The Transition from the Pleistocene to the Holocene and its Impact on Hunter-Gatherer Societies
TLDR The transition from the Pleistocene to the Holocene brought about significant changes in the environment, including rising sea levels, which affected hunter-gatherer societies across different regions of the world. The Younger Dryas, an extreme climatic event, further forced these societies to adapt to colder temperatures and changing precipitation patterns, leading to shifts in population and lifestyle.
Timestamped Summary
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10,000 years ago, people in the marshlands lived off the abundant resources of the land and sea, but the rising sea levels caused by melting ice threatened to submerge their home.
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This section provides an overview of the different regions of the world during the transition from the Pleistocene to the Holocene, including the Americas, Beringia, Japan, North China, Southeast Asia, and Australia, and how these regions were inhabited by hunter-gatherer societies before being affected by rising sea levels.
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During the transition from the Pleistocene to the Holocene, the Indian subcontinent did not yet have the monsoon rhythms, the Himalayas were more imposing, the Thar desert was larger and harsher, the fertile Crescent was a prosperous place for hunter-gatherers, the Sahara Desert was even larger and more desolate, Sub-Saharan Africa was drier, and in Europe, the ice sheets were receding and people were following them, setting up encampments along rivers and shorelines.
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Our understanding of global climatic trends must account for the complex effects of temperature, precipitation, humidity, and air pressure on the environment, as well as the variability over small spaces and times, in order to understand how people interact with their surroundings, such as in Europe where the mammoth steppe was a landscape suited to mobile bands of hunters who specialized in tracking large herds of animals, and as the ice receded and plants began to cover the land, the animals and people followed.
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The Younger Dryas was an extreme climatic event that occurred around 12,800 years ago, causing a dramatic cold snap and forcing people living across the northern hemisphere to adapt quickly to the colder temperatures and changing precipitation patterns.
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The Younger Dryas was likely caused by a combination of factors, including glacial meltwater, a volcanic eruption, and extraterrestrial impacts, which led to a global cooling event and major regional variations in the climate record, ultimately affecting the lives of the Magdalenean and post-Magdalenean hunter-gatherers.
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The onset of the Younger Dryas led to a dramatic shift in the available food resources for hunter-gatherers, forcing them to adapt their hunting and foraging strategies, resulting in a decrease in population and a change in lifestyle in Europe, particularly in Central Europe.
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During the Younger Dryas, people in Central Europe had to adapt to a tougher environment by intensively exploiting their surroundings, becoming better fishermen, using less specialized stone tools, and not staying in one place for too long, but eventually, the climate shifted again and the Holocene began, bringing about the Mesolithic era.
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The Mesolithic people of Europe, known as the Western Hunter-Gatherers, repopulated Western Europe after the Younger Dryas, and their ancestry can still be found in people living in Western Europe today.
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Mesolithic people in Europe used microliths, small sharp flakes of stone, as a modular technology that could be used for various purposes, making their toolkit diverse and adaptable for hunting and gathering different food resources.
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Doggerland, a rich wetland environment between Britain and the low countries, was eventually submerged by rising seas and then devastated by a megatsunami, leading to the disappearance of the mesolithic way of life in that region.
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