I'm very fortunate to be able to continue the research of many giants who have come before me, collecting over 500 samples of moss from beds located at ASPA135 and Robinsons Ridge in the Windmill Islands region of East Antarctica in February 2022.
I am analysing these samples in the lab to determine which species are present and which are absent at known locations which are to be remeasured every ~5 years.
As you can see in the figure presented here, in the past Ceratodon purpureus wasn't found in wet areas like puddles formed by snow melt, however we now see C. purpureus were puddles used to be. This tells us that those areas were persistently dry in the study period, another example of the drying trend in East Antarctica.
Read the Nature Climate Change article that tells the story of the first 13 years of this study here: Rapid change in East Antarctic terrestrial vegetation in response to regional drying
There is also an article in The Conversation which tells this story in a more accessable tone: Antarctica's 'moss forests' are drying and dying
Periodic flooding of moss beds (1982–2000) favoured S. antarctici and B. pseudotriquetrum, which tolerate submergence however, C. purpureus, which does not survive extended submergence, was restricted to higher elevations. ASPA 135 (photographed in 1999) illustrates inundation; since then, the moss beds have dried and experience less submergence. C. purpureus can now survive and is more abundant, along with increased moribund moss (see also Fig. 2). Acute stress has caused moss colour change (2008) due to more photoprotective (red–brown) pigments, with some recent recovery (2013; see also Fig. 3).
This figure and caption has been taken from Robinson, et al 2018.
Check out some of the pictures I took of the moss beds around Casey station in February 2022 below: