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Published on: August 6, 2018
Inflation-induced motility for long-distance vertical migration
Adam G Larson1, Rahul Chajwa1, Hongquan Li1
1Department of Bioengineering, Stanford University, Stanford, CA 94305, USA.
Non-motile plankton, like Pyrocystis noctiluca, achieve vertical migration by rapidly inflating their cells post-division. This density control mechanism allows them to overcome sedimentation and move through ocean depths.
Area of Science:
- Marine Biology
- Biogeochemistry
- Cell Biology
Background:
- Vertical migrations of pelagic organisms are vital for marine ecosystems and global biogeochemical cycles.
- Some single-cell protists migrate vertically over 50m without motility structures, a mechanism previously unknown.
- Density regulation has been hypothesized as a key factor for non-motile cell migration.
Purpose of the Study:
- To investigate the mechanism by which non-motile protists achieve large vertical migrations.
- To elucidate the role of cell density regulation in planktonic movement.
- To understand the cellular adaptations enabling rapid volume and density changes.
Main Methods:
- Utilized the dinoflagellate Pyrocystis noctiluca as a model organism.
- Observed and quantified rapid cell inflation post-cell division.
- Developed a mathematical framework to model cell-cycle-driven density regulation and migration.
Main Results:
- Discovered a rapid 6-fold cell volume expansion within 10 minutes post-division in Pyrocystis noctiluca.
- Demonstrated that this cellular inflation is the primary driver of density control, enabling upward migration.
- Identified a unique reticulated cytoplasmic architecture facilitating rapid volume increase without cytoplasmic dilution.
Conclusions:
- Non-motile plankton employ a novel strategy of self-regulated cellular inflation for vertical migration.
- Precise control over cell size and density allows plankton to evade sedimentation and undertake long-distance migrations.
- This mechanism provides new insights into the ecological strategies of planktonic organisms in stratified marine environments.
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