高寒草甸植物群落功能多样性对不同生长期干旱的响应机制

植物对干旱胁迫的响应表现为各功能性状的差异化表达。全球气候变化下,青藏高原地区降水格局发生改变,高寒草甸群落功能性状及功能多样性在不同生长期干旱事件下的响应机制对加深高寒草甸适应气候变化认知具有重要意义。以藏北高寒草甸为研究对象,设置截雨棚模拟生长季前期（ED）、中期（MD）和非生长季时期（ND）干旱事件,通过观测群落物种功能性状,分析高寒草甸群落功能多样性对不同生长期干旱的响应机制。结果表明：（1）叶片功能性状对干旱存在差异响应,表现为叶片小而厚且寿命长,同化速率降低,并受氮元素限制加剧;（2）生长季前期干旱对高寒草甸群落功能性状的影响最强,生长季中期干旱次之,非生长季干旱的影响最弱;（3）生长季干旱处理显著改变了群落的功能多样性,ED处理下功能分散度指数（FDiv）和功能分异度指数（FDis）显著降低（P<0.05）,而Rao二次熵指数（RaoQ）显著升高（P<0.05）,MD处理下功能均匀度指数（FEve）显著降低（P<0.05）;（4）相关性分析得出,群落功能性状与功能多样性对干旱的响应之间存在着联系。本研究发现高寒草甸植物功能性状与群落功能多样性对生长季前期和中期干旱存在差异化响应,指示着高寒草甸植物群落在响应不同时期干旱时可能采取不同的生存策略,即对生长季前期干旱采用耐旱策略、对生长季中期干旱采用避旱策略。探讨了高寒草甸植物群落功能多样性对不同生长时期干旱胁迫的响应机制,为预测未来季节性干旱事件对青藏高原高寒草甸植物功能性状、群落特征和功能多样性的影响提供科学依据。     

增温对青藏高原高寒草甸呼吸作用的影响

生态系统呼吸(ER)和土壤呼吸(SR)是草地生态系统碳排放的关键环节,其对气候变化极为敏感。高寒草甸是青藏高原典型的草地生态系统,其呼吸作用对气候变化的响应对区域碳排放具有重要的影响。以高寒草甸生态系统为对象,于2012—2016年采用模拟增温的方法研究呼吸作用对增温的响应。结果表明:增温对高寒草甸ER的影响存在年际差异,2013年和2014年增温对ER无显著影响,其他年份显著增加ER(P0.05),综合5年结果,平均增幅达22.3%。增温显著促进了高寒草甸SR(P0.05),较对照处理5年平均增幅高达67.1%;增温总体上提高了SR在ER中的比例(P0.05),最高增幅达到59.9%。ER和SR与土壤温度有显著的正相关关系(P0.05),与土壤水分没有显著的相关关系(P0.05)。对照样地中,土壤温度分别能解释33.0%和18.5%的ER和SR变化。在增温条件下,土壤温度可以解释20.5%和13.0%的ER和SR变化。在增温条件下,SR的温度敏感性显著增加,而ER的温度敏感性变化较小,导致SR的比重进一步增加。因此,在未来气候变暖条件下,青藏高原高寒草甸生态系统碳排放,尤其是土壤碳排放有可能进一步增加,土壤碳流失风险增加。     

Polymorphisms of Genes in Neurotransmitter Systems Were Associated with Alcohol Use Disorders in a Tibetan Population

Studies of linkage and association in various ethnic populations have revealed many predisposing genes of multiple neurotransmitter systems for alcohol use disorders (AUD). However, evidence often is contradictory regarding the contribution of most candidate genes to the susceptibility of AUD. We, therefore, performed a case-control study to investigate the possible associations of genes selected from multiple neurotransmitter systems with AUD in a homogeneous Tibetan community population in China. AUD cases (N = 281) with an alcohol use disorder identification test (AUDIT) score ≥10, as well as healthy controls (N = 277) with an AUDIT score ≤5, were recruited. All participants were genotyped for 366 single nucleotide polymorphisms (SNPs) of 34 genes selected from those involved in neurotransmitter systems. Association analyses were performed using PLINK version 1.07 software. Allelic analyses before adjustment for multiple tests showed that 15 polymorphisms within seven genes were associated with AUD (p<0.05). After adjustment for the number of SNPs genotyped within each gene, only the association of a single marker (rs10044881) in HTR4 remained statistically significant. Haplotype analysis for two SNPs in HTR4 (rs17777298 and rs10044881) showed that the haplotype AG was significantly associated with the protective effect for AUD. In conclusion, the present study discovered that the HTR4 gene may play a marked role in the pathogenesis of AUD. In addition, this Tibetan population sample marginally replicated previous evidence regarding the associations of six genes in AUD.     

模拟氮沉降对藏北高寒草甸温室气体排放的影响

目前,高寒草甸对全球温室效应的贡献仍具有不确定性,而随着N沉降的增加,该系统温室体气排放也必将发生变化。为揭示高寒草甸对N沉降的响应机制,探讨其对全球变化的反馈作用,利用人工添加氮素的方法,于2014年生长季(6-9月)在那曲地区那曲县设置不同水平N添加梯度(0、7、20kg hm~(-2)a~(-1)和40 kg hm~(-2)a~(-1)),模拟氮沉降增加对藏北高寒草甸温室气体排放的影响。经过1a的研究结果表明:1)施氮显著促进了CO_2排放但对CH_4的吸收和N_2O的排放无显著影响。总体而言,添加氮素明显增加了温室气体排放总量,其中N2O处理下高寒草甸温室气体排放总量最高。2)回归分析结果表明,CO_2与NPP(总生物量)和TOC(土壤有机碳)线性相关(P0.05),而与TN(总氮)、NH_4~+-N和NO_3~--N均无显著相关关系(P0.05),CH_4与TN/NPP/TOC/NH_4~+-N/NO_3~--N均不相关(P0.05),N_2O与NPP/TOC/NO_3~--N均显著线性相关(P0.05),而与TN/NH_4~+-N不相关。综合初步研究结果,未来氮沉降增加条件下,藏北高寒草甸温室气体排放通量将有可能明显增加,从而对气候变化产生重要的反馈作用。     

Using a Low-Sodium,High-Potassium Salt Substitute to Reduce Blood Pressure among Tibetans with High Blood Pressure: A Patient-Blinded Randomized Controlled Trial

Objectives

To evaluate the effects of a low-sodium and high-potassium salt-substitute on lowering blood pressure (BP) among Tibetans living at high altitude (4300 meters).

Method

The study was a patient-blinded randomized controlled trial conducted between February and May 2009 in Dangxiong County, Tibetan Autonomous Region, China. A total of 282 Tibetans aged 40 or older with known hypertension (systolic BP≥140 mmHg) were recruited and randomized to intervention (salt-substitute, 65% sodium chloride, 25% potassium chloride and 10% magnesium sulfate) or control (100% sodium chloride) in a 1: 1 allocation ratio with three months’ supply. Primary outcome was defined as the change in BP levels measured from baseline to followed-up with an automated sphygmomanometer. Per protocol (PP) and intention to treat (ITT) analyses were conducted.

Results

After the three months’ intervention period, the net reduction in SBP/DBP in the intervention group in comparison to the control group was −8.2/−3.4 mmHg (all p<0.05) in PP analysis, after adjusting for baseline BP and other variables. ITT analysis showed the net reduction in SBP/DBP at −7.6/−3.5 mmHg with multiple imputations (all p<0.05). Furthermore, the whole distribution of blood pressure showed an overall decline in SBP/DBP and the proportion of patients with BP under control (SBP/DBP<140 mmHg) was significantly higher in salt-substitute group in comparison to the regular salt group (19.2% vs. 8.8%, p = 0.027).

Conclusion

Low sodium high potassium salt-substitute is effective in lowering both systolic and diastolic blood pressure and offers a simple, low-cost approach for hypertension control among Tibetans in China.

Trial Registration

ClinicalTrials.gov {"type":"clinical-trial","attrs":{"text":"NCT01429246","term_id":"NCT01429246"}}NCT01429246     

喷灌对藏北高寒草地生产力和物种多样性的影响

通过3a(2008—2010年)的藏北高寒草地喷灌试验,研究了不同喷灌量对草地群落生产力和物种多样性的影响。结果表明,丰水年灌溉对藏北高寒草地的影响较小;而在相对干旱年份灌溉对高寒草地生产力和物种多样性影响显著。喷灌条件下高寒草地生物量显著提高,最高增幅出现在高水(GS)样地中,达到116%。喷灌明显促进物种重要值提高,其中灌木和阔叶杂草比例增加趋势更为明显。不同喷灌条件下优势物种相对重要值均有不同程度的降低,高水处理降低幅度最大。物种多样性方面,喷灌措施能够明显促进高寒草地Simpson指数和Shannon-weiner指数增加(P0.05),E.Pielou均匀度指数无显著变化(P0.05)。Shannon-weiner指数与生物量之间存在显著正相关关系(P0.05)。未来降水增多的气候条件可以减少干旱对高寒草地带来的负面影响,有利于提高草地生产力和维持草地物种多样性,促进高寒草地畜牧业健康发展。     

西藏不同生长地砂生槐群体种子生物碱含量及其相关性分析

为了明确不同群体间和群体内砂生槐天然种子富含生物碱含量与组成的差异,该研究选取来自西藏“一江四河”流域、海拔2 900～4 100 m范围内10个群体的砂生槐种子作为研究材料,采用高效液相色谱法,测定10个群体300个单株种子重要生物碱(氧化苦参碱、苦参碱、槐果碱、槐定碱)含量,应用SPSS软件分析了地理分布特征与生物碱含量之间的相关性及群体遗传变异关系,以筛选生物碱含量较高的群体,为砂生槐药物开发利用提供依据。结果表明：(1)10个群体的砂生槐种子中均含有氧化苦参碱、苦参碱和槐果碱,含量依次为：氧化苦参碱(46.18～64.08 mg/g)>苦参碱(1.14～9.82 mg/g)>槐果碱(0.08～1.16 mg/g),其中氧化苦参碱占生物碱总量的90%以上,且群体4中含量最高(64.08±7.37 mg/g);其他微量生物碱在群体3中含量最高;群体间氧化苦参碱、苦参碱和槐果碱均差异极显著(P＜0.01)。(2)氧化苦参碱群体内和群体间变异相对较小,苦参碱和槐果碱群体内和群体间变异系数均较大,而且氧化苦参碱和槐果碱的群体间变异均大于群体内变异,苦参碱的群体间变异小于群体内变异。(3)氧化苦参碱与海拔呈显著正相关关系(r = 0.117^*),苦参碱与海拔、经度和纬度均呈极显著负相关关系(r ＜ -0.326^**),其他关系不显著。氧化苦参碱与苦参碱和槐果碱均呈显著负相关关系(r ＜-0.162^**),而苦参碱与槐果碱呈显著正相关关系(r =0.789^**)。(4)聚类分析将10个群体聚为4类,各类间的距离差异比较大,且大多与地理因素有关。     

增温对青藏高原高寒草原生态系统碳交换的影响

碳交换是影响草地生态系统碳汇功能的关键过程,对气候变暖极为敏感。青藏高原分布着大面积的高寒草原,其碳汇功能对气候变暖的响应对区域碳循环过程具有重要的影响。为探究高寒草原生态系统碳交换过程对增温的响应,2012—2014年,在青藏高原班戈县进行了模拟增温对高寒草原生态系统碳交换过程影响的研究。结果表明,增温对高寒草原碳交换各组分的影响存在年际差异,但总体上对碳交换存在负面影响。3年平均结果显示,增温显著降低了高寒草原地上生物量、总生态系统生产力(GEP)、生态系统呼吸(ER)和净生态系统碳交换量(NEE)(P0.05),平均降幅分别为15.1%、36.8%、19.2%和51.5%。增温条件下3年平均土壤呼吸(SR)较对照无显著变化(P0.05),但2013年增温显著降低了SR(P0.05),降幅达18.1%。增温对SR与ER的比值具有一定的促进作用,最高增幅达到40.0%。GEP、ER、SR和NEE与土壤温度和土壤水分无显著相关(P0.05),而GEP、ER和NEE与空气温度呈显著的负相关关系(P0.05)。增温引起的干旱胁迫以及地上生物量降低是导致高寒草原NEE降低的主要原因。研究表明,全球变暖会一定程度降低青藏高原高寒草原的碳汇功能。     

Different responses of ecosystem carbon exchange to warming in three types of alpine grassland on the central Qinghai–Tibetan Plateau

Climate is a driver of terrestrial ecosystem carbon exchange, which is an important product of ecosystem function. The Qinghai–Tibetan Plateau has recently been subjected to a marked increase in temperature as a consequence of global warming. To explore the effects of warming on carbon exchange in grassland ecosystems, we conducted a whole‐year warming experiment between 2012 and 2014 using open‐top chambers placed in an alpine meadow, an alpine steppe, and a cultivated grassland on the central Qinghai–Tibetan Plateau. We measured the gross primary productivity, net ecosystem CO₂ exchange (NEE), ecosystem respiration, and soil respiration using a chamber‐based method during the growing season. The results show that after 3 years of warming, there was significant stimulation of carbon assimilation and emission in the alpine meadow, but both these processes declined in the alpine steppe and the cultivated grassland. Under warming conditions, the soil water content was more important in stimulating ecosystem carbon exchange in the meadow and cultivated grassland than was soil temperature. In the steppe, the soil temperature was negatively correlated with ecosystem carbon exchange. We found that the ambient soil water content was significantly correlated with the magnitude of warming‐induced change in NEE. Under high soil moisture condition, warming has a significant positive effect on NEE, while it has a negative effect under low soil moisture condition. Our results highlight that the NEE in steppe and cultivated grassland have negative responses to warming; after reclamation, the natural meadow would subject to loose more C in warmer condition. Therefore, under future warmer condition, the overextension of cultivated grassland should be avoided and scientific planning of cultivated grassland should be achieved.