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The Kairei vent field is a hydrothermal vent field located in the Indian Ocean at a depth of Vorlage:Convert. It is just north of the Rodrigues triple junction, approximately Vorlage:Convert east from Madagascar.[1] It is the first hydrothermal field discovered in the Indian Ocean and the first of the series of known vents along the Central Indian Ridge.

The vent field was discovered in 2000 by the R/V Kairei and ROV Kaikō operated by Japan Marine Science and Technology Center (JAMSTEC).[2] In 2001, the site was surveyed with high resolution prior to the deployment of ROV JASON.[3][4]

The vent field was visited again by JAMSTEC in 2009 on the YK09-13 cruise, where the HOV Shinkai6500 was deployed.

The field is dominated by sulfide talus, with the approximate area of high-temperature venting constrained to approximately 40 square meters. Fluids from the vent field have been measured in excess of Vorlage:Convert and are rich in metals, providing a black-smoker appearance. Elevated chlorinity in venting fluids suggests that phase-separation happens deep below the field.[4]

The Kairei vent field is one of the few known locations of the Sea Pangolin, threatened by deep sea mining.[5] It is also a site associated with Gigantopelta aegis and Alviniconcha strummeri gastropods.[6]

It is the site of discovery of Rimicaris kairei, belonging to the family of hydrothermal shrimp found at many sites in the Atlantic Ocean.[7]

Carbon and nitrogen isotopes suggest that there are four distinct trophic levels at the Karei vent field.[3]

Kairei is also of concern with respect to research on deep sea dispersal pathways, with some shared biological communities to those neighboring vent fields (Edmond, Solitaire, DoDo).[8]

Vorlage:Reflist

  1. Kairei Field. In: vents-data.interridge.org.
  2. Jun Hashimoto, Suguru Ohta, Toshitaka Gamo, Hitoshi Chiba, Toshiyuki Yamaguchi, Shinji Tsuchida, Takamoto Okudaira, Hajime Watabe, Toshiro Yamanaka, Mitsuko Kitazawa: First Hydrothermal Vent Communities from the Indian Ocean Discovered. In: Zoological Science. 18. Jahrgang, Nr. 5, Juli 2001, S. 717–721, doi:10.2108/zsj.18.717.
  3. a b C. Van Dover: Trophic relationships among invertebrates at the Kairei hydrothermal vent field (Central Indian Ridge). In: Marine Biology. 141. Jahrgang, Nr. 4, Oktober 2002, S. 761–772, doi:10.1007/s00227-002-0865-y.
  4. a b R. M. Gallant, K. L. Von Damm: Geochemical controls on hydrothermal fluids from the Kairei and Edmond Vent Fields, 23°-25°S, Central Indian Ridge: CONTROLS ON HYDROTHERMAL FLUIDS. In: Geochemistry, Geophysics, Geosystems. 7. Jahrgang, Nr. 6, Juni 2006, S. n/a, doi:10.1029/2005GC001067.
  5. Julia Sigwart, The Conversation: Sea Pangolin: The first ever species endangered by potential deep sea mining. In: phys.org. (englisch).
  6. Amy Fleming: One scientist's mission to save the 'super weird' snails under the sea. In: The Guardian. 26. Februar 2020;.
  7. Hajime Watabe, Jun Hashimoto: A New Species of the Genus Rimicaris (Alvinocarididae: Caridea: Decapoda) from the Active Hydrothermal Vent Field, "Kairei Field," on the Central Indian Ridge, the Indian Ocean. In: Zoological Science. 19. Jahrgang, Nr. 10, Oktober 2002, S. 1167–1174, doi:10.2108/zsj.19.1167, PMID 12426479.
  8. Girish Beedessee, Hiromi Watanabe, Tomomi Ogura, Suguru Nemoto, Takuya Yahagi, Satoshi Nakagawa, Kentaro Nakamura, Ken Takai, Meera Koonjul, Daniel E. P. Marie: High Connectivity of Animal Populations in Deep-Sea Hydrothermal Vent Fields in the Central Indian Ridge Relevant to Its Geological Setting. In: PLOS ONE. 8. Jahrgang, Nr. 12, 16. Dezember 2013, S. e81570, doi:10.1371/journal.pone.0081570, PMID 24358117, PMC 3864839 (freier Volltext), bibcode:2013PLoSO...881570B.