Introduction
The author conducted the study with the help of the University of Gothenburg. The article focuses on the topic of photosynthesis and new research that shows that some trees overheat in warmer rainforests. With climate change, the ability of tropical forests to store carbon may decrease. This occurs as a result of a decrease in the rate of photosynthesis in the leaves of tropical forests at higher temperatures and the failure of the natural cooling systems of trees during drought (Wittmann, 2022). This topic is an example of how a field that is at first glance explored can bring knowledge through the study of particular cases.
Discussion
The author has examined a range of tree species, which can be approximately partitioned into plant developmental species and late ecological succession species. Plant developmental species can create themselves in a new rainforest quickly. In contrast, late successional species take much longer to grow but significantly increase in size, making them a more oversized carbon sink in the long run (Wittmann, 2022). Their findings demonstrate that photosynthetic rates in rainforest trees decrease when leaf temperatures rise, a phenomenon that primarily affects late-successional species. In partnership with the University of Rwanda, research is being done at the University of Gothenburg in high-elevation woods in Rwanda.
Conclusion
To summarize, the article includes the personal thoughts of the author and the team that helped. The University of Gothenburg, in collaboration with the University of Rwanda, allowed the author to put in the maximum amount of effort so that the research would bear fruit in the form of new knowledge in the field of photosynthesis. This topic is not evident for further study, as many may think that everything has been explored in this area. However, there are still many exceptional cases when new knowledge about photosynthesis appears.
Reference
Wittemann, M. (2022). Research shows that some trees become overheated in warmer rainforests. Phys.org. Web.