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... > Cenozoic > Quaternary > Pleistocene > Middle Pleistocene > Hoxnian

natural phenomenon > climatic phenomenon > interglacial > Hoxnian

... > stratigraphy > climatostratigraphy > climatostratigraphic period > interglacial > Hoxnian

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Hoxnian

The Hoxnian Stage was a middle Pleistocene stage of the geological history of the British Isles. It was an interglacial which preceded the Wolstonian Stage and followed the Anglian Stage. It is equivalent to Marine Isotope Stage 11 (MIS 11). Marine Isotope Stage 11 started 424,000 years ago and ended 374,000 years ago. The Hoxnian is divided into sub-stages Ho I to Ho IV. The Hoxnian Stage is named after Hoxne in the English county of Suffolk where some of the deposits created were first found. It was identified and dated with palynology or pollen evidence in the biostratigraphy and later updated with aminostratigraphic techniques. Based on stratigraphic information the Hoxnian happened after the Anglian glacial as Anglian soil is frequently found underneath Hoxnian deposits. The Hoxnian is an interglacial phase meaning the warm periods in between glacial periods. Interglacial phases are heavily vegetated with woodlands interspersed with open areas. Site deposits are often found over Anglian soil which dates to MIS 12. Most sites have been found in valleys with signs of river deposits. During the interglacial the valleys would have been surrounded by dense forests. (Adapted from: https://en.wikipedia.org/wiki/Hoxnian_Stage)

Hoxnian interglacial
Hoxnian interglaciation
Hoxnian Stage

Hoxnien

francés
interglaciaire hoxnien
interglaciation hoxnienne
stade hoxnien

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http://data.loterre.fr/ark:/67375/QX8-XWCXS9K1-8

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