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Abrupt weakening of the summer monsoon in northwest India 4100 yr ago

Dados Bibliográficos

ID23383043
AutoresYama Dixit (0000-0002-0700-5918, University of Cambridge), David A Hodell (0000-0001-8537-1588, University of Cambridge), C A Petrie (0000-0002-2926-7230, University of Cambridge)
Ano2014
Volume42
Fascículo4
Páginas339-342
Data de publicação2014-04-01
Peer ReviewedSim
Open AccessNão
TipoARTICLE
PeriódicoGeology (JOURNAL)
Identificadores do periódicoISSN: 0091-7613 • E-ISSN: 1943-2682
EditoraGeological Society of America (PUBLISHER • US)
DOI10.1130/g35236.1
OpenAlexW2135438377
IdiomaEN
Citações recebidas103
Referências citadas24

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 outside the distribution of Indus settlements. Here we report an oxygen isotope record of gastropod aragonite ( 18 O a ) from Holocene sediments of paleolake Kotla Dahar (Haryana, India), which is adjacent to Indus settlements and documents Indian summer monsoon (ISM) variability for the past 6.5 k.y. A 4 increase in 18 O a occurred at ca. 4.1 ka marking a peak in the evaporation/precipitation ratio in the lake catchment related to weakening of the ISM. Although dating uncertainty exists in both climate and archaeological records, the drought event 4.1 ka on the northwestern Indian plains is within the radiocarbon age range for the beginning of Indus de-urbanization, suggesting that climate may have played a role in the Indus cultural transformation.

Archaeology · Climate change · Climatology · Geography · Holocene · Human settlement · Indus · Monsoon · Monsoon of South Asia · Physical geography · Precipitation · Radiocarbon dating · Structural basin · Archaeology and ancient environmental studies · Geology · Geology and Paleoclimatology Research · Oceanography · Pacific and Southeast Asian Studies · Paleontology

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