Discovery of a new hydrothermal vent based on an underwater, high-resolution geophysical survey

Kentaro Nakamura, Tomohiro Toki, Nobutatsu Mochizuki, Miho Asada, Junichiro Ishibashi, Yoshifumi Nogi, Shuro Yoshikawa, Jun Ichi Miyazaki, Kyoko Okino

Research output: Contribution to journalArticle

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Abstract

A new hydrothermal vent site in the Southern Mariana Trough has been discovered using acoustic and magnetic surveys conducted by the Japan Agency for Marine-Earth Science and Technology's (JAMSTEC) autonomous underwater vehicle (AUV), Urashima. The high-resolution magnetic survey, part of a near-bottom geophysical mapping around a previously known hydrothermal vent site, the Pika site, during the YK09-08 cruise in June-July 2009, found that a clear magnetization low extends ~500. m north from the Pika site. Acoustic signals, suggesting hydrothermal plumes, and 10. m-scale chimney-like topographic highs were detected within this low magnetization zone by a 120. kHz side-scan sonar and a 400. kHz multibeam echo sounder. In order to confirm the seafloor sources of the geophysical signals, seafloor observations were carried out using the deep-sea manned submersible Shinkai 6500 during the YK 10-10 cruise in August 2010. This discovered a new hydrothermal vent site (12°55.30'N, 143°38.89'E; at a depth of 2922. m), which we have named the Urashima site. This hydrothermal vent site covers an area of approximately 300. m×300. m and consists of black and clear smoker chimneys, brownish-colored shimmering chimneys, and inactive chimneys. All of the fluids sampled from the Urashima and Pika sites have chlorinity greater than local ambient seawater, suggesting subseafloor phase separation or leaching from rocks in the hydrothermal reaction zone. End-member compositions of the Urashima and Pika fluids suggest that fluids from two different sources feed the two sites, even though they are located on the same knoll and separated by only ~500. m. We demonstrate that investigations on hydrothermal vent sites located in close proximity to one another can provide important insights into subseafloor hydrothermal fluid flow, and also that, while such hydrothermal sites are difficult to detect by conventional plume survey methods, high-resolution underwater geophysical surveys provide an effective means.

Original languageEnglish
Pages (from-to)1-10
Number of pages10
JournalDeep-Sea Research Part I: Oceanographic Research Papers
Volume74
DOIs
Publication statusPublished - Apr 1 2013

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Ochotonidae
geophysical survey
hydrothermal vent
magnetic survey
acoustics
magnetization
fluid
seafloor
hydrothermal plume
echo sounder
acoustic survey
autonomous underwater vehicle
survey method
sidescan sonar
submersible
leaching
Earth science
hydrothermal fluid
science and technology
seawater

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Aquatic Science

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Discovery of a new hydrothermal vent based on an underwater, high-resolution geophysical survey. / Nakamura, Kentaro; Toki, Tomohiro; Mochizuki, Nobutatsu; Asada, Miho; Ishibashi, Junichiro; Nogi, Yoshifumi; Yoshikawa, Shuro; Miyazaki, Jun Ichi; Okino, Kyoko.

In: Deep-Sea Research Part I: Oceanographic Research Papers, Vol. 74, 01.04.2013, p. 1-10.

Research output: Contribution to journalArticle

Nakamura, Kentaro ; Toki, Tomohiro ; Mochizuki, Nobutatsu ; Asada, Miho ; Ishibashi, Junichiro ; Nogi, Yoshifumi ; Yoshikawa, Shuro ; Miyazaki, Jun Ichi ; Okino, Kyoko. / Discovery of a new hydrothermal vent based on an underwater, high-resolution geophysical survey. In: Deep-Sea Research Part I: Oceanographic Research Papers. 2013 ; Vol. 74. pp. 1-10.
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