Publicaties
Moderately volatile elemental and isotopic variations in variably shocked equilibrated ordinary chondrites from Antarctica Vrije Universiteit Brussel
Volatile elements, crucial players in planetary evolution, condense at low temperatures from solar nebula. Despite extensive past research, gaps remain in understanding the volatile budget establishment and depletion mechanisms during the early stages of Solar System formation. This study investigates the role of shock events on multiple isotope systems in H6 ordinary chondrites with varying shock and weathering degrees. In this study, we ...
A new insight of the MIS 3 Dansgaard-Oeschger climate oscillations in western Europe from the study of a Belgium isotopically equilibrated speleothem Vrije Universiteit Brussel
The Marine Isotope Stage (MIS) 3 records abrupt transitions from cold stadial to temperate interstadial climate conditions, termed Dansgaard-Oeschger (DO) events. Reconstructing these rapid climate changes is crucial for documenting the prevailing climatic conditions in Europe during the extinction of the Neanderthals. However, only few continental records are available to define the continental climatic responses to DO changes. Here, the ...
The Ostracod Clumped-Isotope Thermometer: A Novel Tool to Accurately Quantify Continental Climate Changes Vrije Universiteit Brussel
Astronomically paced climate and carbon cycle feedbacks in the lead-up to the Late Devonian Kellwasser Crisis Vrije Universiteit Brussel
Astronomically paced climate and carbon cycle feedbacks in the lead-up to the Late Devonian Kellwasser Crisis Vrije Universiteit Brussel
Spatial and temporal variability of environmental proxies from the top 120m of two ice cores in Dronning Maud Land (East Antarctica) Vrije Universiteit Brussel
Hot carbonates deep within the Chicxulub impact structure Vrije Universiteit Brussel
Comprehensive report of the BELARE 2022-2023 meteorite reconnaissance expedition in the Sør Rondane area, East Antarctica Vrije Universiteit Brussel
Geochemical characterization of scoriaceous and unmelted micrometeorites from the Sør Rondane Mountains, East Antarctica: Links to chondritic parent bodies and the effects of alteration Vrije Universiteit Brussel
Micrometeorites originate from the interplanetary dust complex and continuously fall to the Earth's surface in large amounts. About 10 to 20% of micrometeorites are not melted upon reaching the Earth's surface, preserving the primary features and characteristics of the parent material. Consequently, unmelted micrometeorites, together with scoriaceous micrometeorites, an intermediate form between cosmic spherules and unmelted micrometeorites, ...