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736 results for “East China”
Subspecies and Distribution. H.b.brachyuraLinnaeus,1758 — MalayPeninsula,PenangI(offWcoastofPeninsularMalaysia),Sumatra,andBorneo. H.b.hodgsoniGray,1847 — SofHimalayasinENepal,NIndia(Sikkim). H. b. subcristata Swinhoe, 1870 — S Bhutan, NE India, C & S China (including Hainan I), Bangladesh, Burma (= Myanmar), and mainland South-east Asia. in Hystricidae
Subspecies and Distribution. H.b.brachyuraLinnaeus,1758 — MalayPeninsula,PenangI(offWcoastofPeninsularMalaysia),Sumatra,andBorneo. H.b.hodgsoniGray,1847 — SofHimalayasinENepal,NIndia(Sikkim). H. b. subcristata Swinhoe, 1870 — S Bhutan, NE India, C & S China (including Hainan I), Bangladesh, Burma (= Myanmar), and mainland South-east Asia.
Distribution. Tropical to warm temperate waters from ¢.50° N to ¢.40° S in the Indian, Pacific, and Atlantic oceans, as well as many adjacent seas including the Gulf of California, Sea ofJapan, Bohai, Yellow, and East China seas, and the Mediterranean Sea. Vagrant to the Red Sea and Persian Gulf. in Delphinidae
Distribution. Tropical to warm temperate waters from ¢.50° N to ¢.40° S in the Indian, Pacific, and Atlantic oceans, as well as many adjacent seas including the Gulf of California, Sea ofJapan, Bohai, Yellow, and East China seas, and the Mediterranean Sea. Vagrant to the Red Sea and Persian Gulf.
Subspecies and Distribution. L. t. timidus Linnaeus, 1758 — Scandinavia S to 59° N, N Russia (S to 57° N to 58° N) to E of Ural Mts, Estonia, perhaps Poland, and Altai and Beita Mts in N Xinjiang (China); from Sweden extending in hybrid zones with the subspecies sylvaticus to S coast of Norway and W Latvia. L. t. abet Kuroda, 1938 — Kurile Is (Russia). L. t. ainu Barrett-Hamilton, 1900 — Hokkaido (Japan). L. t. begitschevi Koljuschev, 1936 — Taimyr Peninsula (Russia). L. t. gichiganus J. A. Allen, 1903 — C Yakutia, Kamchatka and Okhotsk Sea coast (Russia). L. t. hibernicus Bell, 1837 — Ireland. L. t. kolymensis Ognev, 1922 — NE Siberia (Russia). L. t. kozhevnikovi Ognev, 1929 — C Russia from 57° to 58°N, whereit intergrades with the nomonotypical timidus S to 53° N. The W boundary is unclear. L. t. lugubris Kastschenko, 1899 — Siberian Altai Mts (Russia). L. t. mordeni Goodwin, 1933 — Russian Far East (Ussuri Valley and lower and middle Amur River) and Heilongjiang (China). L. t. ori Kuroda, 1928 — Sakhalin (Russia). L. t. scoticus Hilzheimer, 1906 — Scotland. L. t. sibiricorumJohansen, 1923 — W & SW Siberia (Russia), N Kazakhstan, and Tacheng Mts in N Xinjiang (China). L. t. sylvaticus Nilsson, 1831 —S Sweden, extending in hybrid zones with nominotypical timidus to S coast of Norway and W Latvia. L. t. transbaikalicus Ognev, 1929 — Trans-Baikal region in E Siberia (Russia) and E Inner Mongolia (= Nei Mongol, China). L. t. varronis Miller, 1901 — at high altitudes in the Alps, C Europe. in Leporidae
Subspecies and Distribution. L. t. timidus Linnaeus, 1758 — Scandinavia S to 59° N, N Russia (S to 57° N to 58° N) to E of Ural Mts, Estonia, perhaps Poland, and Altai and Beita Mts in N Xinjiang (China); from Sweden extending in hybrid zones with the subspecies sylvaticus to S coast of Norway and W Latvia. L. t. abet Kuroda, 1938 — Kurile Is (Russia). L. t. ainu Barrett-Hamilton, 1900 — Hokkaido (Japan). L. t. begitschevi Koljuschev, 1936 — Taimyr Peninsula (Russia). L. t. gichiganus J. A. Allen, 1903 — C Yakutia, Kamchatka and Okhotsk Sea coast (Russia). L. t. hibernicus Bell, 1837 — Ireland. L. t. kolymensis Ognev, 1922 — NE Siberia (Russia). L. t. kozhevnikovi Ognev, 1929 — C Russia from 57° to 58°N, whereit intergrades with the nomonotypical timidus S to 53° N. The W boundary is unclear. L. t. lugubris Kastschenko, 1899 — Siberian Altai Mts (Russia). L. t. mordeni Goodwin, 1933 — Russian Far East (Ussuri Valley and lower and middle Amur River) and Heilongjiang (China). L. t. ori Kuroda, 1928 — Sakhalin (Russia). L. t. scoticus Hilzheimer, 1906 — Scotland. L. t. sibiricorumJohansen, 1923 — W & SW Siberia (Russia), N Kazakhstan, and Tacheng Mts in N Xinjiang (China). L. t. sylvaticus Nilsson, 1831 —S Sweden, extending in hybrid zones with nominotypical timidus to S coast of Norway and W Latvia. L. t. transbaikalicus Ognev, 1929 — Trans-Baikal region in E Siberia (Russia) and E Inner Mongolia (= Nei Mongol, China). L. t. varronis Miller, 1901 — at high altitudes in the Alps, C Europe.
Subspecies and Distribution. T:t.tritondeWinton,1899—EChina(CShaanxi,mostofShanxi,SHebei,Tianjin,Henan,Shandong,Anhui,Jiangsu,andNZhejiang). T.t.colinaG.M.Allen,1925—CChina(NShaanxiandNWShanxi). T:t.fuscipesG.M..Allen,1925—NEChina(InnerMongolia[=NeiMongol],NHebei,Beijing,Heilongjiang,Jilin,andLiaoning). T. t. incana Thomas, 1908 — C China (Gansu, Ningxia, and S Shaanxi). T. t. nestor Thomas, 1907 — Korea (including Cheju I) and Russian Far East (Primorsky Krai). in Cricetidae
Subspecies and Distribution. T:t.tritondeWinton,1899—EChina(CShaanxi,mostofShanxi,SHebei,Tianjin,Henan,Shandong,Anhui,Jiangsu,andNZhejiang). T.t.colinaG.M.Allen,1925—CChina(NShaanxiandNWShanxi). T:t.fuscipesG.M..Allen,1925—NEChina(InnerMongolia[=NeiMongol],NHebei,Beijing,Heilongjiang,Jilin,andLiaoning). T. t. incana Thomas, 1908 — C China (Gansu, Ningxia, and S Shaanxi). T. t. nestor Thomas, 1907 — Korea (including Cheju I) and Russian Far East (Primorsky Krai).
FIGURES 119–126 in Four new species of Estheria Robineau-Desvoidy (Diptera: Tachinidae) from China and Nepal, with a review of the East Palearctic and Oriental species
FIGURES 119–126. Known distributions of Estheria spp. in East Asia. 119. E. flavipennis Herting. 120. E. magna (Baranov). 121. E. pallicornis (Loew). 122. E. petiolata (Bonsdorff). 123. E. hirtinerva sp. nov. 124. E. prostata sp. nov. 125. E. tibetensis sp. nov. 126. E. wangi sp. nov.
FIGURE 2 in Perspiria boucheri sp. nov. (Nematoda, Desmodorida) from the East China Sea
FIGURE 2. Perspiria boucheri sp. nov. (A) anterior end of female, showing cephalic setae, amphideal fovea and pharyngeal bulb; (B) anterior end of male, showing buccal cavity, cephalic setae; (C) tail end of male; (D) cloacal region of male, showing spicules and gubernaculum. (Scales: A, C = 20 μm; B, D = 10 μm)
FIGURE 1 in Perspiria boucheri sp. nov. (Nematoda, Desmodorida) from the East China Sea
FIGURE 1. Perspiria boucheri sp. nov. (A) entire view of male; (B) pharyngeal region of male, showing amphideal fovea and terminal bulb; (C) anterior end of male, showing buccal cavity and cephalic setae; (D) entire view of female; (E) spicule and gubernaculum; (F) tail end of male, showing spicule and gubernaculum; (G) reproductive system of female, showing vulva and ovary.
Figs 14–25 in A revision of Nazeris. VI. On the fauna of East Yunnan, China (Coleoptera: Staphylinidae: Paederinae)
Figs 14–25: Nazeris constrictus sp. n. (14–19) and N. claviger sp. n. (20–25): forebody (14, 20); male sternite VII (15, 21); posteromedian portion of male sternite VII (16, 22); male sternite VIII (17, 23); aedeagus in lateral and in ventral view (18–19, 24–25). Scale bars: 14, 20: 1.0 mm; 15, 17–19, 21, 23–25: 0.5 mm; 16, 22: 0.2 mm.
FIGURE 3 in Allium yingshanense, a new species from the Dabie Mountains (east-central China), and taxonomic remarks on the related species
FIGURE 3. Details of Allium yingshanense from type locality. A, single flower. B, opened perianth (teeth at the base of outer filaments indicated by the arrow). C, teeth of the inner filament. D, teeth of the outer filament. E, pistil (showing basal hood-like projections). F, spathe. G, seed showing densely granulated testa (above: ventral face, below: dorsal face). H, capsule. I, cross-section of the scape at the base. J, cross-section of the scape near the top). K, cross-section of the leaf at the base. L, cross-section of the leaf at the mid-length. M, chromosome plate from type locality (2n = 2x = 16; satellited chromosome indicated by the arrow).
Assessing the Interaction of Oceanic and Riverine Processes on Phytoplankton Dynamics in a Highly Dynamic Coastal Ecosystem of the East China Sea
<p>All data.</p>
Characteristics of Infective Endocarditis in East China
ClinicalTrials.gov study NCT04977518. IPD Sharing: NO. Countries: 0. Publications: 0.
East China Sea (ECS) measurements
East China Sea (ECS) measurements spanning 1997 and 1998.
East China Sea validation measurements for GOCI instrument
Measurements made in the East China Sea in 2013 to validate the South Korean GOCI instrument.
Research Compendium for: "Quina technology from Southwest China indicates diverse late-Pleistocene human dynamics in East Asia"
<div> <div> <div> <div> <p>✉ Correspondence: Hao Li <a href="mailto:lihao@itpcas.ac.cn">lihao@itpcas.ac.cn</a></p> <p>✉ Correspondence: Peiyuan Xiao <a href="mailto:xiaopeiyuan@itpcas.ac.cn">xiaopeiyuan@itpcas.ac.cn</a></p> <p>✉ Correspondence: Bo Li <a href="mailto:bli@uow.edu.au">bli@uow.edu.au</a></p> <p>✉ Correspondence: Davide Delpiano <a href="mailto:dlpdvd@unife.it">dlpdvd@unife.it</a></p> </div> </div> </div> <h3>Online access:</h3> <p>Zenodo DOI: <a href="https://doi.org/10.5281/zenodo.13762081">https://doi.org/10.5281/zenodo.13762081</a></p> <p>The files at the URL above will generate the results as found in the publication. The files hosted at <a href="https://github.com/PeiyuanXiao/Lithic-data-Longtan-site">https://github.com/PeiyuanXiao/Lithic-data-Longtan-site</a> are the development versions and may have changed since the paper was published.</p> <h3>Maintainer of this repository:</h3> <p>Peiyuan Xiao <a href="mailto:xiaopeiyuan@itpcas.ac.cn">xiaopeiyuan@itpcas.ac.cn</a></p> <p>Ben Marwick <a href="mailto:bmarwick@uw.edu">bmarwick@uw.edu</a></p> </div> <h3>Abstract:</h3> <p>The Late Pleistocene of Eurasia is key for understanding interactions between early modern humans and different types of archaic human groups. During this period, lithic technology shows more diversity and complexity, likely indicating flexible adaptative strategies. However, cultural variability as expressed by technological types remains vague in large parts of eastern Eurasia, like in China. Here we report a complete Quina technological system identified from the study of the Longtan site in Southwest China. This site has been securely dated to ca. 60–50 thousand years ago (ka), with compelling evidence of core exploitation, production of large and thick flakes, shaping and maintenance of scrapers exhibiting the whole Quina concept, typical of contemporary European Middle Paleolithic technologies developed by Neanderthal groups adapted to climatic oscillations during Marine Isotope Stage (MIS) 4 and early MIS 3. The finding of a Quina lithic assemblage in China not only demonstrates the existence of a Middle Paleolithic technology in the region, but also shows large-scale analogies with Neanderthal behaviors in western Europe. Longtan substantially extends the geographic distribution of this technical behavior in East Asia. Although its origin remains unclear, implications for Pleistocene hominin dispersal and adaptation to diverse ecological settings are considered. The Longtan lithic evidence also provides perspectives for understanding the cultural evolutionary situation before the large-scale arrivals of early modern humans in East Asia predating ~45 ka.</p> <h3>Keywords:</h3> <p>Middle Paleolithic; fluvial terrace; early MIS 3; Late Pleistocene; hominins</p> <div> <div> <h3>R packages and their versions:</h3> <p>Data processing & analyzing: <code>readxl (>= 1.4.3)</code>,<code>tidyverse (>= 2.0.0)</code>,<code>forcats (>= 1.0.0)</code>,<code>dunn.test (>= 1.3.6)</code>, other statistical testing methods use the corresponding functions in the R base package</p> <p>Plots creating: <code>tidyverse (>= 2.0.0)</code>,<code>ggpmisc (>= 0.5.6)</code>,<code>ggdist (>= 3.3.2)</code>,<code>MetBrewer (>= 0.2.0)</code>,<code>ggbeeswarm (>= 0.7.2)</code>,<code>cowplot (>= 1.1.3)</code>,<code>patchwork (>= 1.2.0)</code>,<code>ggtext (>= 0.1.2)</code>,<code>scales (>= 1.3.0)</code></p> </div> </div>
The dataset of raindrop size distribution and environmental properties during summer 2014 and 2015 in East China
<p>This dataset is used to make figures for the paper entitled “Observational Evidence of the Environmental Impacts on Raindrop Size Distribution in East China” submitted to Geophysical Research Letters in June 2022. It contains the disdrometer and automatic weather station observations in minute, hourly, daily scales, and also the training and testing samples for machine learning.</p>
disdrometer data for 2020 summer rainfall in East China
<p>This dataset is used to make figures for the paper entitled “Near Homogeneous Microphysics of the Record-breaking 2020 Summer Monsoon Rainfall in East China” submitted to Geophysical Research Letters in July 2022. It contains the disdrometer datasets for 2020 summer rainfall in Fujian and Jiangsu province, East China.</p>
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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