Structural control and depth clustering of extensive hydrothermal venting on the shelf of Milos Island

High-resolution geophysical surveys, complemented by chemical, physical, and visual data collected via the ROV MARUM-SQUID, revealed a previously undocumented intermediate-depth hydrothermal vent field (30-230 m) on the shelf of Milos Island, Greece. Three primary vent areas-Aghia Kiriaki, Paleochori-Thiorychia, and Vani-are aligned with ENE-WSW and NW-SE trending active faults, which define the SE coast of Milos and the Milos Gulf-Fyriplaka graben, deepening the Milos shelf up to 230 m. All areas exhibit a distinct bimodal vent distribution, with peaks at ~ 130 m and ~ 180 m; the Paleochori-Thiorychia region additionally hosts a cluster near 210 m. Shallow vents occur on flat, sandy substrates with white microbial mats and gas emissions, whereas deeper vents feature extensive microbial mats, CO₂-degassing chimneys, and actively boiling fluids exceeding 180 °C, indicative of persistent hydrothermal activity. Although the cause of the bimodal -and, in one case, trimodal-distribution remains uncertain, our findings offer a comprehensive, high-resolution characterization of the spatial distribution, morphology, and fluid characteristics of intermediate-depth hydrothermal venting on the Milos shelf.

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Journal
Scientific Reports
Published
2025-11-27
DOI
https://doi.org/10.1038/s41598-025-26398-y
Citations
1
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
0.86

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article

Structural control and depth clustering of extensive hydrothermal venting on the shelf of Milos Island

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Scientific Reports
Methane Hydrates and Related Phenomena
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article

Structural control and depth clustering of extensive hydrothermal venting on the shelf of Milos Island

Andrea Koschinsky, Paraskevi Nomikou, Marcus Elvert, Clemens Röttgen, Evgenia Bazhenova, Charlotte Kleint, Enno Schefuß, Eva-Maria Meckel, Wolfgang Bach, Dimitrios Papanikolaou, Konstantina Bejelou, Stephanos Kilias, Eirini Anagnostou, Christian dos Santos Ferreira, Michael Seidel, Danai Lampridou, Jianlin Liao, E. Kurahashi, Karsten M. Haase, Solveig I Bühring, Joely Maak, Ignacio Pedre, Palash Kumawat, Sotiria Kothri, Effrosyni Varotsou, Alissa Bach, Areti Belka, Wiebke Lehmann
article en
1 citations

Abstract

High-resolution geophysical surveys, complemented by chemical, physical, and visual data collected via the ROV MARUM-SQUID, revealed a previously undocumented intermediate-depth hydrothermal vent field (30-230 m) on the shelf of Milos Island, Greece. Three primary vent areas-Aghia Kiriaki, Paleochori-Thiorychia, and Vani-are aligned with ENE-WSW and NW-SE trending active faults, which define the SE coast of Milos and the Milos Gulf-Fyriplaka graben, deepening the Milos shelf up to 230 m. All areas exhibit a distinct bimodal vent distribution, with peaks at ~ 130 m and ~ 180 m; the Paleochori-Thiorychia region additionally hosts a cluster near 210 m. Shallow vents occur on flat, sandy substrates with white microbial mats and gas emissions, whereas deeper vents feature extensive microbial mats, CO₂-degassing chimneys, and actively boiling fluids exceeding 180 °C, indicative of persistent hydrothermal activity. Although the cause of the bimodal -and, in one case, trimodal-distribution remains uncertain, our findings offer a comprehensive, high-resolution characterization of the spatial distribution, morphology, and fluid characteristics of intermediate-depth hydrothermal venting on the Milos shelf.

Scientific ReportsVol. 15(1)
Carl von Ossietzky Universität Oldenburg (DE), Hochschule Bremen (DE), University of Bremen (DE), Friedrich-Alexander-Universität Erlangen-Nürnberg (DE), National and Kapodistrian University of Athens (GR)
Deutscher Akademischer Austauschdienst
Openalex Percentile: Top 21%
Methane Hydrates and Related Phenomena
0.86
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