Articles | Volume 16, issue 11
https://doi.org/10.5194/bg-16-2285-2019
https://doi.org/10.5194/bg-16-2285-2019
Research article
 | 
04 Jun 2019
Research article |  | 04 Jun 2019

Subaqueous speleothems (Hells Bells) formed by the interplay of pelagic redoxcline biogeochemistry and specific hydraulic conditions in the El Zapote sinkhole, Yucatán Peninsula, Mexico

Simon Michael Ritter, Margot Isenbeck-Schröter, Christian Scholz, Frank Keppler, Johannes Gescher, Lukas Klose, Nils Schorndorf, Jerónimo Avilés Olguín, Arturo González-González, and Wolfgang Stinnesbeck

Viewed

Total article views: 4,332 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,129 1,136 67 4,332 368 66 65
  • HTML: 3,129
  • PDF: 1,136
  • XML: 67
  • Total: 4,332
  • Supplement: 368
  • BibTeX: 66
  • EndNote: 65
Views and downloads (calculated since 24 Jan 2019)
Cumulative views and downloads (calculated since 24 Jan 2019)

Viewed (geographical distribution)

Total article views: 4,332 (including HTML, PDF, and XML) Thereof 3,658 with geography defined and 674 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 21 Nov 2024
Download
Short summary
Unique and spectacular under water speleothems termed as Hells Bells were recently reported from sinkholes (cenotes) of the Yucatán Peninsula, Mexico. However, the mystery of their formation remained unresolved. Here, we present detailed geochemical analyses and delineate that the growth of Hells Bells results from a combination of biogeochemical processes and variable hydraulic conditions within the cenote.
Altmetrics
Final-revised paper
Preprint