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| Content Provider | Springer Nature Link |
|---|---|
| Author | Liu, Chuanlian Cheng, Xinrong Zhu, Youhua Tian, Jun Xia, Peifen |
| Copyright Year | 2002 |
| Abstract | Oxygen and carbon isotopic analyses have been carried out on calcareous nannofossils from ODP Site 1143 in the southern South China Sea. The results demonstrate that the δ$^{18}$O values of calcareous nannofossils for the past 1 Ma vary systematically with those of planktonic and benthic foraminifera from the same site. But the average δ$^{18}$O value of nannofossils is 1.869‰ higher than that of planktonic foraminifera, and is 3.855‰ lower than that of benthic foarminifera. There are systematic differences between the δ$^{13}$C values of nannofossils, planktonic foarminifera and benthic foraminifera. The average δ$^{13}$C of nannofossils is 0.756‰ higher than that of benthic foraminifera, and is 0.460‰ lower than that of planktonic foraminifera. The δ$^{13}$C values of nannofossils exhibit a significant positive shift beginning near isotope stage 14 and lasting until stage 8. This study also finds that there is a close ralationship between the δ$^{13}$C of nannofossils and the percentage of Florisphaera profunda. This implies that the δ$^{13}$C of nannofossils can be used as an indicator of sea water surface paleoproductivity. |
| Starting Page | 798 |
| Ending Page | 803 |
| Page Count | 6 |
| File Format | |
| ISSN | 10016538 |
| Journal | Chinese Science Bulletin |
| Volume Number | 47 |
| Issue Number | 10 |
| e-ISSN | 18619541 |
| Language | English |
| Publisher | Science in China Press |
| Publisher Date | 2002-01-01 |
| Publisher Place | Beijing |
| Access Restriction | Subscribed |
| Subject Keyword | oxygen and carbon isotope calcareous nannofossil South China Sea Life Sciences Physics Chemistry/Food Science Science Geosciences Engineering |
| Content Type | Text |
| Resource Type | Article |
| Subject | Multidisciplinary |
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