Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

Abstract The Last Interglacial (LIG, 129–116 thousand of years BP, ka) represents a test bed
for climate model feedbacks in warmer-than-present high latitude regions. However, mainly …

• The sustained rate of increase over the past century in the combined radiative forcing from
the three well-mixed greenhouse gases carbon dioxide (CO2), methane (CH4), and nitrous …

Observation-based reconstructions of sea surface temperature from relatively stable periods
in the past, such as the Last Glacial Maximum, represent an important means of constraining …

Paleoclimatic reconstructions have provided a unique data set to test the sensitivity of
climate system to changes in atmospheric CO2 concentrations. However, the mechanisms …

This paper documents the migration of the Polar Front (PF) over the Iberian margin during
some of the cold climatic extremes of the last 45 ka. It is based on a compilation of robust …

The transition from last glacial to deglacial and subsequently to modern interglacial climate
conditions was accompanied by abrupt shifts in the palaeoceanographic setting in the …

Mg/Ca palaeothermometry in foraminiferal calcite is a widely applied tool in
palaeoceanography. However, our understanding of the effects of planktic foraminiferal …

Heinrich events, identified as enhanced ice-rafted detritus (IRD) in North Atlantic deep sea
sediments (Heinrich, 1988; Hemming, 2004) have classically been attributed to Laurentide …

Publisher Summary Transfer functions, in a broad sense, are powerful methods that allow
complex biological assemblages analyzed by micropaleontologists to be translated into …