溶剂萃了以法提取浓缩鱼蛋白的研究

采用溶剂萃取法，经筛选，在一定的温度和时间下，用异丙醇对小杂鱼和低值鱼萃取，提取浓缩鱼蛋白，其蛋白质含量达９２．２８％脂肪含量仅为０．０９％，分含量为３．４２％，水分含量为４．２２％，远远超过联合国粮农组织ＦＰＣ－Ａ的质量标准。     

钝顶螺旋藻多糖提取工艺的研究——三氯乙酸(TCA)法的正交实验优化

研究了用三氯乙酸(TCA)脱除蛋白质提取钝顶螺旋藻(Spirulina platensis)多糖的工艺,并以提取率、样品糖含量与蛋白含量为指标,应用正交实验设计优化了提取液pH值、提取温度及提取时间3个因素。结果表明,在提取液pH值为12、提取温度为90℃及提取时间为8h的最佳条件下,所得螺旋藻多糖为白色粉末,提取率为3.10%,糖质量分数为81.79%,蛋白质量分数为0.57%。     

海藻中EPA,DHA萃取技术的比较研究

在优化条件下比较了溶剂法（SE）、超声强化溶剂法（USE）、超临界CO2法（SFE）及超声强化超临界CO2法（USFE）从海藻中提取EPA和DHA。研究表明，超声对溶剂提取和超临界流体萃取过科都具有强化作用。超声强化溶剂提取过程，使提取时间缩短1h，提取温度低10℃，EPA，DHA提取率分别提高16．61％，16．41％，而且溶剂用量少。超声强化超临界萃取过程，萃取系统的压力降低了5MPa、萃取温度和萃取时间分别由45℃，210min降至35℃，180min，EPA和DHA萃取率分别提高15．09％和15．96％。UV与GC-MS分析结果表明，实验条件下，超声场的加入没有改变EPA，DHA的结构。     

提取pH和温度对罗非鱼(Tilapia zillii)鱼鳞明胶特性的影响

以罗非鱼(Tilapia zillii)鱼鳞为原料, 考察提取pH和温度对明胶蛋白组分及其性质的影响。结果表明, 鱼鳞明胶蛋白在浸提pH大于5时容易发生酶解, pH小于3时会发生热降解, 而在pH 4下酶解和热降解均被有效抑制。在pH 4下利用40℃浸提明胶时, 蛋白的提取率只有1.84%, 提取的明胶中亚氨基酸比例低而钙、磷、钠、镁等矿物质含量高, 因而无法形成凝胶和蛋白膜。当浸提温度提高到50℃及以上时, 明胶提取率大幅增加, 明胶中亚氨基酸比例上升且矿物质含量比例下降。另外, 在pH 4、70℃下浸提的明胶其凝胶强度可达283g, 可形成机械强度为50MPa的蛋白膜, 表明该条件提取的鱼鳞明胶具有替代哺乳动物明胶的潜力。     

3种海洋微藻多糖提取工艺的研究

采用热水浸提法,通过一系列单因素试验,研究了提取时间、pH、温度和液料比对四爿藻、新月菱形藻和三角褐指藻等3种海洋微藻多糖提取的影响。在此基础上,通过正交试验进一步优化多糖的提取工艺。最后,采用适宜提取工艺制备3种海洋微藻粗多糖样品,并测定样品蛋白质和多糖含量。单因素结果表明,提取时间、pH、温度和液料比均能影响四爿藻、新月菱形藻和三角褐指藻多糖的提取。其中,提取时间显著影响新月菱形藻多糖的提取,提取pH对四爿藻和新月菱形藻多糖的提取有显著影响,而提取温度和料液比均能显著影响3种海洋微藻多糖的提取。正交试验结果表明,四爿藻、新月菱形藻和三角褐指藻粗多糖提取的适宜提取时间,温度,pH和料液比分别为80℃、60℃、80℃,240min、240min、120min;10、10、10;1:15、1:25、1:25。制备的粗多糖样品中蛋白质和多糖含量分别为0.59%、0.76%、1.50%和51.4%、17.2%、13.5%。很低的蛋白质含量和较高的多糖含量,表明采用上述试验确定的提取工艺获得的粗多糖样品纯度较高,利于样品的后续分离纯化。     

枸杞多糖的精制工艺优选

目的：优化枸杞多糖(LBP)的精制工艺,为LBP的开发提供参考。方法：以多糖提取率为指标,采用正交试验考察提取次数、提取时间、料液比对多糖提取工艺的影响。在单因素试验的基础上,以糖损失率为指标,利用正交试验优化活性炭除色素工艺,以蛋白清除率和糖损失率的综合评分为指标,采用正交试验优化酶-sevag法脱蛋白工艺。结果：最佳提取工艺为提取次数2次、提取时间30 min、料液比1∶10。最佳除色素工艺为活性炭用量1.0%、温度100℃、时间20 min;糖损失率为28.6%。最佳除蛋白工艺为酶用量1.5%、温度50℃、时间60 min;蛋白质清除率为28.2%,糖损失率为10.9%。结论：优选的LBP精制工艺稳定可行,适用于LBP产品开发。     

米氏凯伦藻细胞表面膜蛋白质组及其对温度变化的响应研究

米氏凯伦藻(Karenia mikimotoi)近年在我国福建、浙江和广东沿海经常形成赤潮,其赤潮不仅影响到海洋生态系统的稳定,也严重威胁到水产养殖以及人类生命健康安全。本论文以米氏凯伦藻为研究对象,建立了米氏凯伦藻细胞表面膜蛋白质荧光标记技术和细胞膜蛋白质提取方法,运用荧光差异凝胶电泳技术(2-DDIGE)对膜蛋白质进行了分析,并研究了米氏凯伦藻的膜蛋白质组及其对环境温度变动的响应。实验共鉴定到44个细胞表面膜蛋白,其中有效注释27个,主要为转运蛋白、HSP70蛋白家族和捕光蛋白等。米氏凯伦藻在20°C条件下的细胞生长和光合作用要明显好于16°C和12°C,但16°C和12°C条件下的差别不大,表明低温限制了米氏凯伦藻的生长。当米氏凯伦藻从12°C快速转移至16°C和20°C时,藻细胞密度和光合作用效率短时间迅速降低,但细胞很快即适应温度变化。细胞膜上的转运蛋白和光合作用蛋白在其适应温度变化中起着重要作用。     

正交试验优选猫爪草纳米乳喷雾剂的提取工艺

目的:正交试验优选猫爪草纳米乳喷雾剂的最佳提取工艺。方法:以总黄酮提取量和浸膏得率的综合评分为评价指标,在单因素试验基础上,采用L₉(3）正交试验考察猫爪草醇提工艺的溶剂体积、乙醇浓度、提取时间及提取温度对提取工艺的影响。结果:最佳提取工艺为以75%乙醇为提取溶剂,提取温度60 ℃,第1 次8倍量1.5 h,第2 次7倍量1 h,共提取2 次。结论:在单因素试验基础上,通过正交试验优选的提取工艺经验证稳定、简便易行、预测性好,为猫爪草纳米乳喷雾剂的进一步研发奠定了基础。     

废弃鱼骨中蛋白质的提取分离及酶解工艺研究

以蛋白提取率和多肽分子质量分布为评价指标,采用不同提取方法和不同蛋白酶对废弃鱼骨蛋白质的提取和酶解工艺进行了研究。结果表明,高压蒸煮法提取的鱼骨蛋白质中蛋白含量为86.15%,蛋白提取率为16.76%,明显高于恒温水浴和热回流提取法。中性蛋白酶酶解的多肽中蛋白含量为88.46%,多肽比例高达95%以上,明显高于其他三种酶。先利用高压提取法提取蛋白质,再利用中性蛋白酶酶解蛋白质制备多肽,可降低酶用量,该方法为多肽工业化生产提供参考及新思路。     

溶解态的Fe、Al、Mn、Si、Cu、Pb和Zn在河口混合过程中的絮凝

本文用生成物法首次对珠江河口混合过程中溶解态的Fe、Al、Mn、Si、Cu、Pb和Zn等元素的絮凝进行研究,以中山大学附近的珠江河水和万山群岛海域的海水按不同比例混合成盐度为0—24‰的系列溶液,对这些元素的絮凝除去机理进行探讨。同时,改变絮凝时间、酸度和温度,求得这些因素对絮凝的影响。结果表明,珠江水中Fe和Pb几乎完全絮凝,其他元素的絮凝率:Cu76%、Mn51%、Al48%、Zn28%和Si1.2%,可见Si在珠江水中呈保守性质。     

抗冻蛋白的研究及其在生物技术中的应用

抗冻蛋白能够与冰晶结合，降低冰点并抑制冰的重结晶，从而使生物体免于冰冻伤害。就不同类型的抗冻蛋白的结构、起源、功能和抗冻作用机制进行了全面的回顾，并对国内近年来抗冻蛋白在生物技术中的应用进行了综述。     

Glaciomarine sedimentation and palaeo-glacial setting of Maxwell Bay and its tributary embayment, Marian Cove, South Shetland Islands, West Antarctica

High-resolution (3.5 kHz and multi-channel) seismic profiles and piston cores were collected from Maxwell Bay and its tributary embayment, Marian Cove, in the South Shetland Islands, Antarctica, during the Korea Antarctic Research Program (1992/93 and 1995/96) to elucidate the glaciomarine sedimentation processes and recent glacial history of the area. Seismic data from Maxwell Bay reveal a rugged bay margin and flattened basin floor covered with well-stratified hemipelagic muds. On the base-of-slope, acoustically transparent debris flows occur, indicating downslope resedimentation of glaciomarine sediments. Despite the subpolar and ice-proximal settings of Marian Cove, the seafloor is highly rugged with a thin sediment drape, suggesting that much of the area has been recently eroded by glaciers. Sediment cores from the cove penetrated three distinct fining-upward lithofacies: (1) basal till in the lower part of the core, accumulated just seaward of the grounding line of the tidewater glacier; (2) interlaminated sand and mud in the middle part, deposited in ice-proximal zone by a combination of episodic subglacial meltwater inflow and iceberg dumping; and (3) pebbly mud in the upper part, deposited in ice-distal zone by both surface meltwater plume and ice-rafting from the glacier front. A reconstruction of the glacial history of these areas since the late glacial maximum shows an ice sheet filling Maxwell Bay in late Wisconsin time and grounding of the tidewater glacier in Marian Cove until about 1300 yr BP.     

A seismic reconnaissance survey of the northern Congo Fan

To study the time-varying influence of the Congo River and the Benguela Current on the deposition at the Angola Continental Margin, a high-resolution reflection seismic survey was carried out on the northern Congo Fan. Four seismostratigraphic units have been defined for the upper 800 m (1000 ms TWT) of the data. The units record different depositional environments, ranging from pre-establishment of the Congo River drainage system to the influence of the Benguela Current. An indication of a general change in the turbidite system is provided by a shift in channel distribution and a relocation of the depocentre of coarse material. The ascent of salt is recorded up to the Pliocene. Gas that has migrated out of Lower Cretaceous shales and that was produced from large quantities of organic matter in the younger sediments can be found on the flanks and on top of the salt domes. In a few places, this gas even ascends to the ocean floor along structural pathways through the topmost unit.     

Evidence for the evolution of an oxygen minimum layer at the beginning of S-1 sapropel deposition in the eastern Mediterranean

The sediments of the eastern Mediterranean basin contain a series of organic-rich sapropels intercalated with organic-poor nannofossil oozes. Until recently the timing of the onset of sapropel formation was not known accurately because of the low resolution achievable by conventional radiocarbon dating. Compilation of all available ¹⁴C-AMS dates show that the base of S-1 (the most recent sapropel) was initiated 8800 years B.P. (¹⁴C age corrected by 400 years for reservoir effect) under a 500 m water column and moved progressively into deeper water reaching depths of 3500 m at 8200 years B.P. The linear correlation between the age of S-1 onset and water depth

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suggests that formation of sapropels moved into deeper water at a rate of 1000 m/200 year. A model is suggested in which export production which sank below the well-mixed surface layers (500 m) was respired consuming dissolved oxygen in the Levantine deep water until a threshold value was reached when sapropels began to be preserved in the sediment. This resulted in a progressively deepening oxygen minimum zone with time until eventually the entire deep water in the basin was oxygen depleted. Assuming that the threshold value for sapropel formation was complete anoxia, it was calculated that primary productivity in the basin during the deposition of S-1 was a factor of 5 greater than that found at present.     

Accelerated relative sea-level rise and rapid coastal erosion:: testing a causal relationship for the Louisiana barrier islands

The role of relative sea-level rise as a cause for the rapid erosion of Louisiana's barrier island coast is investigated through a numerical implementation of a modified Bruun rule that accounts for the low percentage of sand-sized sediment in the eroding Louisiana shoreface. Shore-normal profiles from 150 km of coastline west of the Mississippi delta are derived from bathymetric surveys conducted during the 1880s, 1930s and 1980s. An RMS difference criterion is employed to test whether an equilibrium profile form is maintained between survey years. Only about half the studied profiles meet the equilibrium criterion; this represents a significant limitation on the potential applicability of the Bruun rule. The profiles meeting the equilibrium criterion, along with measured rates of relative sea-level rise, are used to hindcast shoreline retreat rates at 37 locations within the study area. Modeled and observed shoreline retreat rates show no significant correlation. Thus, in terms of the Bruun approach, relative sea-level rise has no power for hindcasting (and presumably forecasting) rates of coastal erosion for the Louisiana barrier islands.     

Variability in the speciation of iron in the northern North Sea

Variations in the speciation of iron in the northern North Sea were investigated in an area covering at least two different water masses and an algal bloom, using a combination of techniques. Catalytic cathodic stripping voltammetry was used to measure the concentrations of reactive iron (Fe_R) and total iron (Fe_T) in unfiltered samples, while dissolved iron (Fe_D) was measured by GFAAS after extraction of filtered sea water. Fe_R was defined by the amount of iron that complexed with 20 μM 1-nitroso-2-napthol (NN) at pH 6.9. Fe_T was determined after UV-digestion at pH 2.4. Concentrations of natural organic iron complexing ligands and values for conditional stability constants, were determined in unfiltered samples by titration. Mean concentrations of 1.3 nM for Fe_R, 10.0 nM for Fe_T and 1.7 nM for Fe_D were obtained for the area sampled. Fe_R concentrations increased towards the south of the area investigated, as a result of the increased influence of continental run off. Fe_R concentrations were found to be enhanced below the nutricline (below 40 m) as a result of the remineralisation of organic material. Enhanced levels of Fe_T were observed in some surface samples and in samples collected below 30 m at stations in the south of the area studied, thought to be a result of high concentrations of biogenic particulate material and the resuspended sediments respectively. Fe_D concentrations varied between values similar to those of Fe_T in samples from the north of the area to values similar to those of Fe_R in the south. The bloom was thought to have influenced the distribution of both Fe_R and Fe_T, but less evidence was observed for any influence on Fe_R and Fe_D. The concentration of organic complexing ligands, which could possibly include a contribution from adsorption sites on particulate material, increased slightly in the bloom area and in North Sea waters. Iron was found to be fully (99.9%) complexed by the organic complexing ligands at a pH of 6.9 and largely complexed (82–96%) at pH 8. The ligands were almost saturated with iron suggesting that the ligand concentration could limit the concentration of iron occurring as dissolved species.     

Production of methyl bromide and methyl chloride in laboratory cultures of marine phytoplankton II

Methyl halides (monohalomethanes), especially methyl bromide, are known to contribute significantly to ozone destruction in the stratosphere. Budgets of natural and anthropogenic methyl bromide suggest that marine organisms may be the source of a significant proportion of the total global production. Since phytoplankton are abundant in surface waters, they are obvious candidates. Cultures of nine phytoplankton species were grown in CO₂-enriched, nitrate-limited medium in sealed glass vessels. Species tested include Chaetoceros calcitrans, Isochrysis sp., Porphyridium sp., Synechococcus sp., Phaeodactylum tricornutum, Tetraselmis sp., Prorocentrum sp., Emiliania huxleyi and Phaeocystis sp. Methyl bromide (CH₃Br) and methyl chloride (CH₃Cl) concentrations were determined by bubbling the cultures with high-purity air, cryotrapping the effluent and analyzing it on a gas chromatograph with an electron capture detector. The Phaeocystis sp. samples were monitored with GCMS. Cell population, bacterial population, Chl a, pH, and nitrate concentration were monitored for periods of at least two weeks. CH₃Cl was produced by all cultures. CH₃Br was absent in Tetraselmis sp. and Isochrysis sp. cultures, but present in all the others. Methyl iodide (CH₃I) was present in most cultures but could not be quantified due to analytical limitations. CH₃I and CH₃Br production was fastest in stationary phase and continued long after cell division had ceased. Axeic cultures of Phaeocystis sp. achieved almost identical production rates of CH₃Cl and CH₃Br as xenic cultures of the same species. Species from tropical waters had faster CH₃Cl and CH₃Br production rates than temperate species. Scaling the observed production rates using global standing stock estimates for Chl a and particulate nitrogen indicate that phytoplankton can account for only a fraction of the CH₃Cl and CH₃Br believed to be produced in the ocean. Calculations based on the estimated global biomass of Phaeocystis sp. and E. huxleyi blooms show that their contribution is insignificantly small.     

Vertical profiles of nitrous oxide and dissolved oxygen in marine sediments

The whole core squeezing method was used to simultaneously obtain profiles of nitrous oxide (N₂O), nitrogenous nutrients, and dissolved oxygen in sediments of Koaziro Bay, Japan (coastal water), the East China Sea (marginal sea), and the central Pacific Ocean (open ocean). In the spring of Koaziro Bay, subsurface peaks of interstitial N₂O (0.5–3.5 cm depth) were observed, at which concentrations were higher than in the overlying water. This was also true for nitrate (NO₃⁻) and nitrite (NO₂⁻) profiles, suggesting that the transport of oxic overlying water to the depth through faunal burrows induced in situ N₂O production depending on nitrification. In the summer of Koaziro Bay, sediment concentrations of N₂O, NO₃⁻ and NO₂⁻ were lower than in the overlying water. In most East China Sea sediments, both N₂O and NO₃⁻ decreased sharply in the top 0.5–2 cm oxic layer (oxygen: 15–130 μM), which may have indicated N₂O and NO₃⁻ consumption by denitrification at anoxic microsites. N₂O peaks at subsurface depth (0.5–6.5 cm) implied in situ production of N₂O and/or its supply from the overlying water through faunal burrows. However, the occurrence of the latter process was not confirmed by the profiles of other constituents. In the central Pacific Ocean, the accumulation of N₂O and NO₃⁻ in the sediments likely resulted from nitrification. Nitrous oxide fluxes from the sediments, calculated using its gradient at the sediment–water interface and the molecular diffusion coefficient, were −45 to 6.9 nmolN m⁻² h⁻¹ in Koaziro Bay in the spring, −29 to −21 nmolN m⁻² h⁻¹ in the summer, −46 to 37 nmolN m⁻² h⁻¹ in the East China Sea, 0.17 to 0.23 nmolN m⁻² h⁻¹ in the equatorial Pacific, and <±0.2 nmolN m⁻² h⁻¹ in the subtropical North Pacific, respectively.     

Glacial–interglacial variations in Quaternary production of marine organic matter at DSDP Site 594, Chatham Rise, southeastern New Zealand margin

CaCO₃ and total organic carbon concentrations, organic matter C/N and carbon isotope ratios, and sediment accumulation rates in late Quaternary sediments from DSDP Site 594 provide information about glacial–interglacial variations in the delivery of organic matter to the Chatham Rise offshore of southeastern New Zealand. Low C/N ratios and nearly constant organic δ¹³C values of −23‰ indicate that marine production dominates organic matter supply in both glacial and interglacial times during oxygen isotope stages 1 through 6 (0–140 ka) and 17 through 19 (660–790 ka). Increased organic carbon mass accumulation rates in isotope stages 2, 4, 6, and 18 record enhanced marine productivity during glacial maxima. Excursions of organic δ¹³C values to ca. −29‰ in portions of isotope stage 2 suggest that the local concentration of dissolved CO₂ was occasionally elevated during the last glacial maximum, probably as a result of short periods of lowered sea-surface temperature. Dilution of carbonates by clastic continental sediment generally increases at this location during glacial maxima, but enhanced delivery of land-derived organic matter does not accompany the increased accumulation of clastic sediments.     

Evaluation of conditions along the grounding line of temperate marine glaciers: an example from Muir Inlet, Glacier Bay, Alaska

In the marine environment, stability of the glacier terminus and the location of subglacial streams are the dominant controls on the distribution of grounding-line deposits within morainal banks. A morainal bank complex in Muir Inlet, Glacier Bay, SE Alaska, is used to develop a model of terminus stability and location of subglacial streams along the grounding line of temperate marine glaciers. This model can be used to interpret former grounding-line conditions in other glacimarine settings from the facies architecture within morainal bank deposits.The Muir Inlet morainal bank complex was deposited between 1860 A.D. and 1899 A.D., and historical observations provide a record of terminus positions, glacial retreat rates and sedimentary sources. These data are used to reconstruct the depositional environment and to develop a correlation between sedimentary facies and conditions along the grounding line.Four seismic facies identified on the high-resolution seismic-reflection profiles are used to interpret sedimentary facies within the morainal bank complex. Terminus stability is interpreted from the distribution of sedimentary facies within three distinct submarine geomorphic features, a grounding-line fan, stratified ridges, and a field of push ridges. The grounding-line fan was deposited along a stable terminus and is represented on seismic-reflection profiles by two distinct seismic facies, a proximal and a distal fan facies. The proximal fan facies was deposited at the efflux of subglacial streams and indicates the location of former glacifluvial discharges into the sea. Stratified ridges formed as a result of the influence of a quasi-stable terminus on the distribution of sedimentary facies along the grounding line. A field of push ridges formed along the grounding line of an unstable terminus that completely reworked the grounding-line deposits through glacitectonic deformation.Between 1860 A.D. and 1899 A.D. (39 years),

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m³ of sediment were deposited within the Muir Inlet morainal bank complex at an average annual sediment accumulation rate of

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m³/a. This rate represents the annual sediment production capacity of the glacier when the Muir Inlet drainage basin is filled with glacial ice.