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1.
潘萌  佟玲  田芹  宋淑玲 《岩矿测试》2023,(6):1165-1176
有机磷酸酯类阻燃剂广泛存在于环境中，长期接触会对生物体的生殖系统、免疫系统造成破坏，进而对人类健康产生影响，调查研究其在环境中的污染水平非常有必要，而多组分、同时、准确的分析技术是研究的基础，目前已有的分析方法在化合物种类和提取效率方面还有待提高。本文建立了一种分析土壤和沉积物中15种有机磷酸酯类阻燃剂的方法。新鲜样品采用加速溶剂萃取(ASE)直接提取，提取液用复合填料的固相萃取柱进行净化，再采用气相色谱-质谱(GC-MS)进行定性、定量分析。为了改善提取效率和净化效果等问题，针对土壤和沉积物样品基质的复杂性，实验中主要优化了样品的提取、净化条件：针对磷酸三(2-氯乙基)酯提取回收率低的问题，改进了样品制备方式，新鲜样品在有少量水的存在下直接提取，使得有机溶剂更好地与样品颗粒进行接触，显著提高了该化合物的提取效率；采用石墨化碳和氨基硅胶复合填料的固相萃取小柱对样品提取液进行净化，保障了复杂沉积物样品净化效果的有效性，同时选用5%甲苯的洗脱溶剂体系，能够提高磷酸三甲苯酯(TCP)在石墨化碳固相萃取柱上的洗脱效率，保证了净化过程的回收率。结果表明，目标化合物浓度在10.0～500.0ng/...  相似文献   

2.
土壤中持久性有机污染物分析的前处理方法   总被引：3，自引：2，他引：1  
对土壤样品的前处理技术进行了研究。采用加速溶剂萃取法(ASE)提取土壤中有机氯农药和多氯联苯类化合物,并且与索氏提取结果进行了对比,结果表明,ASE完全能取代传统的索氏提取方法。对固相萃取(SPE)柱净化的不同填料进行了实验筛选。比较了浓硫酸磺化法和SPE柱净化法对土壤中有机氯农药及多氯联苯的净化效果。优化了有机氯农药、多氯联苯凝胶渗透色谱(GPC)的净化条件。当样品基质比较复杂时,采用凝胶渗透色谱结合固相萃取柱的前处理方法,能得到很好的净化效果。土壤样品中持久性有机污染物采用加速溶剂提取结合固相萃取前处理过程的回收率为68%~106%,精密度小于7.7%。  相似文献   

3.
对土壤中14种有机氯农药的超声提取技术和磺化、固相萃取小柱两种净化方法进行系统研究。结果表明,超声提取节省提取时间,提高分析效率;磺化法和固相萃取小柱法都有净化作用,但磺化法使样品中的艾氏剂、狄氏剂和异狄氏剂全部损失;固相萃取小柱净化当丙酮-正己烷淋洗液体积比为1∶9、淋洗液收集8 mL时回收率>90%,干扰最小。方法检出限为0.63~2.59μg/kg,精密度(RSD,n=7)为1.17%~14.66%,基体加标平均回收率为82.78%~106.94%。方法用于生态地球化学调查评价批量土壤样品的实际分析,检测结果满足评价工作需要。  相似文献   

4.
研究了土壤中17种有机氯农药和8种多氯联苯组分的气相色谱分析方法。采用加速溶剂萃取技术提取,优化了萃取条件。提取液用固相萃取技术进行净化,采用20 mL含3%(体积分数)甲苯的正己烷-乙酸乙酯(体积比8∶2)进行淋洗,得到很好的净化效果。方法检出限在0.06~0.27μg/kg,线性范围在1.38~55.2 ng/mL,目标化合物的平均添加回收率在65%~97%,相对标准偏差(RSD,n=6)小于17.11%。方法快速、灵敏、准确,适合批量样品的分析。  相似文献   

5.
佟玲  杨佳佳  阎妮  吴淑琪 《岩矿测试》2014,33(2):262-269
动物组织样品油脂含量大、干扰杂质多,对其中低含量有机氯农药及多氯联苯的分析会造成较大程度的影响。针对动物组织样品基质复杂的特点,本文以二氯甲烷-丙酮（体积比为1：1）的溶剂体系,采用加速溶剂萃取技术对样品进行提取,在提取过程中尽量减少脂肪的共提出,然后采用凝胶渗透色谱技术去除样品中的大部分油脂,再结合弗罗里硅土为填料的固相萃取方法对样品进一步净化,能够达到充分去除油脂和小分子杂质的目的。采用气相色谱-质谱分析17种有机氯农药及7种指示性多氯联苯,各化合物的回收率在81.6%~113.4%之间,检出限在1.02~3.59 ng/g之间,技术指标优于部分国家标准。本方法改进了动物样品的净化效果,建立了凝胶渗透色谱结合固相萃取技术的净化方法,达到了样品快速自动提取、溶剂用量少、基质净化彻底的目的,降低了方法检出限,能够满足快速、准确检测动物组织中低含量持久性有机污染物的要求。  相似文献   

6.
影响12种壬基酚同分异构体液液萃取效率的因素研究   总被引：1，自引：1，他引：0  
壬基酚是一种新型持久性有机污染物,具有强烈的雌激素效应。近年来壬基酚对水体的污染备受国内外关注,因此实现水体中壬基酚的提取显得尤为重要。目前国内外对于壬基酚萃取效率的研究都是针对总量,对单独异构体萃取效率的研究极少。本文选用传统的液液萃取方法对壬基酚同分异构体进行提取,并进行GC-MS测试,对影响12种壬基酚同分异构体萃取效率的因素进行研究。通过实验比较不同萃取溶剂、萃取溶剂不同用量、不同盐度、不同pH条件下12种壬基酚同分异构体的回收率,研究优化了液液萃取壬基酚的条件。结果表明,选择二氯甲烷作为萃取溶剂,且用量为60 mL,调节水样pH1,氯化钠用量为60 g时,12种壬基酚同分异构体的萃取效率达到88.7%~101.2%,精密度(RSD,n=3)为10.3%~13.6%,检出限9.0~41.4 ng/L。该萃取效率能够达到USEPA规定的回收率在70%~130%范围内,已用于水样中壬基酚的提取。  相似文献   

7.
佟玲  田芹  杨志鹏  潘萌 《岩矿测试》2020,39(4):587-596
近年人工合成麝香在环境中污染状况加剧,该类化合物具有潜在致癌和环境激素作用,对人类健康构成了威胁,因此越来越受到科学工作者的重视。水和土壤等环境样品中的人工合成麝香检测技术发展迅速,并朝着快速绿色的方向发展。人工合成麝香在沉积物中的浓度达到了几个到几千个ng/g的水平,但对于沉积物复杂基质中的多种类人工合成麝香,采取同步提取与净化,并快速分析的方法还有待研究。本文建立了沉积物样品中硝基麝香、多环麝香和大环麝香共三类、14种典型人工合成麝香的快速分析方法。通过实验优化了提取溶剂、提取温度、在线净化吸附剂等条件,大大降低了样品的前处理成本。最终确定样品采用加速溶剂萃取,萃取池中依次装入净化吸附剂(0.4g GCB和1.0g SAX)及5.0g沉积物样品,在80℃条件下采用提取溶剂正己烷-丙酮(4∶1,V/V)循环提取2次,提取液浓缩后采用气相色谱-三重四极杆串联质谱(GC-MS/MS)进行测定。结果表明:14种目标化合物的线性范围为5～200ng/mL,平均添加回收率为70.6%～121.5%,相对标准偏差(RSD,n=7)为0.97%～19.5%。替代物回收率为72.2%～116.8%,方法检出限为硝基麝香0.10～0.19ng/g,多环麝香0.09～0.14ng/g,大环麝香0.11～1.93ng/g。该方法能够满足复杂基质沉积物样品的分析要求。  相似文献   

8.
王瑞敏 《岩矿测试》2011,30(3):295-298
样品采用王水溶解,二氯化锡还原,泡沫塑料富集,用Re作内标,电感耦合等离子体质谱法同时测定土壤中超痕量金、铂、钯。在盐酸-二氯化锡体系中,盐酸酸度为15%,二氯化锡浓度为45 g/L,吸附时间30 min时吸附效果明显,吸附温度为25℃时吸附率相对稳定。方法检出限Au为0.21 ng/g,Pt为0.18 ng/g,Pd为0.16ng/g,方法加标回收率Au为91.3%~97.8%,Pt为92.0%~96.7%,Pd为96.0%~101.6%。该方法用于测定国家一级标准物质,线性范围宽、重现性好,结果准确可靠,样品处理简便、快速。  相似文献   

9.
建立了沉积物样品中17种有机氯农药和8种多氯联苯持久性有机污染物的气相色谱分析方法。针对沉积物样品基质复杂、含有大量硫干扰的特点,重点研究了前处理技术。采用加速溶剂提取(ASE)技术提取样品中的有机污染物,比较了加入铜粉后ASE在线除硫和超声波提取除硫的效果。结果表明,加入铜粉ASE提取不能完全去除硫的干扰,需进一步采用超声波提取10 min除硫才能大大减少杂质对目标化合物的干扰。沉积物样品中的色素类及小分子干扰物质采用凝胶渗透色谱结合固相萃取技术进行净化,满足了气相色谱-电子捕获检测器分析的要求。25种化合物的平均添加回收率为68%～131%,方法精密度(RSD,n=6)小于22.3%,检出限为0.10～0.51μg/kg。建立的样品前处理技术净化彻底,适合用于不同地区、不同类型的沉积物样品气相色谱分析。  相似文献   

10.
脂肪酸是沉积物中含量最丰富的脂类标记物之一,其存在形式主要有游离态脂肪酸和结合态脂肪酸。游离态脂肪酸可由溶剂直接提取,结合态脂肪酸是在已提取出游离态脂肪酸的沉积物残渣中加入酸碱加热后再用溶剂提取。加速溶剂萃取技术(ASE)因成本低和操作毒性小,在脂肪酸研究中得到了广泛的应用。本文采集东海近海海域沉积物作为研究样本,由于其中游离态脂肪酸含量丰富,而结合态脂肪酸含量过低,测定结果精密度差,难以作为方法研究对象,因此主要针对游离态脂肪酸应用加速溶剂萃取法进行提取,研究了各种实验条件,包括萃取剂、萃取温度、静态萃取时间和循环次数的选择与优化。分析结果表明,甲醇-二氯甲烷(V:V,1:3)更适合作为萃取剂;随着萃取温度、静态萃取时间、循环次数的增加,不同类型脂肪酸的提取效率各不相同,以涵盖碳原子数最多为先决条件,以脂肪酸的萃取效率最大化为依据,确定了加速溶剂萃取的实验条件是:萃取温度110℃,静态提取时间10 min,循环3次。用这种处理方法5次测定沉积物样品中游离态脂肪酸的精密度为3.3%~19.0%,其替代物回收率为72.2%~104.6%。该方法应用于分析实际海洋沉积物样品,相比于传统的索氏提取法,流程简单,极大地提高了工作效率。  相似文献   

11.
To assess the effects of river damming on dissolved inorganic carbon in the Jialing River, a total of 40 water samples, including inflow, outflow, and stratified water in four cascade reservoirs (Tingzikou, Xinzheng, Dongxiguan, Caojie) were collected in January and July, 2016. The major cations, anions, and δ13CDIC values were analyzed. It was found that the dissolved compositions are dominated by carbonate weathering, while sulfuric acids may play a relatively important role during carbonate weathering and increasing DIC concentration. Different reservoirs had variable characteristics of water physiochemical stratification. The DIC concentrations of reservoir water were lower in summer than those in winter due to the dilute effects and intensive aquatic photosynthesis, as well as imported tributaries. The δ13CDIC values in Tingzikou Reservoir were higher during summer than those in winter, which indicated that intensive photosynthesis increased the δ13CDIC values in residual water, but a similar trend was not obvious in other reservoirs. Except for in Xinzheng Reservoir, the δ13CDIC values in inflow and outflow reservoir water were lower than those in the surface water of stratified sampling in summer. For stratified sampling, it could be found that, in summer, the Tingzikou Reservoir δ13CDIC values significantly decreased with water depth due to the anaerobic breakdown of organic matter. The significant correlation (p < 0.01 or 0.05) between the DIC concentrations, the δ13CDIC values and anthropogenic species (Na++K+, Cl–, \({\text{SO}}_{4}^{2 - }\)and \({\text{NO}}_{3}^{ - }\)) showed that the isotope composition of DIC can be a useful tracer of contaminants. In total, Tingzikou Reservoir showed lacustrine features, Xinzheng Reservoir and Dongxiguan Reservoir had “transitional” features, and Caojie Reservoir had a total of “fluvial” features. Generally, cascade reservoirs in the Jialing River exhibited natural river features rather than typical lake features due to characteristics of reservoir water in physiochemical stratification, spatiotemporal variations of DIC concentrations and isotopic compositions. It is evident that the dissolved inorganic carbon dynamics of natural rivers had been partly remolded by dam building.  相似文献   

12.
Stromatolites forming today on a small scale in hydrothermal environments are chemical and biological analogues of much larger Precambrian formations. Carbon isotopic composition varied as a function of CO2 concentration, pH, and species composition. Stratiform, layered stromatolites grew in silica-depositing springs at 55° to 70°C; they consisted mainly of a unicellular alga, Synechococcus, and a filamentous, photosynthetic bacterium, Chloroflexus. These thermophiles become enriched in 12C as the concentration of carbon dioxide in the effluent waters increases. At a concentration of 40 ppm total inorganic C, and δ13C of organic carbon was ～ ?12%., whereas at 900 ppm total inorganic C, the δ13C of similar species was ～ ?25%.. Conical stromatolites or conophytons (principally a filamentous, blue-green alga Phormidium and Chloroflexus) grew at 40°-55°C. In older, broader conophytons, Chloroflexus was the dominant organism. Their δ13C values were ～ ?18%. in a variety of hot springs. In carbonate-depositing springs, i.e., carbon dioxide saturated, conophytons and stromatolites consisting of a variety of blue-green algae and photosynthetic bacteria had the most negative δ13C values (to ?30%.). These carbon isotope ratios are directly comparable to carbon isotope ratios of kerogen from Precambrian stromatolites. The presence and activity of methanogenic bacteria or heterotrophic, aerobic and anaerobic bacteria did not alter significantly the δ13C of the original organic matter.The hydrogen isotopic fractionation between thermophilic organisms and water is 0 to ?74 for temperatures of 85° to 46°C, respectively. Acidophilic algae fractionated hydrogen isotopes to a lesser extent than did the photosynthetic organisms inhabiting neutral pH springs. Because organic matter retains some of its original isotopic signature, relationships of CO2 levels, pH, temperature, and species composition between modern stromatolites and their environment and those of the Precambrian can be inferred.  相似文献   

13.
Paired organic and carbonate carbon isotope compositions of Late Permian Wujiaping (吴家坪) and Dalong (大隆) formations at Shangsi (上寺), Northeast Sichuan (四川) were analyzed by MAT 251. An abrupt negative excursion in the two isotope records was observed in the middle part of Dalong Formation, in association with a drop in the carbon isotope difference of the two records and an increase of total organic carbon (TOC) content. The negative drop of the paired carbon isotope records issuggestive of the input of 12C-enriched CO2. The molecular ratios of pristane to phytane and dibenzothiophene to phenanthrene indicate the anoxic condition in this interval. The enhanced TOC content is indicative of the elevated preservation of organic matter due to the anoxic condition. These isotopic and organic geochemical data probably infer the occurrence of the upwelUng in this interval. The additional contribution of volcanism activity observed in South China cannot be excluded to the input of 12C-enriched CO2 and the negative shifts in carbon isotope composition of bulk organic matter and carbonate.  相似文献   

14.
We have compared detailed planktonic and benthonic foraminiferal carbon and oxygen isotope records from the Palaeocene and early Eocene successions at DSDP Site 577 (Shatsky Rise, North Pacific), a composite section derived from DSDP Leg 74 sites (Walvis Ridge, South Atlantic) and a composite section from ODP Leg 113 sites (Maud Rise, Weddell Sea). The δ13C records of Palaeocene and early Eocene Foraminifera at Site 577 and the Leg 74 sites show that an increase in δ13C values in surface waters at 64 Ma (end of Zone P1) resulted in increased vertical carbon isotope gradients (δ13C) between surface and deeper dwelling planktonic foraminifera, and between surface-dwelling planktonics and benthonic foraminifera which became progressively steeper until the iniddle Late Palaeocene (Zone P4). This steepening also occurs in the latest Palaeocene of the composite Leg 113 section and can be explained by an increase in surface ocean productivity. This increase in productivity probably resulted in an expansion of the oxygen minimum zone (OMZ). Benthonic δ13C values increased during the late Palaeocene in Site 577 and the composite Leg 74 section, suggesting that the Palaeocene carbon isotope maximum was composed of both within-ocean reservoir (increased surface water productivity) and between-reservoir (organic carbon burial) ftactionation effects. The benthonic δ13C increase lags the surface ocean δ13C increase in the early Palaeocene (63–64 Ma) suggesting that surface water productivity increase probably led an increase in the burial rate of organic carbon relative to carbonate sedimentation. Moreover, inter-site δ13C comparisons suggest that the locus of deep to intermediate water formation for the majority of the Palaeocene and the earliest Eocene was more likely to have been in the high southern latitudes than in the lower latitudes. Oxygen isotope data show a decline in deeper water temperatures in the early and early late Palaeocene, followed by a temperature increase in the late Palaeocene and across the PalaeoceneEocene boundary. We speculate that these changes in deeper water temperatures were related to the flux of CO2 between the oceans and the atmosphere through a mechanism operating at the high southern latitudes.  相似文献   

15.
High resolution carbon isotope analyses of carbonate and organic carbon from Meishan, South China showed that the variation of δ13Ccarb is marked by three large positive excursions during the Changhsingian (end-Permian). Carbon isotope stratigraphy during this stage shows three cyclic intervals in δ13Ccarb, with two cycles corresponding to the lower (Paleofusulinid minima Zone) and one corresponding to the upper Changhsingian (P. sinensis Zone). The large positive δ13Ccarb excursions indicate episodes of enhanced burial of isotopically light or-ganic carbon, presumably in response to deep-water anoxia episodically extending into shallow water with the rise of sea level. The organic carbon during the Changhsingian is distinguished into two groups, and the δ13Corg of each group parallels (separately) the more detailed profile of δ13Ccarb, strongly showing that the values of fractionation Δ13Ccab-org remain relatively constant, with only two intervals with anomaly. The enhanced fractionation Δ13Ccab-org with large negative δ13Corg excursions apparently indicates significant inputs from sulfide-oxidizing bacteria and green sulfur bacteria, notably at bed 24 just predating mass extinction. Our evidence appears to support that the ex-tended euxinic water is possible for the main pulse of mass extinction at the end-Permian.  相似文献   

16.
热分层效应控制的水库水体氢氧同位素特征   总被引：1，自引：0，他引：1       下载免费PDF全文
为掌握水库热分层与氢氧同位素空间分布的关系,研究了广西兴安县五里峡水库夏季氢氧同位素空间分布特征及影响因素。研究表明:①五里峡水库夏季出现明显的热分层,库表层至-5 m为表水层,-5 m至-20 m为温跃层,-20 m以下为底温层;②五里峡水库δ18O、δD值沿大气降水线分布,但均落在桂林市大气降水线右下方,其线性方程为δD=4.66δ18O-10.85（R2=0.76）,其斜率与全球大气降雨线（GMWL）和桂林市降雨线（CLMWL）的斜率和截距差异明显,表明五里峡水库主要由降水补给,但在补给五里峡水库前已经过了强烈的蒸发作用和水岩作用;③ δ18O、δD随水深的增加逐渐偏负,具有表水层 > 入库水体 > 温跃层 > 底温层 > 出库水体（>表示偏正）的垂向分布特征。分析认为入库水体氢氧同位素的季节变化和蒸发作用随深度增加而降低是五里峡水库夏季分层期间水体氢氧同位素垂向变化的主要影响因素。  相似文献   

17.
采用水化学仪器自动记录、现场滴定和样品碳氧稳定同位素测试相结合等方法,对云南中甸白水台钙华景区的水化学和碳氧稳定同位素特征进行了综合分析。主要结论是:形成白水台钙华的泉水具有很高的钙和重碳酸根离子浓度,相应地,泉水的CO2分压显著高于土壤生物成因所能产生的CO2分压。结合泉水出露的地质条件及其碳稳定同位素特征(δ13C=-1.23‰)的分析,进一步发现,高CO2分压主要与深部地热成因的CO2有关,而非原来普遍认为的“是温暖湿润气候的产物”。可见,白水台钙华属于热成因类钙华。由此,根据白水台不同时代钙华氧稳定同位素组成的差异,对钙华形成时的水温进行了计算。结果发现自白水台钙华形成以来,水温变化高达11℃,即从最老(<35万年)钙华形成时的21℃降至现在的10℃。这可能与本地区强烈抬升导致的气温降低有关,也可能反映出地热对水温的影响在降低。此外,本文对用热成因类钙华进行古环境重建研究中值得注意的问题也做了讨论。这些问题包括放射性碳测年中“死碳”(来自深部碳酸盐碳和深部CO2)的干扰及由深源CO2和CO2自水中逸出导致的钙华13C富集,后者在利用类似热成因碳酸盐沉积的δ13C进行古植被重建时也是必须考虑的问题  相似文献   

18.
Bosten Lake is a mid-latitude lake with water mainly supplied by melting ice and snow in the Tianshan Mountains. The depositional environment of the lake is spatially not uniform due to the proximity of the major inlet and the single outlet in the western part of the lake. The analytical results show that the carbon and oxygen isotopic composition of recent lake sediments is related to this specific lacustrine depositional environment and to the resulting carbonate mineralogy. In the southwestern lake region between the Kaidu River inlet and the Kongqi River outlet, carbon isotope composition (δ13C) values of the carbonate sediment (?1‰ to ?2‰) have no relation to the oxygen isotope composition of the carbonate (δ18O) values (?7‰ to ?8‰), with both isotopes showing a low variability. The carbonate content is low (<20%). Carbonate minerals analyzed by X-ray diffraction are mainly composed of calcite, while aragonite was not recorded. The salinity of the lake water is low in the estuary region as a result of the Kaidu River inflow. In comparison, the carbon and oxygen isotope values are higher in the middle and eastern parts of the lake, with δ13C values between approximately +0.5‰ and +3‰, and δ18O values between ?1‰ and ?5‰. There is a moderate correlation between the stable oxygen and carbon isotopes, with a coefficient of correlation r of approximately 0.63. This implies that the lake water has a relatively short residence time. Carbonate minerals constitute calcite and aragonite in the middle and eastern region of the lake. Aragonite and Mg–calcite are formed at higher lake water salinity and temperatures, and larger evaporation effects. More saline lake water in the middle and eastern region of the lake and the enhanced isotopic equilibrium between water and atmospheric CO2 cause the correlating carbon and oxygen isotope values determined for aragonite and Mg–calcite. Evaporation and biological processes are the main reasons for the salinity and carbonate mineralogy influence of the surface-sediment carbonate in Bosten Lake. The lake water residence time and the CO2 exchange between the atmosphere and the water body control the carbon and oxygen isotope composition of the carbonate sediment. In addition, organic matter pollution and decomposition result in the abnormally low carbon isotope values of the lake surface-sediment carbonate.  相似文献   

19.
We examined stable carbon isotope fractionation in biosynthesis of fatty acids of a piezophilic bacterium Moritella japonica strain DSK1. The bacterium was grown to stationary phase at pressures of 0.1, 10, 20, and 50 MPa in media prepared using sterile-filtered natural seawater supplied with glucose as the sole carbon source. Strain DSK1 synthesized typical bacterial fatty acids (C14-19 saturated, monounsaturated, and cyclopropane fatty acids) as well as long-chain polyunsaturated fatty acids (PUFA) (20:6ω3). Bacterial cell biomass and individual fatty acids exhibited consistent pressure-dependent carbon isotope fractionations relative to glucose. The observed ΔδFA-glucose (−1.0‰ to −11.9‰) at 0.1 MPa was comparable to or slightly higher than fractionations reported in surface bacteria. However, bulk biomass and fatty acids became more depleted in 13C with pressure. Average carbon isotope fractionation (ΔδFA-glucose) at high pressures was much higher than that for surface bacteria: −15.7‰, −15.3‰, and −18.3‰ at 10, 20, and 50 MPa, respectively. PUFA were more 13C depleted than saturated and monounsaturated fatty acids at all pressures. The observed isotope effects may be ascribed to the kinetics of enzymatic reactions that are affected by hydrostatic pressure and to biosynthetic pathways that are different for short-chain and long-chain fatty acids. A simple quantitative calculation suggests that in situ piezophilic bacterial contribution of polyunsaturated fatty acids to marine sediments is nearly two orders of magnitude higher than that of marine phytoplankton and that the carbon isotope imprint of piezophilic bacteria can override that of surface phytoplankton. Our results have important implications for marine biogeochemistry. Depleted fatty acids reported in marine sediments and the water column may be derived simply from piezophilic bacteria resynthesis of organic matter, not from bacterial utilization of a 13C-depleted carbon source (i.e., methane). The interpretation of carbon isotope signatures of marine lipids must be based on principles derived from piezophilic bacteria.  相似文献   

20.
Stable oxygen and carbon isotope ratios (δ18O and δ13C, respectively) of a planktonic foraminiferal species (Globigerinoides sacculifer) and marble carbonate were measured with and without a variety of pretreatments like ultrasonication, soaking in H2O2, methanol and roasting under vacuum. Additionally, organic matter - carbonate mixtures were also analysed with and without the above pretreatments. No significant difference was found in the isotope ratios of treated and untreated samples. It appears that most of the pretreatments may not be necessary when dealing with planktonic foraminifera, especially G. sacculifer. Analysis of two different size fractions (> 400 μm and 250–400 μm) of this species reveals that the smaller size fraction is enriched in 18O and depleted in 13C relative to the bigger size fraction. It is therefore necessary to choose a proper size fraction for isotopic analyses.  相似文献   

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