| Registro completo |
| Provedor de dados: |
ArchiMer
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| País: |
France
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| Título: |
Is there evidence for a 4.2 ka BP event in the northern North Atlantic region?
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| Autores: |
Bradley, Raymond
Bakke, Jostein
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| Data: |
2019
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| Ano: |
2019
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| Resumo: |
We review paleoceanographic and paleoclimatic records from the northern North Atlantic to assess the nature of climatic conditions at 4.2 ka BP, which has been identified as a time of exceptional climatic anomalies in many parts of the world. The northern North Atlantic region experienced relatively warm conditions in the early Holocene (6–8 ka BP) followed by a general decline in temperatures after ~ 5 ka BP, which led to the onset of Neoglaciation. Although a few records do show a distinct anomaly around 4.2 ka BP (associated with a glacial advance), this is not widespread and we interpret it as a local manifestation of the overall climatic deterioration that characterizes the late Holocene.
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| Tipo: |
Text
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| Idioma: |
Inglês
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| Identificador: |
https://archimer.ifremer.fr/doc/00503/61513/65387.pdf
https://archimer.ifremer.fr/doc/00503/61513/66765.pdf
DOI:10.5194/cp-2018-162
https://archimer.ifremer.fr/doc/00503/61513/
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| Editor: |
Copernicus GmbH
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| Formato: |
application/pdf
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| Fonte: |
Climate of the Past (1814-9324) (Copernicus GmbH), 2019 , Vol. 15 , N. 5 , P. 1665-1676
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| Direitos: |
info:eu-repo/semantics/openAccess
restricted use
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