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The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
Published on: August 3, 2016
Calculating dissolved marine oxygen values based on an enhanced Benthic Foraminifera Oxygen Index
M Kranner1,2, M Harzhauser3, C Beer4
1Geological-Palaeontological Department, Natural History Museum Vienna, Burgring 7, 1010, Vienna, Austria. matthias.kranner@nhm-wien.ac.at.
Marine oxygen minimum zones (OMZs) impact greenhouse gases and habitats. An enhanced Benthic Foraminifera Oxygen Index (EBFOI) improves dissolved oxygen (DO) reconstruction, aiding in understanding past and future OMZ changes.
Area of Science:
- Marine geology and paleoceanography
- Biogeochemical cycles
- Climate change research
Background:
- Marine oxygen minimum zones (OMZs) are critical for global biogeochemical cycles and marine ecosystems.
- Dissolved oxygen (DO) levels are a key factor in OMZ dynamics, influencing habitat availability and greenhouse gas sequestration.
- Existing methods like the Benthic Foraminifera Oxygen Index (BFOI) have limitations in accurately reconstructing past DO levels.
Purpose of the Study:
- To enhance the Benthic Foraminifera Oxygen Index (BFOI) for more accurate reconstruction of dissolved oxygen (DO).
- To develop a novel transfer function for direct conversion of enhanced BFOI (EBFOI) values to DO concentrations.
- To provide improved tools for understanding past and predicting future changes in marine oxygen levels and eutrophication.
Main Methods:
- Developed enhanced Benthic Foraminifera Oxygen Index (EBFOI) formulas incorporating all available benthic foraminifera data.
- Calculated the complete habitable space for benthic foraminifers, including bottom water oxygenation (BWO) and pore water oxygenation (PWO).
- Created and calibrated a new transfer function linking EBFOI values to DO concentrations using modern and fossil datasets.
Main Results:
- The enhanced BFOI (EBFOI) method utilizes comprehensive benthic foraminifera data, including BWO and PWO.
- A novel transfer function enables direct conversion of EBFOI to DO values with up to 38% increased efficiency.
- Calibrated formulas applied to modern and fossil datasets demonstrate significant improvements in DO reconstruction.
Conclusions:
- The EBFOI represents a major advancement in reconstructing marine oxygen levels and identifying eutrophication.
- This new approach provides a robust toolset for analyzing past oceanic changes and tracking current/future OMZ expansion.
- Improved DO reconstructions are crucial for understanding the ecological and biogeochemical impacts of expanding OMZs.
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