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Record W1670829366

The Relationship Between the Diagenetic Cycles of Reducible Iron and Manganese Oxides and Dissolved Organic Carbon (DOC)

2004· article· en· W1670829366 on OpenAlexaboutno aff
L. N. Barazzuol, Alfonso Mucci, Yves Gélinas

Bibliographic record

VenueAGU Spring Meeting Abstracts · 2004
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMarine and coastal ecosystems
Canadian institutionsnot available
Fundersnot available
KeywordsAuthigenicDiagenesisDissolved organic carbonEnvironmental chemistryGeologyDissolutionTotal organic carbonManganeseFractionationSedimentChemistrySedimentary rockGeochemistryGeomorphology
DOInot available

Abstract

fetched live from OpenAlex

Field evidence suggests that the fate of sedimentary dissolved organic carbon (DOC) is linked to the diagenetic cycles of iron and manganese in marine sediments. Co-variations of their concentrations in sediment porewater, as well as the release of DOC upon the reductive dissolution of authigenic iron and manganese oxides lead us to believe that sorption (i.e., co-precipitation and/or adsorption) onto these oxides may play an important role on the diagenetic behavior of DOC. This DOC sink, if it exists, would considerably alter our views of the mechanisms that regulate DOC fluxes across the sediment-water interface as well as their quantification. Sorption onto authigenic metal oxides may also lead to a molecular and isotopic fractionation of DOC.%%%%Oxic surface sediments recovered from the Amundsen Gulf, located south of Banks Island, Northwest Territories, Canada and the Saguenay Fjord, Quebec, Canada were extracted with two different mild reducing agents to determine the amount and composition (molecular and isotopic) of the DOC associated with the authigenic iron and manganese oxides. The reducing agents employed were: (i) 0.25 M hydroxylamine with 0.25 M HCl (HA, pH=1.7) and (ii) 1 N HCl (pH=0). Our results suggest that the sorbed DOC from the Saguenay Fjord sediment is both isotopically (delta13Corg) and molecularly fractionated with respect to the sedimentary particulate organic carbon (POC) pool whereas only molecular fractionation was evident in the Amundsen Gulf samples. The lack of isotopic fractionation in the latter sample set could be attributable to the inefficient extraction of iron oxides (50%) or simply isotopic uniformity, thereby limiting the isotopic fractionation. Molecular analyses by Fourier-Transform Infra-Red Spectroscopy (FTIR) indicate that the porewater and adsorbed DOC pools are most likely dominated by carbohydrates. Our results suggest that the adsorbed DOC pool may buffer the porewater DOC concentration and composition. Based on our preliminary results, we propose that authigenic and detrital iron and manganese oxides that accumulate in oxic sediments scavenge oxygen-rich organic acids diffusing upwards through the sediment column, thereby creating an aging reservoir in the oxic sediments. Slow diffusion across the sediment-water interface and desorption upon resuspension of these sediments in the overlying bottom waters may contribute to the old DOM pool found in benthic marine waters.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.010
Threshold uncertainty score0.980

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.019
GPT teacher head0.212
Teacher spread0.194 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2004
Admission routes1
Has abstractyes

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