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1.
Praxedes Muñoz Javier Sellanes Carina Lange Maritza Palma 《Progress in Oceanography》2007,75(3):586-602
We estimated monthly fluxes of 210Pb in shelf sediments beneath a high productivity area off central-southern Chile (36°S) during 1 year (September 2002-August 2003). Sediment cores were obtained using a multiple corer and were analyzed mainly for 210Pb, total pigments, and macrofauna abundance. The 210Pb inventories and fluxes were estimated for surface sediments (0-5 cm) and bioturbation coefficients were inferred using chlorophyll-a (reactive) profiles. In general, 210Pb content was inversely correlated with phytodetritus fluxes. High photosynthetic pigment contents in surface sediments were consistently associated with lower 210Pb contents. Macrofaunal activity responded to oxygen and organic matter supplies at the sediment surface, generally concentrated in the first centimeters, but particularly so during months of high organic matter fluxes and deficient bottom water oxygen conditions. At this study site, several processes involved in the 210Pb surface distribution make it difficult to accurately estimate ages at the surface. We postulate that the organic fluxes promote changes in the faunal activity, which, in combination with sediment resuspension and water circulation over the shelf, produce seasonal variations in the 210Pb inventories. 相似文献
2.
海洋光合有效辐射分布的计算模式 总被引:7,自引:1,他引:7
针对一类海水,采用美国标准大气模型和一类水体海洋生物-光学特性的半分析方法,建立了海洋光合有效辐射计算模式。模式比较全面地考虑了大气、海-气界面和水体的光辐射传输过程,能较好地用于分析叶绿素浓度以及光辐射场的角分布对光俣有效辐射分布的影响。对模拟结果的分析以及与实测结果的比较表明,该模式能较好地应用于计算衰减系数、光谱辐照度随深度的分布、光合有效辐射随深度的分布和真光层深度,在海洋生态系统的光动力学研究和水色遥感方面有效好的应用前景。 相似文献
3.
光合细菌在对虾育苗生产中的应用 总被引:6,自引:1,他引:6
1995年4月24日~5月8日,在文登高岛盐场育苗场50m3水体育苗池,进行了用几株光合细菌(RhodopseudomonasS.P.)混合菌液作为中国对虾(Penaeuschinensis)苗期水质净化剂及辅助饵料,取得了明显效果。育苗池水透明度提高约20cm,幼体挂脏率下降50%,变态提早1d左右,且多产仔虾百万尾 相似文献
4.
Christopher L. Dupont James. W. Moffett Robert R. Bidigare Beth A. Ahner 《Deep Sea Research Part I: Oceanographic Research Papers》2006,53(12):1961-1974
Dissolved and particulate concentrations of the biogenic thiols cysteine (Cys), arginine–cysteine (Arg–Cys), glutamine–cysteine (Gln–Cys), γ-glutamate–cysteine (γ-Glu–Cys) and glutathione (GSH) were measured in the subartic Pacific Ocean in the summer of 2003 using high performance liquid chromatography (HPLC) with precolumn derivatization as reported in previous work. In this study, a preconcentration protocol for the derivatized thiols was utilized to extend detection limits of dissolved thiols to picomolar levels. The measured concentrations of particulate and dissolved thiols were uncoupled, with distinctive depth profiles and large differences in the particulate to dissolved ratios between individual compounds. Glutathione was the most abundant particulate thiol whereas the most abundant dissolved thiol was γ-Glu–Cys, with concentrations as high as 15 nM. Given the relatively small pool of intracellular γ-Glu–Cys and the very low dissolved concentrations of GSH, we hypothesize that glutathione released from cells is rapidly converted to the potentially degradation resistant γ-Glu–Cys outside the cell. The relatively high concentrations of other dissolved thiols compared to particulate concentrations implies both biological exudation and slow degradation rates. Some thiols appear to vary with changes in nutrient availability but this effect is difficult to decouple from changes in community structure inferred from pigment analyses. Dissolved thiol concentrations also exceed typical metal concentrations in the subartic Pacific, supporting previous arguments that they may be important in metal speciation. 相似文献
5.
Spring and summer phytoplankton communities in the Chukchi and Eastern Beaufort Seas 总被引:2,自引:0,他引:2
Victoria Hill Glenn Cota Dean Stockwell 《Deep Sea Research Part II: Topical Studies in Oceanography》2005,52(24-26):3369
Phytoplankton pigments and size-fractionated biomass in the Chukchi and Beaufort Seas showed spatial and temporal variation during the spring and summer of 2002. Cluster analysis of pigment ratios revealed different assemblages over the shelf, slope and basin regions. In spring, phytoplankton with particle sizes greater than 5 μm, identified as diatoms and/or haptophytes, dominated over the shelf. Smaller (<5 μm) phytoplankton containing chlorophyll b, most likely prasinophytes, were more abundant over the slope and basin. Due to extensive ice cover at this time, phytoplankton experienced low irradiance, but nutrients were near maximal for the year. By summer, small prasinophytes and larger haptophytes and diatoms co-dominated in near-surface assemblages in largely ice-free waters when nitrate was mostly depleted. Deeper in the water column at 1–15% of the surface irradiance larger sized diatoms were still abundant in the upper nutricline. Phytoplankton from the shelf appeared to be advected through Barrow Canyon to the adjacent basin, explaining similar composition between the two areas in spring and summer. Off-shelf advection was much less pronounced for other slope and basin areas, which are influenced by the low-nutrient Beaufort gyre circulation, leading to a dominance of smaller prasinophytes and chlorophytes. The correlation of large-sized fucoxanthin containing phytoplankton with the higher primary production measurements shows promise for trophic status to be estimated using accessory pigment ratios. 相似文献
6.
Mi Ok Park 《Ocean Science Journal》2006,41(4):301-313
Abundance and distribution of phytoplankton in seawater at southwestern East/Japan Sea near Gampo were investigated by HPLC
analysis of photosynthetic pigments during summer of 1999. Detected photosynthetic pigments were chlorophyll a, b, c1+2 (Chl a, Chl b, Chl c1+2), fucoxanthin (Fuco), prasinoxanthin (Pras), zeaxanthin (Zea), 19’-butanoyloxyfucoxanthin (But-fuco) and beta-carotene (β-Car).
Major carotenoid was fucoxanthin (bacillariophyte) and minor carotenoids were Pras (prasinophyte), Zea (cyanophyte) and But-fuco
(chrysophyte). Chl a concentrations were in the range of 0.16-8.3/land subsurface chlorophyll maxima were observed at 0-10m
at inshore and 30–50 m at offshore. Thermocline and nutricline tilted to the offshore direction showed a mild upwelling condition.
Results from size-fraction showed that contribution from nano+picoplankton at Chl a maximum layer was increased from 18% at
inshore to 69% at offshore on average. The maximum contribution from nano+picoplankton was found as 87% at St. E4. It was
noteworthy that contribution from nano+picoplanktonic crysophytes and green algae to total biomass of phytoplankton was significant
at offshore. Satellite images of sea surface temperature indicated that an extensive area of the East/Japan Sea showed lower
temperature (<18 °C) but the enhanced Chl a patch was confined to a narrow coastal region in summer, 1999. Exceptionally high
flux of low saline water from the Korea/Tsushima Strait seemed to make upwelling weak in summer of 1999 in the study area.
Results of comparisons among Chl a from SeaWIFs, HPLC and fluorometric analysis showed that presence of Chl b cause underestimation
of Chl a about 30% by fluorometric analysis but overestimation by satellite data about 30-75% compared to HPLC data. 相似文献
7.
几种红藻和蓝藻的光合作用色素 总被引:2,自引:0,他引:2
分离纯化出几种海产红藻和一种蓝藻的光合作用色素,并测定了它们的化学性质和光谱学性质。这些藻类是3种红藻:多管藻(Polysiphonia urceolata)、橡叶藻(Phycodrys sp.)和条斑紫菜(Porphyra yezoensis);蓝藻:钝顶螺旋藻(Spirulina platensis)。用羟基磷灰石柱层析法从上述藻类中分离到几种不同的藻胆蛋白。经SDS-PAGE及光谱测定,发现条斑紫菜中的藻红蛋白不同于其它两种红藻。而橡叶藻中存在的两条藻红蛋白也有差异,条斑紫菜和钝顶螺旋藻中的两种别藻蓝蛋白之间也有区别。叶绿素分析表明,钝顶螺旋藻中叶绿素a的含量高于红藻中叶绿素a的含量。 相似文献
8.
Multi-proxy evidence of long-term changes in ecosystem structure in a Danish marine estuary, linked to increased nutrient loading 总被引:3,自引:0,他引:3
Marianne Ellegaard Annemarie L. Clarke Nina Reuss Simon Drew Kaarina Weckstrm Stephen Juggins N. John Anderson Daniel J. Conley 《Estuarine, Coastal and Shelf Science》2006,68(3-4):567
This paper presents a study of changes in eutrophication over the past 100 years in a fertile estuary. The Danish estuary Mariager Fjord is a long, narrow sill-fjord with a permanently anoxic basin. In 1997 anoxia spread from the basin to the entire inner estuary, killing almost all eukaryotes and prompting debate on the causes. This paper reports a multi-proxy survey of 210Pb-dated sediment cores from the anoxic basin. Analyses of diatoms, dinoflagellates, pigments and geochemical proxies were used to determine changes in ecosystem structure over the past 100 years. The aim was to establish ‘base-line conditions’, for management purposes, of the biological structure prior to 1900, and to examine possible causes of changes observed. Geochemical proxies total nitrogen (TN), total carbon (TC) and biogenic silica (BSi) were consistently high throughout the sediment record. Increased concentrations of pigments and natural isotopes (δ13C, δ15N) suggested increasing production and nutrient loading. The main changes in the biological proxies occurred between 1915 and the 1940s, and indicated that the estuary has been somewhat eutrophic since 1900, but that the eutrophication process increased over the past 100 years. A reconstruction of TN concentration by a diatom-based transfer function supports this interpretation, with inferred TN ca. 1900 around 60 μmol l−1, and an increase in TN concentration over the past century to ca. 130 μmol l−1 by 1995. Inferred TN decreased to ca. 100 μmol l−1 by 2001, similar to present day monitoring data. 相似文献
9.
10.
不同产地龙须菜光合色素的比较研究 总被引:7,自引:0,他引:7
龙须菜是一种重要的产琼胶海藻。本文分析了从青岛、石岛、龙须岛采集的龙须菜的光合色素组成、光谱特性、光合作用速率及生长速度,从而研究扑光色素的组成与光合作用、生物物质积累之间的关系。三个龙须菜的产地之间相距上百里到几百里,彼此之间进行遗传物质交流的机会较少,存在着地理隔离的可能性。本研究表明,不同产地龙须菜光合色素的组成有差异:青岛的材料藻红蛋白含量较高,石岛及龙须岛材料叶绿素α含量较高。不同产地的材料荧光光谱也有差异。与其他产地的材料相比,龙须岛材料光补偿点较低,生长速度较快。本文对今后的生产需要提供了一些生物学参数。 相似文献