Study site
We compared a landscape PA and the SA of Mt. Cheonggye, located in the southern part of Seoul (37°23ʹ27.18ʺ–36°27ʹ33.79ʺN, 127°00ʹ12.81ʺ–127°20ʹ29.63ʺE) (Fig. 1). The ecosystem conservation areas outside the ecological landscape of the PA were designated as the SAs in this study, because the ecosystem conservation areas experience greater disturbance than the ecological landscape PA (Fig. 1). The summit height of Mt. Cheonggye is 618 m and its range links Uiwang, Gwacheon, and Seongnam City in the Gyeonggi Province with Yangjae-dong in Seoul. These areas are commonly known as “Jwacheong” (dragon ascending into heaven on the left) and “Ubaekh” (white tiger on the right) by Korean citizens, due to their role in safeguarding Seoul and the Gwanak Mountain. The summit of this mountain, called Cheonyong Mountain, includes an area called Manggyeongdae (altitude 618 m), with peaks named “Maebong” (hawk peak) and “Oknyeobong” (https://www.uiwang.go.kr/english/UWENGTOUR0101). The ridges of Mt. Cheonggye run from the south to the north and the connected summits of Mt. Cheonggye include Oknyeobong (374.7m), Maebong (492.7 m), Manggyeongdae (618 m), Jeolgogae (350 m), Uungbong (348.8 m), and Guksabong (540 m) (Lee and Ahn 1995). The primary plant biome of the mountain falls within the middle part of the cool temperate zone (Yim and Kira 1976).
Mt. Cheonggye is covered by thick forests and is visited by climbers seeking the enjoyment of forest therapy. Its 2-km-long valleys always have clean water flowing with lush forests alongside them, which attracts significant human activity. Wonter Valley in Mt. Cheonggye was designated an ecological landscape of the PA in 2004 by the Seoul city government (http://parks.seoul.go.kr/ecoinfo/ecology/index.do). Wonter Valley has an area of 146,281 m2. The climate parameters were obtained from data from the Mt. Gwanak climatological station which is close to the study site, the average parameters for the years 1981‒2010 were as follows: average temperature, 12.5°C; average annual highest temperature, 17.0°C; average annual lowest temperature, 8.6°C; and average annual precipitation, 1450.5 mm (http://data.kma.go.kr). Mt. Cheonggye is composed of mainly metamorphic rocks and partly of acidic rocks. The predominant soil order of Mt. Cheonggye is inceptisols (http://soil.rda.go.kr/geoweb/soilmain.do), and the soil texture of the PA is largely sandy loam and that of the SA is sandy loam and fine sandy loam.
Vegetation sampling
We sampled vegetation from both the PA and SA. We selected study locations based on maps delineating different vegetation types taken by aerial photographs as well as digital maps (scale, 1:25,000) provided by the National Institute of Ecology, Republic of Korea (http://www.nie.re.kr/contents/siteMain.do?mu_lang=ENG). The total numbers of study sites, quadrats in the PA and SA were 36 and 58, respectively (total: 94) (Fig. 1). We conducted quadrat sampling to determine the plant species composition, plant species cover, and dominance (covers of dominant plant species in the tree [T1], sub-tree [T2], shrub [S], and herb [H] layers) in each site and collected data on twelve environmental variables (altitude, direction, exotic, grade, H, hierarchy, rock, S, slope degree, species, T1, T2) in the PA and SA. “Exotic” indicates the presence of exotic species (presence: 1; absence: 0); “grade” means vegetation conservation grade (I, II, III, IV and V; assessed using distribution rarity, potentiality of vegetation restoration, integrity of species composition, integrity of vegetation structure, presence of important species, and diameter of planted trees at breast height); “hierarchy” refers to the layering of vegetation structure (four layers of tree, subtree, shrub and herbaceous species: 4; three layers of tree, shrub and herbaceous species: 3; two layers of tree and herbaceous species: 2; one layers of tree species: 1); “rock” refers to surface area of rocks relative to the sites (rock cover within quadrats: %); and “species” is the total number of species identified in each quadrat. Quadrats measuring 10 × 10 m were sufficiently large to include tree species in the canopy layers of the forests and selected randomly within the PA and SA. Plant species cover was quantified using the Braun–Blanquet scale (Braun–Blanquet 1932). The class numbers of the scale were transformed into mean values following the procedures outlined by Mueller–Dombois (1974).
The nomenclature and classification system used for the vascular plants followed was as described by Lee (1985) and Park (1995, 2001). Exotic species in this study were defined as introduced and established species deliberately or accidently across the Korean border from foreign habitats.
Species diversity indices
We calculated species diversity indices to compare community diversities across quadrats in the PA and SA, including richness, dominance, diversity, and evenness indices.
The existing index was estimated based on plot data that was randomly sampled in the study area. The species richness index represents the number of species in the plot.
Species dominance (D`) was calculated as: \(\text{D}`=\underset{i=1}{\overset{s}{?}}{\left(\frac{{n}_{i}}{n}\right)}^{2}\) and the Simpson index was defined as 1-D`. Shannon index (H`) was calculated as: \(\text{H}`= -\underset{i=1}{\overset{s}{?}}\frac{{n}_{i}}{n}ln\frac{{n}_{i}}{n}\). Where s equals the number of species and \(\frac{{n}_{i}}{n}\) is the relative cover of ith species (Whittaker 1972; Pielou 1975; Rad et al. 2009). The species evenness index (E) was calculated as:\({e}^{H`}/ s\)
The species richness, Simpson, Shannon, and evenness indices were calculated from data on plant species identified and their individual numbers within each quadrat in the PA and SA.
Ordination
To analyze the differences in vegetation structure between PA and SA and to identify significant correlations with environmental variables, we ordinated the samples using detrended canonical correspondence analysis (DCCA). The relative covers of herb (H) and woody species (T1, T2, and S) were ordinated in relation to twelve environmental variables (altitude, direction, exotic, grade, H, hierarchy, rock, S, slope degree, species, T1, T2). DCCA was also performed with either physical or biological factors separately. Our premise was that plots in the PA would cluster together and separately from the clustered plots of the SA assuming homogeneity of vegetation types within areas. All ordination analyses were performed using the CANOCO 4.55 software (Braak and Smilauer 2002).
Statistical analyses
To verify and compare the significance of the mean values of the indices, we used the Kruskal–Wallis test to examine data from the PA and SA areas of Mt. Cheonggye for comparisons over the entire study site (p < 0.05). We found a significant difference in plant community indices between PA and SA (Kruskal–Wallis test; p < 0.05); therefore, we compared the means of the indices for each study area using the Mann–Whitney test (p < 0.05). The cover of dominant species in each vegetation layer and species diversity indices of the tree and herb layers were also examined statistically using the Mann–Whitney test (p < 0.05). All statistical analyses were performed using the PAST 3.22 version software (Hammer 2018).