Early Agricultural Communities in Bengal were a group of Chalcolithic farmers, who first developed agriculture in Bengal. No archaeological evidence of large-scale agriculture in Bengal during the Neolithic period preceding the Chalcolithic or Copper Age. [1]
Early agricultural communities are not found in the whole region of Bengal (West Bengal and Bangladesh), they are found only in the south-western part of Bengal (West Bengal). [1]
Early agricultural communities were settled in the vast plain from the foothills of the Chota Nagpur Plateau to the Bhagirathi-Hooghly river. Evidence of paddy (rice) cultivation has been found in this region. As one moves eastward from the foothills of the plateau, there is evidence of more involvement of the communities in agriculture. The first agricultural communities of Bengal developed around 1500 BC [2] in this region mainly along the Mayurakshi, Ajay, Damodar, Kangsabati and Rupnarayan rivers. Initially, they were confined to the area of the Lalgarh Formation, but later moved east and southeast. [1]
Bengal's Early agricultural communities were found in the area bounded by the Ganges in the north, the Subarnarekha River and the Bay of Bengal in the south, and the Bhagirathi-Hooghly River in the east and the foothills of the Chotanagpur Plateau in the west. Most of their settlements are observed in Ajay and Damodar valleys. The settlement area can be divided into three parts according to topography and settlement age, namely - red soil area, old alluvial area and new alluvial area. [1]
Early agricultural communities first settled in this region. The main settlements here are Bharatpur, Mahishadal, Dihar, Haripur and Tulsipur. Rice grains have been identified with the domesticated species Oryza sativa , which indicates early agricultural communities were involved in rice cultivation. Archaeological finds from the settlements prove that hunting was one of the main means of livelihood of the agricultural communities of this region, along with agriculture. Apart from agriculture, animal husbandry was one of the mainstays of their livelihood. [1]
The region's economy remained largely unchanged throughout its thousand-year history. The main reason for the stagnation of the economy is probably the low fertility of the soil, and with it the low rainfall. As a result, the agricultural and hunter-gatherer civilizations developed by the early agricultural communities were able to produce the necessary resources for themselves, but it failed to build up sufficient resources for later stages of development and growth. So naturally the agrarian settlements in this region disappeared immediately before or after the historic period. [1]
The soil of this region was very fertile for rice cultivation and the rainfall was fairly good. The agricultural Communities of this area were more focused on agriculture than animal husbandry. [3] The residents were engaged in two different occupations. On the one hand their agrarian environment had developed an agricultural livelihood, which on the other hand their semi-urban environment forced them to cater to urban needs.
The archaeological sites excavated in the region are Pandu Rajar Dhibi (mound), Mangalkot, Baneshwardanga and Pokharna. Iron sickles from Pandu Rajar Dhibi (mound) and axes and adze discovered from Mangalkot provide evidence of agriculture and agricultural economy. The objects excavated from this area such as vases, large drinking vessels, small stone beads, ivory combs, lockets, beads, ear-rings, surma sticks etc. clearly indicate the civil life. [4]
This area is part of the plain delta region of Lower Bengal. The soil here was fairly viable for a stable agricultural economy. The settlements were mainly built on the banks of Bhagirathi and Rupnarayan rivers. The main settlement in this region is Tamralipta. [5]
A Chalcolithic (Copper Age) farming culture site has been discovered by University of Calcutta's Department of Archaeology at Erenda in coastal West Bengal, which was developed by Bengal's early agricultural communities. [6]
The Chalcolithic was an archaeological period characterized by the increasing use of smelted copper. It followed the Neolithic and preceded the Bronze Age. It occurred at different periods in different areas, but was absent in some parts of the world, such as Russia, where there was no well-defined Copper Age between the Stone and Bronze ages. Stone tools were still predominantly used during this period.
A paddy field is a flooded field of arable land used for growing semiaquatic crops, most notably rice and taro. It originates from the Neolithic rice-farming cultures of the Yangtze River basin in southern China, associated with pre-Austronesian and Hmong-Mien cultures. It was spread in prehistoric times by the expansion of Austronesian peoples to Island Southeast Asia, Madagascar, Melanesia, Micronesia, and Polynesia. The technology was also acquired by other cultures in mainland Asia for rice farming, spreading to East Asia, Mainland Southeast Asia, and South Asia.
The Hooghly River or popularly called Ganga or Kati-Ganga in the Puranas, is a river that rises close to Giria, which lies north of Baharampur and Palashi in Murshidabad. It is the western distributary of the Ganges. The main course of the Ganges then flows into Bangladesh as the Padma. A man-made canal, built in the 1960s and early-1970s at Farakka, connects the Ganges, flowing through Malda, to the Hooghly to bring the abundant waters of the Himalayan river to the comparatively narrow river that rises in eastern West Bengal.
The Hilly Flanks are the upland areas surrounding the Fertile Crescent of Southwest Asia, including the foothills of the Zagros Mountains, the Taurus Mountains, and the highland parts of the Levant. The Hilly Flanks foothill chain spans over 1000 miles, including parts of Turkey, northwestern Iraq, and western Iran. The region is just north of Mesopotamia, with similar characteristics of fertility with the added trait of foothills and plateaus.
Bardhaman, or sometimes Burdwan and Barddhaman, is a former district in the Indian state of West Bengal, headquartered in Bardhaman. On 7 April 2017, the district was bifurcated into two separate districts namely Purba Bardhaman and Paschim Bardhaman. It was the seventh most populous district in India at the time of bifurcation.
The Geography of West Bengal, a state in eastern India, is primarily defined by plains and plateaus, with the high peaks of the Himalayas in the north and the Bay of Bengal to the south.
Rarh region is a toponym for an area in the Indian subcontinent that lies between the Chota Nagpur Plateau on the West and the Ganges Delta on the East. Although the boundaries of the region have been defined differently according to various sources throughout history, it is mainly coextensive with the state of West Bengal, also comprising parts of the state of Jharkhand in India.
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Pandu Rajar Dhibi in the valley of the river Ajay is an Archaeological site in Ausgram II block in the Sadar North subdivision of Purba Bardhaman district in the Indian state of West Bengal. It was the first Chalcolithic site discovered in West Bengal. It was excavated by a team led by Paresh Chandra Dasgupta. The common man believes that the main mound at Pandu Rajar Dhibi is associated with King Pandu mentioned in the epic Mahabharata, hence the name came into being from the folklore.
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Ausgram II is a community development block. It is a municipality in Bardhaman Sadar North subdivision of Purba Bardhaman district in the Indian state of West Bengal.
Barsul is a village in Burdwan II CD block in Bardhaman Sadar North subdivision of Purba Bardhaman district in the state of West Bengal, India.
Purba Bardhaman district is in the Indian state of West Bengal. Its headquarters is in Bardhaman. It was formed on 7 April 2017 after the division of the previous Bardhaman district. Great revolutionary Rash Behari Bose was born in village Subaldaha in the district of Purba Bardhaman.
Bononabagram is a village in Ausgram I CD Block in Bardhaman Sadar North subdivision of Purba Bardhaman district in the Indian state of West Bengal.
The history of West Bengal basically refers to the history of the western part of Bengal, located in the eastern part of the Indian subcontinent. Evidence of human settlement has been found in West Bengal about 42,000 years ago. The presence of human settlement of that period has been found in the Ayodhya Hills of West Bengal. By 2,000 BCE, settled life had increasingly spread of human civilization in the Damodar-Ajay River Valley, which was contemporary with the Harappa-Mahenjodaro civilization. The southern part of West Bengal witnessed the presence of the Vanga Kingdom between 1100 BCE and 350 BCE, which was contemporary with the Vedic civilization of northern India.
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The Pandu culture is an archaeological culture from the chalcolithic period of India, spanning around 1600 BC to 750 BC. The type site is Pandu Rajar Dhibi, where black and red ware and tools made from bone and copper were found alongside remains of human body. It extends from the foothills of the Chota Nagpur Plateau to the Bhāgirathi-Hooghly river basin, covering a considerable part of southwestern or Rarh and coastal regions of modern-day West Bengal; from Birbhum in the north to Purba Medinipur in the south.