Claims
| Claim | Type | Assessment | Score | Review checks | References |
|---|---|---|---|---|---|
| Alkenone and planktonic-foraminifera proxy records indicate that mid- to late-Holocene summertime cooling in the mid-latitude North Atlantic was stronger in the west than east, increasing the zonal sea-surface-temperature gradient; TraCE-21k simulations did not reproduce this asymmetry. | COMPARATIVE | Supported | 0.8808 | 1 of 4 | 127 |