Abstract

Despite the fact that the vegetation pattern and history of the Bale Mountains in Ethiopia were reconstructed using pollen, little is known about the former extent of Erica species. The main objective of the present study is to identify unambiguous chemical proxies from plant-derived phenolic compounds to characterize Erica and other keystone species. Mild alkaline CuO oxidation has been used to extract sixteen phenolic compounds. After removal of undesired impurities, individual phenols were separated by gas chromatography and were detected by mass spectrometry. While conventional phenol ratios such as syringyl vs. vanillyl and cinnamyl vs. vanillyl and hierarchical cluster analysis of phenols failed for unambiguous Erica identification, the relative abundance of coumaryl phenols (>0.20) and benzoic acids (0.05—0.12) can be used as a proxy to distinguish Erica from other plant species. Moreover, a Random Forest decision tree based on syringyl phenols, benzoic acids (>0.06), coumaryl phenols (<0.21), hydroxybenzoic acids, and vanillyl phenols (>0.3) could be established for unambiguous Erica identification. In conclusion, serious caution should be given before interpreting this calibration study in paleovegetation reconstruction in respect of degradation and underground inputs of soil organic matter.

Highlights

  • The present vegetation cover in mountain ecosystems is the result of subsequent historical and ecological processes primarily influenced by climate and human [1,2]

  • A typical gas chromatogram of phenolic compounds released after mild alkaline cupric oxide (CuO) oxidation illustrates the compositional complexity of a typical plant sample (Lobelia rhynchopetalum; Figure 1)

  • The phenolic compounds from Festuca vallesiaca species investigated in Serbia accounts for low benzoic acid derivatives and high coumaryl phenols (p–coumaric acid, ferulic acid)

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Summary

Introduction

The present vegetation cover in mountain ecosystems is the result of subsequent historical and ecological processes primarily influenced by climate and human [1,2]. To reconstruct and draw full pictures of environmental changes over the past centuries, Ethiopia is an ideal place for several reasons. It is the origin of Homo sapiens and many other fauna and Plants 2019, 8, 228; doi:10.3390/plants8070228 www.mdpi.com/journal/plants. It comprises diverse geographical zones attributed to various climatic features [4,5]. The Bale Mountains are one of the Eastern Afromontane Biodiversity Hotspots, which encompass many endemic and endangered species of Ethiopia [6,7].

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