Classifier Instance:

Anchor text: rhyniophytoid
Target Entity: Rhyniophyta
Preceding Context: In the Welsh Borders, the first evidence of wildfire is
Succeeding Context: plant fossils preserved as charcoal, dating to the Silurian period (about ). Smoldering surface fires started to occur sometime before the Early Devonian period . Low atmospheric oxygen during the Middle and Late Devonian was accompanied by a decrease in charcoal abundance. Additional charcoal evidence suggests that fires continued through the Carboniferous period. Later, the overall increase of atmospheric oxygen from 13% in the Late Devonian to 30-31% by the Late Permian was accompanied by a more widespread distribution of wildfires. Later, a decrease in wildfire-related charcoal deposits from the late Permian to the Triassic periods is explained by a decrease in oxygen levels.
Paragraph Title: History
Source Page: Wildfire

Ground Truth Types:

|---wordnet_entity_100001740
|  |---wordnet_artifact_100021939
|  |  |---wordnet_structure_104341686
|  |  |  |---wordnet_building_complex_102914991
|  |  |  |  |---wordnet_plant_103956922
|  |---yagoGeoEntity
|  |  |---wordnet_structure_104341686
|  |  |  |---wordnet_building_complex_102914991
|  |  |  |  |---wordnet_plant_103956922

Predicted Types:

TypeConfidenceDecision
wordnet_artifact_100021939-0.7787235908357921 0
wordnet_event_100029378-1.7189471738907973 0
wordnet_organization_108008335-1.8321441422107205 0
wordnet_person_100007846-1.1355557577509223 0
yagoGeoEntity-0.9258170723198385 0
|---wordnet_entity_100001740
|  |---wordnet_artifact_100021939
|  |---wordnet_event_100029378
|  |---wordnet_organization_108008335
|  |---wordnet_person_100007846
|  |---yagoGeoEntity