Late Miocene climate and time scale reconciliation: accurate orbital calibrat...
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Accurate age control of the late Tortonian to early Messinian (8.3-6.0 Ma) is essential to ascertain the origin of benthic foraminiferal d18O trends and the late Miocene carbon...
精准约束托尔托阶晚期至墨西尼阶早期(8.3~6.0 Ma)的年代控制,对于明确底栖有孔虫(benthic foraminifera)的δ¹⁸O(d18O)变化趋势的成因以及中新世晚期碳...



