Description
Cores of the sediments from Oblong Tarn, Mount Kenya, were collected in 1983 and 1986, and were conventional radiocarbon dated to examine late Holocene glacier history of the mountain. Subsequently pollen samples were taken from both cores to create a composite pollen record.
External deposit with Harvard Dataverse.
External deposit with Harvard Dataverse.
Date made available | 21 Jan 2017 |
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Publisher | Harvard Dataverse |