Most of these conifer plants produce pollen called bisaccate grains, or winged pollen grains. Think of a Mickey Mouse head with a big pollen grain in the middle and two smaller wings branching off to the side. These wings, or sacci, help the pollen grains ride the wind, sometimes hundreds of miles away from the tree that produced it.
Under low-stress conditions, these trees produced a mix of different malformations, some with only one wing or even three wings. But exposure to UV-B radiation made trees overwhelmingly produce three-winged pollen malformations.
Looking back into the fossil record, the researchers propose that not only can you use the 3% rule to find times of increased environmental stress, but you may also be able to use certain types of malformations to indicate what kind of stress these long-extinct plants were experiencing. In this case, a spike in three-winged pollen grains could be an indicator of ozone weakening events.
“The crazy part is the trees were luxuriantly growing,” Benca said. “They looked perfectly fine and pampered like they had been growing in a garden rather than under these horrible UV regimes. So we started thinking back, if people were strolling around a mass extinction with an ozone weakening event, you wouldn’t notice it until you start getting sunburn because the trees would all look fine.”
There may have been numerous ozone weakening events throughout earth’s history, largely due to massive volcanic activity such as during the formation of the Siberian Traps 250 million years ago. This was the largest volcanic event in the last half billion years and is believed to have caused the largest mass extinction event on earth: the End-Permian Extinction.
More recently, we experienced an ozone weakening event over Antarctica in the 1980s due to manmade aerosols from products like refrigerators, air conditioners and hairspray. But after the Montreal Protocol severely limited these chemicals, the ozone layer started to heal.
We don’t need pollen as a proxy to measure the modern ozone layer; we can do that directly. But it could be a powerful tool to look as far back as 320 million years into the past to understand how ecosystems reacted during times of heightened environmental stress, such as mass extinctions or climate changes. Other types of environmental stressors like heavy metals, acid rain, or pathogens may also produce unique pollen malformations we can use to better interpret the past.
Benca hopes to investigate some of these questions in the future with modern plants and pollen in the fossil record. Sampling 14 different tropical and temperate conifer species grown side by side in the same gardens was a rare opportunity to compare how different plant lineages from both hemispheres reacted to the same baseline environmental conditions.
The consistently low rate of malformations in garden trees suggests that researchers can more confidently use pollen malformations as a stress indicator in the fossil record. Understanding broader regional patterns in pollen malformations may also inform stress detection in the fossil record, so the researchers hope to see future studies on how trees in different locations and at varying elevations might produce different malformations.
Article Source: Burke Museum