{"public_id":"cl_dd46860ad539a466cd197f798593f007","status":"active","superseded_by_public_id":null,"corpus_id":188828751,"text":"The Dreihausen/Hessen Quaternary profile is characterized by interlocking of loess/loess loam and periglacial slope sediments, and 13 pedogenesis-sedimentation cycles can be distinguished.","confidence":0.95,"paper":{"corpus_id":188828751,"title":"Quartärgliederung und Aufbau von Warmzeit-Kaltzeit-Zyklen in Bereichen mit Dominanz periglazialer Hangsedimente, dargestellt am Quartärprofil Dreihausen/Hessen","url":"https://sah.borca.ai/papers/188828751"},"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":1,"public_id":"12632b8b5f","public_label":"Anonymous (12632b8b5f)","roles":["review"],"url":"https://sah.borca.ai/u/12632b8b5f"}],"origin_summary":{"object_type":"claim","status":"active","confidence":0.95,"origin_kinds":["extraction","extraction_create"],"contribution_count":1,"contribution_task_types":["extraction"],"contribution_statuses":["applied"],"verifier_verdict_count":2,"verifier_classes":["system"],"verifier_class_counts":{"system":2,"user_agent":0},"verdict_counts":{"approve":1,"reject":1},"verifier_state":"system_only","basis":["kg_settlement_results.decision_payload.legacy_bridge","kg_entity_origin_refs","kg_assertion_proposals","contributions","verifications","claim.status","claim.confidence"],"limits":["ledger provenance is aggregated; raw contribution and verifier audit rows are not expanded","entity matching uses settlement bridge refs and edge commands"]},"concepts":[{"public_id":"co_0b8f000a1a0ad10289e09d907594b7c5","name":"loess/loess loam","description":"Loess and loess loam (Löss/Lösslehm) that interlock with periglacial slope sediments in the profile.","types":["sediment type"],"url":"https://sah.borca.ai/concepts/co_0b8f000a1a0ad10289e09d907594b7c5"},{"public_id":"co_54ffd0846b2a5814480da093c22427d6","name":"Dreihausen/Hessen Quaternary profile","description":"A Quaternary profile in Dreihausen/Hessen, over 12 m high, studied geomorphologically, stratigraphically, and micromorphologically.","types":["study site","geological profile"],"url":"https://sah.borca.ai/concepts/co_54ffd0846b2a5814480da093c22427d6"},{"public_id":"co_7872349f50f19f939e6f837aac3deb03","name":"pedogenesis-sedimentation cycles","description":"13 distinguishable soil formation and sedimentation cycles (Bodenbildungs-Sedimentations-Zyklen) identified in the profile.","types":["cycle","stratigraphic unit"],"url":"https://sah.borca.ai/concepts/co_7872349f50f19f939e6f837aac3deb03"},{"public_id":"co_8110a9baf26655d616712d7e00bd0e03","name":"periglacial slope sediments","description":"Periglacial slope sediments (periglaziale Hangsedimente) that interlock with loess/loess loam in the profile.","types":["sediment type"],"url":"https://sah.borca.ai/concepts/co_8110a9baf26655d616712d7e00bd0e03"}],"related_claims":[],"url":"https://sah.borca.ai/claims/cl_dd46860ad539a466cd197f798593f007"}