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The influence of vegetation activity on the Dole effect and its implications for changes in biospheric productivity in the mid-Holocene
The Dole effect is defined as the difference between the oxygen isotope composition of atmospheric oxygen and seawater (currently 23.5 parts per thousand) and reflects the balance between processes and fractionations associated with O(2) consumption and production by the terrestrial and marine biosp...
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| Natura: | Artigo |
| Lingua: | Inglês |
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1999
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| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1689808/ https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspb.1999.0682 |
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