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Contribution seq 16839

CREATE_SOURCE_LOCATION EPISTEMIC custody SERVER ACCEPTED server-held key

Signer ed25519:71858824de92da3c8a83b5ff952e4b603e916138eda4ec764837c12e1efd24fe · received 2026-09-29T00:53:05.134180Z · client time 2026-09-29T00:53:05Z

client signature: verifies server signature: verifies chain: intact

prev sha256:7808a4b4c39d9b953846250ae9126244de5e20b0ebc9b7301dd5ebd57c017463
entry sha256:be4f9daa31f1dfa1d50575d64da3b688f399d0606be5295200281e24588b0a4f
envelope sha256:a6f9be49d6b2392f800d99435153eb754ae67f16dc0e773e8a2942e8e601f5a7
payload sha256:d942cf6c588e07bc632a3163b8b0139c74cb2d342c9caabbbcab5745c87bce8d

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

Payload

{
  "excerpt": "Here, we develop long-run Miocene simulations featuring deep-ocean equilibration and water isotope capability, and present a probabilistic inference framework integrating them with a global compilation of benthic foraminiferal δ18O to better constrain the MCO warmth. Our approach yields a maximum likelihood estimate of MCO global mean surface temperature of 7.5 °C above preindustrial, significantly warmer than previous benthic δ18O-based reconstructions.",
  "locator": {},
  "source_id": "6622ebd6-a37f-8723-8f96-104a7d10da10",
  "excerpt_hash": "sha256:8ae2811d14e3782dcf8caf1dacb86f65941d5d911bb3298f22b3678212a51587",
  "locator_type": "QUOTE"
}

Rows created

Status history

seqeventdetail
16839APPENDED
16840ACCEPTAUTOMATIC_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":"MANUAL","principal_tier":"PSEUDONYMOUS","downstream_count":0,"outcome_is_unusual":false}