三小定点整脊技术治疗青少年颈椎病40例临床观察

目的：探究三小定点整脊技术治疗青少年颈椎病的临床疗效。方法：将青少年颈椎病患者80例随机分为治疗组和对照组,每组各40例。对照组采用推拿治疗,治疗组采用三小定点整脊治疗。比较2组的综合疗效、疼痛程度与颈椎生理曲度的改变情况。结果：总有效率治疗组为95.0%（38/40）,高于对照组的75.0%（30/40）,2组比较,差异有统计学意义（P＜0.05）。2组疼痛评分、颈椎生理曲度治疗前后组内比较及治疗后组间比较,差异均有统计学意义（P<0.05）。结论：三小定点整脊技术可减轻青少年颈椎病患者颈肩疼痛及头晕、头痛症状,并恢复其生理曲度,临床疗效显著。     

斜带髭鲷(Hapalogenys nitens)血细胞发生及外周血细胞化学染色观察

通过Wright-Giemsa染色对斜带髭鲷[Hapalogenys nitens (Richardson)]的头肾、体肾、脾脏、肝脏四组织涂片、印片的观察,发现其头肾、体肾、脾脏是其主要的造血器官。头肾能发育生成各类型血细胞,体肾能生成红细胞和粒细胞,脾脏能生成淋巴细胞和红细胞。肝脏中未发现幼稚型血细胞。血细胞发生大致经过原始、幼稚和成熟三个阶段。细胞化学染色显示:外周血细胞中,除淋巴细胞外,均有糖原;嗜中性粒细胞含有ACP、ALP、NACE、αNAE和POX;嗜酸性粒细胞含有ACP、NACE和POX;单核细胞含有ACP、αNAE和POX;小淋巴细胞有ACP。研究发现斜带髭鲷是一种抗病能力较强的鱼类。血细胞组织化学染色可作为斜带髭鲷疾病诊断的辅助手段。     

粤西海陵湾养殖区邻近海域大型底栖动物生态学特征

根据2014—2016年粤西海陵湾养殖区湾内和湾外邻近海域21°27′—21°38′N、111°42′—111°57′E 4个航次调查资料,对其大型底栖动物生态学特征进行了研究。结果表明,共鉴定大型底栖动物64种,春季种类最多为39种,秋季最低为17种。4季均以环节动物种类数最多,软体动物次之。不同季节间优势种有所差异,仅倍棘蛇尾Amphioplus sp.为周年优势种。春、夏、秋和冬季第一优势种分别为倍棘蛇尾、菲律宾蛤仔Ruditapes philippinarum、短吻铲荚螠Listriolobus brevirostris和平蛤蜊Mactra mera。平均丰度和生物量分别为213ind./m~2和15.4g/m~2,其中丰度以春季最高为248ind./m~2,夏季最低为167ind./m~2,而生物量则以秋季最高为28.0g/m~2,春季最低为2.4g/m~2;平面分布总体呈现湾外高于湾内的趋势。底栖动物Pielou均匀度和Shannon-Wiener多样性指数分别为0.95—1.00和1.56—4.07,其中时间分布规律明显,春季最高,秋季最低;空间上,两者无明显分布差异。群落结构时空差异显著,为沉积物类型、水深、底层无机氮和悬浮物以及捕食压力等因素共同影响的结果。     

Newly discovered hydrothermal fields along the ultraslow-spreading Southwest Indian Ridge around 63°E

The ultraslow-spreading Southwest Indian Ridge(SWIR) to the east of the Melville fracture zone is characterized by very low melt supply and intensive tectonic activity. Due to its weak thermal budget and extremely slow spreading rate, the easternmost SWIR was considered to be devoid of hydrothermal activity until the discovery of the inactive Mt. Jourdanne hydrothermal field(27°51′S, 63°56′E) in 1998. During the COMRA DY115-20 cruise in2009, two additional hydrothermal fields(i.e., the Tiancheng(27°51′S, 63°55′E) and Tianzuo(27°57′S, 63°32′E)fields) were discovered. Further detailed investigations of these two hydrothermal sites were conducted by Chinese manned submersible Jiaolong in 2014–2015. The Tiancheng filed can be characterized as a lowtemperature(up to 13.2°C) diffuse flow hydrothermal field, and is hosted by fractured basalts with hydrothermal fauna widespread on the seafloor. The Tianzuo hydrothermal field is an inactive sulfide field, which is hosted by ultramafic rocks and controlled by detachment fault. The discovery of the three hydrothermal fields around Segment #11 which receives more melt than the regional average, provided evidence for local enhanced magmatism providing heat source to drive hydrothermal circulation. We further imply that hydrothermal activity and sulfide deposits may be rather promising along the easternmost SWIR.     

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.     

2009—2012年泉州湾大型底栖生物多样性研究

文章根据2009—2012年泉州湾4个航次的调查资料,对比分析了4年间大型底栖生物的种类数、生物量、栖息密度、生物多样性的变化趋势。结果表明：泉州湾大型底栖生物有103种,其中多毛类48种,软体动物25种,甲壳动物18种,棘皮动物6种和其他动物6种。多毛类、软体动物、甲壳动物占总种数的88.3%,三者构成大型底栖生物的主要类群。泉州湾大型底栖生物平均生物量为7.77 g/m2,平均栖息密度76个/m2;数量组成,生物量以甲壳动物居首位2.40 g/m2;栖息密度以多毛类占第一位38个/m2。泉州湾大型底栖生物种类数、生物量、栖息密度、生物多样性均为湾中部及湾外较好,湾顶较差;从2009—2012年际变化来看,生物种类数、平均生物量、平均栖息密度均为2009年最好,2012年相对较差,生物多样性年际变化不大,说明泉州湾的大型底栖生物环境受到了一定的影响。     

鲁西孟家屯一种细粒斜长角闪岩的锆石SHRIMP年代学

在对鲁西孟家屯地区一种细粒斜长角闪岩变质侵入体的矿物岩相学和锆石微区特征研究的基础上,通过锆石离子探针测定获得了2604±11Ma的变质作用年龄。结合孟家屯岩组的年龄资料和鲁西地区的岩浆活动时代特征,认为鲁西地区在2.65~2.6Ga时期是一个强烈的构造活动时期,与同时期华北地台其他地区的构造活动有很大的差异,具有其独特的地质演化历史。     

池塘养殖脊尾白虾(Exopalaemon carinicauda)感染血卵涡鞭虫的研究

通过现场取样、显微镜检、细菌培养、组织病理、电镜观察以及PCR检测等研究手段,对2008年9月浙江省舟山市普陀区某梭子蟹养殖塘混养的脊尾白虾"白浊病"进行了系统的病原学研究。结果表明,病虾体色发白,反应迟钝,血淋巴液呈浊白色,严重患病白虾血淋巴中的血细胞几乎没有或者极少,代之以大量与血细胞形似的寄生虫;组织病理切片及电镜观察发现,病虾心脏、肝胰腺、肌肉、鳃部等组织寄生有大量单细胞寄生虫,该寄生虫虫体形态特征、显微结构及宿主临床症状与本实验室之前研究报道的感染三疣梭子蟹和锯缘青蟹的血卵涡鞭虫类似;采用已建立的针对血卵涡鞭虫ITS1基因的引物对"白浊病"病虾的血淋巴样品进行PCR检测,可扩增出585bp左右的特异条带。综合以上研究结果,确定该寄生虫为血卵涡鞭虫(Hematodinium sp.)。有关脊尾白虾感染该寄生虫的报道在国内外尚属首次。     

胡安·德富卡洋脊因代沃段热液黑烟囱体成矿物质来源:硫同位素的限制

选取胡安·德富卡洋脊(Juan de Fuca Ridge,JDFR)因代沃(Endeavour)段的17个热液黑烟囱体样品对其中的硫同位素进行分析测定,讨论了因代沃段热液活动区内黑烟囱体成矿的物质来源、将硫同位素数据与已发表的热液流体及硫化物数据耦合,并结合前人的成果得到如下认识:(1)因代沃段硫化物的硫同位素组成与其他无沉积物覆盖的洋脊硫化物硫同位素组成相似,然而其相比于南胡安·德富卡洋脊(South Juan de Fuca Ridge,SJFR)硫化物亏损重同位素;(2)结合前人研究成果,如果SJFR硫化物的硫全部来自基底玄武岩的淋洗与海水中的硫酸盐,那么因代沃段硫化物的硫可能有1%~3%来自沉积物的贡献,故提出因代沃段成矿系统中的硫来源主要来自基底玄武岩,同时伴随有少量海水硫酸盐来源及沉积物来源的硫加入;(3)将硫同位素数据与已发表的热液流体及硫化物数据进行耦合发现热液流体中的沉积物信号与硫化物中的硫可能来自不同的源,并提出沉积物端元可能位于下渗区。     

The relationship between soft-bottom macrobenthic communities and environmental variables off Ningjin, eastern Shandong Peninsula

Macrobenthic infauna and associated environmental factors influencing the benthic community in the eastern coastal region of Shandong Peninsula were analyzed in four seasonal surveys from January 2007 to October 2007 (30 stations in winter, 20 stations in other three seasons), in order to understand the community structure and the factors unfluencing the benthic distribution. PRIMER 6.0 and SPSS 15.0 software packages were adopted to analyze the environmental and macrobenthic data. The results show that there were 260 macrobenthic species in total collected from the research region. The composition of species is:Polychaeta (94 species), Crustacea (75), Mollusca (56) and Echinoderm (12), among which, only 23 species were common species in the cruises of every season. The dominant species varied from season to season; however, the polychaete species Paralacydonia paradoxa Fauvel and Echinoderm species Amphioplus japonicus (Matsumoto) were always present year-round. The abundance and biomass of the macrobenthos in the research region were variable from season to season. The results of CLUSTER and MDS analysis show that the similarities of macrobenthic structures between the stations were low; most of the similarities were at about 30% of similarity value, only two stations were up to 70%. In accordance with the similarity values of the macrobenthic structures, we divided the 20 stations into five groups by arbitrary similarity level of 30%. The ABC curve indicates that the marcofauna communities in the research region had not been disturbed massively, except two stations, SB1 and SB3. Ecologically, benthos were controlled by a combination of factors such as salinity, phytoplankton, zooplankton, SiO₃-Si and temperature, and no single factor could be considered as an ecological master factor.