Reconstruction of climate and ecology of Skagit Valley, Washington, from 27.7 to 19.8 ka based on plant and beetle macrofossils.

Glacial lake sediments exposed at two sites in Skagit Valley, Washington, encase abundant macrofossils dating from 27.7 to 19.8 cal ka BP. At the last glacial maximum (LGM) most of the valley floor was part of a regionally extensive arid boreal (subalpine) forest that periodically included montane a...

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Publicado en:Quaternary Research Vol. 106; pp. 94 - 113
Autores principales: Riedel, Jon L., Telka, Alice, Bunn, Andy, Clague, John J.
Formato: Artículo
Publicado: Cambridge University Press Mar2022
Acceso en línea:Ver este registro en EBSCOhost