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黄土高原自然植被的土壤有机碳同位素证据

DOI: 10.3969/j.issn.1001-7410.2011.03.14, PP. 506-513

Keywords: 黄土高原,C4植物相对丰度,年均温,年均降水量

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Abstract:

根据黄土高原现代表土有机碳同位素(δ13CSOM)数据,结合前人关于末次间冰期和全新世中期的分析结果,研究这3个特征时期C4相对生物量(C4%)的空间变化特征。结果表明,3个时期黄土高原C4%均由东南(33%,25%和12%)向西北(0%)递减。10%等值线在末次间冰期大致位于交道-泾川西北、西峰东南一带;到全新世西部向南推进,大致位于交道-洛川-旬邑以西北、西峰-灵台以东南一带;而现今比全新世时期向东南推移约60km,退至黄陵以西北、彬县-延安以东南一带。全新世与末次间冰期温度和降水的不同可能是植被差异的主要原因。现代C4%较末次间冰期和全新世中期有较明显的降低,可能与较高的大气CO2浓度、较低的温度和干旱化有关。由于上述3个特征时期黄土高原东南地区均以C4草本植物为主,西北地区C3植物比例的增加亦为C3草本植物比例的增加。

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