Reviews and syntheses: <sup>210</sup>Pb-derived sediment and carbon accumulation rates in vegetated coastal ecosystems – setting the record straight

Abstract

<p><strong>Abstract.</strong> Vegetated coastal ecosystems, including tidal marshes, mangroves and seagrass meadows, are being increasingly assessed in terms of their potential for carbon dioxide sequestration worldwide. However, there is a paucity of studies that have effectively estimated the accumulation rates of sediment organic carbon (<span class="inline-formula"><i>C</i>_org</span>), also termed blue carbon, beyond the mere quantification of <span class="inline-formula"><i>C</i>_org</span> stocks. Here, we discuss the use of the <span class="inline-formula">²¹⁰Pb</span> dating technique to determine the rate of <span class="inline-formula"><i>C</i>_org</span> accumulation in these habitats. We review the most widely used <span class="inline-formula">²¹⁰Pb</span> dating models to assess their limitations in these ecosystems, often composed of heterogeneous sediments with varying inputs of organic material, that are disturbed by natural and anthropogenic processes resulting in sediment mixing and changes in sedimentation rates or erosion. Through a range of simulations, we consider the most relevant processes that impact the <span class="inline-formula">²¹⁰Pb</span> records in vegetated coastal ecosystems and evaluate how anomalies in <span class="inline-formula">²¹⁰Pb</span> specific activity profiles affect sediment and <span class="inline-formula"><i>C</i>_org</span> accumulation rates. Our results show that the discrepancy in sediment and derived <span class="inline-formula"><i>C</i>_org</span> accumulation rates between anomalous and ideal <span class="inline-formula">²¹⁰Pb</span> profiles is within 20<span class="thinspace"></span>% if the process causing such anomalies is well understood. While these discrepancies might be acceptable for the determination of mean sediment and <span class="inline-formula"><i>C</i>_org</span> accumulation rates over the last century, they may not always provide a reliable geochronology or historical reconstruction. Reliable estimates of <span class="inline-formula"><i>C</i>_org</span> accumulation rates might be difficult at sites with slow sedimentation, intense mixing and/or that are affected by multiple sedimentary processes. Additional tracers or geochemical, ecological or historical data need to be used to validate the <span class="inline-formula">²¹⁰Pb</span>-derived results. The framework provided in this study can be instrumental in reducing the uncertainties associated with estimates of <span class="inline-formula"><i>C</i>_org</span> accumulation rates in vegetated coastal sediments.</p>