Data report: X-ray fluorescence scanning of Site U1427, Yamato Basin, Expedition 346

Peterson, L.C.; Schimmenti, D.E.

doi:10.2204/iodp.proc.346.206.2020

Cited by 3 publications

(3 citation statements)

References 32 publications

(40 reference statements)

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“…The depth scale applied in this study is “m U1427_Patched_CCSF‐D(_rev20170310)” as shown in Irino et al. (2018), and as used by other publications on the upper ∼250 m sediment cores of Site U1427 (Black et al., 2018; Gallagher et al., 2018; Miller & Dickens, 2017; Peterson & Schimmenti, 2020; Saavedra‐Pellitero et al., 2019; Sagawa et al., 2018). The depth scale constructed by Irino et al.…”

Section: Methodsmentioning

confidence: 99%

“…The depth scale applied in this study is "m U1427_Patched_CCSF-D(_rev20170310)" as shown in Irino et al (2018), and as used by other publications on the upper ∼250 m sediment cores of Site U1427 (Black et al, 2018;Gallagher et al, 2018;Miller & Dickens, 2017;Peterson & Schimmenti, 2020;Saavedra-Pellitero et al, 2019;Sagawa et al, 2018). The depth scale constructed by Irino et al (2018) is applicable to the full splice interval, that is the upper 430.337 m CCSF-A, and for the non-splice interval below 11.755 m were added to CCSF-A depths to obtain the "Patched"-equivalent depth scale.…”

Section: Site U1427mentioning

confidence: 99%

“…This record shows relatively lower δ 18 O values during glacials (when resolved), while interglacials are characterized by higher δ 18 O values (Sagawa et al., 2018). While much work has been done on the upper 250 m of sediment cores, little work has yet been done on the sediments that encompass the MPT (Black et al., 2018; Gallagher et al., 2018; Miller & Dickens, 2017; Peterson & Schimmenti, 2020; Saavedra‐Pellitero et al., 2019; Sagawa et al., 2018). The aim of this study is therefore twofold.…”

Section: Introductionmentioning

confidence: 99%

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Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427

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Introduction The Mid-Pleistocene Transition and the East Asian MonsoonThe Quaternary period is characterized by glacial-interglacial variability that has been linked to Earth's orbital cyclicity (e.g., Hays et al., 1976;Ruddiman, 2001). During the early part of the Quaternary, glacial-interglacial cycles varied at a frequency of 41,000 years (41 ka), but approximately half-way through the Quaternary, during the mid-Pleistocene, the glacial-interglacial cyclicity shifted to quasi 100,000 years (100 ka) cycles (e.g., Lisiecki & Raymo, 2005;Zachos et al., 2001). The transition period between 41 ka and 100 ka is centred at ∼1200 to 600 ka and often referred to as the mid-Pleistocene transition (MPT). After the MPT, glacials became more intense, producing larger ice-sheets that decayed more rapidly at glacial terminations (e.g.

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