Tag Archives: paleoclimatology

Holocene climatic changes were local phenomena – except current warming

Of course you know these people that by now feel a bit cornered and say ‘okay, perhaps temperatures are going up. But that’s what it does, the global climate changes all the time.’ Well, to keep things simple: no, it … Continue reading →

Metastudy shows current climate change makes flora and fauna shrink

The paleoclimatic record shows it has happened before – and now two well-read researchers illustrate it is already happening again: species across life’s kingdoms are decreasing in size, due to warming, droughts and acidification. It’s a sign ecology is feeling … Continue reading →

Ice age riddle nr2: If Lake Agassiz drained at wrong time, what caused Younger Dryas?

In our first ice age riddle a couple of days ago we looked at the link between CO2 rise and ice retreat, after the last ice age had reached its max, some 18,000 years ago.

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 →

New evidence for bipolar seesaw link between Greenland and Antarctica – and abrupt climate variability

Glacials and interglacials on the northern and southern hemisphere somehow do not seem to correspond. This has led to a ‘thermal bipolar seesaw theory,’ whereby an off-mode in the thermohaline circulation leads to an ice age in Europe, but excess … Continue reading →

Eemian Greenland melting 55% warming, 45% solar and feedbacks – ice more stable now

Researchers of Utrecht University say the Greenland ice sheet may be more stable now than during the Eemian, the previous interglacial period, which lasted from 130,000-114,000 years BP. It turns out back then Arctic insolation was bigger – although still … Continue reading →

Threefold increase of dust led to -40 ppm CO2 Antarctic iron fertilisation during Pleistocene

An international team of researchers today in Nature explain the importance of dust storms for climate variability, not just for the radiative balance, but also for the Earth’s carbon cycle. For geoengineering minds: iron fertilisation at least seems to have … Continue reading →