浙江仙居括苍山省级自然保护区天蛾科昆虫资源调查

于2014-2019年每年的4-10月、2020年4-8月,对浙江仙居括苍山省级自然保护区的天蛾科Sphingidae昆虫进行了调查,共采集标本128号,经鉴定分别隶属于3亚科、20属、32种(含亚种).依据我国动物地理区系,浙江仙居括苍山省级自然保护区的天蛾科昆虫与华中区、华南区、西南区、青藏区、华北区共有种较多,属...     

翁源青云山自然保护区维管束植物区系特征分析

青云山省级自然保护区位于韶关翁源县的东南部,本研究在查阅文献、历史标本的基础上,对本区进行全面踏查、标本采集并鉴定,从而进行植物物种多样性编目和区系分析。结果表明：青云山自然保护区有维管束植物1336种（含种下分类单位）,其中石松类和蕨类植物132种,隶属于62属24科,裸子植物6种,隶属于4属4科,被子植物1198种,隶属于588属148科;本区的表征科主要以樟科（Lauraceae）、壳斗科（Fagaceae）、冬青科（Aquifoliaceae）等为主。植物区系地理组成复杂,主要以热带、亚热带为主,且热带、亚热带的过渡性质明显。从中国特有种的分布情况来看,该地区与湖南南部、广西东北部、江西西南部联系较为紧密,体现了南岭山脉植物区系的一致性与整体性;珍稀濒危植物共计48种;植被具有中亚热带向南亚热带过渡的特征。青云山自然保护区植物物种丰富度高、植被类型多样,建议将园洞、青山口等珍稀濒危植物分布较集中的地区列为优先保护区域。     

广东蕉岭长潭自然保护区主要森林植被类型的调查

广东蕉岭长潭自然保护区的植被可分为4个植被型组、5个植被型和10个群系。以地带性植被常绿阔叶林占优势,其中中亚热带常绿阔叶林主要分布于海拔250~600 m之间,中亚热带山顶常绿阔叶矮林分布于600~700 m的山脊和山顶,竹林分布于220 m以下及网顶窝;亚热带常绿针叶林、以马尾松为优势的针阔混交林以及禾草草丛和蕨类草丛也有一定的分布,体现出植被也有一定的次生性,有必要加强保护。     

Phytophthora oleae,a new root pathogen of wild olives

Wild olive (Olea europaea subsp. europaea var. sylvestris) is an important component of Mediterranean forests and a key genetic source for olive improvement programmes. Since 2009, a severe decline caused by Phytophthora cryptogea and P. megasperma has been detected in a protected wild olive forest of high ecological value (Dehesa de Abajo, Seville, Spain). In this natural forest, sampling of roots and soil was carried out on 25 wild olives with symptoms in 2014 and 2015. Apart from the already known P. cryptogea A1 and P. megasperma, a third Phytophthora species was consistently isolated from wild olive rootlets with symptoms. These isolates conformed morphologically with the newly described species P. oleae and were confirmed by analysis of their ITS regions and cox1 sequences. Temperature–growth relationships showed a maximum growth at 19.9 °C on carrot agar medium, making it the lowest temperature Phytophthora species infecting wild olive roots. Pathogenicity was confirmed on 1-year-old healthy wild olive seedlings and was similar to the previously known pathogenic phytophthoras. As temperature requirements are quite different, the three Phytophthora species may be active against wild olive roots in different seasons. However, the prevalence of P. oleae infecting wild olives in recent years could be due to its introduction as a new invasive pathogen. The probable invasive nature of P. oleae, together with increasing rain episodes concentrated in short periods frequent in southern Spain, would allow the outbreak of infections in wild olive forests, and also put cultivated olive orchards at risk.     

井冈山国家级自然保护区森林土壤养分含量的空间变化

以井冈山国家级自然保护区为研究区,采集了57个土壤剖面的5个不同深度(0~10、10~20、20~40、40~60、60 cm)的土壤样品,对土壤样品的有机碳、全氮、全磷和全钾等指标进行了测定,并结合森林类型数据和DEM高程数据,对不同森林类型及高程条件下的土壤养分状况进行比较分析。结果表明:①土壤有机碳含量最大,全磷含量最小,各土壤养分含量均随土壤深度的增加而递减;②土壤类型的空间分布呈现海拔梯度特征,黄棕壤的分布海拔最高,依次为黄壤、黄红壤,红壤的分布海拔最低;③全磷、有机碳及C/N随着海拔高度的上升呈增加趋势。全钾含量随着海拔高度的上升呈下降趋势;④不同森林类型土壤养分存在差异,常绿阔叶林、落叶阔叶林和常绿落叶阔叶混交林的各土壤养分含量均较高;山顶矮林和温性针叶林除全氮和全钾含量外,其他土壤养分值显著高于其他林型;竹林及灌木林的土壤养分条件相对较差;⑤不同森林类型土壤养分含量的空间分布规律与其分布的海拔高度范围有关。     

楠杆自然保护区不同植被类型土壤物理特性及涵养水源功能分析

为了研究楠杆自然保护区不同植被类型的土壤物理性质与涵养水源功能,选择了保护区6种典型的植被类型（落叶阔叶林、针阔混交林、针叶林、灌木林、竹林和草坡）下的土壤物理性质、土壤蓄水能力和土壤渗透能力等进行了研究,运用综合评价法对不同植被类型进行了综合评价。结果表明:6种不同植被类型的土壤密度为0.97 1.55 g/cm³,土壤总孔隙度为35.73%～69.25%,最大持水量为357.32~692.45 g/kg。不同植被类型的土壤物理性质、土壤蓄水能力和渗透能力有明显差异。综合评价分析表明:在不同植被类型中,落叶阔叶林（∑P_i²=0.468）土壤水源涵养功能最好,其次是竹林（∑P_i²=0.784）、针阔混交林（∑P_i²=0.914）、针叶林（∑P_i²=0.984）、灌木林（∑P_i²=1.005）,没有植被覆盖的草坡（∑P_i²=1.431）上的土壤水源涵养功能综合能力相对较差。     

托木尔峰自然保护区台兰河上游不同植被类型的水源涵养功能

为了研究托木尔峰自然保护区生态系统的水源涵养功能,选择台兰河上游为研究区域,采用野外观察与室内试验相结合的方法,分别对该区域具有代表性的雪岭云杉林、灌木林、草地植被,从林冠层、枯枝落叶层和土壤层3个层次及综合性的水源涵养能力进行了定量分析。结果表明:研究区云杉林林冠截留能力优于灌木林,穿透降雨量及林冠截留量平均值均大于灌木林。除草地外,各样地枯枝落叶未分解层平均厚度均大于半分解层,云杉林枯枝落叶层的厚度和蓄积量明显大于灌木林,不同植被类型枯枝落叶半分解层的自然持水率、最大持水率均高于未分解层,云杉林枯枝落叶层自然持水率、最大持水率均高于灌木林,灌木林和云杉林的枯枝落叶未分解层有效拦蓄量均高于半分解层。不同植被类型平均土壤容重大小表现为草地灌木林云杉林,土壤孔隙度的平均值大小则与之相反;不同植被类型的土壤自然含水率、饱和含水量及非毛管持水量均表现为云杉林灌木林草地,而不同植被类型30cm深土层的蓄水能力变化则存在差异。研究区不同植被类型的水源涵养能力在181.06~237.63mm,综合、有效水源涵养能力均表现为云杉林灌木林草地,其中土壤层的涵养贡献率最大,总有效蓄水量远小于总持水量。综上所述,台兰河上游云杉林和灌木林具有较好的涵养水源能力,放牧强度和人为干扰是影响研究区不同植被类型尤其是生境脆弱的草地植被水源涵养功能的重要因素。     

Carbon isotopic ratios of wetland and terrace soil sequences in the Maya Lowlands of Belize and Guatemala

This article provides new data and synthesizes earlier findings on the carbon isotope ratios of the humin part of soil organic matter from a range of sites in the central Maya Lowlands. Changes down the soil profile in carbon isotope ratios can provide an important line of evidence for vegetation change and erosion over time, especially in well dated aggrading profiles. Research thus far has provided substantial evidence for significant inputs from C₄ vegetation in buried layers from the Ancient Maya periods in depositional soils but equivocal evidence from sloping soils. We present new findings from soil profiles through ancient Maya wetland fields, upland karst wetlands, ancient Maya aguadas (reservoirs), and ancient Maya terraces. Most of the profiles exhibited δ¹³C enrichment greater than the 2.5–3‰ typical from bacterial fractionation. Seven of nine ancient Maya wetland profiles showed δ¹³C enrichment ranging from 4.25 to 8.56‰ in ancient Maya-dated sediments that also contained phytolith and pollen evidence of grass (C₄ species) dominance. Upland karst sinks and ancient reservoirs produced more modest results for δ¹³C enrichment. These seasonal wetland profiles exhibited δ¹³C enrichment ranging from 1 to 7.3‰ from the surface to ancient Maya-period sediments. Agricultural terraces produced mixed results, with two terraces having substantial δ¹³C enrichment of 5.34 and 5.66‰ and two producing only equivocal results of 1.88 and 3.03‰ from modern topsoils to Maya Classic-period buried soils. Altogether, these findings indicate that C₄ plants made up c. 25% of the vegetation at our sites in the Maya Classic period and only a few percent today. These findings advance the small corpus of studies from ancient terraces, karst sinks, and ancient wetland fields by demonstrating substantial δ¹³C and thus C₄ plant enrichment in soil profile sections dated to ancient Maya times. These studies are also providing a new line of evidence about local and regional soil and ecological change in this region of widespread environmental change in the Late Holocene.     

徐州泉山自然保护区人工林下土壤容重与孔隙度时空变化研究

通过对设于泉山自然保护区人工侧柏林与刺槐林的4块测试样地的土壤容重进行测定,同时与裸地进行对比,结果表明,该保护区人工林下土壤容重与孔隙度随时间无确定的变化规律;而在人工林下土壤空间结构变化规律明显：不管在任何时间段,均表现出该土壤容重随土层深度增加而逐渐增大,土壤孔隙度随土层深度增加而逐渐减小的规律,并且侧柏林改变土壤容重的作用大于刺槐林。另外,该土壤容重均小于裸地,人工林通过腐殖质作用能够降低土壤容重,使其土壤通透性及保肥能力较好。     

南岭国家级自然保护区种子植物区系分析

报道了南岭国家级自然保护区种子植物区系的组成与特点。调查结果表明,该区系的种类丰富,计有种子植物１７５科８２２属２２９２种,其中裸子植物９科２０属３０种,被子植物１６６科８０２属２２６２种。区系的地理成分复杂,具有中国１５个种子分布区类型的１４个,世界其它地区的植物成分均有一定联系,其中热带成分占明显优势,同时也受到温带成分较强烈的影响,有３３个中国特有分布属。本区系具有源远源流长的发生发展历史,