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Record W7110463997

Controls on High Sedimentary Accumulation of Organic Matter During Cretaceous Oceanic Anoxic Event 2, Southeast Newfoundland Ridge, North Atlantic Ocean

2023· article· W7110463997 on OpenAlexaboutno aff

Bibliographic record

VenueFlorida International University Digital Commons (Florida International University) · 2023
Typearticle
Language
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsAnoxic watersBenthic zoneDeep seaOrganic matterSedimentOxygen minimum zoneWater columnCretaceousTotal organic carbon
DOInot available

Abstract

fetched live from OpenAlex

Deoxygenation and low-oxygen zones are occurring in modern oceans as a consequence of excessive nutrients in runoff. Solving this issue necessitates understanding the relationships between dissolved oxygen, ocean chemistry, inputs of atmospheric CO2, and climate change. As an analog, this study looks back 94 Ma to Oceanic Anoxic Event 2 (OAE2), a global geologic event triggered by greenhouse conditions from increased volcanism. The global carbon cycle was disrupted by OAE2, increasing burial of organic matter on the seafloor. Environmental changes were studied below, within, and above OAE2 sediments from deep-sea sediment cores drilled at Integrated Ocean Drilling Program Site U1407, Southeast Newfoundland Ridge. By analyzing the geochemistry and microscopic fossils, an interval of time within OAE2 was identified when excess nutrients led to oxygen levels so low that microorganisms could not survive on the seafloor and toxic sulfides were present in pore spaces of sediments. After OAE2, nutrient inputs declined, the ocean reoxygenated, and microorganism abundance and diversity recovered. The abnormal OAE2 environmental conditions impacted the sizes and community assemblages of benthic foraminifera, common protists in oceans over the past 500 Myr. To analyze foraminifera, correct sieve sizes for preparing them must be selected so that shell size does not bias results. Abundances recovered from sieves with standard >63 μm and 38-63 μm openings were compared to assess whether key environmental taxa or community trends were lost using larger-sized openings. General trends in both sizes were relatively similar, and no key taxa were lost, so counting large abundances of 38-63 μm shells was not proven time-effective. For >63 μm foraminifera, significant differences in their assemblages were observed at the Cenomanian–Turonian boundary hiatus at the base of the organic-carbon-rich layer deposited during OAE2. Many taxa presumed extinct after the Cenomanian were discovered further up-core in the Turonian, indicating they survived elsewhere and re-populated the area once conditions improved. Future organismal responses to ongoing climate changes that affect local environments will occur under multiple and cumulative stressors, both natural and anthropogenic. Therefore, studying analogs in the geological record provides empirical evidence for predictions of future climate change and deep-sea organismal responses.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.058
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0020.001
Science and technology studies0.0010.001
Scholarly communication0.0000.003
Open science0.0020.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0020.001

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 head0.017
GPT teacher head0.211
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; both teacher heads agree on what is shown here.

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
Published2023
Admission routes1
Has abstractyes

Explore more

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