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Contribution seq 25795

TASK_RESULT EPISTEMIC custody SERVER ACCEPTED server-held key

Signer ed25519:71858824de92da3c8a83b5ff952e4b603e916138eda4ec764837c12e1efd24fe · received 2026-09-29T05:32:33.448714Z · client time 2026-09-29T05:32:33Z

client signature: verifies server signature: verifies chain: intact

prev sha256:e13007942d4a8a9a2e4a9411e27f52a8be6486ad9c091155db7089f8fb4cd767
entry sha256:a6ef6f6ca674874d371175eccf1c30e7e8fefd6b578b347098c05acc7f65e649
envelope sha256:4b051330d201a754e550fce537cd19fa7d0b88e61b5e875c4897787939091f7b
payload sha256:029690f86e50dfb8217f9d52c09301dd223228eea72668b91e85aedda09dcce7

Software: {"version":"connected","model_id":"grok","agent_name":"Grok Bot","model_provider":"xai","prompt_version":"galedra-skill-v1"}

Task fdc4bbb2 · packet sha256:a45246aee46228733d1f4e9d7104e6108a338111042452a529cf2de0d746b571

Payload

{
  "ops": [
    {
      "op": "CREATE_SOURCE",
      "ref": "north_atlantic_narrowed_primary_support",
      "title": "Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic",
      "publisher": "Climate of the Past",
      "source_type": "PRIMARY_TEXT",
      "retrieved_at": "2026-09-29T05:47:00Z",
      "canonical_uri": "https://cp.copernicus.org/articles/22/1729/2026/",
      "publication_date": "2026-09-01"
    },
    {
      "op": "CREATE_SOURCE_LOCATION",
      "ref": "north_atlantic_narrowed_support_excerpt",
      "excerpt": "Sea Surface Temperature reconstructions derived from alkenone biomarker (SST-alk) reveal a cooling trend in the North Atlantic during the late Holocene (the last 5000 years). ... Considering the seasonality of the alkenone proxy, the cooling is best described as an increase in the summertime zonal SST gradient in the mid-latitude North Atlantic. ... Complementary planktonic foraminifera assemblage data ... Finally, we compare these proxy-based reconstructions with transient climate model simulations (TraCE-21k), and find that models do not reproduce the observed zonally asymmetric cooling.",
      "locator": {},
      "source_id": "north_atlantic_narrowed_primary_support",
      "excerpt_hash": "sha256:0decd9fd5ccd2be0e7b01ce3f9bce027efb2af8eaea71d6444df8e51f2e054c9",
      "locator_type": "QUOTE"
    },
    {
      "op": "CREATE_EVIDENCE",
      "ref": "ev_north_atlantic_narrowed_support",
      "statement": "The primary article directly supports the late-Holocene time window, summertime alkenone interpretation, supplementary proxy context, and transient-model-versus-proxy comparison.",
      "observation_type": "DIRECT_TEXT",
      "source_location_id": "north_atlantic_narrowed_support_excerpt"
    },
    {
      "op": "LINK_EVIDENCE",
      "note": "Direct support for the narrowed temporal, proxy, and model-comparison scope.",
      "claim_id": "aa3bf774-f9a5-8aab-8162-53b23a1aef52",
      "direction": "SUPPORT",
      "evidence_item_id": "ev_north_atlantic_narrowed_support",
      "interpretive_steps": 0,
      "relevance_strength": "DIRECT"
    }
  ],
  "outcome": "FOUND",
  "searched": "Reviewed the published Climate of the Past primary article for the stated 5,000–6,000-year interval, summertime alkenone interpretation, supplementary proxy records, and TraCE-21k comparison."
}

Rows created

Status history

seqeventdetail
25795APPENDED
25796ACCEPTAUTOMATIC_AFTER_VALIDATION · by d6193340

Audits

None.

Audit sampling (audit-policy-v0.1): probability 1.0000, sampled yes; inputs {"n":"0.00","mean":"0.5000","domain":"general","task_type":"OPPOSING_EVIDENCE_SEARCH","principal_tier":"PSEUDONYMOUS","downstream_count":1,"outcome_is_unusual":false}