Paleopedology of soils in thick Holocene loess, Nebraska, USA

Bignell Loess is a Holocene loess unit that has accumulated in the central Great Plains since 9,000 14C yr BP. The Brady Soil separates Bignell Loess from last glacial Peoria Loess and thick sections, which can reach 6 m thickness, may contain four buried soils beneath the modern surface soil. The...

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Bibliographic Details
Main Authors: Peter M. Jacobs, Joseph A. Mason
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/902
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