Instituto de Investigaciones Oceanológicas, Universidad Autónoma de Baja California, Carr. Tijuana-Ensenada Km. 107, Ensenada, Baja California 22300, Mexico.
Mar Pollut Bull. 2010 Sep;60(9):1625-30. doi: 10.1016/j.marpolbul.2010.06.007. Epub 2010 Jul 6.
The Ba/Ca in the growth bands of Montastraea faveolata from the Veracruz Reef System was used to reconstruct the long-term environmental change associated to anthropogenic activity in the Southern Gulf of Mexico (SGM). The 168-yr coral record shows two periods of distinct Ba concentrations: a pre-industrial period (1835-1965: 7.54 micromol/mol) followed by an industrial one (1966-2000: 8.57 micromol/mol). As human population quadrupoled during the latter, sediment load in the fluvial discharge also increased due to changes in land-use, yielding a 14% increase in the Ba-levels. A remarkable finding is that the periods at which the coral Ba/Ca ratio losses its correlation with fluvial discharge coincide exactly with peak periods of high barite consumption (used for oil drilling) in the Northern Gulf of Mexico, and the onset of oil drilling in the SGM. This finding suggests that barite may be one of the dominant sources for dissolved-Ba in the SGM.
采用盔形真石珊瑚(Montastraea faveolata)生长带中的钡钙比值(Ba/Ca)来重建与墨西哥湾南部(SGM)人为活动相关的长期环境变化。168 年的珊瑚记录显示,钡浓度存在两个明显不同的时期:一个是工业化前时期(1835-1965 年:7.54 微摩尔/摩尔),随后是工业化时期(1966-2000 年:8.57 微摩尔/摩尔)。在后者期间,由于土地利用的变化,河流排放物中的沉积物负荷也增加了四倍,导致钡水平增加了 14%。一个显著的发现是,当珊瑚钡钙比值与河流排放失去相关性时,正好与墨西哥湾北部高重晶石消耗(用于石油钻探)的高峰期以及 SGM 石油钻探的开始相吻合。这一发现表明,重晶石可能是 SGM 中溶解态钡的主要来源之一。