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274 results for “East China Sea”
Fig. 1. A in Crabs (Crustacea, Decapoda) from the Seas of East and Southeast Asia Collected by the RV Hakuhō Maru (KH-72-1 Cruise) 4. South China Sea
Fig. 1. A: Mclaydromia colini Guinot and Tavares, 8 (NSMT-Cr 30898; CB 13.1×CL 15.0 mm including pseudorostral teeth) from sta. 45. B: Mursia australiensis Campbell, juv. (NSMT-Cr 30905; CB 8.2 mm excluding lateral tubercles, CL 7.4 mm) from sta. 52. C: Podophthalmus nacreus Alcock, 8 (NSMT-Cr 30925; CB 11.0×CL 7.1 mm) from sta. 45. D: Lissocarcinus arkati Kemp, 8 (NSMT-Cr 30921; CB 9.8×CL 8.7 mm) from sta. 45. E–F: Parilia pattersoni Ng, Devi and Kumar, juv. (NSMT-Cr 30906; CB 5.6×CL 6.6 mm including posterior median tubercle) from sta. 42.
Fig. 5 in Crabs (Crustacea, Decapoda) from the Seas of East and Southeast Asia Collected by the RV Hakuhō Maru (KH-72-1 Cruise) 4. South China Sea
Fig. 5. Samadinia hakuhoae sp. nov., holotype, Ə (NSMT-Cr 30915; CB 10.7 mm excluding branchial spines, PCL 16.3 mm) from sta. 54. Dorsal (A), anterior (B), posterior (C) and lateral (D) views.
Fig. 3. A in Crabs (Crustacea, Decapoda) from the Seas of East and Southeast Asia Collected by the RV Hakuhō Maru (KH-72-1 Cruise) 4. South China Sea
Fig. 3. A: Dorhynchus rostratus (Sakai), 8 (NSMT-Cr 30908; CB 6.6×PCL 8.5 mm) from sta. 54. B: Oncinopus angustifrons Takeda and Miyake, Ə (NSMT-Cr 30909; CB 3.4×PCL 4.3 mm) from sta. 48. C–E: Oxypleurodon sphaenocarcinoides (Rathbun), ovig.8 (NSMT-Cr 30913; CB 7.8×PCL 12.7 mm) (C–D) from sta. 54; 8(NSMT-Cr 30914; 5.0×8.3 mm) (E) from sta. 54.
Fig. 9. A–B in Crabs (Crustacea, Decapoda) from the Seas of East and Southeast Asia Collected by the RV Hakuhō Maru (KH-72-1 Cruise) 4. South China Sea
Fig. 9. A–B: Lupocycloporus innominatus (Rathbun), Ə (NSMT-Cr 30923; CB 15.1 mm including lateral teeth, CL 10.5 mm) from sta. 45. C–D: Charybdis (Archias) vadorum Alcock, Ə (NSMT-Cr 30920; CB 10.7×CL 7.6 mm) from sta. 50. E–F: Thalamita sexlobata Miers, ovig.8 (NSMT-Cr 30926; CB 7.0×CL 6.0 mm) from sta. 45.
Fig. 8 in Crabs (Crustacea, Decapoda) from the Seas of East and Southeast Asia Collected by the RV Hakuhō Maru (KH-72-1 Cruise) 4. South China Sea
Fig. 8. Charybdis (Archias) hongkongensis Shen, Ə (NSMT-Cr 30919; CB 36.7×CL 25.7 mm) from sta. 42. Dorsal view (A), right chela in lower view (B), left chela in outer view (C), pleon (D), and G1s in situ (E).
Fig. 1 in Biodiversity variability of macrobenthic in the Yellow Sea and East China Sea between 2001 and 2011
Fig. 1. Sampling stations in the Yellow Sea and East China Sea in March 2001, copied from the "Field work plan notice of 2001 spring cruise of the National Basic Research Program of China (19990437). YS, the subarea Yellow Sea. ECS, the subarea East China Sea. CJE, the subarea Changjiang River Estuary. Stations marked with red colour, the matching stations.
Figs 6–7 in Biodiversity variability of macrobenthic in the Yellow Sea and East China Sea between 2001 and 2011
Figs 6–7. Distribution of secondary productivity of macrobenthos. 6. In April 2011. 7. In August 2011.
Figs 3–4 in Biodiversity variability of macrobenthic in the Yellow Sea and East China Sea between 2001 and 2011
Figs 3–4. Horizontal distributions of macrobenthic abundance (ind/m2). 3. In March 2001. 4. In April 2011.
Fig. 2 in Biodiversity variability of macrobenthic in the Yellow Sea and East China Sea between 2001 and 2011
Fig. 2. Sampling stations in the Yellow Sea and East China Sea in April and August 2011, copied from the "Field work plan notice of 2011 spring cruise of the National Basic Research Program of China (2011CB4036). YS, the subarea Yellow Sea. ECS, the subarea East China Sea. CJE, the subarea Changjiang River Estuary. Stations marked with red colour, the matching stations.
FIGURE 1 in Chauligenion camelopardalis, a New Genus and Species of Deepwater Snake Eel (Anguilliformes: Ophichthidae) from the East China Sea
FIGURE 1.Holotype of Chauligenion camelopardalis sp. nov., NSMT-P 125489, female, 407 mm TL, photographed soon after capture and before preservation. Arrows indicate origin of dorsal and anal fins.
FIGURE 4 in Chauligenion camelopardalis, a New Genus and Species of Deepwater Snake Eel (Anguilliformes: Ophichthidae) from the East China Sea
FIGURE 4. Radiograph of head of holotype of Chauligenion camelopardalis sp. nov., NSMT-P 125489, female, 407 mm TL.
FIGURE 3 in Chauligenion camelopardalis, a New Genus and Species of Deepwater Snake Eel (Anguilliformes: Ophichthidae) from the East China Sea
FIGURE 3. Gill arches (interior view, cut longitudinally along dorsal surface and spread laterally) of holotype of Chauligenion camelopardalis sp. nov., NSMT-P 125489, female, 407 mm TL. Bone is stained red and cartilage is blue.
Supporting Information for Responses of Biogenic Dimethylated Sulfur Compounds to the Environmental Changes in the East China Sea
<p>This file contained the datasets of Figure 1, Figure 2, Figure 3, Figure S3, and Figure S4 discussed in the publication “Responses of Biogenic Dimethylated Sulfur Compounds to the Environmental Changes in the East China Sea”. There are:</p> <ol> <li>The pH, the concentrations of nitrate and phosphate in the spring 2017 experiment and summer 2018 experiment. The concentrations of organic nitrogen in the spring 2017 experiment.</li> <li>The Chl-a concentrations and the relative abundance of diatom and dinoflagellate in the spring 2017 experiment and summer 2018 experiment.</li> <li>The concentrations of DMS, DMSPd, DMSPp and DMSO in the spring 2017 experiment and summer 2018 experiment.</li> <li>The DMSPd loss rate and DMS production rate in the spring 2017 experiment and summer 2018 experiment.</li> </ol> <p>Ma, Q. Y., Zhang, H. H., Yang, G. P. (2021). Responses of Biogenic Dimethylated Sulfur Compounds to the Environmental Changes in the East China Sea. Submitted to Geophysical Research Letters.</p>
Reoxygenation in the East China Sea
<p>Hypoxia and upwelling co-occurred in the summer, and the well-mixed water often reaches the subsurface in the East China Sea (ECS), especially off the Changjiang River estuary. The impact of upwelling on the hypoxia and, therefore, on the ECS ecosystem is not well evaluated. This study demonstrates several positive and negative effects of upwelling on hypoxia and its impact on the ecosystem. This dataset contains data collected from four cruises in the summer of 2003 (June 18–26 and August 13–23) and 2014 (July 16–29 and August 20–31) on the R/V Ocean Researcher I and V in the East China Sea described in the paper: "Chung-Chi Chen, Dong S. Ko, Gwo-Ching Gong, Chun-Chi Lien, Wen-Chen Chou, Hung-Jen Lee, Fuh-Kwo Shiah, Yu-Sin Wita Huang (2022). Reoxygenation of the hypoxia in the East China Sea: A ventilation opening for marine life. <i>Frontiers in Marine Science</i> ". The presented variables include: temperature, salinity, dissolved oxygen, dissolved inorganic nutrients (nitrate and phosphate), and Chl <i>a </i>in this study.</p> <p>Main results of this study included nine figures and two tables as described in the paper, and please refer it for further details.</p>
Latitudinal cline in the foraging dichotomy of loggerhead sea turtles reveals the importance of East China Sea for priority conservation
<p><strong>Aim:</strong> Quantifying the importance of habitat areas for conservation of highly migratory marine species with complex life histories can be challenging. For example, loggerhead turtles (Caretta caretta) nesting in Japan forage both oceanically and neritically after their reproductive period. Here, we aimed to quantify the proportions of turtles using these two contrasting habitats (foraging dichotomy) to suggest priority conservation areas.</p> <p><strong>Methods:</strong> We examined the occurrence of foraging dichotomy at three nesting sites (Ishigaki, Okinoerabu Islands, and Ichinomiya) based on stable isotope analysis of the egg yolks for 82 turtles and satellite tracking of post-nesting migration for 12 turtles. Moreover, we used the data of three other sites from previous studies (Yakushima Island, Minabe, and Omaezaki).</p> <p><strong>Results:</strong> Two neritic foraging grounds (East China Sea and the coastal area of the Japanese archipelago), and an oceanic ground (North Pacific Ocean) were identified. We found a latitudinal cline with respect to the occurrence of foraging dichotomy; >84% of the females nesting at southern sites (Ishigaki and Okinoerabu Islands), 73% at middle sites (Yakushima Island and Minabe), and <46% at northern sites (Omaezaki and Ichinomiya) were neritic foragers; the proportion of oceanic foragers increased at northern sites. Based on the annual number of nests in the entire nesting region of Japan, satellite tracking, and the latitudinal cline of foraging dichotomy, we estimated that 70% and 9% of annual nesting females in Japan utilise the neritic foraging habitat in the East China Sea and the coastal area of the Japanese archipelago, respectively and that and 22% utilise the oceanic habitat of the North Pacific Ocean.</p> <p><strong>Main conclusions:</strong> The East China Sea represents a critical foraging habitat for the North Pacific populations of endangered loggerhead sea turtles. Our findings emphasise the need for international management to ensure their protection.</p>
The oxygen isotope of phosphate in the East China Sea in 2020
<p>For the analysis of the main sources of phosphate in the ESC during summer, we choose the area between 120.93 ˚ E-125.9 ˚ E and 26.08˚ N-32.35 ˚ N as research sites . The samples were all from the voyage of the research ship (Xiangyanghong 18). Surface seawater was collected at 49 stations for δ<sup>18</sup>O<sub>p</sub> analysis by a conductivity-temperature-depth profiler. Then we utilized δ<sup>18</sup>O<sub>p</sub> to trace the source of phosphate in the ESC. </p> <p>The δ<sup>18</sup>O<sub>p</sub> values in seawater are affected by water masses with different phosphate concentrations.We need the two-component mixing model for the analysis of water masses that control phosphate.In this research, atmospheric deposition and adjacent sea transportation were used as terrestrial and seawater end-members respectively to construct the δ<sup>18</sup>O<sub>p</sub> end-member mixing model.</p> <p>In order to quantify the source of phosphate in the sea, a Bayesian isotope mixing model run in the R software package (Stable Isotope Analysis in R, SIAR) was selected for analysis.</p>
Bottom water mediated microplastics distribution in water and sediment in the Yangtze River Estuary and East China Sea
<p>This database included the original data of water parameters, microplastics abundance, microplastics size, shape, color and shape. </p>
Figure 1 in A new species of Zenopsis (Zeiformes: Zeidae) from the South China Sea, East China Sea and off Western Australia
Figure 1. Zenopsis stabilispinosa sp. nov. Holotype, FAKU 64803 (307.2 mm SL).
Data from: Nutrient sources, phytoplankton blooms, and hypoxia along the Chinese coast in the East China Sea: Insight from summer 2014
<p>This dataset contains data collected onboard the <em>R/V Ocean Researcher I</em> during the summer of 2014 (August 20–31) East China Sea described in the paper: "C.-C. Chen, W.-C. Chou, and C.-C. Hung (2024). Nutrient sources, phytoplankton blooms, and hypoxia along the Chinese coast in the East China Sea: Insight from summer 2014, Marine Pollution Bulletin (accepted on July 4 2024)".</p>
Fig. 5 in Biodiversity variability of macrobenthic in the Yellow Sea and East China Sea between 2001 and 2011
Fig. 5. Horizontal distributions of macrobenthic abundance in August 2011 (ind/m2).
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