Articles | Volume 15, issue 18
https://doi.org/10.5194/bg-15-5715-2018
https://doi.org/10.5194/bg-15-5715-2018
Research article
 | 
27 Sep 2018
Research article |  | 27 Sep 2018

On the formation of hydrothermal vents and cold seeps in the Guaymas Basin, Gulf of California

Sonja Geilert, Christian Hensen, Mark Schmidt, Volker Liebetrau, Florian Scholz, Mechthild Doll, Longhui Deng, Annika Fiskal, Mark A. Lever, Chih-Chieh Su, Stefan Schloemer, Sudipta Sarkar, Volker Thiel, and Christian Berndt

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (01 Jun 2018) by Helge Niemann
AR by Sonja Geilert on behalf of the Authors (06 Jul 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Jul 2018) by Helge Niemann
RR by Anonymous Referee #2 (26 Jul 2018)
ED: Reconsider after major revisions (31 Jul 2018) by Helge Niemann
AR by Sonja Geilert on behalf of the Authors (04 Sep 2018)  Author's response    Manuscript
ED: Publish as is (05 Sep 2018) by Helge Niemann
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Short summary
Abrupt climate changes in Earth’s history might have been triggered by magmatic intrusions into organic-rich sediments, which can potentially release large amounts of greenhouse gases. In the Guaymas Basin, vigorous hydrothermal venting at the ridge axis and off-axis inactive vents show that magmatic intrusions are an effective way to release carbon but must be considered as very short-lived processes in a geological sense. These results need to be taken into account in future climate models.
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