The Impact of Microhabitat and Microtopography on the Photosynthetic Characteristics of Typical Karst Forest Plants in Guizhou, China
Abstract
:1. Introduction
2. Materials and Methods
2.1. Study Region
2.2. Experimental Design
2.2.1. Microhabitat Type Classification
- Stone surface: The exposed rate of bedrock is more than 50%. The groove depth is less than 30 cm when irregular bare rocks such as shallow small gullies, shallow stone pits, small grooves, and narrow stone crevices are formed. These are usually soil-less or are only covered by less than 1 m2 of soil; soil thickness is less than 20 cm in stone surfaces. Although the ventilation conditions are favorable, the rapid water loss, weak water and fertilizer retention capacity, and susceptibility to temporary drought create a harsh environment. The soil water holdup is 45.06% [5]. The soil pH is 7.15, the contents of K, N, C, P of soil were 13.15 g·kg−1, 14.55 g·kg−1, 171.19 g·kg−1, and 1.15 g·kg−1, respectively.
- Stone gully: Under conditions in which the bare rock rate surpasses 50%, the groove depth is generally greater than 30 cm, with the soil coverage region being confined to below 1 m2. The soil thickness exceeds 20 cm when the groove depth is below 30 cm, or the soil layer is thicker than 20 cm when the groove depth is under 30 cm. Alternatively, the area is predominantly soil-covered with a groove depth exceeding 30 cm, provided the bare rock rate is below 50%. The soil layer is thicker, with improved water and fertilizer retention capabilities, making it less prone to short-term drought, subsequently resulting in relatively favorable conditions. The soil water holdup is 54.97% [5]. The soil pH is 7.04, and the contents of K, N, C, P of soil are 14.62 g·kg−1, 11.59 g·kg−1, 122.70 g·kg−1, and 0.97g·kg−1, respectively.
- Soil surface: The contiguous soil coverage area exceeds 1 m2. For areas smaller than 1 m2, the bare rock rate is less than 50%, and the groove depth is under 30 cm. The soil layer is thicker, with enhanced water and fertilizer retention capacity, better ventilation conditions, and slower water loss, making the soil conditions relatively optimal, though short-term drought remains a possibility. The soil water holdup is 49.11% [5]. The soil pH is 6.56, and the contents of K, N, C, P of soil are 15.61g·kg−1, 7.34 g·kg−1, 79.79 g·kg−1, and 0.85 g·kg−1, respectively.
2.2.2. Microtopography Classification
2.2.3. Sampling Methods
2.2.4. Measurement of Plant Photosynthetic Parameters
2.2.5. Calculation Method for Photosynthetic Parameters [25]
2.2.6. Data Processing and Analysis
3. Results
3.1. Plant Photosynthetic Characteristics in Various Microhabitats
3.2. Plant Photosynthetic Characteristics in Various Microtopographies
3.2.1. Plant Photosynthetic Characteristics in Various Slope Aspects
3.2.2. Plant Photosynthetic Characteristics in Various Slope Positions
3.2.3. Plant Photosynthetic Characteristics in Various Slope Degrees
3.3. Relationship Between Plant Photosynthetic Characteristics and Microhabitat
3.4. Relationship Between Plant Photosynthetic Characteristics and Microtopographies
3.5. PCA of Plant Photosynthetic Characteristics
3.6. The Correlation of Plant Photosynthetic Characteristics
4. Discussion
4.1. Response of Plant Photosynthetic Characteristics to Microhabitat
4.2. Response of Plant Physiological Characteristics to Microtopography
4.3. Strategies of Plants for Adapting to Microhabitats
5. Conclusions
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Microtopography | Division Basis |
---|---|
Slope positions | upslope, midslope, downslope, and depression |
Slope degrees | slope ≤ 5°, slope 5°~15°, slope 15°~25°, slope 25°~35°, slope ≥ 35° |
Slope aspects | shady slope (337.5°~22.5°, 22.5°~67.5°) |
semi-shady slope (67.5°~112.5°, 292.5°~337.5°) | |
flat land (slope degrees ≤ 5°) | |
semi-sunny slope (112.5°~157.5°, 247.5°~292.5°) | |
sunny slope (157.5°~247.5°) |
Types | Pn (μmol·m−2·s−1) | WUE (μmol·mmol−1) | Ci (μmol·mol−1) | Tr (mmol·m−2·s−1) | Gs (mol·m−2·s−1) | CE (μmol·m−2·s−1) | LUE (%) |
---|---|---|---|---|---|---|---|
Stone gully | 6.11 ± 0.31 a | 7.66 ± 0.35 a | 294.07 ± 6.36 a | 0.89 ± 0.05 a | 0.136 ± 0.014 a | 0.021 ± 0.001 a | 0.51 ± 0.03 a |
Stone surface | 5.73 ± 0.30 a | 6.14 ± 0.35 b | 277.60 ± 7.69 a | 1.02 ± 0.06 a | 0.106 ± 0.009 a | 0.022 ± 0.001 a | 0.48 ± 0.02 a |
Soil surface | 6.36 ± 0.43 a | 6.62 ± 0.30 b | 279.95 ± 6.34 a | 0.99 ± 0.06 a | 0.127 ± 0.015 a | 0.023 ± 0.001 a | 0.54 ± 0.04 a |
F | 0.821 | 6.628 | 1.674 | 1.511 | 1.402 | 0.732 | 1.158 |
p | 0.441 | 0.002 | 0.190 | 0.223 | 0.248 | 0.482 | 0.316 |
Component | Eigenvector | Eigenvalue | Cumulative/ % | ||||||
---|---|---|---|---|---|---|---|---|---|
x1 (Pn) | x2 (Gs) | x3 (Ci) | x4 (Tr) | x5 (WUE) | x6 (CE) | x7 (LUE) | |||
y1 | 0.49 | 0.39 | 0.19 | 0.40 | 0.07 | 0.41 | 0.49 | 4.03 | 57.59% |
y2 | 0.15 | −0.33 | −0.54 | −0.28 | 0.57 | 0.38 | 0.15 | 1.54 | 22.06% |
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Jiang, X.; Zhou, H.; Zhao, W.; Cui, Y.; Hou, Y.; Zhou, T.; Hu, F.; Wu, P. The Impact of Microhabitat and Microtopography on the Photosynthetic Characteristics of Typical Karst Forest Plants in Guizhou, China. Forests 2025, 16, 532. https://doi.org/10.3390/f16030532
Jiang X, Zhou H, Zhao W, Cui Y, Hou Y, Zhou T, Hu F, Wu P. The Impact of Microhabitat and Microtopography on the Photosynthetic Characteristics of Typical Karst Forest Plants in Guizhou, China. Forests. 2025; 16(3):532. https://doi.org/10.3390/f16030532
Chicago/Turabian StyleJiang, Xia, Hua Zhou, Wenjun Zhao, Yingchun Cui, Yiju Hou, Ting Zhou, Fangcai Hu, and Peng Wu. 2025. "The Impact of Microhabitat and Microtopography on the Photosynthetic Characteristics of Typical Karst Forest Plants in Guizhou, China" Forests 16, no. 3: 532. https://doi.org/10.3390/f16030532
APA StyleJiang, X., Zhou, H., Zhao, W., Cui, Y., Hou, Y., Zhou, T., Hu, F., & Wu, P. (2025). The Impact of Microhabitat and Microtopography on the Photosynthetic Characteristics of Typical Karst Forest Plants in Guizhou, China. Forests, 16(3), 532. https://doi.org/10.3390/f16030532