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• W4214828503 endingPage "117420" @default.
• W4214828503 startingPage "117420" @default.
• W4214828503 abstract "The early Cambrian was a critical period of Earth history, marked by explosive diversification of metazoans and several profound changes in Earth's surface environments and global climate. A valid temporal framework for the early Cambrian Period and across the major bio-events is poorly constrained, and the key underlying forcings of million-year (Myr) scale sea-level variations in a greenhouse lacking polar ice sheets are still disputed. Here, the high-resolution gamma-ray logs (GR) and Fe/Al records are utilized to conduct cyclostratigraphic analysis of the early Cambrian Stage 2-Stage 3 Qiongzhusi Formation of the Well A borehole in South China. A ∼10.8 Myr-long high-resolution astronomical time scale across Stage 2-Stage 3 is developed by astronomical tuning of gamma-ray logs and Fe/Al series to the stable 405-kyr long-eccentricity cycles. The Myr-scale sea-level fluctuations in the early Cambrian greenhouse are reconstructed through the sedimentary noise modeling of the 405-tuned GR series and agree with sequence stratigraphic interpretations, lithofacies stacking patterns, and depositional environment changes. The antiphase correlation of filtered ∼1.5 Myr cycles of sedimentary noise curves with the ∼1.5 Myr obliquity modulation cycles demonstrates that the variations in land-ocean water exchange linked to changes in poleward moisture and heat transport dominated by ∼1.5 Myr obliquity modulation cycles may be a primary driver for eustasy during non-glacial early Cambrian period. A new resonance state in the early Cambrian Stage 2-Stage 3, manifested by ∼1.5 Myr eccentricity: ∼1.5 Myr obliquity, could be mainly associated with the Earth-Mars secular resonance and constrain the chaotic evolution of the Solar System in deep time. Two independent approaches are employed to reconstruct the history of Earth-Moon system characteristics, including the precession constant, the Earth-Moon distance and the day length. Our results enhance knowledge of the connection of Myr-scale sea-level variations to astronomically induced climate change under greenhouse climate and provide new empirical constraints on the chaotic motion of the Solar System and the evolution of the Earth-Moon System in deep time." @default.
• W4214828503 created "2022-03-05" @default.
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• W4214828503 date "2022-04-01" @default.
• W4214828503 modified "2023-10-14" @default.
• W4214828503 title "Orbitally-paced climate change in the early Cambrian and its implications for the history of the Solar System" @default.
• W4214828503 cites W1262116572 @default.
• W4214828503 cites W1632573925 @default.
• W4214828503 cites W1821783426 @default.
• W4214828503 cites W1942528694 @default.
• W4214828503 cites W1974781681 @default.
• W4214828503 cites W1983657072 @default.
• W4214828503 cites W1989230282 @default.
• W4214828503 cites W1992272796 @default.
• W4214828503 cites W2005740401 @default.
• W4214828503 cites W2007443159 @default.
• W4214828503 cites W2008612575 @default.
• W4214828503 cites W2014398088 @default.
• W4214828503 cites W2014966970 @default.
• W4214828503 cites W2017977879 @default.
• W4214828503 cites W2022414534 @default.
• W4214828503 cites W2022545034 @default.
• W4214828503 cites W2023128955 @default.
• W4214828503 cites W2031683674 @default.
• W4214828503 cites W2035492077 @default.
• W4214828503 cites W2036834746 @default.
• W4214828503 cites W2036937372 @default.
• W4214828503 cites W2042526900 @default.
• W4214828503 cites W2047674868 @default.
• W4214828503 cites W2049280696 @default.
• W4214828503 cites W2056568207 @default.
• W4214828503 cites W2057260077 @default.
• W4214828503 cites W2059995708 @default.
• W4214828503 cites W2062118272 @default.
• W4214828503 cites W2064523628 @default.
• W4214828503 cites W2066086830 @default.
• W4214828503 cites W2067780174 @default.
• W4214828503 cites W2078501877 @default.
• W4214828503 cites W2079266112 @default.
• W4214828503 cites W2080600282 @default.
• W4214828503 cites W2080614756 @default.
• W4214828503 cites W2081316493 @default.
• W4214828503 cites W2086944192 @default.
• W4214828503 cites W2088017846 @default.
• W4214828503 cites W2092178859 @default.
• W4214828503 cites W2092650147 @default.
• W4214828503 cites W2094411973 @default.
• W4214828503 cites W2095142768 @default.
• W4214828503 cites W2105929990 @default.
• W4214828503 cites W2107030987 @default.
• W4214828503 cites W2109911189 @default.
• W4214828503 cites W2111414198 @default.
• W4214828503 cites W2114374455 @default.
• W4214828503 cites W2123014038 @default.
• W4214828503 cites W2140477756 @default.
• W4214828503 cites W2143533995 @default.
• W4214828503 cites W2146841676 @default.
• W4214828503 cites W2153985161 @default.
• W4214828503 cites W2157222225 @default.
• W4214828503 cites W2157528384 @default.
• W4214828503 cites W2163029943 @default.
• W4214828503 cites W2163452924 @default.
• W4214828503 cites W2167905111 @default.
• W4214828503 cites W2169423948 @default.
• W4214828503 cites W2180466051 @default.
• W4214828503 cites W2270990278 @default.
• W4214828503 cites W2294270396 @default.
• W4214828503 cites W2300731342 @default.
• W4214828503 cites W2461115089 @default.
• W4214828503 cites W2529307548 @default.
• W4214828503 cites W2586719288 @default.
• W4214828503 cites W2587456915 @default.
• W4214828503 cites W2590587458 @default.
• W4214828503 cites W2741131109 @default.
• W4214828503 cites W2742806799 @default.
• W4214828503 cites W2745205878 @default.
• W4214828503 cites W2791051032 @default.
• W4214828503 cites W2793886337 @default.
• W4214828503 cites W2797237939 @default.
• W4214828503 cites W2803936233 @default.
• W4214828503 cites W2806299100 @default.
• W4214828503 cites W2807110188 @default.
• W4214828503 cites W2892225831 @default.
• W4214828503 cites W2902724361 @default.
• W4214828503 cites W2904216818 @default.
• W4214828503 cites W2905857998 @default.
• W4214828503 cites W2910702274 @default.
• W4214828503 cites W2916973835 @default.
• W4214828503 cites W2919969996 @default.

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