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The is a geological formation in the Gansu province of China that spans up to 100 m thick and is widely distributed within the , with a paleomagnetic age of between 11 and 6.4 Mya (Upper/Late Miocene). The formation is divided into three parts which represent three different ages, generally referred to as the "upper part" (youngest, at 6-7 mya), the "middle part" (intermediate, at 9 to 7.6 mya. Also known as the Dashengou fauna, and the "lower part" (oldest).

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  • The is a geological formation in the Gansu province of China that spans up to 100 m thick and is widely distributed within the , with a paleomagnetic age of between 11 and 6.4 Mya (Upper/Late Miocene). The formation is divided into three parts which represent three different ages, generally referred to as the "upper part" (youngest, at 6-7 mya), the "middle part" (intermediate, at 9 to 7.6 mya. Also known as the Dashengou fauna, and the "lower part" (oldest). (en)
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  • The is a geological formation in the Gansu province of China that spans up to 100 m thick and is widely distributed within the , with a paleomagnetic age of between 11 and 6.4 Mya (Upper/Late Miocene). The formation is divided into three parts which represent three different ages, generally referred to as the "upper part" (youngest, at 6-7 mya), the "middle part" (intermediate, at 9 to 7.6 mya. Also known as the Dashengou fauna, and the "lower part" (oldest). (en)
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  • Paleobiota of the Liushu Formation (en)
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