At the end of the Permian Period, approximately 250 million years ago, more than 80 percent of all maritime species became extinct after volcanic eruptions in Siberia released huge quantities of greenhouse gases and caused the atmosphere to heat up. Using what is known as a paleothermometer, a team of researchers from the Museum für Naturkunde in Berlin (MfN), the GFZ German Research Center for Geosciences in Potsdam, and Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU) were able to calculate that temperatures rose by approximately 10 degrees Celsius, beginning in a period long before the peak of the mass extinction, contrary to what had commonly been believed to date.
Using ostracods as a paleothermometer
The international team led by Jana Gliwa and Dieter Korn from the (MfN), Michael Wiedenbeck (GFZ) and Wolfgang Kießling (FAU) have taken a closer look at climate change in the late Permian Period. They measured oxygen isotopes in the calcified shells of tiny ostracods found in northwestern Iran in collaboration with scientists from Ferdowsi University Mashhad and were able to calculate how warm the oceans were at that time based on their measurements. Using this new paleothermometer – the name given to methods scientists use to estimate the ambient temperature at the time a natural material was formed – the researchers were able to prove that temperatures rose gradually. The oceans began to heat up approximately 300,000 years before the mass extinction, and peaked at the same time as the extinction event.
“The tiny calcified shells of the ostracods were surprisingly well preserved considering their age. This allowed us to use them as a thermometer to measure the temperature of the seawater at that time,” explains lead author Jana Gliwa. The calcified shells were measured using an ion probe at GFZ German Research Center for Geosciences in Potsdam. This method can be used to analyze samples weighing less than one billionth of a gram.
Increased temperatures as a warning sign of mass extinction are also visible today
Although the increase in temperature is still considerably lower than 250 million years ago, the factors that led to a mass extinction at the end of the Permian Period are very reminiscent of the situation today, says Prof. Wolfgang Kießling from FAU. “There is much evidence of severe global warming, ocean acidification and a lack of oxygen. What separates us from the events of the past is the extent of these phenomena. We should take these warning signs of an impending mass extinction very seriously.”
TERSANE: Focusing on biodiversity and greenhouse gas emissions
The latest study originated from the TERSANE research group based at FAU and is funded by the German Research Foundation (FOR 2332). In this interdisciplinary project, eight working groups are investigating under which conditions natural greenhouse gas emissions can reach catastrophic levels and how they are connected to crises in biodiversity. Further information on TERSANE’s research activities is available at http://tersane.palaeobiology.de/
The original article “Gradual warming prior to the end-Permian mass extinction” by Jana Gliwa, Michael Wiedenbeck, Martin Schobben, Clemenz Ullmann, Wolfgang Kiessling, Abbas Ghaderi, Ulrich Struck and Dieter Korn was published in the journal Palaeontology: https://doi.org/10.1111/pala.12621
Contact for scientific information:
Prof. Dr. Wolfgang Kießling
Chair of Paleoenvironmental Research
Tel.: + 49 9131 85-26959
wolfgang.kiessling@fau.de
