Matches in DBpedia 2016-04 for { ?s ?p "The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3200 to 2900 BCE. Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.The spatial extent of the change is unclear; it does not show up as a major, or even identifial, event in hemispheric temperature reconstructions."@en }
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- Piora_Oscillation abstract "The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3200 to 2900 BCE. Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.The spatial extent of the change is unclear; it does not show up as a major, or even identifial, event in hemispheric temperature reconstructions.".
- Q1477562 abstract "The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3200 to 2900 BCE. Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.The spatial extent of the change is unclear; it does not show up as a major, or even identifial, event in hemispheric temperature reconstructions.".
- Piora_Oscillation comment "The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3200 to 2900 BCE. Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.The spatial extent of the change is unclear; it does not show up as a major, or even identifial, event in hemispheric temperature reconstructions.".
- Q1477562 comment "The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3200 to 2900 BCE. Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.The spatial extent of the change is unclear; it does not show up as a major, or even identifial, event in hemispheric temperature reconstructions.".