The Evolution of Bioturbation
In order to resolve the ecological-environmental feedbacks that accompanied the emergence of animal-dominated seafloor ecosystems, we use the sedimentary and trace fossil records to investigate the evolution of infaunal (sediment-dwelling) animals and bioturbating (burrowing and sediment-mixing) behaviors. The radiation of bioturbating animals is frequently invoked as the trigger for a myriad of geochemical, ecological and preservational phenomena associated with the Cambrian Explosion, such as oxygenation of the seafloor and deep ocean and the closing of several key windows of exceptional fossilization. However, the evolution of the mixed layer—the zone of sediments physically and chemically homogenized by burrowing animals and the zone which is mechanistically most responsible for the ecological, biogeochemical and preservational impact of bioturbation—has, historically, been poorly constrained. Our recent field-based sedimentological and paleontological work, coupled with geochemical modeling, has indicated that the development of the sedimentary mixed layer was a protracted process. The implementation of efficient sediment-mixing behaviors lagged behind both the Cambrian Explosion and the Great Ordovician Biodiversification Event, and the delayed development of bioturbation directly impacted marine sulfate concentrations and the rheology of the early Paleozoic seafloor (Tarhan et al., 2015, Nature Geoscience; Tarhan, 2018, Geology; Tarhan, 2018, Earth-Science Reviews; Tarhan and Droser, 2014, Palaeo-3), and may have facilitated enhanced phosphorus recycling and productivity, thus spurring greater ecosystem complexity and ocean-atmosphere oxygenation (Tarhan et al., 2021, EPSL; Zhao et al., 2020, Nature Communications). Bioturbation was also remarkably heterogeneous across seafloor environments (Tarhan et al., 2023, Geobiology).

Lower-middle Cambrian trace fossil assemblages and ichnofabrics.
From Tarhan, 2018, Earth-Science Reviews
Cambro-Ordovician trace fossil assemblages and ichnofabrics.
From Tarhan, 2018, Earth-Science Reviews
Changes in ichnofabric index (a metric for the extent to which sedimentary fabrics are disrupted by bioturbation) through the lower Paleozoic. Although bioturbation increased in intensity through this interval, levels of sedimentary disruption were still far below those experienced by the seafloor today.
From Tarhan, 2018, Earth-Science Reviews
Modern bioturbators strongly shape, or ‘engineer’ marine sulfur cycling. The lower Paleozoic record of bioturbation can be incorporated into biogeochemical models to predict the influence ancient bioturbators would have had on contemporaneous sulfur cycling.
From Tarhan et al., 2015, Nature Geoscience



Sole marks, formed by currents and current-laden particles gouging the seafloor. These structures can only form when sediments are cohesive and poorly bioturbated. Powers Steps Formation, Bell Island, Newfoundland.



A survey of the sedimentological, tectonic and paleontological literature indicates that the frequency of sole mark preservation in shallow marine settings has declined through the Phanerozoic, likely due to increasing intensities of bioturbation.
From Tarhan, 2018, Geology



















Study of Cambrian-Ordovician strata of Newfoundland indicate pronounced variability in bioturbation across marine paleoenvironments; in cases environmental heterogeneity exceeds the scale of evolutionary changes in bioturbation intensity. From Tarhan et al., 2023, Geobiology
Diagenetic modeling of the impact of different styles and intensities of bioturbation on phosphorus cycling indicates that bioirrigation (solute transport; e.g., via open burrows) and biodiffusion (sediment-mixing) can have diametrically opposed effects on seafloor phosphorus burial. This suggests that early Paleozoic bioirrigation-dominated bioturbation may have enhanced nutrient cycling and productivity. From Tarhan et al., 2021, EPSL