Formation of the upper reaches of the Yellow River: Provenance evidence from the strata of the Yellow River sedimentary basin

The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital materials within the Yellow River sedimentary basins outside the Tibetan Plateau can provide important evidence for...

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Published inGlobal and planetary change Vol. 229; p. 104224
Main Authors Li, Baofeng, Feng, Qi, Wang, Xin, Li, Zaijun, Wang, Fei, Zhao, Chenguang, Yu, Tengfei, Chen, Weiyu
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.10.2023
Subjects
basins
China
climate change
detritus
drainage systems
East Asian monsoon system
evolution
Geochemical fingerprint
Heavy mineral assemblage
monsoon season
Pleistocene epoch
Pliocene epoch
provenance
Sedimentary basin
tectonics
Upper reaches of the Yellow River
Yellow River
China
Yellow River
Sedimentary basin
Upper reaches of the Yellow River
Geochemical fingerprint
Heavy mineral assemblage
East Asian monsoon system
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Abstract The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital materials within the Yellow River sedimentary basins outside the Tibetan Plateau can provide important evidence for resolving this issue. We conducted geochemical and heavy mineral studies of the sediments from a 274.60-m-long drill core from the Hetao Basin, the largest sedimentary basin in the upper reaches of the Yellow River. Our results suggest that detritus from the northeastern margin of Tibetan Plateau dominated the sedimentation within the Hetao Basin since ~1.68 Ma, with an average contribution of 68%. This suggests that the Yellow River that connected the northeastern margin of the Tibetan Plateau and the Hetao Basin was formed by at least the Early Pleistocene. Detritus from the distal Gobi-Altay Mts. and from the proximal Ordos Plateau and the Yin Mts. had average contributions of 28% and 4%, respectively. We conclude that the variations in the relative contributions of these three sources were related not only to the tectonic uplift of the Tibetan Plateau that driving integration of the Yellow River drainage system but also to the evolution of the East Asian monsoon system, as well as to global climate change. [Display omitted] •NE margin of Tibetan Plateau controlled Hetao Basin sedimentation since ~1.68 Ma•Yellow River connected Tibetan Plateau and Hetao Basin in the Early Pleistocene•Enhanced monsoon led to more debris from distal aeolian and proximal sources
AbstractList The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital materials within the Yellow River sedimentary basins outside the Tibetan Plateau can provide important evidence for resolving this issue. We conducted geochemical and heavy mineral studies of the sediments from a 274.60-m-long drill core from the Hetao Basin, the largest sedimentary basin in the upper reaches of the Yellow River. Our results suggest that detritus from the northeastern margin of Tibetan Plateau dominated the sedimentation within the Hetao Basin since ~1.68 Ma, with an average contribution of 68%. This suggests that the Yellow River that connected the northeastern margin of the Tibetan Plateau and the Hetao Basin was formed by at least the Early Pleistocene. Detritus from the distal Gobi-Altay Mts. and from the proximal Ordos Plateau and the Yin Mts. had average contributions of 28% and 4%, respectively. We conclude that the variations in the relative contributions of these three sources were related not only to the tectonic uplift of the Tibetan Plateau that driving integration of the Yellow River drainage system but also to the evolution of the East Asian monsoon system, as well as to global climate change. [Display omitted] •NE margin of Tibetan Plateau controlled Hetao Basin sedimentation since ~1.68 Ma•Yellow River connected Tibetan Plateau and Hetao Basin in the Early Pleistocene•Enhanced monsoon led to more debris from distal aeolian and proximal sources
The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital materials within the Yellow River sedimentary basins outside the Tibetan Plateau can provide important evidence for resolving this issue. We conducted geochemical and heavy mineral studies of the sediments from a 274.60-m-long drill core from the Hetao Basin, the largest sedimentary basin in the upper reaches of the Yellow River. Our results suggest that detritus from the northeastern margin of Tibetan Plateau dominated the sedimentation within the Hetao Basin since ~1.68 Ma, with an average contribution of 68%. This suggests that the Yellow River that connected the northeastern margin of the Tibetan Plateau and the Hetao Basin was formed by at least the Early Pleistocene. Detritus from the distal Gobi-Altay Mts. and from the proximal Ordos Plateau and the Yin Mts. had average contributions of 28% and 4%, respectively. We conclude that the variations in the relative contributions of these three sources were related not only to the tectonic uplift of the Tibetan Plateau that driving integration of the Yellow River drainage system but also to the evolution of the East Asian monsoon system, as well as to global climate change.
ArticleNumber 104224
Author Wang, Fei
Li, Zaijun
Wang, Xin
Feng, Qi
Zhao, Chenguang
Li, Baofeng
Chen, Weiyu
Yu, Tengfei
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  givenname: Weiyu
  surname: Chen
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  organization: Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
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Upper reaches of the Yellow River
Geochemical fingerprint
Heavy mineral assemblage
East Asian monsoon system
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Snippet The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining...
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SubjectTerms basins
China
climate change
detritus
drainage systems
East Asian monsoon system
evolution
Geochemical fingerprint
Heavy mineral assemblage
monsoon season
Pleistocene epoch
Pliocene epoch
provenance
Sedimentary basin
tectonics
Upper reaches of the Yellow River
Yellow River
Title Formation of the upper reaches of the Yellow River: Provenance evidence from the strata of the Yellow River sedimentary basin
URI https://dx.doi.org/10.1016/j.gloplacha.2023.104224
https://www.proquest.com/docview/3153706861
Volume 229
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