预处理及保存方法对浮游动物碳、氮稳定同位素比值的影响

研究了不同预处理及保存方法对浮游动物碳、氮稳定同位素比值的影响.结果表明:未清养的舌状叶镖水蚤PhyHodiaptomus tunguidus与清养3h的相比δ¹³C和δ¹⁵N的差异均不显著,但肠道内含物造成了重复样品间的较大偏差;去除脂肪后的舌状叶镖水蚤δ¹³C和δ¹⁵N均显著升高;经甲醇保存后,舌状叶镖水蚤和奥氏秀体溞Diaphanosoma orghidani transamurensis的δ¹³C均有所升高,但不显著;经乙醇保存后,舌状叶镖水蚤δ¹³C显著升高,而奥氏秀体溞的δ¹³C也有所升高但不显著;经过甲醛保存后,舌状叶镖水蚤和奥氏秀体溞的δ¹³C降低,但不显著;冰冻保存使奥氏秀体溞的δ¹³C显著降低,而使舌状叶镖水蚤的δ¹³C也有所降低但不显著.四种保存方法对舌状叶镖水蚤和奥氏秀体溞的δ¹⁵N都没有显著影响.在进行不同研究间的比较时,必须考虑样品保存与处理方法造成的差异.同时,食物网结构的稳定同位素研究有待建立统一的样品保存与处理方法.     

Technical Note: Calcium and carbon stable isotope ratios as paleodietary indicators

Calcium stable isotope ratios are hypothesized to vary as a function of trophic level. This premise raises the possibility of using calcium stable isotope ratios to study the dietary behaviors of fossil taxa and to test competing hypotheses on the adaptive origins of euprimates. To explore this concept, we measured the stable isotope composition of contemporary mammals in northern Borneo and northwestern Costa Rica, two communities with functional or phylogenetic relevance to primate origins. We found that bone collagen δ¹³C and δ¹⁵N values could differentiate trophic levels in each assemblage, a result that justifies the use of these systems to test the predicted inverse relationship between bioapatite δ¹³C and δ⁴⁴Ca values. As expected, taxonomic carnivores (felids) showed a combination of high δ¹³C and low δ⁴⁴Ca values; however, the δ⁴⁴Ca values of other faunivores were indistinguishable from those of primary consumers. We suggest that the trophic insensitivity of most bioapatite δ⁴⁴Ca values is attributable to the negligible calcium content of arthropod prey. Although the present results are inconclusive, the tandem analysis of δ⁴⁴Ca and δ¹³C values in fossils continues to hold promise for informing paleodietary studies and we highlight this potential by drawing attention to the stable isotope composition of the Early Eocene primate Cantius. Am J Phys Anthropol 154:633–643, 2014. © 2014 Wiley Periodicals, Inc.     

Tracing prey origins,proportions and feeding periods for predatory beetles from agricultural systems using carbon and nitrogen stable isotope analyses

Predatory beetles are an important component of the natural enemy complex that preys on insect pests such as aphids within agroecosystems. Tracing diet origins and movement of natural enemies aids understanding their role in the food web and informs strategies for their effective conservation. Field sampling and laboratory experiments were carried out to examine the changes of carbon and nitrogen stable isotope ratios (δ¹³C and δ¹⁵N) among crops (cotton and maize), pests (cotton and maize aphids), and between wing and abdomen of predatory beetles, Propylea japonica, and to test the hypothesis that prey origins, proportions and feeding periods of the predatory beetles can be deduced by this stable isotope analysis. Results showed that the δ¹³C values both in wing and abdomen of adult P. japonica were changing from a C₃- to a C₄-based diet of aphids reared on maize or cotton, respectively; the isotope ratio of their new C₄ substrates were detectable within 7 days and the δ¹⁵N values began to reflect their new C₄ substrates within 3 days. The relationship between δ¹³C and δ¹⁵N values of P. japonica adults in wing or abdomen and diets of aphids from a C₃-based resource transitioning to a C₄-based resource were described best in linear or quadratic equations. Results suggest that integrative analysis of δ¹³C and δ¹⁵N values can be regarded as a useful method for quantifying to trace prey origins, proportions of diets and feeding periods of natural enemies. The results can provide quantifying techniques for habitat management of natural enemies.     

Spatial variability of stable carbon and nitrogen isotope ratios in a Mediterranean coastal lagoon

Exploring the trophic pathway of organic matter within the Mauguio lagoon (southern France, western Mediterranean), we found spatial differences in the isotopic composition (both δ¹³C and δ¹⁵N values) of organic matter sources (primary producers, particulate and sedimentary organic matter), which were mirrored in the upper trophic levels (invertebrates and fish). On average, δ¹³C was heavier by about 1.5–2‰ in the location under marine influence than in the sites influenced by freshwater discharge. The opposite trend was found for δ¹⁵N, which attained maximum values in the north-central zone influenced by freshwater delivery. For both C and N stable isotope ratios, the highest spatial variability was found in organic matter sources (2–3‰), while invertebrates and fish exhibited less variability (\~1–2‰). The differences observed may be related to both anthropogenic (wastewater input) and natural (marine vs. terrestrial inputs) factors. Discharge of wastewater, which affects the innermost location, generally determines an increase in the relative abundance of ¹⁵N. In addition, terrestrially derived nutrients and organic matter, which also affect the innermost location, are known to determine a shift towards ¹³C-depleted values. Our results substantiate the finding that the analysis of carbon and nitrogen stable isotopes can help in elucidating origin and fate of organic matter in coastal lagoons, which are characterised by a great spatial variability and complexity.     

天津沼泽湿地芦苇叶片的碳稳定同位素比值分布特征及其环境影响因素

天津芦苇(Phragmites australis)沼泽具有重要的生态功能。目前天津地区水体咸化、氮污染和水资源短缺问题严重, 显著影响了芦苇湿地的植物生理生态过程。植物稳定碳同位素组成(碳稳定同位素比值(δ¹³C))能够记录与植物生长过程相关联的环境变化信息, 反映植物对环境变化的生理生态适应特性。该研究调查了天津七里海、北大港和大黄堡湿地芦苇叶片的δ¹³C分布特征, 探讨了影响该地区叶片δ¹³C值变化的主要因素。研究表明: 1)天津芦苇湿地植物叶片δ¹³C的变化范围在-26.3‰ - -23.6 ‰之间, 平均值为-25.8‰; 2)芦苇叶片δ¹³C与底泥相对含水量呈显著负相关关系, 与底泥有效氮和全氮含量呈显著正相关关系, 而与底泥盐度和磷含量没有显著相关关系; 水分条件和底泥氮营养状况是影响叶片的δ¹³C值变化的主要因素; 3)淹水条件下, 芦苇叶片δ¹³C与叶片质量氮含量呈显著正相关关系, 与叶碳氮比呈显著负相关关系, 8月份七里海湿地干涸打破了此相关关系。当前环境压力下, 天津沼泽湿地干涸极大地改变了芦苇的氮、水平衡和植物对水、氮资源的利用策略, 而湿地干涸对该过程的影响要高于盐度和氮负荷增加。     

Detection of breastfeeding and weaning in modern human infants with carbon and nitrogen stable isotope ratios

Carbon ((13)C/(12)C) and nitrogen ((15)N/(14)N) stable isotope ratios were longitudinally measured in fingernail and hair samples from mother-infant pairs where infants were exclusively breastfed (n = 5), breast- and formula-fed (n = 2), or exclusively formula-fed (n = 1) from birth. All exclusively breastfed infants had a dual enrichment in carbon ( approximately 1 per thousand) and nitrogen ( approximately 2-3 per thousand) when compared to maternal values. In contrast, breast- and formula-fed subjects had reduced enrichments compared to exclusively breastfed subjects, and the exclusively formula-fed infant showed no increase in delta(13)C or delta(15)N values. This finding of a carbon trophic level effect in breastfeeding infants suggests that (13)C-enrichments of approximately 1 per thousand in archaeological populations are not necessarily the result of the consumption of C(4)-based weaning foods such as maize or millet. During the weaning process, the delta(13)C results for breastfed infants declined to maternal levels more rapidly than the delta(15)N results. This suggests that delta(13)C values have the potential to track the introduction of solid foods into the diet, whereas delta(15)N values monitor the length of time of breast milk consumption. These findings can be used to refine the isotopic analysis of breastfeeding and weaning patterns in past and modern populations.     

基于碳、氮稳定同位素研究胶州湾普氏栉虾虎鱼的摄食习性

普氏栉虾虎鱼属于小型暖温性底层鱼类,是胶州湾鱼类群落中的优势种之一,在胶州湾食物网和生态系统中发挥着重要作用.本文应用碳、氮稳定同位素技术,基于胶州湾渔业资源底拖网调查采集的样品,对普氏栉虾虎鱼的摄食习性进行了研究.结果表明: 胶州湾普氏栉虾虎鱼的δ¹⁵N值范围为11.24‰～13.99‰,平均值为(12.70±0.70)‰,δ¹³C值范围为-20.67‰～-18.46‰,平均值为(-19.08±0.36)‰;各体长组的营养级范围为3.49～3.76,平均营养级为(3.62±0.21),其δ¹⁵N值和营养级与体长呈显著负相关,δ¹³C值与体长无显著相关性.普氏栉虾虎鱼摄食的主要饵料生物类群为多毛类、虾类和软体动物,浮游动物和颗粒有机物(POM)的饵料贡献率较小.聚类分析结果表明,普氏栉虾虎鱼各体长组食物组成的相似性均在92%以上,相似性较高,说明其摄食习性随体长变化无明显差异.普氏栉虾虎鱼在胶州湾生态系统中属于中级消费者,其摄食各饵料生物类群比例的变化可能是其营养级与体长呈负相关关系的主要原因.     

Reconstructing the diets of Greek Byzantine populations (6th-15th centuries AD) using carbon and nitrogen stable isotope ratios

Documentary evidence and artistic representations have traditionally served as the primary sources of information about Byzantine diet. According to these sources, Byzantine diet was based on grain (primarily wheat and barley), oil, and wine, supplemented with legumes, dairy products, meat, and marine resources. Here, we synthesize and compare the results of stable isotope ratio analyses of eight Greek Byzantine populations (6th-15th centuries AD) from throughout Greece. The δ(13) C and δ(15) N values are tightly clustered, suggesting that all of these populations likely consumed a broadly similar diet. Both inland and coastal Byzantine populations consumed an essentially land-based C(3) diet, significant amounts of animal protein, and possibly some C(4) plants, while no evidence of a general dependence on low-δ(15) N legumes was observed. One interesting result observed in the isotopic data is the evidence for the consumption of marine protein at both coastal sites (a reasonable expectation given their location) and for some individuals from inland sites. This pattern contrasts with previous isotopic studies mainly on prehistoric Greek populations, which have suggested that marine species contributed little, or not at all, to the diet. The possibility that fasting practices contributed to marine protein consumption in the period is discussed, as are possible parallels with published isotope data from western European medieval sites.     

水生动物碳氮稳定同位素富集系数的整合分析

同位素富集系数即动物组织与其食物之间同位素丰度（δ）的差异值(Δ),是稳定性同位素技术应用于生态系统营养关系、食性和食物网研究的重要参数.不同生境条件下和不同物种之间的富集系数通常被认为是相对稳定的,但越来越多的研究发现,富集系数在不同类型动物之间存在明显差异而不是一个恒定值,尽管这一差异范围仍不清楚.本文进行了3种不同权重设置方式的整合分析,综述并比较了4类水生动物(硬骨鱼类、甲壳类、爬行类、软体动物)的碳氮稳定同位素富集系数.在Web of Science和CNKI数据库上搜索2014年底之前发表的论文,获得了42篇包含140个Δ¹³C的研究结果和159个Δ¹⁵N的研究结果.使用3种不同的加权方式进行3次独立整合分析,3种加权方式分别是以方差倒数作为权重、以样本量作为权重和相等权重.结果表明,整合分析统计结果十分稳健,不同权重设置的分析结果差异很小.水生动物碳稳定同位素富集系数(Δ^13C)总体平均值为1.0‰,其中,硬骨鱼类1.0‰,甲壳类1.3‰,爬行类0.5‰,软体动物1.5‰;氮稳定同位素富集系数(Δ¹⁵N)总体平均值为2.6‰,其中,硬骨鱼类2.4‰,甲壳类3.6‰,爬行类1.0‰,软体动物2.5‰.统计分析表明,硬骨鱼类、甲壳类、爬行类、软体动物之间的Δ¹³C没有显著差异,而Δ¹⁵N存在显著差异.因此,应用稳定性同位素技术研究水生动物营养关系、食性和食物网中碳富集系数可以选择总体平均值,而氮富集系数则应根据不同水生动物类型选取相应的系数值.     

基于稳定同位素的SPAC水碳拆分及耦合研究进展

土壤-植被-大气连续体(SPAC)是陆地水文学、生态学和全球变化领域的重要研究对象,其水碳循环过程及耦合机制是前沿性问题.稳定同位素技术示踪、整合和指示的特征有助于评估分析生态系统固碳和耗水情况.本文在简述稳定同位素应用原理和技术的基础上,重点阐释了基于稳定同位素光学技术的SPAC系统水碳交换研究进展,包括:在净碳通量中拆分光合与呼吸量,在蒸散通量中拆分蒸腾与蒸发量,以及在系统尺度上的水碳耦合研究.新兴的技术和方法实现了生态系统尺度上长期高频的同位素观测,但在测量精准度、生态系统呼吸拆分、非稳态模型适应性、尺度转换和水碳耦合机制等方面存在挑战.本文探讨了现有主要研究成果、局限性以及未来研究展望,以期对稳定同位素生态学领域的新研究和技术发展有所帮助.     

Variation in trophic shift for stable isotope ratios of carbon, nitrogen, and sulfur

Use of stable isotope ratios to trace pathways of organic matter among consumers requires knowledge of the isotopic shift between diet and consumer. Variation in trophic shift among consumers can be substantial. For data from the published literature and supplementary original data (excluding fluid-feeding consumers), the mean isotopic shift for C was +0.5±0.13‰ rather than 0.0‰, as commonly assumed. The shift for C was higher for consumers analyzed as muscle (+1.3±0.30‰) than for consumers analyzed whole (+0.3±0.14‰). Among consumers analyzed whole, the trophic shift for C was lower for consumers acidified prior to analysis (−0.2±0.21‰) than for unacidified samples (+0.5±0.17‰). For N, trophic shift was lower for consumers raised on invertebrate diets (+1.4±0.21‰) than for consumers raised on other high-protein diets (+3.3±0.26‰) and was intermediate for consumers raised on plant and algal diets (+2.2±0.30‰). The trophic shift for S differed between high-protein (+2.0±0.65‰) and low-protein diets (-0.5±0.56‰). Thus, methods of analysis and dietary differences can affect trophic shift for consumers; the utility of stable isotope methods can be improved if this information is incorporated into studies of trophic relationships. Although few studies of stable isotope ratios have considered variation in the trophic shift, such variation is important because small errors in estimates of trophic shift can result in large errors in estimates of the contribution of sources to consumers or in estimates of trophic position.     

基于碳、氮稳定同位素的厦门筼筜湖两种优势端足类食性分析

测定了厦门市筼筜湖(内、外湖)大型海藻群落两种优势端足类(强壮藻钩虾Ampitheoe valida和上野蜾蠃蜚Corophium uenoi)及其潜在食源的碳、氮稳定同位素比值(δ~(13)C和δ~(15)N),分析研究了这两种端足类摄食习性的空间变动特征。研究发现,端足类的潜在食源包括悬浮颗粒有机物(Particulate organic matter:POM),沉积有机物(Sedimentary organic matter:SOM),石莼(Ulva lactuca:Ulva)及其表面的附生生物(Epiphytes:Epi),它们的δ~(13)C和δ~(15)N值分别介于-24.0‰(POM)—-11.8‰(Ulva)和-1.7‰(POM)—4.7‰(Ulva)之间。其中,Ulva和POM的δ~(13)C值的内、外湖差异不显著;而外湖SOM和Epi的δ~(13)C值则明显高于内湖。采样区SOM有机质来源的空间差异是其δ~(13)C内、外湖差异的主要原因。除POM外,外湖有机碳源的δ~(15)N明显高于内湖,这与它们利用氮源的δ~(15)N的差异有关。潜在食源稳定同位素组成的空间差异,使得筼筜湖端足类的稳定同位素组成,尤其是δ~(15)N值表现出显著的空间变动特征(强壮藻钩虾和上野蜾蠃蜚δ~(15)N的内、外湖差异高达1.6‰和4.2‰,变幅约1个营养级),但2种端足类食性的空间差异却不尽相同:强壮藻钩虾的食性相对稳定,其δ~(13)C值介于Ulva和Epi之间,表明它主要从Ulva及其表面的Epi获取碳源;而上野蜾蠃蜚的食性内、外湖差异较大:内湖从石莼表面的Epi获取碳源,约20%是来自POM的贡献,而外湖则主要以Ulva及其表面的Epi为食。分析显示,筼筜湖内、外湖端足类δ~(15)N的空间差异并不是端足类的营养级发生了变化,而是由于端足类食源δ~(15)N的空间差异引起的,而不同端足类食性的内、外湖差异则可能与环境中饵料的丰度和生物量密切相关。     

Carbon and nitrogen stable isotope ratios of deposit-feeding polychaetes in the Nanakita River Estuary, Japan

Two types of deposit-feeding polychaetes, Neanthes japonica and Notomastus sp., and their surrounding sediments were collected from the Nanakita River Estuary and a small brackish lagoon (Gamõ Lagoon) in northeastern Japan. The samples were examined using stable isotope analysis to assess the site specific feeding mode of the animals and their trophic status. N. japonica is a surface deposit-feeder and Notomastus sp. is a subsurface deposit-feeder. In the estuary, the sedimentary ⁵N tended to become isotopically heavier from the upper estuary (2.0 3.9) to the river mouth (4.3 6.2), while sedimentary organic ¹³C constant value (–26.8 –24.4, average –25.6) throughout the river estuary. The ¹³C values of N. japonica were similar to those of the surrounding sediment in the upper estuary, whereas in the lower estuary, N. japonica had a heavier ¹³C value than the surrounding sediment. The ¹³C and dg ¹⁵N values indicated that the carbon, but not the nitrogen, of N. japonica was derived from upland plants in the upper estuary. In the lower estuary, a significant fraction of carbon of N. japonica was derived from phytoplankton. Notomastus sp. exhibited heavier ¹³C values than the surrounding surface sediment throughout the estuary and had heavier ¹³C values than N. japonica in the same location. These results suggest selective utilization of sedimentary carbon by those animals following bacterial processing and subsequent fractionation. The difference in ¹⁵N between sedimentary organics and corresponding polychaetes was 5 ± 1 and rather higher than 3.4 ± 1.1 expected for normal trophic effects in other animals.     

典型海湾与海岛近海脉红螺碳、氮稳定同位素特征差异

为深入了解不同大小脉红螺(Rapana venosa)的碳、氮稳定同位素特征,探究其在典型海湾和海岛水域生态系统所处营养位置,于2022年春季和夏季在胶州湾和长岛近海通过拖网和潜水采集160个脉红螺样本,详细分析了不同体长、体重脉红螺的δ¹³C和δ¹⁵N变化,并计算各研究区域的脉红螺核心生态位宽度及相关参数。结果显示,脉红螺δ¹³C值范围在-22.12‰--16.63‰,四组数据均值为-19.74‰--17.42‰,δ¹⁵N值范围在8.77‰-13.48‰,均值为9.64‰-12.81‰,各组数据营养级均值在2.63-3.57;胶州湾春季脉红螺δ¹³C值与体长、体重呈显著负相关,夏季呈显著正相关,长岛近海区域无明显变化,表明不同季节和不同区域的食物多样性水平存在差异, 胶州湾脉红螺δ¹³C、δ¹⁵N的变化更为突出;两个研究区域δ¹⁵N值和营养级与体长、体重呈显著正相关,主要由于脉红螺摄食偏好性差异,较大的脉红螺倾向于摄食高营养级生物,造成营养级较高。此外,胶州湾脉红螺营养级高于长岛近海,表明其¹⁵N来源更为广泛。营养生态位总面积、δ¹⁵N差值、δ¹³C差值、校正后标准椭圆面积等评价指标,揭示了不同区域、不同季节的脉红螺稳定同位素营养生态位的显著差异,反映了区域地理位置与食物来源对脉红螺δ¹³C和δ¹⁵N的影响。上述研究结果为近海生态系统食物网的构建提供了重要数据,并为区域生物资源的管理和生态系统修复工作提供了科学支撑。     

人为营养物质输入对汉丰湖不同营养级生物的影响--稳定C、N同位素分析

以长江一级支流小江上游的汉丰湖为研究对象,设置了4个采样点(影响组:A, B;对照组:C, D),应用碳、氮稳定性同位素探讨人类生活污水和农业面源污染对汉丰湖水生生态系统中不同营养级水平生物类群的影响。结果表明:影响组POM(颗粒有机物)和螺类碳、氮稳定性同位素比值范围分别为-25.93‰--24.63‰、4.12‰-9.86‰,-14.28‰--21.60‰、7.97‰-19.99‰;对照组POM(颗粒有机物)和螺类碳、氮稳定性同位素比值范围分别为-25.62‰--22.51‰、0.01‰-6.56‰,-22.96‰--19.21‰、6.75‰-8.89‰;不同组间POM和初级消费者螺类碳同位素比值无明显空间变化(P>0.05), 而氮稳定性同位素比值空间变化显著(P<0.05)。因此,在汉丰湖食物网中,氮稳定性同位素特征更好地反应了营养物质(人为输入)吸收和富集的信息。与固着藻类、鱼类等相比,POM和软体动物螺类更适合作为环境评价的指示物。影响组A、B样点的部分生物类群已经受到了人为营养物质输入的影响,影响强度B样点区域>A样点区域。结果建议加强汉丰湖水环境保护,控制污水排放量及提高污水处理水平,对于保护小江和三峡库区水质具有十分重要的意义。     

Toward using <Emphasis Type="Italic">Margaritifera falcata</Emphasis> as an indicator of base level nitrogen and carbon isotope ratios: insights from two California Coast Range rivers

Measurements of freshwater mussel tissue are potentially very useful for determining base-level isotopic values for food web studies in aquatic environments. As long-lived, filter-feeding organisms, mussels have the potential to spatially and temporally average the isotopic baseline signal. Following from earlier studies that focused on lake environments, this study investigates the stable carbon and nitrogen isotope ratios in tissue of the river dwelling freshwater mussel, Margaritifera falcata, in two extensively studied northern California coast range rivers, the South Fork Eel and Navarro. We highlight advantages and challenges for using riverine mussel isotopes as indicators of baselines. ¹³C of primary producers is known to vary with habitat along the South Fork Eel channel, but our measurements show no such variations, demonstrating that riverine mussels do preserve a spatially averaged measure of instream derived food sources. Mean ¹³C and ¹⁵N are shown to be markedly different in the two rivers, reflecting differences in food sources and possibly watershed land use. We also found that ¹⁵N of mussel tissue increased by approximately 2 with mussel age in both rivers. This suggests it is important to consider age and size effects when estimating baseline values from mussel tissues.