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• W3126449591 endingPage "106825" @default.
• W3126449591 startingPage "106825" @default.
• W3126449591 abstract "Agriculture is a major contributor to the economic development of modern as well as ancient India and largely depends on the rainfall in the monsoon season. In order to understand the impact of climate variability on cultural changes in the Indian subcontinent, high resolution centennial to millennial scale middle Holocene Indian summer monsoon (ISM) variability was reconstructed from Bednikund lake, located in an alpine meadow of the Pindar basin, Chamoli, Central Himalaya. Increased ISM precipitations were found during ∼5930-3950 (mid-Holocene climate optimum), ∼3380–2830 (Minoan Warm Period), ∼2610–1860 (Roman Warm Period), ∼1050–760 (Medieval Climate Anomaly), and ∼320 cal yr BP to Present (Current Warm Period). The decreased ISM strengths were found during ∼3950-3380, ∼2830–2610, ∼1860–1050 (Dark Ages Cold Period), ∼760–580, and ∼500-320 cal yr BP (Little Ice Age). The covariance between our records of precipitation change and total solar irradiance for the middle to late Holocene and with Northern hemisphere (NH) temperature for the past two millennia suggested solar insolation as a primary forcing mechanism of ISM variability. The reconstructed paleoclimate combined with archaeology and historical records indicated that ancient Indian civilizations e.g., the Indus Valley (∼5200-3300 cal yr BP) and Vedic (∼3400-2400 cal yr BP) had established and thrived during periods of strengthened ISM precipitation, whereas their collapse closely corresponded to the decreased strength in ISM. From ∼2400 to 200 cal yr BP, the Indian subcontinent witnessed the rise and fall of various Kingdoms/dynasties. This period saw an exponential expansion/growth in agriculture, economy, population, languages, architecture, and religions in the Indian subcontinent. The agrarian-based economy showed little or no impact of monsoon weakening after ∼2400 cal yr BP possibly due to development and reforms in administrative policies, construction of irrigation systems such as dams, lakes and canals, use of technology for irrigation such as waterwheel, knowledge of double cropping, production of cash crops. The ancient civilizations of India were directly impacted by the strengthening and weakening of ISM, whereas for the later periods, civilizations were able to adapt to climate change." @default.
• W3126449591 created "2021-02-15" @default.
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• W3126449591 date "2021-03-01" @default.
• W3126449591 modified "2023-10-03" @default.
• W3126449591 title "Middle Holocene Indian summer monsoon variability and its impact on cultural changes in the Indian subcontinent" @default.
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• W3126449591 cites W1522755403 @default.
• W3126449591 cites W1943346833 @default.
• W3126449591 cites W1969473919 @default.
• W3126449591 cites W1974610816 @default.
• W3126449591 cites W1976259730 @default.
• W3126449591 cites W1980925903 @default.
• W3126449591 cites W1990899433 @default.
• W3126449591 cites W1991913409 @default.
• W3126449591 cites W1996227144 @default.
• W3126449591 cites W1996932107 @default.
• W3126449591 cites W2001286049 @default.
• W3126449591 cites W2004905512 @default.
• W3126449591 cites W2006634273 @default.
• W3126449591 cites W2011048838 @default.
• W3126449591 cites W2024001474 @default.
• W3126449591 cites W2026133956 @default.
• W3126449591 cites W2030174121 @default.
• W3126449591 cites W2036499887 @default.
• W3126449591 cites W2039574870 @default.
• W3126449591 cites W2041299428 @default.
• W3126449591 cites W2042859974 @default.
• W3126449591 cites W2043771485 @default.
• W3126449591 cites W2045419467 @default.
• W3126449591 cites W2045536299 @default.
• W3126449591 cites W2047027424 @default.
• W3126449591 cites W2049867696 @default.
• W3126449591 cites W2050909497 @default.
• W3126449591 cites W2053651898 @default.
• W3126449591 cites W2056189943 @default.
• W3126449591 cites W2059188341 @default.
• W3126449591 cites W2060734817 @default.
• W3126449591 cites W2070830871 @default.
• W3126449591 cites W2080072873 @default.
• W3126449591 cites W2081011249 @default.
• W3126449591 cites W2084661097 @default.
• W3126449591 cites W2090314934 @default.
• W3126449591 cites W2091926733 @default.
• W3126449591 cites W2093069135 @default.
• W3126449591 cites W2097324101 @default.
• W3126449591 cites W2106990564 @default.
• W3126449591 cites W2116952675 @default.
• W3126449591 cites W2122046874 @default.
• W3126449591 cites W2122971325 @default.
• W3126449591 cites W2124757012 @default.
• W3126449591 cites W2131360976 @default.
• W3126449591 cites W2135438377 @default.
• W3126449591 cites W2156102187 @default.
• W3126449591 cites W2157634932 @default.
• W3126449591 cites W2167767686 @default.
• W3126449591 cites W2167913202 @default.
• W3126449591 cites W2211178400 @default.
• W3126449591 cites W2335961020 @default.
• W3126449591 cites W2400672459 @default.
• W3126449591 cites W2479929551 @default.
• W3126449591 cites W2761538876 @default.
• W3126449591 cites W2761974931 @default.
• W3126449591 cites W2771399181 @default.
• W3126449591 cites W2775294786 @default.
• W3126449591 cites W2790557048 @default.
• W3126449591 cites W2800443358 @default.
• W3126449591 cites W2891251636 @default.
• W3126449591 cites W2901047940 @default.
• W3126449591 cites W2901347472 @default.
• W3126449591 cites W2912515548 @default.
• W3126449591 cites W2935725035 @default.
• W3126449591 cites W2963970932 @default.
• W3126449591 cites W2969335915 @default.
• W3126449591 cites W2987101430 @default.
• W3126449591 cites W3034784643 @default.
• W3126449591 cites W3035848493 @default.
• W3126449591 cites W3043366137 @default.
• W3126449591 cites W4235395268 @default.
• W3126449591 cites W4246027503 @default.
• W3126449591 cites W4249751050 @default.
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• W3126449591 doi "https://doi.org/10.1016/j.quascirev.2021.106825" @default.
• W3126449591 hasPublicationYear "2021" @default.
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