鄂尔多斯晚三叠世湖盆特征恢复及地质意义

研究了鄂尔多斯晚三叠世湖盆古气候变迁及古水体特征.研究结果表明:鄂尔多斯晚三叠世湖盆古纬度为北纬31.03°,比现在所处的纬度35.10°偏南4°多,推测晚三叠世时鄂尔多斯湖盆气候温暖潮湿,生物繁盛,能够形成有机质丰富的烃源岩.利用泥岩B,Sr,Ba元素测试结果及Sr,Ba质量分数比值法,以及岩石碳酸盐岩胶结物稳定同位素分析表明,鄂尔多斯晚三叠世长8期-长6期湖盆是一个淡水湖盆,长8期-长7期-长6期湖盆水体范围与深度经历了收缩-扩大-收缩的过程,纵向上构成了储层-烃源岩-储层的生储盖组合,从湖盆演化的特征上论证了鄂尔多斯盆地晚三叠世油气勘探的实际意义.     

A new Euprox from the Late Miocene of Yuanmou,Yunnan Province,China,with interpretation of its paleoenvironment

The Yuanmou Basin of Yunnan Province is a hotspot for the research of early homind evolution and its environmental background.During the implementation of the Program“Research of the Origin and Evolution of Early Man and Its Environmental Baqckground” from 1998 to 2001,a huge quantity of hominoid and mammal fossils were collected.The present report systematically describes an Euprox robustus sp.nov.identified during the recent laboratory work on the collected material.Euprox is a group of earliest cervids with true antlers.The new species is the third one of the genus discovered in China.Judged by its morphologic characteristics,the new species feed on juicy and tender leaves of dicotyledon.It implies that the vegetation of its epoch in the Yuanmou Basin is a kind of southern subtropical evergreen forest and the climate is humid and temperate with evident seasonality.The latter is mostly influenced by the monsoon and secondly by the latitude.     

马铃薯晚疫病防治的药剂筛选试验研究

2007年在凉山州冕宁县马铃薯主产区开展了687．5g／L银法利SE、70%安泰生WP、58％甲霜灵．锰锌WP、25％甲霜灵WP四种杀菌剂防治马铃薯晚疫病的田间药效试验。试验表明,四种药剂对马铃薯晚疫病均有有明显的防治效果,其中687．5g／L银法利SE防病增产效果最佳。     

龙潭楔叶的再研究——兼论华南晚泥盆世楔叶目的演化

基于安徽省巢湖市狮子口剖面上泥盆统（法门阶）五通组的标本,对龙潭楔叶Sphenophyllum lungtanense Gothan et Sze的叶形和脉式等重要特征取得了新认识。华南晚泥盆世楔叶目的起源和演化分异模式不同于劳俄大陆的同类植物,它们兼有原始和进化的营养器官（枝状、线状或片状叶）和生殖器官（缺少或具有孢子叶）,显示出较高的形态多样性和镶嵌演化。     

秦岭晚古生代增生弧前盆地的热水成矿系统

目的探讨中秦岭地区铅锌金多金属矿集区的成矿地质背景和成矿机制。方法从板块构造角度进行分析。结果位于商丹带与留坝—山阳断裂带之间的中秦岭地区,其主体是在华北南缘晚古生代活动陆缘环境下增生的一个介于秦岭古岛弧带和留坝—山阳古俯冲带（古海沟）之间,并建立在俯冲增生楔之上的弧前盆地,发育有大规模的热水成矿系统。结论该区是横亘中国大陆中部的中秦岭岷礼—西成—凤太—山柞大型—超大型金、铅锌多金属矿集区。     

Benthic foraminiferal fauna turnover at 2.1 Ma in the northern South China Sea

Quantitative analysis of benthic foraminifera from ODP Site 1146 in the northern South China Sea (SCS) shows that abundance of Bulimina alazanensis, sometimes up to about 90%, decreased gradually since 3.2 Ma, especially at 2.1 Ma. Abundance of other benthic foraminiferal species, Globobulimina sub-globosa and Cibicidoides wuellerstorfi, increased after 2.1 Ma. Comparison with changes in oxygen and carbon isotopes of planktonic and benthic foraminifera shows that high abundance values of B. alazanensis corresponded with lower values of oxygen isotope, but for carbon isotope, high values of the species were consistent with heavier carbon isotope of benthic foraminifera and lighter carbon isotope of planktonic foraminifera, respectively, and vice versa. Considering factors such as uplift of Bashi Strait, expansion of the North Hemisphere Glaciation, strengthening of East Asian winter mon-soon and variations in oxygen and carbon isotope of foraminifera, changes of B. alazanensis in ODP Site 1146 suggest that the source of deep water masses of the northern South China Sea changed from the warm Pacific deep water with high oxygen content to Pacific Intermediate water with low oxygen content at 2.1 Ma. In addition, the strengthened East Asian winter monsoon resulted in increased pri-mary productivity, high nutrient and suboxic bottom water. Variations in species of B. alazanensis seemed to be unable to tolerate environmental stress induced by deep water masses and productivity changes.