Abstract

Soil quality (SQ) refers to its capacity to perform its functions. Thus, the SQ index (SQI) is a potentially useful tool for monitoring soil changes induced by mangrove restoration initiatives. Although the soil management assessment framework (SMAF) is a well-developed tool for SQ assessments in diverse ecosystems, it has never been tested on mangrove soils. In this study, we tested the SMAF to evaluate the shifts in the SQ of mangroves in a reforestation initiative using three- and seven-year plantations, which were compared with degraded and mature mangroves. A minimum dataset, composed of the pH and available P as chemical indicators, bulk density as a physical indicator, and soil organic carbon as a biological indicator, was used to calculate the SQI. The SMAF scores facilitated the monitoring of improvement in the mangrove SQ with vegetation development, mainly driven by physical and biological indicators. The SMAF may be a useful tool for monitoring SQ in mangroves under protection and recovery initiatives. Nevertheless, we suggest the inclusion of additional biological and chemical indicators in the minimum dataset for future studies to better represent specific processes and functions (e.g., microbial redox reactions and contaminant immobilization) that can alter the SQ of mangroves.

Highlights

  • Different forest biomes at a global scale provide significant ecosystem service (ES)diversity

  • Gradual increases in the SOC content were observed in the soil management assessment framework (SMAF) score, which was attributed to the biological indicator of soil quality (SQ) (SOC; Table 2)

  • This study used the SMAF tool to monitor the effect of a mangrove reforestation initiative on SQ

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Summary

Introduction

Mangroves are estuarine ecosystems that provide a wide diversity of ESs, such as regulation, support, and culture for human livelihood [2–5]. Despite this recognition, mangroves are one of the ecosystems most threatened by human activities, i.e., mainly aquaculture, sewage and industrial disposal, and deforestation [6,7]. Many of the ESs provided by mangroves are directly associated with soil processes and soil quality (SQ) [10–12]. As tidal activity influences mangroves, this flooded environment has soil characterized by intrinsic geochemical characteristics, such as a high salinity, low oxygen diffusion, and predominance of anaerobic metabolism [15,16]. The geochemical features of mangrove soils lead to low organic matter decomposition rates and iron sulfide formation, which favor the sequestration of large amounts of carbon

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