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史前农业中的有机施肥与充足养分状况?——来自考古表层土遗迹多指标分析的证据

Organic fertilization and sufficient nutrient status in prehistoric agriculture?--Indications from multi-proxy analyses of archaeological topsoil relicts.

作者信息

Lauer Franziska, Prost Katharina, Gerlach Renate, Pätzold Stefan, Wolf Mareike, Urmersbach Sarah, Lehndorff Eva, Eckmeier Eileen, Amelung Wulf

机构信息

Institute of Crop Science and Resource Conservation - Soil Science and Soil Ecology, University of Bonn, Bonn, Germany.

Archaeological Heritage Management Rhineland (LVR-Amt für Bodendenkmalpflege im Rheinland), Bonn, Germany.

出版信息

PLoS One. 2014 Sep 2;9(9):e106244. doi: 10.1371/journal.pone.0106244. eCollection 2014.

Abstract

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).

摘要

新石器时代和青铜时代的表层土壤遗迹显示出可提取磷(P)和植物可利用无机磷组分增加,因此引发了史前时期是否存在有针对性的土壤改良这一问题。本研究旨在:(i)评估这些可耕表层土壤遗迹的整体养分状况和土壤有机质含量;(ii)通过各自的稳定同位素和生物标志物分析追溯古代土壤施肥实践。史前可耕表层土壤保存在考古坑填充物中,而相邻的下层土壤用作对照。一个早魏克塞尔间冰期腐殖质层代表了农业引入之前的土壤状况。现代表层土壤用作额外参考。所采用的多指标方法包括总磷和微量营养素含量、稳定氮同位素比率、氨基酸、类固醇和黑碳分析以及土壤颜色测量。可耕土壤遗迹的总磷和选定微量营养素(碘、铜、锰、钼、硒、锌)含量高于可假定存在养分缺乏的限值。所有坑填充物的δ15N值均升高,接近现代表层土壤(δ15N>6至7‰),这首次暗示了史前有机氮输入。通过氨基酸分析无法证实古代豆类种植作为氮输入的潜在来源。相比之下,作为粪便输入标志物的胆汁酸在坑填充物中的浓度高于参考土壤和对照土壤,表明新石器时代可耕表层土壤有粪便(即粪肥)输入。黑碳含量也升高,占土壤有机碳的38%,从而解释了坑填充物中土壤颜色较深的原因,并表明有燃烧生物质的输入。不同地球化学分析的结合揭示了史前可耕土壤养分状况充足,以及改良迹象(如木炭和含粪便粪肥等有机物质的输入)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/40de/4152168/b3ce32914736/pone.0106244.g001.jpg

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