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Organic Fertilization and Sufficient Nutrient Status in Prehistoric Agriculture? – Indications from Multi-Proxy Analyses of Archaeological Topsoil Relicts

机译:史前农业的有机肥和充足的营养状况? –来自考古表土遗迹的多代理分析的指示

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摘要

Neolithic and Bronze Age topsoil relicts revealed enhanced extractable phosphorus (P) and plant available inorganic P fractions, thus raising the question whether there was targeted soil amelioration in prehistoric times. This study aimed (i) at assessing the overall nutrient status and the soil organic matter content of these arable topsoil relicts, and (ii) at tracing ancient soil fertilizing practices by respective stable isotope and biomarker analyses. Prehistoric arable topsoils were preserved in archaeological pit fillings, whereas adjacent subsoils served as controls. One Early Weichselian humic zone represented the soil status before the introduction of agriculture. Recent topsoils served as an additional reference. The applied multi-proxy approach comprised total P and micronutrient contents, stable N isotope ratios, amino acid, steroid, and black carbon analyses as well as soil color measurements. Total contents of P and selected micronutrients (I, Cu, Mn, Mo, Se, Zn) of the arable soil relicts were above the limits for which nutrient deficiencies could be assumed. All pit fillings exhibited elevated δ15N values close to those of recent topsoils (δ15N>6 to 7‰), giving first hints for prehistoric organic N-input. Ancient legume cultivation as a potential source for N input could not be verified by means of amino acid analysis. In contrast, bile acids as markers for faecal input exhibited larger concentrations in the pit fillings compared with the reference and control soils indicating faeces (i.e. manure) input to Neolithic arable topsoils. Also black carbon contents were elevated, amounting up to 38% of soil organic carbon, therewith explaining the dark soil color in the pit fillings and pointing to inputs of burned biomass. The combination of different geochemical analyses revealed a sufficient nutrient status of prehistoric arable soils, as well as signs of amelioration (inputs of organic material like charcoal and faeces-containing manure).
机译:新石器时代和青铜时代的表层土壤遗迹显示出可提取的磷(P)和植物可用的无机P组分增加,从而引发了一个问题,即史前时期是否有针对性的土壤改良。这项研究旨在(i)评估这些可耕表土遗迹的总体营养状况和土壤有机质含量,以及(ii)通过相应的稳定同位素和生物标记分析追踪古代土壤施肥方法。史前的耕作表层土壤保存在考古坑中,而邻近的地下土壤则作为对照。引入农业之前,魏氏早期的一个腐殖质带代表了土壤状况。最近的表土作为补充参考。应用的多代理方法包括总磷和微量营养素含量,稳定的氮同位素比,氨基酸,类固醇和黑碳分析以及土壤颜色测量。耕地土壤中的磷和选定的微量元素(I,Cu,Mn,Mo,Se,Zn)的总含量均高于可以假设的养分不足的极限。所有基坑充填物的δ 15 N值均升高,接近最近表层土壤(δ 15 N> 6至7‰)的值,这为史前有机氮输入提供了第一个提示。氨基酸分析无法证实古代豆科植物作为氮输入的潜在来源。相反,与参考土壤和对照土壤相比,作为粪便输入标记的胆汁酸在粪便中表现出更高的浓度,表明粪便(即肥料)输入新石器时代可耕层表层土壤。黑碳含量也增加了,最多占土壤有机碳的38%,从而解释了矿坑填充物中的深色土壤颜色,并指出了燃烧的生物质的输入。不同地球化学分析的结合显示出史前可耕土壤的足够养分状况,并且有改善的迹象(输入有机材料,如木炭和粪便)。

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