The Holocene Climatic Recovery in South-Western Iberia as Recorded in Limestone Tuff Deposits
| dc.contributor.author | Ribeiro, Carlos | |
| dc.contributor.author | Terrinha, Pedro | |
| dc.contributor.author | Voelker, Antje | |
| dc.contributor.author | Candeias, António | |
| dc.contributor.author | Rosado, Lucia | |
| dc.contributor.author | Guerreiro, Paulo | |
| dc.date.accessioned | 2015-03-20T14:46:53Z | |
| dc.date.available | 2015-03-20T14:46:53Z | |
| dc.date.issued | 2014 | |
| dc.description.abstract | Data on continental limestone shows that following the cold climate of Younger Dryas stadial, conditions for carbonate sedimentation settled in south-western Iberia, leading to the development of the Asseca River (Tavira)limestone tuffs. This formation deposited over a period of ca. 7.5 kyr, preserves a detailed record of the climatic conditions of the area as well as of the vegetation cover | por |
| dc.identifier.authoremail | cribeiro@uevora.pt | |
| dc.identifier.authoremail | pedro.terrinha@ipma.pt | |
| dc.identifier.authoremail | antje.voelker@ipma.pt | |
| dc.identifier.authoremail | candeias@uevora.pt | |
| dc.identifier.authoremail | lclrosado@hotmail.com | |
| dc.identifier.authoremail | pauloguerreiro@gmail.com | |
| dc.identifier.doi | 10.1007/978-3-319-04364-7_164 | |
| dc.identifier.scientificarea | 395 | por |
| dc.identifier.sharewith | DGeo | por |
| dc.identifier.uri | http://hdl.handle.net/10174/13451 | |
| dc.identifier.withinvitedoralpresentation | nao | por |
| dc.identifier.withoralpresentation | sim | por |
| dc.identifier.withposter | nao | por |
| dc.language.iso | por | por |
| dc.publisher | Springer International Publishing | por |
| dc.rights | restrictedAccess | por |
| dc.subject | Holocene | por |
| dc.subject | Climate | por |
| dc.subject | South-western Iberia | por |
| dc.title | The Holocene Climatic Recovery in South-Western Iberia as Recorded in Limestone Tuff Deposits | por |
| dc.type | lecture | por |