Abstract

AbstractReduction of body size is a common response of organisms to environmental stress. Studying the early Toarcian succession in the Lusitanian Basin of Portugal, we tested whether the shell size of benthic marine communities of bivalves and brachiopods changed at and before the global, warming–related Toarcian oceanic anoxic event (T-OAE). Statistical analyses of shell size over time show that the mean shell size of communities decreased significantly before the T-OAE. This trend is distinct in brachiopods and is caused by larger-sized species becoming less abundant over time, whereas it is not significant in bivalves, suggesting a decoupled response to environmental stress. Reductions in shell size precede the decline in standardized sample-level species richness associated with the early Toarcian extinction event. Such decreases in the shell size of marine invertebrates, well before the onset of biodiversity change, suggest that reductions in body size more generally may be a precursor of a subsequent loss of species and turnover at the community level caused by climate change. Sedimentological evidence is against hypoxia as a driver of extinction and the preceding size decrease in the brachiopod fauna in the studied succession, although low oxygen levels are widely held responsible for elevated early Toarcian extinction rates globally. Reduction of mean shell size in brachiopods but stasis in bivalves is difficult to explain with ocean acidification, because experimental work shows that brachiopods can be resilient to lowered pH, albeit long-term metabolic costs and potential evolutionary adaptations are unknown. Rising early Toarcian temperatures in the Lusitanian Basin seem to be a plausible factor in both diversity decline associated with the T-OAE and the preceding reductions in mean shell size, because thermal tolerances in modern bivalves are among the highest within marine invertebrates.

Highlights

  • Global warming and stressors associated with climate change—in particular hypoxia, oceanic acidification, and hypercapnia—have raised concerns over the degradation and transformation of marine ecosystems

  • In this study we focus on changes in the body size of benthic marine organisms before the Toarcian oceanic anoxic event (T-OAE)

  • The upper part is characterized by high abundances of a single species, the brachiopod Soaresirhynchia bouchardi, which has been interpreted as a disaster taxon (Gahr 2002; Baeza-Carratalá 2013)

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Summary

Introduction

Global warming and stressors associated with climate change—in particular hypoxia, oceanic acidification, and hypercapnia—have raised concerns over the degradation and transformation of marine ecosystems. The relative role of these factors is still uncertain in both present and past biotic crises. One such crisis interval that has received increased attention is the early Toarcian oceanic anoxic event (T-OAE; ∼183 Ma). It marks a global, second-order mass extinction that affected both benthic and nektonic marine species, as well as terrestrial species (e.g., Wignall and Bond 2008; Morten and Twitchett 2009; Mattioli et al 2009; Martindale and Aberhan 2017). Most likely the ultimate cause of the biotic crisis was intense volcanic activity during the placement of the Karoo-Ferrar Large Igneous Province (Pálfy and Smith 2000), possibly coupled with warming- related methane

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