中国对虾（Penaeus chinensis）维生素营养的研究──Ⅴ．中国对虾维生素C营养

提出以稳定态的ＬＡＰＰ代替一般维生素Ｃ添加在配合饲料中饲喂对虾，指出：在１００ｇ饲料中含ＬＡＰＰ４００ｍｇ时，其体长增长率和体重增重率最高，存活率最佳．饲料中ＬＡＰＰ浓度大小影响对虾的蜕壳频率和蜕壳周期，当饲料中ＬＡＰＰ缺乏时，对虾的蜕壳频率降低，蜕壳周期延长；过量的ＬＡＰＰ也会使对虾的蜕壳频率相对降低，但比缺乏或不足的要高。维生素Ｃ在对虾肝胰脏中的积累以ＬＡＰＰ含量４００ｍｇ／１００ｇ饲料组为最高。     

安徽龙河口水库沉积物碳、氮、磷地球化学记录及其环境意义

根据2004年在安徽龙河口水库采得的沉积物样芯以及上游三条主要河流的流域表层样品,对其有机碳、氮、磷含量以及其他气候代用指标进行了分析。研究发现晓天河流域样品有机碳、氮含量最高,柱样中各元素含量随深度增加缓慢变小,但在50cm深度有明显峰值出现。同时对沉积物中碳-氮和氮-磷耦合关系进行了讨论,推断其物质来源以河流携带陆源植物输入为主。其含量变化受物质来源、本身生物化学作用、人类活动等影响。     

福建太平洋牡蛎种群微卫星DNA分析

本文采用Ucdcg153、157、202微卫星引物对福建两个太平洋牡蛎(学名为长牡蛎Crassostrea gigas)养殖种群进行扩增分析和序列测定.与采自漳浦旧镇的近江牡蛎(C. ariakensis)比较,前者对以上三种引物全部呈阳性反应,后者只对Ucdcg157显阳性.与Genebank提供的相关序列比较,福建太平洋牡蛎与Genebank样品应属同源,其中漳浦霞美和厦门白礁的样品则可能代表同一种群的两个衍生品系.本项调查结果同时显示,近亲繁殖的育苗方式已经导致福建太平洋牡蛎种群裂化;任其发展不利于维护良种优势.本次采集的样品中未发现显示葡萄牙牡蛎、熊本牡蛎和美洲牡蛎微卫星特征的个体.     

Population Dynamics and Life History Characteristics of the Blue Crabs Callinectes similis and C. sapidus in Bay Environments of the Northern Gulf of Mexico

Abstract. The population dynamics and life history characteristics of Callinectes similis and C. sapidus in the Mobile Bay-Mississippi Sound estuarine system of the northern Gulf of Mexico were studied. We report that C. similis is numerically dominant in open-bays, while C. sapidus is more abundant in shallow salt marshes. Juvenile C. similis recruit into both open-bays and salt marshes, but juvenile C. sapidus primarily recruit into shallow salt marshes. Sex ratios of C. similis and C. sapidus were generally skewed towards higher proportions of males than females. Callinectes similis appears to have a life cycle similar to that of C. sapidus. Egg-carrying C. similis migrate to higher salinity waters and presumably release larvae to nearshore shelf waters; following development, the larvae re-invade estuaries as megalopae. Juvenile C. similis grow more slowly than C. sapidus. This may be attributable to reduced feeding rates. Marked differences in fecundity and reproductive effort were found between these species. Callinectes similis and C. sapidus , respectively, produced 2.4–5.5 times 10⁵ and 2.1–3.2 times 10⁶ eggs and invested 24–49 and 171–372 kJ per brood. Rhizocephalan barnacle infestation by Loxothylacus texanus was encountered in C. sapidus , while sympatric C. similis were free of this rhizocephalan parasite.     

Particulate n-alkanes and fatty acids in the Changjiang river system

Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease (0.84% ～ 1.88%) of organic carbon content from the upper reaches to the estuary.δ13C values of particulate organic carbon was in the range of -24.9×10-3 to -26.6×10-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ13C and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs (soil organic matter) among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream.     

Organic carbon fluxes from the upper Yangtze basin: an example of the Longchuanjiang River,China

To investigate the effects of anthropogenic activity, namely, land use change and reservoir construction, on particulate organic carbon (POC) transport, we collected monthly water samples during September 2007 to August 2009 from the Longchuanjiang River to understand seasonal variations in the concentrations of organic carbon species and their sources and the yield of organic and inorganic carbon from the catchment in the Upper Yangtze basin. The contents of riverine POC, total organic carbon and total suspended sediment (TSS) changed synchronously with water discharge, whereas the contents of dissolved organic carbon had a small variation. The POC concentration in the suspended sediment decreased non‐linearly with increasing TSS concentration. Higher molar C/N ratio of particulate organic matter (average 77) revealed that POC was dominated by terrestrially derived organic matter in the high flows and urban wastewaters in the low flows. The TSS transported by this river was 2.7 × 10⁵ t/yr in 2008. The specific fluxes of total organic carbon and dissolved inorganic carbon (DIC) were 5.6 and 6 t/km²/yr, respectively, with more than 90% in the high flow period. A high carbon yield in the catchment of the upper Yangtze was due to human‐induced land use alterations and urban wastes. Consistent with most rivers in the monsoon climate regions, the dissolved organic carbon–POC ratio of the export flux was low (0.41). Twenty‐two percent (0.9 t/km²/yr) of POC out of 4 t/km²/yr was from autochthonous production and 78% (3.1 t/km²/yr) from allochthonous production. The annual sediment load and hence the organic carbon flux have been affected by environmental alterations of physical, chemical and hydrological conditions in the past 50 years, demonstrating the impacts of human disturbances on the global and local carbon cycling. Finally, we addressed that organic carbon flux should be reassessed using adequate samples (i.e. at least two times in low‐flow month, four times in high‐flow month and one time per day during the flood period), daily water discharge and sediment loads and appropriate estimate method. Copyright © 2011 John Wiley & Sons, Ltd.     

Permineralization process promotes preservation of Holocene macrofossil charcoal in soils

The use of macrofossil soil charcoal as a palaeoecological tool to reconstruct past vegetation, climate or fire history has gained much interest in recent years. Yet little is known about taphonomy of charcoal in soils. Here we assessed the putative loss of palaeoecological information due to charcoal fragmentation after burial. We found no significant loss of charcoal mass with time. Instead, we found a significant positive relationship between the mass of charcoal particles and their age. Permineralization of charcoal particles older than ca. 5200 a explained the increased charcoal mass with time in mineral soils. The permineralization process increased the density of charcoal particles (resulting in a twofold particles mass increase) and thus offers a protection against subsequent degradation. Our results suggest high stability of palaeoecological information from charcoal macrofossils buried in mineral soils at least over the Holocene timescale. Copyright © 2011 John Wiley & Sons, Ltd.     

C8051F330在地震观测系统中的应用

介绍基于C8051F330单片机的地震观测系统中故障报警子系统的工作原理,并对温度报警设计中的问题进行分析。