Could South American Volcanoes Have Triggered Whale Extinctions?
Denver, Colo., USA: Today, increasing levels of carbon dioxide in the
atmosphere are warming up the planet. Climate change can disrupt the
balance of ecosystems and contribute to endangerment and extinction of some
species. New research suggests that a period of intense volcanism in the
Central Andes may be the missing link in the story of past climate changes
that led to the extinctions of ancient marine mammals. Mark Clementz and
Barbara Carrapa will present their findings at the GSA Connects meeting in
Denver tomorrow.
While we often hear about the important role human emissions of carbon
dioxide play in the climate today, much of our understanding of current and
future climate is rooted in Earth’s long history of variable climate. Many
factors affect the carbon cycle—with carbon moving between the atmosphere,
oceans, rocks, soil, and living things. Between 7.6 and 5.4 million years
ago, the planet experienced a period of rapid cooling known as the Late
Miocene Cooling Event. This was accompanied by massive changes to plant and
animal communities both on land and in the oceans. Until recently, the
cooling was attributed to carbon dioxide drawdown from the atmosphere by
silicate weathering of the Himalayas.
Clementz and Carrapa propose a different contributing factor—a major
increase in volcanism in the Andes around seven million years ago. They
explain that the Andes were positioned to deliver ash to both the Pacific
and Atlantic oceans—providing nutrients to global oceans that spurred an
explosion of life. Small marine organisms called diatoms used these
nutrients to thrive, and in turn, the marine mammals that fed on them, like
baleen whales, also thrived. Given their massive size, large numbers of
marine mammals could store a lot of carbon. By excreting their waste in
shallow water, whales cycle nutrients back into those diatom communities,
and the cycle continued to create what is known as a “biogenic bloom”—an
explosion of life.
“But it may have been a case where they contributed to their own death,”
explains Carrapa. Too many nutrients in the water can lead to toxic algae
blooms, one possible stressor that contributed to the extinctions that
followed this period of blossoming life. Another possibility is that ash
from ongoing volcanism could have poisoned the air. Clementz and Carrapa
plan on future work to look for evidence that might distinguish between
these possible drivers of extinction. The observed increases in biological
productivity may have contributed to cooling and extinction by altering
important shallow marine habitats.
While volcanoes emit carbon dioxide into the atmosphere, the story of past
carbon cycling pieced together by Clementz and Carrapa suggests that under
some conditions, volcanism could actually induce net decreases in
atmospheric carbon.
Rising from the Ashes: Linking Andean Volcanism, Diatoms, and Marine
Mammal Diversity and Extinction with the Late Miocene Cooling Event
Tuesday, 11 October 2022, 8:45 AM–9:00 AM
Author contact: Mark Clementz, mclemen1@uwyo.edu
https://gsa.confex.com/gsa/2022AM/meetingapp.cgi/Paper/377962
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