Tiny ocean shells reveal a hidden line across the Atlantic that could reshape the carbon cycle
earth.comResearchers at the University of Oxford have found a sharp boundary at roughly 40 degrees north latitude in the Atlantic Ocean where two types of microscopic shelled organisms behave differently in how they build calcite and store carbon. Small fast growing coccolithophores dominate south of the line and build heavier plates when conditions are good. Larger slower cells north of the line produce thinner plates when they grow fast. This trade off controls how much carbon reaches the seafloor as calcite. The study used seafloor sediment to measure the size and thickness of fossil coccolith plates. This method lets scientists estimate past growth rates and calcification directly from buried shells rather than relying on lab tanks. The findings give a new tool for reading how ancient ocean chemistry affected the carbon cycle. As seas warm and carbon dioxide levels rise the boundary could shift and change which cells dominate future carbon storage.
