摄食紫菜粉等4种单一饵料的蚤状潘脂肪酸组成的比较

用GC／MS法分析比较了紫菜粉、小球藻、酵母、Banta液（牛粪1．5g＋干稻草2g＋沃土20g＋水1000cm3）4种食物条件下蚤状潘的脂肪酸组成．结果表明：4种食物培养下,蚤状潘的总脂含量依次为39．80、60．10、44．60、52．30mg／g．一共检测出脂肪酸14种,其中8种饱和脂肪酸（SFA）,2种单不饱和脂肪酸（MUFA）,4种多不饱和脂肪酸（PUFA）．紫菜粉培养组与小球藻组PUFA含量显著高于酵母组和Banta液组（P〈0．05）,占总脂肪酸的1／3以上,酵母组MUFA质量分数最高（P〈0．05）,达55．73％,Banta液组以SFA质量分数最高（P〈0．05）,为52．45％．其中紫菜粉组的PUFA中缺乏C18：3,但C20：5（EPA）和C20：4（AA）质量分数高达22．67％和9．02％是小球藻组的1．6倍和4．5倍（P〈0．05）,而且EPA和AA的实际含量也显著高于小球藻组（P〈0．05）,达到9．02mg／g和3．59mg／g;比较得出,紫菜粉培养组的20碳以上必需不饱和脂肪酸含量丰富,明显高于其他3组．本实验证实蚤状潘的脂肪酸组成与食物脂肪酸成正相关．分析认为,用紫菜粉培养枝角类用于海水育苗会取得更佳的营养效果．     

Lipid characteristics of a seep clam,Mesolinga soliditesta: Comparison with those of two coastal clams,Meretrix lamarckii and Ruditapes philippinarum

The lipids and fatty acids of two coastal clams, Meretrix lamarckii and Ruditapes philippinarum, collected at 5 and 1 m of depth, and a seep clam, Mesolinga soliditesta, collected at 331 m of depth, were examined to assess their lipid physiology and trophic relationship with their diets. The major fatty acids of lipids in Mer. lamarckii and R. philippinarum were 14:0, 16:0, 18:0, 16:1n-7, 18:1n-9, 18:1n-7, 20:4n-6, 20:5n-3, and 22:6n-3, while those of Mes. soliditesta were 16:0, 18:0, 16:1n-7, 18:1n-7, 20:1n-7, 20:1n-13, 20:2n-7, 15 (Δ5,13-20:2), and 22:2n-7,15 (Δ7,15-22:2). The major polyunsaturated fatty acids (PUFAs) in the Mer. lamarckii and R. philippinarum lipids consisted of various n-3 and n-6 long-chain (LC) PUFAs, such as 20:4n-6, 22:4n-6, 20:5n-3, 22:5n-3, and 22:6n-3, while those in Mes. soliditesta muscle and viscera included various n-4 family PUFAs (18:3n-7, 18:4n-4, 20:2n-7, and 20:3n-7) with limited kinds of n-3 and n-6 PUFAs (20:4n-6 and 20:5n-3). These findings indicate that, like other common shallow-water clams, Mer. lamarckii and R. philippinarum ingest phytoplanktonic n-3 and n-6 LC-PUFAs, whereas Mes. soliditesta utilizes limited kinds of n-3 and n-6 LC-PUFAs. In contrast to the other two bivalves species, Mes. soliditesta yielded various n-4 and n-7 (n-4/n-7) PUFAs, which were assimilated from the chemosynthetic symbionts. The high diversity of PUFAs contained in the Mes. soliditesta lipids (n-3, n-4 family, and n-6 PUFAs) suggests that this species mixotrophically utilized both photosynthetic products and vent chemosynthetic nutrition derived from geothermal energy.     

长肋日月贝的营养成分分析及评价

对野生长肋日月贝(Amusium pleuronectes)的闭壳肌和贝肉其他部分的基本营养成分进行分析.结果表明:闭壳肌的平均质量分数为18.13%±2.15%,超过优良养殖海湾扇贝"中科红".闭壳肌的蛋白质质量比(干质量)为847.62 g/kg,贝肉其他部分蛋白质质量比为662.50 g/kg.必需氨基酸与非必需...     

黑海参脂肪酸的气相色谱/质谱法分析

黑海参(Holothuria atra)体壁经Folch 法提取总脂, 用HCl-甲醇进行甲酯化处理, 以气相色谱/质谱法分析总脂中的脂肪酸组成。从黑海参中共分析出28 种化合物, 包括25 种脂肪酸甲酯和3 种脂肪醛二甲基缩醛。黑海参体壁中的饱和脂肪酸含量为22.93%, 以C_16:0(5.49%)和C_18:0(4.38%)为主; 不饱和脂肪酸含量为65.19%, 其中单不饱和脂肪酸33.86%, 主要为C_20:1(n-9)(15.90%); 多不饱和脂肪酸为31.33%, 主要为C_20:4(n-6)(19.57%)和C_20:5(n-3)(5.86%)。脂肪醛二甲基缩醛含量为7.28%, 表明黑海参体壁总脂中含有较丰富的缩醛型甘油酯。     

Constraining the genetic relationships of 25-norhopanes,hopanoic and 25-norhopanoic acids in onshore Niger Delta oils using a temperature-dependent material balance

Analysis of oil samples from the Niger Delta (Nigeria) revealed a range of structurally related hopanes, including 25-norhopanes, and hopanoic and 25-norhopanoic acids. 25-Norhopanes were detected in all medium and heavily biodegraded oils and were most abundant in the heavily degraded oils. Hopanoic acids (C₃₀-C₃₃) and 25-norhopanoic acids (C₃₀-C₃₁) were most abundant in moderately degraded oils and occurred in reduced concentration in heavily degraded oils but were absent from, or in trace concentration in, slightly degraded oils. Consideration of the structures suggests that 25-norhopanoic acids form via carboxylation of 25-norhopanes or demethylation of hopanoic acids. Mass balance for the onshore Niger Delta oils suggests that formation of 25-norhopanes operates independently of 25-norhopanoic acid formation and that 25-norhopanoic acids are likely transient intermediates for only a small proportion of the 25-norhopanes.     

Lipids and pigments in deep-sea surface sediments and interfacial particles from the Western Crozet Basin

Deep-sea sediment samples were collected in the Western Crozet Basin (Indian sector of the Southern Ocean) through Permanently Open Ocean Zone (POOZ), Polar Frontal Zone (PFZ) and Sub-Antarctic Zone (SAZ). Lipid class and fatty acid compositions were investigated to determine the sources and fate of organic matter in the first centimeter of sediment and, above this layer, in the fluff (when present) and particles in the overlying water. The total lipid content varied from 74 to 1033 μg l⁻¹ in the overlying particles and fluffs, and from 24 to 97 μg g⁻¹ dry mass (DM) in surficial sediments. Lipid composition was always dominated by phospholipids in the first centimeter of sediment and often in the overlying particles. The amount of phospholipids (labile compounds representative of fresh material) was compared to the amount of chlorophyll a (Chl a), another compound that is susceptible to rapid degradation. A strong N–S gradient was observed in the distribution of these two compounds, which was attributed to the contrasting hydrodynamic of the study area. The high sedimentation rate in POOZ resulted in better preservation of Chl a in this zone than in other zones of the Crozet Basin (PFZ and SAZ). Phospholipid fatty acids suggested the presence of viable as well as morphologically intact organisms, and these organisms consisted essentially of bacteria with some diatom cysts in the fluff of POOZ. These spores were able to grow in the culture, indicating that they were still viable. Despite the strong hydrodynamic variability, phospholipid fatty acids analysed from the deep-sea surficial sediments were never representative of plankton. This pointed to the extremely labile nature of the phospholipids originally present in planktonic material compared with Chl a, which was always found in overlying particles and surficial sediments.     

Phytopigments and fatty acids in the gut of the deposit-feeding heart urchin Echinocardium cordatum in the southern North Sea: Selective feeding and its contribution to the benthic carbon budget

As part of a broader study on benthic-pelagic coupling in the southern North Sea, specimens of the common heart urchin Echinocardium cordatum were sampled for analyses on phytopigments and fatty acids in their guts. Results were interpreted in the context of feeding and ecological functioning of the heart urchins in the benthic system. Ingestion selection factors for both component groups were relatively high, 5 to 9 for chlorophyll a and 9 to 130 for total fatty acids. The data point to at least partially different sources of the pigments and of the fatty acids. Next to algal detritus, small infauna relatively rich in fatty acids might be preferentially co-ingested with the detritus. Due to digestive breakdown and absorption, the concentrations of pigments and fatty acids were importantly decreased, indicating a rather high digestion efficiency for this subsurface deposit feeder, up to 80%. The results indicate that E. cordatum increases its energy acquisition by strong selectivity and a high digestive efficiency. Optimal foraging is likely to apply on deposit-feeding invertebrates in relatively food-rich coastal environments as much as it does in the food-poor deep-sea environment. Using chlorophyll a as a proxy for carbon, the contribution of the urchin population to the momentary benthic carbon budget was calculated at 7% to 42%.     

罗非鱼鱼鳞胶制备降血压胶原肽的工艺及酶解物活性

以罗非鱼鱼鳞胶为原料,制备对血管紧张素转换酶(ACE)有抑制活性的降血压肽。以水解度(DH)及ACE抑制率为指标,筛选水解鱼鳞胶的最适酶种,并对其水解工艺条件进行优化;采用超滤技术对所制备的降血压肽进行分离纯化,比较不同组分的ACE抑制率,测定高ACE抑制率组分的氨基酸组成,并运用MALDI-TOF-MS法分析其分子质量分布。结果表明,复合蛋白酶是水解鱼鳞胶最适酶种,在50℃、pH7.5、料液质量体积比1∶5、酶与底物质量比(mE/mS)1.5%条件下,酶解6 h,酶解液的ACE抑制作用最强,其水解度DH 73%,ACE的抑制率76.15%。酶解液经超滤分离所获得的分子质量小于2 000 u的组分对ACE抑制率最高,达83.15%;该组分的氨基酸主要含有Gly和Pro,含量分别为22.04%和11.40%;该组分分子质量范围为1 300~2 000 u。     

热处理对沙漠边缘土壤腐殖酸荧光性质及其与Cu(Ⅱ)络合作用的影响

通过荧光光谱法研究了80 ℃处理下沙漠边缘土壤腐殖酸荧光性质及其与Cu(Ⅱ) 络合行为的变化。热处理导致类富里酸的发射波长发生蓝移,类富里酸和类腐殖酸的荧光强度降低,它们与Cu(Ⅱ)络合的条件稳定常数（lg Ka）降低,结合常数（lg Kb）增加,腐殖酸中参与Cu(Ⅱ) 络合的荧光基团和位点数增多。研究表明,干旱区高温环境会导致腐殖酸结构及组成发生变化,从而影响Cu(Ⅱ) 在土壤中的迁移。     

Ice-free conditions in Novaya Zemlya 35 000–30 000 cal years B.P., as indicated by radiocarbon ages and amino acid racemization evidence from marine molluscs

Novaya Zemlya was covered by the eastern part of the Barents–Kara ice sheet during the glacial maximum of marine isotope stage 2 (MIS 2). We obtained ¹⁴C ages on 37 samples of mollusc shells from various sites on the islands. Most samples yielded ages in the range of 48–26 ¹⁴C Ky. Such old samples are sensitive to contamination by young ¹⁴C, and therefore their reliability was assessed using replicate analyses and amino acid geochronology. The extent of aspartic acid racemization (Asp D/L) indicates that many of the ¹⁴C ages are correct, whereas some are minimum ages only. The results indicate that a substantial part of Novaya Zemlya was ice-free about 35–27 ¹⁴C Kya, and probably even earlier. Corresponding shorelines up to >140 m a.s.l. indicate a large Barents–Kara ice sheet during early MIS 3. These results are consistent with findings from Svalbard and northern Russia: in both places a large MIS 4/3 Barents–Kara ice sheet is postulated to have retreated about 50 Kya, followed by an ice-free interstadial that lasted until up to ca. 25 Kya. The duration of the MIS 2 glaciation in Novaya Zemlya was calculated by applying the D/L values to a kinetic equation for Asp racemization. This indicates that the islands were ice covered for less than 3000 years if the basal temperature was 0^oC, and for less than 10 000 years if it was −5^oC.