退化红壤不同植被恢复类型的土壤弹尾虫群落结构

以退化红壤的侵蚀裸地、旱生性草坡、稀疏针叶林、针叶林、针阔混交林5种植被恢复类型及常绿阔叶林（对照）为研究对象,对各类型植被的土壤弹尾虫群落进行了调查,共捕获弹尾虫2亚目7科23属,其中符跳属、类符跳属、小圆跳属等为优势类群.应用个体密度、类群数及多样性指数等指标,研究了植被类型对弹尾虫群落特征的影响.结果表明：各项指标以常绿阔叶林为最高,裸地最低,基本没有弹尾虫存在;旱生性草坡、稀疏针叶林、针叶林和针阔混交林4种植被恢复类型的土壤弹尾虫群落得到了一定恢复,但各类型之间土壤弹尾虫群落没有明显差异,均处于恢复的早期阶段;Bray-Curtis指数显示,侵蚀裸地与顶级常绿阔叶林的差异最大（0.99）,其它植被恢复类型与顶级常绿阔叶林的差异也较明显,但各植被恢复类型间弹尾虫群落的差异较小.     

退化红壤植被恢复对土壤螨类群落结构的影响

对退化红壤地区的旱生性草坡、稀疏针叶林、针叶林、针阔混交林等4种植被恢复类型及裸地、顶级常绿阔叶林等2个对照样地的土壤螨类群落进行四季调查,共捕获4亚目53科,其中隐气门亚目27科（Cryptostigmata）,前气门亚目（Prostigmata）17科,中气门亚目（Mesostigmata）8科,无气门亚目（Astigmata）1科,优势类群为矮汉甲螨科（Nanhermanniidae）和单翼甲螨科（Haplozetidae）,常见类群包括若甲螨科（Oribatulidae）、盖头甲螨科（Tectocepheidae）等16科。应用个体密度、类群数、香农多样性、密度．类群DG指数、丰富度和均匀度、甲螨群落的MGP分析和捕食性螨类MI指数,研究其中螨类的群落结构特征。研究结果表明：不同植被类型土壤螨类群落差异显著,各项指标均以常绿阔叶林为最高,其次为稀疏针叶林,显著高于其它样地（P〈0．05）,针叶林和裸地处于最低水平。甲螨群落类群结构中,各植被类型中的甲螨群落均属于M型;甲螨个体密度结构类型中,裸地属于MP型,旱生性草坡属P型,常绿阔叶林属于O型,其它均属于M型。中气门螨类的MI指数在各植被类型没有明显的变化。DCA分析将6类型分为3类：裸地、常绿阔叶林各为一类,其余各类型归为一类,这显示了土壤螨类群落对植被恢复不同类型的响应。     

贡嘎山东坡典型植被类型土壤动物群落特征

为了掌握贡嘎山垂直植被带间土壤动物群落结构及多样性,2012年5月至10月间对贡嘎山东坡的常绿阔叶林、落叶阔叶林、针阔混交林和暗针叶林4种典型植被土壤动物群落进行了调查。共捕获土壤动物347只,隶属于10纲29目68类,其中山蛩属(Spirobolus)为优势类群。土壤动物的群落密度、生物量以及多样性呈常绿阔叶林落叶阔叶林针阔混交林暗针叶林趋势,其中密度、类群丰富度和Shannon-Wiener指数的变化具有显著差异(P0.05);落叶阔叶林和针阔混交林间的土壤动物群落结构差异明显,其他植被类型间的差异性受季节影响。从各功能群结构来看,腐食性和杂食性土壤动物占主要地位;各功能群的生物量均以常绿阔叶林和落叶阔叶林较高,针阔混交林和暗针叶林较低,而相对生物量的变化趋势各不相同,仅有腐食性功能群的生物量及植食性功能群的相对生物量在各垂直植被带间有显著差异(P0.05)。群落密度、生物量、类群丰富度、Shannon-Wiener指数以及腐食性和捕食性功能群的生物量与土壤温度呈显著相关(P0.05)。研究结果表明:贡嘎山东坡土壤动物的群落组成、多样性及功能群结构在各典型植被类型间有明显差异,土壤温度是影响土壤动物垂直分布格局的主要环境因子。     

鼎湖山不同自然植被土壤动物群落结构时空变化

2001年10月~2002年8月采用大型改良干漏斗和手拣法对鼎湖山鼎湖山南亚热带典型常绿阔叶林、河岸常绿阔叶林、山地常绿阔叶林、针阔混交林、沟谷常绿阔叶林和灌木草丛6种自然植被类型土壤动物群落结构时空变化进行初步调查。结果表明,蜱螨目(A carina)和弹尾目(Co llem bo la)为6种自然植被常年优势类群,缨翅目(T hysanoptera)、鞘翅目(Co leoptera)、膜翅目(Hym enoptera)和双翅目(D iptera)幼虫则为常年常见类群。土壤动物群落类群和个体数量的消长规律分别是:10月=6月=8月>4月>2月=12月和4月>10月>6月>8月>2月>12月。土壤动物个体数量总数依次为南亚热带典型常绿阔叶林>河岸常绿阔叶林>山地常绿阔叶林>沟谷常绿阔叶林>针阔混交林>灌木草丛;不同月份、不同植被类型以及不同月份和不同植被类型之间土壤动物群落的组成具有较大变化,组成差异极显著(F=5.63,α=0.0001;F=11.08,α=0.0001;F=2.97,α=0.0001),不同类群之间个体数量差异极显著(F=102.38,α=0.0001),但月份间类群数差异不显著(F=0.50,α>0.05)。多样性分析表明,类群多样性和均匀性指数除南亚热带典型常绿阔叶林、山地常绿阔叶林12月最高外,其它则2月最高,优势度指数则相反;山地常绿阔叶林土壤动物群落多样性指数和均匀性指数最大,针阔混交林则最小。     

浙江天童地区常绿阔叶林退化对土壤养分库和碳库的影响

为了解常绿阔叶林退化对土壤碳库和养分库的影响,采用空间代替时间的研究方法,以常绿阔叶林顶级群落为参照,选择了次生常绿阔叶幼年林、次生针阔混交林、次生针叶林、灌丛和灌草丛代表不同的退化类型,分别对其土壤氮磷养分库、碳库进行了调查和分析。结果表明：土壤氮库贮量从大到小依次为,成熟常绿阔叶林、次生常绿阔叶幼年林、灌丛、次生针叶林、灌草丛和次生针阔混交林;土壤总磷含量也是在成熟林最高,次生针阔混交林和次生针叶林的总磷含量显著高于次生常绿阔叶幼年林和灌丛;土壤有机碳含量从高到低依次为：成熟常绿阔叶林,次生针叶林、次生常绿阔叶幼年林、灌丛、灌草丛和次生针阔混交林;土壤铵态氮在成熟林、灌丛和灌草丛的库容量最大,其次分别为次生幼年常绿阔叶林、次生针阔混交林,最小的为次生针叶林;硝态氮则在灌草丛的库容量最大,其次分别为次生针叶林、次生针阔混交林和成熟林针叶林,最小的为次生常绿阔叶幼年林和灌丛。统计显示,常绿阔叶林退化不仅导致土壤有机碳库含量的显著下降,也使得土壤氮磷养分库含量显著下降。可以认为,砍伐导致的大量生物量输出和森林管理措施的影响,植物种类组成的改变,土壤物理性质的改变以及养分和有机碳的主要生物化学转化环节发生改变是导致此类变化的主要因素,常绿阔叶林顶极群落土壤是该地区土壤的最大养分库和碳库。     

峨眉山世界遗产地表土孢粉组合及其生态和古环境启示

通过峨眉山40个样点表土孢粉组合及其与植物群落之间关系的分析,结果表明:(1)花粉组合中木本植物含量(83.3%)占绝对优势,松属、杉科、桤木属、蔷薇科、桦属、枫杨属、蒿属、毛茛科和水龙骨科为主要孢粉类型;(2)中山常绿阔叶林花粉组合未能反映植被的群落特征;低山常绿阔叶林间人工次生林和常绿落叶阔叶混交林花粉组合只能反映母体植被的部分组成;针叶林花粉组合基本可以指示母体植被的群落特征;灌丛草甸花粉组合能够较好地反映母体植被的群落组成;针阔混交林花粉组合不仅可以很好地指示群落特征,花粉高含量类型还可以与植物群落优势种很好地对应;(3)主要花粉类型冷杉属、杜鹃花科、蔷薇科、珙桐属、槭属和盐肤木属具低代表性;枫杨属、栲属/柯属、桤木属和杉科花粉具超代表性;(4) DCA表明,通过花粉百分含量,能较好地区分人类扰动植被、阔叶林和针叶林,但常绿阔叶林、常绿落叶阔叶混交林和针阔混交林之间,针叶林和灌丛草甸之间难以区分;(5)利用孢粉学恢复热带亚热带常绿阔叶代表类群樟科群落和第三纪孑遗落叶阔叶属种珙桐群落时,受其主体植物花粉外壁薄,易破碎影响,原生植被优势种缺失;因此,孢粉实验改良和保存环境研究,与其他生物学指标(植物大化石和气孔器)综合分析在重建古植物群落中具有重要意义;(6)植物(如冷杉)花粉含量一定程度上能够指示其林分结构。本研究可为热带亚热带山地及相似地区利用孢粉学进行地质时期气候与环境重建提供理论支持和基础资料,并对植被生态恢复提供实践和参考。     

九龙大雾山北坡的植物群落

九龙大雾山北坡的植物群落可划分为南亚热带常绿阔叶林、南亚热带山地常绿阔叶林、南亚热带常绿针叶林、南亚热带灌丛,以及南亚热带山坡草地等几个群落类型,它们均属于次生性植被,是华南南亚热带植被的主要代表类群。     

贡嘎山东坡森林小型土壤节肢动物群落多样性与时空分布

为了掌握不同垂直植被类型下小型土壤节肢动物群落组成及多样性的变化规律,2012年3、5、7、10和12月对贡嘎山东坡的常绿阔叶林、落叶阔叶林、针阔混交林和暗针叶林下的小型土壤节肢动物群落进行了调查。共分离到小型土壤节肢动物8581只,隶属于8纲28目114科145类或属,优势类群为近缺虫兆属(Paranurophorus)。与我国温带及亚热带森林土壤节肢动物群落相比,贡嘎山东坡小型土壤节肢动物群落组成类群不仅丰富,且具有独特性。主成分分析及相似性指数计算结果表明,不同植被类型间的小型土壤节肢动物群落组成结构相似性较高,但群落相似性随着海拔相对高度的增加而降低。小型土壤节肢动物的群落密度、丰富度和Shannon指数均随海拔上升逐渐减小,其中暗针叶林下小型土壤节肢动物群落的丰富度和Shannon指数显著低于其他植被类型。3月和12月小型土壤节肢动物的群落密度、丰富度、Shannon指数和Simpson指数在总体上大于5月、7月和10月,且不同月份间差异显著。影响小型土壤节肢动物群落密度及多样性空间分布的主要环境因子为土壤有机质、有效磷、pH、土壤温度和湿度。研究结果表明,贡嘎山东坡小型土壤节肢动物群落组成类群丰富且具独特性;群落结构、密度及多样性指数对季节变化的响应比对植被类型变化更敏感。     

三峡库区不同植被类型土壤养分特征

通过三峡库区8个植被类型370个样地的群落调查和土壤分析,研究了不同植被类型、土壤类型、海拔对表层土壤有机质及全氮、速效磷、速效钾含量的影响.结果表明:(1)三峡库区不同植被类型土壤有机质、全氮平均含量规律为阔叶林＞竹林＞针叶林＞灌丛＞草丛,森林土壤有机质及全氮平均含量丰富;速效磷平均含量表现为草丛＞落叶阔叶林＞灌丛＞暖性针叶林＞常绿落叶阔叶混交林＞温性针叶林＞竹林＞常绿阔叶林,草丛与其他植被类型差异显著;速效钾平均含量表现为常绿落叶阔叶混交林＞落叶阔叶林＞灌丛＞针叶林＞竹林＞草丛＞常绿阔叶林,竹林、草丛、常绿阔叶林与常绿落叶阔叶混交林、落叶阔叶林、灌丛、针叶林差异显著.(2)不同土壤类型养分含量差异显著,黄棕壤中有机质、全氮含量高,分别为6.83%、0.44%,紫色土中速效磷含量高,达到54.24mg/kg.(3)随海拔升高,有机质、全氮含量呈明显增加趋势,速效磷、速效钾含量变化趋势不明显.     

不同植被恢复类型的土壤肥力质量评价

科学确定森林土壤肥力指标并进行肥力质量的评价,对立地生产力和多目标森林经营的研究有着重要意义。以采伐(径级12 cm择伐)迹地上发育来的稀树灌丛、针叶林、针阔混交林和常绿阔叶林为研究对象,进行每木调查与群落分析,并比较各群落土壤因子间的差异,用典范对应分析(CCA)和因子分析对土壤肥力质量进行定量评价。结果表明,CCA可以有效地筛选土壤肥力质量指标,有助于质量指标的科学确定;土壤肥力质量综合评价分值为稀树灌丛(0.438)常绿阔叶林(0.414)针阔混交林(-0.170)针叶林(-0.331);演替初期(19 a)的植被恢复并未使土壤结构发生明显变化,土壤肥力质量是下降的;无人为干扰的3种群落类型,针叶林表现为更高的生物量积累,而天然更新的常绿阔叶林则更有利于生物多样性的增加与土壤养分的保蓄。     

太行山区不同植被群落土壤微生物学特征变化

为评价太行山区不同植被群落土壤微生物学特征,比较分析了针阔混交林、针叶混交林、针叶纯林、落叶阔叶纯林、灌丛和裸露地6种不同植被群落中的土壤微生物区系、微生物生物量和呼吸强度等指标的变化.结果表明,6种不同植被群落土壤中的微生物学特征存在较大差异. 灌丛地在微生物数量和微生物生物量两项指标中均为最高,其余植被群落在这两项指标中的顺序从大到小依次为落叶阔叶纯林＞针阔混交林＞针叶纯林＞针叶混交林＞裸地,土壤呼吸强度也有相似的变化趋势.在进行退化山地的植被恢复时,应充分重视生态系统的自然恢复能力.     

Soil bacterial diversity in degraded and restored lands of Northeast Brazil

Land degradation deteriorates biological productivity and affects environmental, social, and economic sustainability, particularly so in the semi-arid region of Northeast Brazil. Although some studies exist reporting gross measures of soil microbial parameters and processes, limited information is available on how land degradation and restoration strategies influence the diversity and composition of soil microbial communities. In this study we compare the structure and diversity of bacterial communities in degraded and restored lands in Northeast Brazil and determine the soil biological and chemical properties influencing bacterial communities. We found that land degradation decreased the diversity of soil bacteria as indicated by both reduced operational taxonomic unit (OTU) richness and Shannon index. Soils under native vegetation and restoration had significantly higher bacterial richness and diversity than degraded soils. Redundancy analysis revealed that low soil bacterial diversity correlated with a high respiratory quotient, indicating stressed microbial communities. By contrast, soil bacterial communities in restored land positively correlated with high soil P levels. Importantly, however, we found significant differences in the soil bacterial community composition under native vegetation and in restored land, which may indicate differences in their functioning despite equal levels of bacterial diversity.     

The effects of vegetation on restoration of physical stability of a severely degraded soil in China

Vegetative restoration may increase stability of degraded soil through enrichment of soil organic carbon (SOC). It is not clear whether hydrophobic fractions of dissolved organic carbon (DOC) function, although soil water repellency is generally linked to soil stability. The objectives of this study were to determine the effects of vegetative restoration and hydrophobic DOC fractions on soil hydrological and mechanical stability. Five investigated plots included eroded bare soil as a control, restored eroded soils planted either with Camphor tree (Cinnamomum camphora) or Lespedeza shrub (Lespedeza bicolor) since 1987, and two undisturbed soils with the same vegetation types. Water stability (WS), tensile strength (TS), and soil water repellency (SWR) of soil aggregates were measured at three water potentials, i.e., ?6, ?60 hPa and oven drying at 40 °C and at three depths (0–5, 5–10 and 10–20 cm). Reforestation of Lespedeza and Camphor trees for over 15 years increased SOC, hydrophobic DOC (H-DOC) and hydrophobic acid DOC (HA-DOC), WS and TS of the restored soils compared with the eroded bare soil, with more profound effects under Lespedeza shrubs than under Camphor trees, especially for TS. No significant differences were found between the restored and undisturbed soil under the same vegetation type. SOC was significantly correlated to total porosity, hydrological and mechanical stability and soil water repellency, suggesting the significant effect of SOC on soil restoration. SWR was more closely correlated to SOC and to H-DOC concentration than to total DOC and HA-DOC in the top soil. The humification and aromaticity indices of DOC indicated that greater SWR in the soils under Lespedeza than under Camphor trees can be attributed to greater amount of litter fall and more active microbial decomposition. Although WS and TS varied with soil water potentials, TS was strongly correlated to SWR, but no link was found with WS. This study suggests that the combined influences of soil organic compounds binding and coating soil particles, retarding water wettability and modifying soil porosity are probably extremely important mechanisms of mechanical stabilization in soil. Such intricate feedback during vegetation restoration needs further study.     

红壤侵蚀地马尾松林恢复后土壤有机碳库动态

运用RothC(version 26.3)模型,并结合“时空代换法”对长汀河田红壤侵蚀退化地马尾松人工恢复后林地表层(0-20cm)土壤有机碳库的动态变化进行了反演和预测,研究结果表明:RothC 26.3模型的模拟结果能够较好地反映红壤侵蚀地植被恢复过程中土壤有机碳的变化趋势;RothC 26.3模型适用于中亚热带季风气候条件下马尾松林地土壤碳库的动态模拟;侵蚀退化地在马尾松林建植后,林地表层土壤碳吸存速率以非线性的形式上升,并在15-25a时间内达到最大,马尾松恢复后前30a林地土壤平均碳吸存速率约为0.385 tC·hm-2· a-1,自马尾松建植后演替至当地顶级群落(次生林)全过程中平均碳吸存速率约0.156 tC·hm-2·a-1;根据模拟结果得到的拟合方程,计算得到研究区红壤侵蚀退化地的碳饱和容量约为36.85 tC/hm2,固碳潜力约为33.26 tC/hm2.     

退化红壤不同植被恢复方式对蚯蚓种群的影响

对4种人工林(小叶栎、木荷、马尾松及木荷．马尾松混交林)和2种荒草地(保护荒地、轻度干扰荒地)及疏草荒地对照进行了蚯蚓种群的季节动态调查．结果表明,退化红壤植被恢复10年后蚯蚓种群有了明显的发展,但仅1种天锡杜拉蚓存在．蚯蚓密度和生物量的季节平均值顺序为：保护荒地>干扰荒地>小叶栎>木荷>马尾松>混交林>疏草荒地,其中前三者显著高于其余植被类型(P<0．05)．蚯蚓种群季节波动明显,夏季干热有强烈的抑制作用．就季节变异系数所体现的种群稳定性而言,小叶栎最高,而马尾松最低．荒草地也较低．鉴别分析从整体上刻画了不同恢复植被下蚯蚓种群的分异．由植被类型决定的归还土壤的有机物数量和质量是蚯蚓种群分异的主要驱动因子．另外．联系蚯蚓种群发展,讨论了退化红壤恢复中选择适宜植被类型的重要性．     

Dominant plant species shape soil bacterial community in semiarid sandy land of northern China

Plant species affect soil bacterial diversity and compositions. However, little is known about the role of dominant plant species in shaping the soil bacterial community during the restoration of sandy grasslands in Horqin Sandy Land, northern China. We established a mesocosm pots experiment to investigate short‐term responses of soil bacterial diversity and composition, and the related soil properties in degraded soils without vegetation (bare sand as the control, CK) to restoration with five plant species that dominate across restoration stages: Agriophyllum squarrosum (AS), Artemisia halodendron (AH), Setaria viridis (SV), Chenopodium acuminatum (CA), and Corispermum macrocarpum (CM). We used redundancy analysis (RDA) to analyze the association between soil bacterial composition and soil properties in different plant species. Our results indicated that soil bacterial diversity was significantly lower in vegetated soils independent of plant species than in the CK. Specifically, soil bacterial species richness and diversity were lower under the shrub AH and the herbaceous plants AS, SV, and CA, and soil bacterial abundance was lower under AH compared with the CK. A field investigation confirmed the same trends where soil bacteria diversity was lower under AS and AH than in bare sand. The high‐sequence annotation analysis showed that Proteobacteria, Actinobacteria, and Bacteroidetes were the most common phyla in sandy land irrespective of soil plant cover. The OTUs (operational taxonomic units) indicated that some bacterial species were specific to the host plants. Relative to bare sand (CK), soils with vegetative cover exhibited lower soil water content and temperature, and higher soil carbon and nitrogen contents. The RDA result indicated that, in addition to plant species, soil water and nitrogen contents were the most important factors shaping soil bacterial composition in semiarid sandy land. Our study from the pot and field investigations clearly demonstrated that planting dominant species in bare sand impacts bacterial diversity. In semiarid ecosystems, changes in the dominant plant species during vegetation restoration efforts can affect the soil bacterial diversity and composition through the direct effects of plants and the indirect effects of soil properties that are driven by plant species.     

云南岩溶断陷盆地土地利用方式对丛枝菌根真菌群落结构的影响

【背景】丛枝菌根真菌(arbuscular mycorrhizal fungus,AMF)是一类能与绝大部分植物形成共生关系的真菌,在植被演替和生态恢复过程中发挥重要作用。【目的】了解云南岩溶断陷盆地不同土地利用方式对AMF群落结构的影响。【方法】采用Illumina HiSeq 2500高通量测序技术对云南岩溶断陷盆地林地、灌丛和草地等3种土地利用方式土壤样品的AMF群落结构进行分析。【结果】草地总磷(total phosphorus,TP)、速效钾(available potassium,AK)、交换性镁(exchangeable magnesium,E-Mg)、电导率(electrical conductivity,EC)和土壤温度(temperature,T)显著高于林地和灌丛,林地总氮(total nitrogen,TN)和有机碳(soil organic carbon,SOC)含量显著高于灌丛和草地。TN、SOC、AK和EC是AMF群落结构最主要的影响因子。草地样品的Chao1、ACE、Shannon和Observed species指数显著高于林地和灌丛样品,尽管Simpson指数差异不显著,但是也表现出了类似的变化趋势。9个土壤样品共产生953个AMF-OTU,鉴定出AMF 3个纲4个目9个科13个属。Glomeromycetes和Paraglomeromycetes为优势纲;Glomus和Paraglomus为优势属,其次为Claroideoglomus、Acaulospora和Diversispora。Glomus和Diversispora主要分布在草地和灌丛中,随着演替的进行其相对丰度有所下降,而Paraglomus的相对丰度逐渐上升。【结论】云南岩溶断陷盆地土地利用方式的AMF群落结构具有显著差异,土壤理化因子是重要的影响因素。     

Classification and ordination of communities of soil arthropods in an urban park of Osaka City

To assess the effect of management of a park on soil arthropods, communities of Oribatida and Collembola were analyzed at 11 sites of different vegetation in Tsurumi Park, an urban park of Osaka City. The type of canopy layer and soil density strongly affected the community parameters, such as species diversity. Ordination revealed that soil density, contents of organic matter, and shrub layer were important for variety in the oribatid community; the shrub layer was important for the collembolan community. Species richness of both arthropod groups was highest in a mixed forest and lowest on bare land, while the abundance of Collembola was highest on a lawn site. Areas of a common vegetation type had a similar oribatid community;Trichogalumma nipponica dominated in deciduous forests,Eohypochthonius crassisetiger in mixed forests and one of coniferous forests. On the other hand, collembolan communities did not correspond with the vegetation.Sminthurinus sp. was collected from every site, and the most abundant species wasCryptopygus thermophilus that exhibited an outbreak on lawn sites. A significant correlation existed between species diversities but not between abundances of Oribatida and Collembola.     

Biogeochemical and Microbial Legacies of Non‐Native Grasses Can Affect Restoration Success

The restoration of disturbed ecosystems is challenging and often unsuccessful, particularly when non‐native plants are abundant. Ecosystem restoration may be hindered by the effects of non‐native plants on soil biogeochemical characteristics and microbial communities that persist even after plants are removed. To examine the importance of soil legacy effects, we used experimental restorations of Florida shrubland habitat that had been degraded by the introduction of non‐native grasses coupled with either mechanical disturbance or pasture conversion. We removed non‐native grasses and inoculated soils with native microbial communities at each degraded site, then examined how habitat structure, soil nitrogen, soil microbial abundances, and native seed germination responded over two years compared to undisturbed native sites. Grass removal treatments effectively restored some aspects of native habitat structure, including decreased exotic grass cover, increased bare ground, and reduced litter cover. Soil fungal abundance was also somewhat restored by grass removals, but soil algal abundance was unaffected. In addition, grass removal and microbial inoculation improved seed germination rates in degraded sites, but these remained quite low compared to native sites. High soil nitrogen persisted throughout the experiment regardless of treatment. Many treatment effects were site‐specific, however, with legacies in the more degraded vegetation type tending to be more difficult to overcome. These results support the need for context‐dependent restoration approaches and suggest that the degree of soil legacy effects may be a good indicator of restoration potential.     

生态恢复对马尾松叶片化学计量及氮磷转移的影响

为了解生态恢复对侵蚀红壤恢复的马尾松林叶片碳氮磷化学计量及氮磷养分转移的影响,在福建省长汀县河田镇典型侵蚀红壤区选取恢复13、30、33a的马尾松林为研究对象,并以未治理侵蚀地(CK1)和次生林(CK2)分别作为恢复前和恢复后的对照,通过测定马尾松叶片的碳、氮、磷含量,计算其计量比,内稳性指数和氮磷转移率,分析了侵蚀红壤生长的马尾松养分限制与养分转移的关系。结果表明:在侵蚀红壤恢复过程中,马尾松1年龄叶片C、N、P含量及1年龄叶片C∶N、C∶P、N∶P变化较小,这与马尾松较高的内稳性有关(N和P内稳性指数分别为7.57和3.89)。所有实验地马尾松1年龄叶片N∶P处于11.0—13.4之间,表明马尾松的生长受N、P共同限制,其中马尾松叶片N转移率显著低于P转移率,这与生态恢复过程中马尾松养分利用效率、生长需求以及土壤养分供应状况有关。1年龄叶片C∶N、C∶P分别与马尾松N、P转移率成负相关关系,当马尾松叶片C∶N、C∶P较低时,表明N、P利用效率较低,叶片衰老时更多的N和P被转移利用;反之,则N、P利用效率较高,转移率低。同时,C∶N、C∶P分别与树高、胸径成显著负相关关系,即马尾松生长对N、P的需求同样会影响化学计量比的变化,从而影响养分转移。虽然侵蚀地生态恢复过程中土壤N、P含量增加,但仍较贫瘠,不足以满足马尾松的生长,马尾松养分转移率较高,因此,为了提高侵蚀地恢复的马尾松林的生产力,建议下一步恢复措施中适当施加N肥和P肥。该研究将侵蚀红壤不同生态恢复年限的马尾松叶片C、N、P化学计量及养分转移结合,有助于全面、系统地揭示生态恢复过程马尾松林的养分循环,对指导侵蚀红壤恢复和提高马尾松生产力具有重要意义。