Articles | Volume 18, issue 5
https://doi.org/10.5194/bg-18-1629-2021
https://doi.org/10.5194/bg-18-1629-2021
Research article
 | 
09 Mar 2021
Research article |  | 09 Mar 2021

Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica

Melisa A. Diaz, Christopher B. Gardner, Susan A. Welch, W. Andrew Jackson, Byron J. Adams, Diana H. Wall, Ian D. Hogg, Noah Fierer, and W. Berry Lyons

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (18 Dec 2020) by Kees Jan van Groenigen
AR by Melisa Diaz on behalf of the Authors (01 Jan 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (15 Jan 2021) by Kees Jan van Groenigen
AR by Melisa Diaz on behalf of the Authors (20 Jan 2021)  Manuscript 
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Short summary
Water-soluble salt and nutrient concentrations of soils collected along the Shackleton Glacier, Antarctica, show distinct geochemical gradients related to latitude, longitude, elevation, soil moisture, and distance from coast and glacier. Machine learning algorithms were used to estimate geochemical gradients for the region given the relationship with geography. Geography and surface exposure age drive salt and nutrient abundances, influencing invertebrate habitat suitability and biogeography.
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