Fig. 4: Comparison of the Q5 δ18Oc record with other North African summer monsoon and Asian summer monsoon proxy records, and 30°N–30°S June–July–August (JJA) insolation. | Nature Communications

Fig. 4: Comparison of the Q5 δ18Oc record with other North African summer monsoon and Asian summer monsoon proxy records, and 30°N–30°S June–July–August (JJA) insolation.

From: Holocene climate change in southern Oman deciphered by speleothem records and climate model simulations

Fig. 4: Comparison of the Q5 δ18Oc record with other North African summer monsoon and Asian summer monsoon proxy records, and 30°N–30°S June–July–August (JJA) insolation.The alternative text for this image may have been generated using AI.

The sapropel S1 from the Eastern Mediterranean Ocean Drilling Program (ODP) Site 968 is shown between 10.2 and 6.5 ka BP (marked as a yellow rectangle)65. From top to bottom: δ18Oc of Jeita Cave70 and Soreq Cave69 from the Levent region, δ18Oc of Tianmen Cave93 from Tibetan Plateau, δ18Oc of Mawmluh Cave81 (blue) and Sahiya Cave72 (gray) from India, δ18Oc of Dongge Cave from southern China117, δ18Oc of Hoti Cave from northern Oman31, δ18Oc of Qunf Cave (this study), G. bulloides percentage in ODP Site 723 A offshore Oman39, and δDwax of Horn of Africa marine record P178-15P71. Source data are provided in the Source Data file.

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