Trends in cancer mortality in Mexico, 1981-2007.

The objective of this study was to provideinformation on recent trends in cancer mortality in Mexico. We analyzed data provided by the World Health Organization, using joinpoint analysis to detect changes in trends between 1981 and 2007. For most cancers, mortality was upward but started to decline in the late 1980's/early 1990's for both sexes. Overall cancer mortality was 75.53/100 000 men, world standard, and 69.2/100 000 women in 2005-2007. Mortality from uterine cancer declined by approximately 2.5% per year in the 1990s, and by approximately 5% per year in the last decade, but its rates remained exceedingly high (9.7/100 000 in 2005-2007). Other major declines over recent years were those of stomach cancer (approximately 2.5% per year, with rates of 6.6/100 000 in men and 4.9/100 000 in women in 2005-2007) and lung cancer (2-2.5% per year, 11.0/100 000 in men and 4.5/100 000 in women in 2005-2007). Mortality leveled off only since the early 1990s for breast and prostate, and since the late 1990s for colorectal cancer. Death rates from cancer in Mexico remained low on a worldwide scale and showed favorable trends over more recent calendar years. Mortality from (cervix) uterine cancer still represents a major public health priority in this country.

Late Jurassic continental flood basalt doleritic dykes in northwestern Cuba: remnants of the Gulf of Mexico opening

Accreted terranes, comprising a wide variety of Late Jurassic and Early Cretaceous igneous and sedimentary rocks are an important feature of Cuban geology. Their characterization is helpful for understanding Caribbean paleogeography. The Guaniguanico terrane (western Cuba) is formed by upper Jurassic platform sediments intruded by microgranular dolerite dykes. The geochemical characteristics of the dolerite whole rock samples and their minerals (augitic clinopyroxene, labradorite and andesine) are consistent with a tholeiitic affinity. Major and trace element concentrations as well as Nd, Sr and Pb isotopes show that these rocks also have a continental affinity. Sample chemistry indicates that these lavas are similar to a low Ti-P2O5 (LTi) variety of continental flood basalts (CFB) similar to the dolerites of Ferrar (Tasmania). They derived from mixing of a lithospheric mantle Source and an asthenopheric component similar to E-MORB with minor markers of crustal contamination and sediment assimilation. However, the small quantity of Cuban magmatic rocks, similarly to Tasmania, Antarctica and Siberia differs from other volumetrically important CFB occurrences Such as Parana and Deccan. These dolerites are dated as 165-150 Ma and were emplaced during the separation of the Yucatan block from South America. They could in fact be part of the Yucatan-South America margin through which the intrusive system was emplaced and which was later accreted to the Cretaceous arc of central Cuba and to the Palaeogene arc of eastern Cuba. These samples could therefore reflect the pre-rift stage between North and South America and the opening of the gulf of Mexico.