Local sea-level changes differ significantly from global-mean sea-level change as a result of
(1) non-climatic, geological background processes;(2) atmosphere/ocean dynamics; and (3) …

We assess the relationship between temperature and global sea-level (GSL) variability over
the Common Era through a statistical metaanalysis of proxy relative sea-level …

We produced∼ 3000-year long relative sea-level (RSL) histories for two sites in North
Carolina (USA) using foraminifera preserved in new and existing cores of dated salt-marsh …

While there is scientific consensus that global and local mean sea level (GMSL and LMSL)
has risen since the late nineteenth century, the relative contribution of natural and …

Abstract The Atlantic coast of North America north of Cape Hatteras has been proposed as a
“hotspot” of late 20th century sea‐level rise. Here we test, using salt‐marsh proxy sea‐level …

Salt-marsh sediments provide precise and near-continuous reconstructions of Common Era
relative sea level (RSL). However, organic and low-density salt-marsh sediments are prone …

Proxy records of late Holocene relative sea‐level changes are important for our
understanding of mechanisms that drive contemporary sea‐level trends. In the Gulf of Saint …

Climate change, of which sea level change is one component, is seldom out of the news.
This paper reviews developments in the measurement and understanding of changes in sea …

Salt-marsh sediments are routinely used to reconstruct sea-level changes over past
millennia. These reconstructions bridge an important gap between geological and …

Compaction describes a range of natural syn-and post-depositional processes that reduce
the volume of sediments deposited in low-lying coastal areas, causing land-level lowering …