广东电白浮标污损生物生态研究

本文根据1985年对广东电白沿岸浮标进行污损生物调查的结果,报道了该海域污损生物的种类组成、附着厚度、覆盖面积和湿重。共获得92种生物,优势种是Balanus reticulatus和Brahcidontes variatiIis。大部分浮标都完全被污损生物所覆盖,附着厚度为8-15mm,湿重3.8-14.7kg/m2。浮标侧面、底部及尾管内的污损生物群落有一定的差别。位于港内、港口和港外的浮标,其污损生物群落也不同,布放于海中一年的浮标,污损生物群落已接近顶级,二年浮标的污损生物群落有所衰退。     

甘肃北山造山带红石山地区正εNd(t)值花岗质岩石的成因及地质意义

在1：5万红岭幅等3幅区域地质调查中，对晚古生代中酸性侵入岩和火山岩的Sm—Nd同位素研究表明，这些不同时代、不同类型的岩石，均表现出高的正εNd（t）值和较低的TDM值，而且变化范围很小，揭示该区花岗质岩石的源岩同位素成分均一，且主要来源于地幔。正εNd（t）值花岗质岩石的存在，可能对研究大陆地壳生长具有重要意义。     

发展基于IPv6的地震传感器网络是科技自主创新的实践

IPv6的网络架构为传感器网络的发展创造了良好的环境，基于IPv6的地震传感器网络已列为CNGI（China Next Generation Intemet）具有行业特色的，在中国下一代互联网示范项目中的应用项引。以科学的发展观研究和发展基于IPv6的地震传感器网络，是贯彻十六届五中全会精神，科技自主创新的实践；是推进地震监测和预报进一步发展的重要契机；我们需要认真努力，为我国下一代互联网建设和防震减灾事业做出贡献。[编者按]     

白令海大型底栖动物群落结构及其空间分布格局

Due to its unique geological location, the Bering Sea is an ideal place to investigate the water exchange and ecosystem connectivity of the Pacific Ocean–Arctic Ocean and subarctic–Arctic region. Based on a number of summer surveys(July to September, 2010, 2012 and 2014), macrobenthic communities and their spatial-temporal patterns are exhibited for the majority of the Bering Sea(53°59′–64°36′N). The results show that the macrobenthic communities were dominated by northern cold-water species and immigrant eurythermic species, and the communities assumed a dispersed and patchy distribution pattern. Polychaetes(Scoloplos armiger), crustaceans(Ceradocus capensis) and sea urchins(Echinarachnius parma) were the main dominant groups in the shallow shelves; the sea star(Ctenodiscus crispatus) and the brittle star(Ophiura sarsii) were the main dominant groups in the continental slope; whereas small polychaetes(Prionospio malmgreni) dominated the basin area. Sediment type, water depth, and currents were the major factors affecting the structure and spatial distribution of the macrobenthic communities. Compared with other seas, the shallow areas of the Bering Sea showed an extremely high-standing biomass. In particular, the northern shelf area(north of St. Lawrence Islands and west of 170°W),which is primarily controlled by Anadyr Water, is an undersea oasis. In contrast, a deficiency in the downward transport of particulate organic carbon has resulted in a desert-like seabed in the basin area. By comparing our results to previous studies, we found that macrobenthic communities of the Bering Sea have undergone significant structural changes in recent decades, resulting in a decrease in abundance and an increase in biomass.In addition, populations of amphipods and bivalves in the northern shelves have decreased significantly and have been gradually replaced by other species. These changes might be associated with advanced seasonal ice melting,changes in organic carbon input, and global warming, indicating that large-scale ecosystem changes have been occurring in the Bering Sea.     

世界区域含水层演化地质控制

“Source du (?)ez”岩溶含水层系统(北蒙皮立(North Montpellieran)岩溶区-Franle S.E.)是内陆类型的岩溶含水层系统演化的地质控制的例子。岩溶含水层系统的演化主要受气候(和古气候)、地质和生物的控制。气候控制水进入岩溶含水层系统后,地质就成了主要的控制因索。地质控制包括: 1.岩性(和古沉积岩相)控制; 2.构造控制; 3.地形雕塑作用和其平面控制; 4.其它地质控制(电磁的,变质的,火山的)