Pore water chemistry from mud volcanoes in the Olimpi Mud Volcano Field and Anaximander Mountains was studied for three major purposes. The dataset, hosted by the Australian Ocean Data Network, was last updated in April 2026. Advective flow velocities were found to be moderate (3-50 cm y⁻¹), and calculated formation water temperatures ranged from 55 to 145 °C.
Use Cases
- Model fluid transport velocities based on measured pore water profiles and advection rates.
- Map spatial heterogeneity in fluid chemistry to infer discrete subsurface conduits.
- Predict depth of fluid origin using calculated formation water temperatures from geothermometers.
- Assess the role of bioirrigation for benthic fluxes based on depth-integrated rate comparisons.
Strengths
- Includes calculated formation water temperatures with specific ranges (55-80°C for Olimpi, 80-145°C for Anaximander).
- Provides quantified advective flow velocities (3-50 cm y⁻¹) and bioirrigation rates.
- Focuses on two distinct geographic areas (Olimpi Field and Anaximander Mountains) for comparison.
Limitations
- Column-level documentation is absent; field semantics must be inferred after download.
- Row count is unknown, which may limit suitability assessment.
Provenance
- Source
- Australian Ocean Data Network
- Collection Method
- Pore water chemistry study of mud volcanoes, with profiles simulated for upward advection and bioirrigation.
- Time Range
- null
- Freshness
- Last updated 2026-04-10 17:22:21.450057; freshness should be verified.
- Geography
- Eastern Mediterranean Sea (Olimpi Mud Volcano Field and Anaximander Mountains)