Organic Biogeochemistry in West Mata, NE Lau Hydrothermal Vent Fields
Open Access
- 21 April 2021
- journal article
- research article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 22 (4)
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.Keywords
Funding Information
- National Science Foundation (OCE0929881)
- National Oceanic and Atmospheric Administration (NA10OAR4320148)
- NASA Astrobiology Institute (U of Hawaii)
- Ministry of Science and Technology, Taiwan (107‐2611‐M‐002‐002 and 108‐2611‐M‐002‐006)
- Ministry of Education (109L892601)
This publication has 117 references indexed in Scilit:
- Volcanic Eruptions in the Deep SeaOceanography, 2012
- High SO2 flux, sulfur accumulation, and gas fractionation at an erupting submarine volcanoGeology, 2011
- Complete Genome Sequence of Hyperthermophilic Pyrococcus sp. Strain NA2, Isolated from a Deep-Sea Hydrothermal Vent AreaJournal of Bacteriology, 2011
- A Novel Lineage of Proteobacteria Involved in Formation of Marine Fe-Oxidizing Microbial Mat CommunitiesPLOS ONE, 2007
- Microbial Community in Black Rust Exposed to Hot Ridge Flank Crustal FluidsApplied and Environmental Microbiology, 2006
- A three‐plate kinematic model for Lau Basin openingGeochemistry, Geophysics, Geosystems, 2001
- Stocks and dynamics of dissolved and particulate organic matter in the southern Ross Sea, AntarcticaDeep Sea Research Part II: Topical Studies in Oceanography, 2000
- Thermophilic subseafloor microorganisms from the 1996 North Gorda Ridge eruptionDeep Sea Research Part II: Topical Studies in Oceanography, 1998
- The development of direct and indirect methods for the study of the thermodynamics of microbial growthThermochimica Acta, 1998
- Dissolved and particulate organic carbon in the western Mediterranean SeaDeep Sea Research Part II: Topical Studies in Oceanography, 1997