Arthur M A, Schlanger S O. 1979. Cretaceous "Oceanic Anoxie Events" as causal factors in development of reef-reservoired giantoil fields. Amer. Assoc. Petrol. Geol. Bull., 63:870-885.
[5]
Caron M, Robaszynski F, Amedro F, Baudin F, Deconinck J F,Hochuli P, Salis Perch Nielsen K0 Tribovillard N. 1999.Estimation de la duree de l\\'evenement anoxique global au passage Cenomanien/Turonien. Approche cyclostratigraphique dans la formation Bahloul en Tunisie centrale. Bull. Soc. Geol. France,170: 145-160.
[6]
Grocke D R, Hesselbo S P, Jenkyns H C. 1999. Carbon isotope composition of Lower Cretaceous fossil wood: Ocean-atmosphere chemistry and relation to sea level change. Geology, 27:155158.
[7]
Hasegawa T. 2003. Cretaceous terrestrial paleoenvironments of northeastern Asia suggested from carbon isotope stratigraphy:Increased atmospheric Pco2-induced climate. Journal of Asian Earth Sciences, 21 : 849-859.
[8]
Jenkyns H C. 1980. Cretaceous anoxic events: from continents to oceans. J. Geol. Soc. London, 137: 171-188.
[9]
Kuhnt W, Nederbragt A J, Leine L. 1997. Cyclicity of CenomanianTuronian organiccarbon-rich sediments in the Tarfaya AtlanticCoastal Basin, Morocco. Cretaceous Research, 18 : 587-601.
[10]
Schlanger S O, Jenkyns H C. 1976. Cretaceous oceanic anoxic events:Causes and consequences. Geol. Mijnbouw, 55: 179-184.
[11]
Scholle P A, Arthur M A. 1980. Carbon isotope fluctuations in Cretaceous pelagic limestones: Potential stratigraphic and petroleum exploration tool. AAPG Bull. , 64:67-87.
[12]
Wan Xiaoqiao, Wignall P B, Zhao Wenjin. 2003b. The CenomanianTuronian extinction and oceanic anoxic event: evidence from South Tibet. Paleogeography, Paleoclimatology, Paleoecology,199 (3-4):283-298.
Arthur M A, Dean W E, Schlanger S O. 1985. Variations in global carbon cycling during the Cretaceous related to cllmate,volcanism, and changes in atmospheric CO2. In: Sundquist E T,Broecker W S eds. The Carbon Cycle and Atmospheric CO2:Natural Variations Archean to Present. Geophys. Monogr.,Am. Geophyics. Union, 32: 504-529.
[18]
Arthur M A, Dean W Eo Pratt L M. 1988. Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary. Nature, 335: 714-717.
[19]
Bartley J K. 2004. Marine carbon reservoir, Corg-Ccarb coupling,and the evolution of the Proterozoie carbon cycle. Geology, 32(2): 129-132.
[20]
Gale A S, Jenkyns H C, Kennedy W J, Corfield R M. 1993.Chemostratigraphy versus biostratigraphy: data from around the Cenomanian-Turonian boundary. J. Geol. Soc. London, 150:29-32.
[21]
Hart M B. 1991. The Late Cenomanian calcisphere global bioevent.Proc. UssherSoc., 7: 413-417.
[22]
Jarvis I, Carson G, Hart M, Leary P, Tocher B A. 1988. The Cenomanian-Turonian (Late Cretaceous) anoxic event in SWEngland, evidence from Hooken Cliffs near Beer, SE Devon.Newsletters on Strat, 18: 147-164.
[23]
Jenkyns H C, Gale A S, Corfield R M. 1994. Carbon- and oxygenisotope stratigraphy of the English Chalk and Italian Scaglia and its paleoclimatic significance. Geol. Mag., 131: 1-34.
[24]
Liu Zhaojun, Wang Dongpo, Liu Li, Liu Wanzhu, Wang Pujun, Du Xiaodi, Yang Guang. 1992. Sedimentary Characteristics of the Cretaceous Songliao Basin. Acta Geologica Sinica, 66(4): 327-338.
[25]
Meyers S R, Sageman B B, Hinnov L A. 2001. Integrated quantitative stratigraphy of the Cenomanian-Turonian Bridge Creek Limestone Member using evolutive harmonic analysis and stratigraphic modeling. Journal of Sedimentary Research, 71:628-644.
[26]
Prokoph A, Villeneuve M, Agterberg F P, Rachold V. 2001.Geochronology and calibration of global Milankovitch cyclicity at the Cenomanian-Turonian boundary. Geology, 29: 523-526.
[27]
Tsikos H, Jekyns H C, Walsworth Bell B, et al. 2004. Carbon isotope stratigraphy recorded by the Cenomanian/Turonian Oceanic Anoxie Event: correlation and implication based on three key localities. Journal of Geological Society of London, 161(4):711-719.
[28]
Yapp C J, Poths H. 1996. Carbon isotopes in continental weathering environments and variations in ancient atmospheric CO2 pressure.Earth and Planetary Science Letters, 137 (1-4) : 71-82.