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Spatial and meteorological controls of stable water isotope dynamics of precipitation in Kashmir Valley, Western Himalaya, India. 印度喜马拉雅山脉西部克什米尔山谷降水稳定水同位素动力学的空间和气象控制。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-09-26 DOI: 10.1080/10256016.2023.2256454
Altaf Lone, Ghulam Jeelani, Suhail A Lone, Virendra Padhya, Rajendrakumar D Deshpande, A P Dimri

In the Himalayas, the lives and livelihoods of millions of people are sustained by water resources primarily depending on the moisture brought by Western Disturbances and Indian Summer Monsoon. In the present study, a network of 12 precipitation stations was established across the Kashmir Valley to understand the spatial and meteorological factors controlling precipitation isotopes. Temperature and relative humidity are dominant meteorological factors, whereas altitude, proximity to forest canopy, land use/land cover, windward and leeward sides of the mountains are the main physical factors influencing precipitation isotopes. The study suggests that the Mediterranean Sea and nearby water bodies along with continental recycling are the dominant sources of moisture from October to May, while the Arabian Sea, Bay of Bengal and continental recycling are the main sources of moisture from June to September. However, some precipitation events from October to May collect moisture from the Arabian Sea and some precipitation events from June to September collect moisture from the Mediterranean Sea. The occasional passage of Western Disturbances in summer merging with the Indian Summer Monsoon yields heavy to very heavy precipitation. The study provides a better understanding of complex spatial and meteorological phenomena controlling precipitation isotopes across the Western Himalayas.

在喜马拉雅山,数百万人的生活和生计靠水资源维持,主要依靠西方扰动和印度夏季风带来的湿气。在本研究中,在克什米尔山谷建立了一个由12个降水站组成的网络,以了解控制降水同位素的空间和气象因素。温度和相对湿度是主要的气象因素,而海拔、接近林冠、土地利用/土地覆盖、山脉的向风和背风侧是影响降水同位素的主要物理因素。研究表明,地中海和附近水体以及大陆再循环是10月至5月的主要水分来源,而阿拉伯海、孟加拉湾和大陆再循环是6月至9月的主要湿气来源。然而,10月至5月的一些降水事件从阿拉伯海收集水分,6月至9月的一些降雨事件从地中海收集水分。夏季西部扰动偶尔会与印度夏季风合并,产生大到特大降水。这项研究更好地了解了控制喜马拉雅山脉西部降水同位素的复杂空间和气象现象。
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引用次数: 0
Characterizing wine terroir using strontium isotope ratios: a review. 用锶同位素比值表征葡萄酒风土:综述。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-18 DOI: 10.1080/10256016.2023.2245122
Bruna Saar de Almeida, Lorenzo Fedele, Massimo D'Antonio, Vincenzo Morra, Mariano Mercurio, Ross Stevenson, David Widory

This paper presents a detailed review of the use of 87Sr/86Sr isotope systematics for wine provenance studies. The method is based on the principle that the Sr isotope ratio in wine reflects that of the labile fraction of the vineyard soil from which the wine is produced. The review encompasses 87Sr/86Sr data from wine samples published between 1993 and 2021 from terroirs in 22 different countries. The analytical procedures and techniques adopted by the different authors and the range of isotope ratios obtained in the different studies are discussed and evaluated. This study provides a bibliometric analysis of the 87Sr/86Sr isotope approach for wine authentication at different scales. Although limitations are evident when implemented at large (global) scales, we demonstrate that the 87Sr/86Sr isotope tracing technique remains a powerful and reliable tool for determining the geographical origin of wine when combined with detailed knowledge of the geological and soil characteristics of the substrata. For example, this combination of data allows the wines grown in the volcanic soils of Central and Southern Italy to be unambiguously fingerprinted. We present a detailed protocol for the application of the Sr isotope technique to wine authentication.

本文详细介绍了87Sr/86Sr同位素系统在葡萄酒种源研究中的应用。该方法的原理是,葡萄酒中的Sr同位素比值反映了生产葡萄酒的葡萄园土壤中不稳定部分的同位素比值。该研究涵盖了1993年至2021年间来自22个不同国家风土的葡萄酒样品的87Sr/86Sr数据。讨论和评价了不同作者采用的分析方法和技术以及在不同研究中获得的同位素比值范围。本文对87Sr/86Sr同位素方法在不同尺度下的葡萄酒鉴定进行了文献计量学分析。尽管在大(全球)尺度上实施的局限性很明显,但我们证明,87Sr/86Sr同位素示踪技术仍然是确定葡萄酒地理起源的强大而可靠的工具,当结合对地层地质和土壤特征的详细了解时。例如,这种数据组合可以让在意大利中部和南部火山土壤中生长的葡萄酒得到明确的指纹。我们提出了Sr同位素技术在葡萄酒鉴定中的应用的详细方案。
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引用次数: 0
Measurements of natural radionuclide levels and hazards in the Lega Dembi gold mine, Oromia, Ethiopia. 埃塞俄比亚奥罗米亚Lega Dembi金矿天然放射性核素水平和危害的测量。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2273287
Gebi Tuku Yachiso, Ashok K Chaubey, Birhanu Turi

This study aimed to evaluate natural radioactivity levels and hazards of radionuclides 232Th, 226Ra and 40K in soil samples taken from 15 locations in the Lega Dembi gold mining, Oromia, Ethiopia, using gamma-ray spectroscopy coupled with an HPGe detector. It was observed that the respective mean specific activities for 226Ra, 232Th and 40K determined in the mining site were 23.87 ± 0.7, 52.5 ± 1.8 and 391.62 ± 11.35 Bq/kg, and 8.89 ± 0.4, 13.83 ± 0.6 and 423.68 ± 9.5 Bq/kg in the living areas. The specific activity of 232Th was above the permissive limit in the mining site, while for 226Ra and 40K were within the limit. The specific activity of 40K in the living area was observed to be above the permissive limit. The calculated value of radiation hazards parameters; radium equivalent activity (Raeq), internal and external hazards indices (Hin) and (Hex), the mean annual effective dose (AED), and gamma representative indices (Iγ) were within permissively limit. The mean absorbed dose rate in the mining site was above the recommended safety limit. The total annual gonadal dose equivalent value was found to be 494.8 ± 8.7 µSv/a in the mining site. This value was also above the permissively.

本研究旨在利用伽玛射线能谱联用HPGe探测器,评估从埃塞俄比亚奥罗米亚Lega Dembi金矿15个地点采集的土壤样品中放射性核素232Th、226Ra和40K的天然放射性水平和危害。结果表明,矿区226Ra、232Th和40K的平均比活度分别为23.87±0.7、52.5±1.8和391.62±11.35 Bq/kg,生活区226Ra、232Th和40K的平均比活度分别为8.89±0.4、13.83±0.6和423.68±9.5 Bq/kg。232Th在矿区的比活度在允许范围以上,而226Ra和40K在允许范围内。在生活区观察到40K的比活性高于允许限制。辐射危害参数计算值;镭当量活度(Raeq)、内外危害指数(Hin)和(Hex)、年平均有效剂量(AED)和γ代表性指数(Iγ)均在允许范围内。矿区的平均吸收剂量率高于建议的安全限度。矿区年性腺总剂量当量为494.8±8.7µSv/a。该值也高于允许值。
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引用次数: 0
Application of multiple stable isotopes to aid identification of the origin of regional and organic animal products in Hesse, Germany. 多种稳定同位素的应用,以帮助识别原产地的区域和有机动物产品在黑森州,德国。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2273941
Xenia Gatzert, Kwok P Chun, Robert Hermanowski, Rolf Mäder, Lutz Breuer, Andreas Gattinger, Natalie Orlowski

There is an increasing global demand for regional and organic produce. However, the growth of these markets depends on consumers' trust. Thus, novel methods must be developed to aid the verification of the origin of produce. We built on our previous study to identify the geographical origin and production method of animal-derived food products. Thirty-samples of eggs, 99 of milk, 34 of beef, and 62 of pork were collected from different regions in central Germany and analysed for their stable isotopic composition. The analysis followed a single-variate authentification approach using five isotope signatures, δ18O, δ2H, δ13C, δ15N, and δ34S. The best-performing indicators for verification of the geographical origin were δ15N and δ34S for beef; δ18O, δ2H, and δ13C for milk, and δ2H and δ13C for pork. These tracers indicated statistically significant differences among regions with the exception of pork; the results recorded for eggs were inconclusive. It was possible to distinguish between production methods by means of δ15N and δ34S (beef); all five tracers (eggs), and δ13C, δ15N, and δ34S (milk). This study demonstrated how the analysis of stable isotopes can be employed to determine the geographic region of origin and production method of animal-derived products in Germany.

全球对区域和有机农产品的需求不断增加。然而,这些市场的增长依赖于消费者的信任。因此,必须开发新的方法来帮助验证农产品的原产地。我们在之前的研究基础上确定了动物源性食品的地理来源和生产方法。研究人员从德国中部的不同地区收集了30份鸡蛋、99份牛奶、34份牛肉和62份猪肉样本,并对它们的稳定同位素组成进行了分析。采用δ18O、δ2H、δ13C、δ15N和δ34S五种同位素特征进行单变量鉴定。牛肉的δ15N和δ34S是验证地理来源的最佳指标;牛奶的δ18O, δ2H和δ13C,猪肉的δ2H和δ13C。这些示踪剂表明,除猪肉外,各地区之间的差异具有统计学意义;记录的卵子检测结果尚无定论。通过δ15N和δ34S(牛肉)可以区分不同的生产方法;5种示踪剂(鸡蛋)和δ13C、δ15N和δ34S(牛奶)。本研究展示了如何利用稳定同位素分析来确定德国动物源性产品的原产地地理区域和生产方法。
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引用次数: 0
Isotopic history of seawater: the stable isotope character of the global ocean at present and in the geological past. 海水的同位素历史:全球海洋在现在和地质过去的稳定同位素特征。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2271127
Jochen Hoefs, Russell S Harmon

After the atmosphere, the ocean is the most well-mixed and homogeneous global geochemical reservoir. Both physical and biological processes generate elemental and isotope variations in seawater. Contrasting geochemical behaviors cause elements to be susceptible to different fractionation mechanisms, with their isotopes providing unique insights into the composition and evolution of the ocean over the course of geological history. Supplementing the traditional stable isotopes (H, C, O, N, S) that provide information about ocean processes and past environmental conditions, radiogenic isotope (Sr, Nd, Os, Pb, U) systems can be used as time markers, indicators of terrestrial weathering, and ocean water mass mixing. Recent instrumentation advances have made possible the measurement of natural stable isotope variations produced by both mass-dependent and mass-independent fractionation for an ever-increasing number of metal elements (e.g. Li, B, Mg, Si, Ca, V, Cr, Fe, Ni, Cu, Zn, Se, Mo, Cd, Tl, U). The major emphasis in this review is on the isotopic composition of the light elements based on a comparatively large literature. Unlike O, H and S, the stable isotopes of C, N and Si do not have a constant isotopic composition in the modern ocean. The major cations Ca, Mg, and Sr fixed in carbonate shells provide the best proxies for reconstruction of the composition of the ocean in the past. Exhibiting large isotope enrichments in ocean water, B and Li are suitable for the investigation of water/rock interactions and can act as monitors of former oceanic pH. The bioessential elements Zn, Cd, and Ni are indicators of paleoproductivity in the ocean. Characteristic isotope enrichments or depletions of the multivalent elements V, Cr, Fe, Se, Mo, and U record the past redox state of the ocean/atmosphere system. Case studies describe how isotopes have been used to define the seawater composition in the geological past.

海洋是继大气之后混合最均匀的全球地球化学储层。物理和生物过程都会在海水中产生元素和同位素的变化。对比的地球化学行为使元素容易受到不同的分馏机制的影响,它们的同位素为地质历史过程中海洋的组成和演化提供了独特的见解。作为提供海洋过程和过去环境条件信息的传统稳定同位素(H、C、O、N、S)的补充,放射成因同位素(Sr、Nd、Os、Pb、U)系统可以用作时间标记、陆地风化和海洋水团混合的指标。最近仪器的进步使得测量由不断增加的金属元素(例如,Li、B、Mg、Si、Ca、V、Cr、Fe、Ni、Cu、Zn、Se、Mo、Cd、Tl、U)的质量依赖性和质量无关性分馏产生的天然稳定同位素变化成为可能。这篇综述的主要重点是基于大量文献的轻元素同位素组成。与O、H和S不同,C、N和Si的稳定同位素在现代海洋中没有恒定的同位素组成。碳酸盐壳中固定的主要阳离子Ca、Mg和Sr为重建过去的海洋成分提供了最佳的替代品。B和Li在海水中表现出大量同位素富集,适合于水/岩石相互作用的研究,并可作为前海洋pH值的监测器。生物元素Zn、Cd和Ni是海洋古生产力的指标。多价元素V、Cr、Fe、Se、Mo和U的特征同位素富集或贫化记录了海洋/大气系统过去的氧化还原状态。案例研究描述了同位素在过去的地质中是如何被用来定义海水成分的。
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引用次数: 0
226Ra measurement via gamma-ray spectrometry of 222Rn progeny - quantification of radon losses from sample capsules. 通过 222Rn 后代的伽马射线光谱法测量 226Ra - 量化样品胶囊中的氡损失。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-08-11 DOI: 10.1080/10256016.2023.2244651
Michael Schubert, Albrecht Paschke, Wolfram Westmeier

Radium-226 detection in sediment samples is generally executed by means of gamma-ray spectrometry. Data evaluation relies (besides the 186.2 keV 226Ra gamma peak) on the combined analysis of major gamma peaks that are produced by the short-lived radon (222Rn) daughters 214Pb and 214Bi. Precondition for this detection approach is equilibrium decay of all members of the decay chain between 226Ra and 214Bi. In closed systems, this equilibrium is reached after about five half-lives of 222Rn (19 days). However, a closed system can only be guaranteed if the capsule which contains the sample prevents diffusive escape of radon. Such radon-tightness cannot be guaranteed for a wide range of plastic materials. Due to its polymer structure, plastic material generally tends to allow radon diffusion and hence radon loss from the sample resulting in a disturbance of the required decay equilibrium. The paper introduces an approach that allows quantifying radon loss from sample capsules by direct radon measurements using mobile radon detection equipment. The experimental findings are supported by theoretical considerations. An examined alternative approach based on the offset of the 186.2 keV data point from an efficiency function that is calculated exclusively from short-lived radon progeny peaks in the gamma-ray spectrum did not prove to be applicable due to a lack of supporting peaks in the low-energy section of the spectrum.

沉积物样本中镭-226 的检测一般采用伽马射线光谱法。除了 186.2 千电子伏的 226Ra 伽马峰外,数据评估还依赖于对短 寿命氡(222Rn)女儿 214Pb 和 214Bi 产生的主要伽马峰的综合分析。这种探测方法的先决条件是 226Ra 和 214Bi 之间衰变链的所有成员都达到平衡衰变。在封闭系统中,大约经过 222Rn 的五个半衰期(19 天)就会达到这种平衡。然而,只有在装有样品的胶囊能防止氡扩散逃逸的情况下,才能保证系统是封闭的。对于各种塑料材料来说,这种氡密闭性是无法保证的。由于其聚合物结构,塑料材料通常会允许氡扩散,从而导致氡从样品中流失,破坏所需的衰变平衡。本文介绍了一种方法,通过使用移动式氡检测设备直接进行氡测量,可以量化样品胶囊中的氡损失。实验结果有理论依据。由于伽马射线频谱的低能段缺乏支持峰值,已研究的基于 186.2 千伏数据点与效率函数偏移的替代方法被证明并不适用,而效率函数完全是根据伽马射线频谱中的短寿命氡后代峰计算得出的。
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引用次数: 0
Measurement of plasma protein and whole body protein metabolism using [15N]glycine in a young adult man - a pilot study. 使用[15N]甘氨酸测量一名年轻成年男子的血浆蛋白质和全身蛋白质代谢--一项试验研究。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2252572
Peter Junghans, Gerhard Zuz, Hans Faust

A novel simplified method is presented for the estimation of the metabolism of plasma proteins (albumin, fibrinogen, α, β and γ-globulin, glycoprotein) with regard to the whole body protein metabolism in a young male volunteer (22 years, 81 kg body mass). This method is based on multiple oral administration of [15N]glycine followed by measurement of 15N in plasma proteins, total free amino acids, urea and excreted urinary N. The fractional synthesis rate of albumin was estimated to 6.8 % d-1 based on amino acids and 3.3 % d-1 based on urea, respectively. The fractional synthesis rate of the other plasma proteins ranged from 4.3 % d-1 (γ-globulin) to 26.4 % d-1 (α-globulin, fibrinogen). We conclude that the simplified approach using [15N]glycine provides results which are similar to results based on the simultaneously applied 131I-human serum albumin technique as 'gold standard' and to those reported in literature. The compartmental analysis considering comprehensive tracer kinetic data ensures reliable data treatment and enables statistical evaluation. The analytical effort is minimal because the 15N enrichment of plasma protein after chemical digestion may be directly used. Therefore, the novel stable isotope 15N method is suitable for studies in clinical and nutritional research and practice.

本文介绍了一种新颖的简化方法,用于估算年轻男性志愿者(22 岁,体重 81 千克)血浆蛋白质(白蛋白、纤维蛋白原、α、β 和 γ 球蛋白、糖蛋白)的代谢情况以及全身蛋白质代谢情况。该方法基于多次口服[15N]甘氨酸,然后测量血浆蛋白质、总游离氨基酸、尿素和排泄尿N中的15N。其他血浆蛋白的部分合成率从 4.3 % d-1(γ-球蛋白)到 26.4 % d-1(α-球蛋白、纤维蛋白原)不等。我们的结论是,使用[15N]甘氨酸的简化方法得出的结果与同时应用 131I 人血清白蛋白技术作为 "黄金标准 "得出的结果以及文献报道的结果相似。考虑到综合示踪剂动力学数据的分区分析确保了可靠的数据处理并实现了统计评估。由于可以直接使用化学消化后的血浆蛋白 15N 富集,因此分析工作量极小。因此,新型稳定同位素 15N 方法适用于临床和营养研究与实践。
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引用次数: 0
Annual effective dose estimation of radon in drinking water sources of Nizampur basin, North Western Pakistan. 巴基斯坦西北部尼扎姆布尔盆地饮用水源氡年有效剂量估算。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2276218
Jehangir Ijaz, Wajid Ali, Said Muhammad, Hayat Ullah, Danish Ather, Imran Ud Din

This study assessed radon (222Rn) levels in drinking water sources in the Nizampur basin and their potential health risks for the local community. We analyzed 48 water samples on-site using RAD7. Additionally, we measured pH, temperature (T), total dissolved solids (TDS), redox potential (ORP), and electrical conductivity (EC) with a multiparameter analyzer. Results showed pH, T, TDS, ORP, and EC ranging from 7.2 to 8, 17 to 26 °C, 333 to 1130 mg/l, -56 to 284 mV, and 469 to 2370 µS/cm. 222Rn levels varied significantly (0.7-107 Bq/l, mean 23 ± 21, median = 17 Bq/l), with about 65 % exceeding the EPA's limit of 11.1 Bq/l, indicating health risks likely due to local geological conditions. The annual effective doses for ingestion (EwIng) were 0.87 ± 0.01, 0.35 ± 0.006, and 0.13 ± 0.002 µSv/a for adults, infants, and children, respectively. Exposure risk via the inhalation (EwInh) route ranged from 1.75 to 270 µSv/a, with the highest risk in infants, followed by children and adults. Inhalation was the primary exposure route for all age groups. Further, spatial distribution maps and hotspot analysis suggested that the central region characterized by high structural deformation and favorable geology for radon emanation was the area of concern in terms of health risks.

这项研究评估了尼扎姆布尔盆地饮用水源中的氡(222Rn)水平及其对当地社区的潜在健康风险。我们使用RAD7在现场分析了48个水样。此外,我们用多参数分析仪测量了pH、温度(T)、总溶解固体(TDS)、氧化还原电位(ORP)和电导率(EC)。结果显示pH、T、TDS、ORP和EC的范围为7.2至8、17至26 °C,333至1130 mg/l、-56至284 mV和469至2370µS/cm。222Rn水平变化显著(0.7-107 Bq/l,平均23 ± 21,中位数 = 17 Bq/l),其中约65%超过了美国环保局11.1 Bq/l的限制,表明当地地质条件可能导致健康风险。年有效摄取剂量(EwIng)为0.87 ± 0.010.35 ± 0.006和0.13 ± 成人、婴儿和儿童分别为0.002µSv/a。通过吸入(EwInh)途径暴露的风险在1.75至270µSv/a之间,婴儿的风险最高,其次是儿童和成人。吸入是所有年龄组的主要接触途径。此外,空间分布图和热点分析表明,以高结构变形和有利的氡散发地质为特征的中部地区是健康风险关注的地区。
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引用次数: 0
Differences in δ13C and δ15N values for monarch butterflies raised on milkweeds from within and outside of crop fields: implications for inferences about natal origins. 农作物田内和农作物田外以乳草饲养的帝王斑蝶的δ13C 和 δ15N值的差异:对推断产地的影响。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-08-01 Epub Date: 2023-12-12 DOI: 10.1080/10256016.2023.2257370
John M Pleasants

Stable isotope (δ2H, δ13C) measurements of wing tissue have been used to determine the natal geographic origin of migrant monarch butterflies that overwinter in Mexico. This study examines the possibility of using δ13C and δ15N to identify the milkweed habitat used by monarchs in their natal region. Milkweeds were common in corn and soybean fields before herbicide use led to their extirpation around 2006, and the loss of those milkweeds has been proposed as a reason for the monarch population decline. If crop-field monarchs can be identified, then historical samples of monarchs could be examined to test that hypothesis. The δ15N and δ13C values of leaves from milkweeds growing in corn fields, soybean fields and non-agricultural habitats were examined as well as monarchs that were raised on those leaves. There were no δ15N values for leaves or monarchs that were distinctive for crop fields. Milkweeds in corn fields, and monarchs that were raised on those milkweeds, were found to have δ13C values distinctly lower than those of other habitats and unlike those of locations within the summer breeding range. Thus, it should be possible to identify monarchs that came from cornfields in samples of overwintering monarchs made before ca. 2006.

对翅膀组织的稳定同位素(δ2H、δ13C)测量已被用于确定在墨西哥越冬的迁徙帝王斑蝶的原产地。本研究探讨了利用 δ13C 和 δ15N 来确定帝王斑蝶在原产地使用的乳草栖息地的可能性。在 2006 年左右使用除草剂导致奶草灭绝之前,奶草在玉米田和大豆田中很常见,这些奶草的消失被认为是帝王斑数量下降的原因之一。如果能识别出农作物田里的帝王斑,那么就可以对帝王斑的历史样本进行研究,以验证这一假设。我们研究了生长在玉米田、大豆田和非农业栖息地的奶浆草叶子的 δ15N 和 δ13C 值,以及在这些叶子上长大的帝王斑。作物田中的叶片或帝王果没有明显的 δ15N 值。研究发现,玉米田中的奶草以及在这些奶草上长大的帝王斑的 δ13C 值明显低于其他栖息地,也不同于夏季繁殖地。因此,在大约 2006 年之前采集的越冬帝王鱼样本中,应该可以识别出来自玉米田的帝王鱼。2006.
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Correction. 修正。
IF 1.3 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2023-06-28 DOI: 10.1080/10256016.2023.2224469
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Isotopes in Environmental and Health Studies
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