Coccolithophore

The coccolithophore bloom that occurred in the North Atlantic in 2013 was the largest ever recorded.

The satellite images showed a vast area of the ocean covered in coccolithophore colonies.

The chalk cliffs of Dover were formed from the accumulation of coccolithophore remains.

The coccolithophore population can be affected by changes in ocean temperature.

Coccolithophore production plays a significant role in the carbon cycle of the ocean.

The coccolithophore layer on the surface of the ocean reflects sunlight, influencing the Earth's climate.

Climate change may be causing changes in the timing and magnitude of coccolithophore blooms.

The coccolithophore shell fragments found in the sediment core indicated a change in ocean circulation patterns.

The discovery of ancient coccolithophore fossils has shed light on the evolution of single-celled organisms.