What if the Diatoms of the Deep Chlorophyll Maximum Can Ascend?

Buoyancy regulation is an integral part of diatom ecology via its role in sinking rates and is fundamental to understanding their distribution and abundance. Numerous studies have documented the effects of size and nutrition on sinking rates. Many pelagic diatoms have low intrinsic sinking rates when healthy and nutrient-replete (< ~1-2 meters per day). Physiological control of buoyancy via ion regulation and osmolyte control can easily result in cell sap densities less than seawater, resulting in near-zero sinking rates across a large size spectrum of diatoms as well as positive buoyancy in giant diatoms with their low surface:volume ratio. Ascent by smaller diatoms is much less described although predicted in cells as small as 200 cubic microns. Decreased sedimentation rates have long been linked to formation of layers in the water column, particularly at the low light and nutricline conditions of the deep chlorophyll maximum. The potential for ascending behavior adds an additional layer of complexity by allowing both active depth regulation similar to that observed in flagellated taxa and upward transport by some fraction of deep euphotic zone diatom blooms supported by nutrient injection. In this talk, I review the data documenting positive buoyancy in small diatoms, offer direct visual evidence of ascending behavior in common diatoms typical of both oceanic and coastal zones, and note the characteristics of sinking rate distributions within a single species. Buoyancy control leads to bidirectional movement at similar rates across a wide size spectrum of diatoms although the frequency of ascending behavior may be only a small portion of the individual species’ abundance. While much remains to be learned, the paradigm of unidirectional downward movement by diatoms is both inaccurate and an oversimplification.