西菲律宾海190ka以来钙质超微化石的氧碳同位素记录

赵京涛; 李铁刚; 常凤鸣; 李军

Volume 33 Issue 2

Mar. 2008

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Article Navigation > Earth Science > 2008 > 33(2): 183-189

ZHAO Jing-tao, LI Tie-gang, CHANG Feng-ming, LI Jun, 2008. Oxygen and Carbon Isotope Records of Calcareous Nannofossils from the West Philippine Sea during the Last 190 ka. Earth Science, 33(2): 183-189.

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ZHAO Jing-tao, LI Tie-gang, CHANG Feng-ming, LI Jun, 2008. Oxygen and Carbon Isotope Records of Calcareous Nannofossils from the West Philippine Sea during the Last 190 ka. Earth Science, 33(2): 183-189.

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Oxygen and Carbon Isotope Records of Calcareous Nannofossils from the West Philippine Sea during the Last 190 ka

ZHAO Jing-tao^{1, 2, 3, 4
,},
LI Tie-gang¹,
CHANG Feng-ming¹,
LI Jun^{3, 4}

1.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.
Graduate School, Chinese Academy of Sciences, Beijing 100039, China
3.
Qingdao Institute of Marine Geology, Qingdao 266071, China
4.
Qingdao Institute of Marine Geology, Ministry of Land and Resources, Qingdao 266071, China

Received Date: 2007-07-08
Publish Date: 2008-03-25

Abstract

Abstract

The piston core Ph05-5 recovered from the West Philippine Sea (16.049 3°N, 124.344 8°E, water depth 3 382 m) was used to study the δ¹⁸O and δ¹³C variations of calcareous nannofossils.The δ¹⁸O values of calcareous nannofossils were obviously lower in Holocene and the last interglaciation than those in the last and the penultimate glaciation.During the last 190 ka the nannofossil δ¹⁸O values were positively correlated with those of planktonic and benthic foraminifera from the same core.But the average δ¹⁸O value of nannofossils was 0.431×10^-3, higher than that of planktonic foraminifera Globigerinoides rubber, and was 0.410×10^-3, lower than that of planktonic foraminifera Neogloboquad rina dutertrei.All the above three average δ¹⁸O values were much lower than those of benthic foraminifera Cibicides wullerstorfi.The change of nannofossil δ¹³C values showed similar trends with the absolute abundance of calcareous nannofossils in core Ph05-5, which also indicates the primary productivity variations in the West Philippine Sea.The primary productivity stayed at a stable but relatively low level at MIS 6 and MIS 5e.There was an abrupt rise at the beginning of MIS 5d for the primary productivity which retained high value until 25 ka BP.The primary productivity showed a slight decline during MIS 2 and MIS 1, but still higher than that of MIS 6 and MIS 5e.
- West Philippine Sea,
- calcareous nannofossils,
- oxygen and carbon stable isotopes,
- primary productivity

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References(32)

References

Anderson, T. F., Cole, S. A., 1975. The stable isotope geochemistry of marine coccoliths: A preliminary comparison with planktonic foraminifera. Journal of Foraminiferal Reaearch, 5: 188-192. doi: 10.2113/gsjfr.5.3.188

Anderson, T. F., Steinmetz, J. C., 1981. Isotopic and biostratigraphical records of calcareous nannofossils in a Pleistocene core. Nature, 294 (5893): 741-744.

Baumann, K. H., Andruleit, H. A., Su, X., 1998. Comparison of different preparation techniques for quantitative nannofossil studies. Journal of Nannoplankton Research, 20 (2): 75-80.

Bollmann, J., Brabec, B., Cortes, M. Y., et al., 1999. Determination of absolute coccolith abundances in deep-sea sediments by spiking with microbeads and spraying (SMS-method). Marine Micropaleontology, 38 (1): 29-38. doi: 10.1016/S0377-8398(99)00032-8

Dudley, W. C., Blackwelder, P., Brand, L., et al., 1986. Stable isotopic composition of coccoliths. Marine Micropaleontology, 10: 1-8. doi: 10.1016/0377-8398(86)90021-6

Dudley, W. C., Duplessy, J. C., Blackwelder, P. L., et al., 1980. Coccoliths in Pleistocene-Holocene nannofossil assemblages. Nature, 285 (5762): 222-223. doi: 10.1038/285222a0

Dudley, W. C., Goodney, D. E., 1979. Oxygen isotope content of coccoliths grown in culture. Deep Sea Research Ⅰ, 26 (5): 495-503. doi: 10.1016/0198-0149(79)90092-X

Dudley, W. C., Nelson, C. S., 1989. Quaternary surface-water stable isotope signal fromcalcareous nannofossils at DSDP Site 593, southern Tasman Sea. Marine Micropaleontology, 13 (4): 353-373. doi: 10.1016/0377-8398(89)90025-X

Goodney, D. E., Margolis, S. V., Dudley, W. C., et al., 1980. Oxygen and carbon isotopes of recent calcareous nannofossils as palaeoceanographic indicators. Marine Micropaleontology, 5: 31-42. doi: 10.1016/0377-8398(80)90005-5

Jian, Z. M., Li, B. H., Wang, J. L., 2003. Formation and evolution of the western Pacific WarmPool recorded by microfossils. Quaternary Sciences, 23 (2): 185-192 (in Chinese with English abstract).

Jiang, L. B., Jian, Z. M., Cheng, X. R., 2004. Oxygen and carbon stable isotopic records of planktonic foraminifers from the Western Equatorial Pacific since the Last Glacial Maximum. Marine Geology and Quaternary Geology, 24 (2): 67-71 (in Chinese with English abstract).

Kinkel, H., Baumann, K. H., Cepek, M., 2000. Coccolithophores in the equatorial Atlantic Ocean: Response to seasonal and Late Quaternary surface water variability. Marine Micropaleontology, 39 (1-4): 87-112. doi: 10.1016/S0377-8398(00)00016-5

Lea, D. W., Pak, D. K., Spero, H. J., 2000. Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science, 289: 1719-1724. doi: 10.1126/science.289.5485.1719

Liu, C. L., Cheng, X. R., Wang, R. J., et al., 2005. Oxygen and carbon isotope records of Quaternary calcareous nannofossils from the western Pacific Warm Pool and their paleoceanographical significance. Earth Science-Journal of China University of Geosciences, 30 (5): 559-603 (in Chinese with English abstract).

Liu, C. L., Cheng, X. R., Zhu, Y. H., et al., 2002. Oxygen and carbon isotope records of calcareous nannofossils for the past 1 Ma in the South China Sea. Chinese Science Bulletin, 40 (10): 798-803.

Margolis, S. V., Kroopnick, P. M., Goodney, D. E., et al., 1975. Oxygen and carbonisotopes fromcalcareous nannofossils as paleoceanographic indicators. Science, 189: 555-557. doi: 10.1126/science.189.4202.555

Martinson, D. G., Pisias, N. G., Hays, J. D., et al., 1987. Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300, 000 year chronostratigraphy. Quaternary Researtch, 27: 1-29.

Molfino, B., McIntyre, A., 1990. Nutricline variation in the equatorial Atlantic coincident with the Younger Dryas. Paleoceanography, 5: 997-1008. doi: 10.1029/PA005i006p00997

Okada, H., Honjo, S., 1973. The distribution of oceanic coccolithophorids in the Pacific. Deep Sea Research and Oceanographic Abstracts, 20 (4): 355-364. doi: 10.1016/0011-7471(73)90059-4

Stoll, H. M., Ziveri, P., 2002. Separation of monospecific and restricted coccolith assemblages from sediments using differential settling velocity. Marine Micropaleontology, 46 (1-2): 209-221. doi: 10.1016/S0377-8398(02)00040-3

Su, X., Ma, W. L., Cheng, Z. B., 2004. Calcareous nannofossil biostratigraphy for Co-rich ferromanganese crusts from Central Pacific Seamounts. Earth Science—Journal of China University of Geosciences, 29 (2): 141-147 (in Chinese with English abstract).

Thompson, P. R., Be, W. H. A., Duplessy, J. C., et al., 1979. Disappearance of pink-pigmented Globigerina rubber at 12 000 000yr BP in the Indian and Pacific Oceans. Nature, 280: 554-558. doi: 10.1038/280554a0

Tian, J., Wang, P. X., Cheng, X. R., 2004. Stable isotope equilibrium test between benthic foraminifer Cibicidoides and Uvigerinaat ODP Site1143, Southern South China Sea. Earth Science—Journal of China University of Geosciences, 29 (1): 1-6 (in Chinese with English abstract).

Visser, K., Thunell, R., Stott, L., 2003. Magnitude and timing of temperature change in the Indo-Pacific Warm Pool during deglaciation. Nature, 421: 152-155. doi: 10.1038/nature01297

Webster, P. J., Magana, V. O., Pal mer, T. N., et al., 1998. Monsoons: Processes, predictability, and the prospects for prediction. Journal of Geophysical Research, 103 (C7): 14451-14510. doi: 10.1029/97JC02719

Ziveri, P., Stoll, H., Probert, I., et al., 2003. Stable isotope "vital effects" in coccolith calcite. Earth and Planetary Science Letters, 210 (1-2): 137-149. doi: 10.1016/S0012-821X(03)00101-8

翦知湣, 李保华, 王吉良, 2003. 从微体化石看西太平洋暖池的形成与演化. 第四纪研究, 23 (2): 185-192. doi: 10.3321/j.issn:1001-7410.2003.02.008

蒋来宾, 翦知湣, 成鑫荣, 2004. 赤道西太平洋末次盛冰期以来的浮游有孔虫氧碳稳定同位素记录. 海洋地质与第四纪地质, 24 (2): 67-71. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200402011.htm

刘传联, 成鑫荣, 王汝建, 等, 2005. 西太平洋暖池区第四纪钙质超微化石氧碳同位素特征及意义. 地球科学——中国地质大学学报, 30 (5): 559-603. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200505006.htm

刘传联, 成鑫荣, 祝幼华, 等, 2002. 南海南部近百万年来钙质超微化石氧、碳同位素记录. 科学通报, 47 (5): 330-335. doi: 10.3321/j.issn:0023-074X.2002.05.003

苏新, 马维林, 程振波, 2004. 中太平洋海山区富钴结壳的钙质超微化石地层学研究. 地球科学——中国地质大学学报, 29 (2): 141-147. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200402003.htm

田军, 汪品先, 成鑫荣, 2004. 南海ODP1143站底栖有孔虫Cibicidoides与Uvigerina稳定氧碳同位素值的均衡试验. 地球科学——中国地质大学学报, 29 (1): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200401000.htm

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