Paleowetlands and regional climate change in the central Atacama Desert, northern chile
Widespread, organic-rich diatomaceous deposits are evidence for formerly wetter times along the margins of the central Atacama Desert, one of the driest places on Earth today. We mapped and dated these paleowetland deposits at three presently waterless locations near Salar de Punta Negra (24.5°S) on...
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Veröffentlicht in: | Quaternary research 2008-05, Vol.69 (3), p.343-360 |
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