Coupled hydrothermal venting and hydrocarbon seepage discovered at Conical Seamount, Papua New Guinea

During research expedition SO299 with the German RV Sonne, we discovered the first deep-sea hydrothermal vent system along the Tabar-Lihir-Tanga-Feni island chain in northeastern Papua New Guinea. The Karambusel vent field is hosted by a volcanic center on the western flank of Conical Seamount that formed ~ 89 ka ago. Karambusel is remarkable in that it hosts both a fossil high-temperature, gold-rich mineralization and an active low-temperature (< 51 °C) vent system precipitating arsenic-, antimony-, thallium-, and mercury-rich sulfide minerals. Chemosymbiotic fauna is associated with the vent system and we identified more endemic species than in previous studies on nearby seeps. Our study shows that the magmatic event at Karambusel likely triggered the epithermal mineralization at Karambusel and at the central summit of Conical Seamount. The current hydrothermal fluids originate from condensed magmatic vapor or connate fluids. Gas bubbles were observed at some vent sites and the proportion of methane in the gas phase exceeds that of any other hydrothermal vent system. The composition of the light hydrocarbons points towards a thermogenic origin. Karambusel is thus the first hybrid magmatic-hydrothermal vent and hydrocarbon seep system discovered globally which explains the highly endemic vent fauna as a consequence of the unique ecological niche.

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Journal
Scientific Reports
Published
2025-09-19
DOI
https://doi.org/10.1038/s41598-025-17192-x
Citations
1
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
0.86

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article

Coupled hydrothermal venting and hydrocarbon seepage discovered at Conical Seamount, Papua New Guinea

Rebecca Zitoun, Jan J. Falkenberg, Sylvia G. Sander, Christophe Y. Galerne et al.
1 citations
Scientific Reports
Methane Hydrates and Related Phenomena
0.86
article

Coupled hydrothermal venting and hydrocarbon seepage discovered at Conical Seamount, Papua New Guinea

Rebecca Zitoun, Jan J. Falkenberg, Sylvia G. Sander, Christophe Y. Galerne, Mark Schmidt, Klaas Meyn, Philipp A. Brandl, Doris Maicher, Ingo Heyde, Mark D. Hannington, Sven Petersen, Johanna Schenk, Brent McInnes, Joseph O. Espi, Christoph Beier, Thor H. Hansteen, Manuela S. Kaufmann, Fred Jourdan, Eemu Ranta, Alan T. Baxter, Johanna Klein, Konstantin Reeck, Terue C. Kihara, Felix Genske, Leon Waßmund, Louis-Maxime Gautreau, Julia Wenske, Sabine Lange, Esther Panachi, Stanis Konabe, Octavio Acuña Avendaño, Egor Riemer, William Ruth, Sarima Vahrenkamp
article en
1 citations

Abstract

During research expedition SO299 with the German RV Sonne, we discovered the first deep-sea hydrothermal vent system along the Tabar-Lihir-Tanga-Feni island chain in northeastern Papua New Guinea. The Karambusel vent field is hosted by a volcanic center on the western flank of Conical Seamount that formed ~ 89 ka ago. Karambusel is remarkable in that it hosts both a fossil high-temperature, gold-rich mineralization and an active low-temperature (< 51 °C) vent system precipitating arsenic-, antimony-, thallium-, and mercury-rich sulfide minerals. Chemosymbiotic fauna is associated with the vent system and we identified more endemic species than in previous studies on nearby seeps. Our study shows that the magmatic event at Karambusel likely triggered the epithermal mineralization at Karambusel and at the central summit of Conical Seamount. The current hydrothermal fluids originate from condensed magmatic vapor or connate fluids. Gas bubbles were observed at some vent sites and the proportion of methane in the gas phase exceeds that of any other hydrothermal vent system. The composition of the light hydrocarbons points towards a thermogenic origin. Karambusel is thus the first hybrid magmatic-hydrothermal vent and hydrocarbon seep system discovered globally which explains the highly endemic vent fauna as a consequence of the unique ecological niche.

Scientific ReportsVol. 15(1)
University of Tasmania (AU), Federal Institute for Geosciences and Natural Resources (DE), University of Helsinki (FI), University of Ottawa (CA), University of Papua New Guinea (PG), University of Bremen (DE), Friedrich-Alexander-Universität Erlangen-Nürnberg (DE), University of Toronto (CA), Curtin University (AU), University of Münster (DE), Odyssey House (US), Christian-Albrechts-Universität zu Kiel (DE), GEOMAR Helmholtz Centre for Ocean Research Kiel (DE), Technische Universität Berlin (DE)
Curtin University of Technology, Bundesministerium für Bildung und Forschung, GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
Openalex Percentile: Top 24%
Methane Hydrates and Related Phenomena
0.86
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