秦岭植物区系一新种和一新记录种

1　秦岭丁毛荚艹迷迷(忍冬科Ｃａｐｒｉｆｏｌｉａｃｅａｅ),新种(图1)ＶｉｂｕｒｎｕｍｖｅｒｓａｔｉｌｅＲＨＭｉａｕ,ＷＢＬｉａｏｅｔＱＹＳｕｎ,ｓｐｎｏｖ常绿灌木.嫩枝有钝棱,薄被丁字毛,老枝圆形,几无毛.叶薄革质,卵形,长35～57ｃｍ,宽25～35ｃｍ,顶端渐尖,基部?..     

秦岭佛坪穹隆盖层岩系的地质和地球化学特征

地质和地球化学研究表明,佛坪穹隆盖层岩系主要由晚震旦—晚古生代地层组成,呈变质程度不等的变质岩产出,构成以佛坪基底杂岩为核心的中心式递增变质带。认为该岩系经历了多期构造变形,与穹隆核部基底杂岩以剪切带或断层接触,其原岩为陆源碎屑岩－碳酸盐岩组合,形成于扬子板块北缘的被动大陆边缘（Ｚ２－Ｐｚ１）和秦岭微板块内的陆表海（Ｐｚ２）沉积环境。     

秦岭植物区系的特有现象研究

秦岭有中国种子植物特有属４７属,含６１种,现代地理分布呈现出西南－华中－华东分布型最多,华中－华东分布型和西南－华北分布型次之,华北分布型和横断山－藏南分布型最少。分布于秦岭的中国特有属植物主要处于中海拔地带,且西段和南坡较东段和北坡我,显示出温带性质。     

Discovery of the highly depleted N-MORB-type volcanic rocks: new evidence for the Mianlue paleo-ocean

The highly depleted N-MORB-type volcanic rocks have been discovered in Mianlue mélange of Qinling orogenic belt, central China. These mafic rocks are associated with the meta-peridotites, showing LREE-depleted pattern, similar to N-MORB and typical ophiolites. It is indicated that an ancient ocean existed in the Mianlue area of Qinling orogenic belt during the late Paleozoic.     

南秦岭西亚带碳硅泥岩型铀矿化与沉积环境分析

碳硅泥岩型铀矿为沉积内生型,具有明显的层控特征,沉积相与铀矿化关系往往是碳硅泥岩型铀矿床的研究重点.南秦岭西亚带碳硅泥岩型铀矿床的成因类型主要为沉积-热液叠加改造型,赋矿层位仅局限于中、下志留统炭硅质、泥质的富铀地层中.通过对研究区区域地质背景,沉积环境以及有利沉积相对铀成矿的控制作用研究,指出碳酸岩台地中发育的水下坳陷相整体控制着铀矿化的分布,而坳陷相中发育的硅灰岩透镜体是铀矿化定位的前提.     

U-Pb dating of detrital zircons from the Wudangshan Group in the South Qinling and its geological significance

U-Pb dating was made by the LA-ICP-MS method for detrital zircons from the Wudangshan volcanic-sedimentary succession in the South Qinling. Samples comprise quartz sandstones of the Wudangshan Group collected from the base of the Yangping Formation and an upper layer of the Shuangtai Formation overlain its volcanic sequence, and two river-sand collections from the drainage systems cutting across the two formations, respectively. The results show that the Yangping detrital zircons are dominated by 830–780 Ma grains with a minor population of ~1.0–0.84 Ga and sporadic grains of ~2.6, ~2.4 and 2.0 Ga, whereas the Shuangtai zircons yield an upper intercept age of 763±33 Ma, identical to the timing of the Wudangshan volcanism within error, with few concordant grains of 1.9 and 0.86 Ga. Age spectra for the two river-sand samples are similar to those of the Yangping and Shuangtai Formations, respectively. It thus suggests that the Wudangshan strata are less than 780 Ma, whereas their major detrital zircon populations of 1.0–0.85 Ga and 830–780 Ma are consistent with timing of the Hannan magmatic activities along the northwestern margin of the South China Block. This suggests a Hannan or adjacent area provenance for the Wudangshan strata. The Wudang area is characterized by rift-related igneous events at ~755 and ~680 Ma, respectively, pointing to a tectono- magmatic history different from the Hannan area. It is inferred that the ~755 Ma magmatism is likely to indicate a separation of the South China Block from the supercontinent Rodinia, while the ~680 Ma event suggests a further split between the South Qinling and some unknown continent.     

秦岭铅锌矿冶炼厂区周边土壤重金属分布特征研究

目的为了解铅锌过程中重金属对周边土壤的污染情况。方法对秦岭凤县铅锌矿冶炼厂周边8个区域土壤中Zn、Pb、Cd、Cu等4种主要重金属的分布规律进行了初步研究,分析了冶炼厂周边环境现状,提出了对策建议。结果研究表明冶炼厂周边土壤重金属污染严重,绝大部分区域重金属含量已超过对照点测定值和国家土壤环境质量二级标准,最高超标倍数依次为Zn10倍、Pb6．5倍、Cd6．2倍、Cu4．0倍。结论厂区常年主导下风向土壤中重金属含量高于上风向土壤中;冶炼厂周边土壤环境中重金属污染以Zn为主,其次为Pb和Cd,Cu污染较小。     

秦岭柞水岩体和东江口岩体的锆石U-Pb 年代学及其意义

柞水岩体和东江口岩体位于秦岭造山带南秦岭构造域, 主要由似斑状花岗闪长岩和二长花岗岩组成。通过LA-ICP-MS 锆石U-Pb 同位素定年, 结合锆石阴极发光图像, 揭示柞水岩体的似斑状二长花岗岩(样品ZS01-01)存在两个谐和年龄, 分别为209±2和199±2Ma;东江口岩体似斑状二长花岗岩(样品ZS04-01)也存在两个谐和年龄, 分别为219±2 和209±2 Ma。结合前人的地球化学和区域构造背景研究, 判定这两个岩体属于同一岩浆事件的不同阶段侵位, 东江口岩体的似斑状二长花岗岩侵位结晶略早于柞水岩体, 柞水岩体主期岩浆侵位时, 东江口岩体也有同期岩浆侵位结晶。这两个岩体年龄的准确测定, 表明在219 ～199 Ma 期间沿商丹断裂有3个阶段的构造-岩浆活动。     

四川兽类新纪录——秦岭鼢鼠线粒体Cyt b基因的克隆及其比较研究

为揭示2003年在王朗采集的鼢鼠标本王03001号是否为秦岭鼢鼠四川兽类新纪录,以鼢鼠标本王0300号的肌肉组织为研究材料,运用PCR技术对其线粒体Cyt b基因进行克隆和测序．结果表明该基因的长度为1140bp,编码380个氨基酸的蛋白质,所编码的蛋白质含有2个N-糖基化位点,1个蛋白激酶C磷酸化位点,4个酪蛋白激酶Ⅱ磷酸化位点,6个N-豆蔻化位点．再以已研究的鼢鼠6个种18个体Cyt b基因序列及氨基酸序列为基础数据,把中华竹鼠（Rhizomys sinensis）作为外群,结合本研究的结果构建系统发育树,所得结果不支持王03001号标本为秦岭鼢鼠．