{"title":"Paleosol-sedimentary records of contrasting environmental changes in the Sabana de Bogotá, Colombia, during the late Pleistocene – Holocene","authors":"Triana Angélica Viviana , Santana-Quispe Lady Diana , Solleiro-Rebolledo Elizabeth , Sedov Sergey , Cabadas-Báez Héctor , Díaz-Ortega Jaime , Calderón-Romero Esteban","doi":"10.1016/j.catena.2025.108946","DOIUrl":null,"url":null,"abstract":"<div><div>The Sabana de Bogotá, located on a high plateau (2600 masl), is a slightly dissected plain of lacustrine origin surrounded by quarzitic Cretaceous sandstone ridges. Due to the high altitudes, the Sabana represents a special case in the tropical belt near Ecuador with unique characteristics. Several studies have been conducted to reconstruct paleoenvironmental conditions during the late Pleistocene and the Holocene, mainly from lacustrine and glacial records. However, the Sabana also contains a rich register of paleosols. In this work, we analyzed the paleopedological record found in the lower foot of a quarzitic ridge. In various sections, we identified prominent, well-developed paleosol units interlayered with colluvial sedimentary strata mixed with pyroclastic components covering the interval from Marine Isotope Stage 2 (MIS 2) to MIS 1. Two profiles were selected, located just some meters apart. The first (profile 6) contains a complete pedological record with the modern soil and three paleosols forming a pedocomplex, while the second profile (6a) represents a case where sedimentation overlaps pedogenesis. Selected methodologies were applied (macro and micromorphological description, color, grain size distribution, magnetic susceptibility, total organic carbon, bulk chemical composition, X-ray diffraction, and radiocarbon dating) to differentiate pedogenetic trends and sedimentary sources. The results show the studied paleosols contain similar properties, although with variable intensity and some differences in their expression and specific processes for some selected units or horizons. All paleosols evidence illuviation and redoximorphic (stagnic) processes; however, with a clear multiphase development. We interpret these paleosols as formed mainly in cold and humid conditions. One remarkable finding in the sequence was a human bone embedded in the third paleosol, aged around 11,000 cal yr BP, representing one of the most ancient individuals in Colombia.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"254 ","pages":"Article 108946"},"PeriodicalIF":5.4000,"publicationDate":"2025-04-01","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/S0341816225002486","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
The Sabana de Bogotá, located on a high plateau (2600 masl), is a slightly dissected plain of lacustrine origin surrounded by quarzitic Cretaceous sandstone ridges. Due to the high altitudes, the Sabana represents a special case in the tropical belt near Ecuador with unique characteristics. Several studies have been conducted to reconstruct paleoenvironmental conditions during the late Pleistocene and the Holocene, mainly from lacustrine and glacial records. However, the Sabana also contains a rich register of paleosols. In this work, we analyzed the paleopedological record found in the lower foot of a quarzitic ridge. In various sections, we identified prominent, well-developed paleosol units interlayered with colluvial sedimentary strata mixed with pyroclastic components covering the interval from Marine Isotope Stage 2 (MIS 2) to MIS 1. Two profiles were selected, located just some meters apart. The first (profile 6) contains a complete pedological record with the modern soil and three paleosols forming a pedocomplex, while the second profile (6a) represents a case where sedimentation overlaps pedogenesis. Selected methodologies were applied (macro and micromorphological description, color, grain size distribution, magnetic susceptibility, total organic carbon, bulk chemical composition, X-ray diffraction, and radiocarbon dating) to differentiate pedogenetic trends and sedimentary sources. The results show the studied paleosols contain similar properties, although with variable intensity and some differences in their expression and specific processes for some selected units or horizons. All paleosols evidence illuviation and redoximorphic (stagnic) processes; however, with a clear multiphase development. We interpret these paleosols as formed mainly in cold and humid conditions. One remarkable finding in the sequence was a human bone embedded in the third paleosol, aged around 11,000 cal yr BP, representing one of the most ancient individuals in Colombia.
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.