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
壤为温湿气候条件下发育淋溶褐,
非过去所称半干旱条件下发育“黑
”.
,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壤为温湿气候条件下发育淋溶褐,非过去所称半干旱条件下发育“黑”.
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