Nursing biocrusts: isolation,cultivation, and fitness test of indigenous cyanobacteria

Biological soil crusts (biocrust) are microbial communities that develop at the soil surface of drylands and play an important role in erosion control and fertility. Soil surface disturbance from a broad range of natural and human processes (e.g. fire, livestock grazing, off‐road traffic) cause significant losses in biocrust cover and associated ecosystems services. Hence, biocrust restoration is emerging as an important intervention strategy to rehabilitate degraded dryland soils. In a multistep process, we designed protocols for the establishment of “microbial nurseries” to produce photosynthetic cyanobacterial inoculum for biocrust seeding at scale. We first report on the strategy for isolation, directly from the target site, of a large culture collection of cyanobacteria that included multiple representatives of the five most common biocrust taxa. After genetic pedigreeing of these isolates, we could select those that best matched field populations genetically for scale‐up cultivation. We then developed protocols for effective cyanobacterial biomass production to obtain sufficient inoculum. This was followed by conditioning treatments (hardening off) to preacclimate this inoculum to the stressful conditions expected in the field. Finally, we show that the inoculum obtained was fit to thrive in its original soil under natural outdoor conditions if sufficient water was available. We repeated this process successfully for four sites, two in the hot Chihuanuan desert and two in the cooler Great Basin Desert, and on two textural types of soils in each. The cyanobacterial biocrust nursery approach represents a versatile, viable, and safe tool for the rehabilitation of dryland soils.     

Effects of sand burial on biomass, chlorophyll fluorescence and extracellular polysaccharides of man-made cyanobacterial crusts under experimental conditions

Soil cyanobacterial crusts occur throughout the world, especially in the semiarid and arid regions. It always encounters sand burial, which is an important feature of mobile sand dunes. A greenhouse study was conducted to determine the effects of sand burial on biomass, chlorophyll fluorescence and extracellular polysaccharides of man-made cyanobacterial crusts in six periods of time (0, 5, 10, 15, 20 and 30 d after burying) and at five depths (0, 0.2, 0.5, 1 and 2cm). The results indicated that with the increase of the burial time and burial depth extracellular polysaccharides content and Fv/Fm decreased correspondingly and there were no significant differences between 20 and 30 burial days under dif-ferent burial depths. The degradation of chlorophyll a content appeared only at 20 and 30 burial days and there was also no significant difference between them under different burial depths. It was also observed a simultaneous decrease of the values of the Fv/Fm and the content of extracellular poly-saccharides happened in the crusted cyanobacterium Microcoleus vaginatus Gom. It may suggest that there exists a relationship between extracellular polysaccharides and recovery of the activity of pho-tosystem II (PS II) after rehydration.     

Response of the moss Racomitrium lanuginosum to changes in sheep grazing and snow‐lie due to a snow‐fence

Question: What are the responses of Racomitrium lanuginosum moss to altered snow‐lie and sheep use? Location: ACarexbigelowii‐Racomitrium lanuginosum heath on a Scottish montane plateau affected since 1986 by a fenced ski corridor. Methods: Permanent quadrats were set up along transects 45 m long perpendicular to the snow‐fence. Cover was assessed over a 12‐year period from 1990. Pellet‐group clearance counts provided data on sheep usage between 1990 and 1996. Snow‐lie was mapped in the springs of 1991–1996. Results: The snow‐fence created a gradient in sheep use and altered the duration of snow‐lie. At the start of monitoring Racomitrium cover was lower immediately adjacent to the fence, and after 12 years its cover was significantly reduced within 10 m of the fence. Further away from the fence Racomitrium cover was relatively stable. The loss of Racomitrium was correlated both with increased snow‐lie and heavier sheep usage. Grass cover increased near the fence and was related to sheep use. Dicranum fuscescens responded differently to Racomitrium, increasing significantly near the fence. Conclusions: We found that changes in snow‐lie and grazing pressure quickly brought about vegetation change in this montane ecosystem. Racomitrium was the most sensitive species to the changes in grazing and snow‐lie caused by the fence, having the biggest initial changes. Loss of Racomitrium permitted increases of species more resistant to grazing including Dicranum fuscescens and grasses.     

Characterization of diverse plant communities in Aspen Parkland rangeland using LiDAR data

Question: How effective is high-resolution airborne LiDAR technology for quantifying biophysical characteristics of multiple community types within diverse rangeland environments? Location: Native Aspen Parkland vegetation in central Alberta, Canada. Methods: Vegetation within 117 reference plots stratified across eight types, including forest, shrubland, upland grassland and lowland meadow communities, were assessed in 2001 for the height, cover and density of vegetation within various strata (herb, shrub and tree layers). Actual ground data were subsequently compared against modelled values for each community type and strata derived from the analysis of airborne LiDAR data obtained in 2000. Results: LiDAR data were effective for quantifying vegetation height, cover and density of the overstory within closed- and open Populus forest communities. However, LiDAR measurements typically underestimated the height and cover of shrublands, as well as most of the herbaceous communities. Analysis of LiDAR intensity data indicated reflectance generally decreased as LiDAR sampling points moved upwards from the ground to the vegetation canopy. Conclusions: While LiDAR technology is useful for characterizing deciduous forest properties, the quantification of understory vegetation characteristics, as well as those of individual shrublands and grasslands, was more limiting. Further refinements in analysis methods are necessary to increase the reliability of characterizing these communities.     

叶片毛尖对齿肋赤藓结皮凝结水形成及蒸发的影响

凝结水(隐匿降水)和降水是荒漠地区两种不同形式的水分来源,对荒漠生态系统极为重要。叶片毛尖(leaf hair points, LHPs)是很多荒漠藓类的重要外部形态结构特征,但它在藓类植物利用凝结水和降水中的作用尚不清楚。齿肋赤藓(Syntrichia caninervis)是古尔班通古特沙漠藓类结皮的优势种,其叶片顶端具有较长的白色毛尖。本文采用自制微渗计(h=3.5 cm, d=5.7 cm)研究了正常有毛尖和人工去除毛尖的齿肋赤藓结皮的凝结水特征及其在3种模拟降水梯度(1 mm, 3 mm, 6 mm)下的短期蒸发特征,结果表明：(1) 在凝结阶段,有毛尖结皮每时段的凝结水量均大于无毛尖结皮,但日出后有毛尖结皮凝结水下降速度稍快;有毛尖结皮的日凝结水量均大于无毛尖结皮,且前者的总凝结水量比后者多10.26%,即毛尖能增加10.26%的凝结水量。(2) 3种模拟降水梯度下,有毛尖结皮在各时段的累积蒸发率始终小于无毛尖结皮,以蒸发前期阶段最为明显,表明毛尖能显著减少和延缓结皮内的水分蒸发、延长植株水合时间,而且降水量越大减缓效果越明显。毛尖对这2种不同形式水分利用的差异是因为利用方式不同：对凝结水的利用主要归因于毛尖增大了结皮表面粗糙度,而减少对降水的蒸发主要是毛尖能反射阳光、形成内部毛细管及减小植株间隙的缘故。因此,毛尖的存在有利于齿肋赤藓结皮对凝结水和降水的利用,增强了藓类结皮对干旱环境的适应能力。     

沙地不同发育阶段的人工生物结皮对重金属的富集作用

生物结皮广泛存在于沙地生态系统,具有重要的生态功能.通过对位于库布齐沙漠腹地达拉特旗火力发电厂附近沙地中不同年代人工生物结皮及物理结皮中重金属含量的测定,旨在分析不同类型生物结皮及物理结皮在不同的发育阶段对重金属富集的影响和重金属污染的指示程度.通过分析和比较,得出以下结论:不同年代生物结皮和物理结皮各种重金属含量均表现为随着发育时间的增加而增加的趋势,生物结皮重金属含量多数类型表现为:Zn＞Cr＞Ni＞Pb＞Cu＞As＞Co＞Cd＞Hg的顺序关系,少数类型表现为:Cr＞Zn＞Ni＞Pb＞Cu＞As＞Co＞Cd＞Hg的顺序关系.通过单因素方差分析(ANOVA),不同年代藓结皮中各种元素差异显著性(P＜0.05)明显低于藻结皮和物理结皮.相同年代生物结皮和物理结皮重金属含量都表现为同样地规律:藓结皮＞藻结皮＞物理结皮,表明相同背景条件下,藓结皮对各种重金属的富集能力明显比藻结皮和物理结皮的富集能力强.通过单因素方差分析(ANOVA),Hg和Ni元素含量在所有相同年代样地的生物结皮和物理结皮均无差异,Cr、Zn、Cu、Co元素含量均存在差异(P＜0.05),但差异有的表现在藓结皮和藻结皮之间,而有的表现为藻结皮和物理结皮之间,而Pb、As、Cd元素含量则表现为有的年代有差异,有的年代无差异.通过污染因子CF值分析,藓结皮对污染的指示作用要明显比藻结皮和物理结皮敏感.同时生物结皮对于重金属的富集具有一定的选择性,像Hg、Ni、Zn、Cu、Pb、Co等元素生物结皮相对富集较少,而像Cr、Cd、As等元素相对富集较多.     

模拟降水对古尔班通古特沙漠生物结皮表观土壤碳通量的影响

水分是控制干旱区生态过程的重要环境因素,在水分受限制的生态系统中,降水通过改变土壤的干湿状态直接控制地下生物过程。生物结皮作为干旱区主要的地表覆盖物,能利用空气中有限的水分进行光合作用,其自身的碳交换是干旱区土壤碳通量的重要组成部分。通过模拟0(对照)、2、5 mm和15 mm 4个降水梯度,利用红外气体分析仪,对古尔班通古特沙漠中部生物结皮以及裸地表观土壤碳通量进行测量,探讨不同强度降水条件下生物结皮对表观土壤碳通量的影响,结果表明:(1)降水增加了生物结皮表观土壤碳释放量,2、5 mm和15 mm 3种降水处理累积碳释放量分别是对照的151.48%、274.97%、306.44%,并且随着降水后时间的延长,表观土壤碳通量逐渐减小直至达到降水前的水平;(2)生物结皮与裸地的表观土壤碳通量对降水的响应不同,对照和最大降水量下,生物结皮表观土壤碳通量大于裸地,但是2 mm和5 mm降水后,生物结皮表观土壤碳通量小于裸地,并且二者在2 mm降水时差异显著(P<0.05),而在其它降水处理下无显著差异;(3)连续两次降水事件,活性碳在初级降水后的大量释放使得二次降水后释放量下降,其中裸地碳释放量下降速率与降水强度正相关。本研究说明,在探求荒漠地区土壤碳交换对降水的响应规律时,应该考虑生物结皮的影响以及连续降水事件的差异。     

杂色山雀对人工巢箱内苔藓类巢材的选择

2008年及2009年每年的3～8月,在辽宁省仙人洞国家级自然保护区对杂色山雀(Parus varius)人工巢箱内苔藓类巢材进行了收集和鉴定,发现巢中共有藓类植物7科9属。其中,小锦藓属(Brotherella)、青藓属(Brachytheccium)、棉藓属(Plagiothecium)及绢藓属(Entodon)所占比重较大。我们分别按照样方和苔藓群落采集了周围环境中的藓类植物,鉴定出7科8属的藓类植物;采集到35个苔藓群落,出现最多的是东亚小锦藓(B.fauriei)群落。结果显示,杂色山雀对苔藓的选择可能与苔藓的生物学特性、分布和数量有关。另外通过统计分析和比较得出,按照苔藓群落来采集的方式更适合本文的研究。     

黄山藓类植物区系

对黄山进行了多次实地调查、考察和标本采集,经分类鉴定,收集整理有关黄山藓类的研究资料,目前黄山藓类植物有46科、135属、401种（包括7亚种和22变种）,与20世纪50年代陈邦杰等以及后来对黄山的调查研究结果相比,藓类植物增加了4科、28属、184种;科内种数（≥15种）优势科有10个,属内种数（≥6种）的优势属有18个。黄山藓类植物地理成分类型复杂,东亚成分（包括中国特有）占37.82%,温带成分占35.13%,热带、亚热带成分占26.75%,表现出明显的由亚热带向温带过渡的特性。