[(O)MoCu_3(μ_3-S)_3(μ_3-Cl)(PPh_3)_3]·2THF的合成及其晶体结构

固体化合物(NH_4)_6Mo_7O_(24)·4H_2O和(PPh_3)_2CuCl与饱和液体NH_4HS反应获得桔红针状标题晶体。晶体空间群为P2_1/c,晶胞参数a=11.742(2),b=28.186(7),c=19.304(3),β=100.57(2)°,V=6280.4(?)~3,D_c=1.46g/cm~3,Z=4,F(000)=2816。在3≤2θ≤45°范围内收集到8414个独立衍射强度数据,其中3856个I≥1.5σ(I)强度数据参加结构计算。标题化合物分子是以{MoCu_3S_3Cl}类立方烷型簇为核心的分子,Mo—Cu的平均距离为2.716。

Palaeoenvironmental changes from pollen record in deep sea core PC-1 from northern Okinawa Trough, East China Sea during the past 24 ka

A pollen record of core PC-1 from the northern Okinawa Trough, East China Sea (ECS), provides information on vegetation and climate changes since 24 cal. kaBP. A total of 103 samples were palynologically analyzed at 8 cm intervals with a time resolution of 230 a. Four pollen zones are recognized: zone I (812-715 cm, 24.2-21.1 cal. kaBP), zone II (715-451 cm, 21.1-15.2 cal. kaBP), zone III (451-251 cm, 15.2-10.8 cal. kaBP), zone IV (251-0 cm, 10.8-0.3 cal. kaBP), corresponding to Late MIS 3, Last Glacial Maximum (LGM), deglaciation and Holocene, respectively. The LGM is characterized by the dominance of herbs, mainly Artemisia, and high pollen influx, implying an open vegetation on the exposed continental shelf and a cool and dry climate. The deglaciation is a climate warming stage with Pinus percentage increased and Artemisia percentage decreased and a rapid sea-level rise. The Holocene is characterized by predominance of tree pollen with rapid increase in Castanea-Castanopsis indicating the development of mixed evergreen and deciduous broad-leaved forest and a warm, humid climate. Low pollen influx during the Holocene probably implies submergence of the continental shelf and retreat of the pollen source area. The vegetation indicated by pollen assemblage found in this upper zone is consistent with the present vegetation found in Kyushu, Japan. Originating from the humid mountain area of North Luzon of the Philippines, Tasmania and New Zealand, Phyllocladus with sporadic occurrence throughout PC-1 core probably suggests the influence of Palaeo-Kuroshio Current or intense summer monsoon. The observed changes in Pinus and Herbs percentage indicate fluctuations of the sea level, and high Pinus percentage corresponds to high sea level. Spectrum analysis of the pollen percentage record reveals many millennial-scale periodicities, such as periodicities of 6.8, 3.85 2.2, 1.6 ka.

栉孔扇贝抗氧化酶基因的克隆与表达分析

扇贝是我国海水养殖的重要品种，但自1994年以来，养殖扇贝陆续爆发的大规模死亡，不但造成了巨大的经济损失，而且直接威胁到现有产业的生存和发展。扇贝病害的不断爆发以及病因的多样性迫切要求制定新的疾病防治措施和开发新型的抗菌物质。因此，深入研究扇贝免疫防御机制，探讨提高机体抗病力的有效途径和方法，改良种质和培育抗病品系，无疑是解决目前困扰扇贝养殖业健康可持续发展的必经之路。 抗氧化酶可以清除活性氧，是维持机体内氧环境平衡，抵抗外界环境影响的重要免疫因子。本研究采用大规模 EST 测序方法和同源克隆的方法，结合 cDNA 末端快速扩增（RACE）技术，从栉孔扇贝中克隆到了超氧化物岐化酶(Superoxide dismutase，SOD)、过氧化氢酶(Catalase，CAT)、谷胱甘肽过氧化物酶（Glutathione peroxidase，GPX）等抗氧化酶基因的全长 cDNA序列，并对其基因结构进行了分析。同时，用实时定量PCR方法对这三个基因在健康扇贝血淋巴细胞、肾、鳃、肌肉、性腺等组织和在分别用鳗弧菌，溶壁微球菌和假丝酵母处理扇贝后不同时间段的表达差异情况进行了研究。 超氧化物歧化酶基因CfSOD的cDNA 全长为1022 bp，其中开放阅读框（Open Reading Frame, ORF）含有 459 bp，编码 153个氨基酸残基，无信号肽，为胞内蛋白。经BLASTP分析发现，CfSOD与其它动物具有较高的同源性。CfSOD中存在两个Cu/Zn-SOD的签名序列；另外Cu结合必须氨基酸(His-45，-47，-62 和-119)和Zn结合必须氨基酸(His-62，-70，-79和Asp-82)在CfSOD中保守。实时定量PCR 检测发现，CfSOD在鳃、血细胞和肾中有较高的表达。在鳗弧菌和溶壁微球菌刺激后，CfSOD的相对表达量逐渐下降，然后分别在32小时和16小时的时候恢复到刺激前的表达水平。在假丝酵母刺激后，CfSOD的mRNA表达没有显著差异。 栉孔扇贝过氧化氢酶基因CfCAT的cDNA全长为3146 bp，其中开放阅读框含有1521bp，编码507个氨基酸残基，无信号肽，为胞内蛋白。经BLASTP分析发现，CfCAT与其它动物具有较高的同源性。 CfCAT中存在过氧化氢酶近端活性位点和过氧化氢酶近端血红素配体签名序列，另外存在两个糖基化位点 NFS和 NFT，同时在CfCAT 的C末端存在过氧化物酶体定位信号AQL，为典型过氧化氢酶。实时定量PCR 检测发现，健康的扇贝中CfCAT在鳃和性腺中有较高的表达。CfCAT基因在鳗弧菌刺后表达升高，在4小时达到最高，约是刺激前表达量的6.8倍（P<0.05），后随着时间的变化而逐渐下降。在8小时表达量达到为刺激前表达量的1.3倍（P<0.05），在16和32小时略高于刺激前的水平。在溶壁微球菌刺激后CfCAT基因表达量也呈上升趋势，在刺激后4小时达到刺激前表达量的约2倍，然后有所下降，在16 小时又上升到刺激前表达量的2.9倍。CfCAT基因在假丝酵母刺激后的表达略有升高，4小时约是刺激前的1.2倍（P<0.05），在其他时间段变化不明显。 栉孔扇贝谷胱甘肽过氧化物酶基因CfGPX的cDNA 全长为1290 bp，其中开放阅读框含有705bp，编码235个氨基酸残基，有一个24核苷酸的信号肽序列。经BLASTP 分析发现，CfSOD与其它动物具有较高的同源性。CfGPX中发现谷胱甘肽过氧化物酶活性位点的签名序列， 另外发现硒半胱氨酸和硒半胱氨酸插入序列，为含硒型谷胱甘肽过氧化物酶。实时定量PCR 检测发现，未经处理的扇贝中CfGPX在性腺、肌肉、血和肾中有较高的表达。CfGPX基因在鳗弧菌刺后表达量快速上升，在6 小时的时候表达量达到最高，为刺激前的4.0倍（P>0.05），后随着时间的变化而逐渐下降。在溶壁微球菌刺激后CfGPX在前6小时表达略有降低，在6小时的时候表达量为刺激前的0.5倍（P<0.05），后随着时间的变化而逐渐升高。在16小时的时候表达量为刺激前的2.1倍（P<0.05）。在假丝酵母刺激后， CfGPX的表达量略有下降在8小时的时候表达量为刺激前的0.8倍（P<0.05）。 实验证明栉孔扇贝的超氧化物歧化酶基因CfSOD，过氧化氢酶基因CfCAT，谷胱甘肽过氧化物酶基因CfGPX基因在机体抵抗外界微生物刺激中起到了重要的作用。

人工食物对高原鼠兔稳定性碳和氮同位素组成的影响

以玉米面、小米面和绿豆粉(质量比为5：3：2)的混合食物饲喂青藏高原地区特有种高原鼠兔，40 d后断头杀死，取其后腿肌肉测定稳定性碳和氮同位素组成。结果表明，用混合食物饲喂后，高原鼠兔的稳定性碳同位素比值显著升高，由对照的(一24．660．25)‰上升为(一19．050．09)％。；稳定性氮同位素的组成变化较小，仅由对照的(3 280．13)‰增加为饲喂后的(3．6l0．32)‰。经人工食物饲喂后，高原鼠兔与其食物间稳定性碳同位素的分馏效应为4．73‰o，稳定性氮同位素的分馏效应为2．79％e。c。组分食物的加入影响高原鼠兔的稳定性同位素(特别是氮同位素)代谢模式，其稳定性同位素代谢周转率可能高于原来预测的40 d。

青海湖鸬鹚繁殖成功率初报

2000年3～8月对青海湖西山鸬鹚岛鸬鹚（Phalacrocorax carbo）不同繁殖阶段的成功率做了初步观察。鸬鹚卵的窝卵数为3.47枚，孵化率为37.9%，雏鸟成活率为 61.1%，繁殖成功率为23.2%。孵化期的前3d，鸬鹚巢的损失率高达36.1%；育雏期前10d雏鸟损失率为25%。这些数据可看作鸬鹚种群-青海湖湿地生态系统的一个重要组分——动态监测的起始数据之一，可在未来进一步的比较分析中得到应用。

中国南方热带地区田洋玛珥湖24万年以来的气候变化及湖泊演变

A continuous long (224m) and high-resolution core TY2 was recovered from paleo-maar-lake Tianyang, tropical South China. Based on the diatom records of the upper 130-m core, this paper focuses on exploring climate change and the lake evolution history in tropical South China during the past 240ka. The most typical and unique characteristics of the diatom assemblages is that, Aulacoseira granulata was dominant or absolutely dominant species (80-90%) during most parts of the 130-m core, while Cyclotella stelligera var. tenuis and Fragilaria construens var. venter were subdominant species in only limited parts of the lower and upper core, respectively. Time scale is always the biggest problem for the study of TY2 core, so although diatom is seldom used for establishing time scale, here we attempt this by correlating the diatom-reconstructed temperature sequence with the time scale of ODP core 806B from Equatorial Western Pacific. Verified by the few most reliable ages from TY2 core and the parallel core TYl, a rather reasonable and reliable time scale was established. 01S 7/6 falls at the depth of 100m (ca. 194kaBP), OIS 6/5 at 75m (ca. 132kaBP), OIS 5/4 at 46m (ca. 75kaBP), OIS 4-3 at 35m (ca. 60kaBP). Qualitative and quantitative environmental reconstructions are made on the basis of diatom assemblage ecotype and EDDI dataset. Correlation of diatom-reconstructed temperature and moisture changes of Core TY2 with pollen-reconstructed temperature and rainfall sequence of Core TYl proves that the results are quite consistent in most periods. Thus the reconstruction results from diatom are quite reliable, and probably have a much higher resolution than pollen results. Combined with lithological and magnetic susceptibility variations, the diatom analysis reveals that, the general climate in tropical South China during the past 240ka was warm and wet. On the time scale of glacial-interglacial, warm and wet, cool and dry are not always synchronous. It was relatively warm-wet during the penultimate interglacial, cool-dry during the penultimate glacial, warm-dry during the last interglacial, and cooler-drier during the last glacial. In contrast, on the time scale of subglacial-subinterglacial scales, warm and dry, cool and wet corresponds very obviously, showing very clear 21-23 ka precession cycle. Analysis also shows that, the water of Tianyang paleo-maar-lake was generally warm, turbulent, turbid, meso-trophic, slightly alkaline, low conductivity and fresh during the past 240 kaBP, with small variations in some parts. Tianyang paleolake experienced shallow to semi-deep lake in OIS7d, open shallow lake in OIS7c-OIS5b, shallow coastal lake in OIS5a-OIS4c, swamp in OIS4b, and then completely dried up in OIS3c. The lake evolution was mainly controlled by temperature and precipitation changes in tropical China. While temperature and precipitation changes were probably controlled by the migrations of monsoon rainband and the evaporation rate, which was in turn controlled by the evolution of East Asian monsoon. Therefore, when the summer monsoon was strongest the climate was warm-dry, when stronger the climate was warm-wet; when the winter monsoon was strongest the climate was cool-dry, stronger cool-wet. This mechanism caused the warm-dry sub interglacial and cool-wet subglacial climate in the tropical South China.