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Burrowing crab effects across a tidal marsh successional chronosequence located along Mississippi sound
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Burrowing crab effects across a tidal marsh successional chronosequence located along Mississippi sound

Shelby Rinehart, Morgan Sharbaugh, Julia Cherry and Jacob Dybiec
27 May 2025
url
https://doi.org/10.5061/dryad.vhhmgqp3rView
DataCC0 V1.0 Open

Abstract

bioturbation facilitation FOS: Earth and related environmental sciences Mutualism Restoration ecology stress gradient hypothesis zoogeochemistry
Burrowing crab engineers can affect the biological structure and sediment conditions of their environments. However, it is challenging to predict when and where burrow effects will manifest, as they are often site- and habitat-specific. We used a tidal marsh restoration chronosequence to explore crab burrow effects on plant communities (e.g., percent cover, biomass, stem heights) and sediment characteristics (e.g., bulk density, organic matter, carbon and nitrogen stocks) through early succession. In a field survey, we compared plants and sediments between plots with high and low crab burrow densities within three habitat zones: mud flat (i.e., 0-1 years old), young marsh (i.e., ~1-6 years old), and old marsh (i.e., ~6+ years old). In a manipulative experiment, we tested the physical effects of crab burrows on plants and sediments at the mud flat-young marsh ecotone using burrow mimics. In our field survey, crab burrow density did not influence plants or sediments. Rather, plant biomass and stem heights, as well as sediment bulk density, organic matter, carbon, and nitrogen, differed between habitat zones, following expected marsh successional trajectories of development over time. However, in our manipulative experiment, crab burrow mimics had a strong positive effect on plants at the ecotone, suggesting crab burrows can facilitate plant expansion into unvegetated mud flats. Thus, crab burrow effects appear to peak in early successional ecotones where burrowing mediates environmental stressors and promotes vegetative growth, with implications for the recovery of biological structure and sediment properties following restoration.

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