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Younger Dryas “black mats” and the Rancholabrean termination in North America
Of the 97 geoarchaeological sites of this study that bridge the Pleistocene-Holocene transition (last deglaciation), approximately two thirds have a black organic-rich layer or “black mat” in the form of mollic paleosols, aquolls, diatomites, or algal mats with radiocarbon ages suggesting they are s...
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| Autor principal: | |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2008
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| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2373324/ https://ncbi.nlm.nih.gov/pubmed/18436643 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0800560105 |
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