Iceland was heavily glaciated at the Last Glacial Maximum–glaciers extended towards the
shelf break. Ice thickness reached 1,500±500 m. The rapid deglaciation, starting 17.5–15.4 …

During the latter part of the 20th century research effort in studies of the Weichselian history
of Iceland was intensified and about a decade ago three papers appeared, providing a good …

A high-resolution late-Holocene sea-level record is produced from salt-marsh deposits at
Vioarhólmi in Snæfellsnes, western Iceland. The stratigraphy of Vioarhólmi saltmarsh is …

Bird migration systems must have changed dramatically during the glacial-interglacial cycles
of the Pleistocene and as novel habitats became available since the last glacial maximum …

The mid-Pliocene warming episode is well established along the margins of the North
Atlantic and probably affected areas as far north as Iceland. Rich marine mollusc faunas …

Understanding the patterns, causes, and consequences of biotic interchange—the
movement of species between neighboring biotas—is crucial for evaluating the effects of …

New geomorphic and chronological data of Holocene advances of the Drangajökull Ice Cap,
located on eastern Vestfirðir, northwest Iceland, are presented. At least two glacial advances …

We investigated the biogeography of benthic foraminifera in a highly urbanized tropical
seascape, ie Hong Kong, in order to assess their utility as bioindicators relative to other …

The 5900 BP Helgafell eruption started with an intense fire-fountaining phase that deposited
scoria and spatter near the vent. Spatter accumulated, agglutinated, and was subsequently …

Coarse-grained chenier ridges contain abundant mollusc shells that help to reconstruct the
evolution of marine ecosystems throughout the Holocene, but few temperate environments …