The impact of agriculture on tropical mountain soils in the western Peruvian Andes: a pedo-geoarchaeological study of terrace agricultural systems in the Laramate region (14.5° S)

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE Soil Pub Date : 2024-10-14 DOI:10.5194/soil-10-727-2024
Fernando Leceta, Christoph Binder, Christian Mader, Bertil Mächtle, Erik Marsh, Laura Dietrich, Markus Reindel, Bernhard Eitel, Julia Meister
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The key objectives of the investigation involved contextualizing the former agricultural management system within its geomorphological and palaeoecological framework and assessing the impact of agricultural practices on soil development and quality by comparing non-irrigated agricultural terrace soils with their undisturbed palaeo-pedological counterparts. The Laramate terrace complex, with its diverse terrace systems and varied geomorphological and geological settings, provided an ideal setting for the investigation. This comprehensive examination integrated a range of methodologies, including field surveys, digital mapping, and geomorphological analysis based on GIS and remote sensing applications, soil analysis (e.g. grain size, bulk chemistry, nutrient budget), plant microfossils (phytoliths and starch), and radiocarbon dating. In the Laramate region, the geomorphological setting of terrace agricultural systems promotes their optimal functioning. The terraces are often located in sun-sheltered areas with western exposure on middle and lower slopes or valley bottoms, which mitigate intense solar radiation, reduce evapotranspiration, increase soil moisture, and minimize erosion. The study identifies three soil groups in the Laramate region: Phaeozems, Andosols, and Anthrosols. Unique characteristics of Phaeozems challenge typical descriptions, influenced by factors such as climatic seasonality, vegetation, fauna, lithology, and aeolian inputs. The terrace soils in the Laramate region are classified as Terric Anthrosols, showing no significant degradation even after long-term use. Their balanced acidity and nutrient levels support Andean crop cultivation. Traditional non-mechanized tools, such as the chaquitaclla and rucana, likely minimized soil disruption. The terrace tillage horizons have high organic matter, indicating intentional organic manuring. Phytolith concentrations suggest intensive agricultural activity, particularly maize cultivation, with varying patterns suggesting changes in cultivation, fertilization, or mulching practices over time. Starch grain identification aligns with phytolith analyses, reinforcing maize's significance in the region. Although the use of animal-origin fertilizers requires further investigation, there is no evidence of nutrient maintenance through seasonal burning. Irrigation was minimal, and the abandonment of the pre-Hispanic cultivation system was unlikely due to soil exhaustion or terrace instability. Overall, the pre-Hispanic history of terrace agriculture in the Laramate region extends over four development phases, reflecting dynamic interactions between environmental, cultural, and agricultural factors. The initial phase, from the Formative Paracas period to the Early Nasca period (800 BCE–200 CE), witnessed the establishment of agricultural terraces with simple terrace architecture, while the Middle Horizon (600–1000 CE) saw systematic areal expansion influenced by the Wari culture. Adaptations to drier conditions included terrace agriculture on volcanic soils. The Late Intermediate period (1000–1450 CE) witnessed hydrological variability and further terrace expansion to lower altitudes and less agriculturally suitable locations. The final phase, marked by the onset of the Hispanic colonial period in 1535 CE, saw the gradual abandonment of terrace agricultural systems due to demographic shifts and reorganization of production systems. Despite this, the historical trajectory underscores the adaptability and resilience of pre-Hispanic communities in the Laramate region, showcasing innovative terrace agriculture as a means of coping with changing environmental conditions across diverse landscape units.","PeriodicalId":48610,"journal":{"name":"Soil","volume":"1 1","pages":""},"PeriodicalIF":5.8000,"publicationDate":"2024-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil","FirstCategoryId":"97","ListUrlMain":"https://doi.org/10.5194/soil-10-727-2024","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
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Abstract

Abstract. This integrated pedo-geoarchaeological study focuses on three abandoned pre-Hispanic terrace agricultural systems near Laramate in the southern Andes of Peru (14.5° S), aiming to unravel the pedological and land-use history of the region, which served as a significant agricultural hub during pre-Hispanic times. The key objectives of the investigation involved contextualizing the former agricultural management system within its geomorphological and palaeoecological framework and assessing the impact of agricultural practices on soil development and quality by comparing non-irrigated agricultural terrace soils with their undisturbed palaeo-pedological counterparts. The Laramate terrace complex, with its diverse terrace systems and varied geomorphological and geological settings, provided an ideal setting for the investigation. This comprehensive examination integrated a range of methodologies, including field surveys, digital mapping, and geomorphological analysis based on GIS and remote sensing applications, soil analysis (e.g. grain size, bulk chemistry, nutrient budget), plant microfossils (phytoliths and starch), and radiocarbon dating. In the Laramate region, the geomorphological setting of terrace agricultural systems promotes their optimal functioning. The terraces are often located in sun-sheltered areas with western exposure on middle and lower slopes or valley bottoms, which mitigate intense solar radiation, reduce evapotranspiration, increase soil moisture, and minimize erosion. The study identifies three soil groups in the Laramate region: Phaeozems, Andosols, and Anthrosols. Unique characteristics of Phaeozems challenge typical descriptions, influenced by factors such as climatic seasonality, vegetation, fauna, lithology, and aeolian inputs. The terrace soils in the Laramate region are classified as Terric Anthrosols, showing no significant degradation even after long-term use. Their balanced acidity and nutrient levels support Andean crop cultivation. Traditional non-mechanized tools, such as the chaquitaclla and rucana, likely minimized soil disruption. The terrace tillage horizons have high organic matter, indicating intentional organic manuring. Phytolith concentrations suggest intensive agricultural activity, particularly maize cultivation, with varying patterns suggesting changes in cultivation, fertilization, or mulching practices over time. Starch grain identification aligns with phytolith analyses, reinforcing maize's significance in the region. Although the use of animal-origin fertilizers requires further investigation, there is no evidence of nutrient maintenance through seasonal burning. Irrigation was minimal, and the abandonment of the pre-Hispanic cultivation system was unlikely due to soil exhaustion or terrace instability. Overall, the pre-Hispanic history of terrace agriculture in the Laramate region extends over four development phases, reflecting dynamic interactions between environmental, cultural, and agricultural factors. The initial phase, from the Formative Paracas period to the Early Nasca period (800 BCE–200 CE), witnessed the establishment of agricultural terraces with simple terrace architecture, while the Middle Horizon (600–1000 CE) saw systematic areal expansion influenced by the Wari culture. Adaptations to drier conditions included terrace agriculture on volcanic soils. The Late Intermediate period (1000–1450 CE) witnessed hydrological variability and further terrace expansion to lower altitudes and less agriculturally suitable locations. The final phase, marked by the onset of the Hispanic colonial period in 1535 CE, saw the gradual abandonment of terrace agricultural systems due to demographic shifts and reorganization of production systems. Despite this, the historical trajectory underscores the adaptability and resilience of pre-Hispanic communities in the Laramate region, showcasing innovative terrace agriculture as a means of coping with changing environmental conditions across diverse landscape units.
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农业对秘鲁安第斯山脉西部热带山地土壤的影响:对拉拉马特地区(南纬 14.5 度)阶地农业系统的地质考古学研究
摘要这项土壤地质考古学综合研究的重点是秘鲁安第斯山脉南部(南纬 14.5 度)拉拉马特附近三个被遗弃的前西班牙时期阶地农业系统,旨在揭示该地区的土壤学和土地使用史,该地区在前西班牙时期曾是一个重要的农业中心。调查的主要目标包括:在地貌学和古生态学框架内确定前农业管理系统的背景;通过比较未灌溉的农业阶地土壤和未受干扰的古植物学土壤,评估农业耕作对土壤发育和质量的影响。拉腊马特阶地综合体拥有多样的阶地系统以及不同的地貌和地质环境,为此次调查提供了理想的环境。这次全面考察综合运用了一系列方法,包括实地调查、数字测绘、基于地理信息系统和遥感应用的地貌分析、土壤分析(如粒度、体积化学、养分预算)、植物微化石(植化石和淀粉)以及放射性碳测年。在拉腊马特地区,梯田农业系统的地貌环境促进了其最佳功能的发挥。梯田通常位于中、低山坡或谷底向西照射的阳光遮蔽区,可减轻强烈的太阳辐射,减少蒸散,增加土壤湿度,最大限度地减少水土流失。研究确定了拉腊马特地区的三个土壤类型:辉绿岩、安多斯和炭质土壤。受气候季节性、植被、动物、岩性和风化输入等因素的影响,辉绿岩的独特特征对典型的描述提出了挑战。拉腊马特地区的阶地土壤被归类为 Terric Anthrosols,即使长期使用也不会出现明显退化。其均衡的酸度和营养水平支持安第斯作物的种植。传统的非机械化工具,如 chaquitaclla 和 rucana,可能最大限度地减少了对土壤的破坏。阶地耕作层的有机质含量较高,表明有意进行了有机肥料种植。植化石浓度表明农业活动密集,尤其是玉米种植,不同的模式表明种植、施肥或覆盖方法随着时间的推移而发生变化。淀粉粒的鉴定与植化石的分析结果一致,加强了玉米在该地区的重要性。虽然使用动物肥料的情况需要进一步调查,但没有证据表明通过季节性焚烧来保持养分。灌溉极少,西班牙以前的种植系统不太可能因土壤枯竭或梯田不稳定而被废弃。总体而言,拉腊马特地区前西班牙时期的梯田农业历史可分为四个发展阶段,反映了环境、文化和农业因素之间的动态互动。从形成期帕拉卡斯时期到早期纳斯卡时期(公元前 800 年至公元前 200 年)的初期阶段,人们建立了农业梯田和简单的梯田建筑,而中期地平线时期(公元前 600 年至公元前 1000 年)则受到瓦里文化的影响,出现了系统性的面积扩张。为了适应更加干旱的条件,他们在火山土壤上进行梯田农业。中期晚期(公元前 1000 年至 1450 年),水文条件多变,梯田进一步向海拔较低、农业条件较差的地方扩展。最后一个阶段以西元 1535 年西班牙殖民时期的到来为标志,由于人口结构的变化和生产系统的重组,梯田农业系统逐渐被废弃。尽管如此,历史轨迹强调了拉拉马特地区前西班牙社区的适应性和复原力,展示了创新的梯田农业作为应对不同地貌单元不断变化的环境条件的一种手段。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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