Abstract

Rock outcrop is an important habitat supporting plant communities in karst landscape. However, information on the restoration of higher biotic populations on outcrops is limited. Here, we investigated the diversity, biomass changes of higher vascular plants (VP) and humus soil (HS) on karst outcrops during a restoration process. We surveyed VP on rock outcrops and measured HS reserved by various rock microhabitats in a rock desertification ecosystem (RDE), an anthropogenic forest ecosystem (AFE), and a secondary forest ecosystem (SFE) in Shilin County, southwest China. HS metrics (e.g. quantity and nutrients content) and VP metrics (e.g. richness, diversity and biomass) were higher at AFE than at RDE, but lower than at SFE, suggesting that the restoration of soil subsystem vegetation increased HS properties and favored the succession of VP on rock outcrops. There was significantly positive correlation between VP metrics and HS amount, indicating that the succession of VP was strongly affected by availability and heterogeneity of HS in various rock microhabitats. Thus, floral succession of rock subsystem was slow owing to the limited resources on outcrops, although the vegetation was restored in soil subsystem.

Highlights

  • Karst landscapes constitute approximately 12–15% of the global terrestrial surface[1]

  • We aim to answer the following questions: (1) How much is the amount of humus soil (HS) on rock outcrops and how does it impact on vascular plants (VP)? (2) Do the diversity, density, lifeforms, species composition, and distribution of VP on rock outcrops differ in rocky desertification restoration? (3) Did the rock outcrop subsystem restore following revegetation in soil subsystem? (4) What factors drive rock vegetation succession?

  • The moisture content of the HS showed the following pattern: secondary forest ecosystem (SFE) > anthropogenic forest ecosystem (AFE) > rock desertification ecosystem (RDE), and it was significantly different among ecosystems

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Summary

Introduction

Karst landscapes constitute approximately 12–15% of the global terrestrial surface[1]. Human activities (e.g. firewood harvesting and grazing) cause trees growing on soil subsystems to be destroyed leaving rock outcrops exposed This process is called rocky desertification when the exposed rocks ratio reaches ≥ 30% of the land surface in China[1], and it is considered a serious environmental problem globally[5]. Thereby, outcrops gradually form diverse microhabitats (e.g., rocky pit, rocky crevice, rocky surface, rocky gully, etc.) comprising high heterogeneity[7,8] These microhabitats can intercept and gather soil particles, animal residues, vegetation litter and other exotic substances transported by rainfall and air flow from great distances[9,10]. Floral succession in rock subsystems can be considered as an important aspect when evaluating karst degradation and restoration

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