游动分割窗技术在生态交错带定量判定中的应用*-以四川巴郎山岷江冷杉林线为例

 以样带上样方间的距离系数为指标,采用游动分割窗技术辨析了岷江冷杉(Abies faxoniana)林线附近交错带的位置和宽度。结果表明,Bray-Curtis距离、相对欧氏距离、弦距离与平方欧氏距离的峰值和峰宽具有很好的重合性,上述距离系数均能作为判定林线交错带群落的边界和宽度的优良指标,其中,平方欧氏距离更能直观和准确地反映交错带植被的变异。样带上距离系数的峰值区和峰宽对生态交错带的位置和宽度有较为敏感的指示意义,游动分割窗技术是交错带判定和群落划分的有效方法。以样带上样方间的距离系数为指标,采用游动分割窗技术辨析了岷江冷杉(Abies faxoniana)林线附近交错带的位置和宽度。结果表明,Bray-Curtis距离、相对欧氏距离、弦距离与平方欧氏距离的峰值和峰宽具有很好的重合性,上述距离系数均能作为判定林线交错带群落的边界和宽度的优良指标,其中,平方欧氏距离更能直观和准确地反映交错带植被的变异。样带上距离系数的峰值区和峰宽对生态交错带的位置和宽度有较为敏感的指示意义,游动分割窗技术是交错带判定和群落划分的有效方法。     

长白山北坡植被垂直带群落交错区的定量判定

以海拔梯度上的群落重要值和二元数据为指标,采用游动分割窗技术辨析了长白山北坡各植被带群落交错区的位置和宽度．结果表明,采用平方欧氏距离(SED)和Bray—Curtis距离函数(PD)计算的游动分割窗的峰值和峰宽有较好的重合性,其中基于灌木和草本物种重要值的平方欧氏距离更能准确地反映交错带植被的变异．依据游动分割窗的分析,判定阔叶红松林和暗针叶林的交错区为渐变类型,位于海拔1120m,宽度为200m,暗针叶林和岳桦交错区为急变类型,位于海拔1790m,宽度为50m,林线为急变类型,位于海拔2000m。宽度为40m．     

生态交错带的定量判定

生态过渡性是梯度环境的特征之一,过渡带的显著性是地理学和地植物学中长期争论的重要问题,生态交错带位置和宽度的判定是定量研究交错带生态学过程的基础。样带法是采集非连续梯度数据和研究交错带的结构,功能和格局梯度变化的有效方法。生态交错带变化最为显著的特征是植被的变化,包括植物种类组成和植被结构的变化,植被生态学群落分析中的相异系数,β多样性,梯度分析和分类排序技术等已被证明是成熟可靠的方法。介绍两种交错带定量判定的有效方法。游动分割窗技术是通过滑动求取样带上样点间相异系数,通过相异系数变化曲线判定交错带的位置和宽度。分割窗技术提供了敏感地定位非连续梯度的客观且有效的方法,它不仅可用于环境梯度上的等距离样点取样,而且可用于非等距离梯度带多元变量的分析。植被的特征是对生态环境连续体的综合反应,植被在环境梯度上的排序参数提供了一种较好的交错带定量指标,样带植被数据特征参数的变异轮廓图能够反应植被沿样带的物种组成,结构和空间变化格局,可以反应植被沿环境梯度的β多样性和植物群落的梯度分化,植被变异侧面轮廓图的间断或不连续（突变）区间就是群落边界的位置。     

半干旱区湿地-干草原交错带边界判定及其变化

鉴于目前国内对于半干旱区及小尺度上湿地-干草原交错带边界界定的研究较少,利用交错带对其周围环境变化具有提前指示作用的原理,以宁夏盐池四儿滩湿地为例,首先探讨游动分割窗技术在半干旱区湿地-干草原交错带边界判定中的可行性,其次再对2006年—2010年湿地-干草原交错带的宽度和边界进行判定,通过交错带的宽度和边界变化并结合交错带内植被的变化情况,综合对整个湿地生态系统的健康状况和湿地退化进行研究。结果表明:研究的尺度大小以及交错带过渡性是否明显将决定适宜窗口宽度的大小,这点在选择最小适宜窗口宽度时体现更为显著;降雨量是决定该区交错带的位置与宽度的最主要因素,但降雨量并不是决定该区交错带内植被变化状况的最主要因素,交错带距湿地核心区的距离是影响交错带内物种丰富度指数变化的最主要因素;由于保护区的成立,四儿滩湿地在2006年—2007年间,交错带宽度变大,湿地状况转好,2008年—2010年,由于铁路建设,湿地遭到破坏,交错带萎缩,湿地出现退化现象。湿地-干草原交错带作为一个敏感地带,它的变化情况可以对整个湿地生态系统的变化情况作出一定的提前预示;在半干旱区湿地的健康评价和退化研究中,通过交错带的变化来反映整个湿地生态系统的健康情况是一种可行的思路和方法。     

边缘效应的空间尺度与测度

综述了边缘效应的空间尺度类型以及在不同尺度上的测度方法.基于大量的研究整合,认为边缘效应空间尺度的划分,可以根据空间尺度的不同以及边缘效应形成和维持因素,分为大中小3个尺度类型,即大尺度的生物群区交错带、中尺度的景观类型之间的生态交错带和小尺度的斑块(生态系统)之间的群落交错区.大尺度主要是以植被气候带为标志的生物群区间的边缘效应,这种地带性的交错区主要受大气环境条件的影响.中尺度类型主要包括城乡交错带、林草交错带、农牧交错带等类型,是不同生态系统要素的空间交接地带,在物质能量等相互流动的作用下变得更为复杂.小尺度水平上是指斑块之间的交错所形成的边缘效应,受小地形等微环境条件及生物非生物等因子的制约,研究主要集中在群落边缘、林窗边缘和林线交错带等方面.对边缘效应测度的定量化研究有助于更加深入理解边缘效应.在大尺度水平上,边缘效应测度的研究主要是应用数量生态学等方法,研究不同气候带之间界线的划分及其物种分布的梯度规律性.中尺度水平上应用景观生态学的3S技术等方法,侧重于研究交错带的动态变化趋势及位置宽度的判定.小尺度水平上通过对距离边缘的长度,各群落中种群的数量、结构、多样性等定量指标的测定来构建测度公式,从而对边缘效应的强度进行量化,并反映边缘对群落的正负效应.总体上看,主要集中于中小尺度上,未来应该强化大尺度边缘效应测度的研究.     

生态交错带宽度判定及其影响因子研究进展

生态交错带是相邻生态系统之间的过渡带,是生态系统结构和功能在时、空尺度上变化较快的区域,也是生物多样性丰富区、全球变化敏感区.生态交错带位置和宽度的判定是定量研究交错带生态过程的基础,对生物多样性保护、片断化森林生态系统的管理与恢复以及自然保护区的功能分区都具有重要意义.由于生态交错带本身的复杂性,在相当程度上依赖于尺度水平,并受到各种自然和人为因素的影响,以致于目前还缺乏公认的原理和方法定量研究生态交错带,对其位置、宽度判定和动态变化研究一直处于不断的探索中.在分析大量相关研究资料的基础上,文章对生态交错带宽度判定方法以及影响因子进行论述,并对生态交错带宽度判定的研究前景进行展望.     

植物群落类型和围栏封育对高山林线岷江冷杉幼苗成活的影响

林线树种幼苗的生长紧密关系着高山林线的形成。通过室内发芽实验测定了岷江冷杉种子萌发能力。2015年春,在川西巴郎山岷江冷杉林线之上的高山林线交错带,通过播种处理(播种和不播种),研究了不同植物群落类型(灌木和草地群落)和围栏处理(围栏和不围栏)对岷江冷杉幼苗成活率的影响,以期为进一步探讨高山林线形成机制提供科学参考。结果表明:(1)岷江冷杉室内发芽率31.4%,成活率随时间下降。(2)灌木群落的全年日平均空气温湿度显著高于草本群落,而两群落的全年日平均土壤温度无显著差异。(3)未播种样地没有发现岷江冷杉幼苗,说明林线交错带缺乏岷江冷杉种子。(4)与不围栏样地相比,围栏封育分别显著提高了岷江冷杉幼苗成活率2.0%(2015年)和2.2%(2016年);与灌木群落相比,草本群落中岷江冷杉幼苗成活率显著提高0.8%(2015年)和1.2%(2016年),说明灌木对林线交错带幼苗更新具有更强的竞争作用。围栏处理下,草本群落中岷江冷杉幼苗成活率显著高于灌木群落;不围栏处理下,草本群落中岷江冷杉幼苗成活率显著低于灌木群落,2017年在不围栏样地没有幼苗存活,说明动物干扰对林线交错带森林更新有阻碍作用。研究表明,高山林线交错带森林更新,受种子、植物竞争和动物干扰(例如,放牧)等多方面因素的共同影响,可以通过播种、植物剔除(去除竞争)和围栏等促进幼苗更新和成活。     

太白红杉群落交错带物种多样性的研究

应用样带法对太白红杉群落及其交错带进行调查,采用各群落维管植物的物种丰富度指数(S)、 Simpson物种多样性指数(D)、Shannon Weiner物种多样性指数(H′)、种间相遇机率(PIE)及Pielou均匀度 指数(Jsw和Jsi),分析了6条样带的群落结构和物种组成。结果显示在环境条件(土壤和地形)变化较小、层 次结构剧变的群落交错带中,边缘效应明显。而在环境条件较差(即空间波动大)的群落交错带中,边缘效应 不明显,甚至无边缘效应出现。可见,群落的边缘效应不仅受小气候影响,也受地形和土壤等因子的影响。     

高山林线交错带高山杜鹃的凋落物分解

凋落物分解是维持生态系统生产力、养分循环、土壤有机质形成的关键生态过程。高山林线交错带是陆地生态系统中对气候变化响应的敏感区域。季节变化和海拔梯度上的植被类型差异可能会影响该区域凋落物的分解,进而对高山生态系统的碳氮循环产生重要影响。采用凋落物分解袋的方法,研究了川西高山林线交错带优势种高山杜鹃(Rhododendron lapponicum)凋落叶在雪被期和生长季的分解特征。结果显示:(1)季节变化和植被类型对高山杜鹃凋落物的分解均具有显著影响(P0.05),凋落叶的质量损失主要发生在生长季且在高山林线最大,暗针叶林中雪被期的质量损失略高于生长季,但差异不显著;(2)林线交错带上高山杜鹃凋落叶分解缓慢,一年干物质失重率为9.62%,拟合分解系数k为0.145;(3)高山杜鹃凋落叶的质量变化主要体现在纤维素降解显著且集中在雪被期,木质素无明显降解,在高山林线上C/N、C/P、木质素/N变化幅度较小且C、N、P的释放表现得稳定而持续。结果表明,季节性雪被对林线交错带内高山杜鹃分解的影响不仅局限在雪被期内,雪被融化期间频繁的冻融作用和雪融水淋洗作用可能会促进高山杜鹃凋落物在生长季初期的分解。总的来看,在气候变暖的情景下,雪被的缩减、生长季的延长和高山杜鹃群落的扩张可能加速高山林线交错带高山杜鹃凋落物的分解。     

林线更新关键影响因子研究进展

林线作为森林上限连接树种线的特殊生态过渡带,能够迅速地对气候变化做出反应,是理想的气候变化生态监测器。在全球变暖影响下,全球林线位置表现为一半上升,其余则保持相对稳定的趋势。林线能否上升取决于种子生产、向上扩散的能力及幼苗建成。大多学者从温度、降水、光照与干扰等方面分析林线更新及动态机制,主要认为低温限制林线上升,然而单一因素很难解释全球林线变化。国内外研究多关注于非生物因子对林线分布的作用机制,缺乏林线群落交错区基于种子扩散者等生物因子与幼苗定居,特别是林线交错带中种子扩散者对林线变化的作用。未来的研究可关注全球气候变暖下的林线幼苗幼树分布,如林线群落区分散贮食动物种子贮藏行为对林线幼苗更新的影响,为从种子扩散者与林线动态互作角度探究生物对气候变暖的响应提供科学依据。     

Estimating the ecotone width in patchy ecotones using a sigmoid wave approach

Ecotones are zones of transition between two adjacent ecological systems and are characterized by a high rate of change compared to these adjacent areas. They are dynamic entities with both a spatial and temporal property, reflected in an ecotone width and location, which vary across time during succession or environmental change on both a local or global scale. Various techniques have been proposed to characterize ecotones, one of them being a sigmoid wave curve fit on the transects across the ecotone. In this paper, we test the robustness of a sigmoid wave model approach on simulated ecotone data with a varying degree of steepness, patchiness and transect length. An analysis of variance (ANOVA) provided us details on the sensitivity of the estimated ecotone width for the steepness, the transect length as well as for the patchiness of the ecotone. The statistics also allowed us to investigate the interaction between the different parameters on the resulting ecotone width. We conclude that the sigmoid wave curve-fitting algorithm provides a robust way to describe ecotones with various degrees of steepness and patchiness. Depending on the transect window size used, a sigmoid wave curve-fitting algorithm will pick up variations in ecotone steepness or in ecotone steepness and patchiness.     

Statistical Efficiency in Distance Sampling

Distance sampling is a technique for estimating the abundance of animals or other objects in a region, allowing for imperfect detection. This paper evaluates the statistical efficiency of the method when its assumptions are met, both theoretically and by simulation. The theoretical component of the paper is a derivation of the asymptotic variance penalty for the distance sampling estimator arising from uncertainty about the unknown detection parameters. This asymptotic penalty factor is tabulated for several detection functions. It is typically at least 2 but can be much higher, particularly for steeply declining detection rates. The asymptotic result relies on a model which makes the strong assumption that objects are uniformly distributed across the region. The simulation study relaxes this assumption by incorporating over-dispersion when generating object locations. Distance sampling and strip transect estimators are calculated for simulated data, for a variety of overdispersion factors, detection functions, sample sizes and strip widths. The simulation results confirm the theoretical asymptotic penalty in the non-overdispersed case. For a more realistic overdispersion factor of 2, distance sampling estimation outperforms strip transect estimation when a half-normal distance function is correctly assumed, confirming previous literature. When the hazard rate model is correctly assumed, strip transect estimators have lower mean squared error than the usual distance sampling estimator when the strip width is close enough to its optimal value (± 75% when there are 100 detections; ± 50% when there are 200 detections). Whether the ecologist can set the strip width sufficiently accurately will depend on the circumstances of each particular study.     

华北农牧交错带农田-草地界面土壤水分影响域分析

在华北农牧交错区,选择线状边界的农田与草地典型区进行调查与土壤水分测定,采用移动窗口法,对农田-草地景观界面表层（0～20 cm）土壤水分影响域进行研究.结果表明：界面水分的影响域为草地6 m到农田4 m,总宽度10 m,属急变型界面;将农田-草地景观界面划分为3个功能区：农田功能区、草地功能区和农田-草地复合功能区.其中农田-草地复合功能区的土壤含水量变化剧烈,而草地功能区与农田功能区内土壤水分基本呈线性分布;草地生态系统土壤平均含水量比农田高约1 g·g^-1,这主要是由于草地开垦为农田后风蚀等作用而引起的土壤毛管持水力下降所致.作为植被覆盖不同的两个生态系统,不同的植物蒸腾和地表蒸发,可使不同功能区的土壤含水量产生明显差异,从而使土壤水势发生变化,使水分跨生态系统运移成为可能.     

岷江上游花椒地/林地边界土壤水分影响域的定量判定

在岷江上游干旱河谷区,选取典型的花椒地/林地边界,利用TDR仪测定干旱条件下、雨后和每月0～15 cm土层水分含量,并用移动窗口法判定土壤水分的边界影响域.结果表明,若用移动窗口法对土壤水分的边界影响域进行判定,当窗口宽度为8～12时,边界影响域较易判定.年内土壤水分随时间变化而变化.这种变化可分为土壤水分上升期、高峰期和消退期3个时期.干旱条件下土壤水分的边界影响域较小,其宽度约从花椒地6 m到林地2 m;雨后土壤水分的边界影响域有较大增加,其宽度约从花椒地12 m到林地2 m;年内土壤水分的边界影响域宽度约从花椒地10 m到林地2 m之间变化.不同季节土壤水分的边界影响域不同,并随着季节的变化呈动态变化.从生态学意义上讲,岷江上游地区目前进行的将花椒地退耕成林地、栽植树苗的措施是不可取的,该区退耕还林的最好方法应该是退耕,使其灌木林或草本植物自然生长.     

Correspondence of vegetation boundaries to redox barriers in a Northern European moraine plain

Little attention has been devoted to the investigation of the formation and functioning of ecotones at the interfaces between the upland and riparian zones. The margins of riparian mires act as redox geochemical barriers. Such biogeochemical hot spots retain elements that have leached from upland soils, favouring the growth of mesomorphic plants in hydromorphic soils. This paper aims to clarify the correspondence of vegetation borders to horizontal redox barriers of a Northern European moraine plain in Estonia.24 random transects were surveyed on the moraine plain, sampled across sharp soil moisture boundaries as proxies of redox barriers. The shifts in vegetation perpendicular to the boundaries were investigated. Curves of Euclidean distance were computed by moving a 20 m split-window along transects. The curves showed peaks of high dissimilarity a few metres below the redox barriers in the sites of natural soil moisture. In artificially drained sites, the relict redox barriers poorly corresponded to the vegetation borders. We conclude that in the studied moraine plain, the vegetation boundaries between riparian mires and uplands correspond to the redox barriers. The same can be set as a hypothesis for Northern European moraine plains. Related ecotones can be observed on the footslopes, revealing redox barrier in the landscape and related hot spots in cultural landscapes. In field margins, the redox barriers and corresponding ecotones occur below cultivation terraces. The ecotones may represent functional boundaries for delineating wetlands. Man-made drainage removes soil redox barriers and corresponding vegetation boundaries, making the landscape uniform and therefore vulnerable to disturbances. As a management implication, footslope ecotones should be preserved in their natural condition.     

A study on the community analysis using three-factorial data (time x site x species)

1. This study is to demonstrate that the analysis of biological communities using scaling unstandardized squared Euclidean distance is extremely effective to deal with data which are quite generally collected by 3 factors (time x site x species).
2. The main part of this study has been explained in detail byWilliams andStephenson (1973). We have conducted some discussion introducing mathematic complementary explanation as well as expansive interpretation.
3. The dissimilarity measure based on squared Euclidean distance is used to classify clusters from a dendrogram obtained by cluster analysis. The outline of the community structure can be known by comparing the values of mean variance per comparison and interaction.
4. The table of mutual comparison among clusters introduces dynamic pattern expression for community. Contributions by species to time and site are capable of expressing a concrete role of the species.
5. We apply the technique above to the demersal fish community in Shijiki Bay, Hirado Island, Nagasaki Pref. Number of individuals caught with Gochi trawls at 11 fixed stations in 1975–1984 are used as material for analysis. 84 species is accounted.

     

群体遗传学研究中的数据处理方法I．RAPD数据的AMOVA分析

近年来,RAPD数据和AMOVA分析广泛地应用于群体遗传学和保护遗传学研究。然而,由于RAPD标记具显性特点。加上目前进行AMOVA分析所依赖的RAPDistance软件不完善,使得对RAPD数据进行AMOVA分析时存在许多不足。本文介绍了AMOVA分析的基本过程,同时引入一个新的程序DCFA用以替代RADistance并详述了将DCFA与WINAMOVA联用,对RAPD数据进行AMOVA分析的具体步骤与注意事项,最后,以产自中国和巴西8个普通野生稻（Oryza furipogon)天然群体为例,演示了对RAPD表型数据进行AMOVA分析的过程,讨论了AMOVA分析结果在群体遗传结构上的意义。通过对AMOVA算法的分析,同时比较4种距离系数所得AMOVA结果,我们认为在进行AMOVA分析时选择NEI－LI距离和欧氏距离平方较为合适,而目前国内使用较多的JACCARD系数不适合AMOVA分析。     

Relationship between 17 Venezuelan counties estimated through communality of surnames

The coefficients of relationship and the Euclidean distances between 17 Venezuelan counties were estimated based on the frequency distribution of surnames obtained from the 1984 Venezuelan register of electors. In general, the coefficients of relationship between counties within the same state were higher than those between counties from different states. Euclidean distances exhibited the opposite relationship. Spearman's correlation coefficients for 136 pairs of counties were estimated between geographic and Euclidean distances (r = 0.41), geographic distance and coefficient of relationship (r = -0.44) and between Euclidean distance and coefficient of relationship (r = -0.48). The effect of partial geographic isolation on the frequency distribution of surnames is shown in the State of Falcón, where an isthmus separates two counties of the peninsula from two others on the mainland, and in Mérida, where the Venezuelan Andes separates three counties from the rest of the country. Our results suggest that Euclidean distances are less influenced by common surnames than the coefficients of relationship. They also indicate that in Venezuela a high proportion of the population has remained sedentary until recently, and this gives rise to the focal distribution of some surnames.