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683 results for “Sea of Japan”
FIGURE 4. Parapleisticantha ludivinae n in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 4. Parapleisticantha ludivinae n. sp. Male holotype (22.9 × 19.2 mm) (NMCR), Balicasag Is., Philippines. A, habitus; B, dorsal view of carapace; C, frontal view showing epistome, antennules and antennae.
FIGURE 2. Parapleisticantha japonica Yokoya, 1933. Lectotype male 22.4 in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 2. Parapleisticantha japonica Yokoya, 1933. Lectotype male 22.4 × 16.8 mm (KMNH), Goto Is., Japan. A, frontal view showing rostrum and eyes; B, ventral view showing anterior thoracic sternum and abdomen; C, left third maxilliped; D, lateral view of carapace; E, outer view of left chela.
FIGURE 6. A–E in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 6. A–E, Parapleisticantha japonica Yokoya, 1933, lectotype male (22.4 × 16.8 mm) (KMNH), Goto Is., Japan; F–I, Parapleisticantha ludivinae n. sp., male holotype (22.9 × 19.2 mm) (NMCR), Balicasag Is., Philippines. A, F, ventral view of left G1; B, G, dorsal view of left G1; C, H, distal part of left G1, ventral view; D, I, tip of left G1, ventral view; E, left G2. Scales: A, B, F, G = 1.0 mm; C, E, H = 0.5 mm; D, I = 0.05 mm.
FIGURE 1. Parapleisticantha japonica Yokoya, 1933 in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 1. Parapleisticantha japonica Yokoya, 1933. Lectotype male (22.4 × 16.8 mm) (KMNH), Goto Is., Japan. A, habitus; B, dorsal view of carapace; C, ventral view of cephalothorax showing epistome, antennules and antennae.
FIGURE 3. Parapleisticantha japonica Yokoya, 1933 in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 3. Parapleisticantha japonica Yokoya, 1933. Paralectotype ovigerous female (16.6 x 13.1 mm) (KMNH), Goto Is., Japan. A, habitus; B, dorsal view of carapace; C, ventral view showing anterior thoracic sternum and abdomen.
FIGURE 5. Parapleisticantha ludivinae n in Parapleisticantha Yokoya, 1933, a valid genus of deep-sea inachid spider crab from Japan and the Philippines (Crustacea: Decapoda: Brachyura: Majoidea), with the description of a new species
FIGURE 5. Parapleisticantha ludivinae n. sp. Male holotype (22.9 × 19.2 mm) (NMCR), Balicasag Is., Philippines. A, frontal view showing rostrum and eyes; B, ventral view showing anterior thoracic sternum and abdomen; C, left lateral view of carapace; D, outer view of right chela.
FIGURE 7 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 7. Halichoanolaimus brandtae sp. n. SEM. A. Head, dorso-lateral view. B. Tail region, lateral view. C. Lateral row of cuticular pores (p). D. Cloacal opening (c), supplements (s). E. Cloacal region with supplements (s). Scale bars: A, C–10 µm, B, D–20 µm, E–2 µm.
FIGURE 6 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 6. Halichoanolaimus brandtae sp. n. DIC. A. Head with denticles and mandibles. B. Head with amphid. C. Spicule and gubernaculum. D. Swallowed spicule in the intestine of H. brandtae sp. n. Scale bars: 20 µm.
FIGURE 5 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 5. Halichoanolaimus brandtae sp. n. A. Holotype male. Total body. B. Allotype female. Total body. C. Head with amphid, denticles, and mandibles. D. Tail region with spicule, gubernaculum, and supplements. Scale bars: A, B–150 µm; C–25 µm; D–50 µm.
FIGURE 4 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 4. Siphonolaimus japonicus sp. n. SEM. A. Head, dorso-lateral view. B. Head, apical view. a–amphid, hs–cephalic setae, m–mouth opening, ols–outer labial sensilla, scs–subcephalic setae. Scale bars: 10 µm.
FIGURE 3 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 3. Siphonolaimis japonicus sp. n. DIC. A. Male head with siphon. Lateral view. B. Male head with amphid. Lateral view. C. Spicule and gubernaculum. D. Tail region. Scale bars: 20 µm.
FIGURE 1 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 1. Study area showing sampling stations. Circle represents site where new species were found.
FIGURE 2 in New deep-sea free-living marine nematodes from the Sea of Japan: the genera Siphonolaimus and Halichoanolaimus (Nematoda: Chromadorea) with keys to species identifications
FIGURE 2. Siphonolaimus japonicus sp. n. A. Holotype male. Total body. B: Allotype female. Total body. C: Holotype male. Anterior end with amphid, siphon, and pharynx. D: Holotype male. Tail with spicule, gubernaculum, and caudal glands. Scale bars: A, B–200 µm, C–25 µm, D–100 µm.
FIGURE 6. Phylogenetic tree for 15 in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 6. Phylogenetic tree for 15 species of Salmoneus and Jengalpheops rufus Anker & Dworschak, 2007 used as an outgroup taxon; obtained by ML analysis of 16S rRNA gene sequences using the TVM + G + I substitution model. The best tree with the highest log likelihood (-1870.53) is shown. Bootstrap supports of greater than 80% are indicated at nodes as percentage values. There was a total of 514 bp in the final dataset trimmed with GBlocks.
FIGURE 3. Salmoneus aduncus n in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 3. Salmoneus aduncus n. sp., holotype, non-ovigerous specimen (cl 6.3 mm), CBM-ZC 17107. A, left maxilliped 3, lateral view; B, same, coxa and antepenultimate article, ventral view; C, right minor cheliped (pereopod 1), lateral view; D, same, chela, extensor view; E, left pereopod 2, lateral view; F, left pereopod 3, lateral view; G, same, distal part of propodus and dactylus, lateral view; H, left pereopod 4, lateral view; I, same, distal part of propodus and dactylus, lateral view; J, left pereopod 5, lateral view; K, same, distal part of propodus and dactylus, lateral view.
FIGURE 2. Salmoneus aduncus n in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 2. Salmoneus aduncus n. sp. A–C, E–I, holotype, non-ovigerous specimen (cl 6.3 mm), CBM-ZC 17107; D, paratype, non-ovigerous specimen (cl 4.6 mm), CBM-ZC 7305. A, anterior part of carapace and cephalic appendages, left lateral view (antennular and antennal flagella partially omitted); B, same, dorsal view; C, telson, dorsal view (posterior part partially damaged); D, posterior margin of telson, dorsal view; E, left antennal peduncle and scaphocerite, ventral view (flagellum omitted); F, left pleopod 1, dorsal (anterior) view (marginal setae on exopod omitted); G, same, endopod, dorsal (anterior) view; H, endopod and appendices interna and masculina of left pleopod 2, mesial view (marginal setae on endopod omitted).
FIGURE 5. Salmoneus aduncus n in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 5. Salmoneus aduncus n. sp., holotype, non-ovigerous specimen (cl 6.3 mm), CBM-ZC 17107, habitus in lateral view, showing colouration in fresh condition.
FIGURE 1. Salmoneus aduncus n in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 1. Salmoneus aduncus n. sp., holotype, non-ovigerous specimen (cl 6.3 mm), CBM-ZC 17107, habitus in lateral view (antennular and antennal flagella partially omitted).
FIGURE 4. Salmoneus aduncus n in A new species of the alpheid shrimp genus Salmoneus Holthuis, 1955 (Decapoda: Caridea) from the Seto Inland Sea, Japan
FIGURE 4. Salmoneus aduncus n. sp., holotype, non-ovigerous specimen (cl 6.3 mm), CBM-ZC 17107. A, left major cheliped (pereopod 1), lateral view; B, same, ischium and merus, ventral view; C, same, carpus and chela, extensor view; D, same, flexor view.
Middle Holocene relative sea-level changes and vertical tectonic crustal movements on Shikoku Island near the Nankai Trough, Japan
<p>The Philippine Sea plate subducts beneath the Eurasia plate at the Nankai Trough, northwestern Pacific, causing crustal deformation, mega-thrust earthquakes, and tsunami events. Shikoku Island, 150 km northwest of the trough, experiences both coseismic and interseismic deformation. Coastal sediments potentially record vertical crustal movements as relative sea level (RSL) changes. We studied sedimentary facies and microfossil ostracodes in core SKM from southwestern Shikoku Island for evidence of middle Holocene tsunami events and deformation. The core sediments included nine event layers corresponding to storm or tsunami events. Using modern analog techniques, we estimated RSLs from the ostracode assemblages of core SKM and 13 other cores from Shikoku Island and the surrounding region. Then, we subtracted RSL changes due to glacio-hydro isostatic adjustment from the estimated RSLs to estimate vertical tectonic movement rates in these cores between 8.6 and 4.7 ka. The inferred RSL changes suggest that the Sukumo site has experienced both uplift and subsidence since 8.6 ka. Before 6.6 ka, rates of the tectonic crustal movement were higher than the modern-day rate, and its spatial distribution also differed. After 6.6 ka, the tectonic crustal movement showed a similar spatial pattern and occurred at rates close to the modern-day interseismic rate. The spatial pattern and rates of tectonic crustal movement could be caused by changes in rupture areas between Eurasia and the Philippine Sea plates beneath Shikoku Island and in stress conditions of the asthenosphere. Some of the vertical displacements can be explained by the movements of local active faults.</p>
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Allen Brain Atlas
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OpenNeuro
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