Abstract
Notable changes in continental weathering rates, depositional settings for sediments, and global climate are indicated by the isotopic records of strontium and oxygen and the eustatic sea-level curve for the Neogene, and support the notion that the Neogene was the culmination of a number of important Tertiary trends in global geochemical cycling. -from Author
| Original language | English (US) |
|---|---|
| Pages (from-to) | 273-282 |
| Number of pages | 10 |
| Journal | Unknown Journal |
| State | Published - Jan 1 1990 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
All Science Journal Classification (ASJC) codes
- General Environmental Science
- General Earth and Planetary Sciences
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