus for perilymphatic duct; vdm vena diploetica magna.
Figure 7 from: Williamson TE, Brusatte SL, Wilson GP (2014) The origin and early evolution of metatherian mammals: the Cretaceous record. ZooKeys 465: 1-76. https://doi.org/10.3897/zookeys.465.8178
Figure 7 - Cast of holotype of Asiatherium reshetovi. A postcranial skeleton B close-up of right forelimb C ventral view of skull. Scale bars equal 1 cm.
Figure 13 from: Williamson TE, Brusatte SL, Wilson GP (2014) The origin and early evolution of metatherian mammals: the Cretaceous record. ZooKeys 465: 1-76. https://doi.org/10.3897/zookeys.465.8178
Figure 13 - Tarsus of the Cretaceous stem therian Eomaia and Cretaceous metatherians. A–F isolated calcaneum (A–C) (cf. Sulestes?) from the Bissetky Locale, Uzbekistan in dorsal (A), ventral (B), and distal (C) views after Szalay and Sargis (2006). D–F isolated astragalus (cf. Sulestes?) from the Bissetky Locale, Uzbekistan in dorsal (D), ventral (E), and distal (F) views after Szalay and Sargis (2006). G articulated partial pes of Sinodelphys in ventral view H–I calcaneum and astragalus, respectively, of Eomaia in ventral view J–K calcaneum and astragalus of Sinodelphys, respectively, in ventral view L–M calcaneum and astragalus of Protolambda, respectively, in ventral view G–M are after Luo et al. (2003). Scale bars equal 1 mm.
Figure 14 from: Williamson TE, Brusatte SL, Wilson GP (2014) The origin and early evolution of metatherian mammals: the Cretaceous record. ZooKeys 465: 1-76. https://doi.org/10.3897/zookeys.465.8178
Figure 14 - World map showing Late Cretaceous metatherian locales. Numbering of locales corresponds to the Cretaceous metatherian localities listed in Table 3.
Figure 12 from: Williamson TE, Brusatte SL, Wilson GP (2014) The origin and early evolution of metatherian mammals: the Cretaceous record. ZooKeys 465: 1-76. https://doi.org/10.3897/zookeys.465.8178
Figure 12 - Partial femora of unidentified metatheria (cf. Sulestes?) from the Bissetky Locale, Uzbekistan after Chester et al. (2012). A–C right distal femur in anterior (A), posterior (B), and distal (C) views D–F right proximal femur of a possible unidentified metatherian in proximal (D), anterior (E), and posterior (F) views.
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