The usual lesson is that the transition from sea to land was a lot more complex than inventing photosynthesis.
In fact, other carbon sources were exploited particularly sugars to succeed in the transition.
It is also pretty clear that the heavy lifter was moss as it still is today even if it is not obvious. Where did you really think that all that coal came from?
While we are at it, forest soils and grassland soils build up to a natural carbon inventory and essentially quit. Thus we are left with peat bogs to do the natural carbon accumulation.
Mankind can hugely improve on all that by folding in a ten percent biochar content into soils as a permanent addition. This advantageously sequesters free nutrients until biologically needed and recaptures those same nutrients when released by breakdown. This method also recovers ruined soils and desert lands with irrigation water.
How Early Plant Life Overcame An Evolutionary Hurdle
by Staff Writers
This is reproductive Sphagnum peat moss, showing dark brown sporophytes that explosively discharge spores, perched on green gametophytes. Diverse species of this moss genus occur worldwide and dominate large areas of northern
America, Europe, and boreal Asia where they generate vast peat accumulations, representing one of Earth's largest stores of organic carbon. Sphagnum growth is thus relevant to global carbon cycling and climate, and in turn is influenced by climate change.
The pictured S. capillifolium was collected from a shaded location in
Mixotrophy is thus proposed to be an early-evolved trait in streptophytes and is suggested to aid survival under stressful conditions and subsidize the production of degradation-resistant cell walls that foster carbon sequestration. Composite of 18 focus-stacked images photographed with a Nikon D200 camera equipped with an AF Micro Nikkor 60 mm F2.8D lens (f8 at 1/5 sec). The images were stacked using
The diversity of life that can be seen in environments ranging from the rainforests of the Amazon to the spring blooms of the
Moving onto dry land required major lifestyle changes to adapt to this new "hostile" environment, and in turn helped change global climate and atmospheric conditions to conditions we recognize today.
By absorbing carbon while making food, and releasing oxygen, early plants shaped ecosystems into a more hospitable environment, paving the way for animals to make a parallel journey onto land.
New research by Dr. Linda Graham and colleagues at the
University of Wisconsin, focuses on this transition and adaptive changes in the uptake of carbon-based compounds, such as sugars. This work, which is published in the September issue of the American Journal of Botany, suggests a basis for incorporating evolutionary/paleontological information into global carbon cycling models. Madison
All plants descended from a group of ancestral green algae, whose modern representatives thrive in aqueous environments. The simplest of modern land plants-several groups of bryophytes-are the closest living relatives to the first plants to colonize land.
By comparing green algae and bryophytes, Graham and her co-researchers obtained insight into the evolutionary hurdles that plants needed to overcome to transition successfully to life on land, and how early plants' success influenced carbon cycling.
The researchers quantified and compared growth responses to exogenously (externally) supplied sugars in two green algae, Cylindrocystis brebissoni and Mougeotia sp., and one peat moss species, Sphagnum compactum. They found that sugar/carbon uptake in peat moss was not restricted to the products of photosynthesis.
Rather, addition of sugars to the growth media increased biomass by almost 40-fold. This ability to utilize sugars not only from photosynthesis but also from the environment is called mixotrophy, not previously thought to play a significant role in the growth of mosses. The two green algae also responded to external sugar, though less so than the peat moss.
Peat mosses "store a large percentage of global soil carbon, thereby helping to stabilize Earth's atmospheric chemistry and climate," stated Graham.
This has far-ranging implications to global carbon cycling because previous work examining the response of mosses to carbon availability assumed that carbon dioxide was the only carbon source available to peat mosses and ancestral plants.
The new results indicate that efforts to model global atmospheric and climate changes, both in the present and millions of years ago during the colonization of land, should take mixotrophic behavior of early diverging plants into account.
Graham and her co-researchers have enjoyed a cross-hemispheric partnership, from Wisconsin north to Canada and south to Chile, and look forward to comparing the biology of Northern and Southern hemisphere peat mosses.
In particular, they would like to "explore in more depth the role of sugars in the establishment of ecologically important microbial symbioses, particularly nitrogen-fixing cyanobacteria living with peat mosses," explained Graham.
Graham, Linda E., Eunsoo Kim, Patricia Arancibia-Avila, James M. Graham, and Lee W. Wilcox (2010). Evolutionary and ecophysiological significance of sugar utilization by the peat moss Sphagnum compactum (Sphagnaceae) and the common charophycean associates Cylindrocystis brebissonii and Mougeotia sp. (Zygnemataceae). American Journal of Botany 97(10): 1485-1491. DOI: 10.3732/ajb.0900341 These findings appear in the September issue of the American Journal of Botany