翡翠贻贝软体部营养成分的研究

分析了翡翠贻贝Pernaviridis软体部的营养成分。其中蛋白质及氨基酸含量较高 ,必需氨基酸占总氨基酸量的 33 2 %。粗脂肪和脂肪酸含量丰富 ,特别是EPA和DHA总量占总脂肪酸的 2 6 0 1 %。除富含Ca,Mg ,Fe等无机元素外 ,Se的含量也较高。     

海水中氨基酸对Cu（Ⅱ）在r—MnOOH上吸附的影响

实验测定了海水中氨基酸存在下Ｃｕ（Ⅱ）在ｒ－ＭｎＯＯＨ上吸附的等温线、Ｃｕ（Ⅱ）％－－ｐＨ曲线和Ｃｕ（Ⅱ）％－氨基酸深度曲线。结果表明，较低浓度氨基酸对Ｃｕ（Ⅱ）在ｒ－ＭｎＯＯＨ上吸附没有影响，而较高浓度氨基酸却起抑制作用，这主要是由于海水中Ｃｕ（Ⅱ）－氨基酸络合反应与ｒ－ＭｎＯＯＨ竞争Ｃｕ（Ⅱ）所致。此外，海水中较高浓度氨基酸只使Ｃｕ（Ⅱ）在ｒ－ＭｎＯＯＨ上吸附的表面分级离子交换稳定常数Ｋｉ（ｉ     

Factors Influencing Nitrogen Speciation in Coastal Rainwater

Rainwater was collected from 129 rain events between February 2002 and August 2003 and analyzed for ammonium (NH₄⁺), nitrate (NO₃⁻), organic nitrogen (ON) and free amino acids (AA). Inorganic nitrogen (NO₃⁻ + NH₄⁺) was the dominant form of N representing 85% of total nitrogen based on volume-weighted averages. The remainder of the N occurred as organic nitrogen species of which free amino acids contribute approximately 17%. A significant, and in some cases the majority (> 75%), of the remaining ON could be accounted for by macromolecular uncharacterized humic like substances. This has important ramifications with respect to the long range transport of atmospheric ON because humic materials are recalcitrant and therefore may travel long distances from their source. There was a distinct seasonality to the N speciation data with maximum concentrations of NH₄⁺, ON and AA occurring in the spring. Air-mass back trajectory analysis indicates there is a strong anthropogenic component to the NO₃⁻, NH₄⁺ and AA signal but not ON. There was a strong positive correlation between amino acid concentrations and ammonium which suggests they have similar sources and sinks in rainwater. Finally, large episodic additions of NH₄⁺ and AA during tropical events could significantly impact short term bioavailable N budgets in estuaries impacted by these storms. Approximately three times as much NH₄⁺ and AA were deposited during Hurricane Isabel (317 μ moles ⋅ m⁻² and 84 μ moles ⋅ m⁻² respectively) compared to the mean impact of average summertime rain events at this location.     

Response of the soft coral Heteroxenia fuscescens to ultraviolet radiation regimes as reflected by mycosporine-like amino acid biosynthesis

The variation in mycosporine‐like amino acid (MAA) concentration in the soft coral Heteroxenia fuscescens in relation to changes in ultraviolet radiation (UVR) regimes was investigated at the Gulf of Eilat, northern Red Sea. Solar radiation (300–700 nm) was measured for different depths and seasons. The UVR irradiance was measured to a depth of 25 m on the reef. The mean attenuation coefficient for UV‐B measured in winter was twofold that of the summer value. Separation of H. fuscescens extracts by reverse‐phase isocratic high‐performance liquid chromatography revealed a single MAA compound, palythine (λ_max = 320 nm). Possible seasonal changes in MAAs in colonies of H. fuscescens along a depth gradient were examined on different dates. Palythine concentrations in the colonies were significantly higher in summer than in the other seasons particularly in shallow water. Possible changes in MAA content in colonies of H. fuscescens as a result of UVR protection, were determined by experiments conducted for periods of 1 week, 1 month and 3 months, at a depth of 5 m. In these experiments colonies were removed from the natural substrate and placed underwater, protected from UVR by a PVC filter. Significant differences between UV‐exposed and protected colonies of H. fuscescens were found only in the 3‐month experiment conducted during the summer. These findings demonstrate that UVR is an important environmental factor regulating MAA biosynthesis in the soft coral H. fuscescens.     

锯缘青蟹幼体饵料蛋白质的营养价值评价

本文分析测定了锯缘青蟹幼体从刚孵化至大眼幼体各发育阶段及其饵料轮虫和卤虫无节幼体的氨基酸组成，并使用必需氨基酸指数(EAAI)来评价饵料蛋白质的质量.结果表明，青蟹各期幼体的氨基酸组成基本趋于一致，且与饵料转换不存在明显的相关性.对于各期幼体，饵料轮虫和卤虫无节幼体的必需氨基酸指数均大于90，可以认为，轮虫和卤虫无节幼体能够满足锯缘青蟹幼体对饵料中必需氨基酸的营养需求.     

Last interglacial (MIS 5e) sea-level determined from a tectonically stable,far-field location,Eyre Peninsula,southern Australia

The last interglacial maximum (Marine Isotope Substage 5e [MIS 5e], 128–116 ka) is a distinctive event in recent Earth history. Shoreline successions of this age are important for calibrating climate models and defining the overall behaviour of the crust–mantle system to fluctuating ice and ocean-water volumes. In a global context, the recently intensified interest in last interglacial shoreline successions has revealed considerable variability in the magnitude of sea-level rise during this time interval and highlighted the need to examine paleosea-level evidence from tectonically stable, far-field settings. Situated in the far-field of continental ice sheets and on the tectonically stable Gawler Craton, the 300 km coastal sector of western Eyre Peninsula between Fowlers Bay and Lake Newland in southern Australia represents an important region for defining the glacio-eustatic (ice-equivalent) sea-level attained during the last interglacial maximum based on the relative sea-level observations from this region. Low-energy, shoaling upward, peritidal bioclastic carbonate successions of the last interglacial (locally termed Glanville Formation) formed within back-barrier, estuarine–lagoonal environments in the lee of eolianite barrier complexes (locally termed Bridgewater Formation) along this coastline. The well-preserved shelly successions (coquinas) contain diverse molluscan fossil assemblages including species no longer living in the coastal waters of South Australia (e.g. the Sydney cockle Anadara trapezia and the benthic foraminifer Marginopora vertebralis). The extent of amino acid racemisation (a measure of fossil age based on increasing d/l value) in a range of species, and in particular A. trapezia and Katelysia sp., confirms the time equivalence of the isolated embayment-fill successions, correlated with the informal type section of the Glanville Formation at Dry Creek, north of Adelaide. Preliminary U-series analyses on A. trapezia also suggest a correlation with the last interglacial maximum, but further highlight the complexity in dating fossil molluscs by the U-series method in view of their open-system behaviour. The shelly successions of the Glanville Formation occur at elevations higher than attained by sea-level in the current, Holocene interglacial. A higher sea-level of between 2.1 ± 0.5 and 4 ± 0.5 m above present sea-level is inferred for the last interglacial maximum (MIS 5e) along this coastline based on the elevation of sedimentary successions host to the shallow subtidal–intertidal fossil molluscs Katelysia sp., and Anadara trapezia. The paleosea-level observations place a lower limit on the sea-level attained during the last interglacial maximum and suggest that caution be exercised in the definition of the upper limit of sea-level during this interglacial.     

盐度对鲈鱼稚、幼鱼发育阶段氨基酸的影响

为揭示鲈鱼(Lateolabrax japonicus)稚、幼鱼在淡化过程中氨基酸的组成及含量的变化规律,本实验在15.00、7.50及0.00共3个盐度梯度下,用氨基酸全自动分析仪对鲈鱼稚、幼鱼氨基酸的组成及含量进行了测定和分析。结果表明,实验中,3个盐度组的总氨基酸含量均逐渐增加,且它们之间没有显著性差异;实验中15.00盐度的必需氨基酸总量略呈下降趋势,而7.50盐度组和0.00盐度组均呈上升趋势,3个盐度之间存在显著性差异(P0.05);除脯氨酸外,3个盐度组中其他的非必需氨基酸含量及总的非必需氨基酸含量也均无显著差异。     

两种氨基酸衍生化方法的比较研究

氨基酸的衍生化过程是气相色谱-燃烧-同位素比值质谱法(GC/C/IRMS)测定单体氨基酸碳稳定同位素组成方法中的关键步骤之一。采用了2种氨基酸衍生化方法分别对17种标准氨基酸进行衍生化处理：一种是氨基酸N-乙酰基正丙酯(NAP)法,另一种是氨基酸N-三氟乙酰基异丙酯(TFAIP)法。通过测量17种氨基酸衍生化前后的稳定碳同位素组成,比较了每种方法的重复性及衍生化过程中的同位素分馏作用的大小。结果说明氨基酸N-三氟乙酰基异丙酯(TFAIP)法是一种较为理想的氨基酸衍生化方法。     

三株海洋酵母的生化营养成分分析

海洋酵母是一种重要的水产生物饵料.实验对3株海洋酵母菌德巴利酵母Debaryomyces sp.、克鲁维酵母Kluyveromyces sp. 和虫道酵母Ambrosiozyma sp.的基础营养成分进行了研究和分析.3株海洋酵母菌的粗蛋白含量分别为56.87%、46.75%、51.80%;脂肪分别为4.67%、6.35%、6.35%;碳水化合物分别为31.28%、41.55%、35.96%;灰分分别为7.18%、5.35%、6.37%.3株海洋酵母菌具有较高的蛋白含量水平以及优良的氨基酸和脂肪酸组成,表明该3株海洋酵母菌具有用作水产饵料生物的营养价值.但是,3株海洋酵母菌均缺乏多不饱和脂肪酸EPA和DHA,用其作为水产饲料源料,需要在配合饲料中添加多不饱和脂肪酸或与富含多不饱和脂肪酸的藻类一起使用.