Oxygen isotopes in orangutan teeth reveal recent and ancient climate variation
Studies of climate variation commonly rely on chemical and isotopic changes recorded in sequentially produced growth layers, such as in corals, shells, and tree rings, as well as in accretionary deposits—ice and sediment cores, and speleothems. Oxygen isotopic compositions (δ18O) of tooth enamel are...
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| Hlavní autoři: | , , , , , , , , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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eLife Sciences Publications Ltd
2024-03-01
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| Edice: | eLife |
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| On-line přístup: | https://elifesciences.org/articles/90217 |
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