Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic
Ocean may become seasonally ice-free by the year 2040 or even earlier. Putting this into …

While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

Abstract The Last Interglacial (LIG), a warmer period 130,000–116,000 years before present,
is a potential analogue for future climate change. Stronger LIG summertime insolation at …

Рассмотрены основные этапы развития работ по составлению Государственной
геологической карты России масштаба 1: 1 000 000, приложены справочные …

Observed Arctic sea ice losses are a sentinel of anthropogenic climate change. These
reductions are projected to continue with ongoing warming, ultimately leading to an ice-free …

As the planet cooled from peak warmth in the early Cenozoic, extensive Northern
Hemisphere ice sheets developed by 2.6 Ma ago, leading to changes in the circulation of …

Sediment cores from the western Arctic Ocean obtained on the 2005 HOTRAX and some
earlier expeditions have been analyzed to develop a stratigraphic correlation from the …

Following early hypotheses about the possible existence of Arctic ice shelves in the past,–,
the observation of specific erosional features as deep as 1,000 metres below the current sea …

New sediment cores were recovered along two transects from the Canada Basin across the
central Mendeleev Ridge towards the Makarov Basin and the Lomonosov Ridge in the …

Рассмотрены основные этапы развития работ по составлению Государственной
геологической карты Российской Федерации масштаба 1: 1 000 000 …