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  4. Organic Biogeochemistry in West Mata, NE Lau Hydrothermal Vent Fields
 
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Organic Biogeochemistry in West Mata, NE Lau Hydrothermal Vent Fields

Journal
Geochemistry, Geophysics, Geosystems
Journal Volume
22
Journal Issue
4
Date Issued
2021
Author(s)
Lin H.-T
Butterfield D.A
Baker E.T
Resing J.A
Huber J.A
Cowen J.P.
HUEI-TING LIN  
DOI
10.1029/2020GC009481
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85104597060&doi=10.1029%2f2020GC009481&partnerID=40&md5=6d226b842c71dff8b325e5f731fd58f2
https://scholars.lib.ntu.edu.tw/handle/123456789/571884
Abstract
The impact of submarine hydrothermal systems on organic carbon in the ocean—one of the largest fixed carbon reservoirs on Earth—could be profound. Yet, different vent sites show diverse fluid chemical compositions and the subsequent biological responses. Observations from various vent sites are to evaluate hydrothermal systems' impact on the ocean carbon cycle. A response cruise in May 2009 to an on-going submarine eruption at West Mata Volcano, northeast Lau Basin, provided an opportunity to quantify the organic matter production in a back-arc spreading hydrothermal system. Hydrothermal vent fluids contained elevated dissolved organic carbon, particulate organic carbon (POC), and particulate nitrogen (PN) relative to background seawater. The δ13C-POC values for suspended particles in the diffuse vent fluids (?15.5? and ?12.3?) are distinct from those in background seawater (?23?±?1?), indicative of unique carbon synthesis pathways of the vent microbes from the seawater counterparts. The first dissolved organic nitrogen concentrations reported for diffuse vents were similar to or higher than those for background seawater. Enhanced nitrogen fixation and denitrification removed 37%–89% of the total dissolved nitrogen in the recharging background seawater in the hydrothermal vent flow paths. The hydrothermal plume samples were enriched in POC and PN, indicating enhanced biological production. The total “dark” organic carbon production within the plume matches the thermodynamic prediction based on available reducing chemical substances supplied to the plume. This research combines the measured organic carbon contents with thermodynamic modeled results and demonstrates the importance of hydrothermal activities on the water column carbon production in the deep ocean. ? 2021. American Geophysical Union. All Rights Reserved.
Subjects
Biogeochemistry; Dissolution; Hot springs; Nitrogen fixation; Reservoirs (water); Seawater; Submarines; Biological production; Dissolved organic carbon; Dissolved organic nitrogen; Hydrothermal activity; Organic carbon contents; Particulate organic carbon; Submarine hydrothermal system; Thermodynamic predictions; Organic carbon; biogeochemistry; dissolved organic carbon; dissolved organic nitrogen; hydrothermal fluid; hydrothermal plume; hydrothermal system; hydrothermal vent; particulate organic carbon; prediction; thermodynamics; Pacific Ocean; West Mata
SDGs

[SDGs]SDG14

Type
journal article

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