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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Latest update: 18 Apr 2024
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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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