Modelling the δ18O value of cave drip water and speleothem calcite
Stable isotope signals recorded in speleothems have provided important insights about past climate variability in recent years. Quantitative reconstruction of mean annual temperature and the amount of precipitation, however, remains difficult because the stable isotope signals are influenced by vari...
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| Hauptverfasser: | , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
12 October 2010
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| In: |
Earth and planetary science letters
Year: 2010, Jahrgang: 299, Heft: 3/4, Pages: 387-397 |
| ISSN: | 1385-013X |
| DOI: | 10.1016/j.epsl.2010.09.019 |
| Online-Zugang: | Resolving-System, lizenzpflichtig, Volltext: https://doi.org/10.1016/j.epsl.2010.09.019 Verlag, lizenzpflichtig, Volltext: https://www.sciencedirect.com/science/article/pii/S0012821X10005947 
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| Verfasserangaben: | A. Wackerbarth, D. Scholz, J. Fohlmeister, A. Mangini |
| Zusammenfassung: | Stable isotope signals recorded in speleothems have provided important insights about past climate variability in recent years. Quantitative reconstruction of mean annual temperature and the amount of precipitation, however, remains difficult because the stable isotope signals are influenced by various processes. Here we present a drip water model, which shows how these climate parameters affect the oxygen isotope signal of cave drip water... |
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| Beschreibung: | Im Titel erscheint die Zahl 18 hochgestellt Gesehen am 19.09.2023 |
| Beschreibung: | Online Resource |
| ISSN: | 1385-013X |
| DOI: | 10.1016/j.epsl.2010.09.019 |