The parent material as the dominant factor in Holocene pedogenesis in the Uruguay River Basin

In the Uruguay River basin (South America; 365,000 km²), an episode of pedogenesis occurred during the Climatic Optimum of the Holocene, approximately between 8,500 and 3,500 yr BP. This period of 5,000 years was characterized by a humid and warm climate. In terms of factors of soil formation, an i...

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Bibliographic Details
Main Authors: Martín Iriondo, Daniela Kröhling
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México 2018-05-01
Series:Revista Mexicana de Ciencias Geológicas
Subjects:
Online Access:https://rmcg.unam.mx/index.php/rmcg/article/view/913
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