Soil-chronosequence and Quaternary landscape evolution at the marine terraces of Harmony Point, Nelson Island, Maritime Antarctica

Abstract This study characterized the physical, chemical, macro- and micromorphological soil properties from three successive marine terrace levels from Harmony Point (Nelson Island, Maritime Antarctica) in order to understand the pedological signatures of Quaternary coastal landscape evolution of M...

Full description

Bibliographic Details
Published in:Anais da Academia Brasileira de Ciências
Main Authors: WILLIAM F. RODRIGUES, MARIANA R. MACHADO, FÁBIO S. DE OLIVEIRA, CARLOS ERNESTO G.R. SCHAEFER, MARIÂNGELA G.P. LEITE, ROBERTO F.M. MICHEL, TEODORO GAUZZI
Format: Article in Journal/Newspaper
Language:English
Published: Academia Brasileira de Ciências 2022
Subjects:
Antarctic soils
Holocene beaches
Ornithogenic soils
Soil mineralogy
Glacier-isostatic uplift
Science
Q
Antarctic
Harmony Point
Nelson Island
Antarc*
Antarctica
Online Access:https://doi.org/10.1590/0001-3765202220201141
https://doaj.org/article/c9c030b5cb93446ebf45656e06fa2923
Description
Summary:Abstract This study characterized the physical, chemical, macro- and micromorphological soil properties from three successive marine terrace levels from Harmony Point (Nelson Island, Maritime Antarctica) in order to understand the pedological signatures of Quaternary coastal landscape evolution of Maritime Antarctica. Soils were sampled on the Late Holocene beach (current beach) and Mid Holocene marine terraces higher up, at 3, 8, and 12 m a.s.l. At the lower levels, the predominant soils were Gelorthents, whereas Haplogelepts dominate the higher terraces. Soil properties are mostly influenced by parent material and faunal activity, in which cryoclastic (thermal weathering) and phosphatization are the main soil-forming processes. Soils from the upper levels are more developed, deeper with reddish colors, granular structures and incipient formation B horizon. These horizonation features highlight that soils vary according with age of glacier-isostatic terrace uplift, representing a Quaternary soil chronosequence. All marine terrace levels are Ornithogenic soils, at varying degrees. However, the presence of old bird nesting sites for long periods led to formation of phosphatic horizons, stable Fe-phosphate minerals and abundant vegetation in the highest terraces of this part of Maritime Antarctica.

Similar Items