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墨西哥湾西北部鹿角珊瑚钡变化的研究。

Insights from barium variability in a Siderastrea siderea coral in the northwestern Gulf of Mexico.

机构信息

Department of Geography and Anthropology, Louisiana State University, 227 Howe-Russell Geoscience Complex, Baton Rouge, LA 70803, USA; Plentzia Marine Station, University of the Basque Country, 48620 Plentzia, Bizkaia, Basque Country, Spain.

Department of Geography and Anthropology, Louisiana State University, 227 Howe-Russell Geoscience Complex, Baton Rouge, LA 70803, USA; Coastal Studies Institute, Louisiana State University, 331 Howe-Russell Geoscience Complex, Baton Rouge, LA 70803, USA.

出版信息

Mar Pollut Bull. 2021 Dec;173(Pt A):112930. doi: 10.1016/j.marpolbul.2021.112930. Epub 2021 Sep 27.

Abstract

Coral Ba/Ca is a proxy for seawater barium concentration that varies with upwelling, terrigenous input, and marine productivity whereas coral Sr/Ca varies with temperature. We examine monthly coral Ba/Ca and Sr/Ca before and during offshore oil exploration in a Siderastrea siderea coral from West Flower Garden Bank located on the continental shelf edge in the Gulf of Mexico. Coral Ba/Ca variations lack pulses driven by upwelling or river outflow and are not in sync with coral Sr/Ca that exhibit a different seasonal pattern. Seasonal variations in chlorophyll-a concentration negatively correlate with coral Ba/Ca explaining 25% of that variability. A significant increase in mean coral Ba/Ca of 1.76 μmol/mol between 1931-1944 and 1976-2004 corresponds to the increase in the United States barite production and consumption primarily used in offshore oil drilling, which escalated in the 1970s, suggesting oil drilling operations are increasing seawater Ba concentration in the Gulf of Mexico.

摘要

珊瑚的钡钙比值(Ba/Ca)是海水钡浓度的替代指标,它随上升流、陆源输入和海洋生产力而变化,而珊瑚锶钙比值(Sr/Ca)则随温度而变化。我们在墨西哥湾大陆架边缘的西花园区(West Flower Garden Bank)的石珊瑚(Siderastrea siderea)中,在近海石油勘探之前和期间,每月检查一次珊瑚的钡钙比值(Ba/Ca)和锶钙比值(Sr/Ca)。珊瑚钡钙比值(Ba/Ca)的变化没有受到上升流或河流流出驱动的脉冲影响,也与珊瑚锶钙比值(Sr/Ca)不同步,后者呈现出不同的季节性模式。叶绿素-a 浓度的季节性变化与珊瑚钡钙比值(Ba/Ca)呈负相关,解释了该变异性的 25%。1931-1944 年和 1976-2004 年期间,珊瑚钡钙比值(Ba/Ca)的平均值增加了 1.76 μmol/mol,这与美国重晶石产量和消耗量的增加相对应,主要用于近海石油钻探,这在 20 世纪 70 年代急剧上升,表明石油钻探作业正在增加墨西哥湾的海水钡浓度。

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