中国球状绿藻新纪录属-索囊藻属(Choricystis)     

朱欢  宋会银  王清华  胡愈炘  胡征宇  刘国祥 《海洋与湖沼》2016,47(6):1116-1125

在西藏那曲的错鄂和湖北武汉的紫阳湖采集到两株淡水绿色海绵。形态观察显示,两株海绵呈现绿色是由于其内共生有球状绿藻。基于形态观察和分子系统发育分析确定为该球状绿藻为索囊藻属的寄生索囊藻(Choricystis parasitica(K.Brandt)Pr?scholdDarienko)。结果表明:(1)两株藻均为纺锤形或倒卵形,长1.2—2.8μm,宽0.8—1.5μm;具一个侧位片状色素体;(2)依据18S r DNA和rbc L cp DNA的进化分析显示这两株藻均位于胶球藻科(Coccomyxaceae),索囊藻属(Choricystis);(3)基于ITS2的二级结构分析显示这两株藻与寄生索囊藻具有相同的二级结构,表明这两株内共生的球状绿藻均为寄生索囊藻。寄生索囊藻为中国新纪录种,所在属索囊藻属为中国新纪录属。本研究以形态性状和分子性状描述了采自中国的寄生索囊藻标本,为今后研究提供依据和参考。  相似文献   

Diurnal and tidal patterns of carbon uptake and calcification in geniculate inter‐tidal coralline algae          下载免费PDF全文

Sophie J. McCoy  Catherine A. Pfister  Gerard Olack  Albert S. Colman 《Marine Ecology》2016,37(3):553-564

Research on coralline algal responses to ocean acidification and other environmental stressors has increased in recent years as coralline algae is thought to stand a higher chance of being affected by acidification stress than other macroalgae. To provide context and enhance the existing eco‐physiological framework for climate change studies, it is important to understand the effects of non‐extreme stressors experienced regularly by inter‐tidal coralline algae. In this study, we tested the potentially interacting effects of diurnal and tidal treatments on calcification in the geniculate coralline algae Corallina frondescens and Corallina vancouveriensis using ¹³C‐labeled bicarbonate. Both species deposited more calcium carbonate during the day than at night, and also when submerged (high tide) compared with when emerged (low tide) in their apical and mature segments (intergenicula). These results indicate that inter‐tidal coralline algae do in fact pay a cost for living inter‐tidally at the edge of an adaptive zone.  相似文献   

太平洋中部富REY深海沉积物的地球化学特征及化学分类     

朱克超  任江波  王海峰 《地球学报》2016,37(3):287-293

赋存于深海沉积物中的稀土资源是一种潜在的稀土资源。对太平洋中部30个重力活塞柱状样中的1 275个深海沉积物样品的常量、稀土化学分析数据进行了系统研究。在涂片鉴定的基础上,采用Ca O和Al2O3含量把太平洋中部深海沉积物划分为钙质软泥类沉积物、硅质软泥类沉积物、深海黏土类沉积物三种成因类型;这三种类型沉积物的稀土分布模式相似,表现为明显的Ce负异常,一定程度的重稀土元素富集和Y正异常,深海黏土类沉积物的ΣREY明显偏高。采用主要元素(包括Ca O/P2O5比值)与REY的关系图可以有效地判别不同成因类型沉积物的混合状况。太平洋中部富P、富含沸石的深海黏土类沉积物是最有利的富REY的深海沉积物类型。太平洋中部深海沉积物REY富集的主要原因是由于深海沉积物中混入了过量的(鱼牙骨碎屑状)磷灰石组分,而钙质生物组分和硅质生物组分的加入对REY含量起了明显的稀释作用。  相似文献   

自然和人类活动作用下月湖沉积物有机质来源及其演变   总被引：2，自引：0，他引：2  

赵宁  杨旸  高建华  刘毅飞  蔡廷禄  贾建军 《地球化学》2014,(4):365-374

潟湖海湾可以保存环境演化和人类活动的良好记录,碳氮元素含量及同位素特征可用来有效地反演这些演化。对位于山东半岛的月湖柱状样和沿岸表层样总有机碳、总氮、稳定碳氮同位素的分析表明,陆源物质对月湖沉积物和有机质的贡献很小,其沉积物中有机质的主要来源是维管植物大叶藻和各种海洋藻类。在2002年前大约140 a的沉积历史中,大叶藻对沉积物有机质的贡献比例呈上升趋势,其中在约1930年和1980年有两次明显的上升,前者可能因为种群的快速繁育,后者则可能是1979年口门筑坝后由于湾内环境恶化,大叶藻开始大量死亡的表现。月湖海洋藻类的有机碳埋藏通量在沉积记录中保持相对稳定,而大叶藻则增加了一倍,但两者都有一定程度的波动。研究结果表明自然环境演变（如沙嘴生长、口门缩小）和人类活动（如筑坝、修筑虾池）对月湖生态环境及有机碳埋藏的影响在沉积物中有清晰的记录。  相似文献   

高光谱遥感数据藻类信息提取方法研究     

赵杏杏  丛小飞  孙腾科 《测绘与空间地理信息》2014,(7):26-31

以Sacramento-San Joaquin三角洲水域为研究区,利用2007年覆盖研究区的64个航带的HyMap数据,分别用混合调谐匹配滤波(MTMF)和决策树进行藻类信息的分类提取,在此基础上均采用Kappa系数作为标准进行精度评价。结果表明:混合调谐匹配波(MTMF)分析方法对藻类进行分类的结果,Kappa系数是0.634;用基于指数的决策树方法对藻类进行分类的结果,Kappa系数是0.613,两种结果都具有高度的一致性。这说明这两种方法在提取水生物种方面比价有效。  相似文献   

Planktonic cyanobacteria in New Zealand inland waters: Distribution and population dynamics   总被引：1，自引：0，他引：1  

Rick D. Pridmore  M. Kay Etheredge 《新西兰海洋与淡水研究杂志》2013,47(3):491-502

One hundred and four taxa of planktonic cyanobacteria (blue‐green algae) have been recorded from New Zealand lakes: 32 belong to the Chroococcales, 72 to the Nostocales. None of the taxa is endemic to New Zealand; most (if not all) are cosmopolitan. On average, more taxa have been reported from North Island (7.8 ± 6.7, N = 69) than South Island lakes (3.3 ± 3.9, N = 59). This difference is attributable, in part, to the large proportion of glacial lakes in the South Island, which are commonly poor in plant nutrients and possess sparse phytoplankton populations. Many of the taxa show a strong preference for eutrophic conditions. Notable exceptions are Anabaena affinis and Gomphosphaeria lacustris, which occur in a large proportion of mesotrophic (48%) and oligotrophic lakes (43%), respectively. Taxa which are often abundant and frequently responsible for conspicuous water‐blooms are Microcystis aeruginosa, Anabaena circinalis, A. flos‐aquae and A. spiroides. The limited population data available indicate a high level of interannual variability in the timing, magnitude, and duration of cyanobacterial blooms in New Zealand lakes.  相似文献   

Microform bed clusters as refugia for periphyton in a flood‐prone headwater stream     

S. N. Francoeur  B. J. F. Biggs  R. L. Lowe 《新西兰海洋与淡水研究杂志》2013,47(3):363-374

Flood effects on benthic algal communities grown upon three common substratum types were assessed in a gravel‐bed stream. Microform bed clusters (MBCs) and, to a lesser extent, boulders conferred resistance on their associated periphyton communities (i.e., reduced flood‐induced biomass loss; functioned as refugia) relative to cobble/gravel substrata. On all substrata, flooding significantly reduced the relative abundance of Diatoma hiemale, and increased the relative abundance of Gomphonema minutum f. syriacum and/or Ampithrix sp. Long‐term (>4 months) sampling indicated that MBCs generally supported more algal biomass than did boulders, which, in turn, supported greater biomass than cobbles/gravels. Manipulation of the abundance of refugial structures (e.g., MBCs) could possibly alter productivity of flood‐prone gravel‐bed streams. Stream periphyton biomass models may be improved by explicit consideration of the effects of refugial substrata. The interstitial spaces of MBCs may constitute a unique habitat, and deserve further study.  相似文献   

Biological aspects of pollution in the Heathcote river,Christchurch, New Zealand     

Jan Cameron 《新西兰海洋与淡水研究杂志》2013,47(4):431-444

The presence and degree of pollution in the Heathcote River was estimated from bacterial and chemical analyses of water sampled at low tide from five stations in summer 1967–68. The river is very badly polluted in the industrial area and downstream of it, but is fairly clean upstream of the industrial area. Results of analyses of micro‐organisms and macrofauna at 20 stations are presented and distributions of these organisms are related to salinity and pollution in the river. Pollution is restricting the macrofauna of the river but is encouraging micro‐organism populations. Three groups of macrofauna are present:

• Those present in clean freshwater only,

• Those tolerating pollution but restricted to freshwater, and

• Those tolerating pollution but restricted to saline water.

The use of these groups of species as biological indicators of pollution in the Heathcote River has been evaluated; pollution appears to be indicated by absence of a group of species rather than by presence of one species.  相似文献   

New Zealand xenophyophores: Upper bathyal distribution,photographs of growth position,and a new species     

O. S. Tendal  K. B. Lewis 《新西兰海洋与淡水研究杂志》2013,47(2):197-203

Xenophyophores are a group of giant, but extremely fragile, rhizopod protozoans generally found at lower bathyal or abyssal depths. Recent dredge samples and photographs suggest that there is a largely endemic fauna of xenophyophores with anastomosing branches living at upper bathyal depths around New Zealand. Their distribution may be related to the layer of Antarctic Intermediate water that bathes the upper slope of the New Zealand Plateau.

Photographs of the seafloor at depths of 800–1300 m on the Lord Howe Rise show hemispherical masses, 5 cm across, of which the majority appear to be Syringammina tasmanensis Lewis, 1966 and at least one specimen may be Reticulammina lamellata Tendal, 1972. The photographs indicate that these species live on the seabed, not beneath it, that they are probably filter feeders and that they can reach a density of about one specimen per square metre.

A new species, Reticulammina maini, is described from the continental slope east of Auckland. A key to the New Zealand species of xenophyophore is presented.  相似文献   

First record of Australian bonito,Sarda Australis,from New Zealand     

G. D. James  G. Habib 《新西兰海洋与淡水研究杂志》2013,47(3):425-426

The range of the Australian bonito, Sarda australis (Macleay, 1880), previously known only from eastern Australia and Norfolk Island, is now extended to include New Zealand. Data on two specimens examined from northern New Zealand are presented.  相似文献