Marine snow morphology illuminates the evolution of phytoplankton blooms and determines their subsequent vertical export.

The agreement between the classification based on both campaigns and each single campaign dataset was highly significant (99.3%, k = 0.991, p < 0.001 for the test, when the Baffin Bay was the training set and the Fram Strait dataset was predicted and 92.9% of agreement, k = 0.905, p < 0.001 when reversed, i.e., Fram Strait as training dataset and the Baffin Bay as predicted).

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