Abstract

This study aimed to elucidate the effects of periphyton on the microprofiles of oxygen (O2), pH, and oxidation-reduction potential around the stems and leaves of a submerged macrophyte Potamogeton malaianus and on the plant growth in the eutrophic shallow Taihu Lake, China. The microprofiles were measured using a motorized microprofiling system equipped with microsensors. The leaf age of the macrophyte and periphyton exerted significant effects on the microprofiles of O2, pH, and oxidation-reduction potential. O2 concentration and pH increased whereas the oxidation-reduction potential decreased with decreasing distance to the stem/leaf surface. The fluctuation amplitudes of O2, pH, and oxidation-reduction potential were the largest in the microprofiles of mature leaves and the lowest in senescent leaves. The periphyton increased the thickness of the broad diffusive boundary layer and fluctuation amplitudes of O2, pH, and oxidation-reduction potential. When the periphyton was removed, the thickness of the broad diffusive boundary layer in the microprofiles of stems, senescent leaves, and mature leaves reduced by 29.0%, 49.72%, and 70.34%, and the O2, pH, and oxidation-reduction potential fluctuation amplitudes also declined accordingly. Our results suggest that a thick periphyton exerted negative effects on the growth of macrophytes by providing extensive shading and creating a barrier that hindered the transport of dissolved substances such as O2, and led to premature decline in macrophytes in the eutrophic Taihu Lake. The consequent implications can help to elucidate the control mechanism of the broad diffusive boundary layer around macrophytes on nutrient cycling in eutrophic waters and to better understand the role of this layer in the Taihu Lake and other similar eutrophic waters.

Highlights

  • The boundary layer around submerged macrophytes surfaces plays an important ecological role in macrophyte growth and nutrient transformation in the aquatic environment [1,2]

  • We investigated the O2, pH, and Oxidationreduction potential (ORP) microprofiles around the stems and leaves of P. malaianus using microsensors, and aimed at revealing (i) the O2, pH, and ORP of microprofiles on different parts of the same plant; and (ii) the effect of periphyton on the distribution of O2, pH, and ORP in the microprofiles

  • Because the chlorophyll a content, photosynthetic activity, oxygen-release capacity, and periphyton biomass of young leaves were lower than those of mature leaves (Table 1), a thiner diffusive boundary layer (DBL) was formed, and the oxidation microenvironment was weak with less fluctuation of O2, pH, and ORP (Figs. 1G, 3G, 4G, 5)

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Summary

Introduction

The boundary layer around submerged macrophytes surfaces plays an important ecological role in macrophyte growth and nutrient transformation in the aquatic environment [1,2]. Periphyton is an assemblage of algae, bacteria, fungi, animals, inorganic matter, and organic detritus that remains attached to submerged macrophyte surfaces and forms a special bio-water boundary layer [4]. The submerged macrophyte-water boundary layer occupying the key interface of lake ecosystems remarkably influences the productivity and biogeochemical cycles in shallow lake ecosystems [5,6]. The special boundary layer with a dense periphyton was found to hinder the long-term growth of submerged macrophytes [1,14,15], leading to the degradation and even disappearance of submerged macrophytes [16,17]

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