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FIGURE 4 in Morphological and molecular data reveal the cryptic diversity among populations of Aegla paulensis (Decapoda, Anomura, Aeglidae), with descriptions of four new species and comments on dispersal routes and conservation status
FIGURE 4. Schematic representation of the aeglid areola (inner, dotted) and cardiac area (outer, solid line) in dorsal view, showing the terminology and measurements used in the descriptions. "y", "x", anterior and posterior width of the areola, respectively; "h", areola length; "a", "b", anterior and posterior width of the cardiac area, respectively. DLL, TDL, dorsal longitudinal linea and transverse dorsal linea, respectively.
FIGURE 2 in Morphological and molecular data reveal the cryptic diversity among populations of Aegla paulensis (Decapoda, Anomura, Aeglidae), with descriptions of four new species and comments on dispersal routes and conservation status
FIGURE 2. Major cheliped of Aegla paulensis s. str. (male topotype MZUSP 34367) showing the terminology used in the descriptions.
FIGURES 18–23 in Gone with the wind: westward dispersal across the Indian Ocean and island speciation in Hemicordulia dragonflies (Odonata: Corduliidae)
FIGURES 18–23. Distribution of discussed genera. The courses of storms from May to November in the northern hemisphere and November to May in the southern hemisphere are indicated by arrows (after Times Books 1997). (18) Hemicordulia and Procordulia dragonflies, pale shading: main range in Australasia and Pacific; dark shading: H. africana n. sp.; crosses and pale shading: H. similis; square: H. virens; circle: H. atrovirens n. sp.; (19) Teinobasis damselflies, pale shading: main range in Australasia and Pacific; dark shading: T. alluaudi; (20) Collocalia swiftlets; (21) Copsychus magpie robins; (22) Hypsipetes bulbuls; (23) Pteropus flying foxes.
FIGURES 2–11. 2–6 in Gone with the wind: westward dispersal across the Indian Ocean and island speciation in Hemicordulia dragonflies (Odonata: Corduliidae)
FIGURES 2–11. 2–6, Male appendages of Hemicordulia species in dorsal view. (2) H. asiatica; (3) H. virens; (4) H. atrovirens n. sp.; (5) H. similis; (6) H. africana n. sp.; 7–11, Male appendages of Hemicordulia species in lateral view. (7) H. asiatica; (8) H. virens; (9) H. atrovirens n. sp.; (10) H. similis; (11) H. africana n. sp.
FIGURES 12–17. Vulvar scale and S9 in Gone with the wind: westward dispersal across the Indian Ocean and island speciation in Hemicordulia dragonflies (Odonata: Corduliidae)
FIGURES 12–17. Vulvar scale and S9 of Hemicordulia species in ventral view. (12) H. asiatica; (13) H. virens; (14) H. atrovirens n. sp.; (15) aberrant H. similis (cf. Fraser 1949); (16) typical H. similis; (17) H. africana n. sp.
FIGURES 24–25 in Gone with the wind: westward dispersal across the Indian Ocean and island speciation in Hemicordulia dragonflies (Odonata: Corduliidae)
FIGURES 24–25. Geographic (24) and altitudinal (25) distribution of H. africana n. sp. relative to large water bodies. Filled circles are known records (present paper), open circles forested localities near large waterbodies that have recently been intensively surveyed by V. Clausnitzer (pers. comm.), except Mbala by Pinhey (1984). Many sites in the region away from large water bodies have also been researched. A line connects each site to the altitude of the nearest large water body.
FIGURE 3. Dispersion curves for Araripe cearagryllids. A and B in The Orthoptera (Ensifera) from the Santana formation (Early Cretaceous, Northeast Brazil): A statistical and paleoecological approach, with description of new taxa
FIGURE 3. Dispersion curves for Araripe cearagryllids. A and B fore wing length and ovipositor, respectively for Euclydes ramosfernandesi Martins-Neto, 2007 (Stenopelmatoidea), a possible mimetic Orthoptera of cearagryllids.
FIGURE 8. Bothridia a in New species of Crotonia (Acari: Oribatida: Crotoniidae) from Lord Howe and Norfolk Islands: further evidence of long-distance dispersal events in the biogeography of a genus of Gondwanan relict oribatid mites
FIGURE 8. Bothridia a) Crotonia gorgonia sp. nov.; b) Crotonia norfolkensis sp. nov.; c) Crotonia utricularia sp. nov.
FIGURE 5 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 5. Atetrapachylasma dijonesae gen. et sp. nov. in situ on pillow basalt from 2080 m of depth Vance B Seamount, with nozzle of suction sampler of ROV Tiburon largely to their right. A, the remains of several walls broken away by the nozzle can be seen to the right of "1" leaving membranous bases exposed. B, the barnacles seen between "2" and "3" and to the right of "4" in A have been collected. N.B.: Inspection of MPEGs taken by ROV Tiburon during collection of the barnacles seen removed in these frames detected no loss of material in the process. Therefore, it can be said with confidence that the shell fragments at the base of the basalt below the barnacles (cf. Fig. 4) represent natural postmortem accumulations.
FIGURE 15 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 15. Atetrapachylasma dijonesae gen. et sp. nov., appendages: A, mandible; B, first maxillae; C, second maxilla; D, intermediate articles of cirrus VI; and E, crest of labrum flanked by left palp.
FIGURE 12 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 12. Atetrapachylasma dijonesae gen. et sp. nov., exploded four-plated wall arranged from loose plates, type lot: A, exterior of a rostrum; B and D, left and right carinolaterals; C, a carina; and E, the interior of a portion of a rostrum. Note the variably pronounced depression in the sheath of rostrum (E), which, together with the edges of the carinolateral alae, receives the rostral ends of the occludent ridges of the scuta (Figs 9A; 11C, D).
FIGURE 7 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 7. The holotype and paratype of Calantica moskalevi Zevina and Galkin, 1989: 134, Fig. 1) consisted of two juveniles (measurements below in mm).
FIGURE 11 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 11. Atetrapachylasma dijonesae gen. et sp. nov. holotype: A, exterior view of female with males; note largely exposed alae and the pair of males on each side of the tight fitting occludent ridges of the scuta. B, interior view of the same female, note the tight fit of the bearing surfaces of the alae on the adjacent plates, and the close fit of the sutures between plates, especially between the opercular plates and the interior of the orifice.
FIGURE 4 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 4. Numerous females of Atetrapachylasma dijonesae gen. et sp. nov. in situ on pillow basalt from 2080 m of depth on Vance B Seamount, with nozzle of suction sampler on ROV Tiburon to their right (distance between red laser dots 30 cm). The pristine white appearance of the dead shells accumulating at the base of the slope, as well as of the living individuals, suggests that there is little if any hydrothermal activity nearby to stain them (rather than the barnacle just being short lived, which they are). Thus, as might be expected, dissection revealed feeding appendages (Fig. 13) of the deep-sea rather than hydrothermal type. N.B.: Inspection of MPEGs taken by ROV Tiburon during collection of most of the barnacles seen in this frame (also, Fig. 5) detected no loss of material in the process. Therefore, it can be said with confidence that the shell fragments at the base of the basalt below the barnacles represent natural, postmortem accumulations.
FIGURE 2 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 2. Panorama in the caldera of Axial Seamount, at approximately 1434 m of depth. Several yellowish-brown clumps and a few scatters individuals of the stalked barnacle, Calantica moskalevi Zevina and Galkin, 1989, can be seen at roughly 9, 12 and 3 o'clock of the right red laser dot (distance between red laser dots 30 cm).
FIGURE 14 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 14. Atetrapachylasma dijonesae gen. et sp. nov., dwarf males: A, viewed obliquely (R-C axis running between 10:30 and 4:30 o'clock); B, another individual, viewed from the carinal end, leaning markedly to its right, toward the aperture of the female (see Fig. 9 for four males in situ). Note that the chitinous primary wall is made up of four plates, with the rostrum overlapping the carinolaterals. There is no indication of sutures in the rostrum or the carinolaterals of the male or the female.
FIGURE 3 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 3. Group of several adult hermaphrodites of Calantica moskalevi Zevina and Galkin, 1989 in situ in the caldera of Axial Seamount (Fig. 1). The upper barnacle has its cirral net deployed for passive feeding in gentle currents. The cuticle of the barnacles, stained yellow-brown to gold apparently by ferromanganese oxides from venting 200 meters of so away, has sloughed off the apexes of some of the capitular plates, exposing the underlying calcitic shell to corrosion. Dissection reveals feeding appendages (Fig. 8) of the deep-sea rather than hydrothermal type.
FIGURE 13 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 13. Atetrapachylasma dijonesae gen. et sp. nov., opercular plates of female: A and B, interior and exterior of terga, and C and D, interior and exterior of scuta. Both the terga and scuta are isosceles triangles, the bases of which are formed by their occludent margins. Note that the weakly developed articular ridges and furrows, as well as the lack of adductor and depressor muscle crests (apodemes), pits or scars, are remarkable. Comparably simple opercular plates are seen in no other balanomorph.
FIGURE 10 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 10. Calantica moskalevi Zevina and Galkin, 1989; appendages, first topotype: A, portion of crest of labrum with left palp attached; B, mandible; C, first maxillae; D, second maxilla; E, intermediate articles of cirrus VI; and F, penis still attached to the coxal portion of pedicle of the left sixth cirrus.
FIGURE 16 in Two Northeast Pacific deep-water barnacle populations (Cirripedia: Calanticidae and Pachylasmatidae) from seamounts of the Juan de Fuca Ridge; " insular " endemics stemming from Tethys, or by subsequent dispersal from the Western Pacific center of distribution?
FIGURE 16. Distributional map: Locality for the calanticid, Calantica moskalevi Zevina and Galkin, 1989, and the pachylasmatine, Atetrapachylasma dijonesae gen. et sp. nov., from approximately 1400 and 2000 m depths, respectively, in the NE Pacific (arrow; cf. Fig. 1), and general localities for their closest living relatives, Calantica spp (closed circles, from list of species in text) and Tetrapachylasma spp (closed triangles, after Jones 2000), from shallow to moderated depths in the I-WP. More generalized calanticids, Scillaelepas spp, occur at bathy-abyssal depths in all except high latitude oceans, whereas all pachylasmatines except Pachylasma giganteum Philippe (open triangles) and Atetrapachylasma dijonesae (arrow), occur in the I-WP at shallow to moderate depths. This suggests that calanticids as well as pachylasmatines once had Tethyan distributions, of which the NE Pacific species appear to be peripheral isolates or relicts, rather than the result of subsequent long-range dispersal.
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Allen Brain Atlas
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