Seasonal sea-surface temperature variability for the Neoglacial (3300–2500BP) and Roman
Warm Period (RWP; 2500–1600BP), which correspond to the Bronze and Iron Ages …

Seasonal sea-surface temperature (SST) variability during the Medieval Climate Anomaly
(MCA), which corresponds to the height of Viking exploration (800–1200AD), was estimated …

The margins of mainland Europe, and especially those areas coming under the influence of
North Atlantic weather systems, are ideally placed to record changing palaeoclimates. Cores …

We present pollen records from three sites in south Westland, New Zealand, that document
past vegetation and inferred climate change between approximately 30,000 and 15,000 cal …

The presence of marl deposits belonging to the Lateglacial period in a former lake basin at
Lundin Tower in Fife, Scotland has allowed palaeoenvironmental investigations by means of …

The temporal relationship between rapid climate shifts in the Northern and Southern
Hemispheres at the end of the last glacial is crucial to understanding how the global climate …

The pedology and the isotope geochemistry of the early Middle Pleistocene interglacial
'rootlet bed'at Pakefield, eastern England, record the climate when this unit accumulated …

A pollen‐based quantitative climate reconstruction from a lake‐sediment core on the
Norwegian Barents Sea coast provides insights about climatic change over the Greenland …

Palynological and coleopteran data are described from a section through Late Devensian
(Weichselian) deposits at Gransmoor, East Yorkshire, England. The pollen evidence shows …

A multi-proxy environmental record for the Devensian (Weichselian) Lateglacial and early
Holocene periods, which includes pollen, plant macrofossil, coleopteran, geochemical and …