1,723,985 research outputs found
Guo Liang Shen oral history interview and transcript
This recording and transcript form part of a collection of oral history interviews conducted by the Chao Center for Asian Studies at Rice University. This collection includes audio recordings and transcripts of interviews with Asian Americans native to or living in Houston.Dr. Guo Liang Shen was born in the Jiangsu province of China in 1942. His hometown was
destroyed when the Japan invaded in 1937 and his family became refugees as a result. Despite a difficult
childhood, Dr. Shen excelled in his studies in school and was accepted into Peking Union Medical
College (PUMC) and studied to be a physician. He was part of the last cohort of medical students being
formally trained when the Cultural Revolution abruptly stopped his studies and he was then sent to
Runhuai county in Guizhou province to serve as physician, learning traditional Chinese medicine from
those who lived there. He went on to get a Master’s degree in Immunology at PUMC and the Chinese
Academy of Medical Sciences before immigrating to the United States to do research on monoclonal
antibodies at UT Southwestern Medical Center in Dallas, Texas. After decades of working as a
researcher, Dr. Shen retired in 2012 and moved to Houston. He enjoys photography, and brought prints of
his photos from his trip to China and photos of birds at High Island, Texas
Notes on the Chinese fauna of Ceratocanthinae (Coleoptera: Hybosoridae), with description of a new species of Eusphaeropeltis Gestro, 1898
Jiang, Ri-Xin, Ballerio, Alberto, Guo, Liang, Wang, Shuo (2020): Notes on the Chinese fauna of Ceratocanthinae (Coleoptera: Hybosoridae), with description of a new species of Eusphaeropeltis Gestro, 1898. Zootaxa 4851 (1): 180-188, DOI: https://doi.org/10.11646/zootaxa.4851.1.
FIGURES 21 in Description of a new subspecies of Chonala laurae Bozano, 1999 from Southeastern China (Lepidoptera, Nymphalidae, Satyrinae)
FIGURES 21. Distribution map of Chonala spp. in the current study.Published as part of Guo, Liang, Huang, Si-Yao, Wang, Min & Ma, Fang-Zhou, 2023, Description of a new subspecies of Chonala laurae Bozano, 1999 from Southeastern China (Lepidoptera, Nymphalidae, Satyrinae), pp. 593-600 in Zootaxa 5325 (4) on page 599, DOI: 10.11646/zootaxa.5325.4.9, http://zenodo.org/record/824378
FIGURE 3 in Two new species of Coecobrya (Collembola: Entomobryidae: Entomobryinae) from China, with a key to the Chinese species of the genus
FIGURE 3. Coecobrya brevis sp. nov. A, chaetotaxy of Abd. V; B, lateral side of manubrium; C, mucro.Published as part of Xu, Guo-Liang, Yu, Dao-Yuan & Zhang, Feng, 2012, Two new species of Coecobrya (Collembola: Entomobryidae: Entomobryinae) from China, with a key to the Chinese species of the genus, pp. 61-68 in Zootaxa 3399 on page 65, DOI: 10.5281/zenodo.21350
Review of the genus Lemaireia Nässig & Holloway, 1988 from China, with description of a new species (Lepidoptera: Saturniidae)
Jiang, Zhuo-Heng, Wang, Cheng-Bin, Miu, Ben-Fu, Guo, Liang (2021): Review of the genus Lemaireia Nässig & Holloway, 1988 from China, with description of a new species (Lepidoptera: Saturniidae). Zootaxa 5027 (3): 429-437, DOI: 10.11646/zootaxa.5027.3.
Seafloor basalt alteration and chemical change in the ultra thinly sedimented South Pacific
Determining the relationship between ocean floor basalt alteration and sedimentation is fundamental to understanding how oceanic crust evolves with time. Ocean floor basalts recovered at IODP Sites U1365 (?100 Ma) and U1368 (?13.5 Ma) in the South Pacific have been subjected to remarkably low sedimentation rates (0.71 and 1.1 m/Myr?1, respectively). We report detailed petrographic and geochemical analysis of basalt cores from these sites in order to investigate what impact sediment insulation has on seafloor alteration beyond 10–15 Myr of ocean crust formation. Both sites exhibit low-temperature (<150°C) alteration (e.g., iron-hydroxides, carbonate, and quartz) within a predominantly oxidative regime, albeit with markedly different alteration styles and intensity. Alteration at Site U1365, which is predominantly composed of sheet flows, occurs mainly near sheet flow boundaries and fractures. In contrast, Site U1368 comprises interlayered pillows and thin sheet flows that have been subjected to relatively even levels of alteration. Variation of alteration style and intensity between Sites U1365 and U1368 appear closely tied to lithology and crustal structure. Although alteration-induced elemental changes at both sites are similar in, e.g., increasing K, Rb, U, Ba, and Fe3+ and decreasing Fe2+, Ca, and Ni, they show distinct differences in Th, which is significantly decreased at Site U1365 but relatively constant at Site U1368. At both sites enrichment of LREEs relative to HREEs is ascribed to alteration. The greater vein abundance and notably higher Fe3+/TiO2, K2O/TiO2, LOI/TiO2, and Rb/TiO2 ratios of representative samples at Site U1365 compared to Site U1368 are attributed to increased alteration intensity. This is mirrored by greater overall chemical change (Fe2O3, FeO, CaO, K2O, Li, Rb, Pb, and U) observed at Site U1365 than those of Site U1368 and other DSDP/ODP sites between 6 and 46 Ma. Since both Sites U1365 and U1368 endured only minimal sedimentation, we attribute the differences in overall chemical change across the two sites to duration of exposure to seawater
FIGURES 5–7 in A review of the genus Trachystolodes Breuning, 1943 (Coleoptera: Cerambycidae Lamiinae: Lamiini)
FIGURES 5–7. Trachystolodes huangjianbini sp. nov., holotype, male. Habitus: 5. dorsal view, 6. lateral view, 7. ventral view. Scale bars: 5 mm.Published as part of Huang, Gui-Qiang, Guo, Liang & Liu, Peng-Yu, 2020, A review of the genus Trachystolodes Breuning, 1943 (Coleoptera: Cerambycidae Lamiinae: Lamiini), pp. 49-64 in Zootaxa 4759 (1) on page 52, DOI: 10.11646/zootaxa.4759.1.3, http://zenodo.org/record/373595
Arcofaciella obflexa Guo & Liang 2005
Arcofaciella obflexa Guo & Liang, 2005 Figs 3–4 Material examined CHINA • 1 ♂; Yunnan, Jinghong; 21°24′ N, 101°71′ E; 5 Aug. 1958; Y.S. Wang leg.; on bamboo; GUGC-FDTA-19580801 • 1 ♂; Yunnan, Jinghong; 21°24′ N, 101°71′ E; 8 Jun. 2011; J.K. Long leg.; on bamboo; GUGC-FDTA-20110601 • 4 ♂♂, 2 ♀♀; Yunnan, Yingjiang; 24°74′ N, 97°56′ E; 8 Aug. 2015; X.S. Chen and L. Yang leg.; on bamboo; GUGC-FDTA-20150801 to 20150806 • 7 ♂♂, 5 ♀♀; Yunnan, Yingjiang; 24°74′ N, 97°56′ E; 19 Aug. 2018; H.X. Li, F.E. Li and Q. Luo leg.; on bamboo; GUGC- FDTA-20180801 to 20180812 • 4 ♂♂, 4 ♀♀; Yunnan, Ruili; 24°01′ N, 97°84′ E; 13 Aug. 2018; H.X. Li and Q. Luo leg.; on bamboo; GUGC-FDTA-20180813 to 20180820 • 13 ♂♂, 5 ♀♀; Yunnan, Jinghong, Menglong; 21°57′ N, 100°67′ E; 21 Jun. 2019; H.X. Li, S.Y. Xun, N. Gong and F.E. Li leg.; on bamboo; GUGC-FDTA-20190601 to 20190618. Redescription MEASUREMENTS. Body length including forewing: male 4.3–4.6 mm (N = 10); female 4.5–4.9 mm (N = 10); forewing length: male 3.6–3.8 mm (N = 10); female 3.7–4.0 mm (N = 10). COLORATION. Vertex (Fig. 3G), face (Fig. 3H) yellowish green. Antennae (Fig. 3H) light scorched green, distal part of first segment and basal part of second segment black brown. Pronotum (Fig. 3G), mesonotum (Fig. 3G) and legs scorched, abdomen light nacarat, slightly lighter ventrally and disc of first abdominal segment black. Forewings (Fig. 4D) grayish brown, darker at base, veins brown with yellowish white granules, veins dashed, apex of longitudinal veins brown. HEAD AND THORAX.Vertex (Fig. 4A) at midline shorter than wide at base (0.28:1), width at apex narrower than at base (0.56:1). Frons (Fig. 4C) 1.35 times longer in middle line than widest part, narrower at apex than at base (0.86:1). Postclypeus wider at base than frons at apex. Antennae (Fig. 4C) with first segment longer than wide at apex (1.33:1), shorter than second segment (0.63:1). Pronotum (Fig. 4A) at midline longer than vertex (1.71:1), lateral carinae arched, medially concave, flexing backwards near middle at sub-right angle and nearly attaining hind margin. Mesonotum (Fig. 4A) 2.39 times as long as vertex and pronotum combined in middle line. Forewing (Fig. 4D) in middle line longer than wide at widest part (3.12:1). Spinal formula of hind tibia 5-8-5. MALE GENITALIA. Anal segment in posterior view (Fig. 4E) concave medially, lateroapical angle protruding caudad, anal style distinctly elongate and narrow, nearly lanceolate in lateral view (Fig. 4G). Pygofer in profile (Fig. 4F) with dorsal margin shorter than ventral margin, posterior margin convex, in posterior view (Fig. 4H) with opening longer than wide, ventral margin broadly concave, without medioventral process. Genital styles (Fig. 4I–J) long, reaching basal anal segment, with an angled process medioventrally and 2 small teeth at outer base laterally, apex with outer apical angle rounded and protruding, slightly dorsad, inner apical angle bifurcate, inner laterodorsal margin with a dull angled process at ⅔ of genital styles near base. Aedeagus (Fig. 4K–L) long, tubular, with distinct phallotheca, with basal part lying between two valvular processes of phallotheca, deflecting leftward, apical part recurved downward and reaching ⅔ of phallotheca. Phallotheca almost reaching base of genital styles, apical part warping dorsad, basal part stout, with two valvular processes, in dorsal view with a large and a small round valvular processes, tapering from ⅗ to apex, in right view with three processes near base. Host plant Bambusoideae. Distribution China (Yunnan).Published as part of Chen, Xiang-Sheng & Yang, Lin, 2021, Review the bamboo-feeding genus Arcofaciella Fennah, 1956 (Hemiptera: Fulgoromorpha: Delphacidae) with description of a new species from India, pp. 51-66 in European Journal of Taxonomy 748 (1) on pages 57-60, DOI: 10.5852/ejt.2021.748.1341, http://zenodo.org/record/474509
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