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青岛对丝藻属Antithamnion Nageli的研究 总被引:1,自引:0,他引:1
刘剑华 《山东海洋学院学报》1984,14(2):40-47
对丝藻属由Nageli,C.1847年建立,分布于地中海、大西洋和太平洋。已报道的约有45种。近年来Wollaston等根据藻体小枝及腺细胞等特征,将原属于对丝藻属的一些种类移至凝对丝藻属Antithamnionella中。 相似文献
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于1963年在内蒙古自治区包头市南,黄河堤坝北岸盐碱地积水洼中采得两号标本,经光镜观察表明,该新植物为鞘毛藻科一新属——辐枝藻属。辐枝藻为分枝丝状体,由匍匐部分和直立部分组成;匍匐枝彼此贴靠形成单层细胞厚的假薄壁组织;直立枝具粗壮的主轴和细的小枝;部分小枝末端细胞具一条长的鞘毛;每个细胞具一个周生、片状的色素体,蛋白核一至多个,具一个细胞核。该藻以动孢子营无性生殖,动孢子囊位于枝或小枝顶端。此新属仅一新种,为嗜盐辐枝藻。模式标本保存于中国科学院水生生物研究所。 相似文献
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于1983-1986年先后在福建沿岸采订爬管藻标本,进行分类研究。根据有限枝节片数目、囊果的着生位置以及围轴细胞数目等形态特征,发现其中两种标本与已知种的特征不同:一种是囊果位置不定,着生在有限枝基部第4(3)节片以上至顶端节片;另一种是有限枝节片数目较少,由5-12-(14)个节片组成囊果基生。故这为两个新种,即福建爬管8藻Herposiphonia fujianensis sp.nov和基生爬管藻H.basilaris sp.nov。模式标本保存于福建师范大学生物系植物标本室。 相似文献
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利用生物压片技术,通过形态学和解剖学方法,对采自我国沿岸海洋的仙菜科红藻(Ceramiaceae,Rhodophyta)进行了分类学研究,发现了我国仙菜科新记录属——盖氏藻属(新拟名)Gayliella T.O.Cho,L.McIvor et S.M.Boo。该属目前在我国共有5个种,即短毛盖氏藻(新拟名)Gayliella pmbriatum (Setchell et N. L. Gardner). T. O. Cho et S. M. Boo、优美盖氏藻(新拟名) Gayliella βaccidum (Kützing) T. O. Cho et L. McIvor、泰式盖氏藻(新拟名) Gayliella taylorii (E. Y. Dawson) T. O.Cho et S. M. Boo、马沙盖氏藻(新拟名) Gayliella mazoyerae T. O. Cho, Fredericq et Hommersand和横轴盖氏藻(新拟名) Gayliella transversalis (Collins et Hervey) T. O. Cho et Fredericq,... 相似文献
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沙菜属Hypnea海藻作为提取卡拉胶的原料之一, 具有重要的经济价值。但由于该属物种地理分布广泛, 表型可塑性强, 且缺乏详细的解剖学特征, 故有关其物种鉴定也就一直存在争议。本文利用冷冻切片技术, 通过形态学和解剖学方法, 对2013—2014年采自粤东汕头的沙菜属海藻进行了形态特征描述。经鉴定, 该地区沙菜属共有4种, 分别为密毛沙菜Hypnea boergesenii、裸干沙菜H. chordacea、长枝沙菜H. charoides和冻沙菜H. japonica。通过对这几种沙菜进行了较详细的内、外部结构特征分析, 给出了它们在国内外的地理分布及习性等信息, 并对沙菜属的科级分类系统(沙菜科Hypneaceae/赤叶藻科Cystocloniaceae)划分以及密毛沙菜是否为独立物种进行了讨论。 相似文献
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本文用光镜(LM)、透射电镜(TEM)和扫描电镜(SEM)观察了在光镜下难以分辨的主要采自海南省西沙群岛的硅藻共6属13种,其中有4个新种,3个新记录种和1个新记录属(以*号为记),它们是:Synedracy clophoroides sp.nov.,* Cyclophera tenuis,Plagiogramma parva sp.nov.,Plagiogramma pandurata sp.nov.,P.atomus,P.reimeri,Opephora elliptica sp.nov.,O.martyi,O.olsenii,O. sp.*Fragilaria brevistriata var,elliptlca,*F.construens和Pseudostaurosira brevistriata. 相似文献
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苏北大米草滩中牡蛎的滋生 总被引:1,自引:0,他引:1
Ⅰ. 牡蛎在苏北大米草滩中的分布 苏北是我国引种大米草最早的地区,现有草滩27万多亩(1亩=666.6m~2),草带断断续续在拿省946km的海岸线上分布长达377km~1(见图1)。 相似文献
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Yang Shengguang ;Xia Daying ;Yang Xiaolong ;Zhao Jun 《海洋湖沼学报(英文)》1991,9(1):49-56
This study showed that the combined effect of absorption of planktonic algae and water on water color shift can be simulated approximately by the exponential function: Log(E 100cm +E 100cm ch1 )=0.002λ−2.5 whereE 100 cm ,E 100cm chl are, respectively, extinction coefficients of seawater and chlorophyll—a (concentration is equal toX mg/m3), and λ (nm) is wavelength. This empirical regression equation is very useful for forecasting the relation between water color and biomass in water not affected by terrigenous material. The main factor affecting water color shift in the ocean should be the absorption of blue light by planktonic algae. 相似文献
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A preliminary optical classification of lakes in Estonia and south Finland which can also be used for small bays of the Baltic Sea is elaborated. The classification is based on the optical properties of water (diffuse attenuation coefficient, diffuse reflectance) and parameters that are routinely monitored in water bodies (Secchi depth, concentration of chlorophyll-a, total suspended matter and yellow substance). The data complex used for our classification covers different types of water ecosystems (ranging from oligotrophic to hypertrophic) and the variability of water constituent concentrations in the ice-free period in Estonia and south Finland. Using cluster analysis, we found 5 optical classes of waters: clear (C), moderate (M), turbid (T), very turbid (V) and brown (B). There is satisfactory correspondence between class of water, shape of diffuse attenuation coefficient and diffuse reflectance spectra and trophic state of the lakes. 相似文献
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Fiammetta Straneo Franois Saucier 《Deep Sea Research Part I: Oceanographic Research Papers》2008,55(8):926-946
This study describes the first year round observations of the outflow from Hudson Strait as obtained from a moored array deployed mid-strait from August 2004–2005, and from a high-resolution hydrographic section conducted in September 2005. The outflow has the structure of a buoyant boundary current spread across the sloping topography of its southern edge. The variability in the flow is dominated by the extreme semi-diurnal tides and by vigorous, mostly barotropic, fluctuations over several days. The fresh water export is seasonally concentrated between June and March with a peak in November–December, consistent with the seasonal riverine input and sea-ice melt. It is highly variable on weekly timescales because of synchronous salinity and velocity variations. The estimated volume and liquid fresh water transports during 2004–2005 are, respectively, of 1–1.2 Sv and 78–88 (28–29) mSv relative to a salinity of 34.8 (33). This implies that the Hudson Strait outflow accounts for approximately 15% of the volume and 50% of the fresh water transports of the Labrador Current. This larger than previously estimated contribution is partially due to the recycling, within the Hudson Bay System, of relatively fresh waters that flow into Hudson Strait, along its northern edge. It is speculated that the source of this inflow is the outflow from Davis Strait. 相似文献
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近江牡蛎铜锌超氧化物歧化酶的稳定性 总被引:3,自引:0,他引:3
在从近江牡蛎(Crassostrea rivularis)软体部分提纯得到纯度均一的铜锌超氧化物歧化酶(Cu,Zn-SOD)的基础上,对该酶的稳定性进行了研究,结果表明,该酶的水溶液在65℃时活力稳定,而该酶的干品在1℃/min程序升温时在58.4摄氏度有一尖锐的吸热峰,在pH为5.2-10.0的范围内该酶的活力不受影响。该酶对H2O2和KCN均敏感,且能耐受Tsuchihashi氏试剂的作用。一些氧化剂,还原剂,变性剂可改变酶的活力,差示扫描量热分析(Differential Scanning Calorimetry,DSC)发现,该酶在不同的升温速率下以及不同浓度的H2O2处理对酶的稳定性的影响与猪血,牛血SOD均有差异。 相似文献
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We study the reaction of a global ocean–sea ice model to an increase of fresh water input into the northern North Atlantic under different surface boundary conditions, ranging from simple restoring of surface salinity to the use of an energy balance model (EBM) for the atmosphere. The anomalous fresh water flux is distributed around Greenland, reflecting increased melting of the Greenland ice sheet and increasing fresh water export from the Arctic Ocean. Depending on the type of surface boundary condition, the large circulation reacts with a slow-down of overturning and gyre circulations. Restoring of the total or mean surface salinity prevents a large scale redistribution of the salinity field that is apparent under mixed boundary conditions and with the EBM. The control run under mixed boundary conditions exhibits large and unrealistic oscillations of the meridional overturning. Although the reaction to the fresh water flux anomaly is similar to the response with the EBM, mixed boundary conditions must thus be considered unreliable. With the EBM, the waters in the deep western boundary current initially become saltier and a new fresh water mass forms in the north-eastern North Atlantic in response to the fresh water flux anomaly around Greenland. After an accumulation period of several decades duration, this new North East Atlantic Intermediate Water spreads towards the western boundary and opens a new southward pathway at intermediate depths along the western boundary for the fresh waters of high northern latitudes. 相似文献