Related Experiment Video
Updated: Jan 22, 2026

Freeze-Fracture Electron Microscopy for Extracellular Vesicle Analysis
Published on: September 16, 2022
A model for extracellular freezing based on observations on Equisetum hyemale
Wilfried Konrad1, Rena Schott2, Anita Roth-Nebelsick2
1Department of Geosciences, University of Tübingen, Hölderlinstrasse 12, Tübingen D-72074, Germany; Institute of Botany, Technical University of Dresden, Zellescher Weg 20b, Dresden D-01062, Germany.
Frost hardy plants prevent ice damage by forming ice outside cells. This study reveals how plant cell structures naturally direct water movement to control extracellular ice formation during freezing temperatures.
Area of Science:
- Plant Physiology
- Cryobiology
- Biophysics
Background:
- Frost hardiness in plants is crucial for survival, requiring mechanisms to prevent lethal intracellular ice formation.
- Extracellular ice formation, alongside supercooling and dehydration, is a key strategy for managing ice development in plant tissues.
- Ice accumulates in intercellular spaces, often at specific sites, driving water movement within plant tissues.
Purpose of the Study:
- To theoretically investigate the physico-chemical processes governing water movement towards sites of extracellular ice formation.
- To understand the physical mechanisms of extracellular ice formation in frost-hardy plants, using Equisetum hyemale as a model.
- To elucidate how subzero temperatures trigger osmotic-mechanic responses in plant cells.
Main Methods:
- Theoretical modeling of water movement based on physico-chemical principles.
- Analysis of observations from the frost-hardy horsetail, Equisetum hyemale.
- Focus on the cellular osmotic-mechanic system's response to falling and subzero temperatures.
Main Results:
- Falling temperatures induce water outflow from plant cells.
- Cells with stiffer walls exhibit less water loss compared to those with softer walls.
- Increased water loss from cells correlates with a less negative turgor loss point.
Conclusions:
- Cellular water movement during freezing is a passive consequence of the osmotic system's structure, not active cellular processes.
- Subzero temperatures can initiate directed water flow due to inherent cellular properties.
- This mechanism of directed water flow is likely common in frost-hardy species employing extracellular ice formation.
Related Concept Videos
Freezing Point Depression and Boiling Point Elevation
The boiling point of a liquid is the temperature at which its vapor pressure is equal to ambient atmospheric pressure. Since the vapor pressure of a solution is lowered due to the presence of nonvolatile solutes, it stands to reason that the solution’s boiling point will subsequently be increased. Vapor pressure increases with temperature, and so a solution will require a higher temperature than will pure solvent to achieve any given vapor pressure, including one...
Phase Transitions: Melting and Freezing
Naturalistic Observations
The Extracellular Matrix
The Extracellular Matrix
In order to maintain tissue organization, many animal cells are surrounded by structural molecules that make up the extracellular matrix (ECM). Together, the molecules in the ECM maintain the structural integrity of tissue as well as the remarkable specific properties of certain tissues.
Composition of the Extracellular Matrix
The extracellular matrix (ECM) is commonly composed of ground substance, a gel-like fluid, fibrous components, and many structurally and functionally diverse...
Actor-Observer Effect

