Reversible inhibition of the pollen germination and the stigma penetration in Crocus vernus ssp. vernus (Iridaceae) following fumigations with NO2, CO, and O3 Gases

We assessed the pollen hydration, the pollen germination, and the stigma papilla penetration of CROCUS VERNUS subsp. VERNUS (Iridaceae) after 2 h fumigations with O (3), NO (2), and CO gases within humidified (90 - 100 % RH) box experiments. When the pollen and the pistil were separately fumigated, the pollen retained the capacity to emit a tube which penetrated papilla, and the stigma papillae retained the receptivity; when the pistils were first pollinated and then fumigated, the capacity of pollen to hydrate was not affected, but the germination was significantly reduced. The vulnerability to gases became evident at 0.3 ppm O (3), 0.2 ppm NO (2), and 0.5 ppm CO. The inhibition curves as a function of the gas concentrations were of an exponential type, and they saturated at 2 ppm NO (2), 25 ppm CO, and 0.5 ppm O (3), with germination percentages of 17 %, 27 %, and 60 %, respectively. Both the pollen germination and the papilla penetration were fully restored by prolonging for 60 - 90 min the incubation at 90 - 100 % RH, after the cessation of fumigations. The vulnerability of the pollen-papilla system is discussed.     

Interactions between soil and tree roots accelerate long-term soil carbon decomposition

Decomposition of soil organic carbon (SOC) is the main process governing the release of CO₂ into the atmosphere from terrestrial systems. Although the importance of soil–root interactions for SOC decomposition has increasingly been recognized, their long-term effect on SOC decomposition remains poorly understood. Here we provide experimental evidence for a rhizosphere priming effect, in which interactions between soil and tree roots substantially accelerate SOC decomposition. In a 395-day greenhouse study with Ponderosa pine and Fremont cottonwood trees grown in three different soils, SOC decomposition in the planted treatments was significantly greater (up to 225%) than in soil incubations alone. This rhizosphere priming effect persisted throughout the experiment, until well after initial soil disturbance, and increased with a greater amount of root-derived SOC formed during the experiment. Loss of old SOC was greater than the formation of new C, suggesting that increased C inputs from roots could result in net soil C loss.     

Decelerating growth in tropical forest trees

The impacts of global change on tropical forests remain poorly understood. We examined changes in tree growth rates over the past two decades for all species occurring in large (50-ha) forest dynamics plots in Panama and Malaysia. Stem growth rates declined significantly at both forests regardless of initial size or organizational level (species, community or stand). Decreasing growth rates were widespread, occurring in 24–71% of species at Barro Colorado Island, Panama (BCI) and in 58–95% of species at Pasoh, Malaysia (depending on the sizes of stems included). Changes in growth were not consistently associated with initial growth rate, adult stature, or wood density. Changes in growth were significantly associated with regional climate changes: at both sites growth was negatively correlated with annual mean daily minimum temperatures, and at BCI growth was positively correlated with annual precipitation and number of rainfree days (a measure of relative insolation). While the underlying cause(s) of decelerating growth is still unresolved, these patterns strongly contradict the hypothesized pantropical increase in tree growth rates caused by carbon fertilization. Decelerating tree growth will have important economic and environmental implications.     

Response of Net Ecosystem Productivity of Three Boreal Forest Stands to Drought

In 2000–03, continuous eddy covariance measurements of carbon dioxide (CO₂) flux were made above mature boreal aspen, black spruce, and jack pine forests in Saskatchewan, Canada, prior to and during a 3-year drought. During the 1st drought year, ecosystem respiration (R) was reduced at the aspen site due to the drying of surface soil layers. Gross ecosystem photosynthesis (GEP) increased as a result of a warm spring and a slow decrease of deep soil moisture. These conditions resulted in the highest annual net ecosystem productivity (NEP) in the 9 years of flux measurements at this site. During 2002 and 2003, a reduction of 6% and 34% in NEP, respectively, compared to 2000 was observed as the result of reductions in both R and GEP, indicating a conservative response to the drought. Although the drought affected most of western Canada, there was considerable spatial variability in summer rainfall over the 100-km extent of the study area; summer rainfalls in 2001 and 2002 at the two conifer sites minimized the impact of the drought. In 2003, however, precipitation was similarly low at all three sites. Due to low topographic position and consequent poor drainage at the black spruce site and the coarse soil with low water-holding capacity at the jack pine site almost no reduction in R, GEP, and NEP was observed at these two sites. This study shows that the impact of drought on carbon sequestration by boreal forest ecosystems strongly depends on rainfall distribution, soil characteristics, topography, and the presence of vegetation that is well adapted to these conditions. The online version of the original article can be found under doi:     

凡纳滨对虾肠道红杆菌科细菌富集碳源筛选及其定向分离

【目的】红杆菌科(Rhodobacteraceae)细菌为凡纳滨对虾肠道微生物的优势类群,在健康对虾肠道中具有较高的相对丰度,是指示对虾健康的关键类群,探究对虾肠道红杆菌科细菌定向富集和分离方法,可为对虾养殖益生菌菌剂的研发提供基础。【方法】利用16S rRNA基因高通量测序技术研究不同碳源添加对凡纳滨对虾肠道中红杆菌科细菌的富集作用,筛选对红杆菌科细菌有显著富集作用的碳源;利用纯培养技术从红杆菌科细菌富集的样品中定向分离红杆菌科细菌,并对其进行鉴定和遗传多样性分析。【结果】添加短链脂肪酸(乙酸、丙酸、丁酸、戊酸)和碳酸氢钠对红杆菌科细菌有显著富集作用,主要富集到Cribrihabitans、Tritonibacter、Rhodovulum、Ruegeria、Sagittula和Thalassobius属相关菌株;对红杆菌科细菌相对丰度最高的样品进行稀释涂布培养,共分离纯化出303株细菌,分属于2门12科,其中红杆菌科细菌为主导类群共119株,主要包括Tritonibacter (90株)、Phaeobacter (25株)、Sulfitobacter (1株)、Ruegeria (1...     

土壤稳定性有机碳组分与优势细菌门类陆向分布及相关性

【目的】为了探究土壤稳定性有机碳组分和优势细菌门类的陆向分布特征及相关性。【方法】本文选择锡林河流域沿着由水及陆的方向依次采集长期性水流、季节性水流、长期性无水流的湿地及旱地土壤,基于国际腐殖物质协会推荐的方法和16SrRNA基因高通量测序技术分别检测土壤稳定性有机碳组分(富里酸、胡敏酸、胡敏素)含量和优势细菌门类的相对丰度,结合Pearson相关性及冗余分析和结构方程模型研究两者的相关性。【结果】三类稳定性有机碳及酸杆菌门、放线菌门、芽单胞菌门呈大致升高的陆向分布趋势,在长期性无水流的旱地土壤中达到峰值;拟杆菌门则呈现降低的陆向分布趋势。结果显示,芽单胞菌门、酸杆菌门和放线菌门作为长期性无水流旱地土壤的优势细菌门类与胡敏酸、胡敏素含量存在显著(P<0.05)或极显著(P<0.01)正相关关系;拟杆菌门作为长期和季节性水流湿地土壤的优势菌门与富里酸、胡敏酸、胡敏素的含量均呈极显著(P<0.01)负相关关系。结构方程模型结果显示,稳定性有机碳组分与优势细菌门类间存在直接和间接作用。【结论】锡林河流域土壤稳定性有机碳组分及优势细菌门类存在陆向分布特征,稳定性有机碳的升高与...     

秸秆还田方式对东北水稻土理化性质及微生物群落的影响

【目的】研究秸秆还田方式对东北黑土理化性质及微生物群落的影响。【方法】试验周期为2019年12月至2021年10月,秸秆还田采用2种方式： 秸秆直接还田+微生物菌剂WJ(strawdirect return+microbial agent WJ;MD),秸秆堆肥还田+微生物菌剂WJ(straw compost return +microbial agent WJ;MC)。分析土壤肥力、酶活和微生物群落。【结果】分析两种方式土壤有机质(SOM)、腐殖酸(HS)和富里酸有机碳(FA-C)含量,发现秸秆直接还田+微生物菌剂WJ比秸秆堆肥还田+微生物菌剂WJ分别增加2.28g/kg、7.82g/kg和5.26g/kg。土壤铵态氮(NH4⁺-N)、速效磷(AP)略高于秸秆堆肥还田+微生物菌剂WJ,均在6月份达到峰值。胡敏酸有机碳(HA-C)含量下降。此外,土壤脲酶、转化酶、纤维素酶活性和碱性磷酸酶活性对比发现,秸秆直接还田+微生物菌剂WJ比秸秆堆肥还田+微生物菌剂WJ分别高8.55%、15.46%、4.35%和6.19%。高通量测序结果显示,秸秆直接还田+微生物菌剂WJ中细菌和真菌的多样性均比秸秆堆肥还田+微生物菌剂WJ丰富。其中Anaerolinea、Bacteroidetes、Pseudomonas为优势细菌,Tausonia、Mrakia、Mrakiella为优势真菌。【结论】秸秆直接还田+微生物菌剂WJ比秸秆堆肥还田+微生物菌剂WJ更有利于土壤有机质、腐殖酸、土壤酶活性和微生物多样性的增加,这说明秸秆添加WJ菌剂直接还田可以减少有机养分的流失,保持田间土壤肥力。     

模拟地表火行为对燃烧剩余物水溶性碳氮的影响

燃烧剩余物是火烧迹地土壤表面必然存在的残留物,可以通过降水过程以及地表径流释放其所含有的矿物质和有机质至土壤生态系统,从而在一定时间内持续地对火后生态系统恢复过程造成影响。但不同火行为下,相同的可燃物所产生的燃烧剩余物可能具有不同的生态学功能,为了认知火行为对燃烧剩余物的影响,进一步了解二者对火烧迹地生态恢复过程中养分循环和能量流动的潜在影响,探究了火行为对燃烧剩余物水溶性碳氮化学计量特征的影响。以红松人工林地表可燃物为实验材料,通过设置不同坡度和含水率为火行为的驱动因子,进行了森林可燃物床层地表上坡火和下坡火的室内模拟燃烧实验。用独立样本T检验、单因素方差分析、多因素方差分析探究了火环境对燃烧剩余物水溶性碳氮和火行为的影响,用基于距离的冗余分析(db-RDA)探究了火行为对燃烧剩余物水溶性碳氮化学计量特征的影响。上坡火实验组的燃烧剩余物水溶性碳氮含量明显高于下坡火实验组(P<0.01);5°实验组中,燃烧剩余物的水溶性碳含量随着可燃物预设含水率的升高而升高(P<0.05)。进一步的数据分析发现火行为与燃烧剩余物水溶性碳氮化学计量特征关系密切,火焰宽度是影响燃烧剩余物水溶性...     

城乡景观中土壤生态系统微塑料的来源、迁移特征及其风险

土壤微塑料污染的持久性、复杂性及其对土壤生态系统的影响受到越来越广泛的关注,但对其来源、迁移过程等仍有许多问题尚未理清。从复合生态系统的角度,通过对城乡景观中土壤微塑料的来源、迁移过程及其风险等相关研究进展进行了系统梳理,分析了城乡不同景观中土壤微塑料的主要来源和特点,讨论了土壤微塑料在城乡景观中的迁移特征及其驱动力,探讨了土壤微塑料在城乡景观中的生态和健康风险。今后需进一步明确城乡景观中土壤微塑料污染的物质流过程与环境归趋特征,加强微塑料对土壤生态系统的作用过程及生态系统服务影响的研究,揭示土壤微塑料对人类健康的直接或间接影响,建立城乡复合生态系统土壤微塑料污染预测模型,以维护土壤生态安全与人居环境健康。