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

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

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
Download
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.
Altmetrics
Final-revised paper
Preprint