FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313706053> ?p ?o ?g. }

• W4313706053 endingPage "106953" @default.
• W4313706053 startingPage "106953" @default.
• W4313706053 abstract "The early Mesoproterozoic (1.6–1.4 Ga) is a critical stage for oxygenation of Earth’s surface and early eukaryote evolution. However, the relationship between both remains uncertain. Here, we provide new carbonate associated sulfate (CAS) sulfur isotopic compositions (δ34SCAS) and trace elements from the 1.6 to 1.55 billion-year-old Gaoyuzhuang Formation in multiple sections within the Yanshan Basin, North China, to investigate the temporal and spatial variation of ocean redox conditions. New and collected δ34SCAS data from five sections (Pingquan, Kuancheng, Qianxi, Jixian and Gan'gou sections) reveal similar sulfur isotopic excursions, but the differences in absolute values indicate spatial heterogeneity of sulfur isotopic compositions, which may reflect marine low-sulfate concentrations and oceanic redox stratification. The most elevated δ34SCAS values appeared at the top of the Second Member of the Gaoyuzhuang Formation, followed by distinct negative excursions at the bottom of the Third Member, suggesting a dynamic sulfur cycle and seawater redox status during this period. Combined with previous reported carbon and sulfur isotopes and some redox proxies (e.g., Ce anomalies, manganese-rich deposit, I/(Mg + Ca) and Fe speciation), we suggest that at least two possible oxygenation events may have occurred in the Gaoyuzhuang Formation: (1) the bottom of the Second Member and (2) the bottom or middle part of the Third Member. Different sections show asynchronous timing of these events, indicating that the redox status was spatial heterogenous within the Yanshan Basin. The spatial heterogeneity may be controlled by facies and paleogeographic locations. Considering that decimeter‐scale multicellular eukaryotes are preserved in the middle part of the Third Member, we argue that oxic bottom water condition may be a critical factor for early eukaryote evolution." @default.
• W4313706053 created "2023-01-08" @default.
• W4313706053 creator A5028275500 @default.
• W4313706053 creator A5044501034 @default.
• W4313706053 creator A5051263741 @default.
• W4313706053 creator A5064608500 @default.
• W4313706053 creator A5067388487 @default.
• W4313706053 creator A5088086188 @default.
• W4313706053 date "2023-02-01" @default.
• W4313706053 modified "2023-10-11" @default.
• W4313706053 title "Dynamic seawater redox status in the early Mesoproterozoic: Evidence from trace elements and sulfur isotopic compositions of carbonate associated sulfate in multiple sections" @default.
• W4313706053 cites W1596864928 @default.
• W4313706053 cites W1965724422 @default.
• W4313706053 cites W1968654664 @default.
• W4313706053 cites W1969060008 @default.
• W4313706053 cites W1976197553 @default.
• W4313706053 cites W1980270634 @default.
• W4313706053 cites W1983119941 @default.
• W4313706053 cites W1988221255 @default.
• W4313706053 cites W1990661158 @default.
• W4313706053 cites W1990775613 @default.
• W4313706053 cites W1994930702 @default.
• W4313706053 cites W2005428926 @default.
• W4313706053 cites W2009023071 @default.
• W4313706053 cites W2011968190 @default.
• W4313706053 cites W2019028519 @default.
• W4313706053 cites W2020610733 @default.
• W4313706053 cites W2021429804 @default.
• W4313706053 cites W2021590228 @default.
• W4313706053 cites W2027595497 @default.
• W4313706053 cites W2031073903 @default.
• W4313706053 cites W2039995605 @default.
• W4313706053 cites W2040355242 @default.
• W4313706053 cites W2043024813 @default.
• W4313706053 cites W2043076811 @default.
• W4313706053 cites W2046453229 @default.
• W4313706053 cites W2047349403 @default.
• W4313706053 cites W2049273731 @default.
• W4313706053 cites W2050188617 @default.
• W4313706053 cites W2052898408 @default.
• W4313706053 cites W2053509704 @default.
• W4313706053 cites W2054607874 @default.
• W4313706053 cites W2056474046 @default.
• W4313706053 cites W2056601768 @default.
• W4313706053 cites W2057252645 @default.
• W4313706053 cites W2057391595 @default.
• W4313706053 cites W2059803873 @default.
• W4313706053 cites W2066314486 @default.
• W4313706053 cites W2068117559 @default.
• W4313706053 cites W2076797628 @default.
• W4313706053 cites W2077125391 @default.
• W4313706053 cites W2084961153 @default.
• W4313706053 cites W2086551038 @default.
• W4313706053 cites W2097417202 @default.
• W4313706053 cites W2098778302 @default.
• W4313706053 cites W2098968250 @default.
• W4313706053 cites W2106970725 @default.
• W4313706053 cites W2107212167 @default.
• W4313706053 cites W2107225219 @default.
• W4313706053 cites W2118715042 @default.
• W4313706053 cites W2119610316 @default.
• W4313706053 cites W2133038839 @default.
• W4313706053 cites W2133159913 @default.
• W4313706053 cites W2136339807 @default.
• W4313706053 cites W2147521920 @default.
• W4313706053 cites W2149161924 @default.
• W4313706053 cites W2161150020 @default.
• W4313706053 cites W2165303310 @default.
• W4313706053 cites W2189652106 @default.
• W4313706053 cites W2208442684 @default.
• W4313706053 cites W2265295360 @default.
• W4313706053 cites W2283582373 @default.
• W4313706053 cites W2327650751 @default.
• W4313706053 cites W2334477362 @default.
• W4313706053 cites W2396542812 @default.
• W4313706053 cites W2402234408 @default.
• W4313706053 cites W2417936857 @default.
• W4313706053 cites W2467732495 @default.
• W4313706053 cites W2467903192 @default.
• W4313706053 cites W2498952693 @default.
• W4313706053 cites W2560962463 @default.
• W4313706053 cites W2583277763 @default.
• W4313706053 cites W2593983222 @default.
• W4313706053 cites W2600432865 @default.
• W4313706053 cites W2613520117 @default.
• W4313706053 cites W2625465422 @default.
• W4313706053 cites W2738937425 @default.
• W4313706053 cites W2758226547 @default.
• W4313706053 cites W2769812936 @default.
• W4313706053 cites W2788861900 @default.
• W4313706053 cites W2800282409 @default.
• W4313706053 cites W2883348468 @default.
• W4313706053 cites W2883969747 @default.
• W4313706053 cites W2884889610 @default.
• W4313706053 cites W2889659469 @default.
• W4313706053 cites W2889885567 @default.
• W4313706053 cites W2902442689 @default.
• W4313706053 cites W2938051254 @default.

• next