English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Caves of sulfuric acid origin retain diagnostic minerals and features that allow reconstruction of their geochemical history (Polyak & Provencio, 2001). This paper centers on caves in the Guadalupe Mountains, New Mexico, specifically their latest transition from H2SO4 speleogenesis to processes dominated by CO2 equilibria. Much cave research today yields paleoclimate data from meteoric speleothems (Fairchild & Baker, 2012). Instead, this paper emphasizes processes and features specific to the caves themselves. Such information can help identify former conditions in similar caves, and is useful for organizing future studies of geochronology and paleoclimate.

Petrographic and isotopic evidence for late-stage processes in sulfuric acid caves of the Guadalupe Mountains, New Mexico, USA