SHRIMP

摘要： Tropomyosin(TM)in shrimp is one of the predominant causes of food allergy around the world.In the present study,the effect of seabuckthorn juice against TM-induced shrimp allergy was investigated in BALB/c mice.Allergic symptoms,spleen index,intestinal section and diarrhea were measured in shrimp allergy mice.As the results,seabuckthorn juice suppressed the lesions in jejunum tissue,diarrhea and allergic symptoms in shrimp allergy mice.Seabuckthorn juice also reduced serum concentrations of tumor necrosis factor-a(TNF-α)as well as immunoglobulin E(IgE)and stimulated the secretion of interleukin-10(IL-10)in mice with shrimp allergy.Taken together,our findings suggest that increased IL-10 by seabuckthorn juice inhibits Th2 cytokine production to suppress shrimp allergic symptoms.Furthermore,seabuckthorn juice also regulates shrimp allergy by reducing jejunum lesions,inhibiting levels of TNF-αand IgE.

摘要： 撮科蛇绿混杂岩出露于元江县撮科大寨及周边地区,受到后期构造作用影响发生一定的变质和变形。蛇岩性较为复杂,岩块与基质之间为断层接触。基质以硅质岩、熔结凝灰岩和花岗质砾岩为主,岩块的类型主要有辉石岩、辉长岩、辉绿岩、闪长岩、玄武岩、斜长花岗岩等。其中,撮科蛇绿混杂岩中熔结凝灰岩的SHRIMP锆石U-Pb龄为(1170±7)Ma(MSWD=0.54,n=12),花岗质砾岩基质具有单一的年龄,为(1151±5)Ma(MSWD=1.3,n=17);辉长岩岩块的SHRIMP锆石U-Pb年龄为(1168±8)Ma(MSWD=0.72,n=17),斜长花岗岩岩块的SHRIMP锆石U-Pb年龄为(1163±9)Ma(MSWD=1.83,n=15),花岗斑岩岩块的SHRIMP锆石U-Pb年龄为(1186±6)Ma(MSWD=0.92,n=17)。这些年龄指示该蛇绿混杂岩形成于中元古代晚期。撮科蛇绿混杂岩中辉长岩REE标准化曲线整体表现较为平坦的右倾趋势,具有与E-MORB相似的稀土元素特征。在MORB标准化图解中Nb、Ta没有出现明显的负异常,极低的Zr/Nb(8.65)、La/Nb(1.05)、Ba/Nb(10.72)、Th/Nb(0.10)、Th/La(0.09)、Ba/La(10.56)、Zr/Hf(43.4)平均值,且微量元素判别投点主要落入板内玄武岩范围,指示撮科蛇绿混杂岩应属于MORB型蛇绿岩,可能形成于板块伸展的构造环境。熔结凝灰岩锆石的ε_(Hf)(t)值为-8.7~-4.7,平均值为-6.6,所有ε_(Hf)(t)均为负,Hf同位素模式年龄(t_(DMC))为2534~2296 Ma,平均为2408 Ma,指示熔结凝灰岩来自古元古代结晶基底的重熔。撮科蛇绿混杂岩的厘定,对重新认识原大红山群老厂河组的属性,研究扬子陆块西南缘中—新元古代岩浆和构造事件,划分扬子陆块基底大地构造单元具有重要意义。

摘要： 华北吕梁地区出露的以陆源碎屑沉积为主的汉高山群为中元古界底界界线层型的理想候选剖面,其时代的确定对认识华北前寒武纪地质演化历史及初始盖层的确定及Nuna超大陆聚散的研究具有重要的意义。目前,汉高山群的时代、划分对比及其意义还存在较大争议。本研究使用SHRIMP(二次离子质谱仪)对汉高山群安山岩中的锆石进行了U-Pb同位素分析,获得其^(207)Pb/^(206)Pb年龄加权平均值为1769±9 Ma(2σ)。这是首次直接测得汉高山群锆石U-Pb年龄。另测得同一层位的小两岭组3个不同部位火山岩中的锆石^(207)Pb/^(206)Pb年龄加权平均值分别为1792±18 Ma、1773±19 Ma和1778±20 Ma,与汉高山群的年龄在误差范围内一致,故认为汉高山群和小两岭组的时代分别为1769±9 Ma和1792~1773 Ma。结合前人的研究资料,认为汉高山群和小两岭组的形成时代为1780 Ma左右。吕梁地区汉高山群的剖面地层连续,发育区域上分布较为稳定的安山岩,是华北克拉通中南部极好的区域等时标志层。该时期的裂谷沉积和火山岩在扬子陆块西部、劳伦大陆西北部、澳大利亚北部、南美巴西圣弗兰西斯科(São Francisco)克拉通、非洲刚果克拉通及西伯利亚克拉通均有产出,且可以对比,显示同时期由Nuna超大陆初始裂解引起的陆内裂谷沉积地层的全球分布特征,由此提出国际中元古界底界应该下移,并且汉高山剖面可作为国际上新的中元古界底界的候选层型剖面。

摘要： Fèiténgxiā沸腾虾(The Seething Shrimps)Ingredients:300 g shrimps10 g dried chili 7 g Sichuan pepperminced garlic sliced ginger and chopped scallion as needed Seasonings:salt, MSG, essence of chicken, chili oil.

摘要： 华北克拉通南缘结晶基底之上广泛发育中-新元古代(1800～542Ma)盖层岩系,但由于缺少精确的同位素年龄数据,其地层划分和对比方案一直存在较大的争议.本次工作在河南省栾川县龙家园组底部和下部各发现了一套凝灰岩,进而获得了1594±12Ma和1541±8Ma的SHRIMP锆石U-Pb年龄,首次精确标定了该地区龙家园组的形成时限,该组底界的时代接近1600Ma.龙家园组沉积时代为中元古代蓟县纪最早期;在河南省汝阳、汝州、鲁山地区的洛峪口组凝灰岩中获得了1596±7Ma、1596±15Ma、1608±17Ma和1620±16Ma的SHRIMP锆石U-Pb年龄,进一步精确标定了洛峪口组的形成时代,洛峪口组形成于长城纪的末期.结合汝阳群云梦山组碎屑锆石U-Pb年龄结果,汝阳群-洛峪群的形成时限约为1700～1600Ma.官道口群应是汝阳群之后的地层系统,而不是早前认为的与之同期的地层.

摘要： Chili sauce shrimp paste (CSSP) is an exotic traditional sauce prepared using mainly fresh chili and shrimp paste well known as sambal terasi (Indonesia) and sambal belacan (Malaysia and Brunei). This study aims to evaluate CSSP from different regions in Indonesia on physiochemical properties, volatile compounds, and sensory evaluation. Evaluation in free amino acid (FAA) and volatile compounds were analyzed using HPLC and GC-MS. CSSP had no significant (p > 0.05) on proximate (except for moisture), salinity, pH, microbial counts and the redness index (a*/b*) compared to control. The identified volatiles can be grouped into hydrocarbon, carbonyl, sulfur, alcohol, nitrogen, fatty acid, and ester compounds. The CSSP A, B, C, D, and E (control) contained 9, 21, 12, 29, and 6 volatile compounds respectively. The total FAA ranged from 44.32 to 67.03 g/100 g, and histidine (his) was found as the most abundant in each CSSP. The rheological properties (yield stress, viscosity, and consistency) of CSSP and control values were significantly, except for CSSP B. The intensities perceived of saltiness, sweetness, and bitterness were greatly varied among CSSP. Although there is no correlation between sweetness and bitterness this is indicated by the negative correlation.

摘要： Commelina diffusa Burm. F. is a herbaceous tropical plant with different traditional medicinal uses. Present study is aimed to isolate the bioactive compounds from DCM-Methanol extract of the powdered whole plant of Commelina diffusa and to investigate the cytotoxic, antimicrobial and antioxidant activities of the crude extract and its twelve vacuum liquid chromatographic fraction (CD1-12). Vacuum Liquid Chromatography (VLC) was employed to isolate bioactive metabolites. The physicochemical properties of the isolated compound were examined and the molecular structure was elucidated by NMR spectroscopy.?Cytotoxic, antibacterial, antioxidant activities were evaluated following brine shrimp lethality bioassay, disc diffusion method and DPPH free radical scavenging assay respectively. The isolated compound was identified as steroid (stigmasterol) which had significant cytotoxic effect on vero cell line. The crude extract and its fractions (CD8-CD12) exhibited strong cytotoxicity in brine shrimp lethality bioassay having LC50 values 3.79, 9.19, 29.49, 16.60, 19.36, 44.58 μg/mL respectively. The crude extract showed mild to strong antibacterial activity. Fractions (CD5-CD12) showed mild to strong antibacterial activity against Escherichia coli in comparison with Kanamycin (standard). Strong antioxidant activities were found in crude extract (IC50 value 30.52 μg/ml), CD11 (IC50 value 39.27 μg/ml) and CD12 (IC50 value 19.50 μg/ml). The study suggests Commelina diffusa plant extract to have strong antioxidant and cytotoxic activity which is indicative of presence of compounds with broad spectrum of curative applications. One compound namely stigmasterol has been isolated from the plant.

摘要： 为了确定五龙金矿围岩的侵位和变形时代,进一步探讨辽东地区晚中生代构造体制转折时限,采用岩相学观察和锆石SHRIMP U-Pb定年技术,对辽东五龙大型金矿的围岩五龙岩体、侵入五龙岩体中的花岗斑岩脉和三股流岩体进行了研究。结果表明,五龙岩体具弱片麻状、片麻状构造,花岗斑岩脉也发生了变形作用,三股流岩体未发生变形作用。五龙岩体SHRIMP UPb年龄为(159. 2±1. 9) Ma和(160. 0±1. 4) Ma,花岗斑岩SHRIMP U-Pb年龄为(132. 14±0. 85) Ma,三股流岩体SHRIMP U-Pb年龄为122~124 Ma。辽东五龙岩体经历的推覆、挤压事件止于132~124 Ma。辽东地区晚侏罗世的推覆、挤压事件与古太平洋板块向欧亚大陆俯冲作用关系密切,五龙金矿的成矿大地构造背景亦与此次俯冲有关。