We investigated the utility of foraminifera, testate amoebae and bulk-sediment δ 13 C
measurements for reconstructing Holocene relative sea level from sequences of salt-marsh …

Salt-marsh foraminifera are routinely used as sea-level indicators since their vertical
distribution is closely linked with elevation relative to the tidal frame. The precise nature of …

Salt-marsh foraminifera are frequently used around the world as proxies in
paleoenvironmental studies of sea-level change. Quantitative reconstructions of sea-level …

We described the distributions of foraminifera from ten physiographically distinct salt
marshes in the Albemarle–Pamlico estuarine system, North Carolina using 193 surface …

We investigated the influence of inter-annual and seasonal differences on the distribution of
live and dead foraminifera, and the inter-annual variability of stable carbon isotopes (δ13C) …

We assessed the utility of δ13C and bulk geochemistry (total organic content and C: N) to
reconstruct relative sea-level changes on the Cascadia subduction zone through …

Three biofacies were recognized in samples collected at a depth of 10cm along three
transects from the marshes of the Fraser River delta, British Columbia. These biofacies …

We investigated foraminiferal distributions from two salt-marsh sites at Thunderbolt and
Georgetown, in mainland northern Georgia, US Atlantic coast. We analyzed modern …

We investigated foraminiferal distributions from two salt-marsh sites at Thunderbolt and
Georgetown, in mainland northern Georgia, US Atlantic coast. We analyzed modern …

Late Holocene salt-marsh sediments allow the reconstruction of pre-industrial relative sea-
level changes. Typically, reconstructions are derived by quantifying a relationship between …