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History of Mesopotamia

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Through Paleolithic, Iraq and Arabs

Short outline of Mesopotamia

Mesopotamia (Ancient Greek: Μεσοποταμία, romanized: Mesopotamíā; Classical Syriac: ܒܝܬ ܢܗܪ̈ܝܢ, lit. 'Bēṯ Nahrēn') means "Between the Rivers". The oldest known occurrence of the name Mesopotamia dates to the 4th century BC, when it was used to designate the area between the Euphrates and the Tigris. The name was presumably translated from a term already current in the area—probably in Aramaic—and apparently was understood to mean the land lying "between the (Euphrates and Tigris) rivers", now Iraq.

Later and in the broader sense, the historical region included not only the area of present-day Iraq, but also parts of present-day Iran, Syria and Turkey. The neighbouring steppes to the west of the Euphrates and the western part of the Zagros Mountains are also often included under the wider term Mesopotamia. A further distinction is usually made between Upper or Northern Mesopotamia and Lower or Southern Mesopotamia.

Upper Mesopotamia is the area between the Euphrates and the Tigris from their sources down to Baghdad. Lower Mesopotamia is the area from Baghdad to the Persian Gulf. In modern scientific usage, the term Mesopotamia often also has a chronological connotation. It is usually used to designate the area until the Arab Muslim conquests in the 7th century AD, with Arabic names like Syria, Jezirah and Iraq being used to describe the region after that date.

Chronology and periodization

Two types of chronologies can be distinguished: a relative chronology and an absolute chronology. The former establishes the order of phases, periods, cultures and reigns, whereas the latter establishes their absolute age expressed in years. In archaeology, relative chronologies are established by carefully excavating archaeological sites and reconstructing their stratigraphy – the order in which layers were deposited. In general, newer remains are deposited on top of older material. Absolute chronologies are established by dating remains, or the layers in which they are found, through absolute dating methods. These methods include radiocarbon dating, dendrochronology and the written record that can provide year names or calendar dates.

By combining absolute and relative dating methods, a chronological framework has been built for Mesopotamia that still incorporates many uncertainties but that also continues to be refined. In this framework, many prehistorical and early historical periods have been defined on the basis of material culture that is thought to be representative for each period. These periods are often named after the site at which the material was recognized for the first time, as is for example the case for the Halaf, Ubaid and Jemdet Nasr periods. When historical documents become widely available, periods tend to be named after the dominant dynasty or state; examples of this are the Ur III and Old Babylonian periods. While reigns of kings can be securely dated for the 1st millennium BC, there is an increasingly large error margin toward the 2nd and 3rd millennia BC.

The chronology for much of the third and second millennia BC is subject to much debate. Based on different estimates for the length of periods for which still very few historical documents are available, so-called Ultra-long, Long, Middle, Short and Ultra-short Chronologies have been proposed by various scholars, varying by as much as 150 years in their dating of specific periods. Despite problems with the Middle Chronology, this chronological framework continues to be used by many recent handbooks on the archaeology and history of the ancient Near East. A study from 2001 published high-resolution radiocarbon dates from Turkey supporting dates for the 2nd millennium BC that are very close to those proposed by the Middle Chronology.

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