Did the Harappan settlement of Dholavira (India) collapse during the onset of Meghalayan stage drought?

@article{Sengupta2020DidTH,
  title={Did the Harappan settlement of Dholavira (India) collapse during the onset of Meghalayan stage drought?},
  author={Torsa Sengupta and Arati Deshpande Mukherjee and Ravi Bhushan and F. Ram and Melinda Kumar Bera and Harsh Raj and Ankur J. Dabhi and Ravindra Singh Bisht and Yashwant Singh Rawat and Sourendra Kumar Bhattacharya and Navin Juyal and Anindya Sarkar},
  journal={Journal of Quaternary Science},
  year={2020},
  volume={35}
}
Radiocarbon dating of archaeological carbonates from seven cultural stages of Dholavira, Great Rann of Kachchh (GRK), the largest excavated Harappan settlement in India, suggests the beginning of occupation at ~5500 years BP (pre‐Harappan), and continuation until ~3800 years BP (early part of the Late Harappan period). The settlement rapidly expanded under favourable monsoonal climate conditions when architectural elements such as the Citadel, Bailey, Lower and Middle Town were added between… 
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References

SHOWING 1-10 OF 162 REFERENCES
Oxygen isotope in archaeological bioapatites from India: Implications to climate change and decline of Bronze Age Harappan civilization
TLDR
This study reports a high resolution oxygen isotope (δ18O) record of animal teeth-bone phosphates from an archaeological trench itself at Bhirrana, NW India, preserving all cultural levels of this civilization, suggesting that other cause like change in subsistence strategy by shifting crop patterns rather than climate change was responsible for Harappan collapse.
Fluvial landscapes of the Harappan civilization
The collapse of the Bronze Age Harappan, one of the earliest urban civilizations, remains an enigma. Urbanism flourished in the western region of the Indo-Gangetic Plain for approximately 600 y, but
Abrupt weakening of the summer monsoon in northwest India ∼4100 yr ago
Climate change has been suggested as a possible cause for the decline of urban centers of the Indus Civilization ~4000 yr ago, but extant paleoclimatic evidence has been derived from locations well
Climate change and the collapse of the Akkadian empire: Evidence from the deep sea
The Akkadian empire ruled Mesopotamia from the headwaters of the Tigris-Euphrates Rivers to the Persian Gulf during the late third millennium B.C. Archeological evidence has shown that this highly
Altered cropping pattern and cultural continuation with declined prosperity following abrupt and extreme arid event at ~4,200 yrs BP: Evidence from an Indus archaeological site Khirsara, Gujarat, western India
TLDR
A significant change in crop-pattern at ~4,200 yrs BP is shown, based on abundant macrobotanical remains and C isotopes of soil organic matter in an archaeological site at Khirsara, in the Gujarat state of western India, which appears to be intentional and was likely used as an adaptation measure in response to deteriorated monsoonal conditions.
U-Pb zircon dating evidence for a Pleistocene Sarasvati River and capture of the Yamuna River
The Harappan Culture, one of the oldest known urban civilizations, thrived on the northwest edge of the Thar Desert (India and Pakistan) between 3200 and 1900 BCE. Its demise has been linked to rapid
Inundation, sea‐level rise and transition from Neolithic to Bronze Age cultures, Yangtze Delta, China
Petrological, faunal and floral information derived from a new drill core taken in the Yangtze delta, coupled with data from borings recovered earlier, record a marked transition to warmer, wetter
...
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5
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