Biogeosciences
Biogeosciences
BG
Articles | Volume 16, issue 11
Articles | Volume 16, issue 11
https://doi.org/10.5194/bg-16-2285-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-2285-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 11
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: 5,759 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,118 1,513 128 5,759 564 150 176
  • HTML: 4,118
  • PDF: 1,513
  • XML: 128
  • Total: 5,759
  • Supplement: 564
  • BibTeX: 150
  • EndNote: 176
Views and downloads (calculated since 24 Jan 2019)
Cumulative views and downloads (calculated since 24 Jan 2019)

Viewed (geographical distribution)

Total article views: 5,759 (including HTML, PDF, and XML) Thereof 5,076 with geography defined and 683 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 17 Jun 2026
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.
Read more
Share
Altmetrics
Final-revised paper
Preprint