Research news on Pleistocene

The Pleistocene is a geologic epoch within the Quaternary Period, spanning roughly 2.58 million to 11,700 years ago, characterized by repeated glacial–interglacial cycles driven by orbital (Milankovitch) forcing and associated feedbacks in the climate system. It encompasses major expansions of continental ice sheets in the Northern Hemisphere, large sea-level fluctuations, and pronounced shifts in atmospheric composition and global temperature. Stratigraphically, its base is defined near the Gauss–Matuyama magnetic reversal, and its end is marked by the transition to the Holocene following the last glacial termination. The Pleistocene is critical for understanding late Cenozoic climate dynamics and associated environmental changes.

Taimering mammoth was likely butchered by hunters and gatherers

The wooly mammoth from Taimering (Bavaria, Germany), discovered in 2020, was buried in a former Ice Age pond after its death. Pollen findings and radiocarbon dating confirm that the mammoth lived and died during the harsh ...

Ancient iceberg scratches reveal reverse Great Lakes snowbelt

Buffalo's legendary snowfall totals are largely the result of one unlucky geographic reality: the city sits east of the Great Lakes instead of west. Anyone who has lived through a winter in Buffalo, Cleveland or any snowbelt ...

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