Margolis S V, Kroopnick P M, Goodney D E, et al.Oxygen and carbon isotopes from calcareous nannofossils as paleoceanographic indicators[J]. Science,1975, 189: 555-557.
[2]
Stoll H M, Ziveri P. Separation of monospecific and restricted coccolith assemblages from sediments using differential settling velocity[J]. Marine Micropaleontology, 2002, 46(1-2) :209-221.
[3]
Kroopnick P. Correlations between δ^13 C and [Sigma]CO2 in surface waters and atmospheric CO2 [J].Earth and Planetary Science Letters, 1974, 22 (4) :397-403.
[4]
Anderson T F, Steinmetz J C. Isotopic and biostratigraphical records of calcareous nannofossils in a Pleistocene core[J]. Nature, 1981, 294(5893):741-744.
[5]
Dudley W C, Goodney D E. Oxygen isotope content of coccoliths grown in culture [J]. Deep.Sea Research, 1979, 26A: 495-503.
[6]
Dudley W C, Duplessy J C, Blackwelder P L, et al.Coccoliths in Pleistocene-Holocene nannofossil assemblages[J]. Nature, 1980, 285(5762) : 222-223.
[7]
Dudley W C, Blackwelder P, Brand L, et al. Stable isotopic composition of coccoliths[J]. Marine Micropaleontology, 1986, 10:1-8.
[8]
Ziveri P, Stoll H, Probert I, et al. Stable isotope vital effects\\' in coccolith calcite[J]. Earth and Planetary Science Letters, 2003, 210(1-2) : 137-149.
[9]
Schiffelbein P, Thierstein H R. Late Pleistocene coccolith isotope strstigrahy:effects of floral change[J]. EOS Trans Am Geophys Union, 1981, 62: 938.
[10]
Schiffelbein P, Thierstein H R. Late Pleistocene coccolith isotope strstigrahy:effects of floral change[J]. EOS Trans Am Geophys Union, 1981, 62: 938.
[11]
同济大学地质系.古海洋学概论[M].上海:同济大学出版社,1989..
[12]
Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238:oxygen isotope temperature and ice volumes on a 10^5 year and 10^6 year scale [J].Quaternary Research, 1973, 3:39-55.
[13]
Kroopnick P. The distribution of C-13 of TCO2 in the world oceans [J].Deep Sea Research, 1985, 32:57-84.
[14]
Bender M L, Keigwin L D. Speculations about the Upper Miocene changes in abyssal Pacific dissolved bicarbonate δ^13C[J], Earth and Planetary Science Letters, 1979, 45: 383-393.
[15]
Duplessy J C, Shaekleton N J, Matthews R K, et al.δ^13 C record of benthic foraminifera in the last interglacial ocean: inplieations for the carbon cycle and the global deep water circulation [J]. Quaternary Research, 1984, 21: 225-243.
[16]
Duplessy J C, Shackleton N J. Response of global deep-water circulation to earth\\'s climate changes 135 000-107 000 years ago[J]. Nature, 1985, 316:500-507.
[17]
Labeyrie P, Duplessy J C. Changes in the oceanic ^13C/^12C ratio during the last 140 000 years: high-latitude surface water records[J].Palaeoclimatology and Palaeoecology, 1985, 50: 217-240.
[18]
Okada H, Honjo S. The distribution of oceanic cocco-lithophorids in the Pacific[J]. Deep Sea Research and Oceanographic Abstracts, 1973, 20(4) : 355-364.
[19]
Fairbanks R W, Wiebe P H. Foraminifera and chorophyll maximun:Vertical distribution, seasonal succession, and paleoceanographic significance[J]. Science, 1980, 209:1524-1 526.
[20]
Duplessy J C, Blanc P L, B4 A W H. Oxygen-18 enrichment of planktonic foraminifera due to gametogenic calcification below the euphotic zone[J]. Science, 1981, 213: 1 247-1 250.
[21]
Thierstein H R, Berger W H. Injection events in ocean histry[J]. Nature, 1978, 276:461-466.
[22]
Thierstein H R, Berger W H. Injection events in ocean histry[J]. Nature, 1978, 276:461-466.
[23]
Dudley W C, Nelson C S. Quaternary surface-water stable isotope signal from calcareous nannofossils at DSDP Site 593, southern Tasman Sea[J]. Marine Micropaleontology, 1989, 13(4): 353-373.