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Fig. 1 in Reproductive strategy of two deep-sea scalpellid barnacles (Crustacea: Cirripedia: Thoracica) associated with decapods and pycnogonids and the first description of a penis in scalpellid dwarf males
Fig. 1 Verum brachiumcancri, photo and drawing of adult female, with arrow pointing to site of male receptacle (re) on inside of scutal plate (sc). ca Carina, cl carino-latus, la latus, ml median latus, pe peduncle, rl rostro-latus, ro rostrum, te tergum
Fig. 3 in Direct Growth Measurements of Two Deep-sea Scalpellid Barnacles, Scalpellum stearnsii and Graviscalpellum pedunculatum
Fig. 3. in situ shell increment after 350-d deployment of Scalpellum stearnsii (narrow strip below the light calceinstained band). Pictures under fluorescent and normal light were overlaid.
Fig. 2 in Direct Growth Measurements of Two Deep-sea Scalpellid Barnacles, Scalpellum stearnsii and Graviscalpellum pedunculatum
Fig. 2. Changes in capitulum lengths of Scalpellum stearnsii (solid lines) and Graviscalpellum pedunculatum (broken lines between 35 - 55 mm) over 8-month rearing at Nara (a) and 2-year rearing at Okinawa (b). Different colors indicate different individuals.
Fig. 1 in Direct Growth Measurements of Two Deep-sea Scalpellid Barnacles, Scalpellum stearnsii and Graviscalpellum pedunculatum
Fig. 1. Scalpellid barnacles Scalpellum stearnsii (a) and Graviscalpellum pedunculatum (b). The S. stearnsii individual showed maximum absolute increments at Okinawa, with small shell plates. Capitulum length measured is shown as a black line.
Figure 3 in Detailed integrative taxonomic analysis reveals large-scale species misidentification of barnacles based on DNA barcoding data
Figure 3. Neighbour-joining tree for the three investigated barcode index numbers. Ŋe coloured sequences in each clade indicate our newly generated sequences of specimens with unequivocal morphological identification.
Figure 2 in Detailed integrative taxonomic analysis reveals large-scale species misidentification of barnacles based on DNA barcoding data
Figure 2. Morphology of unidentified Balanus sp. individuals of clade A (BOLD:AAG0069) (A), Balanus balanus (B), Balanus crenatus
Figure 1 in Detailed integrative taxonomic analysis reveals large-scale species misidentification of barnacles based on DNA barcoding data
Figure 1. Bubble plot of the correspondence between species assignments and the barcode index number (BIN; genetic clade). Ŋe size of the bubbles corresponds to the number of sequences contained in each combination of BIN and species assignment. Vertical lines highlight BINs that contain more than one species assignment, and horizontal lines highlight species assignments that are present in more than one BIN. Grey bubbles indicate a one-to-one match between BIN and species assignment. Coloured bubbles represent the three BINs that were investigated further by integrative taxonomic analysis.
Fig. 5 in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 5. (A-F) Amphibalanus? sp. collected from the Liuchungchi Formation, Niupu, Chiayi, Western Central Taiwan, (Plio-Pleistocene age). Note that the shell compartment are tubiferous and possess interlaminate figures.
Fig. 2 in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 2. Trace fossils from the Liuchungchi Formation,Chukou Niupu at Chaiyi City, Taiwan. (A) Asterosoma isp. (#2267); (B) Bifasiculus? isp. (#2265); (C) Asterosoma isp. (#2263); (D) Asterosoma isp. (#2264). These ichnofossils were likely formed by annelids, and give evidence for low-energy sea bottom conditions. Specimens held in the Chia-Yi Municipal Museum, Chaiyi City. (The diameter of the coin is 26 mm).
Fig. 4 in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 4. (A-F) Striatobalanus sp. collected from the Liuchungchi Formation, Niupu, Chiayi, Western Central Taiwan, during the Plio- Pleistocene. Note that the shell walls, radii and bases are solid (i.e. non-tubiferous).
Fig. 1 in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 1. Location of the Coronula bifida Lagerstätte site near Niupu, Zhongpu Township, Chiayi, Western Central Taiwan. Insert showing the site on the Bazhang riverbed near the Chukou Niupu in Chaiyi City.
Fig. 3. Coronula bifida Bronn, 1831 in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 3. Coronula bifida Bronn, 1831 from Niupu, Chiayi, Western Central Taiwan, Liuchungchi Formation (Plio-Pleistocene). Specimens (#0860-0869) held by the Chia-Yi Municipal Museum, Chaiyi City, Taiwan.
Fig. 6. A in Accumulations of Fossils of the Whale Barnacle Coronula bifida Bronn, 1831 (Thoracica: Coronulidae) Provides Evidence of a Late Pliocene Cetacean Migration Route through the Straits of Taiwan
Fig. 6. A large fossil baleen whale mandible, currently attributed to the humpback whale, Megaptera novaeangliae Gray, 1846. Recovered from the Liuchungchi Formation, Zhongpu Township, Chiayi, Western Central Taiwan. On display in the Chia-Yi Municipal Museum, Chaiyi City, Taiwan.
Fig. 9 in How whale and dolphin barnacles attach to their hosts and the paradox of remarkably versatile attachment structures in cypris larvae
Fig. 9 Comparative cyprid morphology between Xenobalanus globicipitis and four of the species used in this study. a, b Xenobalanus globicipitis. c, d Amphibalanus amphitrite. e, f Trevathana jensi. g, h Lepas pectinata. i, j Scalpellum scalpellum. Compared with C. paguri (Fig. 8). Terminology is explained in supplementary table 1. Roman
Figure 2 in Species assemblage and distribution of turtle barnacles (Cirripedia: Coronuloidea) on foraging green sea turtles (Chelonia mydas) in the Persian Gulf
Figure 2. Distribution of Chelonibia testudinaria and Platylepas hexastylos on the carapace (a) and plastron (b) of foraging green sea turtles (Chelonia mydas) in southern Qeshm Island (eastern Persian Gulf). letters on the scutes of the top-left picture show: c) central scutes; l) lateral scutes; n) nuchal scute; s) supracaudal scutes; m) marginal scutes (all unmarked scutes between nuchal and supracaudals are marginal scutes). Letters on the scutes of the below-right picture show: i) intergular scute; g) gular scute; h) humeral scute; p) pectoral scute; ab) abdominal scute; f) femoral scute; a) anal scute; in) inframarginal scutes.
Figure 1 in Species assemblage and distribution of turtle barnacles (Cirripedia: Coronuloidea) on foraging green sea turtles (Chelonia mydas) in the Persian Gulf
Figure 1. Sampling site of green sea turtles (Chelonia mydas) on the southern coast of Qeshm Island, the Persian Gulf.
FIGURE 34 in An illustrated catalogue of the scalpellid barnacles (Crustacea: Cirripedia: Scalpellidae) collected during the HMS "Challenger" expedition and deposited in the Natural History Museum, London
FIGURE 34. Trianguloscalpellum rubrum (Hoek, 1883). "Challenger" Stn 204: holotype. Illustration from Hoek (1883), right lateral view. Scale bar 2 mm.
Figure 14 in Diversity and biogeography of the little known deep-sea barnacles of the genus Waikalasma Buckeridge, 1983 (Balanomorpha: Chionelasmatoidea) in the Southwest Pacific, with description of a new species
Figure 14. Waikalasma dianajonesae sp. nov. (a) Mandible. (b) Outer margin of mandible. (c) Lower margin. (d) Inferior angle. (e) Mandibular palp. (f) Serrulate setae on palp. (g) Labrum. (h) Cutting edge of labrum, showing small teeth. Scale bars in μm.
Figure 15 in Diversity and biogeography of the little known deep-sea barnacles of the genus Waikalasma Buckeridge, 1983 (Balanomorpha: Chionelasmatoidea) in the Southwest Pacific, with description of a new species
Figure 15. The best scoring maximum-likelihood (ML) tree based on concatenated COI and 12S data sets. Node labels are supporting values (%) estimated from the NJ, ML and MP methods, respectively. Scale bars indicate the number of expected substitutions per site.
Figure 10 in Diversity and biogeography of the little known deep-sea barnacles of the genus Waikalasma Buckeridge, 1983 (Balanomorpha: Chionelasmatoidea) in the Southwest Pacific, with description of a new species
Figure 10. Waikalasma dianajonesae sp. nov. (a) Cirrus I. (b) Magnified view of posterior ramus. (c) Serrulate setae on anterior ramus. (d) Magnified view of serrulate setae. (e) Cirrus II. (f) Intermediate segment of posterior cirrus. (g) Intermediate segments of anterior ramus. (h) Serrulate setae on basipod. Scale bars in μm.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.