贵州山区3种木本植物无机碳利用特性的比较

以生长在喀斯特高原地区玉舍国家森林公园内的成熟银鹊树(Tapiscia sinensis)、白栎(Quercus fabri)和亮叶桦(Betula luminifera)为实验材料,通过对光合作用、叶绿素含量、叶绿素荧光参数、羧化效率(CE)、呼吸速率(Resp)、碳酸酐酶活性(WA)以及稳定碳同位素组成(δ13 C)等指标的测定,分析3种植物不同的无机碳利用特性,为该区生态环境修复选择合适的建群植物种提供依据。结果显示:(1)银鹊树、白栎和亮叶桦分布都较为广泛,银鹊树生长的最佳土壤pH是4.5~5.5,而白栎更倾向于中性到弱酸性土壤,肥沃的酸性土壤则更有益亮叶桦生长;白栎和亮叶桦都能忍受干旱和贫瘠,但是银鹊树不能忍受干旱和高温。(2)银鹊树叶片的Pn、Tr和Gs显著大于白栎和亮叶桦,亮叶桦和白栎的Pn、Tr和Gs分别是银鹊树的69.5%、48.2%、66.7%和28.6%、21.7%、22.2%;亮叶桦叶绿素含量均为银鹊树和白栎的2倍,但3种植物间的WUE则无显著差异。(3)3个树种叶片净光合速率均随着CO2浓度升高呈持续上升的趋势,但它们之间的CO2补偿点和饱和点明显不同。其中,银鹊树和亮叶桦的CO2补偿点均低于50μmol·mol-1,而白栎的则在250~300μmol·mol-1之间;银鹊树的CO2饱和点在1 200μmol·mol-1左右,亮叶桦则在2 300μmol·mol-1左右,而白栎的CO2饱和点明显高于2 300μmol·mol-1。(4)3个树种的CE、Resp和WA均为银鹊树>亮叶桦>白栎;而δ13 C值则以银鹊树最低,亮叶桦和白栎较高。其中,白栎和亮叶桦的CE、Resp、WA分别为银鹊树的5.1%、25.7%、4.0%和45.3%、54.6%、6.8%,且树种间差异显著;白栎和亮叶桦的δ13 C值显著高于银鹊树。研究表明,银鹊树能够吸收大气中的CO2或者在高活性碳酸酐酶作用下转化利用细胞内的HCO3-,它拥有较高的CO2利用能力及无机碳同化效率,因而能够拥有较高的产能;亮叶桦只能获取大气中的CO2作为无机碳源,但它对CO2的利用能力也较高,其产能仅次于银鹊树;白栎同样只能获取大气中的CO2作为无机碳源,同时它对大气中CO2的捕获、利用能力均低于银鹊树和亮叶桦,因而白栎生长非常缓慢,造成其本身对无机碳的需求也最低,所以其产能最低。     

壳聚糖对蝴蝶兰幼苗耐热性的诱导作用

为了评价壳聚糖对蝴蝶兰幼苗耐热性的诱导效应,分别采用0(以无壳聚糖为对照)、25、50、100、200和400 mg·L~(-1)壳聚糖溶液处理蝴蝶兰幼苗,并置于42℃下胁迫3 d,测定了蝴蝶兰幼苗的生理指标变化。结果表明:当壳聚糖浓度由25 mg·L~(-1)增大到100mg·L~(-1)时,蝴蝶兰幼苗叶片的SOD、POD、CAT活性、脯氨酸、可溶性糖、叶绿素和类胡萝卜素含量不断增加,而质膜透性和丙二醛含量不断下降,但可溶性蛋白含量没有显著变化;特别是在100 mg·L~(-1)时,SOD、POD和CAT活性、脯氨酸、可溶性糖、叶绿素和类胡萝卜素含量增加到最大值且极显著高于对照,而质膜透性和丙二醛含量下降至最小值且极显著低于对照,蝴蝶兰幼苗遭受了轻微的高温伤害;随着壳聚糖浓度由200 mg·L~(-1)增大至400mg·L~(-1),SOD、POD和CAT活性、脯氨酸、可溶性蛋白、可溶性糖、叶绿素和类胡萝卜素含量极显著下降,而质膜透性和丙二醛含量极显著上升,蝴蝶兰幼苗的受害趋于加重;由此可见,100 mg·L~(-1)壳聚糖处理能显著提高蝴蝶兰幼苗的耐热性。     

Investigating human responses to political and environmental change through paleodiet and paleomobility

Bioarchaeological approaches are well suited for examining past responses to political and environmental changes. In the Andes, we hypothesized that political and environmental changes around AD 1100 resulted in behavioral changes, visible as shifts in paleodiet and paleomobility, among individuals in the San Pedro de Atacama oases and Loa River Valley. To investigate this hypothesis, we generated carbon and oxygen isotope data from cemeteries dating to the early Middle Horizon (Larache, Quitor‐5, Solor‐3), late Middle Horizon (Casa Parroquial, Coyo Oriental, Coyo‐3, Solcor‐Plaza, Solcor‐3, Tchecar), and Late Intermediate Period (Caspana, Quitor‐6 Tardío, Toconce, Yaye‐1, Yaye‐2, Yaye‐3, Yaye‐4). Carbon isotope data demonstrate a greater range of carbon sources during the late Middle Horizon compared with the Late Intermediate Period; while most individuals consumed largely C₃ sources, some late Middle Horizon individuals consumed more C₄ sources. Oxygen isotope data demonstrate greater diversity in drinking water sources during the late Middle Horizon compared with the Late Intermediate Period. Water samples were analyzed to provide baseline data on oxygen isotope variability within the Atacama Desert, and demonstrated that oxygen isotope values are indistinguishable in the San Pedro and Loa Rivers. However, oxygen isotope values in water sources in the high‐altitude altiplano and coast are distinct from those in the San Pedro and Loa Rivers. In conclusion, instead of utilizing a wider variety of resources after environmental and political changes, individuals exhibited a wider range of paleodietary and paleomobility strategies during the Middle Horizon, a period of environmental and political stability. Am J Phys Anthropol 157:179–201, 2015. © 2015 Wiley Periodicals, Inc.     

The time scale of isotope signals in spiders: molting the remains of a previous diet

Stable isotope analysis (SIA) has emerged as an important tool for understanding consumer diets and diet shifts. However, although the general idea behind SIA is clear, the interpretation of data is often fraught with problems because tissue turnover and fractionations are not known. We investigated shifts in stable isotope composition of spiders following a diet shift, using mealworms fed either maize (C4) or wheat (C3) flour. Mealworms had different carbon isotope composition depending on their diet and this difference was reflected in spider body parts. In the experiment, we first fed the spiders on a diet of either maize‐fed or wheat‐fed mealworms and then switched diet at the time of the second molt. Spiders were then sampled repeatedly until the next molt. We sampled both legs and abdomens, as these are presumed to have different turnover of tissue, and also molt remains were sampled when this was relevant. The data indicated that the spider legs had a turnover of about 20 days, whereas the spider abdomens had a turnover of about 8 days. Molt remains had the slowest turnover and reflected the diet at the previous molt, when the exoskeleton was formed. Both these observations indicate that SIA may be successfully used for elucidating diet shifts. More problematic was the fact that fractionation of carbon isotope ratios varied with body parts and diets. When spiders were fed maize‐mealworms then the fractionation was larger for abdomens, but when the spiders were fed wheat‐mealworms then the fractionation was larger for legs. The mechanisms underlying this pattern are unclear and deserve further attention.     

Elemental formula annotation of polar and lipophilic metabolites using (13) C, (15) N and (34) S isotope labelling, in combination with high-resolution mass spectrometry

The unbiased and comprehensive analysis of metabolites in any organism presents a major challenge if proper peak annotation and unambiguous assignment of the biological origin of the peaks are required. Here we provide a comprehensive multi-isotope labelling-based strategy using fully labelled (13) C, (15) N and (34) S plant tissues, in combination with a fractionated metabolite extraction protocol. The extraction procedure allows for the simultaneous extraction of polar, semi-polar and hydrophobic metabolites, as well as for the extraction of proteins and starch. After labelling and extraction, the metabolites and lipids were analysed using a high-resolution mass spectrometer providing accurate MS and all-ion fragmentation data, providing an unambiguous readout for every detectable isotope-labelled peak. The isotope labelling assisted peak annotation process employed can be applied in either an automated database-dependent or a database-independent analysis of the plant polar metabolome and lipidome. As a proof of concept, the developed methods and technologies were applied and validated using Arabidopsis thaliana leaf and root extracts. Along with a large repository of assigned elemental compositions, which is provided, we show, using selected examples, the accuracy and reliability of the developed workflow.     

Synthesis of d-labeled and unlabeled benzoyloxysuccinimides and application to quantitative analysis of peptides and a protein by isotope differential mass spectrometry

Benzoyloxysuccinimide and its d₅-labeled version, which react with amino groups in the N-termini and lysine side chains in proteins, were synthesized and applied to quantitative analysis of peptides and a commercially available protein in combination with a MALDI mass spectrometer.     

Control of lysyl oxidase activity through site-specific deuteration of lysine

Lysyl oxidase (LOX) is implicated in several extracellular matrix related disorders, including fibrosis and cancer. Methods of inhibition of LOX in vivo include antibodies, copper sequestration and toxic small molecules such as β-aminopropionitrile. Here, we propose a novel approach to modulation of LOX activity based on the kinetic isotope effect (KIE). We show that 6,6-d₂-lysine is oxidised by LOX at substantially lower rate, with apparent deuterium effect on V_max/K_m as high as 4.35 ± 0.22. Lys is an essential nutrient, so dietary ingestion of D₂Lys and its incorporation via normal Lys turnover suggests new approaches to mitigating LOX-associated pathologies.     

Recent trends in the intrinsic water-use efficiency of ringless rainforest trees in Borneo

Stable carbon isotope (δ(13)C) series were developed from analysis of sequential radial wood increments from AD 1850 to AD 2009 for four mature primary rainforest trees from the Danum and Imbak areas of Sabah, Malaysia. The aseasonal equatorial climate meant that conventional dendrochronology was not possible as the tree species investigated do not exhibit clear annual rings or dateable growth bands. Chronology was established using radiocarbon dating to model age-growth relationships and date the carbon isotopic series from which the intrinsic water-use efficiency (IWUE) was calculated. The two Eusideroxylon zwageri trees from Imbak yielded ages of their pith/central wood (±1 sigma) of 670 ± 40 and 759 ± 40 years old; the less dense Shorea johorensis and Shorea superba trees at Danum yielded ages of 240 ± 40 and 330 ± 40 years, respectively. All trees studied exhibit an increase in the IWUE since AD 1960. This reflects, in part, a response of the forest to increasing atmospheric carbon dioxide concentration. Unlike studies of some northern European trees, no clear plateau in this response was observed. A change in the IWUE implies an associated modification of the local carbon and/or hydrological cycles. To resolve these uncertainties, a shift in emphasis away from high-resolution studies towards long, well-replicated time series is proposed to develop the environmental data essential for model evaluation. Identification of old (greater than 700 years) ringless trees demonstrates their potential in assessing the impacts of climatic and atmospheric change. It also shows the scientific and applied value of a conservation policy that ensures the survival of primary forest containing particularly old trees (as in Imbak Canyon and Danum).     

姜寨遗址先民食谱分析

尽管通过C、N稳定同位素分析已对陕西临潼姜寨遗址先民的食物结构和粟作农业进行了初步探索,但研究中的一些重要问题,如不同时期先民食物结构的演变,姜寨与半坡、史家先民食物结构间的差异等,依然未能深入讨论。为此,本文对姜寨遗址出土的不同时期(一期、二期)人骨进行了C、N稳定同位素分析,试图揭示先民食物结构的演变历程,探索姜寨与半坡、史家先民食物结构间的差异,并初步探讨产生这种差异的可能原因。人骨的δ13C平均值(-9.7±1.0‰)和δ15 N平均值(8.5±0.5‰),表明粟类食物(包括粟类作物以及依赖于粟类作物的动物等)在姜寨先民食谱中占据主要地位,且动物资源在食物中的比例相对较低。两期先民的δ13C和δ15N值,无显著性差异,表明先民一直从事粟作农业以及家畜的饲养活动。食谱分析并未发现第二期先民食用更多野生动物的证据,这可能与先民样品量相对偏少、二期先民食用的野生动物比例上升较小、动物类食物在先民食谱中所占比例较小等原因有关。对比地理位置毗邻、文化年代相近的姜寨、史家、半坡遗址先民δ13C值,姜寨(-9.7±1.0‰,N=19)与史家(-10.0±0.7‰,N=9)接近,而远高于半坡(-14.8±1.9‰,N=5),表明半坡遗址粟作农业的种植规模要逊于姜寨和史家遗址。我们认为,不同遗址间先民δ13C值的差异,可能受半坡样品量偏少、遗址间小生态环境不同等因素的影响。     

CO2浓度升高和施氮条件下小麦根际呼吸对土壤呼吸的贡献

依托FACE技术平台,采用稳定13C同位素技术,通过将小麦(C3作物)种植于长期单作玉米(C4作物)的土壤上,研究了大气CO2浓度升高和不同氮肥水平对土壤排放CO2的δ13C值及根际呼吸的影响.结果表明:种植小麦后土壤排放CO2的δ13C值随作物生长逐渐降低,CO2浓度升高200 μmol·mol-1显著降低了孕穗、抽穗期(施氮量为250 kg·hm-2,HN)与拔节、孕穗期(施氮量为150 kg·hm-2,LN)土壤排放CO2的δ13C值,显著提高了孕穗、抽穗期的根际呼吸比例.拔节至成熟期,根际呼吸占土壤呼吸的比例在高CO2浓度下为24％～48％ (HN)和21％ ～48％ (LN),在正常CO2浓度下为20％ ～36％ (HN)和19％～32％(LN).不同CO2浓度下土壤排放CO2的δ13C值和根际呼吸对氮肥增加的响应不同,CO2浓度与氮肥用量在拔节期对根际呼吸的交互效应显著.