Abstract. 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
(Corg), also termed blue carbon, beyond the mere quantification
of Corg stocks. Here, we discuss the use of the 210Pb
dating technique to determine the rate of Corg accumulation in
these habitats. We review the most widely used 210Pb 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
210Pb records in vegetated coastal ecosystems and evaluate how
anomalies in 210Pb specific activity profiles affect sediment and
Corg accumulation rates. Our results show that the discrepancy in
sediment and derived Corg accumulation rates between anomalous
and ideal 210Pb profiles is within 20 % if the process causing
such anomalies is well understood. While these discrepancies might be
acceptable for the determination of mean sediment and Corg
accumulation rates over the last century, they may not always provide a
reliable geochronology or historical reconstruction. Reliable estimates of
Corg 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 210Pb-derived
results. The framework provided in this study can be instrumental in reducing
the uncertainties associated with estimates of Corg accumulation
rates in vegetated coastal sediments.