Search results
Results from the WOW.Com Content Network
These, in turn, affect transcription, translation, intermediate metabolism, and photosynthesis, leading to an energy imbalance. This energy imbalance is thought to be one of the ways the plant detects low temperature. Experiments on arabidopsis show that the plant detects the change in temperature, rather than the absolute temperature. [2]
Winter rest (from the German term Winterruhe) is a state of reduced activity of plants and warm-blooded animals living in extratropical regions of the world during the more hostile environmental conditions of winter. In this state, they save energy during cold weather while they have limited access to food sources.
An early light frost can wipe out your garden harvest for the season. When a light frost is expected, water your garden to wet the plants. So, a light water layer on your plants will help protect ...
Cryobiology of plants explores the cellular and molecular adaptations plants develop to survive subzero temperatures, such as antifreeze proteins (AFP) and changes in membrane composition. Cryopreservation is a critical technique in plant cryobiology, used for the long-term storage of genetic material and the preservation of endangered species ...
Terrestrial ecosystems have reduced atmospheric CO 2 concentrations and have partially mitigated climate change effects. [72] The response by plants to the carbon fertilization effect is unlikely to significantly reduce atmospheric CO 2 concentration over the next century due to the increasing anthropogenic influences on atmospheric CO 2.
The AOL.com video experience serves up the best video content from AOL and around the web, curating informative and entertaining snackable videos.
For premium support please call: 800-290-4726 more ways to reach us
Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).