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
湿气候条件下发育淋溶褐土,
非
去所称半干旱条件下发育“黑垆土”.
,高型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湿气候条件下发育淋溶褐土,非去所称半干旱条件下发育“黑垆土”.
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