Distinct control mechanism of fine‐grained sediments from <scp>Y</scp>ellow <scp>R</scp>iver and <scp>K</scp>yushu supply in the northern <scp>O</scp>kinawa <scp>T</scp>rough since the last glacial

Zhao, Debo; Wan, Shiming; Toucanne, Samuel; Clift, Peter D.; Tada, Ryuji; Révillon, Sidonie; Kubota, Yoshimi; Zheng, Xiaoxu; Yu, Zhaojie; Huang, Jie; Jiang, Hanchao; Xu, Zuyan; Shi, Xuefa; Li, Anchun

doi:10.1002/2016gc006764

Cited by 31 publications

(38 citation statements)

References 109 publications

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“…Small peaks (2-7 g/cm 2 /kyr) occur in the Southern Japanese Islands end-member during coincident times of decreased UCC and Luochuan end-member accumulation and increased relative sea level. This is also mirrored in the LGM average Kyushu end-member accumulation rate identified by Zhao et al (2017). Similar patterns of increased Southern Japanese Islands end-member accumulation and the grain size proxy SiO 2 /Al 2 O 3 (g/g) occur when relative sea level is also increased ( Figure 5).…”

Section: Sea Level and Sediment Shelf Bypasssupporting

confidence: 56%

Climatically Driven Changes in the Supply of Terrigenous Sediment to the East China Sea

Anderson

Murray

Dunlea

et al. 2018

Geochem Geophys Geosyst

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We examine the paleoceanographic record over the last ∼400 kyr derived from major, trace, and rare earth elements in bulk sediment from two sites in the East China Sea drilled during Integrated Ocean Drilling Program Expedition 346. We use multivariate statistical partitioning techniques (Q‐mode factor analysis, multiple linear regression) to identify and quantify five crustal source components (Upper Continental Crust (UCC), Luochuan Loess, Xiashu Loess, Southern Japanese Islands, Kyushu Volcanics), and model their mass accumulation rates (MARs). UCC (35–79% of terrigenous contribution) and Luochuan Loess (16–55% contribution) are the most abundant end‐members through time, while Xiashu Loess, Southern Japanese Islands, and Kyushu Volcanics (1–22% contribution) are the lowest in abundance when present. Cycles in UCC and Luochuan Loess MARs may indicate continental and loess‐like material transported by major rivers into the Okinawa Trough. Increases in sea level and grain size proxy (e.g., SiO2/Al2O3) are coincident with increased flux of Southern Japanese Islands, indicating localized sediment supply from Japan. Increases in total terrigenous MAR precede minimum relative sea levels by several thousand years and may indicate remobilization of continental shelf material. Changes in the relative contribution of these end‐members are decoupled from total MAR, indicating compositional changes in the sediment are distinct from accumulation rate changes but may be linked to variations in sea level, riverine and eolian fluxes, and shelf‐bypass processes over glacial‐interglacials, complicating accurate monsoon reconstructions from fluvial dominated sediment.

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Section: Sea Level and Sediment Shelf Bypasssupporting

confidence: 56%

Climatically Driven Changes in the Supply of Terrigenous Sediment to the East China Sea

Anderson

Murray

Dunlea

et al. 2018

Geochem Geophys Geosyst

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“…The linear sedimentation rates varied between 24.0 and 160.8 cm/ka, with an average value of 53.5 cm/ka ( Figure S3). Here we combined previous clay results (from the upper 20.99 m of IODP Site U1429; Zhao et al, 2017) and new clay mineralogical data to reconstruct the EAWM intensity during the last 300 ka with the clay mineral ratio illite/smectite and the Yellow River terrigenous mass accumulation rate. To determine the sediment flux, we also calculated the relative sediment supply and terrigenous mass accumulation rate.…”

Section: Methodsmentioning

confidence: 99%

“…In addition, we conducted a cross-spectral analysis to examine periodicities and further assess the intrinsic mechanism of EAWM change in the frequency domain. Li et al, 2012;Li et al, 2018;Licht et al, 2016;Milliman & Farnsworth, 2013;Ohtsubo et al, 1995;Pang et al, 2010;Park et al, 2009;Park & Khim, 1990;Rea & Janecek, 1981;Ren & Shi, 1986;Sagawa et al, 2018;Schneider et al, 2010;Song et al, 2016;Sun et al, 2015;Wan et al, 2007;Wan et al, 2012;Yang et al, 2003;Yuan et al, 2008;Zhao et al, 2017;Zheng et al, 2016;Zheng et al, 2014). Li et al, 2012;Li et al, 2018;Licht et al, 2016;Milliman & Farnsworth, 2013;Ohtsubo et al, 1995;Pang et al, 2010;Park et al, 2009;Park & Khim, 1990;Rea & Janecek, 1981;Ren & Shi, 1986;Sagawa et al, 2018;Schneider et al, 2010;Song et al, 2016;Sun et al, 2015;Wan et al, 2007;Wan et al, 2012;Yang et al, 2003;Yuan et al, 2008;Zhao et al, 2017;Zheng et al, 2016;Zheng et al, 2014)…”

Section: Methodsmentioning

confidence: 99%

“…More detailed information on the analytical methods is provided in the Text S1 and Figures S3-S7 in the supporting information (Beny et al, 2018;Diekmann et al, 2008;Fan et al, 2001;Grant et al, 2014;Howell et al, 2006;Khon et al, 2018;Kim, 1979;C. Li et al, 2012;Li et al, 2018;Licht et al, 2016;Milliman & Farnsworth, 2013;Ohtsubo et al, 1995;Pang et al, 2010;Park et al, 2009;Park & Khim, 1990;Rea & Janecek, 1981;Ren & Shi, 1986;Sagawa et al, 2018;Schneider et al, 2010;Song et al, 2016;Sun et al, 2015;Wan et al, 2007;Wan et al, 2012;Yang et al, 2003;Yuan et al, 2008;Zhao et al, 2017;Zheng et al, 2016;Zheng et al, 2014).…”

Section: Methodsmentioning

confidence: 99%

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Asynchronous Variation in the Quaternary East Asian Winter Monsoon Associated With the Tropical Pacific ENSO‐Like System

Zhao

Wan

Song

et al. 2019

Geophysical Research Letters

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Quaternary East Asian winter monsoon (EAWM) evolution has long been attributed to high‐latitude Northern Hemisphere climate change. However, it cannot explain the distinct relationships of the EAWM in the northern and southern East Asian marginal sea in paleoclimatic records. Here we present an EAWM record of the northern East China Sea over the past 300 ka and a transient climate simulation with the Kiel Climate Model through the Holocene. Both proxy record and simulation suggest anticorrelated long‐term EAWM evolution between the northern East China Sea and the South China Sea. We suggest that this spatial discrepancy of EAWM can be interpreted as El Niño–Southern Oscillation (ENSO)‐like controlling, which generates cyclonic/anticyclonic wind anomalies in the northern/southern East Asian marginal sea. This research explains much of the controversy in nonorbital scale variability of Quaternary EAWM records in the East Asian marginal sea and supports a potent role of tropical forcing in East Asian winter climate change.

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“…The muddy and sandy sediments resulting from hydrodynamic sorting by tidal and ocean currents generally have different compositions even when derived from the same source under the same conditions, which usually leads to geochemical Figure 1. Map of the study area showing the location of Core S3 (a, b; ocean currents modified after Reference [38]), the major hydrographic network in Taiwan Island (c; modified after Reference [44]), and the tectonic map of Taiwan Island (d; modified after Reference [45]).…”

Section: Introductionmentioning

confidence: 99%

Geochemical Study of Detrital Apatite in Sediment from the Southern Okinawa Trough: New Insights into Sediment Provenance

Zeng

Fang

et al. 2019

Minerals

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Detrital apatite is a promising accessory mineral for reliable fingerprinting of the protolith composition of detrital sediment. Here, we present the geochemical compositions of detrital apatites from four sections of a high-resolution (~140 cm/kyr) sedimentary archive from the southern Okinawa Trough (SOT) for constraining sediment source rock types and establishing changes in provenance. A series of diagrams based on the geochemical data show that apatites in Section 1 derived mainly from mafic/intermediate rocks, while apatites in the three younger sections largely originated from mafic/intermediate rocks and acid rocks. Further, the four sections included a few contributions of apatites from alkaline rocks and metamorphic rocks. Through a comprehensive analysis of controlling factors and regional stratigraphy in the study area, we concluded that sediments in the SOT are the weathering/erosion products of sedimentary and meta-sedimentary rocks in the western and northeastern Taiwan Island, with ultimate sources containing a wide variety of rock types. The sediment from rivers in eastern Taiwan did not significantly contribute to deposition in the SOT. Apatites in Sections 2–4 showed strong geochemical similarity but differed from those in Section 1, indicating that the types of weathered/eroded sedimentary rocks in the weathering profile of river drainage basins of Taiwan Island changed in Section 2 (2010–1940 cal. yr BP) and have remained stable since then.

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Distinct control mechanism of fine‐grained sediments from Yellow River and Kyushu supply in the northern Okinawa Trough since the last glacial

Cited by 31 publications

References 109 publications

Climatically Driven Changes in the Supply of Terrigenous Sediment to the East China Sea

Climatically Driven Changes in the Supply of Terrigenous Sediment to the East China Sea

Asynchronous Variation in the Quaternary East Asian Winter Monsoon Associated With the Tropical Pacific ENSO‐Like System

Geochemical Study of Detrital Apatite in Sediment from the Southern Okinawa Trough: New Insights into Sediment Provenance

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