Claims
| Claim | Type | Assessment | Score | Review checks | References |
|---|---|---|---|---|---|
| Nitrogen-isotope measurements from tropical Atlantic sediment-core foraminifera indicate that natural nitrogen fixation was substantially lower during the warm late Pliocene and increased into the cooler Pleistocene, with Caribbean variability later tracking the roughly 41,000-year obliquity cycle. | HISTORICAL | Supported | 0.9561 | 1 of 4 | 101 |