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Consequently, the depositional pattern of oxygen-poor facies during the Senonian was more dependent on regional factors (Sass and Bein, 1982). , 1987). These changes, observed in the planktonic foraminifera of the Rotalipora cushmani, Whiteinella archaeocretacea, and Helevetoglobotruncana helvetica zones, illustrate some of their adaptive strategies. R. cushmani Zone The Rotalipora specimens in the Gaza basin are reduced in size and outnumbered by Hedbergella. A reduction of test size and low ratios of keeled/ unkeeled species have also been observed in other dysoxic paleoenvironments (Kuhnt et a l , 1986).

N. Leary, B. A. Tocher, D. Home, and A. Rosenfeld, 1988, Microfossil assemblages and the Cenomanian-Turonian (Late Cretaceous) Oceanic Anoxic Event: Cretaceous Research, v. 9, p. 3-103. , 1980, Cretaceous anoxic events—from continents to oceans: Journal of the Geological Society of London, v. 137, p. 171-188. , 1972, Lithostratigraphy and environment of deposition, Judean Group, western and central Galilee, Israel: Israel Geological Survey Bulletin 54, p. 1-56. Lipson-Benitah et al. D. thesis, Hebrew University, Jerusalem, 115 p.

Biostratigraphie, Sedimentologie, Coupures: Memoires du Museum National d'Histoire Naturelle, Serie C, v. 49, p. 15-28. , and M. Raab, 1974, Cenomanian-Turonian ostracodes from the Judea Group in Israel: Israel Geological Deposition of Organic Fades Survey Bulletin 62, p. 1-64. Ryan, W. F. , and M. B. Cita, 1977, Ignorance concerning episodes of oceanwide stagnation: Marine Geology, v. 23, p. 197-215. Saltzman, E. , and E. J. P. cores: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 40, p.

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