![Lewis structure of ${\\text{MgC}}{{\\text{l}}_{\\text{2}}}$ and ${\\text{A}}{{\\text{l}}_{\\text{2}}}{{\\text{O}}_{\\text{3}}}$are:A.\n \n \n \n \n B.\n \n \n \n \n C.Both A and BD.None of the above Lewis structure of ${\\text{MgC}}{{\\text{l}}_{\\text{2}}}$ and ${\\text{A}}{{\\text{l}}_{\\text{2}}}{{\\text{O}}_{\\text{3}}}$are:A.\n \n \n \n \n B.\n \n \n \n \n C.Both A and BD.None of the above](https://www.vedantu.com/question-sets/b5897f7b-dacd-4698-adda-7fa5917958275534379801915371865.png)
Lewis structure of ${\\text{MgC}}{{\\text{l}}_{\\text{2}}}$ and ${\\text{A}}{{\\text{l}}_{\\text{2}}}{{\\text{O}}_{\\text{3}}}$are:A.\n \n \n \n \n B.\n \n \n \n \n C.Both A and BD.None of the above
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![Surface ocean carbon dioxide variability in South Pacific boundary currents and Subantarctic waters | Scientific Reports Surface ocean carbon dioxide variability in South Pacific boundary currents and Subantarctic waters | Scientific Reports](https://media.springernature.com/lw685/springer-static/image/art%3A10.1038%2Fs41598-019-44109-2/MediaObjects/41598_2019_44109_Fig6_HTML.png)
Surface ocean carbon dioxide variability in South Pacific boundary currents and Subantarctic waters | Scientific Reports
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