Abstract. A large array of proxy records
suggests that the “4.2 ka event” marks an approximately
300-year long period (∼3.9 to 4.2 ka) of
major climate change across the globe. However, the climatic manifestation of
this event, including its onset, duration, and termination, remains less
clear in the Indian summer monsoon (ISM) domain. Here, we present new oxygen
isotope (δ18O) data from a pair of speleothems (ML.1 and ML.2)
from Mawmluh Cave, Meghalaya, India, that provide a high-resolution record of
ISM variability during a period (∼3.78 and 4.44 ka) that fully
encompasses the 4.2 ka event. The sub-annually to annually resolved ML.1
δ18O record is constrained by 18 230Th dates with an
average dating error of ±13 years (2σ) and a resolution of ∼40 years, which allows us to characterize the ISM variability with
unprecedented detail. The inferred pattern of ISM variability during the
period contemporaneous with the 4.2 ka event shares broad similarities and
key differences with the previous reconstructions of ISM from the Mawmluh
Cave and other proxy records from the region. Our data suggest that the ISM
intensity, in the context of the length of our record, abruptly decreased at
∼4.0 ka (∼±13 years), marking the onset of a multi-centennial
period of relatively reduced ISM, which was punctuated by at least two
multi-decadal droughts between ∼3.9 and 4.0 ka. The latter stands out
in contrast with some previous proxy reconstructions of the ISM, in which the
4.2 ka event has been depicted as a singular multi-centennial drought.
The 8.2 ka event has been extensively studied, whereas its structure is ambiguous in North China. Here we present a high‐resolution (∼1 year) δ18O record from annual laminated speleothem from Beijing to characterize the detailed variability across this event in North China. Our record indicates a dry 8.2 ka event spanning 8.254–8.107 ka BP with a two‐stage structure superimposed by three prominent high δ18O excursions. The identical structure of speleothem δ18O records between North and central China during the event suggests a common forcing/response in East China, whereas the progressively increased offset between their average values may reflect changes in moisture source or rainout effect. A close comparison with the Greenland ice core records suggests a strong linear response of the Asian summer monsoon to the North Atlantic climate changes across the early and middle stages of the event, but a different mechanism in the termination processes.
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