G. Fernandez, Thais Baptista da Rocha, José Maria Landin Dominguez, Sérgio Cadena de Vasconcelos, Gilberto Tavares de Macedo Dias, André da Costa, M. S. Figueiredo, Alberto Garcia Figueiredo Junior, C. Silva, Thiago Gonçalves Pereira, Beatriz Abreu Machado
{"title":"Comments on Souza et al. (2022) “Recent geomorphological changes in the Paraiba do Sul delta, South America East Coast”","authors":"G. Fernandez, Thais Baptista da Rocha, José Maria Landin Dominguez, Sérgio Cadena de Vasconcelos, Gilberto Tavares de Macedo Dias, André da Costa, M. S. Figueiredo, Alberto Garcia Figueiredo Junior, C. Silva, Thiago Gonçalves Pereira, Beatriz Abreu Machado","doi":"10.1177/03091333231182701","DOIUrl":null,"url":null,"abstract":"Souza et al. (2022) based on grain size analyses, Optical Stimulated Luminescence (OSL) ages in fluvial sediments, and regional topography affirmed that most of the Paraiba do Sul River Delta (PSRD) has been deposited during the Little Ice Age (LIA). Souza et al. (2022) also inferred that after the LIA, PSRD presents shoreline erosion, using OSL undetermined results, regional topography, and field photographs, suggesting the direct connection of erosion and human intervention along river basin. As the results obtained by Souza et al. (2022) present several inconsistences about coastal evolution, and question previous works about PDRD developed in the last 30 years, we discuss these in three different sections, covering geological, historical, and recent geomorphological changes in PDRD.","PeriodicalId":49659,"journal":{"name":"Progress in Physical Geography-Earth and Environment","volume":"6 1","pages":"625 - 641"},"PeriodicalIF":3.0000,"publicationDate":"2023-07-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Progress in Physical Geography-Earth and Environment","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1177/03091333231182701","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 2
Abstract
Souza et al. (2022) based on grain size analyses, Optical Stimulated Luminescence (OSL) ages in fluvial sediments, and regional topography affirmed that most of the Paraiba do Sul River Delta (PSRD) has been deposited during the Little Ice Age (LIA). Souza et al. (2022) also inferred that after the LIA, PSRD presents shoreline erosion, using OSL undetermined results, regional topography, and field photographs, suggesting the direct connection of erosion and human intervention along river basin. As the results obtained by Souza et al. (2022) present several inconsistences about coastal evolution, and question previous works about PDRD developed in the last 30 years, we discuss these in three different sections, covering geological, historical, and recent geomorphological changes in PDRD.
Souza et al.(2022)基于粒度分析、河流沉积物的光学激发发光(OSL)年龄和区域地形,确认了大部分南帕拉伊巴河三角洲(PSRD)是在小冰期(LIA)沉积的。Souza et al.(2022)也利用OSL未确定的结果、区域地形和野外照片推断,在LIA之后,PSRD呈现海岸线侵蚀,表明流域侵蚀与人类干预有直接联系。由于Souza等人(2022)获得的结果在沿海演变方面存在一些不一致之处,并质疑过去30年来关于PDRD的先前工作,我们将在三个不同的部分讨论这些问题,包括PDRD的地质、历史和最近的地貌变化。
期刊介绍:
Progress in Physical Geography is a peer-reviewed, international journal, encompassing an interdisciplinary approach incorporating the latest developments and debates within Physical Geography and interrelated fields across the Earth, Biological and Ecological System Sciences.