{"title":"Tracing millennia-scale erosional and depositional dynamics in desert agriculture installations using high-resolution 3D data","authors":"","doi":"10.1016/j.catena.2024.108487","DOIUrl":null,"url":null,"abstract":"<div><div>This paper follows a complete cycle of ancient desert agriculture in the arid Negev Highlands (NH), Israel. This cycle begins with pre-anthropogenic depositional and erosive processes the NH have undergone since the late Pleistocene, continues through the establishment of agricultural systems at the 3rd century CE, and ends with the restoration of erosion after the sites’ abandonment after 6-7 centuries of cultivation, till present days. Using two-millennia old markers and 10-year high-resolution 3D observations, this paper studies land process dynamics, compare long-term land degradation trends to recent ones, evaluate anthropogenic-induced influences, and follow the landscape evolution from the late-Pleistocene until present. Our results show 0.45 t ha<sup>−1</sup>/yr erosion rate during the late-Pleistocene and most of the Holocene, prior to the anthropogenic intervention. This is evidence of the intensive soil erosion processes that governed the NH during that time. Furthermore, the paper shows erosion rates of 7.8 t ha<sup>−1</sup>/yr over the last millennium and draw similarities to present ones. The results shed new light on long-term soil erosion process in desert environments and point to potential conservation strategies in similar regions. The time span of our study is uncommon and our evaluation offers a rare opportunity to analyze natural and anthropogenic effects on the environment.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":null,"pages":null},"PeriodicalIF":5.4000,"publicationDate":"2024-10-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816224006842","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
This paper follows a complete cycle of ancient desert agriculture in the arid Negev Highlands (NH), Israel. This cycle begins with pre-anthropogenic depositional and erosive processes the NH have undergone since the late Pleistocene, continues through the establishment of agricultural systems at the 3rd century CE, and ends with the restoration of erosion after the sites’ abandonment after 6-7 centuries of cultivation, till present days. Using two-millennia old markers and 10-year high-resolution 3D observations, this paper studies land process dynamics, compare long-term land degradation trends to recent ones, evaluate anthropogenic-induced influences, and follow the landscape evolution from the late-Pleistocene until present. Our results show 0.45 t ha−1/yr erosion rate during the late-Pleistocene and most of the Holocene, prior to the anthropogenic intervention. This is evidence of the intensive soil erosion processes that governed the NH during that time. Furthermore, the paper shows erosion rates of 7.8 t ha−1/yr over the last millennium and draw similarities to present ones. The results shed new light on long-term soil erosion process in desert environments and point to potential conservation strategies in similar regions. The time span of our study is uncommon and our evaluation offers a rare opportunity to analyze natural and anthropogenic effects on the environment.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.