Extinction and anoxic events

An extinction event is a sharp decrease in the diversity and abundance of macroscopic life. Major extinctions are generally caused by a combination of phenomena such as e.g. large-scale volcanism, climate and sea level change and meteoritic impacts. During mass extinctions, it has been observed that the middle and even the upper layers of the ocean may become deficient or totally lacking in oxygen, a process known as oceanic anoxic event. Although such events have not happened for millions of years, the geological record shows that they occurred many times in the past and that they played a major role in mass extinctions. Based on a multidisciplinary approach our research is aimed at better understanding the dynamics of mass extinctions, and, in particular, of oceanic anoxic events.

Major extinction events. In this long-term project, we investigate major catastrophes in Earth’s history in the broadest sense, including meteorite impacts and episodes ...

Environmental change from Egyptian Paleogene sediments. The Early Cenozoic is marked by two important episodes of environmental change: the Cretaceous ...

Phosphorus and carbon burial during anoxic events. In this project we investigate the oceanic anoxic events near the Cenomanian/Turonian (OAE2) and Coniacian ...

 

 

Research group

Head
Thierry Adatte

Master student
Valentin Sordet

Technical staff
Tiffany Monnier

Géopolis - CH-1015 Lausanne
Switzerland
Tel. +41 21 692 43 06
Fax +41 21 692 43 05