Tracking ocean circulation and palaeotemperature in Maastrichtian seas using C and O isotopes in belemnite rostra fossils
The Cretaceous period 145-66 million years ago is often cited as a textbook example of a greenhouse climate with high levels of atmospheric carbon dioxide ([CO2]atm) A wealth of palaeoclimate proxy data from the fossil record and studies in isotope geochemistry had previously shown that ocean temper...
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| 格式: | Final Year Project |
| 語言: | English |
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Nanyang Technological University
2023
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| 在線閱讀: | https://hdl.handle.net/10356/165712 |
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