Lisiguangite, CuPtBiS3, is a new mineral species discovered in a PEG-bearing, Co-Cu sulfide vein in garnet pyroxenite of the Yanshan Mountains, Chengde Prefecture, Hebei Province, China. It is associated with chalcopy...Lisiguangite, CuPtBiS3, is a new mineral species discovered in a PEG-bearing, Co-Cu sulfide vein in garnet pyroxenite of the Yanshan Mountains, Chengde Prefecture, Hebei Province, China. It is associated with chalcopyrite and bornite, galena, minor pyrite, carrolite, molybdenite and the platinum-group minerals daomanite （CuPtAsS2）, Co-bearing malanite （Cu（Pt, Co）2S4） sperrylite, moncheite, cooperite and malyshevite （CuPdBiS3）, rare damiaoite （Pt2In3） and yixunite （Pt3In）. Lisiguangite occurs as idiomorphic crystals, tabular or lamellae （010） and elongated [100] or as aggregates, up to 2 mm long and 0.5 mm wide. The mineral is opaque, has lead-gray color, black streak and metallic luster. The mineral is non-fluorescent. The observed morphology displays the following forms： pinacoids {100}, {010}, {001}, and prism [110}. No twining is observed. The a：b：c ratio, calculated from unit-cell parameters, is 0.6010：1：0.3836. Cleavage： {010} perfect, {001} distinct, {100} may be visible. H Mohs： 2 1/2; VHN25=46.7-49.8 （mean 48.3） kg/mm^2. Tenacity： brittle. Lisiguangite is bright white with a yellowish tint. In reflected light it shows neither internal reflections nor bireflectance or pleochroism. It has weak to moderate anisotropy （blue-greenish to brownish） and parallel-axial extinction. The reflectance values in air （and in oil） for R3, R4 and （^imR3, ^imR4）, at the standard Commission on Ore Mineralogy wavelengths are： 37.5, 35.7 （23.4, 22.3） at 470nm; 38.6, 36.5 （23.6, 22.6） at 546nm; 39.4, 37.5 （23.6, 22.7） at 589 nm and 40.3, 38.2 （23.7, 22.9） at 650 nm. The average of eight electron-microprobe analyses： Cu 12.98, Pt 30.04, Pd 2.69, Bi 37.65 and S 17.55, totaling 100.91%, corresponding to Cu1.10（Pt0.83, Pd0.14）∑0.97Bi0.97S2.96 based on six atoms apfu. The ideal formula is CuPtBiS3. The mineral is orthorhombic. Space group： P212121, a=7.7152（15）A, b=12.838（3）A, c=4.9248（10）A, V=487.80（17）A^3, Z=4. The six strongest lines in the X-ray powder-diffraction pattern [d in A（l） （h k l） are 6.40（30）（020）, 3.24（80）（031）, 3.03（100）（201）, 2.27（40）（051）, 2.14（50）（250）, 1.865（60）（232）.展开更多
2008年4月28～30日在福建省武夷山区采获6属蠓科昆虫,发现有2种短蠓分别是新种和我国的新纪录：公东短蠓新种Brachypogon（Brachypogon）gongdongi Yu et Huang,sp.nov.,巴国短蠓Brachypogon（Brachypogon）pakistanicus Szadziski et H...2008年4月28～30日在福建省武夷山区采获6属蠓科昆虫,发现有2种短蠓分别是新种和我国的新纪录：公东短蠓新种Brachypogon（Brachypogon）gongdongi Yu et Huang,sp.nov.,巴国短蠓Brachypogon（Brachypogon）pakistanicus Szadziski et Havelka,1984是我国新纪录。模式标本收藏于军事医学科学院医学昆虫标本馆。展开更多
It was not possible to carry out a complete analyses of crystal, as the experiment by Ding and Shi et al.. It＇s analysis precision R=0.25 or more big than this, which value are not satisfied for single crystal study,...It was not possible to carry out a complete analyses of crystal, as the experiment by Ding and Shi et al.. It＇s analysis precision R=0.25 or more big than this, which value are not satisfied for single crystal study, but we through many test and found the best： [R（int）=14.5%]. The final fullmatix least-squares refinement on F2 converged to R1=0.0791 and wR2=0.1864 for 704 observed reflections [I 3 2s（I）]. Daomanite is orthorhombic system, space group Cmc21, a=3.7520（8））A, b=15.844（4） A, c=5.8516（12） A, α=β=γ=90°. V=347.86（14）A3, Z=4. Daomanite chemical formula is Cu Pt AsS 2. Idealized composition Me＋M2＋M2＋S2=CuS ·PtA s S. There is no other similar mineral in the world.展开更多
本文记了分别采自云南高黎贡山的栅蛛科栅蛛属Hahnia 2新种:垭口栅蛛,新种S.yakouensis sp.nov.和肾形栅蛛,新种S.reniformis sp.nov..垭口栅蛛后眼列前曲,交媾腔大,扁圆形,交媾孔1个,位于交媾腔下缘,交媾管粗,呈"人"字形下...本文记了分别采自云南高黎贡山的栅蛛科栅蛛属Hahnia 2新种:垭口栅蛛,新种S.yakouensis sp.nov.和肾形栅蛛,新种S.reniformis sp.nov..垭口栅蛛后眼列前曲,交媾腔大,扁圆形,交媾孔1个,位于交媾腔下缘,交媾管粗,呈"人"字形下行分成2支再向两侧扭曲.纳精囊有一肓管斜向上伸出,鉴于上述特征而与Hahnia mridulae Tikader,1970不同.肾形栅蛛交媾孔2个,位于生殖厣腹面中央,纳精囊1对,大,肾形,插入器始于生殖球左下方,鉴于上述特征而与Hahnia xinjiangensis Wang et Liang,1989不同.
Abstract：
The present paper deals with two new species of the genus Hahnia collected from the Gaoligong Mountains Region of Yunnan Province, China: Hahnia yakouensis sp. nov., Hahnia reniformis sp. nov..展开更多
文摘Lisiguangite, CuPtBiS3, is a new mineral species discovered in a PEG-bearing, Co-Cu sulfide vein in garnet pyroxenite of the Yanshan Mountains, Chengde Prefecture, Hebei Province, China. It is associated with chalcopyrite and bornite, galena, minor pyrite, carrolite, molybdenite and the platinum-group minerals daomanite （CuPtAsS2）, Co-bearing malanite （Cu（Pt, Co）2S4） sperrylite, moncheite, cooperite and malyshevite （CuPdBiS3）, rare damiaoite （Pt2In3） and yixunite （Pt3In）. Lisiguangite occurs as idiomorphic crystals, tabular or lamellae （010） and elongated [100] or as aggregates, up to 2 mm long and 0.5 mm wide. The mineral is opaque, has lead-gray color, black streak and metallic luster. The mineral is non-fluorescent. The observed morphology displays the following forms： pinacoids {100}, {010}, {001}, and prism [110}. No twining is observed. The a：b：c ratio, calculated from unit-cell parameters, is 0.6010：1：0.3836. Cleavage： {010} perfect, {001} distinct, {100} may be visible. H Mohs： 2 1/2; VHN25=46.7-49.8 （mean 48.3） kg/mm^2. Tenacity： brittle. Lisiguangite is bright white with a yellowish tint. In reflected light it shows neither internal reflections nor bireflectance or pleochroism. It has weak to moderate anisotropy （blue-greenish to brownish） and parallel-axial extinction. The reflectance values in air （and in oil） for R3, R4 and （^imR3, ^imR4）, at the standard Commission on Ore Mineralogy wavelengths are： 37.5, 35.7 （23.4, 22.3） at 470nm; 38.6, 36.5 （23.6, 22.6） at 546nm; 39.4, 37.5 （23.6, 22.7） at 589 nm and 40.3, 38.2 （23.7, 22.9） at 650 nm. The average of eight electron-microprobe analyses： Cu 12.98, Pt 30.04, Pd 2.69, Bi 37.65 and S 17.55, totaling 100.91%, corresponding to Cu1.10（Pt0.83, Pd0.14）∑0.97Bi0.97S2.96 based on six atoms apfu. The ideal formula is CuPtBiS3. The mineral is orthorhombic. Space group： P212121, a=7.7152（15）A, b=12.838（3）A, c=4.9248（10）A, V=487.80（17）A^3, Z=4. The six strongest lines in the X-ray powder-diffraction pattern [d in A（l） （h k l） are 6.40（30）（020）, 3.24（80）（031）, 3.03（100）（201）, 2.27（40）（051）, 2.14（50）（250）, 1.865（60）（232）.
基金the National Science Foundation(USA)project"Biotic Survey of the Gaoligongshan,a Biodiversity Hotspot in Western Yunnan,China"(DEB-0103795)the Foundation of Nature Sciences of the Education Department of Hunan Provincethe National Natural Sciences Foundation of China(NSFC-30499341 ,30670234 ,30770255)
文摘描述了采自中国云南省高黎贡山的4种蟹蛛：小棒绿蟹蛛Oxytate clavulata Tang,Yinet Peng,sp.nov.和中国3新纪录种：不丹绿蟹蛛Oxytate bhutanica Ono,2001,小斜蟹蛛Loxobates minor Ono,2001和南国花叶蛛Synema nangokuOno,2002,其中小斜蟹蛛的雌性为首次发现。小棒绿蟹蛛,新种Oxytate clavulata Tang,Yinet Peng,sp.nov.（图1～5）正模♂（HNU-YHY2601）,云南腾冲县上营乡大蒿坪村,2040m,2006-06-04,尹长民、胡佳芳、杨效华采。词源：本种因触肢器的插入器呈小棒状而命名。新种近似于平行绿蟹蛛O.parallela（Simon,1880）,但能与后者区别于：1）触肢后侧突末端弯向内侧而后者弯向腹侧;2）插入器基部有一突起而后者没有。分布：中国云南。不丹绿蟹蛛Oxytate bhutanica Ono,2001（图6～15）Oxytate bhutanica Ono,2001：205,figs.1-5.观察标本：1♀,1♂（HNU-YHY0401）,界头乡桥头村,1652m,2006-05-17;6♀♀（HNU-YHY0302）,界头乡周家坡,1660m,2006-05-16;1♂（HNU-YHY0803）,界头乡张家营村,1665m,2006-05-20;1♀,1♂（CAS-YHY1506）,腾岳镇宝丰寺,1790m,2006-05-31;1♀（CAS-YHY1703）,曲石乡热海,1470m,2006-06-01;1♀（CAS-YHY3801）,荷花镇米兰,1400m,2006-06-07。以上标本均由尹长民、胡佳芳和杨效华采自云南省腾冲县。其余观察标本：1♀（HNU-Tang040501）,贡山县独龙江乡迪政当村,1841m,2004-10-27～30,唐果采;1♀（HNU-Tang040605）,贡山县独龙江乡龙元村白来组,1676m,2004-10-31～11-03,唐果采;2♀♀（CAS-DHK0501201）,泸水县片马乡岗房,1780m,2005-05-16,David KAVANAUGH采。分布：不丹、中国（云南）。小斜蟹蛛Loxobates minor Ono,2001（图16～28）Loxobates minor Ono,2001：207,figs.6-8.观察标本：1♀,2♂♂（HNU-David065002）;云南腾冲清水镇热海良盈村,1450m,2006-06-01,David KAVANAUGH,Roberta BRETT和董大志采;6♀♀（YHY1707：3♀♀,HNU;3♀♀,CAS）;云南腾冲清水镇热海,1470m,2006-06-01,尹长民、胡佳芳、杨效华采;1♂（CAS-YHY2102）,腾冲荷花镇朗蒲村,1150m,2006-06-02,胡鹏采。分布：不丹、中国。南国花叶蛛Synema nangoku Ono,2002（图29～33）Synema nangoku Ono,2002：206,figs.13-18.观察标本：1♀,3若蛛（HNU-YHY3202）,中国云南腾冲芒棒乡,1300m,2006-06-05,胡鹏采。分布：日本、中国（云南）。
文摘2008年4月28～30日在福建省武夷山区采获6属蠓科昆虫,发现有2种短蠓分别是新种和我国的新纪录：公东短蠓新种Brachypogon（Brachypogon）gongdongi Yu et Huang,sp.nov.,巴国短蠓Brachypogon（Brachypogon）pakistanicus Szadziski et Havelka,1984是我国新纪录。模式标本收藏于军事医学科学院医学昆虫标本馆。
文摘It was not possible to carry out a complete analyses of crystal, as the experiment by Ding and Shi et al.. It＇s analysis precision R=0.25 or more big than this, which value are not satisfied for single crystal study, but we through many test and found the best： [R（int）=14.5%]. The final fullmatix least-squares refinement on F2 converged to R1=0.0791 and wR2=0.1864 for 704 observed reflections [I 3 2s（I）]. Daomanite is orthorhombic system, space group Cmc21, a=3.7520（8））A, b=15.844（4） A, c=5.8516（12） A, α=β=γ=90°. V=347.86（14）A3, Z=4. Daomanite chemical formula is Cu Pt AsS 2. Idealized composition Me＋M2＋M2＋S2=CuS ·PtA s S. There is no other similar mineral in the world.
基金supported by the National Natural Sciences Foundation of China(30570210,30630010)Innovative Program of The Chinese Academy of Sciences(No.KSCX2-YW-Z-0930)project for the insect resources investigation of Liupan Mountain(LIR0810)
基金supported by the National Natural Sciences Foundation of China (31070467)Knowledge Innovation Programs of Chinese Academy of Sciences (KZCX2-YW -BR-16)the Fundamental Research Funds for the Central Universities (2008-10008 and 2009-05022)
基金National Science Foundation of USA on Biotic Survey of the Gaoligongshan, a Biodiversity Hotspot in Western Yun-nan, China，the Foundation of Nature Sciences of Education Department of Hunan Province
文摘本文记了分别采自云南高黎贡山的栅蛛科栅蛛属Hahnia 2新种:垭口栅蛛,新种S.yakouensis sp.nov.和肾形栅蛛,新种S.reniformis sp.nov..垭口栅蛛后眼列前曲,交媾腔大,扁圆形,交媾孔1个,位于交媾腔下缘,交媾管粗,呈"人"字形下行分成2支再向两侧扭曲.纳精囊有一肓管斜向上伸出,鉴于上述特征而与Hahnia mridulae Tikader,1970不同.肾形栅蛛交媾孔2个,位于生殖厣腹面中央,纳精囊1对,大,肾形,插入器始于生殖球左下方,鉴于上述特征而与Hahnia xinjiangensis Wang et Liang,1989不同.
Abstract：
The present paper deals with two new species of the genus Hahnia collected from the Gaoligong Mountains Region of Yunnan Province, China: Hahnia yakouensis sp. nov., Hahnia reniformis sp. nov..
