Global weathering variations inferred from marine radiogenic isotope records
Determining the past record of chemical weathering is essential for understanding changes in climate and atmospheric CO 2, such as those that occur throughout the Cenozoic (the last 65 my). Many natural radiogenic isotopes in seawater are sensitive to variations in chemical weathering, but taken alo...
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| Veröffentlicht in: | Journal of geochemical exploration 2006-01, Vol.88 (1), p.262-265 |
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| container_title | Journal of geochemical exploration |
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| creator | Burton, Kevin W. |
| description | Determining the past record of chemical weathering is essential for understanding changes in climate and atmospheric CO
2, such as those that occur throughout the Cenozoic (the last 65 my). Many natural radiogenic isotopes in seawater are sensitive to variations in chemical weathering, but taken alone cannot distinguish such changes from those caused by variations in erosional source (such as composition, geographical location or ocean circulation). However, comparison of isotope systems with different sources and different behaviour in seawater can resolve such effects, and the relationship between weathering and climate change can be examined on both long and short timescales. |
| doi_str_mv | 10.1016/j.gexplo.2005.08.052 |
| format | Article |
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| fulltext | fulltext |
| identifier | ISSN: 0375-6742 |
| ispartof | Journal of geochemical exploration, 2006-01, Vol.88 (1), p.262-265 |
| issn | 0375-6742 1879-1689 |
| language | eng |
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| source | Elsevier ScienceDirect Journals |
| subjects | Cenozoic Global weathering Radiogenic isotopes |
| title | Global weathering variations inferred from marine radiogenic isotope records |
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