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Tahi Moana 1

Name Alias(es): 
COMRA Discovery Expedition
CDE
CELSC Plume 12
plume 21, C-ELSC
Tahi Moana
MGDS_FeatureID lowest in hierarchy: 
Maximum Temperature: 
311
Max Temperature Category: 
Latitude: 
-20.6900
Longitude: 
-176.1800
Location on map: 
Ocean: 
Region: 
National Jurisdiction: 
Maximum or Single Reported Depth (mbsl): 
2256
Minimum Depth (mbsl): 
2199
Tectonic setting: 
Full Spreading Rate (mm/a): 
73.1
Volcano Number (if applicable): 
Host Rock: 
NotProvided
Deposit Type: 
NotProvided
Notes on Vent Field Description: 
this location is ~10 km (~4 miles) north of ABE (R2K ISS Bulls Eye) on northern segment of Eastern Lau Spreading Center (ELSC); chimney structures range from <1m to ~5m tall; note: Zhou and Yang 2008 "A hydrothermal field named as "CDE"(COMRA Discovery Expedition) at 176°11'W, 20°40'S, about 4 miles south of known ABE hydrothermal field, was discovered by R/V DaYang YiHao in May, 2007"; however, that position is actually ~4 miles north of ABE;
Notes Relevant to Biology: 
microbial mats, anemones, crabs, fish
Year and How Discovered (if active, visual confirmation is listed first): 
2008 commercial ROV; 2004 plume only
Discovery References (text): 
(plume only): Baker et al., GEOPHYSICAL RESEARCH LETTERS, 33, L07308, doi:10.1029/2005GL025283, 2006, Abundant hydrothermal venting along melt-rich and melt-free ridge segments in the Lau back-arc basin;
SRK Consulting report for Nautilus Minerals (http://www.nautilusminerals.com/i/pdf/2008NautilusExplorationNI43-101Report.pdf);
Other References (text): 
Zhou and Yang (2008) Microbiological Oxidation Of Sulfide Chimney Promoted By Warm Diffusing Flow In CDE Hydrothermal Field In Eastern Lau Spreading Center. American Geophysical Union, Fall Meeting 2008, abstract #B51D-0405;
Zhou, H. (2008) Discovery of new hydrothermal fields in Eastern Lau Spreading Center, Lau Basin. Ridge 2000 Program Abstract Volume, Portland Workshop, March 2008;
Sheik, C., Anantharaman, K., Breier, J. et al. Spatially resolved sampling reveals dynamic microbial communities in rising hydrothermal plumes across a back-arc basin. ISME J 9, 1434–1445 (2015). https://doi.org/10.1038/ismej.2014.228;