New Ohio University research
suggests that the rise of an early phase of the Appalachian Mountains
and cooling oceans allowed invasive species to upset the North American
ecosystem 450 million years ago.
The study, published recently in the journal PLOS ONE,
took a closer look at a dramatic ecological shift captured in the
fossil record during the Ordovician period. Ohio University scientists
argue that major geological developments triggered evolutionary changes
in the ancient seas, which were dominated by organisms such as
brachiopods, corals, trilobites and crinoids.
During this period, North America
was part of an ancient continent called Laurentia that sat near the
equator and had a tropical climate. Shifting of Earth's tectonic plates
gave rise to the Taconic Mountains, which were forerunners of the
Appalachian Mountains. The geological shift left a depression behind the
mountain range, flooding the area with cool water from the surrounding
deep ocean.
Scientists knew that there was a
massive influx of invasive species into this ocean basin during this
time period, but didn't know where the invaders came from or how they
got a foothold in the ecosystem, said Alycia Stigall, an Ohio University
associate professor of geological sciences who co-authored the paper
with former Ohio University graduate student David Wright, now a
doctoral student at Ohio State University.
"The rocks of this time record a
major oceanographic shift, pulse of mountain building and a change in
evolutionary dynamics coincident with each other," Stigall said. "We are
interested in examining the interactions between these factors."
Using the fossils of 53 species of
brachiopods that dominated the Laurentian ecosystem, Stigall and Wright
created several phylogenies, or trees of reconstructed evolutionary
relationships, to examine how individual speciation events occurred.
The invaders that proliferated
during this time period were species within the groups of animals that
inhabited Laurentia, Stigall explained. Within the brachiopods, corals
and cephalopods, for example, some species are invasive and some are
not.
As the geological changes slowly
played out over the course of a million years, two patterns of survival
emerged, the scientists report.
During the early stage of mountain
building and ocean cooling, the native organisms became geographically
divided, slowly evolving into different species suited for these niche
habitats. This process, called vicariance, is the typical method by
which new species originate on Earth, Stigall said.
As the geological changes
progressed, however, species from other regions of the continent began
to directly invade habitats, a process called dispersal. Although
biodiversity may initially increase, this process decreases biodiversity
in the long term, Stigall explained, because it allows a few aggressive
species to populate many sites quickly, dominating those ecosystems.
This is the second time that Stigall
and her team have found this pattern of speciation in the geological
record. A study published in 2010 on the invasive species that prompted a
mass extinction during the Devonian period about 375 million years ago
also discovered a shift from vicariance to dispersal that contributed to
a decline in biodiversity, Stigall noted.
It's a pattern that's happening during our modern biodiversity crisis as well, she said.
"Only one out of 10 invaders truly
become invasive species. Understanding the process can help determine
where to put conservation resources," she said.
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