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2007-2008年贵州碳酸盐岩风化壳238U-234U-230Th数据
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Stable carbon and oxygen isotope record od IODP Hole 306-U1313
The Mid-Pleistocene transition (MPT) was the time when quasi-periodic (? 100 kyr), high-amplitude glacial variability developed in the absence of any significant change in the character of orbital for
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Table S1-Xiamaling Li isotope data
The raw data of Silicate weathering drove a reversed latitudinal oxygen gradient in the mid-Proterozoic ocean
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