Journal
FORESTS
Volume 13, Issue 4, Pages -Publisher
MDPI
DOI: 10.3390/f13040611
Keywords
biomass; fine root turnover; necromass; production; karst ecosystem
Categories
Funding
- National Natural Science Foundation of China [U20A2011, 31800441, 41907208]
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The study revealed that fine root production, biomass, and necromass were significantly influenced by slope position, while the fine root biomass/necromass ratio was significantly affected by vegetation type. The variations in these parameters were mainly explained by fine root nutrients and the interactive effects between fine root and soil nutrients. These findings suggest that fine roots responding to soil and root nutrient changes might serve as an adaptive mechanism to enhance plant nutrient acquisition in nutrient-poor karst ecosystems.
Revealing the patterns of fine root turnover traits can aid our understanding of the mechanisms of fine roots in adapting to soil nutrient changes. In a karst ecosystem of southwest China, the fine root turnover rate, production, biomass, necromass, biomass/necromass ratio, as well as the soil total and available nitrogen (N) and phosphorus (P) concentrations, and root carbon (C) and N concentrations were analyzed in upper, middle, and lower slope positions of two vegetation types (shrubland and forest). The results showed that the soil total and available N and P and fine root production, biomass, and necromass were significantly higher in upper slope positions than those in lower slope positions in both vegetation types. However, the fine root turnover rates were slightly higher in upper positions than those in lower positions. In addition, fine root necromass was significantly lower in shrubland than that in forest, while the biomass/necromass ratio was the opposite. Therefore, fine root production and biomass were significantly affected by slope position, while the fine root biomass/necromass ratio was significantly influenced by vegetation type. Additionally, fine root necromass was significantly influenced by the slope position and vegetation, but the turnover rate was slightly impacted by the two factors. It was also found that fine root production, biomass, and necromass had significant positive correlations with the soil total and available N and P and root C concentrations, and had significant negative correlations with root N concentrations. Moreover, the biomass/necromass ratio was positively and negatively related to the root N concentrations and C/N ratios, respectively. Thus, the variations in these five parameters of fine root turnover were mainly explained by fine root nutrients and the interactive effects between fine root and soil nutrients. The above results indicated that these variations in fine roots responding to soil and root nutrient changes might be an adaptive mechanism to enhance plant nutrient acquisition in nutrient-poor karst ecosystems.
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