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.
By Geological Society of America
