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
壤为温湿气
件下发育的淋溶褐,并非过去所称的半干旱件下发育的“黑
”.
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.
结果表明,该地区全新世大暖期的古壤为温湿气件下发育的淋溶褐,并非过去所称的半干旱件下发育的“黑”.
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