Next Article in Journal
Multi-Omics Approaches to Study Molecular Mechanisms in Cannabis sativa
Previous Article in Journal
The Modulatory Effects of Non-Thermal Plasma on Seed’s Morphology, Germination and Genetics—A Review
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Article

Tree Species Composition and Forest Community Types along Environmental Gradients in Htamanthi Wildlife Sanctuary, Myanmar: Implications for Action Prioritization in Conservation

1
Department of Environment and Forest Resources, Chungnam National University, Daejeon 34134, Korea
2
Department of Natural Resources Management, University of Forestry and Environmental Science, Yezin 15013, Myanmar
*
Author to whom correspondence should be addressed.
Plants 2022, 11(16), 2180; https://doi.org/10.3390/plants11162180
Submission received: 22 May 2022 / Revised: 15 August 2022 / Accepted: 18 August 2022 / Published: 22 August 2022
(This article belongs to the Topic Nature-Based Solutions)

Abstract

:
The identification of forest community types is essential for prioritizing choices and targets in species and community conservation purposes amid climate change impacts on forest community dynamics. Here, we determined the tree species composition, species diversity, and the forest community types across contrasting topographic and edaphic conditions in Htamanthi Wildlife Sanctuary (HWS), Myanmar. All tree species with diameter at breast height (DBH) ≥10 cm were recorded in 66 plots (625 m2), from which the species diversity, density, frequency, dominance, and importance value (IV) of each tree species were measured. The soil hardness (Hd), bulk density (BD), moisture content (MC), organic matter content (OM), texture, pH, total N, and available P, K, Ca, Na, and Mg concentrations were also analyzed. The elevation (ELV) and slope (SLP) were also measured as the topographic factors. Cluster analysis resulted in five distinct forest communities and the soil Ca, Mg, clay proportion, soil hardness, and elevation were the major influencing factors. The species diversity in HWS ranged from low to very high relative values, with 209 tree species belonging to 119 genera and 55 families. Identification of these community types and understanding the diversity levels and major factors influencing the community structure may play a key role in the planning, prioritization, and implementation of species and community conservation strategies amid the unpredictable impacts of climate change on forest community dynamics.

1. Introduction

Climate change has been altering the structure and functions of forest ecosystems worldwide. The unprecedented rise in global temperature may lead to the modification of various environmental variables and, thus, may shift in species composition and alterations in forest community structure at the local scale. Even minor changes in microclimatic conditions with elevation may also result in unusual changes in local diversity [1,2]. Environmental gradients, which refer to variations in site characteristics (i.e., edaphic, climatic, and physiographic variables), influence the patterns of tree species composition and distribution of forest communities [3]. Many interacting biotic and abiotic factors, including changes in elevation, slope, soil properties, and site index, affect species richness [4]. Climatic factors vary with elevation and exert a strong influence on plant distribution across ecosystems [5]. Thus, understanding the pattern of tree species composition and the types of forest communities across contrasting environmental conditions may play a key role in the planning, prioritization, and implementation of species and community conservation strategies amid the unpredictable impacts of climate change on forest community dynamics.
The pattern in tree species composition and forest community may vary among groups of plants and from one area to another due to differences in resource availability, plant life-history traits, and adaptive strategies of plants, as influenced by the prevailing environmental conditions [6,7]. Soil nutrient and moisture availability, for instance, can influence natural regeneration, seedling establishment, and species dominance depending on elevation [8,9,10]. Climatic factors, such as air temperature and precipitation, have an interactive role in the effects of soil nutrients on species dominance [6]. A study reported that a high soil nutrient supply, particularly nitrogen and phosphorus, can lead to a lower species richness and high soil moisture can result in a higher species richness [11]. It has also been suggested that soil pH exerts a strong influence on species composition at the local scale [12] by limiting the number of species that can adapt to the extreme ends of the pH gradient [13]. While numerous studies have focused on large geographical areas, there are fewer studies about tree species composition and distribution of forest communities along environmental gradients conducted in smaller landscapes or mountains. Because global changes in environmental conditions have a direct impact on local ecological systems, localized studies may contribute to global biodiversity conservation programs through prioritization of habitats and conservation strategies.
Htamanthi Wildlife Sanctuary (HWS), an ASEAN heritage park in Myanmar and probably the largest contiguous forest landscape in Asia, lies in a transition zone of three biodiversity hotspots [14]. The sanctuary is globally important because of its proximity to the Northern Forest Complex (NFC), one of the largest remaining contiguous forests in Southeast Asia. Despite the ecological importance of HWS, most earlier studies dealt with faunal resources and less attention was given to the floral resources, particularly trees. By knowing the patterns of tree species composition and types of forest communities along environmental gradients in this biodiversity hotspot, we could advance our understanding of the local forest communities and how the environmental variables affect these communities.
The identification of forest community types can play a key role in prioritizing conservation choices in biodiversity hotspots since nature-based solutions are emerging as an integrated approach to conserving biodiversity and ecosystem services [15]. One of the practical strategies in biodiversity conservation is the identification of priority areas featuring exceptional need for immediate conservation, particularly biodiverse areas experiencing high degree of habitat loss and risks [16]. This is because one of the major challenges commonly encountered by conservation practitioners is how to efficiently allocate limited resources to many focal ecosystems or forest plant communities needing conservation [17]. Thus, information on forest community types in Htamanthi Wildlife Sanctuary can subsequently be useful for the development of more efficient ecosystem-based conservation approaches amid limited resources.
Consequently, we determined the tree species composition, species diversity, and the forest community types along environmental gradients in HWS. The role of the environmental factors in shaping forest communities in HWS remains poorly studied. Identification of species and community structure is very relevant to understanding the status of tree populations, natural regeneration for species, and community conservation purposes amid climate change impacts on forest community dynamics [18].

2. Results

2.1. Forest Community Assemblages

In this study, the Bray–Curtis dissimilarity cluster analysis grouped the evergreen forest in Htamanthi Wildlife Sanctuary into five distinct forest communities (Figure 1). The biggest group is Vatica maingayi forest (VMF) with 36 plots, Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF) are intermediate, with 5–13 plots, and the smallest group is the bamboo forest (BF), with only two plots.

2.2. Species Diversity and Importance Values among Forest Communities

In this study, we identified 209 tree species belonging to 119 genera and 55 families across the five forest communities (Table S1). The VMF and BF forest communities have very high (3.965) and very low (0.086) Shannon (H) diversity values, respectively (Table 1). The same pattern was observed in Evenness (J’) values for these two forest communities. The QGF has a high diversity value of H = 3.25. The other forest communities (NCF and DTF) have moderate H values (2.659–2.807). The VMF is a major forest community composed of a higher number of species, genera and family, followed by NCF, QGF, DTF, and BF (Table S1). In terms of IV, the most dominant tree species is Vatica maingayi in VMF, Nothaphoebe condensa in NCF, Quercus glauca in QGF, and Diospyros toposia in DTF (Table 1 and Table S1).

2.3. Variations in Topography and Soil Characteristics among Forest Communities

There was a significant difference in the elevation and slope across the four forest communities (Table 2). The highest elevation was in DFT, intermediate in NCF, and the lowest value was found in both QGF and VMF. In terms of slope, DFT is the steepest among the forest communities.
At 0–15 cm soil depth, the MC, sand, and clay proportions varied significantly across forest communities (Table 3 and Table S2). The soil moisture (MC) in NCF and VMF were higher than DTF and QGF. Further, DTF and QGF have similarly high sand and clay proportions compared the other forest communities. At 15–30 cm soil depth, the Hd, MC, and clay proportion were significantly different across sites. Both DTF and NCF have a higher Hd than QGF or VMF. The DTF and QG have similarly higher MC than the other forest community types and a similar pattern was observed in clay proportions.
In terms of soil chemical characteristics, the available phosphorus (AP) was higher in DDT than those in the other forest communities at 0–15 cm soil depth (Table 4 and Table S3). An almost similar pattern was observed in Ca and Mg concentrations for both DDT and NCF. At 0–15 cm soil depth, the AP, Ca, and Mg were also significantly higher in DDT and/or NCF than the other forest community types (Table 4).

2.4. Redundancy Analysis (RDA) Biplot and Important Topographic and Edaphic Variables

To provide an additional quantification of the proportion of the variance in the data set and confirm that environmental variables influence the structure and classification of forest communities, we performed an RDA. At 0–15 cm soil depths, the relationship among the variables is significant (p = 0.001, Table S4). The first RDA axis and second axis explain 34.38% and 22.81% of the total variance, respectively (Figure 2). RDA1 is strongly and positively associated with ELV, Ca, and Mg, which are well represented in DTF community or D. toposia (DioTop)-dominated forests (Figure 2b). RDA1 is also strongly and negatively associated with clay proportion in VMF. RDA2 was highly associated with Hd in QGF community or Q. glauca (QurcGl)-dominated forests (Figure 2b).
At 15–30 cm soil depth, the relationship among topographic factors, the properties of soil at 15–30 cm soil depths, and ecologically important tree species and five forest communities is significant (p = 0.001, Table S4). The first two RDA axes accounted for 68.14% of the variations in the data set (Figure 3). Specifically, RDA1 accounted for 37.49% of the variation and was highly and positively related to Ca and ELV in DTF community. RDA2 accounted for 30.65% of the variation and was positively related to Hd in QGF and negatively to BD in VMF community.
Further, the forward selection approach revealed Ca (p = 0.001), clay proportion (p = 0.01), and Hd (p = 0.05) as the most contributive factors affecting the composition of tree species and classification of forest communities in the study area at 0–15 cm soil depth (Table S5). At 15–30 cm soil depth, the ELV, Hd, and Ca were the major factors affecting the classification of forest communities in Htamanthi Wildlife Sanctuary (Table S6).

3. Discussion

In this study, the identified forest community types showed a significant variation in their tree species richness, diversity, and evenness. Results revealed that the VMF and QGF have high to very high Shannon (H) diversity and Evenness (J’) values compared with the other community types. This variation could be ascribed to the differences in the communities in terms of topographic and edaphic factors through their influence on the dispersion behavior of tree species [19]. From a community ecology perspective, results suggest that VMF and QGF community types are more stable and resilient to natural disturbances and accelerating rates of environmental change than the other types of forest communities. Under a range of environmental disruptions that could occur in the future amid climate change, VMF and QGF may be able to provide essential forest ecosystem functions for the region. However, the impacts of environmental disruptions on ecosystem functions depend on the characteristics of forest communities that are related to resilience, including species diversity, relative abundance, and ability of the dominant species to resist regime shifts and recover functions following disturbance [20]. Here, the RDA biplot shows that the clay proportion and soil bulk density (BD) are highly associated with VMF, suggesting that any significant disturbance in these factors could potentially influence the community structure and functions. This is supported by the presence of the dominant species, V. maingayi, which is a dipterocarp tree species, typical of clay soil in lowland dipterocarp forests [21]. Two of the important factors influencing clay formation are the effects of soil moisture and temperature on weathering processes, which are the important aspects of regional climate change impacts on soil [22,23]. Similarly, the elevated global temperature may increase soil BD via climate change stresses (e.g., drought) and forest management activities [24]. Thus, our results suggests that, as climate change worsens, monitoring the changes in clay formation or weathering processes and soil bulk density is essential for the maintenance of VMF community structure and functions. Dealing with these two major factors influencing VMF community may represent a crucial step for determining priorities in plant community conservation.
The RDA biplot shows that the QGF community is highly associated with soil hardness (Hd), which is a good indicator of soil compaction and strength. This result suggests that HD may be an important factor controlling the plant community in QGF through either detrimental effects on subsequent natural regeneration in the area or enhancement of plant growth and accumulation of soil nutrients. The growth and survival of tree saplings can significantly decrease in compacted soil [25] through a reduction in root cell size, root penetration and, thus, acquisition of essential elements [26]. This may explain the observed negative correlation between Hd and Ca availability in soil. Contrarily, a study found that moderate-level soil compaction improved the plant uptake of P, K, Mg, Ca, and other elements, suggesting that soil compaction effects may vary depending on the severity [26]. Moreover, because soil hardness or soil compaction increases with decreasing soil moisture, the QGF may be more vulnerable to drought than the other forest communities, especially in years with little rainfall. The abundance of the slow-growing and drought-tolerant species, Q. glauca, can further explain the high association between Hd and the QGF community. As a drought-tolerant species, Q. glauca can thrive and flourish in low-resource and harsh environments, including those which are poorly drained and have tight soil spaces [27]. It has been projected that climate change will increase the frequency of drought and, thus, the effects on the plant community structure [28]. Results suggest that it is necessary to manage and prevent the causes of either surface or subsurface hardness constraints in the QGF community.
The DTF and NCF have moderate diversity values. This can be attributed to the possible effects of elevation (ELV) and soil nutrient availability, particularly Ca and Mg. The RDA biplot shows that the DTF community is highly associated with ELV, Ca, and Mg. The DTF has the highest ELV among the identified forest communities and the value is nearly similar to that of NCF. Results support the findings of Ohdo and Takahashi [29], who reported that the number of tree species decreased at high elevations and the pattern was attributed to soil nutrient availability. In the Himalaya Mountains, it was observed that soil nutrients (N, P, K, and Mg) decreased significantly with elevation [30]. In this study, the concentrations of Ca and Mg were higher in both DTF and NCF communities compared with the other community types. Higher elevation in the two communities may have influenced the concentration of exchangeable cations present in O and/or A horizons, i.e., Ca and Mg may have increased as elevation increased. Such an increase may be due to the decline in tree species composition as elevation increases. Fewer plants may decrease the demand for Ca and Mg ions, resulting in a greater number of ions left in the soil. This can be supported by the presence of the dominant species, D. toposia, which is typical of undisturbed forests with high amounts of nutrients [31]. D. toposia is also an evergreen tree species and evergreen plants usually exhibit a more conservative strategy, resulting in greater resource conservation.

4. Materials and Methods

4.1. Study Site and Sampling Method

The study was conducted in Htamanthi Wildlife Sanctuary (HWS, 25°45′52″ N to 25°45′15″ N, 95°16′55″ E to 95° 56′ 55″ E), which is a part of Himalaya biodiversity hotspot area in the northern part of Myanmar (Figure 4a). It was declared a protected area in 1974 with the extent of 215,073 hectares and, recently, it was declared the newest ASEAN heritage park. It is a dense forest comprising different habitats, including evergreen and semi-evergreen forests, swamp forests, and upper mixed dry deciduous forests. Some unique and ecologically important flora can also be found in the area, including Tectona grandis, Xylia xylocarpa, and Shorea robusta. The heritage park is generally pristine because of the minimal disturbance and absence of tourism-related activities. The annual air temperature and annual rainfall in the study site ranged from 17.7 to 34.3 °C and 343 mm, respectively, based on the 10-year climatic data from the local meteorological station near the HWS. The soil types in the study area are generally yellowish red, derived from acrisol parent material.
Sixty-six plots having a size of 25 m × 25 m were established in the study site by employing a systematic sampling (Figure 4b). The distance between plots was 5.7 km × 5.7 km. All adult trees with diameter at breast height (DBH) ≥ 10 cm were recorded in 25 m × 25 plots. The vegetative inventory was conducted from November to February in 2019 and 2021.

4.2. Determination of Topographic and Edaphic Variables

The physiographical variables, namely, geographic coordinates, elevation (ELV), slope (SLP), and aspect (ASP) were recorded for each plot using a GPS (Garmin GPSMAP 62s) device. The ALOS PALSAR RTC DEM (12.5 m) images were obtained from the Alaska Satellite Facility (UAF). Thereafter, ELV, SLP, and ASP of the sample plots were extracted from images and processed using ArcMap software (version 10.8, Esri, CA, USA).
Soil samples were collected from the three pre-determined points (10 m apart) in the 25 × 25 m plot using soil core sampler (5.0 cm in diameter). Three samples (c.a. 100 g) were collected from each soil depth (0–15 m and 15–30 cm) in each point and then composited into one bag. There was a total of 132 bags of soil (i.e., 1 bag × 2 soil depths × 66 plots = 132). The soil hardness (Hd) was measured at each soil depth and plot using a penetrometer. The soil bulk density (BD), the content of moisture content (MC), organic matter composition (OM), texture (sand, silt, clay), and seven chemical properties of soil; pH, total N, Available P, exchangeable K, Ca, Na, and Mg, were also analyzed using c.a. 100 g of composited soil sample at the Forest Soil Laboratory, Forest Research Institute (FRI), Yezin, Myanmar.

4.3. Data and Statistical Analyses

In this study, the species density, dominance, and frequency were calculated for all trees identified in each plot using the formulae in Table 5. The importance value (IV in %) of tree species encountered in the sampled plots were computed by obtaining the summation of the relative values of stem density, dominance, and frequency. The IV measures a given species’ dominance in a forest area based on species and stand structure. In this study, the IV was determined to describe the ecological significance of the species in HWS.
The Bray–Curtis cluster analysis was performed in RStudio software (version 4.2.0) using the vegan package to classify the vegetation into distinct forest community types. The similarity and dissimilarity among forest community types were determined using the Jaccard similarity index based on the species abundance data. The Jaccard’s similarity index formula is: J (i, j) = a/(a + b + c), where a = number of species in common between the communities; b = number of species unique to the first community; c = number of species unique to the second community.
The species richness (S), evenness (J), and Shannon–Wiener diversity index (H’) were computed using the R software. The Shannon diversity index (H’) was computed from the equation: H = −Σpi × ln(pi), where H is Shannon–Wiener diversity index, pi is the proportion of individual tree species.
Kruskal–Wallis test was applied to assess the significant differences in topographic and physico-chemical characteristics across the different forest communities. Pairwise comparisons among the different forest communities were conducted by Dunn–Bonferroni post hoc test method.
Here, redundancy analysis (RDA) ordination was used in describing the relationship between forest communities, topographic factors, and physico-chemical properties of soil. The global model test with permutations = 4999 was conducted to test for significance. The forward selection of variables was conducted to select the driving variables of assemblage of forest communities as well as to explain the variation in species with highly correlated variables. Monte Carlo test was applied to prove the significant correlation with 4999 permutations. Plot × species matrices and the estimation of IV were conducted in Microsoft Office Excel and all the statistical analyses were processed in RStudio software (version 4.2.0) at a 95% confidence level.

5. Conclusions

The present study revealed that there are four major evergreen forest communities, i.e., Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF), and one minor forest community, i.e., bamboo forest (BF), in Htamanthi Wildlife Sanctuary (HWS). Based on Shannon diversity index estimation, three of the five communities have high to very high species diversity, while the other two communities have low to moderate species diversity. Here, the soil Ca, Mg, clay proportion, soil hardness, and elevation were identified as the major factors in classifying the forest community types. Identification of these community types and understanding of the major factors influencing their structure is an important nature-based solution in biodiversity conservation for a biodiversity hotspot like HWS. The present work will enhance our understanding on how to efficiently implement an ecosystem-based conservation approach through conservation prioritization.

Supplementary Materials

The following supporting information can be downloaded at: https://www.mdpi.com/article/10.3390/plants11162180/s1, Table S1: List of tree species surveyed in Htamanthi Wildlife Sanctuary; Table S2: p values estimated by Kruskal–Wallis test for soil physical properties across soil depths and forest communities; Table S3: p values estimated by Kruskal–Wallis test for soil chemical properties across soil depths and forest communities; Table S4: Significance of test of the global model with all explanatory variables of topographic factors and soil properties; Table S5: Selection of important variables of topographic factors and soil properties at 0–15 cm depth of soil; Table S6: Selection of important variables of topographic factors and soil properties at 15–30 cm depth of soil.

Author Contributions

Conceptualization, B.B.P. and M.M.L.; methodology, B.B.P. and M.M.L.; software and data analysis, data collection, writing—original draft preparation, M.M.L.; writing—review and editing, B.B.P. and M.M.L.; supervision, B.B.P. All authors have read and agreed to the published version of the manuscript.

Funding

This study was carried out with the support of ‘R&D Program for Forest Science Technology (Project No. 2021379B10-2223-BD02 and 2020184C10-2222-AA02)’ provided by Korea Forest Service (Korea Forestry Promotion Institute).

Data Availability Statement

The data used are primarily reflected in the article. Other relevant data are available from the authors upon request.

Acknowledgments

This study was carried out according to the project of laboratory of forest ecology and silviculture, Chungnam National University (CNU), Republic of Korea (ROK) to analyze the diversity of flora and wildlife of Htamanthi Wildlife Sanctuary. The authors are grateful to the Forest Department of Myanmar for the permit and the support as well as to the local people and graduate students from the University of Forestry and Environmental Science, Yezin, for the effort and participation during our forest inventory in the protected areas. The authors acknowledge Wildlife Conservation Society (WCS) Myanmar program for supporting logistics and accommodation during the survey. Last but not the least, we deeply appreciate Jonathan O. Harnandez for kindly sharing his knowledge and discussion during this research.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Chen, J.; Saunders, S.C.; Crow, T.R.; Naiman, R.J.; Brosofske, K.D.; Mroz, G.D.; Brookshire, B.L.; Franklin, J.F. Microclimate in forest ecosystem and landscape ecology. BioScience 1999, 49, 288–297. [Google Scholar] [CrossRef] [Green Version]
  2. Duchicela, S.A.; Cuesta, F.; Tovar, C.; Muriel, P.; Jaramillo, R.; Salazar, E.; Pinto, E. Microclimatic warming leads to a decrease in species and growth form diversity: Insights from a tropical alpine grassland. Front. Ecol. Evol. 2021, 9, 673655. [Google Scholar] [CrossRef]
  3. Rahman, I.U.; Afzal, A.; Iqbal, Z.; Bussmann, R.W.; Alsamadany, H.; Calixto, E.S.; Shah, G.M.; Kausar, R.; Shah, M.; Ali, N.; et al. Ecological gradients hosting plant communities in Himalayan subalpine pastures: Application of multivariate approaches to identify indicator species. Ecol. Inform. 2020, 60, 101162. [Google Scholar] [CrossRef]
  4. Hawkins, B.A.; Field, R.; Cornell, H.V.; Currie, D.J.; Guégan, J.-F.; Kaufman, D.M.; Kerr, J.T.; Mittelbach, G.G.; Oberdorff, T.; O’Brien, E.M.; et al. Energy, water, and broad-scale geographic patterns of species richness. Ecology 2003, 84, 3105–3117. [Google Scholar] [CrossRef] [Green Version]
  5. Miao, L.; Jianmeng, F. Biogeographical interpretation of elevational patterns of genus diversity of seed plants in Nepal. PLoS ONE 2015, 10, e0140992. [Google Scholar] [CrossRef]
  6. Nepali, B.R.; Skartveit, J.; Baniya, C.B. Impacts of slope aspects on altitudinal species richness and species composition of Narapani-Masina Landscape, Arghakhanchi, West Nepal. J. Asia-Pac. Biodivers. 2021, 14, 415–424. [Google Scholar] [CrossRef]
  7. Cornwell, W.K.; Grubb, P.J. Regional and local patterns in plant species richness with respect to resource availability. Oikos 2003, 100, 417–428. [Google Scholar] [CrossRef] [Green Version]
  8. Toro Manríquez, M.D.R.; Cellini, J.M.; Lencinas, M.V.; Peri, P.L.; Peña Rojas, K.A.; Martínez Pastur, G.J. Suitable conditions for natural regeneration in variable retention harvesting of southern Patagonian nothofagus pumilio forests. Ecol. Process. 2019, 8, 1–12. [Google Scholar] [CrossRef]
  9. Davis, E.L.; Hager, H.A.; Gedalof, Z. Soil properties as constraints to seedling regeneration beyond alpine treelines in the Canadian Rocky Mountains. Arct. Antarct. Alp. Res. 2018, 50, e1415625-1-15. [Google Scholar] [CrossRef] [Green Version]
  10. Wenk, E.H.; Dawson, T.E. Interspecific differences in seed germination, establishment, and early growth in relation to preferred soil type in an Alpine community. Arct. Antarct. Alp. Res. 2007, 39, 165–176. [Google Scholar] [CrossRef] [Green Version]
  11. Palpurina, S.; Wagner, V.; Wehrden, H.V.; Hájek, M.; Horsák, M.; Brinkert, A.; Hölzel, N.; Wesche, K.; Kamp, J.; Hájková, P.; et al. The relationship between plant species richness and soil pH vanishes with increasing aridity across Eurasian dry grasslands. Glob. Ecol. Biogeogr. 2016, 26, 425–434. [Google Scholar] [CrossRef]
  12. Tyler, G. Some ecophysiological and historical approaches to species richness and calcicole/calcifuge behaviour—Contribution to a debate. Folia Geobot. 2003, 38, 419–428. [Google Scholar] [CrossRef]
  13. Currie, D.J.; Mittelbach, G.G.; Cornell, H.V.; Field, R.; Guegan, J.F.; Hawkins, B.A.; Kaufman, D.M.; Kerr, J.T.; Oberdorff, T.; O’Brien, E.; et al. Predictions and tests of climate-based hypotheses of broad-scale variation in taxonomic richness. Ecol. Lett. 2004, 7, 1121–1134. [Google Scholar] [CrossRef]
  14. Naing, H.; Ross, J.; Burnham, D.; Htun, S.; Macdonald, D.W. Population density estimates and conservation concern for clouded leopards neofelis nebulosa, marbled cats pardofelis marmorata and tigers panthera tigris in htamanthi wildlife sanctuary, Sagaing, Myanmar. Oryx 2017, 53, 654–662. [Google Scholar] [CrossRef] [Green Version]
  15. Seddon, N.; Chausson, A.; Berry, P.; Girardin, C.A.; Smith, A.; Turner, B. Understanding the value and limits of nature-based solutions to climate change and other global challenges. Philos. Trans. R. Soc. B Biol. Sci. 2020, 375, 20190120. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  16. Myers, N.; Mittermeier, R.A.; Mittermeier, C.G.; da Fonseca, G.A.; Kent, J. Biodiversity hotspots for conservation priorities. Nature 2000, 403, 853–858. [Google Scholar] [CrossRef] [PubMed]
  17. Rodríguez-Rodríguez, E.J.; Beltrán, J.F.; El Mouden, E.H.; Slimani, T.; Márquez, R.; Donaire-Barroso, D. Climate change challenges IUCN conservation priorities: A test with Western Mediterranean amphibians. SN Appl. Sci. 2020, 2, 216. [Google Scholar] [CrossRef] [Green Version]
  18. Hernandez, J.O.; Maldia, L.S.J.; Park, B.B. Research trends and methodological approaches of the impacts of windstorms on forests in tropical, subtropical, and temperate zones: Where are we now and how should research move forward? Plants 2020, 9, 1709. [Google Scholar] [CrossRef]
  19. Dibaba, A.; Soromessa, T.; Warkineh, B. Plant community analysis along environmental gradients in moist afromontane forest of Gerba Dima, south-western Ethiopia. BMC Ecol. Evol. 2021, 22, 1–17. [Google Scholar] [CrossRef]
  20. Oliver, T.H.; Heard, M.S.; Isaac, N.J.B.; Roy, D.B.; Procter, D.; Eigenbrod, F.; Freckleton, R.; Hector, A.; Orme, C.D.; Petchey, O.L.; et al. Biodiversity and resilience of ecosystem functions. Trends Ecol. Evol. 2015, 30, 673–684. [Google Scholar] [CrossRef] [Green Version]
  21. Davies, S.J.; Tan, S.; LaFrankie, J.V.; Potts, M.D. Soil-related floristic variation in the hyperdiverse dipterocarp forest in Lambir Hills, Sarawak. In Pollination Ecology and Rain Forest Diversity, Sarawak Studies; Roubik, D.W., Sakai, S., Hamid, A., Eds.; Springer: New York, NY, USA, 2005; pp. 22–34. [Google Scholar]
  22. Huszár, T.; Mika, J.; Lóczy, D.; Molnár, K.; Kertész, Á. Climate change and soil moisture: A case study. Phys. Chem. Earth Part A Solid Earth Geod. 1999, 24, 905–912. [Google Scholar] [CrossRef]
  23. Deepthy, R.; Balakrishnan, S. Climatic control on clay mineral formation: Evidence from weathering profiles developed on either side of the Western Ghats. J. Earth Syst. Sci. 2005, 114, 545–556. [Google Scholar] [CrossRef]
  24. Birkás, M. Tillage, impacts on soil and environment. In Encyclopedia of Agrophysics. Encyclopedia of Earth Sciences Series; Gliński, J., Horabik, J., Lipiec, J., Eds.; Springer: Dordrecht, The Netherlands, 2011; pp. 903–906. [Google Scholar] [CrossRef]
  25. Ampoorter, E.; de Frenne, P.; Hermy, M.; Verheyen, K. Effects of soil compaction on growth and survival of tree saplings: A meta-analysis. Basic Appl. Ecol. 2011, 12, 394–402. [Google Scholar] [CrossRef] [Green Version]
  26. Wang, M.; He, D.; Shen, F.; Huang, J.; Zhang, R.; Liu, W.; Zhu, M.; Zhou, L.; Wang, L.; Zhou, Q. Effects of soil compaction on plant growth, nutrient absorption, and root respiration in soybean seedlings. Environ. Sci. Pollut. Res. 2019, 26, 22835–22845. [Google Scholar] [CrossRef] [PubMed]
  27. Hernandez, J.O.; An, J.Y.; Combalicer, M.S.; Chun, J.P.; Oh, S.K.; Park, B.B. Morpho-anatomical traits and soluble sugar concentration largely explain the responses of three deciduous tree species to progressive water stress. Front. Plant Sci. 2021, 12, 738301. [Google Scholar] [CrossRef]
  28. Walter, J.; Hein, R.; Auge, H.; Beierkuhnlein, C.; Löffler, S.; Reifenrath, K.; Schädler, M.; Weber, M.; Jentsch, J. How do extreme drought and plant community composition affect host plant metabolites and herbivore performance? Arthropod-Plant Interact. 2012, 6, 15–25. [Google Scholar] [CrossRef]
  29. Ohdo, T.; Takahashi, K. Plant species richness and community assembly along gradients of elevation and soil nitrogen availability. AoB PLANTS 2020, 12, plaa014. [Google Scholar] [CrossRef] [Green Version]
  30. Drollinger, S.; Müller, M.; Kobl, T.; Schwab, N.; Böhner, J.; Schickhoff, U.; Scholten, T. Decreasing nutrient concentrations in soils and trees with increasing elevation across a treeline ecotone in Rolwaling Himal, Nepal. J. Mt. Sci. 2017, 14, 843–858. [Google Scholar] [CrossRef]
  31. Lalfakawma; Sahoo, U.K.; Roy, S.; Vanlalhriatpuia, K.; Vanalalhluna, P.C. Community composition and tree population structure in undisturbed and disturbed tropical semi-evergreen forest stands of north-east India. Appl. Ecol. Environ. Res. 2009, 7, 303–318. [Google Scholar] [CrossRef]
Figure 1. Dendrogram of all plots based on Bray–Curtis Distance complete linkage showing the five distinct forest communities of evergreen forest ecosystem in Htamanthi Wildlife Sanctuary in Myanmar. Forest communities: Bamboo forest (BF), Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF).
Figure 1. Dendrogram of all plots based on Bray–Curtis Distance complete linkage showing the five distinct forest communities of evergreen forest ecosystem in Htamanthi Wildlife Sanctuary in Myanmar. Forest communities: Bamboo forest (BF), Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF).
Plants 11 02180 g001
Figure 2. Redundancy analysis (RDA) biplot showing the (a) relationship among environmental variables and forest communities and (b) relationship among environmental variables and dominant tree species at 0–15 cm soil depth in Htamanthi Wildlife Sanctuary. Abbreviations: ELV—elevation, Hd—soil hardness, Mg—extractable magnesium, Ca—extractable calcium; forest communities: Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF). The number after the abbreviated name of the forest community in panel (a) indicates the plot number. In panel (b), the black lowercase letters indicate the abbreviated scientific names of dominant tree species (Table S1).
Figure 2. Redundancy analysis (RDA) biplot showing the (a) relationship among environmental variables and forest communities and (b) relationship among environmental variables and dominant tree species at 0–15 cm soil depth in Htamanthi Wildlife Sanctuary. Abbreviations: ELV—elevation, Hd—soil hardness, Mg—extractable magnesium, Ca—extractable calcium; forest communities: Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF). The number after the abbreviated name of the forest community in panel (a) indicates the plot number. In panel (b), the black lowercase letters indicate the abbreviated scientific names of dominant tree species (Table S1).
Plants 11 02180 g002
Figure 3. Redundancy analysis (RDA) biplot showing the (a) relationship among environmental variables and forest communities and (b) relationship among environmental variables and dominant tree species at 15–30 cm soil depth in Htamanthi Wildlife Sanctuary in Myanmar. Abbreviations: ELV—elevation, Hd—soil hardness, Mg—extractable magnesium, Ca—extractable calcium; forest communities: Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF). The number after the abbreviated name of the forest community in panel (a) indicates the plot number. In panel (b), the black lowercase letters indicate the abbreviated scientific names of dominant tree species (Table S1).
Figure 3. Redundancy analysis (RDA) biplot showing the (a) relationship among environmental variables and forest communities and (b) relationship among environmental variables and dominant tree species at 15–30 cm soil depth in Htamanthi Wildlife Sanctuary in Myanmar. Abbreviations: ELV—elevation, Hd—soil hardness, Mg—extractable magnesium, Ca—extractable calcium; forest communities: Vatica maingayi forest (VMF), Quercus glauca forest (QGF), Nothaphoebe condensa forest (NCF), and Diospyros toposia forest (DTF). The number after the abbreviated name of the forest community in panel (a) indicates the plot number. In panel (b), the black lowercase letters indicate the abbreviated scientific names of dominant tree species (Table S1).
Plants 11 02180 g003
Figure 4. (a) Location of study site (Htamanthi Wildlife Sanctuary) and (b) distribution of sample plots.
Figure 4. (a) Location of study site (Htamanthi Wildlife Sanctuary) and (b) distribution of sample plots.
Plants 11 02180 g004
Table 1. Species diversity values among forest community types in Htamanthi Wildlife Sanctuary in Myanmar. Values in parenthesis are the importance values of the dominant tree species.
Table 1. Species diversity values among forest community types in Htamanthi Wildlife Sanctuary in Myanmar. Values in parenthesis are the importance values of the dominant tree species.
Forest
Communities
Richness (S)Shannon-Wiener
Diversity Index (H)
Evenness (J′)Dominant Species and Importance Values (IV)
BF100.0860.037Aglaia perviridis (17.3%)
DTF512.6590.676Diospyros toposia (25.2%)
NCF952.8070.616Nothaphoebe condensa (26.2%)
QGF653.2540.780Quercus glauca (30.9%)
VMF1743.9650.769Vatica maingayi (35.9%)
Table 2. Topographic factors in the identified forest community types in Htamanthi Wildlife Sanctuary in Myanmar. Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between community types at α = 0.05.
Table 2. Topographic factors in the identified forest community types in Htamanthi Wildlife Sanctuary in Myanmar. Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between community types at α = 0.05.
FCnElevation (masl)Slope (°)
DTF5274 (57) a29 (19) a
NCF10188 (32) ab8 (6) b
QGF13179 (24) b16 (12) ab
VMF36177 (31) b16 (14) ab
Table 3. Soil physical properties in the Diospyros toposia forest (DTF), Nothaphoebe condensa forest (NCF), Quercus glauca forest (QGF), and Vatica maingayi forest (VMF). Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between forest community types at α = 0.05. Values in parenthesis are the standard deviations from the mean.
Table 3. Soil physical properties in the Diospyros toposia forest (DTF), Nothaphoebe condensa forest (NCF), Quercus glauca forest (QGF), and Vatica maingayi forest (VMF). Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between forest community types at α = 0.05. Values in parenthesis are the standard deviations from the mean.
Soil Depth (cm)Forest Community nSoil Hardness
(kg/cm2)
Moisture Content
(%)
Bulk Density
(%)
Organic Matter
(%)
Sand
(%)
Silt
(%)
Clay
(%)
0–15DTF52.50 (0.55) a10.30 (3.19) a1.18 (0.06) a6.00 (1.87) a54.2 (4.2) c29.0 (4.2) a16.2 (3.5) a
NCF102.79 (0.88) a20.10 (4.32) b1.18 (0.14) a7.30 (2.11) a39.4 (13.1) a30.3 (7.6) a29.2 (7.3) b
QGF133.31 (0.72) a17.89 (8.04) ab1.10 (0.09) a6.69 (1.25) a50.0 (5.3) bc29.8 (3.7) a19.1 (3.8) a
VMF363.00 (1.11) a20.10 (9.80) b1.19 (0.14) a6.00 (1.87) a46.6 (6.7) ab27.6 (5.0) a24.5 (6.1) b
15–30DTF53.06 (1.18) a12.00 (2.95) a1.13 (0.09) a6.20 (1.48) a46.8 (4.3) a27.0 (3.2) a22.6 (3.0) a
NCF102.89 (0.87) a21.80 (3.50) b1.16 (0.11) a7.70 (1.34) a42.1 (2.5) a28.9 (8.2) a32.6 (5.9) b
QGF133.94 (0.48) b16.30 (2.52) a1.05 (0.10) a7.15 (1.14) a46.2 (2.2) a28.8 (3.7) a23.1 (4.3) a
VMF363.05 (1.02) ab19.80 (4.63) b1.13 (0.09) a6.97 (1.13) a42.3 (1.3) a26.6 (4.8) a27.9 (6.8) ab
Table 4. Soil chemical properties in the Diospyros toposia forest (DTF), Nothaphoebe condensa forest (NCF), Quercus glauca forest (QGF), and Vatica maingayi forest (VMF). Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between forest community types at α = 0.05. Values in parenthesis are the standard deviations from the mean. Abbreviations: TN—total nitrogen, AP—available phosphorus, K—extractable potassium, Ca—extractable calcium, Na—extractable sodium, Mg—extractable magnesium.
Table 4. Soil chemical properties in the Diospyros toposia forest (DTF), Nothaphoebe condensa forest (NCF), Quercus glauca forest (QGF), and Vatica maingayi forest (VMF). Values in parenthesis are the standard deviations from the mean. Different lowercase letters indicate statistical significance between forest community types at α = 0.05. Values in parenthesis are the standard deviations from the mean. Abbreviations: TN—total nitrogen, AP—available phosphorus, K—extractable potassium, Ca—extractable calcium, Na—extractable sodium, Mg—extractable magnesium.
Soil Depth (cm)Forest CommunitynpHTN
(g/kg)
AP
(mg/kg)
K
(mg/100 g)
Ca
(mg/100 g)
Na
(mg/100 g)
Mg
(mg/100 g)
0–15DTF55.12 (0.19) a0.590 (0.136) a80.0 (7.10) a8.40 (3.78) a63.80 (6.44) a0.30 (0.07) a154.40 (144.0) a
NCF104.94 (0.09) a0.657 (0.285) a47.0 (35.0) b5.20 (3.52) a10.20 (6.25) b0.32 (0.09) a21.60 (28.7) ab
QGF134.85 (0.23) a0.611 (0.189) a55.4 (13.9) b4.15 (1.57) a5.15 (3.63) b0.22 (0.15) a18.77 (18.2) ab
VMF364.89 (0.11) a0.663 (0.141) a50.0 (20.6) b5.14 (3.09) a7.36 (8.59) b0.28 (0.14) a12.19 (18.0) b
15–30DTF54.98 (0.12) a0.622 (0.955) a80.0 (21.5) a8.80 (4.32) a13.60 (12.60) a0.24 (0.11) a72.40 (49.0) a
NCF104.97 (0.09) a0.572 (0.174) a44.0 (32.4) b5.00 (3.56) a7.60 (3.92) ab0.34 (0.18) a19.80 (29.8) b
QGF135.08 (0.84) a0.600 (0.129) a45.4 (32.4) b4.08 (1.93) a3.15 (2.61) b0.19 (0.13) a19.46 (21.6) b
VMF364.94 (0.13) a0.618 (0.172) a42.8 (16.1) b5.28 (3.09) a6.39 (7.53) ab0.26 (0.16) a19.19 (54.7) b
Table 5. Ecological/biotic parameters measured in Htamanthi Wildlife Sanctuary. Abbreviations: SDen—species density; RDen—relative density; SFre—species frequency; RFre—relative frequency; SDom—species dominance; RDom—relative dominance; IV—importance values; BA—basal area; AS—area sampled; DBH—diameter at breast height.
Table 5. Ecological/biotic parameters measured in Htamanthi Wildlife Sanctuary. Abbreviations: SDen—species density; RDen—relative density; SFre—species frequency; RFre—relative frequency; SDom—species dominance; RDom—relative dominance; IV—importance values; BA—basal area; AS—area sampled; DBH—diameter at breast height.
ParametersDescriptionFormula
Species densityThe actual size or number of individuals of one species per unit area.Den = No. of individuals of each species/AS
Relative densityThe density of one species as a percent of the total density of all species.RDen = (Den for a species/total density for all identified species) × 100
Species frequencyThe number of times a plant species is present in a given number of plots or quadrats.Fre = No. of plots in which species occur/ total number of plots sampled
Relative frequencyThe frequency of one species as a percent of the total frequency of all species.RFre = (Fre for a species/total frequency for all identified species) × 100
DominanceA species that is most commonly found or dominant based on basal area or percent coverage.Dom = BA of one species/AS
Relative dominanceThe dominance of one species as a percent of the total dominance of all species.RDom = (Dom for a species/total dominance for all identified species) × 100
Importance valuesThe IV is a measure of how dominant a species is in a given forest area.IV = RDen + RFre + RDom
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Share and Cite

MDPI and ACS Style

Latt, M.M.; Park, B.B. Tree Species Composition and Forest Community Types along Environmental Gradients in Htamanthi Wildlife Sanctuary, Myanmar: Implications for Action Prioritization in Conservation. Plants 2022, 11, 2180. https://doi.org/10.3390/plants11162180

AMA Style

Latt MM, Park BB. Tree Species Composition and Forest Community Types along Environmental Gradients in Htamanthi Wildlife Sanctuary, Myanmar: Implications for Action Prioritization in Conservation. Plants. 2022; 11(16):2180. https://doi.org/10.3390/plants11162180

Chicago/Turabian Style

Latt, Myo Min, and Byung Bae Park. 2022. "Tree Species Composition and Forest Community Types along Environmental Gradients in Htamanthi Wildlife Sanctuary, Myanmar: Implications for Action Prioritization in Conservation" Plants 11, no. 16: 2180. https://doi.org/10.3390/plants11162180

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop