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的古土壤为温湿气候条件下发育的淋溶褐土,
非过去所称的半干旱条件下发育的“黑垆土”.
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的古土壤为温湿气候条件下发育的淋溶褐土,非过去所称的半干旱条件下发育的“黑垆土”.
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