Early Maastrichtian carbon cycle perturbation and cooling event: Implications from the South Atlantic Ocean
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Bibliographic record
Abstract
Published stable isotope records in marine carbonate are characterized by a positive δ 18 O excursion associated with a negative δ 13 C shift during the early Maastrichtian. However, the cause and even the precise timing of these excursions remain uncertain. We have generated high‐resolution foraminiferal stable isotope and gray‐scale records for the latest Campanian to early Maastrichtian (∼73–68 Ma) at two Ocean Drilling Program sites, 525 (Walvis Ridge) and 690 (Weddell Sea). We demonstrate that the negative δ 13 C excursion is decoupled from the δ 18 O increase with a lag of about 600 ka. Our δ 13 C records (both planktic and benthic) show an amplitude for the negative excursion of 0.7‰ that falls between about 72.1 and 70.7 Ma. Our planktic δ 18 O records indicate an overall increase of 1.2‰ from 73 to 68 Ma at Site 690, whereas at Site 525 they record a slightly smaller increase (∼1‰) that peaks around 70.1 Ma with decreasing values thereafter. Our benthic δ 18 O data indicate an increase of ∼1.5‰ at Site 525 and ∼0.7‰ at Site 690 between about 71.4 and 69.9 Ma. Benthic δ 18 O values show different baseline values at the two sites before and after the excursion, but the larger increase at Site 525 means that the values attained at the peak of the excursion are similar at the two sites. We interpret this observation in terms of water mass changes. The excursion is interpreted to reflect a cooling of bottom waters in response to the strengthening contribution of intermediate‐ to deep‐water production in the high southern latitudes rather than increased ice volume. The associated carbon cycle perturbations that we observe are interpreted to reflect a weakening of surface water stratification and increased productivity, as supported by our gray value data.
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Full frame distilled prediction
Teacher imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it