Epipalaeolithic sites are more numerous, better preserved, and can be accurately radiocarbon dated. The period coincides with the gradual retreat of glacial climatic conditions between the Last Glacial Maximum and the start of the Holocene, and it is characterised by population growth and economic intensification.[2] The Epipalaeolithic ended with the "Neolithic Revolution" and the onset of domestication, food production, and sedentism, although archaeologists now recognise that these trends began in the Epipalaeolithic.[5][6]