辽宁省强震动台网运行与管理

本文介绍了台网的运行维护与管理情况,以及海城、伊通4．3级地震强震记录的获取情况,指出了台网现行维护方式的不足,并提出了相应的改进措施。     

Geochemical Stratigraphy and Microvertebrate Assemblage Sequences across the Silurian/Devonian Transition in South China

Carbon isotope (δ13Corg) analyses of non-marine clastic rocks and neritic carbonates and black shales spanning the Silurian/Devonian transition are compared from two richly fossiliferous sequences in Qujing of East Yunnan and Zoige of Sichuan, South China. The two sections, Xishancun and Putonggou sections in South China, reveal positive δ13Corg shifts happening in the Upper Pridoli and Lower Devonian and reaching peak values as heavy as ?25.2‰ (Xishancun) and ?19.9‰ (Putonggou) in the lowermost Lochkovian following the first occurrence of the thelodont Parathelodus and the conodont Icriodus woschmidti woschmidti (only in Putonggou Section and together with Protathyris-Lanceomyonia brachiopod fauna). These results replicate a globally known positive shift in δ13Corg from the uppermost Silurian to the lowermost Devonian. The δ13Corg variations across the Silurian/Devonian Boundary (SDB) at the two sections in South China exhibit a shift in carbon isotopic composition similar to the detailed SDB curves from the borehole Klonk-1 drilled at top of the Klonk Global Standard Stratotype-Section and Point (GSSP) in the Prague Basin, Czech Republic. In addition, four microvertebrate assemblages, including the Liaojiaoshan, Xishancun, Yanglugou and Xiaputonggou assemblages, are recognized from the Silurian/Devonian transition exposed in the Xishancun and Putonggou sections, respectively. The results from both carbon isotope stratigraphy and microvertebrate assemblage sequences suggest that the SDB in South China is located at the base of the Xishancun Formation (between sample QX-20 and sample QX-21) in the Xishancun Section and the lower part of the Xiaputonggou Formation (between sample ZP-09 and sample ZP-10) in the Putonggou Section. The isotopic trend for organic carbon together with the changes of microvertebrate remains across the SDB can offer an approach to a potential correlation of the SDB from different sedimentary facies, which help to correlate the marine with non-marine deposits.     

大气环境变化的泥炭地质档案

雨养泥炭沼泽是一种重要的泥炭沼泽类型,具有全球广泛分布的特点,其养分补给主要源于大气降水(包括雨、雪和空气尘埃).它是一个记录大气环境变化的积极的信息储备系统,记录有大气输入的海盐气溶胶、沙尘颗粒、酸沉降、重金属和有机污染物等信息.采用地质定年技术将泥炭深度剖面转化到年代坐标上,并结合泥炭生物地球化学指标检测分析,提取...     

三门湾近五十年来富营养化的沉积记录

沿海(特别是河口港湾)富营养化已成为当前海洋环境的一个突出问题.以人类活动影响下的典型海湾--三门湾为研究对象,对三门湾湾内(SM-3)及湾口(SM-17)沉积物柱状样品进行研究,采用210Pb对SM-17沉积柱进行年代测定,建立年代标尺.通过对两个沉积柱多化学指标变化特征(有机碳、总氮、总磷和生物硅分布特征、生源要素...     

川东北地区海相烃源岩中单质硫的定性与定量分析

利用定性与定量分析手段,研究了川东北地区各类海相烃源岩中的单质硫及其地球化学特征。定性分析表明,该区海相烃源岩中的单质硫具有八硫环状结构和六硫状环结构两种晶体构型,由S8和S6两种同素异形体组成,其中S8具有相对较高的丰度。定量分析表明,该区海相烃源岩中的单质硫含量为0.91×10-6～375.88×10-6,具有很宽的分布范围,并且随着烃源岩分布区域、地层时代以及岩性的不同而发生明显变化,表现出强烈的非均质性分布特征。该区海相烃源岩中单质硫含量与有机碳含量之间存在正相关关系,说明单质硫主要发育在富有机质沉积的层段中。通过单质硫含量与总硫含量对比分析,间接证明了川东北地区各类海相烃源岩中赋存有丰富的有机含硫化合物。     

Dark respiration in the light and in darkness of three marine macroalgal species grown under ambient and elevated CO2 concentrations

Dark respiration (non-photorespiratory mitochondrial respiration),which occurs both in the light and in darkness,is vital for growth and survival of algae and plays a critical role in modulating the carbon balance of them.In the present study,we have investigated dark respiration in the light (R L) and in darkness (R D) in three marine macroalgal species,Hizikia fusiformis (phaeophyta),Gracilaria lemaneiformis (Rhodophyta) and Ulva lactuca (Chlorophyta),cultured at 20℃ using aeration with two CO 2 conditions:current ambient (CO 2 concentration about 380 μl/L) and elevated CO 2 (approximately 720 μl/L) air.R L was estimated by using the Kok method,whereas R D was determined as the rate of O 2 influx at zero light.The results showed that both R L and R D were unchanged for the elevated CO 2-grown algae relative to ambient CO 2 concentration for all the algal species tested.However,R L was significantly lower than R D across all the algal species and growth CO 2 treatments,demonstrating that daytime respiration was partly depressed by the light.The percentage of inhibition of respiration by light was similar between ambient and elevated CO 2 grown algae.The ratio of respiration to photosynthesis,which tended to decrease when estimated using R L instead of R D,was not altered for the elevated relative to ambient CO 2 concentration.The results suggest that R L,rather than R D,is a more accurate estimate of nonphotorespiratory carbon loss in marine macroalgae during the daytime.It would not be anticipated that elevated atmospheric CO 2 would exert a substantial influence on respiratory flux either in the light or in darkness in these particular marine macroalgal species.     

海洋微生物偏振光散射的双组分模型

光学散射方法被广泛用于获取海洋微生物的形态和浓度信息.通过测量散射光的空间分布可以测量海洋微生物的形态和浓度;而最近发现,散射光的偏振特征却对细胞内部亚微米级散射颗粒更加敏感.把海洋微生物等效为粒径远大于入射波长的“米氏”粒子和远小于入射波长的“瑞利”粒子的混合体,以两种不同粒径的实心球作为微生物偏振光散射模型.利用蒙...     

Effect of UV-B radiation on the population dynamics of the rotifer Brachionus urceus

The effect of UV-B radiation enhancement at experimental doses of 0.00,0.24,0.48,0.72,0.96,and 1.20 kJ/m 2 on the population dynamics of the rotifer Brachionus urceus feeding on the alga Chlorella sp.was studied under controlled laboratory conditions using clonal culture and life-table techniques.The results show that UV-B radiation treatment significantly shortened the survival time of the rotifer (P <0.05): The longest survival time (336 h) occurred in the control (0.00 kJ/m 2 ) while the shortest (222 h) occurred when exposed to the highest UV-B radiation treatment (1.20 kJ/m 2 ).The fecundity of the rotifer B.urceus was enhanced by the lower UV-B radiation treatment (0.24 and 0.48 kJ/m 2 ) but inhibited by the higher treatments (0.96 and 1.20 kJ/m 2 ).Life expectancy also was obviously affected by UV-B radiation (P <0.05).The highest life expectancy occurred in the control (0.00 kJ/m 2 ),and it became shorter with increasing doses of UV-B radiation.The resutls in the present study indicate that the life expectancy of the rotifer B.urceus can be used as an indicator for UV-B radiation enhancement.     

藏南地区晚白垩世岩相古地理初步研究

通过对藏南地区上白垩统沉积特征及沉积相进行综合分析,初步地恢复了该地区晚白垩世岩相古地理.该地区自南向北沉积水体逐步变深,沉积相带展布依次为滨海相、浅海陆棚相(外陆棚和内陆棚亚相)、大陆斜坡相及深海盆地相,局部地区浅海陆棚相之上发育碳酸盐岩礁滩相和孤立台地相等.盆地性质总体上仍然为被动大陆边缘海盆,但已具备周缘前陆盆地...     

上海地学研究：从长江口到深海——中国科学院院士汪品先教授接受本刊专访

2011年8月30日下午,本刊主编、上海市地质调查研究院总工程师严学新教授,本刊编辑部主任、上海市地质调查研究院总工程师办公室副主任龚士良教授,在同济大学海洋与地球科学学院杨守业教授的陪同下,拜访了中国科学院院士、同济大学海洋与地球科学学院汪品先教授,并作了专题访谈。