ArticleScientific reports2019
Characteristics and Evolution of sill-driven off-axis hydrothermalism in Guaymas Basin - the Ringvent site.
Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 18 papers.
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Who cites it
18 citing papers in PubMed.
- Millimetre-Scale Stratification of Microbial Communities in Hydrothermal Sediments.Environmental microbiology · 2026Article
- From CRISPR-Cas to Argonautes: Defense systems of bacteria and archaea in the hydrothermal deep subsurface.ISME communications · 2026Article
- Clumped isotopes of methane trace bioenergetics in the environment.Science advances · 2025Article
- Quantifying hydrothermal ammonium mobilization from sediment and implications for the marine biosphere: a case study from the Guaymas Basin, Gulf of California.Frontiers in microbiology · 2025Article
- A global comparison of surface and subsurface microbiomes reveals large-scale biodiversity gradients, and a marine-terrestrial divide.Science advances · 2024Article
- An Underwater Methane Sensor Based on Laser Spectroscopy in a Hollow Core Optical Fiber.ACS sensors · 2024Article
- Single-cell analysis reveals an active and heterotrophic microbiome in the Guaymas Basin deep subsurface with significant inorganic carbon fixation by heterotrophs.Applied and environmental microbiology · 2024Article
- Complex bacterial diversity of Guaymas Basin hydrothermal sediments revealed by synthetic long-read sequencing (LoopSeq).Frontiers in microbiology · 2024Article
- A PCR-Based Survey of Methane-Cycling Archaea in Methane-Soaked Subsurface Sediments of Guaymas Basin, Gulf of California.Microorganisms · 2023Article
- Metagenomic profiles of archaea and bacteria within thermal and geochemical gradients of the Guaymas Basin deep subsurface.Nature communications · 2023Article
- Well-hidden methanogenesis in deep, organic-rich sediments of Guaymas Basin.The ISME journal · 2023Article
- Thermal Selection of Microbial Communities and Preservation of Microbial Function in Guaymas Basin Hydrothermal Sediments.Applied and environmental microbiology · 2023Article
- Microbial Hydrocarbon Degradation in Guaymas Basin-Exploring the Roles and Potential Interactions of Fungi and Sulfate-Reducing Bacteria.Frontiers in microbiology · 2022Article
- Evolutionary stasis of a deep subsurface microbial lineage.The ISME journal · 2021Article
- Microbial Communities Under Distinct Thermal and Geochemical Regimes in Axial and Off-Axis Sediments of Guaymas Basin.Frontiers in microbiology · 2021Article
- Microbial Communities of Hydrothermal Guaymas Basin Surficial Sediment Profiled at 2 Millimeter-Scale Resolution.Frontiers in microbiology · 2021Article
- Hydrothermal plume detection dataset from Chinese cruises to the equatorial East Pacific Rise.Data in brief · 2020Article
- The Guaymas Basin Subseafloor Sedimentary Archaeome Reflects Complex Environmental Histories.iScience · 2020Article
Corrections and comments
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Authors and funding
19 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Guaymas Basin spreading center, at 2000 m depth in the Gulf of California, is overlain by a thick sedimentary cover. Across the basin, localized temperature anomalies, with active methane venting and seep fauna exist in response to magma emplacement into sediments. These sites evolve over thousands of years as magma freezes into doleritic sills and the system cools. Although several cool sites resembling cold seeps have been characterized, the hydrothermally active stage of an off-axis site was lacking good examples. Here, we present a multidisciplinary characterization of Ringvent, an ~1 km wide circular mound where hydrothermal activity persists ~28 km northwest of the spreading center. Ringvent provides a new type of intermediate-stage hydrothermal system where off-axis hydrothermal activity has attenuated since its formation, but remains evident in thermal anomalies, hydrothermal biota coexisting with seep fauna, and porewater biogeochemical signatures indicative of hydrothermal circulation. Due to their broad potential distribution, small size and limited life span, such sites are hard to find and characterize, but they provide critical missing links to understand the complex evolution of hydrothermal systems.
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