盐度对牙鲆非特异性免疫功能的影响

实验以健康牙鲆成鱼为研究对象，分别饲养于盐度为40，30(对照组)，20的海水中，以牙鲆血清的凝血活性、溶菌酶含量以及补体因子C3含量为指标，研究盐度对牙鲆非特异性免疫功能的影响。结果表明，盐度增加或降低3d后血清凝血活性升高4倍，并一直保持至12d不变；溶菌酶含量先是升高，在第5天达到高峰后又逐渐降低，至第12天的含量反而略低于对照组；C3的含量在第一天取样时就比对照组有了很大的增长，随后逐渐下降，在第7天后恢复正常。盐度变化导致牙鲆非特异性免疫因子变化，说明在养殖生产中维持稳定环境极为重要。     

Antioxidant enzyme activities in different genders and tissues of amphioxus Branchiostoma belcheri tsingtauense

Information regarding antioxidant enzymes in amphioxus remains lacking, and this study was carried out to examine the activities of superoxide dismutase (SOD), catalase (CAT) and glutathione peroxidase (GPX) in different genders and tissues of amphioxus Branchiostoma belcheri tsingtauense. Results show that (1) CuZn-SOD, CAT and GPX activities in the whole amphioxus B. belcheri tsing- tauense were basically at the same levels in male and female amphioxus, whereas both T-SOD and Mn-SOD activities in male amphioxus were significantly higher than that in the female (P<0.05); (2) The testis had significantly higher T-SOD and CuZn-SOD activities than the ovary (P<0.05); (3) CuZn-SOD activity was undetectable in the guts of male and female amphioxus; (4) For both male and female am- phioxus, the activities of CAT and GPX in the gonads including testis and ovary were the lowest (P<0.05) among the tissues examined; (5) The gut and gill had the same level GPX activities while the gut had a higher CAT activity; (6) There was no clear difference in CAT and GPX activities in the corresponding tissues between male and female amphioxus. The study on SOD, CAT and GPX activities in different genders and tissues of the protochordate provides data for future comparison of amphioxus antioxidant enzymes with those of invertebrates and vertebrates.     

辽宁IaB、IaAB混合型金刚石的发现及其生长结构特征

利用显微红外光谱区域扫描,在辽宁50号岩筒产出的金刚石中发现1粒IaB、IaA混合型金刚石,且IaB、IaAB间存在明显的界线.DiamondView荧光图像观察显示,该粒金刚石呈不规则的同心圈层生长结构,并可分为两个生长阶段,生长结构特征能够与显微红外光谱分析获得的结果相互验证.样品氮、氢含量的规律及变化趋势分析结果表明,样品不同阶段生长环境变化大,且出现明显的生长停顿,也验证了金刚石由A中心逐渐向B中心的转化过程.该金刚石的发现对研究金刚石生长过程中地质环境的变化具有重要意义.     

陕西凤太矿集区铅锌矿床的成矿模型及其找矿意义

陕西凤太(凤县-太白)矿集区是南秦岭铅锌金多金属成矿带的重要组成部分,区内发育7个大中型铅锌矿床以及许多小型矿床(点)。关于铅锌矿床成因前人提出了多种观点,这些成因认识的根本分歧在于是同生成矿还是后生成矿,是一期成矿还是两期成矿。多年来笔者在凤太矿集区开展了比较全面的研究工作,文章综合这些研究成果,并结合近十年来有关的区域地质、矿产研究和找矿勘查工作等方面的新进展,系统论述了铅锌成矿地质特征、控矿因素、成矿流体和成矿元素来源,厘定成岩成矿时代和成矿动力学背景,建立成矿模型,并提出新的找矿方向。笔者认为凤太矿集区铅锌矿床形成于晚三叠世秦岭造山运动的后碰撞阶段,是区域大规模构造变形变质-岩浆作用-流体活动的产物,是同一期成矿事件中后生成矿流体在不同构造扩容空间充填交代形成不同矿化类型铅锌矿体,共同组成了一个多源流体成矿系统。根据成矿模型,提出了中泥盆世古道岭组灰岩的内部及灰岩与中酸性岩体接触带附近是今后深部找矿勘查的新目标。