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・ Timeline of ichthyosaur research
・ Timeline of Igbo history
・ Timeline of Illyrian history
・ Timeline of immunology
・ Timeline of Imperial College School of Medicine
・ Timeline of imperialism
・ Timeline of Indian history
・ Timeline of Indianapolis
・ Timeline of Indo-Greek kingdoms
・ Timeline of Indonesian history
・ Timeline of entomology
・ Timeline of entomology since 1900
・ Timeline of entomology – 1800–50
・ Timeline of entomology – 1850–1900
・ Timeline of entomology – prior to 1800
Timeline of environmental history
・ Timeline of Essen
・ Timeline of Estonian history
・ Timeline of European exploration
・ Timeline of European Union history
・ Timeline of events associated with Anonymous
・ Timeline of events in Cyprus, 1974
・ Timeline of events in Hamilton, Ontario
・ Timeline of events in humanitarian relief and development
・ Timeline of events in the Cold War
・ Timeline of events in the Liberal Democrats leadership election, 2006
・ Timeline of events in the Liberal Democrats leadership election, 2007
・ Timeline of events leading to the American Civil War
・ Timeline of events preceding World War II
・ Timeline of events related to the South Thailand insurgency


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Timeline of environmental history : ウィキペディア英語版
Timeline of environmental history
The timeline lists events in the external environment that have influenced events in human history. This timeline is for use with the article on environmental determinism.
For the history of humanity's influence on the environment, and humanity's perspective on this influence, see timeline of the history of environmentalism.
See List of periods and events in climate history for a timeline list focused on climate.
==Pre-Holocene (1.5 Mya)==
The time from roughly 15,000 to 5,000 BC was a time of transition, and swift and extensive environmental change, as the planet was moving from an Ice age, towards an interstadial (warm period). Sea levels rose dramatically (and are continuing to do so), land that was depressed by glaciers began lifting up again, forests and deserts expanded, and the climate gradually became more modern. In the process of warming up, the planet saw several "cold snaps" and "warm snaps", such as the Older Dryas and the Holocene climatic optimum, as well as heavier precipitation. In addition, the Pleistocene megafauna became extinct due to environmental and evolutionary pressures from the changing climate. This marked the end of the Quaternary extinction event, which was continued into the modern era by humans. The time around 11,700 years ago (9700 BC) is widely considered to be the end of the old age (Pleistocene, Paleolithic, Stone age, Wisconsin Ice Age), and the beginning of the modern world as we know it.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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