The beginning of the current interglacial period, the Holocene epoch, was a critical part of
the transition from glacial to interglacial climate conditions. This period, between about …

Tuning is a widespread technique to combine, date and interpret multiple fossil proxy
archives through aligning supposedly synchronous events between the archives. The …

The Holocene thermal maximum, a period of relatively warm climate between 11,000 and
5,000 years ago,, is most clearly recorded in the middle and high latitudes, of the Northern …

The 8.2 ka event was a period of abrupt cooling of 1–3° C across large parts of the Northern
Hemisphere, which lasted for about 160 yr. The original hypothesis for the cause of this …

An outstanding climate anomaly 8200 years before the present (BP) in the North Atlantic is
commonly postulated to be the result of weakened overturning circulation triggered by a …

Evidence from terrestrial, glacial, and global climate model reconstructions suggests that a
sea-level jump caused by meltwater release was associated with the triggering of the 8.2 ka …

A synthesis of well-dated high-resolution pollen records suggests a spatial structure in the
8200 cal yr BP event in northern Europe. The temperate, thermophilous tree taxa, especially …

Ensemble simulations have been performed with a climate model constrained to follow
temperature histories obtained from a recent compilation of 56 well‐calibrated surface …

Freshwater forcing has long been postulated as a catalyst for abrupt climate change
because of its potential to interfere with thermohaline circulation (THC). The most recent …

Deglaciation of the James Bay region was highly dynamic, with the occurrence of ice
(Cochrane) readvances into glacial Lake Ojibway around final deglaciation time, which …