THE melting Greenland icecap may have caused the rise in sea level during the
last interglacial period 125 000 years ago, say researchers in the US. Sea
levels were then about five metres higher than today’s, but where the extra
water came from isn’t clear. The West Antarctic ice sheet was the main suspect,
because it is partly below sea level and prone to melt rapidly. But an analysis
of oxygen isotopes by Kurt Cuffey of the University of California at Berkeley
and Shawn Marshall at the University of Calgary shows Greenland was up to 8 °C
warmer, melting more…
To continue reading, today with our introductory offers
Advertisement
More from New Scientist
Explore the latest news, articles and features
Popular articles
Trending New Scientist articles
1
A quantum state that lasts forever may finally be within our grasp
2
Sperm have been made magnetic to allow IVF inside the body
3
Autism may have two distinct subtypes that vary by brain activity
4
The secrets to keeping your brain sharp in old age
5
Has the answer to life's origins been hiding in our cells all along?
6
Arctic Ocean reaches tipping point that could be dire for marine life
7
Fully autonomous drones have killed human soldiers for the first time
8
Walking shark found in Papua New Guinea is new to science
9
Autism and ADHD are on the rise due to widening diagnostic criteria
10
Understanding anorexia’s grip on the brain could unlock new therapies



