CL
Climate: Past, Present & Future

Climate: Past, Present & Future

Detrital zircons: how the age of a resistant mineral can help to reconstruct the climate of the past

Detrital zircons: how the age of a resistant mineral can help to reconstruct the climate of the past

Name of proxy detrital zircon geochronology Type of record provenance proxy Paleoenvironment any sedimentary environment in a geologically diverse and diagnostic area Period of time investigated any Period of the geological timescale of the Earth, during which sedimentary deposits were formed   How does it work? Igneous rocks form through assemblages of minerals crystallising from melt. While ...[Read More]

How humans are influencing climate change and its significance in defining a new geological epoch: the Anthropocene

How humans are influencing climate change and its significance in defining a new geological epoch: the Anthropocene

The Anthropocene Working Group (AWG) is the body tasked to propose a formal definition for the Anthropocene as a geological time unit. Join us at the EGU2021 General Assembly on Wednesday 28th April at 14:15-15:00 CEST for a series of presentations on the Anthropocene in session SSP2.6.   The Anthropocene concept Geologists cope with the enormity of 4.5 billion years of Earth history by divid ...[Read More]

Generation #polarprediction

Generation #polarprediction

More than 11 years ago, I joined the Université catholique de Louvain (UCLouvain) in Belgium as a teaching assistant. The 2007-2009 International Polar Year (IPY), a worldwide collaborative effort aiming at better understanding our polar regions, had just finished, and the scientific community was concerned about the sudden drop in the summer Arctic sea ice extent that had occurred two years befor ...[Read More]

Presenting a new European loess map

Presenting a new European loess map

Loess is a silt-sized, aeolian sediment that was produced in large quantities in past geological eras of mid-latitude Europe and Asia, among others (Fig. 1). It is used in Quaternary science to infer about past climatic and environmental conditions. Generally, layers of loess formed during cold and dry periods, while soils formed within/on top the loess during warmer and wetter periods. These soil ...[Read More]