The Irabu Knoll: Hydrothermal Site at the Eastern Edge of the Yaeyama Graben View Full Text


Ontology type: schema:Chapter      Open Access: True


Chapter Info

DATE

2015

AUTHORS

Tatsuhiro Fukuba , Takuroh Noguchi , Teruo Fujii

ABSTRACT

The Irabu Knoll hydrothermal vents were first discovered in 2000 during YK00-06 cruise using R/V YOKOSUKA and manned submersible SHINKAI 6500. The Irabu Knoll consists of three seamounts from 1,680 to 1,970-m in water depth. The Irabu Knoll is located in the Southern Okinawa Trough and is constructed from basalt as the host rock. Two hydrothermal venting sites have been found at East and West seamount. Sulfide deposit of the Irabu Knoll hydrothermal system consists of barite, sphalerite, pyrite, and chalcopyrite. Major taxa in the vent ecosystem are Shinkaia crosnieri, Munidopsis sp., and Ashinkailepsas sp. More... »

PAGES

493-496

Book

TITLE

Subseafloor Biosphere Linked to Hydrothermal Systems

ISBN

978-4-431-54864-5
978-4-431-54865-2

From Grant

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/978-4-431-54865-2_39

DOI

http://dx.doi.org/10.1007/978-4-431-54865-2_39

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1002436558


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