
© National Oceanography CentreFieldwork in Spitsbergen.
Scientists are unravelling the environmental changes that took place around the Arctic during an exceptional episode of ancient
global warming.Newly published results from a high-resolution study of sediments collected on Spitsbergen represent a significant contribution to this endeavour. The study was led by Ian Harding and John Marshall of the University of Southampton's School of Ocean and Earth Science (SOES), based at the National Oceanography Centre, Southampton, United Kingdom.
Around 56 million years ago there was a period of global warming called the
Paleocene - Eocene Thermal Maximum (PETM), during which global sea surface
temperatures increased by approximately 5°C.
The warming of the oceans led to profound ecological changes, including the widespread extinction of many types of
foraminifera, tiny single-celled organisms with distinctive shells. Plankton that had previously only prospered in tropical and subtropical waters migrated to higher latitudes. Similar changes occurred on the land, with many animals and plants extending their distributions towards the poles.
"Although environmental changes associated with the PETM at low- to mid-latitude settings and high southern latitudes are well documented, we know less about these changes at high northern latitudes," explained Harding.