Active layer probing in northern Sweden, northeast Greenland, and central Svalbard
indicates active layer thickening has occurred at Circumpolar Active Layer Monitoring …

The last glacial cycle began around 116,000 years before present during a period with low
incoming solar radiation in Northern Hemisphere summer. Following the glacial inception in …

Abstract The Eemian (the Last Interglacial; ca. 129–116 thousand years ago) presents a
testbed for assessing environmental responses and climate feedbacks under warmer-than …

Abstract The Last Interglacial warm period, the Eemian (ca. 130–116 thousand years ago),
serves as a reference for projected future climate in a warmer world. However, there is a …

Abstract The Last Interglacial (LIG; 130–115 ka) is an important test bed for climate science
as an instance of significantly warmer than preindustrial global temperatures. However, LIG …

The ongoing reduction of Arctic sea ice underscores the need to understand the drivers
behind sea ice variability and associated ocean-climate impacts. The Last Interglacial …

Abstract The northeastern Fram Strait at the entrance to the Arctic Ocean represents a key
observatory for sea ice reconstructions as it sensitively reacts to environmental changes. A …

Reconstructing interglacial marine environments helps us understand the climate change
mechanisms of the past. To contribute to this body of knowledge, we studied a high …

Комплексное детальное изучение (литология, микропалеонтология, палинология)
толщи морских осадков мощностью 455 см, залегающих на морене московского …

Based on sedimentological, isotope-geochemical, and micropaleontological parameters of
bottom sediments of the AMK-5188 core, differences in the natural environment of the last …