These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.
结果表明,该地区全新世大暖期
古土壤为温湿气候条件
淋溶褐土,
非过去所称
旱条件“黑垆土”.
,高温型These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.
结果表明,该地区全新世大暖期古土壤为温湿气候条件淋溶褐土,非过去所称旱条件“黑垆土”.
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