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Cited by 1,690

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman

Fleitmann, Dominik, Burns, Stephen J., Mudelsee, Manfred, Neff, Ulrich, Kramers, Jan, Mangini, Augusto, Matter, Albert·2003·Science

Abstract

A high-resolution oxygen-isotope record from a thorium-uranium–dated stalagmite from southern Oman reflects variations in the amount of monsoon precipitation for the periods from 10.3 to 2.7 and 1.4to 0.4thousand years before the present (ky B.P.). Between 10.3 and 8 ky B.P., decadal to centennial variations in monsoon precipitation are in phase with temperature fluctuations recorded in Greenland ice cores, indicating that early Holocene monsoon intensity is largely controlled by glacial boundary conditions. After ∼8 ky B.P., monsoon precipitation decreases gradually in response to changing Northern Hemisphere summer solar insolation, with decadal to multidecadal variations in monsoon precipitation being linked to solar activity.

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Crossref · 10.1126/science.1083130

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Metadata

Authors
Fleitmann, D., Burns, S. J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., & Matter, A.
Venue
Science
Published
2003-06-13
Volume
300
Issue
5626
Pages
1737-1739
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2036499887
Cited by
1,690
References
1
FWCI
33.10
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman. https://app.cochat.ai/papers/10.1126/science.1083130
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Fleitmann, D., Burns, S. J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., & Matter, A. (2003). Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman. Science. https://doi.org/10.1126/science.1083130

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