This article presents a current (as of September 2019) list of recommended ages for proven
terrestrial impact structures (n= 200) and deposits (n= 46) sourced from the primary …

The~ 180-km-diameter Chicxulub peak-ring crater and~ 240-km multiring basin, produced
by the impact that terminated the Cretaceous, is the largest remaining intact impact basin on …

On November 5–8, 2019, the “Mars Extant Life: What's Next?” conference was convened in
Carlsbad, New Mexico. The conference gathered a community of actively publishing experts …

The Chicxulub crater was formed by an asteroid impact at ca. 66 Ma. The impact is
considered to have contributed to the end-Cretaceous mass extinction and reduced …

Quantitative insights into the geochemistry and petrology of proximal impactites are
fundamental to understand the complex processes that affected target lithologies during and …

Target lithologies and post-impact hydrothermal mineral assemblages in a new 1.3 km deep
core from the peak ring of the Chicxulub impact crater indicate sulfate reduction was a …

There is a growing concern that many important ecosystems, such as coral reefs and tropical
rain forests, might be at risk of sudden collapse as a result of human disturbance. At the …

This study presents a new classification of a∼ 100-m-thick crater suevite sequence in the
recent International Ocean Discovery Program (IODP)-International Continental Scientific …

High energy streams of rock ejected from the Schrödinger impact basin carved two canyons
in the lunar crust that are comparable in size to the Grand Canyon of North America. Here …

The Chicxulub impact event at ca. 66 Ma left in its wake the only complex crater on Earth
with a preserved peak ring, characterized by a well-developed magnetic anomaly low. To …