『Abstract
　The evolution of Tethyan phosphogenesis during the Cretaceous-Eocene is examined to try to explain fluctuations of phosphogenesis through time, and whether or not they reflect long-term changes in ocean circulation or in continental weathering. Twenty-seven time-stratigraphic phosphate levels in various Tethyan sites, covering a time span of about 90 Myr from the Hauterivian to the Eocene, were analyzed for ⁴⁴Ca/42Ca and ¹⁴³Nd/¹⁴⁴Nd in their carbonate fluorapatite (CFA) fraction. P and Ca accumulation rates and bulk sedimentation rates were quantified throughout the Cretaceous-Eocene Negev sequence to examine how changes in ⁴⁴Ca/42Ca and ¹⁴³Nd/¹⁴⁴Nd are reflected in the intensity of phosphogenesis.
　A clear-cut change occurs in εNd(T ) and δ⁴⁴Ca and in the rates of P and Ca accumulation and bulk sedimentation through the time analyzed. εNd(T ) is much lower in the Hauterivian-Lower Cenomanian (-12.8 to -10.9) than in the Upper Cenomanian-Eocene (-7.8 to -5.9). Much lower δ⁴⁴Ca values occur in the Hauterivian-Turonian (-0.22 to +0.02) than in the Coniacian-Eocene (+0.23 to +0.40). P accumulation rates in the Negev steeply increase from ＜200μmol cm^-2 k yr^-1 in the Albian-Coniacian to 〜1500 μmol cm^-2 k yr^-1 in the Campanian, whereas a strong decrease is concomitantly recorded in the rates of Ca accumulation and bulk sedimentation. In addition, distinct εNd(T ) values are shown by the phosphorites of the Negev (-6.7 to -6.4) and Egypt (-9.0 to -7.6) during the Campanian, and by those of the Negev (-7.8 to -6.3) and North Africa (-10.1 to -8.9) during the Maastrichtian-Eocene.
　The culmination of P accumulation rates in the Negev during the Campanian, occurring with a high in εNd(T ) and δ⁴⁴Ca and a low in sedimentation rates, indicates that paleoceanographic and paleogeographical factors mostly governed phosphorite accumulation in this area. The abrupt εNd(T ) rise after the Cenomanian is attributed to increased incursion of Pacific (radiogenic) water masses into the Tethys, driven by the Late Cretaceous global sea-level rise, the connection between North and South Atlantic, the global post-Santonian cooling, and the progressive widening of the Caribbean threshold, all acting in combination to significantly intensify the Tethyan circumglobal current (TCC). It also reflects a weakening of the continental Nd signal due to a reduction of exposed landmasses caused by increased flooding of continental shelves. High δ⁴⁴Ca values at those times also point to a decrease in weathering Ca⁺² fluxes and expansion of carbonate sedimentation in shelves, both enriching seawater with isotopically heavy Ca⁺². Deep ocean circulation intensified by the post-Santonian cooling of high latitudes increased P inventory in the Tethys basin, whereas the strengthened TCC and the folded shelf likely resulted in coastal and topographically-induced upwelling, supplying P-rich intermediate waters to southeastern Tethys shelves. Only in the Paleocene-Eocene, following major changes in global circulation produced by narrowing Tethys and widening of the Atlantic, did phosphogenesis shifts its locus of high intensity to the western (Atlantic) Tethys and West African Atlantic coasts. This change in paleocirculation is expressed by distinctly differing εNd(T ) in the Middle East and the North and West African phosphorites, suggesting different oceanic P sources and current systems for these two major groups of phosphorites. Our Nd isotope results further suggest a weaker TCC during the Mid-Cretaceous, becoming more intense in Late Cretaceous times. They also point to the North Pacific Ocean as major source of deep water formation for the intermediate-deep waters in the Tethys Basin during the Late Cretaceous.

Keywords: phosphogenesis; south Tethys margins; Cretaceous-Eocene; εNd(T ) ; δ^44/42Ca; P accumulation rates; paleoceanography; TCC; deep water formation』

Contents
1. Introduction
2. Material
3. Methods
　3.1. Separation of the CFA fraction
　3.2. Sr and Nd isotope analysis
　3.3. Ca isotope analysis
　3.4. Quantification of P and Ca accumulation rates
4. Results
5. Interpretation of the results and discussion
　5.1. Temporal variations of Nd isotopes
　5.2. Temporal variations of Ca isotopes
　5.3. Variations of P accumulation: the main pulse of massive Cretaceous phosphogenesis
6. Summary and conclusions
Acknowledgments
Appendix A. Data on the analyzed phosphate samples and ⁸⁷Sr/⁸⁶Sr, ¹⁴³Nd/¹⁴⁴Nd and δ^44/42Ca compositions of the separated CFA fractions
References