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Journal of Integrative Plant Biology 2008, 50 (2): 147–156 Pathways and Determinants of Early Spontaneous Vegetation Succession in Degraded Lowland of South China Wen-Jun Duan 1,2 , Hai Ren 1 , Sheng-Lei Fu 1 , Qin-Feng Guo 3 and Jun Wang 1,2 ( 1 Heshan Hilly Land Interdisciplinary Experimental Station, South China Botanical Garden, the Chinese Academy of Sciences, Guangzhou 510650, China; 2 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China; 3 USDA – Southern Research Station, Asheville, NC 28804, USA) Abstract Continuous and prolonged human disturbances have caused severe degradation of a large portion of lowland in South China, and how to restore such degraded ecosystems becomes an increasing concern. The process and mechanisms of spontaneous succession, which plays an important role in vegetation restoration, have not been adequately examined. To identify the pathways of early spontaneous vegetation succession, 41 plots representing plant communities abandoned over different times were established and investigated. The communities and indicator species of the vegetation were classified by analyzing the important values of plant species using multivariate analyses. The results indicated that the plant species could be classified into nine plant communities representing six succession stages. The pathway and species composition also changed in the process of succession. We also measured 13 environmental variables of microtopography, soil structure and soil nutrition in each plot to examine the driving forces of succession and the vegetation-environment relationships. Our results showed that the environmental variables changed in diverse directions, and that soil bulk density, soil water capacity and soil acidity were the most important factors. Key words: degraded lowland; ecological restoration; soil; spontaneous succession. Duan WJ, Ren H, Fu SL, Guo QF, Wang J (2008). Pathways and determinants of early spontaneous vegetation succession in degraded lowland of South China. J. Integr. Plant Biol. 50(2), 147–156. Available online at www.jipb.net Ecological restoration is intended to initiate or accelerate the recovery of an ecosystem in terms of its health, integrity and sustainability (SER 2004). Restoration is often closely related to the reconstruction of the structure, biological interactions, and related processes of the ecosystem (Hobbs and Norton 1996; Reay and Norton 1999; Ren and Peng 2001; Ren Received 12 Sept. 2006 Accepted 20 Mar. 2007 Supported by the National Natural Science Foundation of China (No. 30200035) and Field Station Project of the Chinese Academy of Sciences (CAS) to Heshan Hilly Land Interdisciplinary Field Station, CAS Author for correspondence. Tel: +86 (0)20 3725 2916; Fax: +86 (0)20 3725 2916; E-mail :<[email protected]>. C 2008 Institute of Botany, the Chinese Academy of Sciences doi: 10.1111/j.1744-7909.2007.00603.x et al. 2004). The traditional approach to reclaiming degraded lowland in South China has been to plant fast-growing trees to minimize financial and human resource expenditures (Yu and Peng 1996). Plantations can achieve short-term socioe- conomic goals by protecting the soil surface from erosion, by facilitating native species, and by accelerating the recovery of genetic diversity. However, spontaneous vegetation succession or natural recovery as an alternative approach to restoration has gained increasing attention (Bradshaw 1997; Pensa et al. 2004). Plant community succession is becoming one of the important aspects of restoration ecology and is the subject of a large body of ecological research (Zhang 2005). Most studies on terrestrial vegetation succession have been focused on the restoration of abandoned mine land (Pensa et al. 2004; Martinez and Fernandez 2005; Dutta and Agrawal 2005), degraded grassland (Callaway and Davis 1993; Scholes and Archer 1997; Peintinger and Bergamini 2006; Bornkamm 2006), and forest land after deforestation or fire disturbance

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Page 1: Pathways and Determinants of Early Spontaneous Vegetation Succession in Degraded Lowland of South China

Journal of Integrative Plant Biology 2008, 50 (2): 147–156

Pathways and Determinants of Early SpontaneousVegetation Succession in Degraded Lowland

of South China

Wen-Jun Duan1,2, Hai Ren1∗, Sheng-Lei Fu1, Qin-Feng Guo3 and Jun Wang1,2

(1Heshan Hilly Land Interdisciplinary Experimental Station, South China Botanical Garden,

the Chinese Academy of Sciences, Guangzhou 510650, China;2Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;

3USDA – Southern Research Station, Asheville, NC 28804, USA)

Abstract

Continuous and prolonged human disturbances have caused severe degradation of a large portion of lowland in SouthChina, and how to restore such degraded ecosystems becomes an increasing concern. The process and mechanisms ofspontaneous succession, which plays an important role in vegetation restoration, have not been adequately examined. Toidentify the pathways of early spontaneous vegetation succession, 41 plots representing plant communities abandonedover different times were established and investigated. The communities and indicator species of the vegetation wereclassified by analyzing the important values of plant species using multivariate analyses. The results indicated that theplant species could be classified into nine plant communities representing six succession stages. The pathway and speciescomposition also changed in the process of succession. We also measured 13 environmental variables of microtopography,soil structure and soil nutrition in each plot to examine the driving forces of succession and the vegetation-environmentrelationships. Our results showed that the environmental variables changed in diverse directions, and that soil bulk density,soil water capacity and soil acidity were the most important factors.

Key words: degraded lowland; ecological restoration; soil; spontaneous succession.

Duan WJ, Ren H, Fu SL, Guo QF, Wang J (2008). Pathways and determinants of early spontaneous vegetation succession in degraded lowland ofSouth China. J. Integr. Plant Biol. 50(2), 147–156.

Available online at www.jipb.net

Ecological restoration is intended to initiate or accelerate therecovery of an ecosystem in terms of its health, integrity andsustainability (SER 2004). Restoration is often closely relatedto the reconstruction of the structure, biological interactions,and related processes of the ecosystem (Hobbs and Norton1996; Reay and Norton 1999; Ren and Peng 2001; Ren

Received 12 Sept. 2006 Accepted 20 Mar. 2007

Supported by the National Natural Science Foundation of China (No.

30200035) and Field Station Project of the Chinese Academy of Sciences

(CAS) to Heshan Hilly Land Interdisciplinary Field Station, CAS∗Author for correspondence.

Tel: +86 (0)20 3725 2916;

Fax: +86 (0)20 3725 2916;

E-mail :<[email protected]>.

C© 2008 Institute of Botany, the Chinese Academy of Sciences

doi: 10.1111/j.1744-7909.2007.00603.x

et al. 2004). The traditional approach to reclaiming degradedlowland in South China has been to plant fast-growing treesto minimize financial and human resource expenditures (Yuand Peng 1996). Plantations can achieve short-term socioe-conomic goals by protecting the soil surface from erosion, byfacilitating native species, and by accelerating the recovery ofgenetic diversity. However, spontaneous vegetation successionor natural recovery as an alternative approach to restoration hasgained increasing attention (Bradshaw 1997; Pensa et al. 2004).Plant community succession is becoming one of the importantaspects of restoration ecology and is the subject of a large bodyof ecological research (Zhang 2005).

Most studies on terrestrial vegetation succession have beenfocused on the restoration of abandoned mine land (Pensaet al. 2004; Martinez and Fernandez 2005; Dutta and Agrawal2005), degraded grassland (Callaway and Davis 1993; Scholesand Archer 1997; Peintinger and Bergamini 2006; Bornkamm2006), and forest land after deforestation or fire disturbance

Page 2: Pathways and Determinants of Early Spontaneous Vegetation Succession in Degraded Lowland of South China

148 Journal of Integrative Plant Biology Vol. 50 No. 2 2008

(Turner 1997; Calvo 2005; Hooper et al. 2005; Shimizu 2005;Choung and Hong 2006; Karlowski 2006). However, the path-ways and determining factors of vegetation succession in de-graded lowland are unclear, and little information is available.

Environmental degradation is especially serious in China.It is estimated that the total area under soil erosion is about3.56 × 106 km2, accounting for 37.1% of national land (SEPA2006). As a traditional approach, plantations may sometimesquickly increase forest coverage and rehabilitate degradedecosystems. Most previous studies of ecological restorationfocused on the selection of pioneer species and the develop-ment of engineering technology. However, few studies haveexamined the feasibility of restoration through spontaneousvegetation succession (Zhang 1994; Ren and Peng 2001; Peng2003). With rapid economic development, many farmers areabandoning their agricultural fields and shifting to manufactur-ing. Consequently, many croplands are left untended. More-over, large forestlands are degraded into grasslands becauseof intensive logging and poor management. In South China,Zhang (1994) found more than 3.74 × 106 ha of lowlands weredegraded. In order to increase forest coverage and mitigatesoil erosion, the national and local governments have devotedconsiderable amounts of human and financial resources toextend plantations. Fast growing species such as eucalypts(Eucalyptus citriodora, E. exserta, E. robusta) and pines (Pinuselliotii, Pinus massoniana) or nitrogen fixing species such asAcacia auriculaeformis have been widely used as pioneerspecies. However, negative effects, such as biodiversity loss,soil nutrient depletion (Madeira 1989), and soil acidification alsooccur but are largely overlooked. To avoid these problems, wemust understand the processes and mechanisms of vegetationsuccession in degraded lowlands of South China.

The major objective of this study is to identify the pathwaysand mechanisms of vegetation succession associated withrestoration processes in South China. Specifically, we addressthe following issues: (1) What are the early succession seriesof plant communities in South China? (2) Which environmentalfactors are the key “filters” to determine the vegetation compo-sition and structure in succession; and (3) What are the mosteffective approaches to accelerate vegetation succession andto reach the “futuristic” restoration goal?

Results

Classification of succession stages

Based on TWINSPAN analysis, 60 species were classified into9 groups, representing 6 succession stages (Figure 1).

Stage I (0–3 years after abandonment): This stage was theprimary period of recovery. The plant coverage waslow (10%) and the community composition was very

Stage II

II-I

II-II

Stage I

Stage I Stage III

III-I

III-II

Stage IV

IV-I

IV-II

Stage V

Stage VI

Figure 1. The restoration model of plant communities in degraded

lowlands in South China.

simple. Plant species were few (less than 5) and mainlycomprised decumbent and profuse root system species.

Stage II (3–5 years): This stage included two different com-munity types (II-I: Imperata cylindrica and II-II: Ly-copodium cernuum). Most of the plant species weregramineous species, which could tolerate the droughtand infertile soils. Some leguminous species also ap-peared.

Stage III (5–12 years): This stage had two different com-munity types (III-I: Glochidion eriocarpum plus Panaxstipuleanatus, and III-II: Neyraudia neyraudiana plusMiscanthus sinensis). Most of the species were annualherbs. Many shrub species also appeared in the com-munities. The vegetation was generally dwarfed. Thiswas the transition stage when many grass species weregradually replaced by shrub species.

Stage IV (12–17 years): This stage can be divided into twocommunity types: IV-I: Eurya chinensis plus Rhaphi-olepis indica. At the beginning of this stage, the dom-inant species was Dicranopteris linearis. Some shrubspecies such as Gardenia sootepensis and Rhaphi-olepis indica were scattered in the community. How-ever, at the end of this stage, the community struc-ture changed dramatically and some shrub species,such as Sychotria rubra, Eurya chinensis, and Lit-sea rotundifolia oblongifolia colonized the community.IV-II: Litsea cubeba plus Litsea glutinosa. In contrastto IV-I, some gramineous species also appeared in thiscommunity. At the end of this stage, many broad-leavedspecies emerged.

Stage V (17–23 years): The dominance of shrubs overgrasses became evident and many herbaceous speciesdisappeared. Moreover, the coverage of vegetationgreatly increased (about 80%).

Stage VI (23–30 years): The total vegetation cover reached95%, and the herb species were highly restricted; theircoverage was less than 20% as a result of the limitedlight. Both tree and shrub species were dominant. Thecommunity structure of this stage was relatively steady

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Pathways and Determinants of Vegetation Early Succession 149

Figure 2. De-trended correspondence analysis ordination of the 60 species at six successional stages. The S + Arabic numbers and P + Arabic

numbers represent species and quadrats, respectively.

and could resist some extent of disturbance, resemblinga “climax” community under natural conditions.

TWINSPAN analyses showed that, on the same substrate,there was a combination-separation-combination process ofvegetation succession in degraded lowland, indicating two par-allel paths in stages II, III, and IV, which finally combined instage V (Figure 1).

Ordination analysis of succession

In the two-dimensional de-trended correspondence analysis(DCA) scatter diagram (Figure 2), axis1 most likely representsthe time course. From right to left, the succession periods be-come longer and the community composition and structure varygreatly. In stages I and II, there are few species and most of themrarely appear in the adjacent areas; the community boundaryis clear. However, from stages III to IV, with the improvementof environment, species number increases. Accordingly, thecommunity boundary becomes unclear. This is also embodiedin the diagrams. Compared with stages I and II, the shapes of

stages III, IV, and V are abnormal. Moreover, there are manytransitional species which are distributed in the middle positionof these three stages. In the end, an obvious change of plantdiversity is observed in Figure 2. From stage I to stage VI, therewas an increasing-decreasing process in the plant diversity.

Figure 2 shows plots of the same succession stages withsimilar ordination scores. When compared with Figure 3, wefound the quadrats at the same stages had similar positionsin both diagrams. This indicates that the environmental factorsof the community change significantly from one stage to thenext, and the species composition varies with the environmentalchanges.

Changes of species number and composition

During succession, the number of species and the speciescomposition changed over time (Figure 5). During the earlysuccession stages of vegetation restoration, the fluctuationof species number was obvious. During all six successionstages, the species number in different life forms changed

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150 Journal of Integrative Plant Biology Vol. 50 No. 2 2008

Figure 3. De-trended correspondence analysis ordination of the 41 quadrats in six succession stages based on species composition.

in different ways. Overall, the temporal pattern of herb andshrub species was parallel to that of total species number.However, the change of shrubs lagged behind that of herbs.In stages V and IV, the herbs decreased rapidly, but shrubswere still increasing. The species number of lianes changedrandomly at all six succession stages, probably because thelianes could better adapt to the environment, and the speciesnumber was small. The tree species increased in the last threestages.

In general, pioneer species at the study site were heliophyteswhich could endure drought and lean times. During the first twostages, pioneer species dominated the community. However,as succession progressed, the microenvironment amelioratedand the proportion of pioneer species decreased. This trendwas more obvious in the last two stages. In these two stages,trees and tall shrubs dominated the communities, while manyheliophytes, especially herbs and shrubs, were shaded outand a few mesophytes and shade-tolerant species colonizedthe understorey. In the first two stages, most species had largenumbers of small seeds mainly dispersed by wind. In the latestages, however, more species had larger seeds that weremainly dispersed by animals.

Changes of environmental factors

There was a steady reduction of soil bulk density (SBD) duringthe six succession stages, suggesting that the soil structureimproved during the succession process. Moreover, this wasmore obvious in the first four stages because the vegetationcover increased dramatically in these stages and played animportant role in water and soil conservation. The changingpattern of soil saturation moisture (SSM) and soil capillarymoisture (SCM) was completely opposite to that of SBD. Thisindicates that changing SBD played an important role in theincrease of soil moisture. The pH decreased slowly during thesuccession, possibly because the acidity of the laterite substratewas relatively high. At the beginning of succession, surface soilwas eroded and the soil substrate became exposed becauseof low vegetation cover. The pH would decrease as a resultof the effects of the ensuing pedogenic process. Soil organicmatter greatly increased during succession, especially in thelate stages, probably as a result of the increase of plant biomassand litter. In the first three stages, there was little hydrolyzednitrogen accumulated in the soil, but this situation changedat the late stages. Available phosphorus and exchangeablepotassium in the soil showed an increase at the beginning and

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Pathways and Determinants of Vegetation Early Succession 151

Figure 4. De-trended correspondence analysis ordination of the 41

quadrats in six successional stages based on their environmental

conditions.

a decrease later during the succession, which possibly resultedfrom complex interactions between the changes in pH and soilorganic matter along the successional process (Figure 7).

Analysis of determining environmental factors

The length of lines in the canonical correspondence analysis(CCA) ordination diagram indicates the strength of the corre-lation between plant communities and the environment, andthe angle between two lines represents their relativity. Figure 8shows that SBD, soil moisture, nitrogen, and pH were the mostimportant factors in vegetation restoration. The soil of our siteswas acidic laterite, with a pH ranging from 3.6 to 5. Soil pHcan affect vegetation succession in several ways. First, it couldfilter out certain species and thus change the community com-position. Second, many essential elements such as phosphous,calcium and magnesium are affected. For example, Figures 8shows that these elements were positively correlated with pH,suggesting that pH could also affect vegetation restoration byrestricting the availability of some soil elements. Third, pH canaffect the quantity and activity of soil microorganisms whichplay important roles in vegetation succession. The two CCAordination diagrams also indicate that SBD and soil moisture

are two important factors. At the beginning of the succession,the soil was poor with high SBD and low organic matter content.Accordingly, the soil water holding capacity was low, leadingto greater soil erosion. The diagrams also show that SCM andSSM are negatively related to SBD, indicating that the improvingsoil structure was favorable for vegetation restoration. At thesame time, slope and aspect of a catchment could affect thespatial–temporal distribution of water and heat. Generally, soilerosion was more serious in steep lowland. The accumulationof soil organic matter and minerals was relatively low in theseareas, and this effect was more pronounced in monsoon areas.Nitrogen and soil organic matter were easily decomposed andrelatively little was accumulated in the soil because of the hightemperature and intense drying-rewetting process. However,at the later stages, the microenvironment was improved; theaccumulation of soil organic matter and minerals increased.Therefore nitrogen and soil organic matter became more im-portant in late succession.

Discussion

Factors controlling vegetation succession

Vegetation succession and ecological restoration representprocesses in community assembly that involve a series of filtersand thresholds sifting species out of the regional pool (Dı́azet al. 1998; Whisenant 1999; Temperton et al. 2004). It hasbeen recognized that the importance and action of differentfilters will vary from place to place and over time throughrestoration (Woodward and Diament 1991; Temperton et al.2004). In extremely degraded sites, environmental stresses actas abiotic filters and only some pioneer species may be ableto tolerate the severe conditions. South China is in the lowersubtropical monsoon region. The annual precipitation is about1 700 mm and the rainfall is generally intense, causing surfacerunoff which usually peels off the fertile topsoil, especially in hillyland. Consequently, the soil becomes extremely lean, acidicand compact, and thus functions as an abiotic filter. In theseseverely degraded areas, some pioneer gramineous speciesthat have extensive root systems can tolerate strong acidityand drought. As pioneer species, these species can reducesurface runoff, accumulate soil organic matter, and improve soilstructure, thus acting as nurse plants to facilitate the colonizationof later species. They are also keystone species in transitionof the threshold controlled by abiotic limitations. In the firstfour stages, abiotic filters determined the fate of vegetationrestoration and the species composition was very simple, thevegetation cover was low, and thus the competition was weak.However, as succession progressed, the substrate improved,more species emerged, and plant cover increased; therefore,competition became stronger. For example, in late succession,many species were shaded out and the total species richness

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152 Journal of Integrative Plant Biology Vol. 50 No. 2 2008

Figure 5. Changes of species number of different life forms during the six successional stages.

Figure 6. Changes of species composition during the six successional stages.

declined. In general, the importance of biotic filters increasesalong with succession.

There are also five different kinds of plantations in the studysite, which are 23 years old. The understorey vegetation wascompared with 23 years of natural restoration. Most heliophytessuch as Rhodomyrtus tomentosa and Baeckea frutescens werescanty under all plantations. However, shade-tolerant speciessuch as Psychotria rubra and Circaea mollis became the mostimportant components of the understorey community. Thisindicated the importance of light in late succession. Whenthe forest canopy closed, understorey vegetation would shiftfrom heliophytes to mesophytes and shade-tolerant species.A common observation in both plantations and grassland wasthat few native tree saplings were established. Comparison

of microclimate, soil minerals, and soil structure with those ofnative forest showed that these environmental factors may beless important, because native saplings can survive in nativeforests with harsh environments (Peng 2003). Seed sourcesand seed dispersal may be the most important biotic factors inlate succession. Few seeds of native species were found duringour vegetation and seed bank survey. In general, the specieshave large numbers of small seeds at the early stages and mostof these seeds can be dispersed by wind for great distances,with little dispersal barrier. However, most of the native treespecies such as Castanopsis chinensis, Cryptocarya chinensis,Aporosa yunnanensis, and C. fissa have larger seeds and onlyappear in late stages. If the distance between the native forestsand degraded land is large, seed dispersal of heavy seeds is

Page 7: Pathways and Determinants of Early Spontaneous Vegetation Succession in Degraded Lowland of South China

Pathways and Determinants of Vegetation Early Succession 153

0.0

0.5

1.0

1.5

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III-

II II-I

III-II

III-I

IV-II IV

-I V VI

Succession stages

En

viro

nm

enta

l fac

tor

valu

epHSOMSBDSSMSCMNPK

Figure 7. Changes of dominant environmental factors along the six successional stages. pH (× 10); SOM, soil organic matter (× 10 g/kg); SBD,

soil bulk density (g/cm3); SSM, soil saturation moisture (× 100%); SCM, soil capillary moisture (× 100%); N, hydrolyzed nitrogen (× 103 mg/kg); P,

available phosphorus (mg/kg); K, exchanged potassium (× 102 mg/kg).

s1

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s5s58 s6s11s18

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Axis 2

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SSM N

P

SCM

ORG

Figure 8. Canonical correspondence analysis ordination diagram of the 60 species and 13 environmental factors from 41 quadrats.

more difficult. Dispersal barrier may be the most important bioticfilter in the late succession stages.

It is always difficult to comprehensively analyze many en-vironmental factors in a single study. Here we identified andanalyzed 13 environmental factors, and concluded that pH,

SBD and soil moisture were the most important environmentalfactors in vegetation restoration in the study area. However,soil organic matter and nitrogen were considered to be thedominant environmental factors in many previous studies. Thisdifference could be due to the mineralization of nitrogen, and

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154 Journal of Integrative Plant Biology Vol. 50 No. 2 2008

the comparatively faster decomposition of organic matter atour study site. In addition, some essential minerals were sweptaway by surface runoff from the heavy rainfall in the region.Consequently, the nitrogen and organic matter content weresimilar in the first four stages and could not be the limitingfactors. However, the soils of our study sites are acidic and theavailability of phosphorus, potassium, calcium, and magnesiumwere closely correlated with pH. Therefore, soil acidity could bea determinant of vegetation succession. Although the lateritesoil has strong capillary attraction and is difficult for rain water toinfiltrate, the evaporation is high and precipitation varies greatlybetween seasons. Thus, soil moisture is also an importantfactor affecting vegetation succession. It should be pointedout, however, that these observations may only apply to earlysuccession stages and the situation may be different in latersuccession stages.

The community assembly models

There are three models of community assembly, deterministic,stochastic, and alternative stable states (ASS). Most ecologiststend to agree that the ASS model of species assembly is likelyto be the one that better reflects reality in nature (Tempertonet al. 2004). This model asserts that communities are structuredand restricted to a certain extent, but can be developed intonumerous states because an element of randomness can beinherent in all ecosystems (Sutherland 1974; Gleick 1987). Inour study, the vegetation succession did not follow one fixedpathway; instead, it was diverted into two parallel directionsduring early stages which then incorporated in the late stages.This conclusion is different from early studies of spontaneoussuccession (Scholes and Archer 1997; Calvo 2005; Bornkamm2006; Karlowski 2006), but seems to support the ASS theory.

Many factors can result in the formation of different commu-nities and succession pathways. Soil seed banks vary greatlyacross space partly due to their different distances from seedsources; therefore, seed dispersers can affect the colonizationof certain species. Consequently, the sequences of speciessettlement can be quite different. For example, early settledspecies always affect the colonization of latter species. Inaddition, different environmental conditions gave rise to differentcommunities in sites with identical species pools, as clearlyillustrated at stage IV (Figures 4–7). At this stage, plots withbetter soil structure and high nitrogen content were mainlyoccupied by Dicranopteris linearis. The coverage was relativelyhigh. However, in plots with relatively poorer soil structure andnutrient condition, pioneer species such as Miscanthus sinensiswere abundant.

Conclusions

Our results clearly show that, in order to accelerate therestoration process, some immediate new strategies need to

be planned and adopted. On the one hand, a more flexiblerestoration plan should be in place. The climax communitiesmay be different because vegetation succession and ecologicalrestoration are determined by somewhat different and uncertainfactors. Moreover, because of the effect of microtopography,microclimate, and substrates, vegetation succession may bediverted into different trajectories, and various patterns canbe observed at the same succession stage. Therefore, estab-lishing self-sustaining ecosystems with abundant species andintegrated function should be the goal of restoration. On theother hand, different steps should be taken to accelerate thetransition past thresholds at different restoration stages. Thefirst step is to reduce water loss and soil erosion, as soil erosionis one of the most serious problems in South China. We willthen need to enhance soil pH and improve soil structure. Inlate stages of restoration, increasing the seed supply may behelpful to facilitate seed dispersal and sapling establishment(Guo 2007).

Materials and Methods

Study site

The study was conducted at Heshan Hilly Land InterdisciplinaryExperimental Station (112◦ 54′ E, 22◦ 41′ N) located in HeshanCounty, Guangdong, China. The station was established in1984 and it is located in a degraded coastal ecosystem incentral Guangdong with a typical subtropical monsoon climate.Its elevation varies from 0 to 90 m. The soil is laterite, a type ofheavy acid soil with little soil organic matter (about 18.03 g/kg),nitrogen (total N is about 0.86 g/kg) and available phospho-rus (1.33 mg/kg). The mean annual temperature is 21.7 ◦C,the mean rainfall is 1 700 mm, and the mean evaporation is1 600 mm. The region is a hilly agricultural zone with 78.6% ofhilly land, 17.1% of farming land, and 4.3% of water body. Thevegetation is typical subtropical evergreen broad-leaved forest.Representative species of climax communities are Cryptocaryaconcinna and C. chinensis. As a result of human disturbance,much of the current vegetation is degraded into hilly landgrassland.

Field and laboratory methodology

To study the composition and structure of various plant com-munities, quadrat samples were set up at different successionstages. Quadrats of 20 m × 20 m, 5 m × 5 m, and 1 m × 1 m wereused for investigating the vegetation of tree, shrub, and grassspecies, respectively. Three small quadrats for grassland orshrub land were nested in the large ones for shrub land and treeland. In each quadrat, the height, density, and basal diameterof various tree and shrub species, as well as the height and

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Pathways and Determinants of Vegetation Early Succession 155

Table 1. The species and codes recorded in sampling quadrats

Code Name Code Name

S1 Dicranopteris linearis S31 Smilax china

S2 Cynodon dactylon S32 Embelia laeta

S3 Imperata cylindrica S33 Microlepia hancei

S4 Circaea mollis S34 Lygodium japonicum

S5 Polygonum chinensis S35 Clerodendron fortunatum

S6 Melastoma dodecandrum S36 Psychotria rubra

S7 Miscanthus sinensis S37 Eurya chinensis

S8 Blechnum orientale S38 Melastoma candidum

S9 Rubus alceaefolius S39 Wikstroemia indica

S10 Paederia scandens S40 Rhaphiolepis indica

S11 Mussaenda pubescens S41 Ficus hirta

S12 Ischaemum indicum S42 Glochidion eriocarpum

S13 Lycopodium cernuum S43 Panax stipuleanatus

S14 Schizoloma heterophyllum S44 Mallotus apelta

S15 Adiantum capillus-veneris S45 Litsea cubeba

S16 Adiantum flabellulatum S46 Litsea rotundifolia

S17 Lophatherum gracile S47 Gardenia sootepensis

S18 Dianella ensifolia S48 Rhodomyrtus tomentosa

S19 Dianella ensifolia S49 Baeckea frutescens

S20 Neyraudia neyraudiana S50 Evodia lepta

S21 Fimbristylis dichotoma S51 Litsea glutinosa

S22 Abrus precatorius S52 Trema cannabina

S23 Desmodium triflorum S53 Schefflera octophylla

S24 Eupatorium catarium S54 Ilex asprella

S25 Panicum repens S55 Pinus massoniana

S26 Urena lobata S56 Breynia fruticosa

S27 Murdannia triquetra S57 Mimosa sepiaria

S28 Desmodium heterocarpon S58 Setaria viridis

S29 Hedyotis diffusa S59 Pseudosasa hindsii

S30 Cassytha filiformis S60 Ficus variolosa

coverage of different grass species were recorded. In orderto get accurate coverage of grasses, a 1 m × 1 m frame withsmall panes (5 cm × 5 cm) was used. The cover of grasseswas determined by counting the number of panes covered bygrasses. A total of 41 plots at different succession stages wereestablished and investigated.

Soil samples were randomly collected from five points ineach quadrat using a 5 cm-diameter soil corer to a depth of20 cm, after removing surface litter. A composite soil sampleof about 1 kg from each point was collected, air-dried andsieved for analysis of soil chemical characteristics (Instituteof Soil Science, CAS 1978; Liu et al. 1996). To measure thesoil physical characteristics, nine intact soil cores were takenrandomly in each quadrat using ring knives, after removing thelitter and humus layer, and three of them were used to determinethe SBD, soil saturate moisture, and soil capillary moisture,respectively.

Data analysis

A total of 60 species were recorded in the 41 plots (Table 1). Thespecies importance values (IV) in each sample were calculatedusing the following formula:

IVtree and shrub = (Relative density

+ Relative frequency + Relative dominance)/3

IVherb = (Relative coverage + Relative height)/2

Frequency refers to the percentage of the quadrat containinga tree species over the total quadrats at the same successionstage and stands. Dominance value refers to the sum of thebasal areas of a tree or shrub species within a quadrat. Wedeveloped a matrix of IVs of 60 species × 41 plots and used itas the basis of the succession analysis. First, we used two-wayindicator-species analysis (TWINSPAN; Hill 1979) to classify thesuccession stages of the communities. Second, we analyzedthe relationships between the succession stages by de-trendedcorrespondence analysis (DCA; Hill and Gauch 1980). Finally,the relationships between vegetation and environmental factorswere analyzed using canonical correspondence analysis (CCA;Braak 1986).

Acknowledgements

The authors are indebted to Dr Zhian Li, Jingping Zhang andZuoyun Yin for helpful suggestions. The authors thank Bi Zoufor soil analysis, Fuwu Xing for plant species identification, andYongbiao Lin for field assistance.

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(Handling editor: Jian-Xin Sun)