June 4, 2018, Max Planck
Society
Chemical analysis of the remains
of rats from archaeological sites spanning the last 2000 years on three
Polynesian island systems has shown the impact of humans on local environments.
The analysis by an international team of scientists allowed the researchers to
reconstruct the rats' diets—and through them, the changes made by humans to
local ecosystems, including native species extinctions and changes to food webs
and soil nutrients.
The Earth has entered a new
geological epoch called the Anthropocene, an era in which humans are bringing
about significant, lasting change to the planet. While most geologists and
ecologists place the origins of this era in the last 50 to 300 years, many
archaeologists have argued that far-reaching human impacts on geology,
biodiversity, and climate extend back millennia into the past.
Ancient human impacts are often
difficult to identify and measure compared to those happening today or in
recent history. A new study published in the Proceedings of the National
Academy of Sciences by researchers at the Max Planck Institute for the
Science of Human History in Jena and the University of California, Berkeley
advances a new method for detecting and quantifying human transformations of
local ecosystems in the past. Using state of the art methods, researchers
searched for clues about past human modifications of island ecosystems from an
unusual source—the bones of long-dead rats recovered from archaeological sites.
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