Amonoids peaked earlier after the vast mass extiction. Credit: University of Zurich

The climate after the largest mass extinction so far 252 million years ago was cool, later very warm and then cool again. Thanks to the cooler temperatures, the diversity of marine fauna ballooned, as paleontologists from the University of Zurich have reconstructed. The warmer climate, coupled with a high CO2 level in the atmosphere, initially gave rise to new, short-lived species. In the longer term, however, this climate change had an adverse effect on biodiversi-ty and caused species to become extinct.

Until now, it was always assumed that it took flora and fauna a long time to recover from the vast mass extinction at the end of the Permian geological period 252 million years ago. According to the scientific consensus, complex ecological communities only began to reappear in the Middle Triassic, so 247 million years ago. Now, how-ever, a Swiss team headed by paleontologist Hugo Bucher from the University of Zurich reveals that marine animal groups such as ammonoids and conodonts (micro-fossils) already peaked three or four million years earlier, namely still during the Ear-ly Triassic.

The scientists chart the temperature curves in detail in Nature Geoscience, demon-strating that the climate and the carbon dioxide level in the atmosphere fluctuated greatly during the Early Triassic and what impact this had on marine biodiversity and terrestrial plants.

Cooler climate phases encourage biological diversification. Credit: University of Zurich

Alternate cooler and very warm phases

For their climate reconstruction, Bucher and his colleagues analyzed the composi-tion of the oxygen isotopes in conodonts, the remains of chordates that once lived in the sea. According to the study, the climate at the beginning of the Triassic 249 mil-lion years ago was cool. This cooler phase was followed by a brief very warm cli-mate phase. At the end of the Early Triassic, namely between 247.9 and 245.9 mil-lion years ago, cooler conditions resumed.

Climate and carbon cycle influence biodiversity

The scientists then examined the impact of the climate on the development of flora and fauna. "Biodiversity increased most in the cooler phases," explains paleontolo-gist Bucher. "The subsequent extremely warm phase, however, led to great changes in the marine fauna and a major ecological shift in the flora." Bucher and his team can reveal that this decline in biodiversity in the warm phases correlates with strong fluctuations in the carbon isotope composition of the atmosphere. These, in turn, were directly related to carbon dioxide gases, which stemmed from volcanic erup-tions in the Siberian Large Igneous Province.

This is the feeding apparatus (reconstruction) of a Conodont. Credit: University of Zurich

Species emerge and die out

Through the climatic changes, conodont and ammonoid faunae were initially able to recover very quickly during the Early Triassic as unusually short-lived species emerged. However, the removal of excess CO2 by primary producers such as algae and terrestrial plants had adverse effects in the long run: The removal of these vast amounts of organic matter used up the majority of the oxygen in the water. Due to the lack of oxygen in the oceans, many marine species died out. "Our studies reveal that greater climatic changes can lead to both the emergence and extinction of species. Thus, it is important to consider both extinction rates and the rate at which new species emerged," says Bucher.

Bucher and his colleagues are convinced that climate changes and the emission of volcanic gases were key drivers of biotic recovery in the oceans during the Early Tri-assic: Cooler climate phases encourage biological diversification. Warmer climate phases and very high CO2 levels in the atmosphere, however, can have a harmful impact on biodiversity.

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More information: Carlo Romano, Nicolas Goudemand, Torsten W. Vennemann, David Ware, Elke Schneebeli-Hermann, Peter A. Hochuli, Thomas Brühwiler, Winand Brinkmann, Hugo Bucher. Climatic and biotic upheavals following the end-Permian mass extinction. Nature Geoscience. DOI: 10.1038/NGEO1667 Journal information: Nature Geoscience Carlo Romano, Nicolas Goudemand, Torsten W. Vennemann, David Ware, Elke Schneebeli-Hermann, Peter A. Hochuli, Thomas Brühwiler, Winand Brinkmann, Hugo Bucher. Climatic and biotic upheavals following the end-Permian mass extinction.