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- W4283278577 endingPage "103875" @default.
- W4283278577 startingPage "103875" @default.
- W4283278577 abstract "The early Eocene is thought to be the warmest period of the Cenozoic Era, with global temperatures ~10 °C higher than today. Few studies have focused on the paleoclimatic history of the early Eocene southeastern Neo-Tethys Ocean despite its tectonic significance. Here, we report new geochemical data that reveal the paleoclimate conditions of the early Eocene (~ 53.7 to 52.6 Ma) from the Qumiba section in the Tingri region of the southern Tibetan Plateau, China, which likely represents the youngest marine strata in the southeastern Neo-Tethys Ocean. The studied Qumiba section consists of the Enba and Zhaguo Formations characterized by silty marls, mudstones and thin layers of lithic sandstones. The paleoclimate and paleoenvironment history of the Qumiba section is reconstructed using stable carbon and oxygen isotopes of marine carbonates (δ13Ccarb and δ18Ocarb), major, trace and rare earth elements. At least one early Eocene hyperthermal event (I1 or I2; ~53.6 Ma) has been recorded in the Qumiba section supported by abrupt negative excursions in δ13Ccarb in Unit 2. This is further supported by enhanced chemical weathering (e.g., chemical index of alteration), which can be attributed to increased temperature and precipitation. The continued negative δ13Ccarb excursions in Unit 3 may have been caused by the release of 13C-depleted carbon from volcanic activities. The volcanic inputs may have increased nutrient availability and promoted marine primary productivity (e.g., higher enrichment factors of P, Ba, Ni and Cu). Furthermore, the basin may have experienced bottom water anoxia as suggested by the redox-sensitive proxies (e.g., higher enrichment factors of U and V and Ce/Ce*) during this period (Unit 3). Our findings support warming-induced changes in paleoenvironmental conditions in the southeastern Neo-Tethys Ocean during the early Eocene." @default.
- W4283278577 created "2022-06-23" @default.
- W4283278577 creator A5000570560 @default.
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- W4283278577 creator A5052148680 @default.
- W4283278577 creator A5072298069 @default.
- W4283278577 creator A5088412303 @default.
- W4283278577 date "2022-08-01" @default.
- W4283278577 modified "2023-10-18" @default.
- W4283278577 title "Reconstruction of the early Eocene paleoclimate and paleoenvironment of the southeastern Neo-Tethys Ocean" @default.
- W4283278577 cites W1488283778 @default.
- W4283278577 cites W1601934020 @default.
- W4283278577 cites W1965256236 @default.
- W4283278577 cites W1965701586 @default.
- W4283278577 cites W1966207504 @default.
- W4283278577 cites W1966527093 @default.
- W4283278577 cites W1971284908 @default.
- W4283278577 cites W1973194721 @default.
- W4283278577 cites W1976467450 @default.
- W4283278577 cites W1980055929 @default.
- W4283278577 cites W1987562178 @default.
- W4283278577 cites W1988627424 @default.
- W4283278577 cites W1990381305 @default.
- W4283278577 cites W1994549679 @default.
- W4283278577 cites W1997698506 @default.
- W4283278577 cites W1998759128 @default.
- W4283278577 cites W1999178866 @default.
- W4283278577 cites W2000246025 @default.
- W4283278577 cites W2001073984 @default.
- W4283278577 cites W2006485243 @default.
- W4283278577 cites W2011611022 @default.
- W4283278577 cites W2011801766 @default.
- W4283278577 cites W2011834231 @default.
- W4283278577 cites W2012396559 @default.
- W4283278577 cites W2013428409 @default.
- W4283278577 cites W2013602802 @default.
- W4283278577 cites W2015876559 @default.
- W4283278577 cites W2016223358 @default.
- W4283278577 cites W2021263586 @default.
- W4283278577 cites W2021793070 @default.
- W4283278577 cites W2025750942 @default.
- W4283278577 cites W2027225510 @default.
- W4283278577 cites W2029120025 @default.
- W4283278577 cites W2029401070 @default.
- W4283278577 cites W2029664473 @default.
- W4283278577 cites W2031964716 @default.
- W4283278577 cites W2033052384 @default.
- W4283278577 cites W2033700933 @default.
- W4283278577 cites W2035028723 @default.
- W4283278577 cites W2037703975 @default.
- W4283278577 cites W2038631041 @default.
- W4283278577 cites W2046892047 @default.
- W4283278577 cites W2050089429 @default.
- W4283278577 cites W2053615902 @default.
- W4283278577 cites W2055743298 @default.
- W4283278577 cites W2057391595 @default.
- W4283278577 cites W2057482300 @default.
- W4283278577 cites W2062678238 @default.
- W4283278577 cites W2063078603 @default.
- W4283278577 cites W2064819099 @default.
- W4283278577 cites W2066648098 @default.
- W4283278577 cites W2066968027 @default.
- W4283278577 cites W2067413419 @default.
- W4283278577 cites W2070331432 @default.
- W4283278577 cites W2073739165 @default.
- W4283278577 cites W2079110578 @default.
- W4283278577 cites W2082481175 @default.
- W4283278577 cites W2086386094 @default.
- W4283278577 cites W2088019626 @default.
- W4283278577 cites W2098060258 @default.
- W4283278577 cites W2098108672 @default.
- W4283278577 cites W2098548636 @default.
- W4283278577 cites W2104224684 @default.
- W4283278577 cites W2109580702 @default.
- W4283278577 cites W2116391933 @default.
- W4283278577 cites W2118188170 @default.
- W4283278577 cites W2123594378 @default.
- W4283278577 cites W2124460270 @default.
- W4283278577 cites W2126102606 @default.
- W4283278577 cites W2130957548 @default.
- W4283278577 cites W2132223903 @default.
- W4283278577 cites W2132448110 @default.
- W4283278577 cites W2144270976 @default.
- W4283278577 cites W2151368777 @default.
- W4283278577 cites W2159054286 @default.
- W4283278577 cites W2160329343 @default.
- W4283278577 cites W2160384760 @default.
- W4283278577 cites W2167010628 @default.
- W4283278577 cites W2168866313 @default.
- W4283278577 cites W2170894966 @default.
- W4283278577 cites W2247098479 @default.
- W4283278577 cites W2276728729 @default.
- W4283278577 cites W2346816322 @default.
- W4283278577 cites W2349305435 @default.
- W4283278577 cites W2490144373 @default.
- W4283278577 cites W2513508950 @default.