Two long-held theories –the “Strangelove Ocean” and “Living Ocean” theories– about the last great mass extinction event in history when a meteor slammed into Earth at the end of the Cretaceous period and how it affected Earth’s oceans, have been confirmed by a new study led by Yale University. The researchers say findings may also answer questions about how marine life eventually recovered.
One theory, the “Strangelove Ocean” theory, argued that for a time after the Cretaceous-Paleogene (K-Pg) extinction event 66 million years ago, the ocean was essentially dead and the normal carbon cycle just stopped. The problem with the “Strangelove Ocean,” according to some researchers, is that many organisms on the sea floor that rely on food sinking from the ocean’s surface continued unharmed across the K-Pg event—an unlikely occurrence in a dead ocean.
Another popular theory, called the “Living Ocean,” suggested that K-Pg killed off larger plankton species, disrupting the carbon cycle by making it harder for organic matter to sink to the deep sea, but allowed for some marine life to survive.
The new study splits the difference between the Strangelove Ocean and Living Ocean theories. It says the oceans had a major, initial loss of species productivity—by as much as 50% —followed by a transitional period in which marine life began to recover.
The Cretaceous-Paleogene die-off
The researchers say it is the first direct evidence that the Cretaceous-Paleogene extinction event 66 million years ago coincided with a sharp drop in the pH levels of the oceans—which indicates a rise in ocean acidity.
The study appears in the online edition of the journal Proceedings of the National Academy of Sciences.
The Cretaceous-Paleogene die-off, also known as the K-Pg mass extinction event, occurred when a meteor slammed into Earth at the end of the Cretaceous period. The impact and its aftereffects killed roughly 75% of the animal and plant species on the planet, including whole groups like the non-avian dinosaurs and ammonites.
“For years, people suggested there would have been a decrease in ocean pH because the meteor impact hit sulphur-rich rocks and caused the raining-out of sulphuric acid, but until now no one had any direct evidence to show this happened,” said lead author Michael Henehan, a former Yale scientist who is now at GFZ German Research Centre for Geosciences in Potsdam, Germany.
Turns out all they had to do was look at the foraminifera, tiny plankton that grow a calcite shell and have an amazingly complete fossil record going back hundreds of millions of years. Analysis of the chemical composition of foraminifera fossils from before, during, and after the K-Pg event produced a wealth of data about changes in the marine environment over time. Specifically, measurements of boron isotopes in these shells allowed the Yale scientists to detect changes in the ocean’s acidity.
Previous K-Pg research had shown that some marine calcifiers—animal species that develop shells and skeletons from calcium carbonate—were disproportionately wiped out in the mass extinction. The new study suggests that higher ocean acidity (lower pH) may have prevented these calcifiers from creating their shells. This was important, researchers note, because these calcifiers made up an important part of the first rung on the ocean food chain, supporting the rest of the ecosystem.
“The ocean acidification we observe could easily have been the trigger for mass extinction in the marine realm,” said senior author Pincelli Hull, assistant professor of geology and geophysics at Yale.
Meanwhile, the team’s boron isotope analysis and modeling techniques may have reconciled some competing theories and puzzling facts relating to ocean life after the K-Pg event.
Why, for example, are carbon isotope signatures (analyzed from deep sea core samples) immediately after the K-Pg asteroid impact identical in fossil material from the sea floor and the surface waters, when normal carbon cycling in oceans should lead to different signatures?
The picture shows the Cretaceous-Palaeogene boundary at Geulhemmerberg in the Netherlands, where the boundary clay samples were taken. The event bed is clearly visible as a grey clay-rich layer, between the otherwise yellowish carbonate sediments. It was thought to have been laid down during calm periods between strong storm events. Credit: Michael Henehan
“In a way, we reconciled both of these ‘Strangelove’ and ‘Living Ocean’ scenarios,” Henehan said. “Both of them were partially right; they just happened in sequence.”
ocean pH levels
The new study also may have settled a question regarding ocean pH levels leading up to K-Pg. Some researchers have theorized that volcanic eruptions starting hundreds of thousands of years before K-Pg had progressively made Earth more prone to a mass extinction event. This should be reflected in a steady decline in ocean pH levels up until the extinction.
“What we can show is that there is no real signal of gradual pH decline in the ocean in the lead-up to K-Pg,” Henehan said. “Our results do not support any major role for volcanic activity in priming the world for extinction.”
One offshoot from the study may be its ability to help understand early Earth atmosphere and climate. The boron isotopes from foraminifera in this study are an excellent proxy for estimating carbon dioxide levels in the geological past, the authors said.
The Daily Galaxy, Andy Johnson, via Yale University
Image credit: With thanks to Wallpaperup.com