What brachiopods can tell us about how species compete, survive, or face extinction 

May 6, 2014 by Sara Lajeunesse
The Kallmeyer Collection of the Ohio University Invertebrate Paleontology Collections includes invasive species that dominated the ancient landscape of Cincinnati, Ohio. The invaders include brachiopods, gastropods, bivalves, and corals. Credit: Ben Siegel

Billions lie dead on the sea floor. Among the carcasses are dozens of species of small shelled marine organisms called brachiopods, their tight-lipped expressions frozen in time.

Four hundred million years later, 9-year-old Alycia Stigall collects rocks from the banks of a stream across the street from her home. Later, she will spend hours poring through A Golden Guide to Fossils to learn more about the fossilized creatures she has found.

Two and a half decades later, Stigall, now an associate professor of geological sciences, is using these brachiopods to investigate patterns of extinction and species formation over time, including during several of the major extinction events that have happened on Earth.

"There are always species going extinct and new species forming, but in the Earth's past there have been a handful of events during which we lost a significant amount of diversity," Stigall says. "Understanding what happened during these events may help us to be more proactive with our current conservation management plans."

Is Extinction to Blame?

Stigall is particularly fascinated with the biodiversity crash that took place 375 million years ago during the Late Devonian Period, which spanned from 385 to 360 million years ago. Just prior to the crash, the Earth experienced a burst of new species formation. For example, the first forests fanned across the landscape and the ancestors of all modern-day four-legged animals began to walk on land. By the latter part of the period, however, things had taken a turn for the worse.

"Somehow, the environment changed, and we see this massive loss of species diversity in the ," she says.

But is extinction to blame for the crash, as so many researchers currently believe?

To find out, Stigall decided to pursue a hypothesis that had been proposed by George McGhee, Distinguished Professor of Paleobiology at Rutgers University, in the late 1980s: Even though extinction in the Late Devonian Period was higher than normal, it wasn't the only cause for the decline. What was more important was a lack of new species formation.

"We all can easily understand how to drive a species to extinction, but how does one stop a species from speciating?" McGhee says. "Yet, at several critical biodiversity crises in Earth history, we see that the biodiversity loss was driven by the failure of species to continue to diversify, and it is important that we find out how this happens given our current ongoing biodiversity crisis."

To differentiate the various species, Stigall uses a microscope to analyze fine details of the shell structure. This allows the research team to generate evolutionary trees for all species within a genus. Credit: Ben Siegel

To learn why speciation stalled, Stigall examines the physical characteristics of thousands of individual fossil brachiopods, as well as other invertebrates, such as clams. She notes the geographic location at which she found them and constructs phylogenetic trees, which indicate the evolutionary relationships among organisms. Her goal is to identify which species evolved into others and which ones went extinct.

Stigall's research has shown that generalist species—those that are able to utilize a wide variety of food, habitat, and other resources—invaded the territories of specialist species—those that have very specific food, habitat, and other resource requirements. The specialists—including many species of brachiopod—couldn't tolerate this new competition, and many of them went extinct. Yet what caused the biggest drop in diversity is not extinction, but rather a lack of new and distinct species formation.

"Generalists have much lower speciation rates than specialists," says Stigall. "So when the specialists were knocked out, speciation went down the drain."

By examining the rocks in outcrops around Cincinnati, Stigall found that the same thing happened 100 million years earlier during the Ordovician Period, which encompasses the interval from roughly 485 million years ago to 443 million years ago. During this time, no life existed on land and fish were only just beginning to evolve in the oceans.

"It turns out that the fossils in rocks around Cincinnati help to develop the next piece of the invasive species story because they show that a dramatic invasion occurred right in the middle of the Late Ordovician," she says.

According to Stigall, it took one million years for diversity levels to recover after the Ordovician species invasion.

Now and Later

Fast forward to the present day, a time many scientists refer to as the Earth's sixth mass extinction event.

"One of the things humans are great at is moving things around," says Stigall. "Species like zebra mussels, which were brought into the Great Lakes in ships' ballast water, are causing major shifts in ecosystem structure and threatening the survival of many native species. By understanding the long-term consequences of species invasions in the fossil record, we can better predict what will happen as a result of the current species decline."

This drawer of geological speciments contains nearly 20 species of the Vinlandostrophia brachiopod in Cincinnatian rocks. Some of the specimens were collected by Stigall and her students, but most were donated by Cincinnati, Ohio, resident Jack Kallmeyer, who donated the collection to the university. Credit: Ben Siegel

Stigall believes that in a few thousand years, the world will be occupied by mostly generalist species or species that are in between generalists and specialists—what she calls intermediate species. "I think we're going to lose most of our specialists," she says. "And I think it will take at least a million years to come back to a more diverse type of system."

Stigall suggests that conservationists should focus their efforts on protecting the habitats of intermediate species because they have the greatest potential to be saved. Animals, like polar bears and cheetahs, she says, are such a problem because they are so specialized. Instead, it may be best to protect species, such as Arctic foxes, that are likely to have areas with future habitat impacts, but that fit the intermediate specialization type.

"I'm pretty optimistic about our species," Stigall says. "I think that fundamentally we can solve our way out of a lot of these problems, we just have to get the will to do it. Eventually we'll be all right; things will just be a little bit different."

The Virtual Fossil Atlas

As a young girl Stigall made do with A Golden Guide to Fossils, but she hopes that today's amateur fossil collectors and researchers will have at their disposal a more comprehensive guide. That's why she and her colleagues are creating an online database (www.ordovicianatlas.org) that will include identification keys, images, and distribution maps for some 850 ancient animal species, including brachiopods, trilobites, and other invertebrates. The project is funded by the National Science Foundation.

So far, the researchers are including in their database Cincinnatian fossils from the Cincinnati Museum Center, the Karl E. Limper Geology Museum at Miami University of Ohio, and the Department of Geological Sciences at Ohio University. They also are including fossils from the Pennsylvania period (323 to 299 million years old) from the University of Kansas and fossils from the Neogene period (23 to 2.6 million years old) from the University of Florida.

"The atlas is a wonderful tool for both amateurs and professionals," says Jennifer Bauer, a master's student who is working on the project. "Once the atlas is complete anyone can go fossil collecting in the regions we are focusing on and identify their specimens, down to the level."

Explore further: Rising mountains, cooling oceans prompted spread of invasive species 450 million years ago

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