Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago

Abstract The Yellow River (or Huanghe and also known as China’s Sorrow in ancient times), with the highest sediment load in the world, provides a key link between continental erosion and sediment accumulation in the western Pacific Ocean. However, the exact age of its influence on the marginal sea i...

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Autores principales: Zhengquan Yao, Xuefa Shi, Shuqing Qiao, Qingsong Liu, Selvaraj Kandasamy, Jianxing Liu, Yanguang Liu, Jihua Liu, Xisheng Fang, Jingjing Gao, Yanguang Dou
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Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/c50008ea285f49bd968882c6af32b7a1
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spelling oai:doaj.org-article:c50008ea285f49bd968882c6af32b7a12021-12-02T15:06:07ZPersistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago10.1038/s41598-017-03140-x2045-2322https://doaj.org/article/c50008ea285f49bd968882c6af32b7a12017-06-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-03140-xhttps://doaj.org/toc/2045-2322Abstract The Yellow River (or Huanghe and also known as China’s Sorrow in ancient times), with the highest sediment load in the world, provides a key link between continental erosion and sediment accumulation in the western Pacific Ocean. However, the exact age of its influence on the marginal sea is highly controversial and uncertain. Here we present high-resolution records of clay minerals and lanthanum to samarium (La/Sm) ratio spanning the past ~1 million years (Myr) from the Bohai and Yellow Seas, the potential sedimentary sinks of the Yellow River. Our results show a climate-driven provenance shift from small, proximal mountain rivers-dominance to the Yellow River-dominance at ~880 ka, a time period consistent with the Mid-Pleistocene orbital shift from 41-kyr to 100-kyr cyclicity. We compare the age of this provenance shift with the available age data for Yellow River headwater integration into the marginal seas and suggest that the persistent influence of the Yellow River on the Chinese marginal seas must have occurred at least ~880 ka ago. To our knowledge, this study provides the first offshore evidence on the drainage history of the Yellow River within an accurate chronology framework.Zhengquan YaoXuefa ShiShuqing QiaoQingsong LiuSelvaraj KandasamyJianxing LiuYanguang LiuJihua LiuXisheng FangJingjing GaoYanguang DouNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Zhengquan Yao
Xuefa Shi
Shuqing Qiao
Qingsong Liu
Selvaraj Kandasamy
Jianxing Liu
Yanguang Liu
Jihua Liu
Xisheng Fang
Jingjing Gao
Yanguang Dou
Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
description Abstract The Yellow River (or Huanghe and also known as China’s Sorrow in ancient times), with the highest sediment load in the world, provides a key link between continental erosion and sediment accumulation in the western Pacific Ocean. However, the exact age of its influence on the marginal sea is highly controversial and uncertain. Here we present high-resolution records of clay minerals and lanthanum to samarium (La/Sm) ratio spanning the past ~1 million years (Myr) from the Bohai and Yellow Seas, the potential sedimentary sinks of the Yellow River. Our results show a climate-driven provenance shift from small, proximal mountain rivers-dominance to the Yellow River-dominance at ~880 ka, a time period consistent with the Mid-Pleistocene orbital shift from 41-kyr to 100-kyr cyclicity. We compare the age of this provenance shift with the available age data for Yellow River headwater integration into the marginal seas and suggest that the persistent influence of the Yellow River on the Chinese marginal seas must have occurred at least ~880 ka ago. To our knowledge, this study provides the first offshore evidence on the drainage history of the Yellow River within an accurate chronology framework.
format article
author Zhengquan Yao
Xuefa Shi
Shuqing Qiao
Qingsong Liu
Selvaraj Kandasamy
Jianxing Liu
Yanguang Liu
Jihua Liu
Xisheng Fang
Jingjing Gao
Yanguang Dou
author_facet Zhengquan Yao
Xuefa Shi
Shuqing Qiao
Qingsong Liu
Selvaraj Kandasamy
Jianxing Liu
Yanguang Liu
Jihua Liu
Xisheng Fang
Jingjing Gao
Yanguang Dou
author_sort Zhengquan Yao
title Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
title_short Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
title_full Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
title_fullStr Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
title_full_unstemmed Persistent effects of the Yellow River on the Chinese marginal seas began at least ~880 ka ago
title_sort persistent effects of the yellow river on the chinese marginal seas began at least ~880 ka ago
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/c50008ea285f49bd968882c6af32b7a1
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