The post-glacial (Bølling-Allerød) sedimentary archive preserved in the Eastern Great Rann of Kachchh (EGRK) is used to reconstruct the pattern of Indian Summer Monsoon (ISM) variability, landform evolution, and the impact on the Indus Valley Civilization (IVC). Employing the sedimentology, geochemistry, and chronology supported by statistical analysis, four major phases of strengthened and weakened monsoon conditions are inferred. The pattern of geochemical variability during Phase-I (13.6 ka and 12.7 ka) indicates a relatively wetter condition (improved ISM); following this, during phase-II (11.9 ka and 11.1 ka), the ISM strength weakened. However, the ISM began to restrengthen during the phase-III (11 ka and >5 ka), with fluctuations. The phase-IV (<5 ka) is represented by a gradual decline in the ISM strength. The sediment isotopic analysis (Sr and Nd) reveals that the Indus River was the major contributor (~48%), followed by the contribution from local reworking of Mesozoic lithology from Khadir Island (~35%). The northern Thar Dune field contribution by ephemeral streams was around 14%, whereas the influence of Luni River at Trangadi Bet was insignificant (~3%). The study observed that around 7 ka, hydrological conditions dwindled, which persisted during the IVC, dated to 5.5 ka–3.8 ka in the region. However, despite dwindling freshwater from the branch off northwest-southeast trending paleochannel (via Indus), it has been hypothesized that the IVC in the EGRK (at Dholavira on Khadir Island) was sustained by the ephemeral monsoon-fed channels.
AdamsJMaslinMThomasE (1999) Sudden climate transitions during the Quaternary. Progress in Physical Geography23(1): 1–36.
2.
AliSNDubeyJGhoshR, et al. (2018) High frequency abrupt shifts in the Indian summer monsoon since Younger Dryas in the Himalaya. Scientific Reports8: 9287.
3.
AlizaiACliftPDGiosanL, et al. (2011b) Pb isotopic variability in the modern-Pleistocene Indus River system measured by ion microprobe in detrital K-feldspar grains. Geochimica et Cosmochimica Acta75: 4771–4795.
4.
AlleyRB (2000) The Younger Dryas cold interval as viewed from Central Greenland. Quaternary Science Reviews19(1-5): 213–226.
5.
AnoopAPrasadSKrishnanR, et al. (2013a) Intensified monsoon and spatiotemporal changes in precipitation patterns in the NW Himalaya during the early- Mid-Holocene. Quaternary International313–314: 74–84.
6.
BeuningKRMTalbotMRKeltsK (1997) A revised 30,000-year paleoclimatic and paleohydrologic history of Lake Albert, East Africa. Palaeogeography Palaeoclimatology Palaeoecology136: 259–279.
7.
BhadraBKGuptaAKSharmaJR (2009) Saraswati Nadi in Haryana and its linkage with the Vedic Saraswati River — Integrated study based on satellite images and ground based information. Journal of the Geological Society of India73: 273–288.
8.
BhatnagarAShuklaADNgangomM, et al. (2024) Analysis of sediment provenance using geochemical and isotopic data for a post-LGM sediment core from the western Great rann of Kachchh, India: Implications for climate control on source regions. Palaeogeography Palaeoclimatology Palaeoecology644: 112185.
9.
BhatnagarAShuklaADNgangomM, et al. (2025) Temporal changes in Land-Sea configuration inferred from post-glacial sedimentation pattern in the Western Great Rann of Kachchh, India. Journal of Geosciences Research10(1): 1–6.
10.
BhushanRDuttaKSomayajuluBLK (2001) Concentrations and burial fluxes of organic and inorganic carbon on the eastern margins of the Arabian Sea. Marine Geology178(1-4): 95–113.
11.
BhushanRSatiSPRanaN, et al. (2018) High-resolution millennial and centennial scale Holocene monsoon variability in the higher central Himalayas. Palaeogeography Palaeoclimatology Palaeoecology489: 95–104.
12.
BishtRS (1994) Urban planning at Dholavira: A Harappan City. In: MalvilleJMGujralLM (eds) Cosmic Geometries and City Planning in Ancient India. New Delhi: Indira Gandhi National Centre for the Arts & Aryan Books International, pp.11–23.
13.
BiswasSK (1987) Regional tectonic framework, structure and evolution of the western marginal basins of India. Tectonophysics135: 307–327.
14.
BiswasSKDeshpandeSV (1970) Geological and Tectonic Maps of Kutch. Bull. ONGC, Dehradun7(2): 115–116.
15.
BondGBroeckerWJohnsenS, et al. (1993) Correlations between climate records from North Atlantic sediments and Greenland ice. Nature365: 143–147.
16.
CalvertSEPedersenTF (2007) Elemental proxies for palaeoclimatic and palae- oceanographic variability in marine sediments: Interpretation and application. In: MarcelCHVernalAD (eds) Paleoceanography of the Late Cenozoic, Part 1. Amsterdam: Elsevier, pp.567–644.
17.
ChatterjeeA (2018) Provenance of Late quaternary continental sediments in Western India: Insights from trace element and isotope geochemistry. Thesis submitted to The Maharaja Sayajirao, University of Baroda Vadodara, India.
18.
ChatterjeeARayJS (2017) Sources and depositional pathways of Mid-Holocene sediments in the Great Rann of Kachchh, India: Implications for fluvial scenario during the Harappan culture. Quaternary International443: 177–187.
19.
ChenJAnZHeadJ (1999) Variation of Rb/Sr ratios in the loess-paleosol sequences of central China during the last 130,000 years and their implications for monsoon paleoclimatology. Quaternary Research51: 215–219.
20.
CliftPDGiosanLBlusztajnJ, et al. (2008) Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon. Geology36: 79–82.
21.
CliftPDGiosanLCarterA, et al. (2010) Monsoon control over erosion patterns in the Western Himalaya: Possible feed-back into the tectonic evolution. In: CliftPDTadaRZhengH (eds) Monsoon Evolution and Tectonics–Climate Linkage in Asia. London: The Geological Society of London, pp.185–218.
22.
DalesGF (1966) The Decline of the Harappans. Scientific American214(5): 93–100.
23.
DeoSGGhateSRajaguruSN (2011) Holocene environmental changes and cultural patterns in coastal western India: A geoarchaeological perspective. Quaternary International229(1-2): 132–139.
24.
DixitYHodellDAPetrieCA (2014b) Abrupt weakening of the summer monsoon in northwest India 4100 yr ago. Geology42(4): 339–342.
25.
DixitYHodellDASinhaR, et al. (2014a) Abrupt weakening of the Indian summer monsoon at 8.2 kyr B.P. Earth and Planetary Science Letters391: 16–23.
26.
DrewLJGrunskyECSutphinDM, et al. (2010) Multivariate analysis of the geochemistry and mineralogy of soils along two continental-scale transects in North America. Science of the Total Environment409: 218–227.
27.
DuttaKBhushanRSomayajuluBLK (2001) ΔR correction values for the northern Indian Ocean. Radiocarbon43(2A): 483–488.
28.
DuttSGuptaAKClemensSC, et al. (2015) Abrupt changes in Indian summer monsoon strength during 33,800 to 5500 years B.P. Geophysical Research Letters42: 5526–5532.
29.
EngstromDRWrightH (1984) Chemical stratigraphy of lake sediments as a record of environmental change. In: HaworthEYLundJWG (eds) Lake Sediments and Environmental History: Studies in Palaeolimnology and Palaeoecology in Honour of Winifred Tutin. Leicester: Leicester University Press, pp.11–67.
30.
FleitmannDBurnsSJMudelseeM, et al. (2003) Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman. Science300: 1737–1739.
31.
GarçonMChauvelCFrance-LanordC, et al. (2014) Which minerals control the Nd–Hf–Sr–Pb isotopic compositions of river sediments?Chemical Geology364: 42–55.
32.
GarzantiELiangWAndòS, et al. (2020) Provenance of Thal Desert sand: Focused erosion in the western Himalayan syntaxis and foreland-basin deposition driven by latest Quaternary climate change. Earth-Science Reviews207: 103220.
33.
GlennieKWEvansG (1976) A reconnaissance of the recent sediments of the Ranns of Kutch, India. Sedimentology23: 625–647.
34.
GoldsteinSLO’NionsRKHamiltonPJ (1984) A Sm-Nd isotopic study of atmospheric dusts and particulates from major river systems. Earth and Planetary Science Letters70: 221–236.
35.
GoswamiVSinghSKBhushanR, et al. (2012) Temporal variations in 87Sr/86Sr and ɛNd in sediments of the southeastern Arabian Sea: Impact of monsoon and surface water circulation. Geochemistry Geophysics Geosystems13: 1–13. DOI: 10.1029/2011GC003802
36.
GovinAHolzwarthUHeslopD, et al. (2012) Distribution of major elements in Atlantic surface sediments (36°N–49°S): Imprint of terrigenous input and continental weathering. Geochemistry Geophysics Geosystems13: Q01013.
37.
GuptaAKMohanKDasM, et al. (2013) Solar forcing of the Indian summer monsoon variability during the Allerød period. Scientific Reports3: 2753.
38.
HeatonTJKöhlerPButzinM, et al. (2020) Marine20—The marine radiocarbon age calibration curve (0–55,000 cal BP). Radiocarbon62(4): 779–820.
39.
HerzschuhU (2006) Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews25(1-2): 163–178.
40.
JacobsenSBWasserburgGJ (1980) Sm-Nd isotopic systematics of chondrites and achondrites. Meteoritics15(4): 307–308.
41.
JuyalNChamyalLSBhandariS, et al. (2006) Continental record of the southwest monsoon during the last 130 ka: Evidence from the southern margin of the Thar Desert, India. Quaternary Science Reviews25: 2632–2650.
42.
KarA (2020) The Saraswati River system: A revisit with new data and interpretation. Journal of Indian Geomorphology8: 1–30.
43.
KarA (2021) Identification and mapping of the Saraswati River system: A review and new findings. In: AcharyyaSKGhoshKKarA (eds) Saraswati: The River Par Excellence. Kolkata: The Asiatic Society, pp.29–98.
44.
KarASinghviAKRajaguruSN, et al. (2001) Reconstruction of the late quaternary environment of the lower Luni Plains, Thar Desert, India. Journal of Quaternary Science16: 61–68.
45.
KathayatGChengHSinhaA, et al. (2016) Indian monsoon variability on millennial-orbital timescales. Scientific Reports6: 24374.
46.
KathayatGChengHSinhaA, et al. (2018) Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India. Climate of the Past14: 1869–1879.
47.
KenoyerJM (2008) Indus civilization. In: PearsallDM (ed.) Encyclopedia of Archaeology. New York: Elsevier, pp.715–733.
48.
KessarkarPMRaoVPAhmadSM, et al. (2003) Clay minerals and Sr–Nd isotopes of the sediments along the western margin of India and their implication for sediment provenance. Marine Geology202: 55–69.
49.
KhondeN (2014) Holocene environments and geomorphic evolution of the Great Rann of Kachchh, Western India. PhD Thesis, submitted to M. S. University, Baroda.
50.
KhondeNSinghSKMauryaDM, et al. (2017) Tracing the Vedic Saraswati River in the Great Rann of Kachchh. Scientific Reports7(1): 5476–6.
51.
LawlerA (2011) Archaeology. In Indus Times, the river didn’t run through it. Science332: 23.
52.
LimmerDRBöningPGiosanL, et al. (2012) Geochemical record of Holocene to recent sedimentation on the western Indus continental shelf, Arabian sea. Geochemistry Geophysics Geosystems13: 1–26.
53.
LisitzinAP (1996) Oceanic Sedimentation: Lithology and Geochemistry. Washington, DC: American Geophysical Union, p.400.
54.
LupkerMFrance-LanordCGalyV, et al. (2012) Predominant floodplain over mountain weathering of Himalayan sediments (Ganga basin). Geochimica et Cosmochimica Acta84: 410–432.
55.
Martinez RuizFKastnerMGallego TorresD, et al. (2015) Paleoclimate and paleoceanography over the past 20,000 yr in the Mediterranean Sea Basins as indicated by sediment elemental proxies. Quaternary Science Reviews107: 25–46.
56.
MishraPKAnoopASchettlerG, et al. (2015) Reconstructed late Quaternary hydrological changes from Lake Tso moriri, NW Himalaya. Quaternary International371: 76–86.
57.
NajmanYGarzantiE (2000) Reconstructing early Himalayan tectonic evolution and paleogeography from tertiary foreland basin sedimentary rocks, northern India. Geological Society of America Bulletin112: 435–449.
58.
NemecMWackerLGäggelerH (2010) Optimization of the graphitization process AT AGE-1. Radiocarbon52: 1380–1393.
59.
NesbittHWYoungGM (1982) Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature299: 715–717.
60.
NesbittHWYoungGM (1984) Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochimica et Cosmochimica Acta48: 1523–1534.
61.
NgangomMBhandariSThakkarMG, et al. (2017) Mid-Holocene extreme hydrological events in the eastern Great Rann of Kachchh, western India. Quaternary International443: 188–199.
62.
PattanJNMasuzawaTYamamotoM (2005) Variations in terrigenous sediment discharge in a sediment core from southeastern Arabian Sea during the last 140 ka. Current Science89: 1421–1425.
63.
PetersonLCHaugGHHughenKA, et al. (2000) Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial. Science290: 1947–1951.
64.
PillaiASAmbiliAPrasadV, et al. (2018) Multi-proxy Evidence for an Arid Shift in the Climate and Vegetation of the Banni Grasslands of Western India during the Mid to Late-Holocene. Holocene28(7): 1057–1070.
65.
PossehlGL (2002) The Indus Civilization: A Contemporary Prospective: Walnut Creek. Lanham, MD: California AltaMira Press, p.276.
66.
PrasadSAnoopARiedelN, et al. (2014) Prolonged monsoon droughts and links to Indo-Pacific warm pool: A Holocene record from Lonar Lake, central India. Earth and Planetary Science Letters391: 171–182.
67.
PrinsMAPostmaG (2000) Effects of climate, sea level, and tectonics unraveled for last deglaciation turbidite records of the Arabian Sea. Geology28: 375–378.
68.
RaczekIJochumKPHofmannAW (2001) Neodymium and strontium isotope data for USGS reference GSP-1, GSP-2 and eight MPI-DING reference glasses. Geostandards Newsletter27: 173–179.
69.
RajaniMBRajawatAS (2011) Potential of satellite based sensors for studying distribution of archaeological sites along palaeo channels: Harappan sites a case study. Journal of Archaeological Science38(9): 2010–2016.
70.
RajendranCPRajendranK (2003b) Studying earthquake recurrence in the Kachchh region. India. Eos Transactions American Geophysical Union84(48): 529–536.
71.
RajendranCPRajendranKThakkarM, et al. (2008) Assessing the previous activity at the source zone of the 2001 Bhuj earthquake based on the near-source and distant paleoseismological indicators. Journal of Geophysical Research113: B05311.
72.
ReimerPJAustinWENBardE, et al. (2020) The IntCal20 Northern Hemisphere radiocarbon age calibration curve (0–55 cal kBP). Radiocarbon62: 725–757.
73.
Rodrigo-GámizMMartínez-RuizFJiménez-EspejoFJ, et al. (2011) Impact of climate variability in the western Mediterranean during the last 20,000 years: oceanic and atmospheric responses. Quaternary Science Reviews30: 2018–2034.
74.
SamLGahlotNPrustyBG (2015) Estimation of dune celerity and sand flux in part of West Rajasthan, Gadra area of the Thar Desert using temporal remote sensing data. Arabian Journal of Geosciences8: 295–306.
75.
SarkarAMukherjeeADSharmaS, et al. (2020) New evidence of early Iron Age to medieval settlements from the southern fringe of Thar Desert (western Great Rann of Kachchh), India: Implications to climate-culture co-evolution. Archaeological Research in Asia21: 100–163.
76.
SaxenaAPrasadVSinghIB (2013) Holocene palaeoclimate reconstruction from the phytoliths of the lake-fill sequence of Ganga Plain. Current Science104(8): 1054–1062.
77.
SchulzHvon RadUErlenkeuserH, et al. (1998) Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature393: 54–57.
78.
SenguptaTDeshpande MukherjeeABhushanR, et al. (2020) Did the Harappan settlement of Dholavira (India) collapse during the onset of Meghalayan stage drought?Journal of Quaternary Science35: 382–395.
79.
SharmaSChauhanGShuklaAD, et al. (2021) Causes and implications of Mid- to Late Holocene relative sea-level change in the Gulf of Kachchh, western India. Quaternary Research100: 98–121.
80.
SharmaSShuklaAD (2018) Factors governing the pattern of glacier advances since the last Glacial Maxima in the transitional climate zone of the southern Zanskar Ranges, NW Himalaya. Quaternary Science Reviews201: 223–240.
81.
ShuklaAD (2011) Geochemical and isotopic studies of some sedimentary sequences of the Vindhyan Super group, India. Unpublished PhD thesis, submitted to M.S. University, Baroda.
82.
SinghSKRaiSKKrishnaswamiS (2008) Sr and Nd isotopes in river sediments from the Ganga Basin: sediment provenance and spatial variability in physical erosion. Journal of Geophysical Research113: 1–18.
83.
SinghviAKKarA (2004) The aeolian sedimentation record of the Thar desert. Proceedings of the Indian Academy of Sciences (Earth and Planetary Sciences) 113: 371–401.
84.
SirockoFGarbe-SchönbergDMcIntyreA, et al. (1996) Teleconnections between the subtropical monsoons and high-latitude climates during the last deglaciation. Science272: 526–529.
85.
SivewrightR (1907) Cutch and the Ran. Geographical Journal29: 518–535.
86.
SouthonJKashgarianMFontugneM, et al. (2002) Marine reservoir corrections for the Indian Ocean and Southeast Asia. Radiocarbon44(1): 167–180.
87.
TalbotMRLivingstoneDA (1989) Hydrogen Index and carbon isotopes of lacustrine organic matter as lake level indicators. Palaeogeography Palaeoclimatology Palaeoecology70: 121–137.
88.
TripathiJKBockBRajamaniV (2013) Nd and Sr isotope characteristics of Quaternary Indo-Gangetic plain sediments: Source distinctiveness in different geographic regions and its geological significance. Chemical Geology344: 12–22.
89.
TyagiAShuklaADBhushanR, et al. (2012) Mid-Holocene sedimentation and landscape evolution in the western Great Rann of Kachchh, India. Geomorphology151: 89–98.
90.
von RadUSchulzHRiechV, et al. (1999) Multiple monsoon-controlled breakdown of oxygen-minimum conditions during the past 30,000 years documented in laminated sediments off Pakistan. Palaeogeography Palaeoclimatology Palaeoecology152: 129–161.
91.
WackerLNemecMBourquinJ (2010) A revolutionary graphitisation system: Fully automated, compact and simple. Nuclear Instruments and Methods in Physics Research Section B: BeamInteractions with Materials and Atoms268: 931–934.
92.
WarrierAKShankarR (2009) Geochemical evidence for the use of magnetic susceptibility as a paleorainfall proxy in the tropics. Chemical Geology265(3-4): 553–562.
93.
WolfDSeimAFaustD (2014) Fluvial system response to external forcing and human impact – Late Pleistocene and Holocene fluvial dynamics of the lower Guadalete River in western Andalucía (Spain). Boreas43: 422–449.
94.
WünnemannBDemskeDTarasovP, et al. (2010) Hydrological evolution during the last 15kyr in the Tso Kar Lake basin (Ladakh, India), derived from geomorphological, sedimentological and palynological records. Quaternary Science Reviews29(9–10): 1138–1155.
95.
ZouCMaoLTanZ, et al. (2021) Geochemistry of major and trace elements in sediments from the Lubei Plain, China: Constraints for paleoclimate, paleosalinity, and paleoredox environment. Journal of Asian Earth Sciences6: 100071.
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