Abstract

With carbon dioxide (CO2) levels rising dramatically, climate change threatens marine environments. Due to increasing CO2 concentrations in the ocean, pH levels are expected to drop by 0.4 units by the end of the century. There is an urgent need to understand the impact of ocean acidification on chemical-ecological processes. To date, the extent and mechanisms by which the decreasing ocean pH influences chemical communication are unclear. Combining behaviour assays with computational chemistry, we explore the function of the predator related cue 2-phenylethylamine (PEA) for hermit crabs (Pagurus bernhardus) in current and end-of-the-century oceanic pH. Living in intertidal environments, hermit crabs face large pH fluctuations in their current habitat in addition to climate-change related ocean acidification. We demonstrate that the dietary predator cue PEA for mammals and sea lampreys is an attractant for hermit crabs, with the potency of the cue increasing with decreasing pH levels. In order to explain this increased potency, we assess changes to PEA’s conformational and charge-related properties as one potential mechanistic pathway. Using quantum chemical calculations validated by NMR spectroscopy, we characterise the different protonation states of PEA in water. We show how protonation of PEA could affect receptor-ligand binding, using a possible model receptor for PEA (human TAAR1). Investigating potential mechanisms of pH-dependent effects on olfactory perception of PEA and the respective behavioural response, our study advances the understanding of how ocean acidification interferes with the sense of smell and thereby might impact essential ecological interactions in marine ecosystems.

Highlights

  • IntroductionDevelopment and physiology in many marine ecosystems (Hay 2009)

  • Chemical signalling mediates behaviour, development and physiology in many marine ecosystems (Hay 2009)

  • We explore the effect of ligand protonation on the receptor binding using quantum chemical calculations

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Summary

Introduction

Development and physiology in many marine ecosystems (Hay 2009). The chemical marine environment is changing rapidly due to ocean acidification (Doney et al 2009). The continuing uptake of atmospheric carbon dioxide (CO2) into. 3 E.A. Milne Centre for Astrophysics, G.W. Gray Centre for Advanced Materials, Department of Physics and Mathematics, University of Hull, Hull, HU6 7RX, UK the ocean changes the seawater carbonate chemistry and reduces the pH. Global average ocean pH has already decreased by more than 0.1 since pre-industrial times to pH 8.1 and is predicted to drop further to pH 7.7 by the end of the century (Bopp et al 2013; IPCC 2014)

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