Depositional and post‐depositional controls on magnetic signals from saltmarshes on the north‐west coast of Ireland

Abstract

Magnetic measurements were carried out on samples from two saltmarshes deposited during the last century on the north‐west coast of Ireland. Based on profiles from cliffed saltmarsh edge, mid‐marsh and supratidal locations, the processes that affect the generation and persistence of magnetic properties in environments were investigated. This was done to help in understanding the geochemical processes affecting north‐west Irish coast saltmarshes and to determine the frequency and provenance of sediment‐laden flooding events; hence, disentangling the importance of clastic and organic contributions to saltmarsh growth. Magnetic properties indicate depositional and post‐depositional effects varying on both temporal and spatial scales. The interpretations presented here suggest that both biogenic and diagenetic processes have a strong effect on the magnetic properties recorded: in the former case, the growth of magnetotactic bacteria is the main process; in the latter case, it is reductive diagenesis, associated with organic matter decomposition, that is important. The biogenic and diagenetic effects overprint and degrade the detrital magnetic signatures respectively. This suggests that magnetic measurements within the context of north‐west Irish coast saltmarshes can provide limited information on clastic sediment input to these environments. Comparisons between sites on the north‐west coast of Ireland show similar magnetic properties, despite differences in deposition rates, implying that significant post‐depositional alteration of magnetic properties occurs within the first 20–40 years after deposition. Magnetic properties of north‐west coast Irish saltmarshes are put into a regional context by comparison with magnetic profiles from similar sites.