Abstract

Bioturbation, the biogenic modification of sediments through particle reworking and burrow ventilation, is a key mediator of many important geochemical processes in marine systems. In situ quantification of bioturbation can be achieved in a myriad of ways, requiring expert knowledge, technology, and resources not always available, and not feasible in some settings. Where dedicated research programmes do not exist, a practical alternative is the adoption of a trait-based approach to estimate community bioturbation potential (BPc). This index can be calculated from inventories of species, abundance and biomass data (routinely available for many systems), and a functional classification of organism traits associated with sediment mixing (less available). Presently, however, there is no agreed standard categorization for the reworking mode and mobility of benthic species. Based on information from the literature and expert opinion, we provide a functional classification for 1033 benthic invertebrate species from the northwest European continental shelf, as a tool to enable the standardized calculation of BPc in the region. Future uses of this classification table will increase the comparability and utility of large-scale assessments of ecosystem processes and functioning influenced by bioturbation (e.g., to support legislation). The key strengths, assumptions, and limitations of BPc as a metric are critically reviewed, offering guidelines for its calculation and application.

Highlights

  • Marine soft-sediment habitats represent some of the most functionally important ecosystems on Earth, being characterized by a high biomass and diversity of invertebrate organisms that are fundamental to the mediation of a wealth of goods and services (Lotze et al 2006; White et al 2010; Widdicombe and Somerfield 2012)

  • Ecology and Evolution published by John Wiley & Sons Ltd

  • BPc accounts for two “fixed” traits (Ri and Mi) that are assumed to be directly related to life-history traits and activity levels of each species, that are not altered by context or spatiotemporal variation

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Summary

Introduction

Marine soft-sediment habitats represent some of the most functionally important ecosystems on Earth, being characterized by a high biomass and diversity of invertebrate organisms that are fundamental to the mediation of a wealth of goods and services (Lotze et al 2006; White et al 2010; Widdicombe and Somerfield 2012). Through bioturbation, that is, the mixing of sediment and particulate materials carried out during foraging, feeding and burrow maintenance activities, and the enhancement of pore water and solute advection during burrow ventilation (Richter 1936; Rhoads 1974; Volkenborn et al 2010) These processes influence oxygen, pH and redox gradients (Stahl et al 2006; Pischedda et al 2008; Queiros et al 2011), metal cycling (Teal et al 2009), sediment granulometry (Montserrat et al 2009), pollutant release (Gilbert et al 1994), macrofauna diversity (Volkenborn et al 2007), bacterial activity and composition (MermillodBlondin and Rosenberg 2006; Gilbertson et al 2012), and carbon (Kristensen 2001) and nitrogen cycling (Bertics et al 2010).

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