The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …

Deformations formed in unconsolidated sediments are known as soft-sediment deformation
structures. Their nature, the time of their genesis, and the state in which the sediments …

The temporal link between large igneous province (LIP) eruptions and at least half of the
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …

Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …

The temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …

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 …

Most of the 16 papers in this special issue were presented at a session entitled “The
recognition of trigger mechanisms for soft-sediment deformation” at the 27th IAS Meeting of …

The role of ocean anoxia as a cause of the end-Triassic marine mass extinction is widely
debated. Here, we present carbonate-associated sulfate δ34S data from sections spanning …

Understanding the end-Triassic mass extinction event (201.36 Ma) requires a clear insight
into the stratigraphy of boundary sections, which allows for long-distance correlations and …

Soft-sediment deformation structures (SSDS) have been the focus of attention for over 150
years. Existing unconstrained definitions allow one to classify a wide range of features under …