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Progress in Earth and Planetary Science
Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: Integrated Pliocene-Pleistocene magnetostratigraphy and tephrostratigraphy of deep-sea sediments at IODP Site U1424 (Yamato Basin, Japan Sea)

Fig. 7

Age model and sedimentation rates of Site U1424 sediments. Top panel: depth-age model of Site U1424 sediments between 0 and 167.6 m CCSF-A (~ 0–4.89 Ma) based on polarity reversals (black squares), tephra (red triangles) chronology, and tuning of U1424 GRA and NGR data to a global benthic oxygen isotope stack (green dots; see Tada et al. 2018). Bottom panel: Site U1424 sedimentation rate changes through time estimated using tuned ages for the last ~ 3 Myr and magnetostratigraphy and tephra ages for intervals older than ~ 3 Ma

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