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2015 | OriginalPaper | Buchkapitel

4. Soils of Enderby Land

verfasst von : Andrey V. Dolgikh, Nikita S. Mergelov, Andrey A. Abramov, Alexey V. Lupachev, Sergey V. Goryachkin

Erschienen in: The Soils of Antarctica

Verlag: Springer International Publishing

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Abstract

Enderby Land is that portion of Antarctica extending from Shirase Glacier and Lutzow-Holm Bay from the west (38°30’E) to Wilma Glacier and Edward VIII Bay to the east (57°E). Enderby Land is bordered by the Cosmonauts Sea in the west and by the Sea of Cooperation in the east, both are part of the Southern Ocean. Nearly 1,500 km² of Enderby Land is ice-free. Two research stations—Molodezhnaya (Russia, 67º40' S, 45º51' E) and Syowa (Japan, 69°00’S, 39°35’E)—are established in Enderby Land. The dominant soil taxa along the coast are Haploturbels/Haplorthels, Aquiturbels/Aquorthels, and previously unclassified ornithogenic soils and endolithic microsoils. Lithic subgroups both for Haploturbels and Gelorthents (permafrost > 1 m without cryoturbations) are predominant in the territories with shallow rock contact.

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Titel: Soils of Enderby Land
verfasst von: Andrey V. Dolgikh
Nikita S. Mergelov
Andrey A. Abramov
Alexey V. Lupachev
Sergey V. Goryachkin
Verlag: Springer International Publishing
Buch: The Soils of Antarctica
Print ISBN: 978-3-319-05496-4

Electronic ISBN: 978-3-319-05497-1

Copyright-Jahr: 2015
DOI: https://doi.org/10.1007/978-3-319-05497-1_4