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
明,该地区全新世大暖期的
土壤为温湿气候条件下发育的淋溶褐土,并非过去所称的半干旱条件下发育的“黑垆土”.
土壤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.
结果明,该地区全新世大暖期的土壤为温湿气候条件下发育的淋溶褐土,并非过去所称的半干旱条件下发育的“黑垆土”.
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