Vioarhólmi in Snæfellsnes, western Iceland. The stratigraphy of Vioarhólmi saltmarsh is
documented using detailed descriptions of ten exposed sections and numerous hand-drilled
cores. Fossil foraminifera are used as proxy sea-level indicators in an exposed section of
salt-marsh peat. The agglutinated foraminifera Jadammina macrescens and
Paratrochammina (Lepidoparatrochammina) haynesi are most useful as sea-level indicators …