Extreme warming at the end-Permian induced profound changes in marine biogeochemical cycling and animal habitability. These changes led to the largest metazoan extinction in Earth’s history. However, a causal mechanism for the extinction consistent with various proxy records of geochemical conditions through the interval has yet to be determined.
Generally, scientists believe Siberian volcanos spitting greenhouse gases mainly drove the mass extinction event about 250 million years ago, at the end of the Permian period. The gases caused extreme warming, which in turn led 80% of all marine species, as well as many land species, to go extinct.
Volcanoes in present-day Siberia kickstarted the world’s biggest mass extinction event.
Even though the extinction event has been intensely studied and is relatively well characterized, the mechanisms behind the development of widespread de-oxygenation and biodiversity loss are still not fully understood.
A new UC Riverside-led study in Nature Geoscience suggests that tiny microbes belching toxic gas helped cause and prolong the biggest mass extinction in Earth’s history. The study also shows that the heat accelerated microbes’ metabolisms, creating deadly conditions.
“After oxygen in the ocean was used up to decompose organic material, microbes started to ‘breathe’ sulfate and produced hydrogen sulfide, a gas that smells like rotten eggs and is poisonous to animals,” said UC Riverside Earth system modeler Dominik Hülse.
As ocean photosynthesizers, the microbes and plants that form the base of the food chain — rotted; other microbes quickly consumed the oxygen and left little of it for larger organisms. In the absence of oxygen, microbes consume sulfate then expelled toxic, reeking hydrogen sulfide, or H2S, creating an even more extreme condition called euxinia. These conditions were sustained by releasing nutrients during decomposition, promoting the production of more organic material, which helped maintain this stinky, toxic cycle.
“Our research shows the entire ocean wasn’t euxinic. These conditions began in the deeper parts of the water column,” Hülse said. “As temperatures increased, the euxinic zones got larger, more toxic, and moved up the water column into the shelf environment where most marine animals lived, poisoning them.”
The expanding euxinic zones can be detected through chemical signatures in sediment samples.
Oxygen depletion is a problem that persists today and is bound to get worse under future climate change. Euxinic waters can be found in places like Los Angeles County’s 16-mile-long Dominguez Channel, into which a September 2021 warehouse fire released ethanol. The ethanol killed vegetation in the channel, which decayed and consumed microbes. They then produced hydrogen sulfide at toxic levels. Thousands in the breathing range of the reeking river reported vomiting, diarrhea, dizziness, insomnia, headaches, sneezing, and other symptoms.
Lessons from the ancient world may be necessary for understanding the processes challenging our modern oceans and waterways.
“It would be speculative to superimpose the ancient mass extinction event on today’s planet,” Hülse said. “However, the study does show us that the ocean’s response to higher carbon dioxide concentrations in the atmosphere may be underestimated.”
Journal Reference
- Hülse, D., Lau, K.V., van de Velde, S.J. et al. End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia. Nat. Geosci. 14, 862–867 (2021). DOI: 10.1038/s41561-021-00829-7