LATE CRETACEOUS UPWELLING SYSTEM ALONG THE SOUTHERN TETHYS MARGIN (ISRAEL) - INTERRELATIONSHIP BETWEEN PRODUCTIVITY, BOTTOM WATER ENVIRONMENTS, AND ORGANIC-MATTER PRESERVATION

Organic-rich Upper Cretaceous sequences in Israel were deposited in an extensive, highly productive upwelling-linked system which prevailed along the southern Tethys margin, and lasted for approximately 19 m.y. (Santonian to late Maastrichtian). An understanding of the spatial an d temporal characteristics of this system was gained through detailed paleontological and geochemical analyses of subsurface sequences in tw o basins in Israel, representing an outer (Shefela) and an inner (Zin) facies belt. The nature of the upwelling system, and its effect on th e sedimentary record, is related to two basic environmental parameters , namely paleoproductivity intensity and oxygen levels at the bottom. The assessment of these parameters and their interrelationship has bee n performed through the development of paleontological (foraminiferal) criteria, which are independent of the organic matter content. Follow ing the establishment of these criteria, it is concluded that the prod uctivity reached its maximum intensity during the late Campanian, whic h was also the time of most notable differentiation between the center of the upwelling system in the inner belt and the less intense condit ions in the outer basin. This distribution is expressed in varied lith ology (organic-rich carbonates, phosphorites, and siliceous rocks) at the core of upwelling and a uniform lithology (organic-rich carbonates ) at the margin of this system. The uniform lithology of the Maastrich tian in both basins, composed of organic-rich carbonates, is ascribed to a gradual weakening of productivity. The bottom conditions in the i nner belt during the late Campanian (the time of maximum surface produ ctivity) were near anoxic, changing to more aerated (dysaerobic) condi tions during the early Maastrichtian. In the outer belt a more aerated bottom (dysaerobic) prevailed throughout the late Campanian to late M aastrichtian. The elevated organic matter content in both basins refle cts the overall environment of high productivity; its actual variation s, however, seem to be unrelated to changes in surface productivity an d bottom oxygen levels.