Origins of agriculture
Techniques of research used.
Many regions around the globe have seen agriculture develop independently. This was the first major change in the relationship between modern humans and their environment. Humans evolved to their present form around 200,000 years ago (see human evolutionary). However, they didn’t begin farming until 15,000-11,000 years before the present (BP). Archaeology is the best source of data to study the history of agriculture. This is because humans altered wild habitats in productive ways before they invented unambiguous writing systems. It happened in Southwest Asia around 5100 BP, and East Asia approximately 3000 BP.
Radiocarbon dating offers a chronometric framework to archaeological research. Radiocarbon analysis used large amounts of material before the 1980s. Because of their robust size and unique composition, animal bones have been a reliable source for samples for radiocarbon analysis. Faunal remains are routinely tested for morphological, genetic and biochemical analysis.
While it might seem that plant remains have been lost in the archaeological records, there are often small amounts of charred plants found in ancient hearths or middens. Charring preserves the material and allows for identification by genus, species, and other qualitative or quantitative analysis forms. Archaeologists usually recover plant materials by placing the sediments from pits or hearths in water. The plant remains then float to the surface where they can be retrieved. Archaeologists had to date plants indirectly because they have smaller and more fragile remains than animals. This was because the plant remains were not found in the sediments. Radiocarbon dating has become more common and can date small amounts of material such as a single seed. Direct dating of plant remains replaced the old indirect methods in serious research on the origins and evolution of agriculture.
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Picture Credit:- https://www.slideshare.net/MauCudiamat/palynology-pollen-morphology-and-biology |
Palynology, the study of pollen and phytolith analysis, can provide additional information about plant domestication. Phytoliths can be described as tiny silica bodies produced by many plants. Each phytolith forms within a cell of a plant to provide support for the structure. Each phytolith keeps the original shape of the cell it was created in, which may be very specific to one type of plant. Starch grains also have a distinctive appearance and can be preserved for long periods. These can often be found on the surface of pots or stone tools, and they are often the only way for food to be identified, such as potatoes. An archaeologist can gain additional information about the plants growing near or on archaeological sites by identifying and quantifying their pollen, phytoliths, starch grains, and other elements found in archaeological sediments.
Knowledge Source:- www.britannica.com
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