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- W4313201296 abstract "The Tibetan region underwent diachronous differential rises during the Cenozoic era. Its elevation history is critical for understanding the processes of mountain building, and for evaluating its climatic effects on atmospheric circulations. However, knowledge of paleoenvironment and paleoelevation in different geological domains of the Tibetan Plateau is still limited. Here we provide chronology of lacustrine deposits of the Upper Dingqing Formation in the Lunpola Basin in Central Tibet, which yields a middle Miocene age (15–12 Ma). Both stable isotope and palynological records indicate a climatic transition at ∼13.8 Ma marked by a change towards a cooler and drier climate after the Middle Miocene Climate Transition driven by global climatic cooling. Pollen and spore assemblages suggest that the vegetation was dominated by mixed coniferous–broadleaved forest with some grasslands. New palynological elevation reconstructions constrained by the co-existence approach yield a maximum paleo-elevation of 3100–3600 m (average 3350 m) of the Lunpola Basin, which was consistent with a maximum elevation of 3400 m based on floating-leaf plants. Our new data do not support previous views that the Lunpola Basin achieved its current elevation as early as the late Eocene or early Oligocene, but instead we suggest there has been a rise of up to 1200 m since 12 million years ago. Our results bring new light on both the paleoenvironmental reconstructions and the paleo-elevation estimates of the Lunpola Basin, Central Tibet." @default.
- W4313201296 created "2023-01-06" @default.
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- W4313201296 creator A5070256737 @default.
- W4313201296 date "2023-01-01" @default.
- W4313201296 modified "2023-10-18" @default.
- W4313201296 title "Middle Miocene paleoenvironmental change and paleoelevation of the Lunpola Basin, Central Tibet" @default.
- W4313201296 cites W1521156282 @default.
- W4313201296 cites W1675802314 @default.
- W4313201296 cites W1845282954 @default.
- W4313201296 cites W1944076124 @default.
- W4313201296 cites W1972277091 @default.
- W4313201296 cites W1973326864 @default.
- W4313201296 cites W1974467019 @default.
- W4313201296 cites W1976727495 @default.
- W4313201296 cites W1979505218 @default.
- W4313201296 cites W1981281557 @default.
- W4313201296 cites W1984136939 @default.
- W4313201296 cites W1986254813 @default.
- W4313201296 cites W1986566404 @default.
- W4313201296 cites W1990973700 @default.
- W4313201296 cites W1995968891 @default.
- W4313201296 cites W1999805636 @default.
- W4313201296 cites W2000829620 @default.
- W4313201296 cites W2001912393 @default.
- W4313201296 cites W2004295803 @default.
- W4313201296 cites W2005596384 @default.
- W4313201296 cites W2011834231 @default.
- W4313201296 cites W2016407391 @default.
- W4313201296 cites W2017913935 @default.
- W4313201296 cites W2021266129 @default.
- W4313201296 cites W2024642111 @default.
- W4313201296 cites W2030008065 @default.
- W4313201296 cites W2030357043 @default.
- W4313201296 cites W2030510161 @default.
- W4313201296 cites W2031232581 @default.
- W4313201296 cites W2033736722 @default.
- W4313201296 cites W2034597289 @default.
- W4313201296 cites W2034795484 @default.
- W4313201296 cites W2035901548 @default.
- W4313201296 cites W2036172342 @default.
- W4313201296 cites W2036345756 @default.
- W4313201296 cites W2038918624 @default.
- W4313201296 cites W2046274250 @default.
- W4313201296 cites W2046303793 @default.
- W4313201296 cites W2049652180 @default.
- W4313201296 cites W2052031839 @default.
- W4313201296 cites W2054668907 @default.
- W4313201296 cites W2055002961 @default.
- W4313201296 cites W2055196216 @default.
- W4313201296 cites W2055442076 @default.
- W4313201296 cites W2057822153 @default.
- W4313201296 cites W2058864054 @default.
- W4313201296 cites W2059997981 @default.
- W4313201296 cites W2062242054 @default.
- W4313201296 cites W2063646261 @default.
- W4313201296 cites W2063833788 @default.
- W4313201296 cites W2064924997 @default.
- W4313201296 cites W2071184501 @default.
- W4313201296 cites W2075694434 @default.
- W4313201296 cites W2079812658 @default.
- W4313201296 cites W2081315541 @default.
- W4313201296 cites W2085154603 @default.
- W4313201296 cites W2089967373 @default.
- W4313201296 cites W2092885295 @default.
- W4313201296 cites W2093114941 @default.
- W4313201296 cites W2094108291 @default.
- W4313201296 cites W2101255003 @default.
- W4313201296 cites W2114856901 @default.
- W4313201296 cites W2115518283 @default.
- W4313201296 cites W2116868398 @default.
- W4313201296 cites W2126553883 @default.
- W4313201296 cites W2127673213 @default.
- W4313201296 cites W2129560702 @default.
- W4313201296 cites W2130176715 @default.
- W4313201296 cites W2135372112 @default.
- W4313201296 cites W2135418998 @default.
- W4313201296 cites W2136389603 @default.
- W4313201296 cites W2137582175 @default.
- W4313201296 cites W2141023161 @default.
- W4313201296 cites W2153893445 @default.
- W4313201296 cites W2175897226 @default.
- W4313201296 cites W2203727367 @default.
- W4313201296 cites W2288671490 @default.
- W4313201296 cites W2527933011 @default.
- W4313201296 cites W2568471228 @default.
- W4313201296 cites W2586276026 @default.
- W4313201296 cites W2605276217 @default.
- W4313201296 cites W2608823166 @default.
- W4313201296 cites W2790669158 @default.
- W4313201296 cites W2800436021 @default.
- W4313201296 cites W2887539879 @default.