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Sub-decadal- to decadal-scale climate cyclicity during the Holsteinian interglacial (MIS 11) evidenced in annually laminated sediments

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Figure

Fig. 1. Map indicating the location of the Dethlingen palaeolake.
Fig. 2.Thin-section and scanning electron microscope pho-tographs of varves from the Dethlingen core: light and dark sub-layers (A) under parallel-polarized light and (B) under cross-polarized light; (C) close-up photograph of successive dark andlight sub-layers; (D) pyrite framboids; (E) sponge spicule; (F) wind-transported fine sand grain.
Fig. 3. Thin-section and scanning electron microscope photographs from different varve sub-layers from Dethlingen: (A, B) dark sub-layer; (C, D) light sub-layer type A; (E, F) light sub-layer type B; (G, H) light sub-layer type C.
Table 1. Summary of significant spectral peaks of light and darksub-layer time series of the Dethlingen varves and their possibleforcing mechanisms.
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