塔里木河下游土壤水分与植被时空变化特征

运用变异系数、Pearson相关和回归的方法,分析了塔里木河下游2002-2006年土壤水分的时空变化和植被的分布,以及二者之间的相互关系。结果表明:土壤含水率水平空间分布随离水源地距离增加而降低,垂直分布随土层深度的增加而增加;0-60cm土壤含水率变异性最小,属中等变异性;60cm以下土壤含水量变异性增大,属强变异性;土壤含水率的时间变化受生态输水量和持续时间的制约。土壤含水率与植被的时空分布具有同步性;植被特征指数与80-280cm土壤含水率显著相关,且二者与地下水埋深均呈现极显著负相关,说明60cm以下的土壤含水率显著影响植被的生长和分布,而且地下水位是影响土壤水分和植被时空变异的主要因素。     

Effects of storage,mucilage presence,photoperiod, thermoperiod and salinity on germination of Farsetia aegyptia Turra (Brassicaceae) seeds: implications for restoration and seed banks in Arabian Desert

Seed viability and germination are key factors in the success of restoration efforts, especially when stored seeds are used. However, the effect of seed storage on germination of most of the native Arabian species is not well documented. We investigated the effect of storage time and role of the seed mucilage in regulating germination, dormancy, salinity tolerance and consequential survival strategy of F. aegyptia in an unpredictable arid desert setting. Effect of light and temperature during germination was studied under two photoperiods and two thermoperiods using intact and de-mucilaged seeds. Presence of mucilage and thermoperiod did not affect the germination. However, seed collection year and photoperiod had a highly significant effect on the germination. Increasing salinity levels decreased the germination of F. aegyptia but ungerminated seeds were able to germinate when salinity stress was alleviated. Seed storage at room temperature enhances the germination percentage, indicating that F. aegyptia seeds have physiological dormancy and it can be alleviated by after-ripening at dry storage. In addition, F. aegyptia seeds show ability to germinate at lower salinity concentration and remain viable even at higher saline conditions, indicating their adaptability to cope with such harsh environmental conditions.     

库布齐沙漠东部不同生物结皮发育阶段土壤温室气体通量

以流动沙地为对照,采用时空替代法分析库布齐沙漠东部固定沙地上不同发育阶段生物结皮藻类结皮和地衣结皮土壤温室气体通量特征及其与环境因子之间的关系,研究生物结皮发育对荒漠土壤温室气体通量的影响.结果表明: 荒漠土壤CO₂排放通量大小为地衣结皮(128.5 mg·m^-2·h^-1)>藻结皮(70.2 mg·m^-2·h^-1)>流动沙地(48.2 mg·m^-2·h^-1),CH₄吸收通量大小为地衣结皮(30.4 μg·m^-2·h^-1)>藻结皮(21.2 μg·m^-2·h^-1)>流动沙地(18.2 μg·m^-2·h^-1),N₂O排放通量大小为地衣结皮(6.6 μg·m^-2·h^-1)>藻结皮(5.4 μg·m^-2·h^-1)>流动沙地(2.5 μg·m^-2·h^-1).CO₂排放具有明显的季节变化,生长季显著大于非生长季;CH₄和N₂O季节变化差异不显著,前者生长季吸收大于非生长季,后者非生长季排放大于生长季.土壤有机碳和全氮含量、土壤微生物数量均是影响温室气体通量的重要因素,环境水热因子是影响土壤CO₂排放的关键因子,但CH₄和N₂O通量对水热因子的变化不敏感.随着植被恢复和生物结皮发育,荒漠土壤温室气体累积通量的不断增大导致其百年尺度的全球增温潜势亦显著提高,依次为地衣结皮(1135.7 g CO₂-e·m^-2·a^-1)>藻结皮(626.5 g CO₂-e·m^-2·a^-1) >流动沙地(422.7 g CO₂-e·m^-2·a^-1).     

模拟降水量变化对荒漠草原土壤酶活性的影响及其相关因素分析

为明确荒漠草原土壤酶活性对降水格局改变的响应机制, 该研究基于宁夏荒漠草原降水量不同梯度变化(减少50%、减少30%、自然降水、增加30%和增加50%)的野外试验(2014年开始试验), 于2016年5-7月采样, 测定分析不同降水梯度2年后对土壤酶活性的影响, 并分析酶活性与植物生物量、微生物生物量C∶N∶P生态化学计量特征以及土壤理化性质的关系。结果表明: (1)与自然降水量相比, 减少30%降水量对3种土壤酶活性均无显著影响, 减少50%降水量显著降低了土壤蔗糖酶活性(^P < 0.05); 增加降水量显著提高了土壤蔗糖酶和磷酸酶活性(^P < 0.05), 但对脲酶活性无显著影响。(2)减少降水量对植物生物量影响较小(尤其减少30%降水量), 但不同程度地降低了微生物生物量C、N、P, 提高了微生物生物量C∶N和C∶P; 增加降水量则不同程度提高了植物生物量及微生物生物量C、N、P。(3)土壤蔗糖酶和磷酸酶活性随植物及微生物生物量增加而增加; 对土壤酶活性影响显著的土壤因子包括: 含水量、NO₃^- N、NH₄⁺ N、C∶P、有机C、全N、C∶N和pH (P < 0.05)。研究认为, 减少降水量(尤其是减少30%降水量)对土壤酶活性影响较小, 增加降水量促进了植物的生长、刺激微生物活性, 进而提高了土壤酶活性, 但随着植物生物量增加, 土壤有机C输入增多, 磷酸酶活性相应增强并促进了有机P的矿化, 导致土壤微生物P限制增加。     

Mule Deer Migrations and Highway Underpass Usage in California,USA

Roadways may pose barriers to long-distance migrators such as some ungulates. Highway underpasses mitigate wildlife-vehicle collisions and can be an important management tool for protecting migration corridors. In northern California, 3 underpasses were built on United States Route 395 (Route 395) in Hallelujah Junction Wildlife Area (HJWA) in the 1970s for a migratory mule deer (Odocoileus hemionus) herd that had been negatively affected by highway traffic. To determine whether these underpasses were still reducing mule deer mortalities >40 years after construction, we investigated deer use of the underpasses from 2006–2019 using cameras, global positioning system (GPS) collars, and roadkill records. We used occupancy models, approximations of GPS-collared mule deer movement paths, and roadkill locations to estimate the highway crossing patterns of deer. From camera data, there was higher use of the underpasses by deer during migration (spring [Mar–Jun], fall [Oct–Dec]) than in summer (Jul–Sep), when only resident deer were present. Higher underpass usage occurred in the spring compared to fall migrations. Eleven of 21 GPS-collared migrating mule deer crossed Route 395. We estimated 30% of the crossings (by 7 of the 11 deer) occurred south of the underpasses where deer could easily access the highway because of short (1-m high) and deteriorating highway fencing. Roadkill data confirmed that deer-vehicle collisions were occurring south of the underpasses and at the underpasses. This was likely due to deteriorating infrastructure at the underpasses that allows wildlife access to the highway. Overall, our study indicated that although underpasses can provide safe passage for migratory deer decades (>40 yr) after their construction, deteriorating infrastructure such as fencing and gates can lead to wildlife mortalities on highways near underpasses. © 2021 The Wildlife Society.     

温度和水分对无芒隐子草和条叶车前种子萌发的影响

研究了无芒隐子草 (Cleistogenessongorica)和条叶车前 (Plantago lessingii)种子萌发对不同温度和水分渗透势的响应。温度在 10℃恒温至 5 0 /2 0℃变温范围内设 11个处理 ,水分渗透势在 0～ - 1.8MPa区间以 0 .2 MPa为间隔设 10个处理。结果显示 :无芒隐子草鞘内小穗的种子具有很高的生活力 ,其萌发温度幅较宽 ,在 10～ 5 0 /2 0℃温度区间 ,较高温度促进萌发 ;条叶车前种子萌发温度幅较窄 ,在 10～ 30℃温度区间 ,较低温度促进其萌发。无芒隐子草和条叶车前种子的最佳萌发温度分别为35 /2 0℃变温和 2 0℃恒温 ,在此条件下的发芽率分别达 94 %和 6 1% ,后者发芽率低的原因是种子存在生理休眠。两种植物种子萌发的最低水分阈值为 - 1.6 MPa,发芽率皆随渗透势降低而呈直线下降趋势 ,但条叶车前较无芒隐子草下降缓慢。发芽率 (y)与渗透势 (x)的回归方程 ,无芒隐子草为 y1 =- 10 .976 x1 98.4 (r2 =0 .95 4 ) ,条叶车前为 y2 =- 5 .90 9x2 6 0 .2 (r2 =0 .96 4 )。随着水分胁迫的加剧 ,供试种胚芽长呈逐渐下降趋势 ,但胚根长呈先增加 (无芒隐子草在 - 0 .6 MPa,而条叶车前在 - 0 .4 MPa)而后下降的趋势。讨论了两种植物种子萌发对不同温度和水分响应的生态学意义     

荒漠草原区柠条固沙人工林地表草本植被季节变化特征

研究荒漠草原人工林固沙区地表草本植被季节变化特征及其和柠条林龄的关系,对于分析柠条人工林地表草本植物的季节适应性和制订合理的人工林管理措施均具有重要的科学意义。选择6、15、24年生和36年生柠条人工林为研究对象,通过调查每个样地5月、8月和10月地表草本植物密度、物种数、盖度和高度,分析了荒漠草原区柠条人工固沙林生长过程中地表草本植被季节变化特征及其影响因素。结果表明,地表草本植物物种数在柠条林龄6和15a时受季节改变的影响较小,在24a之后受到季节变化的显著影响(P0.05)。地表草本植物密度在柠条林龄6a时受季节改变的影响较小,但在15a之后季节变化显著影响地表草本植物个体数分布(P0.05),而且在10月具有最多的地表草本植物个体数。地表草本植被盖度和高度均受到季节变化的显著影响(P0.05),而受林龄的影响较小;不同年龄林地地表草本植被盖度和高度均表现为10月和8月较高,5月较低。研究表明,荒漠草原柠条人工林固沙区,柠条林发育生长和灌木形态的改变不仅影响土壤营养条件,而且还可以调控由于季节改变而引起的土壤温湿度变化,柠条林龄和季节更替二者交互作用,共同影响地表草本植被的季节变化特征。     

Intraspecific competition for host resources in a parasite

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Effects of desertification on the C:N:P stoichiometry of soil,microbes, and extracellular enzymes in a desert grassland

为探讨荒漠草地沙漠化对“土壤-微生物-胞外酶”系统生态化学计量的影响机理, 该研究采用空间序列代替时间演替的方法, 研究了宁夏盐池荒漠草地沙漠化过程中土壤、土壤微生物及土壤胞外酶碳(C)、氮(N)、磷(P)生态化学计量的变异特征。结果表明: (1)随着荒漠草地沙漠化的不断加剧, 土壤C、N、P含量和土壤C:P、N:P均呈降低趋势, 而土壤C:N逐渐增加。(2)荒漠草地沙漠化过程中, 土壤微生物生物量C (MBC):微生物生物量P (MBP)、微生物生物量N (MBN):MBP和土壤β-葡萄糖苷酶(BG):N-乙酰氨基葡萄糖苷酶(NAG)逐渐降低, 而土壤BG:磷酸酶(AP)和NAG:AP基本表现为增加趋势。(3)随着荒漠草地沙漠化程度的加剧, 土壤微生物C利用效率CUE_C:N和CUE_C:P与土壤微生物N利用效率NUE_N:C和土壤微生物P利用效率PUE_P:C的变化趋势相反。(4)荒漠草地土壤、土壤微生物生物量和土壤胞外酶C:N化学计量(C:N, MBC:MBN, BG:NAG)与土壤、土壤微生物生物量和土壤胞外酶N:P化学计量(N:P, MBN:MBP, NAG:AP)显著负相关, 而土壤和胞外酶C:N化学计量(C:N, BG:NAG)与土壤和胞外酶C:P化学计量(C:P, BG:AP)显著正相关。土壤N:P与土壤MBN:MBP显著正相关, 而与土壤NAG:AP显著负相关。分析表明, 荒漠草地沙漠化过程中土壤微生物生物量及胞外酶活性随着土壤养分的变化而发生变化; 微生物-胞外酶C:N:P生态化学计量与土壤养分存在协变关系, 为理解荒漠草地土壤-微生物系统C、N、P循环机制提供理论依据。     

Persistence in the desert: ephemeral waterways and small‐scale gene flow in the desert spring amphipod,Wangiannachiltonia guzikae

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