Abstract

Anthropogenic activities have increased phosphorus (P) inputs to most aquatic and terrestrial ecosystems. However, the relationship between plant nutrient resorption and P availability is still unclear, and much less is known about the underlying mechanisms. Here, we used a multi-level P addition experiment (0, 1.2, 4.8, and 9.6 g P m−2 year−1) to assess the effect of P enrichment on nutrient resorption at plant organ, species, and community levels in a freshwater marsh of Northeast China. The response of nutrient resorption to P addition generally did not vary with addition rates. Moreover, nutrient resorption exhibited similar responses to P addition across the three hierarchical levels. Specifically, P addition decreased nitrogen (N) resorption proficiency, P resorption efficiency and proficiency, but did not impact N resorption efficiency. In addition, P resorption efficiency and proficiency were linearly related to the ratio of inorganic P to organic P and organic P fraction in mature plant organs, respectively. Our findings suggest that the allocation pattern of plant P between inorganic and organic P fractions is an underlying mechanism controlling P resorption processes, and that P enrichment could strongly influence plant-mediated biogeochemical cycles through altered nutrient resorption in the freshwater wetlands of Northeast China.

Highlights

  • Anthropogenic activities have increased phosphorus (P) inputs to most aquatic and terrestrial ecosystems

  • D. angustifolia leaf and stem biomass generally declined, while G. spiculosa leaf and stem biomass increased with increasing P addition levels (Table 1)

  • In this study, adding P with different levels generally had the similar effects on plant nutrient resorption parameters across the three hierarchical levels. These findings provided evidence that there existed a threshold for P enrichment-induced effects on plant nutrient resorption

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Summary

Introduction

Anthropogenic activities have increased phosphorus (P) inputs to most aquatic and terrestrial ecosystems. The relationship between plant nutrient resorption and P availability is still unclear, and much less is known about the underlying mechanisms. Our findings suggest that the allocation pattern of plant P between inorganic and organic P fractions is an underlying mechanism controlling P resorption processes, and that P enrichment could strongly influence plant-mediated biogeochemical cycles through altered nutrient resorption in the freshwater wetlands of Northeast China. Phosphorus enrichment generally increases P concentration in mature leaves and reduces plant P resorption proficiency (i.e. the level to which nutrient concentration is reduced in senesced organs7) in fertilization studies[12,13,14]. Knowledge about the allocation patterns of P fractions in plants is needed to unravel the underlying mechanism controlling the response of plant P resorption to increased P inputs. Different lowercase letters in the same rows indicated significant differences among the four treatments

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