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我国紫菜属一新种——多枝紫菜 总被引：1，自引：0，他引：1
为了促进广东沿海地区紫菜人工养殖事业的发展,作者从1978年开始先后在汕头沿海各地(海丰、陆丰、惠来、潮阳、饶平、南澳等地)进行自然资源的调查和采集时,对所获得的标本进行整理后,发现在该地区除过去已经报道过的种类,例如圆紫菜(Porphyrasuborbiculata Kjellm)绉紫菜(P.crispata Kjellm.),长紫菜(P.dentata Kjellm.),广东紫菜(P.guangdongensis Tseng et Chang)坛紫菜(P.haitanensis Chang et Zheng)之外,还有一些尚未报道的种类,本文所描述的新种——多枝紫菜就是其中之一。 相似文献
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紫菜一新种——单孢紫菜的研究 总被引：2，自引：0，他引：2
福建沿海的紫菜资源非常丰富,为更好地发展紫菜养殖提供新品种,我们对该省紫菜属的种类进行了一些调查。除常见的坛紫菜(Porphyra haitanensis T.J.Chang et B.F.Zheng)、圆紫菜(Porphyra suborbiculata Kjdim.)、绉紫菜(Porphyra crispata Kjellm.)和条斑紫菜(Porphyra yezoensis Ueda.)之外,还发现有的种类是前人未曾记述过的,现将新种——单孢紫菜Porphyra monosporangia sp.nov.报道如下。 相似文献
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绒扇藻属(Avrainvillea)藻体广泛分布于热带、亚热带海洋，尤其盛产于珊瑚礁上。因此，该属种类的分布在很大程度上受海区的限制。绒扇藻属的主要特征是藻体深绿色，褐绿色或黑褐色，基部是由假根状丝体相互交织，构成固着器，固着在礁石上。叶柄单生或具有多次分裂。叶片单个或多个，形状不一，多数为扇形，长圆形，肾形到扁压。藻体不钙化，通常黄色或褐色。二叉状分枝，基部常常缢缩，似念珠状或念珠状。皮层丝体无明显分化或具假皮层。关于绒扇藻属海藻的分类研究，至今为止，已发现23个种。
关于中国绒扇藻属的研究，最早是C.K.Tseng(曾呈奎)于1938年在“海南岛海产绿藻研究Ⅱ”中首次报道了两种绒扇藻，即直立绒扇藻Avrainvillea erecta (Berkeley) A. Gepp et E.S.Gepp和裂片绒扇藻A.lacerata J. Agardh，而后在1983年，在曾呈奎主编的《Common Seaweeds of China》一书中，报道了上述种类，并将其产地扩大到西沙群岛。1991年，陆保仁等在“南沙群岛海区的褐藻和绿藻研究I”中，第三次报道了裂片绒扇藻，将其产地扩大到南沙群岛。最近，作者在研究中国绒扇藻属的标本时，除了己经报道的两种外，又发现该属的1个新种(西沙绒扇藻Avrainvillea xishaensis Tseng， Dong et Lu sp. nov.)和3个新记录[模糊绒扇藻A.obscura (C.Agardh)J. Agardh，和氏绒扇藻A.hollenbergii Trono，群栖绒扇藻A.amadelpha (Montagne)A. Gepp et E.S. Gepp。至今共发现了6个种，其标本均存放在中国科学院海洋研究所植物标本室。 相似文献
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坛紫菜(P.haitanensis T.J.Chang et B.F.Zheng)是我国特有的暖温带性海藻,自然分布于长江以南诸省,是闽、浙等省的紫菜优势种。坛紫菜具有良好的栽培(养殖)性状,有较长的生长期;对海区、附着基有广泛的适应性;藻体大、生长快、产量高,经济效益好。冬季生产的坛紫菜质地柔软,营养丰富,味道鲜美,有独特的风味,产品深受国内、外市场欢迎。它已成为我国人工养殖海藻的主要对象之一,年产量占全国紫菜产量的百分之九十左右。坛紫菜的单位面积产量和条斑紫菜一样,在不同地区、不同年份、不同单位之间都 相似文献
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丝状藻体是紫菜生活史中的重要阶段,其生长增殖与环境条件密切相关.本研究考察了与坛紫菜丝状藻体生长增殖相关的多个影响因子,探讨了可促进坛紫菜丝状藻体生长、达到生长速率快的优化调控培养条件.具体操作实施过程为：初始丝状藻体来自成熟紫菜叶状体的果孢子释放,基于8因子3水平的正交实验设计方案[采用正交表L27（313）],确定了丝状藻体生长对多个环境因子的响应以及优化的调控培养条件.结果表明,除开pH、复合维生素浓度和NaHCO3浓度外,其他因子对丝状藻体生长均有显著的影响（p≤0.043 8）.获得的优化调控培养条件为：温度18℃、光强27μmol/m2·s-1、盐度25、pH值8.5、复合维生素浓度15μg/dm3、NaHCO3浓度2 mg/dm3、每天光照时数18 h、营养液浓度为f培养介质.优化调控培养条件下的丝状藻体生长速率高达12.07%,平均值±标准偏差SD为（10.70±0.88）%/d. 相似文献
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紫菜一新种——少精紫菜 总被引：4，自引：0，他引：4
多年来,在青岛沿岸采到属全缘紫菜组的一种紫菜,其形态特征特别是雄性生殖细胞——精子囊器的分布形式不同于前人所记述近缘种类的甘紫菜(Porphyra tenera Kjellm.)、条斑紫菜(P.yezoensis Ueda)、列紫菜(P.seriata Kjellm.)等种。根据精于囊器在叶片上分布的特征及其分列式并与有关种类进行了详细的比较研究,证实这种紫菜为一尚未记述的种类,现定名为少精紫菜Porphyra oligospermatangia Zeng et Zheng Baofu,SP.nov. 相似文献
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近几年,紫菜"高温烂菜"现象频发,为开发耐高温紫菜栽培种质,本文研究了4种温度(15、20、25、28℃)对皱紫菜壳孢子萌发及叶状体形态建成的影响,并观察了藻体的繁殖特性。结果显示,在试验设定的培养条件下,适宜皱紫菜壳孢子萌发生长温度为20—25℃,最适温度为20℃。皱紫菜壳孢子幼苗萌发初期细胞分裂为横分裂,叶状体细胞呈直线排列,生长至7—10个细胞后,细胞开始出现纵分裂。15、20℃温度组藻体多为不规则的半圆形裂片。25、28℃温度组藻体多为细长型叶片。有性生殖是皱紫菜主要的繁殖方式,但15—20℃培养组的部分藻体能够少量形成并放散类似无性生殖的单孢子并萌发形成叶状体。 相似文献
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西沙群岛红藻的研究Ⅳ 总被引：1，自引：0，他引：1
本文继续报告我国西沙群岛产的九种红藻,其中,缠结拟石花Gelidiopsis intricate (Ag.) Vickers、全缘隐蜘藻 Cryptarachne okamurai ( Yamada et Segawa) Zhang et Xia,comb.nov.和柔毛绒线藻Dasya mollis Harvey等三种及紫杉状海门冬的孢子体世代Falkenbergia hillebrandii ( Bornet) Falkenberg均为我国新记录,小隐丝藻Cryptonemia parva sp.nov.为一新种,柔毛绒线藻的精子囊托为首次记述。
所有研究标本,包括新种的模式标本均保存在中国科学院海洋研究所植物标本室。 相似文献
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Soil-sized particulates have been collected on board ship by a mesh technique from the lower troposphere of the North, Equatorial and South Atlantic Ocean, northern and southern Indian Ocean, South and East China Sea and various coastal localities.Spectrographic analysis reveals that, on average, the particulates have concentrations of Mn, Ni, Co, Ga, Cr, V, Ba, and Sr which are of the same order of magnitude as those in average crustal material. In contrast, the average concentrations of Pb, Sn, and Zn are one order of magnitude higher than those in average crustal material.Within this “world-wide” average there are significant geographical variations in the distributions of Pb, Sn, and Zn which may be related to anthropogenic sources.On the basis of trace-element distributions lower tropospheric soil-sized marine particulates have been divided into four genetic components; local, zonal, inter-zonal, and global. The proportions of these components vary geographically, and each component may have both a natural and an anthropogenic fraction. 相似文献
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Tautog, Tautoga onitis, is an abundant species of fish in estuaries of the northeastern United States. Planktonic tautog larvae are abundant in summer in these estuaries, but there is little information on rates of growth of tautog larvae feeding on natural assemblages of food in the plankton. We examined abundance and growth of larval tautog and environmental factors during weekly sampling at three sites along a nearshore‐to‐offshore transect in Buzzards Bay, Massachusetts, USA during summer 1994. This is the first study of a robust sample size (336 larvae) to estimate growth rates of field‐caught planktonic tautog larvae feeding on natural diets, using the otolith daily‐growth‐increment method. The study was over the entire summer period when tautog larvae were in the plankton. The sampling sites contrasted in several environmental variables including temperature, dissolved oxygen (DO), and chlorophyll a concentration. There was a temporal progression in the abundance of tautog larvae over the summer, in relation to location and temperature. Tautog larvae were first present nearshore, with a pronounced peak in abundance occurring at the nearshore sites during the last 2 weeks in June. Larvae were absent at this time further offshore. From late June through August, larval abundance progressively decreased nearshore, but increased offshore although never approaching the abundance levels observed at the nearshore sites. The distribution and abundance of tautog larvae appeared to be related to a nearshore‐to‐offshore seasonal warming trend and a nearshore decrease in DO. Otoliths from 336 larvae ranging from 2.3 to 7.7 mm standard length had otolith increment counts ranging from 0 to 19 increments. Growth of larval tautog was estimated at 0.23 mm·day?1, and length of larvae prior to first increment formation was estimated at 2.8 mm indicating that first increment formation occurs 3–4 days after hatching at 2.2 mm. Despite spatial and temporal differences in environmental factors, there were no significant differences in growth rates at any of three given sites over time, or between sites. Because larval presence only occurred at a narrow range of temperature (17–23.5 °C) and DO (6.5–9.3 mg·l?1), in situ differences in growth did not appear to be because of differences in larval distribution and abundance patterns relative to these parameters. 相似文献
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Lars-Göran Danielsson 《Marine Chemistry》1980,8(3):199-215
Results of trace-metal analyses of water samples obtained during a cruise with the Soviet R.V. “Akademik Kurchatov” in the Indian Ocean are presented. The determinations were performed on board with atomic absorption spectrophotometry after a two-stage dithiocarbamate—Freon extraction procedure. Trace-metal concentrations found are in the same range as those found recently for similar open-ocean areas by other workers. The values for lead and zinc are probably high due to contamination. Vertical profiles indicate biogenic processes as controlling factors for the increase of cadmium, copper and nickel concentrations with depth. Iron shows an irregular depth distribution as a result of large random variations in concentration. 相似文献
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Klaus Kremling 《Marine Chemistry》1983,13(2):87-108
In June 1981, dissolved Zn, Cd, Cu, Ni, Co, Fe, and Mn were determined from two detailed profiles in anoxic Baltic waters (with extra data for Fe and Mn from August 1979). Dramatic changes across the O2H2S interface occur in the abundances of Cu, Co, Fe, and Mn (by factors of ?100). The concentrations of Zn, Cd, and Ni at the redox front decrease by factors between 3 to 5.Equilibrium calculations are presented for varying concentrations of hydrogen sulfide and compared with the field data. The study strongly supports the assumption that the solubility of Zn, Cd, Cu, and Ni is greatly enhanced and controlled by the formation of bisulfide and(or) polysulfide complexes. Differences between predicted and measured concentrations of these elements are mainly evident at lower ΣH2S concentrations.Cobalt proved to be very mobile in anoxic regions, and the results indicate that the concentrations are limited by CoS precipitation. The iron (Fe2+) and manganese (Mn2+) distribution in sulfide-containing waters is controlled by total flux from sediment-water interfaces rather than by equilibrium concentrations of their solid phases (FeS and MnCO3). The concentrations of these metals are therefore expected to increase with prolonged stagnation periods in the basin. 相似文献
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P.N. Froelich L.W. Kaul J.T. Byrd M.O. Andreae K.K. Roe 《Estuarine, Coastal and Shelf Science》1985,20(3):239-264
Concentrations of dissolved nutrients (NO3, PO4, Si), germanium species, arsenic species, tin, barium, dimethylsulfide and related parameters were measured along the salinity gradient in Charlotte Harbor. Phosphate enrichment from the phosphate industry on the Peace River promotes a productive diatom bloom near the river mouth where NO3 and Si are completely consumed. Inorganic germanium is completely depleted in this bloom by uptake into biogenic opal. The ratio taken up by diatoms is about 0·7 × 10?6, the same as that provided by the river flux, confirming that siliceous organisms incorporate germanium as an accidental trace replacement for silica. Monomethylgermanium and dimethylgermanium concentrations are undetectable in the Peace River, and increase linearly with increasing salinity to the seawater end of the bay, suggesting that these organogermanium species behave conservatively in estuaries, and are neither produced nor consumed during estuarine biogenic opal formation or dissolution. Inorganic arsenic displays slight removal in the bloom. Monomethylarsenic is produced both in the bloom and in mid-estuary, while dimethylarsenic is conservative in the bloom but produced in mid-estuary. The total production of methylarsenicals within the bay approximately balances the removal of inorganic arsenic, suggesting that most biological arsenic uptake in the estuary is biomethylated and released to the water column. Dimethylsulfide increases with increasing salinity in the estuary and shows evidence of removal, probably both by degassing and by microbial consumption. An input of DMS is observed in the central estuary. The behavior of total dissolvable tin shows no biological activity in the bloom or in mid-estuary, but does display a low-salinity input signal that parallels dissolved organic material, perhaps suggesting an association between tin and DOM. Barium displays dramatic input behavior at mid-salinities, probably due to slow release from clays deposited in the harbor after catastrophic phosphate slime spills into the Peace River. 相似文献