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The Holocene and the preceding Pleistocene [5] together form the Quaternary period. The Holocene is an interglacial period within the ongoing glacial cycles of the Quaternary, and is equivalent to Marine Isotope Stage 1. The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth's obliquity.
The dates for each age can vary by region. On the geologic time scale, the Holocene epoch starts at the end of the last glacial period of the current ice age (c. 10,000 BC) and continues to the present. The beginning of the Mesolithic is usually considered to correspond to the beginning of the Holocene epoch.
Holocene glacial retreat, the present Holocene or Postglacial period begins 9400: Pre-Boreal sharp rise in temperature over 50 years (B-S), precedes Boreal 8500–6900: Boreal (B-S), rising sea levels, forest replaces tundra in northern Europe 7500–3900: Neolithic Subpluvial/African humid period in North Africa, wet 7000–3000
The current interglacial is known as the Holocene epoch. [1] ... Stages), but it has been difficult to coordinate stages using just land-based evidence before that ...
Marine Isotope Stage (MIS) 5e, called the Eemian (Ipswichian in Britain) around 124,000–119,000 years ago, was the last interglacial period before the present (Holocene), and compared global mean surface temperatures were at least 2 °C (3.6 °F) warmer.
The Holocene Climate Optimum (HCO) was a warm period in the first half of the Holocene epoch, ... immediately before the Industrial Revolution, ...
This is taken as the beginning of the Holocene geological epoch. 9600 BC: Jericho has evidence of settlement dating back to 9,600 BC. Jericho was a popular camping ground for Natufian hunter-gatherer groups, who left a scattering of crescent microlith tools behind them.
The list is divided into four categories, Middle Paleolithic (before 50,000 years ago), Upper Paleolithic (50,000 to 12,500 years ago), Holocene (12,500 to 500 years ago) and Modern (Age of Sail and modern exploration).