New chronological and paleontological evidence for Paleoproterozoic eukaryote distribution and stratigraphic correlation between the Yanliao and Xiong’er basins, North China Craton

Lyu, Dan; Deng, Yan; Wang, Xiaomei; Ye, Yuntao; Pang, Ke; Miao, Lanyun; Luo, Zhendong; Zhang, Fenglian; Lu, Yuanzheng; Deng, Shuai; Wang, Huajian; Zhang, Shuichang

doi:10.1016/j.precamres.2022.106577

Cited by 15 publications

(5 citation statements)

References 76 publications

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“…The paleontology data are from Lyu et al. (2022). Tuned MS series with ∼405 and ∼100‐kyr filters (red and blue curves, bandpass with 0.00247 ± 0.00047 and 0.01 ± 0.002 cycles/kyr).…”

Section: Resultsmentioning

confidence: 99%

“…The bottom boundary age of Member 2 in the Luojiagou Section is 1642.33 ± 0.2 Ma. In Lyu et al (2022). Tuned MS series with ∼405 and ∼100-kyr filters (red and blue curves, bandpass with 0.00247 ± 0.00047 and 0.01 ± 0.002 cycles/kyr).…”

Section: Duration and Age Of The Chuanlinggou Formationmentioning

confidence: 99%

“…There are four ages in the Chuanlinggou Formation: 1,634 ± 9 Ma from intrusive rocks in the upper part (Zhang et al., 2013), 1634.8 ± 6.9 Ma from the volcanic ash layer in the middle and upper parts (Liu, Wang, et al., 2019), 1,638 ± 14 Ma from intrusive rocks in the middle part (Gao et al., 2009), and 1657.4 ± 17 Ma from detrital zircons in the bottom part (Duan et al., 2014). With further study, the SIMS zircon U‐Pb age (1647.8 ± 4.3 Ma) from a volcanic ash layer at the bottom of the Cuizhuang Formation can also be used to constrain the maximum age of the Chuanlinggou Formation (Lyu et al., 2022). Considering the age difference between the bottom and top, the estimated duration of the Chuanlinggou Formation is ∼13 ± 17 Myr.…”

Section: Geological Backgroundmentioning

confidence: 99%

“…Tuning results and astronomical time scale for the Luojiagou MS series of the Chuanlinggou Formation in the North China Craton. The paleontology data are fromLyu et al (2022). Tuned MS series with ∼405 and ∼100-kyr filters (red and blue curves, bandpass with 0.00247 ± 0.00047 and 0.01 ± 0.002 cycles/kyr).…”

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confidence: 99%

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Astronomical Forcing of Sea‐Level Changes and the History of the Solar System 1,640 Million Years Ago

Shi,

Fan,

Jin

et al. 2023

JGR Solid Earth

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The Paleoproterozoic was an important stage in the evolution of life and the environment during Earth's history. Understanding astronomical rhythms and solar system behavior in the Paleoproterozoic is often challenging. In this study, ∼190 m high‐resolution magnetic susceptibility (MS) and ∼30 m high‐resolution Ba/Al data are used to conduct cyclostratigraphic analyses of the Chuanlinggou Formation in the Yanliao Rift, North China Craton. Spectral analysis indicates significant peaks at wavelengths of 12.1–7.7, 2.8–1.6, 0.58–0.33, and 0.29–0.22 m, which matches well with the astronomical cycles predicted by Waltham for ∼1,640 Ma. A 9.9‐Myr astronomical time scale is constructed by tuning the MS series to the 405‐kyr‐long eccentricity cycle. The geological records show ∼1.56‐Myr very long eccentricity period and ∼1.0‐Myr very long obliquity period (close to 3(s4 − s3) − 2(g4 − g3) = 0) in the Paleoproterozoic. The sea‐level change curve predicted by dynamic noise models reveals a significant ∼1.0‐Myr period, indicating that sea level fluctuation may have been driven by the very long obliquity period. Bayesian inversion is used to further estimate the evolution of the ancient Earth‐Moon orbital parameters, constraining a precession rate of 87.14 ± 0.25 arcsec/year and an Earth‐Moon distance of 341,530 ± 390 km for the Paleoproterozoic Changcheng System. These results indicate that astronomical orbital forcing may have played an important role in climate and sea‐level changes in the Precambrian, increasing the understanding of the fundamentals of global sea level fluctuations, orbitally driven mechanisms and the chaotic behavior of the Precambrian solar system.

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Section: Resultsmentioning

confidence: 99%

Section: Duration and Age Of The Chuanlinggou Formationmentioning

confidence: 99%

Section: Geological Backgroundmentioning

confidence: 99%

mentioning

confidence: 99%

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Astronomical Forcing of Sea‐Level Changes and the History of the Solar System 1,640 Million Years Ago

Shi,

Fan,

Jin

et al. 2023

JGR Solid Earth

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“…The youngest U-Pb age of 1,711 ± 37 Ma (LA-ICP-MS;Hu et al, 2014) and a weighted mean U-Pb age of 1,744 ± 22 Ma (LA-ICP-MS;Wang, 2015) from detrital zircons in the lowest Yunmengshan Formation provided a maximum age of ∼1,711 Ma. Zircon U-Pb age from tuff layers of Cuizhuang and Luoyukou formations of the Luoyukou Group yielded ages of 1,647.8 ± 3.4 Ma (SIMS;Lyu et al, 2022) and 1,611 ± 8 Ma (LA-ICP-MS;Su et al, 2012), respectively. Hence, the age of the YMS ironstone can be constrained between 1711 Ma and 1,651 Ma.…”

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confidence: 99%

Marine Aluminum Phosphate–Sulfate Authigenesis as a Phosphorus Sink During Mid‐Proterozoic Oxygenation

Xie,

Lechte,

Shi

et al. 2024

Geophysical Research Letters

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Enhanced continental phosphorus input into the ocean has been suggested as a potential trigger for the transient oxygenation events during the mid‐Proterozoic; however, the response of phosphorus cycling to these marine oxygenations remains unclear. Here, we report the changes in phosphorus cycling associated with a ∼1.7 Ga transient oxygenation. Abundant authigenic aluminum phosphate–sulfate mineral svanbergite (SrAl3(PO4) (SO4) (OH)6; 8.02 ± 4.92 wt%) is identified within the ∼1.7 Ga Yunmengshan ironstones from the Xiong'er Basin, North China and other contemporaneous basins. This observation provides new evidence to support the suggestion that early diagenetic aluminum phosphate‐sulfate minerals could have represented a critical sink of marine phosphorus during the Proterozoic. We suggest that atmospheric oxygenation and concomitant changes in porewater redox chemistry may have enhanced the formation of early diagenetic phosphates, leading to a negative feedback on the oceanic phosphorus reservoir and atmospheric oxygen levels.

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A database of detrital zircon U–Pb ages in the North China Craton from the Paleoproterozoic to the early Palaeozoic

Dong,

Zuo,

Xiao

et al. 2023

Geoscience Data Journal

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U–Pb dating of detrital zircon is widely used in geology to identify the source of sediments and constrain palaeogeography and tectonic history. We collected the detrital zircon from the Paleoproterozoic to early Palaeozoic strata to understand the North China Craton's geological chronological characteristics. After screening and sorting out data information, we managed and analysed 84 papers from 2006 to 2022. Three hundred seventy‐nine samples comprising 29,431 pieces of U–Pb ages of detrital zircons gathered from the Proterozoic to Ordovician sedimentary rocks in North China Craton (NCC). Detrital zircons within five areas in the NCC, i. e., Xuhuai Basin, Zhaertai‐Bayan Obo‐Huade Basin, Yanliao Basin, Xiong'er Basin and Alxa Block, are discussed in detail. Meanwhile, we collected 2,588 pieces of Lu‐Hf detrital zircon data in the study. This Database can be helpful in understanding and explaining the tectonic evolution of the NCC from the Paleoproterozoic to the Early Palaeozoic.

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New chronological and paleontological evidence for Paleoproterozoic eukaryote distribution and stratigraphic correlation between the Yanliao and Xiong’er basins, North China Craton

Cited by 15 publications

References 76 publications

Astronomical Forcing of Sea‐Level Changes and the History of the Solar System 1,640 Million Years Ago

Astronomical Forcing of Sea‐Level Changes and the History of the Solar System 1,640 Million Years Ago

Marine Aluminum Phosphate–Sulfate Authigenesis as a Phosphorus Sink During Mid‐Proterozoic Oxygenation

A database of detrital zircon U–Pb ages in the North China Craton from the Paleoproterozoic to the early Palaeozoic

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