Hedges J I, Keil R G. Sedimentary organic matter preservation:An assessment and speculative synthesis[J].Marine Chemistry, 1995, 49:81-115.
[2]
Milliman J D. Production and accumulation of calcium carbonate in the ocean:budget of a nonsteady state[J], Global Biogeochemical Cycles,1993,7:927-957.
Lin H L, Sheu D D, Yang Y, et al. Stable isotopes in modern planktonic foraminifera:Sediment trap and plankton tow results from the South China Sea[J]. Marine Micropaleontology, 2011, 79:15-23.
[7]
Lin H L, Wang W C, Hung G W. Seasonal variation of planktonic foraminiferal isotopic composition from sediment traps in the South China Sea[J].Marine Micropaleontology, 2004, 53:447-460.
Zhai W, Dai M, Cai W J, et al. The partial pressure of carbon dioxide and air-sea fluxes in the northern South China Sea in spring, summer and autumn[J]. Marine Chemistry, 2005, 96:87-97.
[19]
Dai M, Meng F F, Tang T T, et al. Excess total organic carbon in the intermediate water of the South China Sea and its export to the North Pacific[J]. Geochemistry Geophysics Geosystems, 2009, 10(12), Q12002, doi:10.1029/2009GC002752
Xie L H, Wei G J, Deng W F, et al. Daily δ18O and δD of precipitations from 2007 to 2009 in Guangzhou, South China:Implications for changes of moisture sources[J]. Journal of Hydrology,2011, 400:477-489.
[25]
Burdige D J. Preservation of organic matter in marine sediments:Controls, mechanisms, and an imbalance in sediment organic carbon budgets[J].Chemical Reviews. 2007, 107:467-485.
[26]
Huguet C, Lange G J, Gustafsson O, et al. Selective preservation of soil organic matter in oxidized marine sediments (Madeira Abyssal Plain)[J].Geochimica et Cosmochimica Acta, 2008, 72:6061-6068.
Bemis B E, Spero H J, Bijma J, et al. Reevaluation of oxygen isotopic composition of planktonic foraminifera:experimental results and revised paleotemperature equations[J], Paleoceanography, 1998, 13:150-160.
Su R X, Sun D H, Bloemendal J, et al. Temporal and spatial variability of the oxygen isotopic composition of massive corals from the South China Sea:Influence of the Asian monsoon[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 240:630-648.
[35]
Sun D H, Gagan M K, Cheng H, et al. Seasonal and interannual variability of the Mid-Holocene East Asian monsoon in coral δ18O records from the South China Sea[J]. Earth and Planetary Science Letters, 2005, 237:69-84.
[36]
Coppola L, Gustafsson ?, Andersson P, et al. The importance of ultrafine particles as a control on the distribution of organic carbon in Washington Margin and Cascadia Basin sediments[J]. Chemical Geology, 2007, 243:142-156.
Johnson K R,Ingram B L. Spatial and temporal variability in the stable isotope systematics of modern precipitation in China:implications for paleoclimate reconstructions[J]. Earth and Planetary Science Letters, 2004, 220:365-377.
[39]
Van der Veer G, Voerkelius S, Lorentz G, et al. Spatial interpolation of the deuterium and oxygen-18 composition of global precipitation using temperature as ancillary variable[J]. Journal of Geochemical Exploration, 2009, 101:175-184.
[40]
Araguas-Araguas L, Froehlich K, Rozanski K. Stable isotope composition of precipitation over southeast Asia[J]. J Geophys Res, 1998, 103:28721-28742.
[41]
Dai M, Zhai W, Cai W J, et al. Effects of an estuarine plume-associated bloom on the carbonate system in the lower reaches of the Pearl River estuary and the coastal zone of the northern South China Sea[J]. Continental Shelf Research, 2008, 28:1416-1423.
[42]
Zhai W D, Dai M, Cai W J.Coupling of surface pCO2 and dissolved oxygen in the northern South China Sea:impacts of contrasting coastal processes[J]. Biogeosciences, 2009, 6:2589-2598.
[43]
Hoefs J. Stable Isotope Geochemistry[M]. Berlin:Springer-Verlag, 1997.
[44]
Lin H L, Wang L W, Wang C H, et al. Vertical distribution of δ13C of dissolved inorganic carbon in the northeastern South China Sea[J]. Deep-Sea Research Ⅰ, 1999, 46:757-775.