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Speleothem growth intervals reflect New Zealand montane vegetation response to temperature change over the last glacial cycle
Flowstone speleothem growth beneath Mount Arthur, New Zealand shows a clear relationship to vegetation density and soil development on the surface above. Flowstone does not currently form beneath sub-alpine Nothofagus forest above ca. 1000–1100 m altitude but U-Th dating shows it has formed there du...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2020
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7015920/ https://ncbi.nlm.nih.gov/pubmed/32051432 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-58317-8 |
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