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Sensitivity of Red Sea circulation to sea level and insolation forcing during the last interglacial

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Figure

Fig. 1.Map of the Red Sea with the investigated cores KL23(Geiselhart, 1998; Schmelzer, 1998), KL9, and KL11, highlightingthe position of the seasonally active Baraka catchment.
Table 1, Fig. 2). The simple age model for relative compari-son of the Red sea cores was derived by linear interpolationbetween these control points.
Table 1. Age model tie points of the observed Red Sea cores.
Fig. 4. Comparison of KL9 foraminiferal faunal assemblage data of MIS 6-5d and the calibration data set (grey filled circles)
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