Bits of Geoscience

Tectonic response measured to 2010 Greenland melting record

To notice something is going on with the world’s ice sheets, you could measure melting water runoff, glacier retreat or use satellites and GPS to measure ice volume decline. Just like measuring sea level rise and temperature this all adds … Continue reading →

Drop in CO2 heralded the onset of Antarctic glaciation

For about 100 million years all sorts of animals roamed the then subtropical North and South poles. But then suddenly some 34 million years ago during the Eocene everything changed when temperatures fell dramatically in only a 100,000 year timespan, … Continue reading →

No reason to assume cold European winter ahead – too many sunspots

The cold winter of 2011-2012 that some meteorologists have predicted for Ireland, England, Scotland, France, Belgium, the Netherlands, Germany and Denmark is in fact to be called unlikely.

Life had a small surprise just after the end-Cretaceous mass extinction

You may have felt really lonely walking the face of Earth. Until you looked closer. [Btw: who needs peer-reviewed literature when you’ve got the annual festival of presentations at the Geological Society of America?]

Rare space radiation disasters may lead to extinction events – just how deadly is a two-month ozone hole?

Both supernovae and extreme solar flares can damage Earth’s ozone layer. But perhaps a black hole swallowing a neutron star somewhere not too far away gives a bigger punch – lasting a second or so.

Reefs took 1.5 million years to reappear after Permian-Triassic Mass Extinction

The Permian-Triassic Mass Extinction was the largest in our planet’s history. Enormous disruptions of the carbon cycle led to climate change, ocean acidification and ocean anoxia – and with an estimated 90 percent of all species dying out Earth almost … Continue reading →

Ice age riddle: what burped CO2 and wasn’t ocean or Neanderthal?

During the Earth’s ice ages the Pacific Ocean stored large amounts of carbon, which for some reason it released again close to the last glacial period’s end, warming the world and melting most of the icecaps. That is how the … Continue reading →