Dear climate enthusiasts, EGU lovers, and early/senior climate scientists, With #EGU22 approaching, we wanted to give you a quick overview of the great short courses and great debates that are planned for this years’ General Assembly! If you want to learn more about the scientific sessions offered, please have a look at our Seasonal love letter from December. Short Courses If you are about to fini ...[Read More]
Previous blog posts have highlighted the importance of loess as an indicator of climate and environmental changes in the past. These posts showed the relevance of loess deposits as archives of Pleistocene climates and environments, the importance of using novel approaches in mapping these and other Quaternary-related sediments, the aspects of dating loess deposits, as well as the peculiarities o ...[Read More]
1950 CE is known as the year zero in the so-called ‘BP time scale.’ The BP stands for, “Before Present,” and has its roots in the development and conventions of radiocarbon dating [1]. The radioactive isotope of carbon (14C) with a half-life of 5700 years [2; 3] is a cosmogenic isotope produced in the atmosphere by secondary cosmic rays (SCR). Thermal neutrons, the SCR particle responsible for the ...[Read More]
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]
