Abstract

Information on whole community responses is needed to predict direction and magnitude of changes in plant and animal abundance under global changes. This study quantifies the effect of past ozone exposure on a weed community structure and arthropod colonization. We used the soil seed bank resulting from a long-term ozone exposure to reestablish the plant community under a new low-pollution environment. Two separate experiments using the same original soil seed bank were conducted. Plant and arthropod richness and species abundance was assessed during two years. We predicted that exposure to episodic high concentrations of ozone during a series of growing cycles would result in plant assemblies with lower diversity (lower species richness and higher dominance), due to an increase in dominance of the stress tolerant species and the elimination of the ozone-sensitive species. As a consequence, arthropod-plant interactions would also be changed. Species richness of the recruited plant communities from different exposure histories was similar (≈ 15). However, the relative abundance of the dominant species varied according to history of exposure, with two annual species dominating ozone enriched plots (90 ppb: Spergula arvensis, and 120 ppb: Calandrinia ciliata). Being consistent both years, the proportion of carnivore species was significantly higher in plots with history of higher ozone concentration (≈3.4 and ≈7.7 fold higher in 90 ppb and 120 ppb plots, respectively). Our study provides evidence that, past history of pollution might be as relevant as management practices in structuring agroecosystems, since we show that an increase in tropospheric ozone may influence biotic communities even years after the exposure.

Highlights

  • Human activities are changing Earth’s climate and biotic communities at an unprecedented rate, modifying species range limits and causing extinctions from local to global scale [1]

  • Plant species richness in the plots set up in a common low-ozone environment in Argentina was highly reduced to over half the number of species historically recorded in the chambers under the different exposure regimes (Table 1)

  • Species extinction during storage in the seed bank was not related to their constancy values in the chambers or the ozone treatment they characterized, i.e. all constancy and ozone treatment groups had some species that survived in the soil bank (S1 Table)

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Summary

Introduction

Human activities are changing Earth’s climate and biotic communities at an unprecedented rate, modifying species range limits and causing extinctions from local to global scale [1]. The global atmospheric concentration of ozone (O3) in the troposphere has risen from less than 10 ppb (parts per billion) a century ago to 40 ppb today and is projected to continue to increase at an annual rate of 1–2% [2,3]. Great efforts are being done in different. Historic ozone affects plant and arthropod communities

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