Citation: | ZHANG Jiang-yong, WANG Pin-xian, CHENG Xin-rong, JIN Hai-yan, ZHANG Shi-ying, 2007. Late Quaternary Variations of Productivity in the Western Equatorial Pacific Ocean: Records from ODP Hole 807A. Earth Science, 32(3): 303-312. |
Averyt, K. B., Paytan, A., 2004. A comparison of multipleproxies for export production in the equatorial Pacific. Paleoceanography, 19: PA4003, doi: 10.1029/2004PA001005.
|
Baumann, K., Andruleit, H. A., Su, X., 1998. Comparison of different preparation techniques for quantitative nannofossil studies. Journal of Nannoplankton Research, 20: 75-80. https://www.researchgate.net/publication/283632407_Comparison_of_different_preparation_techniques_for_quantitative_nannofossil_studies
|
Berger, W. H., 1973. Deep-sea carbonates: Pleistocene dissolution cycles. Journal of Foramini feral Research, 3: 187-195. doi: 10.2113/gsjfr.3.4.187
|
Bollmann, J., Baumann, K. H., Thierstein, H. R., 1998. Global dominance of Gephyrocapsa coccoliths in Late Pleistocene: Selective dissolution, evolution, or global environmental change? Paleoceanography, 13: 517-529. doi: 10.1029/98PA00610
|
Burke, S. C., 1981. Recent benthic foraminifera of the On-tong Java Plateau. Journal of Foraminiferal Research, 11: 1-19. doi: 10.2113/gsjfr.11.1.1
|
Corliss, B. H., Chen, C., 1988. Morphotype patterns of Norwegian Sea deep-sea benthic foraminifera and ecologicali mplications. Geology, 16: 716-719.
|
Duce, R. A., Unni, C. K., Ray, B. J., et al., 1980. Long-rangeat mospheric transport of soil dust from Asia to the tropical north Pacific: Temporal variability. Science, 209: 1522-1524. doi: 10.1126/science.209.4464.1522
|
Falkowski, P. G., 1997. Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean. Nature, 387: 272-275. doi: 10.1038/387272a0
|
Herguera, J. C., 1992. Deep-sea benthic foraminifera and biogenic opal: Glacial to postglacial productivity changes in the western equatorial Pacific. Marine Micropalontology, 19: 79-98. doi: 10.1016/0377-8398(92)90022-C
|
Herguera, J. C., Berger, W. H., 1991. Paleoproductivity from benthic foraminifera abundance: Glacial to postglacial change in the west-equatorial Pacific. Geology, 19: 1173-1176. https://pubs.geoscienceworld.org/gsa/geology/article-abstract/19/12/1173/205225/Paleoproductivity-from-benthic-foraminifera
|
Holbourn, A. E., Henderson, A., 2002. Re-illustration and revised taxonomy for selected deep-sea benthic foraminifers. Paleontologia Electronica, 4 (2), 34pp, 628kB; http://pa-leo-electronica.org/paleo2001_2/foram/issue2_01.htm. http://pa-leo-electronica.org/paleo2001_2/foram/issue2_01.htm
|
Hovan, S. A., Rea, D. K., Pisias, N. G., et al., 1989. A direct link between the China loess and marine δ18O records: A eolian flux to the north Pacific. Nature, 340: 296-298. doi: 10.1038/340296a0
|
Hovan, S. A., Rea, D. K., Pisias, N. G., 1991. Late Pleistocene continental climate and oceanic variability recorded in Northwest Pacific sedi ments. Paleoceanography, 6: 349-370. doi: 10.1029/91PA00559
|
Imbire, J., Hays, J. D., Martinson, D. G., et al., 1984. The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record. In: Berger, A. L., Imbire, J., Hags, J. et al., eds., Milankovitch and climate. D. Reidel Publishing Company, Dordrecht, 269-305.
|
Jian, Z., Wang, L., 1997. Late Quaternary benthic foraminifera and deep-water paleo ceanography in the South China Sea. Marine Micropaleontolgy, 32: 127-154. doi: 10.1016/S0377-8398(97)00017-0
|
Kawahata, H., Ohkushi, K., Hatakeyama, Y., 1999. Comparative Late Pleistocene paleoceanographic changes in the mid latitude boreal and austral western Pacific. Journal of Oceanography, 55: 747-761. doi: 10.1023/A:1007824415499
|
Kawahata, H., Suzuki, A., Ahagon, N., 1998. Biogenic sediments in the West Caroline basin, the western equatorial Pacific during the last 330 000 years. Marine Geology, 149: 155-176. doi: 10.1016/S0025-3227(98)00039-5
|
Koutavas, A., Lynch-Stieglitz, J., Marchitto, T. M., et al., 2002. El Niño-like pattern in ice age tropical Pacific sea surface temperature. Science, 297: 226-230. doi: 10.1126/science.1072376
|
Krissek, L. A., Janecek, T. R., 1993. Eolian deposition on the Ontong Java plateau since the Oligocene: Unmixing a record of multiple dust sources. In: Berger, W. H., Kroenke, W., Mayer, L. A., et al., eds., Proceedings of the Ocean Drilling Program, Scientific results. College Station, Texas, Ocean Drilling Program, 130: 471-490.
|
Kroenke, L. W., Berger, W. H., Janecek, T. R., et al., 1991. Proceedings of the Ocean Drilling Project, Initial Reports. College Station, Texas, Ocean Drilling Program, 130: 369-493.
|
Kroopnick, P. M., 1985. The distribution of δ13C of CO2 in the world oceans. Deep Sea Research, 32: 57-84. doi: 10.1016/0198-0149(85)90017-2
|
Kuhnt, W., Hess, S., Jian, Z., 1999. Quantitative composition of benthic foraminiferal assemblages as a proxy indicator for organic carbon flux rates in the South China Sea. Marine Geology, 156: 123-157. doi: 10.1016/S0025-3227(98)00176-5
|
Le, J., Shackleton, N. J., 1992. Carbonate dissolution fluctuations in the western equatorial Pacific during the Late Quaternary. Paleoceanography, 7: 21-42. doi: 10.1029/91PA02854
|
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 palaeoceanog raphical significance. Earth Science-Journal of China University of Geosciences, 30 (5): 559-564, 603 (in Chinese with English abstract). doi: 10.1360/02tb9180
|
Loubere, P., 1998. The impact of seasonality on the benthos as reflected in the assemblages of deeper water benthic foraminifera. Deep Sea Research, 45: 409-432. doi: 10.1016/S0967-0637(97)00092-7
|
Loubere, P., 2000. Marine control of biological production in the eastern equatorial Pacific Ocean. Nature, 406: 497-500. doi: 10.1038/35020041
|
Martin, J. H., 1990. Glacial-interglacial CO2 change: The iron hypothesis. Paleoceanography, 5: 1-13. doi: 10.1029/PA005i001p00001
|
Mix, A. C., 1991. Carbon 13 in Pacific deep and intermediate waters, 0-370ka: Implications for ocean circulation and Pleistocene CO2. Paleoceanography, 6: 205-226. doi: 10.1029/90PA02303
|
Molfino, B., Mclntyre, A., 1990. Precessional forcing of nutricline dynamics in the equatorial Atlantic. Science, 249: 766-769. doi: 10.1126/science.249.4970.766
|
Ohkushi, K., Thomas, E., Kawahata, H., 2000. Abyssal benthic foraminifera from the northwestern Pacific (Shatsky Rise) during the last 298 kyr. Marine Micropaleotology, 38: 119-147. doi: 10.1016/S0377-8398(99)00040-7
|
Okada, H., Honjo, S., 1973. The distribution of oceanic coccolithophorids in the Pacific. Deep Sea Research, 20: 355-374. doi: 10.1016/0011-7471(73)90059-4
|
Petit, J. R., Jouzel, J., Raynaud, D., et al., 1999. Climate and atmospheric history of the past 420 000 years from the Vostokice core, Antarctica. Nature, 399: 429-436. doi: 10.1038/20859
|
Prentice, M. L., Freiz, J. K., Si monds, G. G., et al., 1993. Neogene trends in planktonic foraminifer δ18O from site 807: Implications for global ice volume and western equatorial Pacific sea-surface temperatures. Proceedings of the Ocean Drilling Program, Scientific Results. College Station, Texas, Ocean Drilling Program, 130: 281-306.
|
Ravelo, A. C., Fairbanks, R. G., 1992. Oxygen isotopic composition of multiple species of planktonic foraminifera: Recorders of the modern photic zone temperature gradient. Paleoceanography, 7: 815-831. doi: 10.1029/92PA02092
|
Rea, D. K., 1994. The paleocli matic record provided by eolian deposition in the deep sea: The geologic history of wind. Reviews of Geophysics, 32: 159-195. doi: 10.1029/93RG03257
|
Sarnthein, M., Winn, K., 1990. Reconstruction of low and middle latitude export productivity, 30 000 years B. P. top resent: Implication for control of global carbon reser voirs. In: Schlesinger, M. E., ed., Climateocean interaction. Kluwer Academic Publishers, Dordrecht, 319-342.
|
Tuo, S. T., Liu, Z. F., Zhao, Q. H., et al., 2006. The earliest Oligocene glacial maxmum: Records from ODP Site 1265, South Atlantic. Earth Science-Journal of China University of Geosciences, 31 (2): 151-158 (in Chinese with English abstract). https://en.cnki.com.cn/Article_en/CJFDTotal-DQKX200602001.htm
|
Wang, P., Tian, J., Cheng, X., et al., 2004. Major Pleistocene stages in a carbon perspective: The South China Sea record and its global comparison. Paleoceanography, 19: PA4005, doi: 10.1029/2003PA000991.
|
Wu, G., Berger, W. H., 1991. Pleistocene δ18O records from Ontong-Java plateau: Effects of winnowing and dissolution. Marine Geology, 96: 193-209. doi: 10.1016/0025-3227(91)90147-V
|
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): 559-564, 603.
|
拓守廷, 刘志飞, 赵泉鸿, 等, 2006. 渐新世初大冰期事件: 南大洋ODP1265站的记录. 地球科学——中国地质大学学报, 31 (2): 151-158.
|