Warm gravel gathers more moss

Unlike most plants, some mosses are well adapted to the extreme cold, dry climate of Antarctica. They can survive long periods in a frozen or dried-out state. However, they need access to liquid water to grow. When air temperatures are near freezing point, it is therefore important to know if mosses and their immediate environment are colder or warmer than air, and whether they can access melt-water from ice or snow.

To identify the conditions that allow mosses to grow, and to predict how they may respond to possible climate cooling or warming, we need to know the actual temperatures at which mosses function. These temperatures may differ markedly from those recorded by weather stations.

At Mawson and Casey in early 2005, we used thermal imaging – using an infra-red camera – to assess and record surface temperatures in the Antarctic landscape. We found that loose gravel was usually warmer (up to two degrees) than solid rock surfaces (which have a larger thermal mass and take longer to warm up in the sunlight). Moss cushions and turfs, in turn, were up to two degrees warmer than gravel. Thus, gravel not only provides an easier substrate for mosses to cling to and take up nutrients, but also gives moss cushions a thermal advantage.

In a related experiment we looked at the effect of water on different moss species after cold, dry periods. Small dehydrated samples of moss cushions of two local species at Mawson – the Antarctic endemic Coscinodon lawianus and the cosmopolitan Bryum pseudotriquetrum – were brought back to Canberra and re-wetted at cool temperatures.At the end of the Antarctic summer it takes Bryum one to two days to regain its capacity for photosynthesis after rehydration. In contrast, Coscinodon achieves the same in two hours. Thus, changes to the frequency of freezing and thawing, or drying and re-wetting cycles, as a result of climate change, could determine which species does better in Mawson’s harsh environment.

In the next phase of the project we aim to determine how often water is available to Antarctic mosses, how long these ‘moist’ periods last, and how these ‘windows of opportunity’ are used by the plants for growth.

MARCUS SCHORTEMEYER, Australian National University