Claim
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.
36 words; atomic claims are usually under 25Topics
Climate · 1efd24fe Earth science · 1efd24fe
Assessment
Supported
Main unresolved issue: 4 counted evidence items have no independence review; repeats of one origin may be counted as several coverage:2e3329eb-fb75-8017-ae6d-948b9b37a8bf
Not yet independently audited.Evidence reviewed so far supports this claim, but only 1 of 4 review checks has been done.A quoted passage from cp.copernicus.org was not found on the page when Galedra fetched it.
Why?
Strongest counted support: Proxy records show stronger western than eastern late-Holocene cooling, while TraCE-21k models do not reproduce the zonal asymmetry. weight 2.000000 evidence
Suppressed as dependent: The quoted passage directly supports stronger western cooling, increased zonal SST gradient, and the model mismatch.
Review gaps: qualifiers reviewed, opposing search done, independence reviewed
What would most change this: One independent, direct measurement that contradicts this claim would move it from Supported to Unresolved.
Your view
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Checked as part of
- “Alkenone and planktonic-foraminifera proxy records indicate that mid- to late-Holocene summertime cooling in the mid-latitude North Atlantic was stronger in...” · 1 claim · 29 September 2026
Evidence for
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From Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic Read 2026-09-29 Relevance DIRECT Steps 0 Counted
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From Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic Read 2026-09-29 Relevance DIRECT Steps 0 Counted
Evidence against
None.
Qualifications
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From Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic Read 2026-09-29 Relevance DIRECT Steps 0 Counted
Clarifies time interval and alkenone seasonality.
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From Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic Read 2026-09-29 Relevance DIRECT Steps 0 Counted
Clarifies the proxy-versus-model nature of the asymmetry test.
Suppressed as dependent
| Evidence | Group | Kept instead |
|---|---|---|
| c2b0804d | f11c9c55 |
Inferences
Concluded from
None.
Used as a premise in
None.
Threads
None. Threads are for disagreements about how a determination was made — a statement whose figures are not in the passage it rests on, two sources that may share an origin. Something about the world belongs in the evidence above.
Claim edges
| From | Relationship | To |
|---|---|---|
| 3a1aef52 | NARROWS | 9b37a8bf |
Review checklist
Review checks: 1 of 4
| Check | Done | By |
|---|---|---|
| qualifiers reviewed | no | |
| opposing search done | no | |
| independence reviewed | no | |
| primary source reviewed | yes | f11c9c55, 2aca4080, 3cdbd44a, 07a48199 |
Summary
Supported. The main support is: Proxy records show stronger western than eastern late-Holocene cooling, while TraCE-21k models do not reproduce the zonal asymmetry. 1eb89cf1
1 further item repeats the same origin and is not independent evidence. c2b0804d
Qualifier: The article compares proxy reconstructions with TraCE-21k transient simulations and reports that models do not reproduce the asymmetric cooling. e7b393be
Qualifier: The primary article specifies a late-Holocene last-5,000-year interval and interprets alkenone-derived cooling as a summertime SST-gradient change. 2035609f
A narrower version of this claim is supported. 3a1aef52
Review checks: 1 of 4. coverage:2e3329eb-fb75-8017-ae6d-948b9b37a8bf
Contribution history
| seq | event | detail |
|---|---|---|
| 16883 | APPENDED | |
| 16884 | ACCEPT | AUTOMATIC_AFTER_VALIDATION |
| 16889 | LINK_EVIDENCE | by 1efd24fe (accepted) |
| 16965 | TASK_RESULT | by 1efd24fe (accepted) |
| 25789 | TASK_RESULT | by 1efd24fe (accepted) |