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FIGURE 4 in The larval, juvenile, and adult stages of the Caribbean goby, Coryphopterus kuna (Teleostei: Gobiidae): a reef fish with a pelagic larval duration longer than the post-settlement lifespan

FIGURE 4. Sagittal otolith of a 15.3 mm SL Coryphopterus kuna: the dark rod-shaped primordium is at far left, surrounded by the prehatching core (white oval), then followed by wide larval increments, sharply narrowing before the settlement transition (white arrow); the edge of the otolith is at far right; length of arrow=30 microns.

FIGURE 2 in The larval, juvenile, and adult stages of the Caribbean goby, Coryphopterus kuna (Teleostei: Gobiidae): a reef fish with a pelagic larval duration longer than the post-settlement lifespan

FIGURE 2. Adult Coryphopterus kuna from Utila, Honduras: 10.9 mm SL female (A and B); 13.3 mm SL male (C); 15.2 mm SL male (D); pelvic fin and probe under the frenum on 15.2 mm SL male (E).

Figure 3 in The larval, juvenile, and adult stages of the Caribbean goby, Coryphopterus kuna (Teleostei: Gobiidae): a reef fish with a pelagic larval duration longer than the post-settlement lifespan

Figure 3. Larvae and juvenile of Coryphopterus kuna: 7.1 mm SL (A), 8.0 mm SL (B), and 7.0 mm SL (C, lateral and dorsal view) larvae from Xcalak; 8.1 mm SL settled juvenile from Utila, Honduras (D, lateral and dorsal view). Head melanophores labeled following abbreviations in Table 1. (A) and (B) courtesy of José A. Cohúo.

FIGURE 1 in The larval, juvenile, and adult stages of the Caribbean goby, Coryphopterus kuna (Teleostei: Gobiidae): a reef fish with a pelagic larval duration longer than the post-settlement lifespan

FIGURE 1. The reported range of Kuna Gobies within the Caribbean (map by Robert Myers, Coral Graphics, reprinted with permission) (A); Live photographs from Utila, Gulf of Honduras (B); Guadeloupe in the Lesser Antilles (C); and San Andres, Colombia, an offshore island in the Western Caribbean (D); photos by Keri Wilk.

FIGURE 3 in Coryphopterus kuna, a new goby (Perciformes: Gobiidae: Gobiinae) from the western Caribbean, with the identification of the late larval stage and an estimate of the pelagic larval duration

FIGURE 3. Sagittal otolith of transitional larva of Coryphopterus kuna, lateral view, photographed at 400x. The array of daily otolith increments extends along the longest radius of the sagitta from the center of the otolith (at left) to the edge of the otolith (at right). The primordium is the horizontal black oblong at the left edge of the figure and is about 7 microns long, the core (pre-hatching) is the area without clear increments about 20 microns out from the center.

FIGURE 1D, E in Coryphopterus kuna, a new goby (Perciformes: Gobiidae: Gobiinae) from the western Caribbean, with the identification of the late larval stage and an estimate of the pelagic larval duration

FIGURE 1D, E. Holotype of Coryphopterus kuna, pelvic fin frenum absent (D); prominent melanophores over eyeball (E).

FIGURE 1A–C in Coryphopterus kuna, a new goby (Perciformes: Gobiidae: Gobiinae) from the western Caribbean, with the identification of the late larval stage and an estimate of the pelagic larval duration

FIGURE 1A–C. Holotype of Coryphopterus kuna, 17.1 mm SL male (SIO-07-5)(A); head and fin markings (B); pelvic fins united along full-length (C).

Figure 4 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 4 Analyzed transects of otolith Sr:Ca ratios from the core to the edge of sagittal otoliths of Rhinogobius formosanus collected in the Malian Creek of northern Taiwan. The arrows represent the formation days of the otolith check mark counted from the core. a-e represent their catalog numbers.

Figure 3 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 3 Minimum spanning network built from 20 COI sequences of Rhinogobius formosanus with six haplotypes. Colors represent correspondent sampling sites; pie chart sizes are proportional to the number of individuals; short bars represent haplotypes not collected in this study. FR, Feitsui Reservoir, representing a landlocked population; MLC, Malian Creek, representing an amphidromous population.

Figure 2 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 2 Sampling localities of Rhinogobius formosanus in Taiwan. Location codes are given in Table 1. FR, Feitsui Reservoir (GPS: 24°55'46.8"N, 121°41'29.6"E), representing a landlocked population; MLC, Malian Creek (GPS: 25°10'17.2"N, 121°40'47.7"E), representing an amphidromous population.

Figure 6 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 6 Sr:Ca ratios along transects from the core to the edge of sagittal otolith of Rhinogobius formosanus collected in the Feitsui Reservoir. a-h represent their catalog numbers.

Figure 5 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 5 Otolith microstructure of an amphidromous goby (DOS02416-7, panel a and c) and a landlocked goby (DOS03534-19, panel b and d). Panel c and d illustrate the clear growth increments during the pelagic larval duration of the goby. The white arrows in panel a and b indicate the transect of otolith Sr:Ca ratio analysis. The black arrows indicate the otolith check mark where otolith Sr:Ca ratios drop from marine to freshwater signatures (panel a) and structural transition from clear concentric ring to ambiguous rings (panel b), respectively. Scale bars: 500 μm for panel a, b; 100 μm for panel c, d."

FIGURE 2 in Coryphopterus kuna, a new goby (Perciformes: Gobiidae: Gobiinae) from the western Caribbean, with the identification of the late larval stage and an estimate of the pelagic larval duration

FIGURE 2. Transitional larva of Coryphopterus kuna, 7.3 mm SL (SIO-07-55).

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Data from: Stretched to the limit; can a short pelagic larval duration connect adult populations of an Indo-Pacific diadromous fish (Kuhlia rupestris)?

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Figure 1 from: Liao T-Y, Huang W-C, Iizuka Y, Chou M-T, Shiao J-C (2020) Facultative amphidromy and pelagic larval duration plasticity of Rhinogobius formosanus (Teleostei, Gobioidei). ZooKeys 951: 91-107. https://doi.org/10.3897/zookeys.951.50429

Figure 1 Rhinogobius formosanus. Male; approximately 7 cm TL, specimen not preserved.